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Hawaii Charity - Education, Culture, Nature, Environment
No matter who you are, or what your interest, the islands of Hawai'i will make the corners of your mouth curl up with endless adventure, excitement, exploration and fun. Wander through some of America's most beautiful spots, take a stroll through one of the many sacred heiau grounds, search for shells on pristine beaches, or climb up a volcano and stand above the clouds. Discover your heritage within our islands own. So much of what makes America great is right here in Hawai'i. The culture, art and folklore of Hawaii's past make enchanting lessons in history and life. Help us continue to preserve and conserve the things that make Hawai'i unique and beautiful; because there is only One Hawaii... One Hawaii is the charitable wing of Hawaiian Style Organiation LLC that supports the Conservation & Preservation of the Hawaiian Islands both Culturally and Naturally. Hawai'i is the most remote place on earth, and one of the most magical to all who visit it. Together we can work together, through Education, Charitable Acts, and our own time to help keep Hawaii what it is; a sacred land rich in beauty and culture... a place where Aloha is more than a word, but a way of life.
Help us continue to preserve and conserve the things that make Hawai'i unique and beautiful; because there is only One Hawaii...
Friday - August 01, 2008
Vog damages Big Island crops
On July 31 a disaster declaration was approved which would allow Big Island farmers to apply for low interest loans to cover losses they sustained due to volcanic gases emitted by Kilauea Volcano. Vog is created when sulfur dioxide released by the volcano mixes with sun and dust. This dangerous mix is currently blanketing the Kau District south of the volcano and drying out crops. Protea (pictured on the right) and other flower farmers are particularly susceptible.
The low interest loans to be offered by the government would allow coverage of up to 100 percent of production or up to $500,000 in physical losses.
Vog has affected all of the Hawaiian Islands' air quality to varying degrees since a new vent opened up in Kilauea's Halema'uma'u Crater in Hawaii Volcanoes National Park.
Thursday - July 31, 2008
Snorkeling spots on Maui closed
Beginning Aug. 1, a portion of the Ahihi-Kinau Natural Area Reserve will be closed for two years to allow the land to recover from damage caused by overuse. Trails to popular snorkeling spots Kalaeloa, known as the "Aquarium," Mokuha, also known as the "Fishbowl" and the trail to Kalua o Lapa (cinder cone area) will be closed. These areas have long been sore spots for preservationists and residents who witness damage to these fragile ecosystems due to excessive use. Those spots that will remain open are Waiala Cove and the coastal area along Ahihi Bay and the "Dumps" surfbreak. La Perouse Bay and areas outside the reserve are also not affected.
About 100 signs will be posted to let visitors know which areas are restricted. Reserve staff and rangers will also be out in increased numbers to monitor the situation.
Sunday - June 29, 2008
Hana Bay gets a face lift
Hana Bay's crumbling pier will soon be a thing of the past. A $20 million project to replace the damaged structure is scheduled to begin in the near future. An additional $3 million has been allotted for a new boat launch as well. These funds were part of a larger $118.3 million bill primarily aimed at renovating the Kahului Harbor over the next six years which was signed into law in late June.Part of the improvements include repairing the breakwater, installing a loading dock and building a boat wash-down area. One of the primary concerns in repairing the pier is keeping a life line open between Hana and nearby residents in case another earthquake like the one in 2006 should cut them off from the rest of the island. The pier would also be useful in bringing in supplies and equipment that cannot traverse the long and windy Hana Highway.
For more information on the Hana Highway or to plan a trip to visit the lovely Hana see our Road to Hana Highway Mile by Mile.
Saturday - March 08, 2008
Lava heads to the ocean
After months of sticking inland, the lava flows from Kilauea Volcano on the Big Island have begun another journey to the sea. The lava is marching toward Royal Gardens Subdivision, an area that was largely buried in lava in 1983.
Officials opened a pedestrian viewing area off Highway 130 in Puna this weekend to accommodate the crowds which are eager to see the goddess Pele at work. The viewing area should be about one quarter mile away from the spot where lava is entering the ocean.
Rangers and officials will monitor the path of the lava daily to ensure that the area is still safe for visitors.
There are several inherent dangers to lava viewing which visitors must be aware of. Fumes or VOG (volcanic gases) can cause problems for people with respiratory and heart conditions as well as pregnant women and children. The lava creates a bench when it enters the ocean. This bench can collapse at any time without warning causing serious injury or death to those reckless enough to venture that close. Always stay within Hawaii Volcanoes National Park designated areas for lava viewing.
Saturday - March 08, 2008
Pi’ilani Highway beyond Kipahulu open by October
County officials in Maui announced this week that the Pi'ilani Highway beyond Kipahulu should be reopened by October 2008 allowing residents and visitors to travel the direct route from Hana to Upcountry. The road was closed in December 2006 due to damage from two severe earthquakes which shook Hawaii on October 15, 2006. Rock slides and undermined roads were the main reasons for the closure. The final project, rock stabilization and road repair at Kalepa and Alelele, is out to bid for the county.
Please check back for further updates.
Silverswords of Hawaii
This unusual plant, unique to Haleakala on Maui and Mauna Kea and Mauna Loa on the Big Island of Hawaii, has thoroughly adapted to the harsh environment of its home. What's even more fascinating is that each volcanic mountain has it's own unique type of silversword. The Haleakala species is unique to all the world on Maui and is considered by many to be the most beautiful. The bloom stalk of the silversword is a true sight to behold, often several feet tall with a hundred or more purple flowers. What makes the blooming of a silversword even more special is that the plants live from 15 to more than 50 years but bloom only once and die. If you see one in bloom, take a moment to realize how unique that opportunity really is.
In the not so distant past on Maui there were so many silverswords on Haleakala they covered the ground like a blanket of snow, but because of livestock and visitors snapping portions for souvenirs, this amazing plant almost became extinct.
In 1927, barely 100 plants were alive on the slopes of Haleakala. It was ultimately the creation of Haleakala National Park that saved the silversword. The protection and work of several dedicated groups have brought them back from that low in 1927 to more than 40,000 today. But even now, the silversword is at risk in its fragile environment, so please let these amazing plants live in peace. Don’t touch or even walk near them, as you could damage their very delicate root structures.
More Information: Argyroxiphium (Silverswords) at Wikipedia
In 1927, barely 100 plants were alive on the slopes of Haleakala. It was ultimately the creation of Haleakala National Park that saved the silversword. The protection and work of several dedicated groups have brought them back from that low in 1927 to more than 40,000 today. But even now, the silversword is at risk in its fragile environment, so please let these amazing plants live in peace. Don’t touch or even walk near them, as you could damage their very delicate root structures.
More Information: Argyroxiphium (Silverswords) at Wikipedia
Hawaii Names converted from English
Our Hawaiian to English names translation page has been combined into an easy to download PDF document. The list of Hawaii names is extremely long and thorough (we'd hate to leave anyone out) and it's easy to download/view in a PDF document. Please make note that this translation is for FUN only. The names used in Hawaiian culture often have meaning, and should not be used lightly or carelessly. Find your name and use it in a respectful manner. Enjoy, have fun, and Mahalo!
DOWNLOAD: Hawaii Names translation chart (48 pages)
Hawaii Culture and Heritage
Hawaii's cultural environment is the result of layer upon layer of various cultural groups. The culture of Hawai'i is arguably one of the strongest remaining in the world, and certainly within the United States. The culture and practices of the Hawaiian people remains very evident on the islands, even though the Hawaiian race itself has become diminished and "diluted" over the years - few pure blood Hawaiians remain in the general population. Remnants of New English culture remain, though not nearly to the degree of early Asian immigrants who came to work in the sugar cane fields in the early 20th century. Additionally, Polynesian influence in the islands is strong as one might expect. Today Hawaii is a truly a melting pot of many cultures, beliefs, and heritage.
The arts are of high interest in the islands, either in the form of music, photography, hula dance, or art. Galleries for art and photography are prominent throughout the islands, music has worked its way around the globe and into several major movies (thanks to the late Israel Kamakawiwo'ole - Brother IZ), and the hula is world renown. Appreciation of classical, modern, and experimental art forms is evident in attendance figures at galleries, concerts, legitimate theater performances, and museums. Many ethnic groups preserve the traditions of their ancestors by combining or modifying music and dance forms.
Since the preservation of the culture and heritage is very important to the people of Hawaii, an assortment of cultural and scientific institutions present a wide variety of opportunities for the appreciation and understanding of the fine arts, history, traditions, and sciences of the Hawaiian people.The Bernice P. Bishop Museum, founded in 1889 in Honolulu, is a research center and museum dedicated to the study, preservation, and display of the history, sciences, and cultures of the Pacific and its people. The Honolulu Academy of Arts, one of the finest in the world, boasts a spectacular collection of Western art, including works by the late 19th- and early 20th-century masters Monet, van Gogh, Matisse, Gauguin, and Picasso. The collection of Asian art found in the HAA is also some of the finest in the Western world.
The active art, music, and drama departments in Hawaiian schools and colleges and at the University of Hawaii contribute to the expanding cultural life of Hawaii, while the state has several theater organizations, professional and amateur. Hawaii remains the only state in the United States with two official languages, English and Hawaiian. As of late, the Hawaiian language is taught frequently in schools and the once nearly "dead" language has seen a revival.
Hawaii has two National Parks - Hawaii Volcanoes National Park, on the island of Hawaii, and Haleakala National park, on Maui, as well as the much-visited U.S.S. Arizona Memorial in Pearl Harbor. Additionally there are many other Federal Preserves, Walkways, Historic Sites, etc. There are also many state and county parks, including the popular Waimea Canyon State Park on Kauai - home to the "Grand Canyon of the Pacific," as Mark Twain called it.
The Hawaiian islands are also home to some of the most fascinating heiau (temples) that remain in the United States. Unfortunately, many of these heiau were destroyed when the ancient kapu system was abolished late in the 19th century and when the early missionaries arrived shortly thereafter. The largest intact heiau in the state, Pi'ilanehale Heiau, was rediscovered in the 1970's on Maui just outside of Hana town. Today all visitors and residents alike can visit this monumental structure.
Surfing originated in ancient Hawaii and is now practiced at some 1,600 recognized surf spots throughout the islands. Holua was a popular game of the ancient ali'i (royalty), involved a sled, and was incredibly dangerous. You can read more about Holua at Hulihe'e Palace.
Additional Resources
You may also want to read our History of Hawaii and Hawaiian language articles.
The active art, music, and drama departments in Hawaiian schools and colleges and at the University of Hawaii contribute to the expanding cultural life of Hawaii, while the state has several theater organizations, professional and amateur. Hawaii remains the only state in the United States with two official languages, English and Hawaiian. As of late, the Hawaiian language is taught frequently in schools and the once nearly "dead" language has seen a revival.
Hawaii has two National Parks - Hawaii Volcanoes National Park, on the island of Hawaii, and Haleakala National park, on Maui, as well as the much-visited U.S.S. Arizona Memorial in Pearl Harbor. Additionally there are many other Federal Preserves, Walkways, Historic Sites, etc. There are also many state and county parks, including the popular Waimea Canyon State Park on Kauai - home to the "Grand Canyon of the Pacific," as Mark Twain called it.
The Hawaiian islands are also home to some of the most fascinating heiau (temples) that remain in the United States. Unfortunately, many of these heiau were destroyed when the ancient kapu system was abolished late in the 19th century and when the early missionaries arrived shortly thereafter. The largest intact heiau in the state, Pi'ilanehale Heiau, was rediscovered in the 1970's on Maui just outside of Hana town. Today all visitors and residents alike can visit this monumental structure.
Surfing originated in ancient Hawaii and is now practiced at some 1,600 recognized surf spots throughout the islands. Holua was a popular game of the ancient ali'i (royalty), involved a sled, and was incredibly dangerous. You can read more about Holua at Hulihe'e Palace.
Additional Resources
You may also want to read our History of Hawaii and Hawaiian language articles.
Hawaii Plants and Animals
Thousand of miles from the nearest continent the volcanic mountains of Hawai'i stood somber and alone in the Pacific, void of nearly all life. Lifeless they would remain if not for the birds, the currents, and the wind. Seeds were carried by the tides that washed across the shores. Storms brought more seeds with their howling winds and rains. The birds, like the small golden plover, brought the rest. Birds would fly from as far as 3,000 miles away, non-stop.Eventually the Hawaiian islands would be covered with extensive forest habitats, shrubbery, and grasslands. Soil and precipitation differences around the islands would cater to all kinds of plant-life. In time, the foreign species would become unique to all the world, found only in Hawai'i.
Today, we call them endemic Hawaiian species like the Nene (Hawaiian goose) and silversword (which is actually a relative of the sunflower). You will find them no where else on the planet. These species had thousands, if not millions, of years to develop into unique flora and fauna.
For thousands and thousands of years they were undisturbed by the ways of humans. Today, many of these species are not so lucky. The 'Akiapola'au (a rare bird found on the Big Island of Hawai'i) is just one example of a species that is fading fast. Most experts predict that their numbers have dwindled to between 1,000-1,500. We were very fortunate to see one as recently as 2006, so perhaps hope still remains for this incredible bird.
It is easy to foget that Hawai'i is much more than just the major islands in the eastern portion of the chain. The Hawaiian archipelago stretches for some 1,600 miles to the north and west, and here you'll find 84 million acres that are home to 7,000 species of birds (especially sea birds), fish and marine mammals, at least a quarter of which are unique to Hawai'i. In 2006, the President officially designated the Northwestern Hawaiian Islands a Marine National Monument creating the largest marine protected area in the world.Food plants grown commercially (or in backyards for home consumption) in Hawai'i include sugarcane, pineapples, papayas, bananas, mangoes, guavas, lichee, coconuts, avocados, breadfruit, macadamia nuts, limes, passion fruit, taro (for poi), and tamarinds.
Wild animal life in Hawai'i includes mongooses (yes that's plural), rats, frogs, toads, and, in the more remote regions of some of the islands, deer, sheep, pigs (boar), donkeys, and goats. On the Big Island, even wild horses roam freely in Waipi'o Valley.
The insect population is multitudinous, and marine life abounds in Hawaiian waters.
Hawai'i also strugles with the many invansive species which have been brought to the islands over the years. This primarily involves plant life, but is most noticeable in the animal populations. The coqui on the Big Island, brought accidently from Puerto Rico, are literally driving many residents out of their minds. The over population of jungle fowl (also known as Chickens) on Kaua'i is definitely noticeable, as is Kauai's lack of mongoose. Mongoose eat eggs of ground nesters, controlling moa (fowl) population. Kauaii never got their mongoose. Legend has it that a mongoose bit a dock worker, got thrown off the dock, and never made it to the island. Mongoose exist on all of the other major Hawaiian islands, as do the rats (also non-native) that they mongoose were imported to kill. One can see how things quickly get out of hand when animals are introduced to a new environment like Hawai'i.
Eclectic Hawaii - Like no other
Hawaii is a land of diversity, a land of much beauty and of many contradictions. Mother Nature pulled out all the stops when forming this place. And the life that has since inhabited these green gems is as diverse as the entire world itself. From lush rainforests to barren deserts, Hawaii is as eclectic a place as you'll ever visit. A favorite get-away for people around the world, Hawai'i has become famous for its miles of beaches, erupting volcanoes, lush rainforests, and exotic flora and fauna. Let's take a look at what makes Hawaii like no place else on earth.Older than Time / Younger Than You
All good things take time. Hawai'i's existence is no different. The islands likely began their journey upward from the seafloor some 70 million years ago, before even the dinosaurs met their end. These islands have been springing up from the sea in assembly line fashion, moving to the north and west on the earth's crust over time, eventually sinking below the Aleutian Islands in Alaska. But as old as the islands are, many hundreds of acres on the island of Hawai'i are likely younger than you are. So young in fact that even if you were born today some of the earth there would be newer than you still. And in another 50,000 years or so a new volcano will likely pop above the waves. Two dozen miles off the southeast coast of the Big Island of Hawaii, Lo'ihi continues its ascent to become the next Hawaiian island.
Lost World / New World
When Michael Crichton wrote his book famously entitled, "The Lost World," many people had flashbacks to “Jurassic Park.” If you've ever watched the show "LOST" on ABC, you might call it a "lost world.” Perhaps this is all more than just ironic. The “Jurassic Park” movies were, of course, filmed on Kauai, and "LOST' is filmed on Oahu. Such visions of a lost world were very real just a short time ago. Hawaii was the true "lost world" until around 2000 years ago. While much of the planet was inhabited by peoples far and wide, Hawai'i stood alone in the middle of the pacific for millions of years. Hawaii is approximately 2,000 miles from the nearest continent. Some 65-million square miles of open water surround the islands without interruption.
Even after the original settlers from the Pacific discovered and inhabited Hawaii, it wasn't another 1700 years that "modern" man would discover the islands. Captain James Cook stumbled upon the islands in 1778. The rest, as they say, is history.
Hot and Cold, Wet and DryConsidering there are 13 climate zones in the world, you'd probably assume Hawaii fell into a single category or two; something in the tropics perhaps? Try 11 – that’s not a typo – ELEVEN!
No place on earth is quite as diverse as Hawaii when it comes to climate and weather on such a small geographical area. From barren lava desert on the leeward side of select islands to lush rainforest directly on the other, you'd think you were in two separate parts of the world. Mauna Kea and Mauna Loa on the Big Island of Hawaii, and even Haleakala on Maui can been seen with a white snowy cap during several months in the winter. Down below the water is a warm 76 degrees. There aren't a lot of places you can surf and ski in the same day.
Consider also that select locations receive but a few inches of rain a year, as in 10 inches or less. Other parts of the islands receive upwards of 440 inches of rain a year. In Wai'ale'ale Crater on the island of Kauai, an average yearly rainfall of 440-470 inches is not uncommon - making it the wettest spot on earth. Hilo, the second largest city in the state, located on East Hawaii, is the wettest city in the United States. Just over 30 miles away, on the western flank of Kilauea exists the Ka’u Desert.
Big and yet so Small
At one end of the chain the mountains reach nearly 14,000 feet above sea level, their peaks often capturing snow during the winter. On the other end of the chain, some 1,600 miles away, many of the oldest Hawaiian Islands barely scratch the surface of the waves that relentlessly pound away at their ever shrinking shores. Even Kauai, the oldest of the main Hawaiian Islands, likely used to reach up to 5,000 foot higher into the clouds then even Mauna Loa and Mauna Kea do today. But five million years of wave action, wind, and erosion have reduced it to a peak of only 5,200 feet at Kawaikini. Over time the Hawaiian Islands will all suffer the same fate and sink beneath the blue ocean once again.
In total area, the seven major islands rank in at number 43 amongst the United States, one of the smallest. When considering only land area, they're a smaller 47th. But if one considers all of the Hawaiian Islands stretching 1,600 miles out into the Pacific, all legally part of the state of Hawaii, and if you include their territorial waters, you might be surprised that you'd have an area more than TWICE the size of Alaska. Move over Alaska, California, and Texas, you're not so big anymore.
Two Fish and some BreadIt's hard to take a little bit of anything and turn it into a lot. But Hawaii isn't playing by the same rules. Here there are some 6,000 birds, plants, sea creatures, and insects found nowhere else on earth. They are endemic to Hawaii and have evolved here and only here. From a few hundred seeds flown in by the birds, blown in by wind, and carried by the currents - Hawaii has bloomed with extraordinary flora. The fauna evolved too, especially the birds, creating some of the most amazing honey creepers found in the entire world. Many are rare or endangered today - many more have already gone extinct. It is important that visitors and locals alike band together to protect these priceless forms of nature. Since the arrival of man, thousands of exotic plant and animal species have been introduced, and many are invasively evasively taking over the true natives.
Hawaii Tourism Statistics
If it's Hawaii tourism data you're looking for, then you're in the right place. We'll cover the latest tourism trends on the Hawaiian islands and provide a series of graphics and summarized data to give you a good idea of what's happening by the numbers.Using 2005-2007 statistics from the tourism authority in Hawaii we can present the following data. The graph seen here (to the right) shows the Total ARRIVAL Data in 2007 to each island (including multi-destination/island arrivals). You can also view the 2006 data graph. A pie chart is not truly the best format to display the visitor totals for the various islands as the number of visitors shown in the chart is greater than the true total, as many visitors go to more than one island. However, for our purposes, it should give you an idea of how many visitors (percentage wise) are arriving/visiting each island. Just keep in mind the actual arrival numbers are "inflated" a bit. A more accurate way to look at this is Visitor Days per island. You can view a chart of the Total Visitor Days per island as well. The percentages are what's important here, and you can see they do not change very much.
The tabular chart shown further below (you can click the box to enlarge it) gives the breakdown of visitors in the islands on a month by month basis (color coded per island). The bold lines that are clearly visible are the 2007 data trends. The faded "background" lines which almost looks like shadows of the darker lines are the 2006 trends. As you can see, 2007 was a better year overall for the Big Island of Hawaii, Maui, and Kauai, but on Oahu, travel dropped in 2007 in comparison with 2006. That is the second consecutive year that travel on Oahu has dropped while overall visitation has increased on the other islands.
In considering the "health" of the tourism market, one must also put emphasis on the two factors that are the most important: "visitor days" and "visitor expenditures." Mahalo for the tip by amberloo at TripAdvisor. In her words, "If there are more visitor days and more money being spent annually over the long-term, the industry is healthy regardless of any other factors; such as mere arrival totals. The goal of many government planners is to increase "days" and "spending" while limiting (or even decreasing) arrival counts."
Why limit arrival counts you might ask? One has to consider tourism "capacities" of the islands and how that will effect future trends. Maui and O'ahu likely reached their carrying capacity (for visitors) years ago, thus have few remaining competitive development opportunities and will not have the statistical fluctuations or upside growth potentials seen on Kaua'i. In fact, due to growth in 2007, Kaua'i has now about reached its own carrying capacity pending completion of on-going development in areas like Po'ipu.
2007 Tourism Authority Final Report
For the full year 2007, total visitor days decreased 1.6 percent, while total arrivals dipped 1.2 percent to 7,368,048 visitors. The average length of stay was virtually unchanged at 9.15 days. Visitors from Canada grew 5.3 percent and arrivals from the U.S. West rose slightly (+.1%), but there were fewer Japanese (-3.5%) and U.S. East (-3.3%) visitors compared to 2006.
"Hawai‘i's visitor industry remained stable in 2007 especially coming off of two robust years of growth," said State Tourism Liaison, Marsha Wienert. "We continue to be encouraged by the increase in visitor spending, as well as ongoing growth in the number of visitors from markets such as Canada, Hawaii's fourth largest market, and the strong performance of Hawai‘i's cruise industry."
Individual Island Data (See chart for reference)
The statistic below are "arrival" data - meaning visitors who arrived in the islands (either from the mainland US, abroad, or from another island). When viewing these statistics, we encourage visitors to keep the geographic size of the islands in mind. For example, the Big Island and Kauai have very similar trends in arrivals. However, the Big Island is significantly larger than Kauai (in fact, it is larger than all of the other islands combined) so numbers alone cannot tell the complete story. Kauai and the Big Island may very well have the exact same number of visitors any given month, but the size of the island will also determine how "crowded" it feels.
The Big Island of Hawaii, the largest in the chain typically ranges between 100,000-150,000 arrivals each month. These numbers were generally higher in 2007 in comparison to either 2006 or 2005. Excluding the summer "hump" felt through all the islands, the number of arrivals fluctuates much less than some other islands in the chain, so visitation is usually about the same in Hawai'i. Spring visitation was notably higher in 2007 when compared to 2006 and Fall visitation was notably lower. The events we noted on the best time to travel to Hawaii page, that are held each spring and fall, can increase visitor ratios on the island.
Maui, the second largest island in the chain, typically ranges between 175,000-250,000 arrivals each month. On some years Maui's arrival numbers bounce around a good bit throughout the year, but in 2007 they remained fairly constant. The summer "hump" is by far the largest period of arrivals, but there are also significant spikes at other times during the year, most notably around the Christmas holidays. Maui also saw more arrivals in 2007 than either 2006 or 2005. March has the largest notable increase in 2007, while December had the most notable decrease.
Kauai, the fourth largest island in the chain, typically ranges between 95,000-120,000 visitors each month. Kauai, in general, is a much quieter island (arrival wise) when compared to the likes of the other islands in the chain. But that may be due to its size and "theme" (all things green). The summer "hump" is the only really busy time on the island, though it's not as distinct as the "hump" Maui and Oahu experience. Kauai, like Maui and the Big Island, saw higher arrival numbers in 2007 than previously in either 2006 or 2005. It is also clear the Kauai saw a notable increase in Spring and early Summer 2007 traffic when compared to 2006.
Oahu, the third largest island in the chain, typically ranges between 350,000-450,000 visitors each month. As you can quickly see, that number quickly dwarfs the other islands arrival data. Oahu is widely popular with visitors abroad, and given that 75% of the state's population lives on this single island, the arrival data can skew accordingly. Oahu's numbers were down in 2007 in comparison to 2006, but Oahu remains the most popular island of choice for many visitors. The drop in visitation, as noted, has now happened twice in a row over the last three years.
Molokai and Lanai only make up 2% of all visitor arrivals combined. If you're heading to the islands, we suggest you look at the detailed statistics provided on the Hawaii government page linked above.
More Information: Hawaii Weather page or Selecting a Hawaiian island to visit
If you want even more detailed tourism specifications, please visit the Hawaii Department of Business, Economic Development & Tourism.
Hawaii Must See and Do
OK, let's get right to it - the very best of the Hawaiian islands. If you're like most visitors, you probably want to know the highlights first, the rest later. Or maybe you don't have three months to spare perusing your way around each island, who does right? Most visitors have a few days to a few weeks at most. So we've given a lot of thought to what places would make the highlight real of Hawaii, the top 10 places for each island, with a few honorable mentions to follow up. It's not to say there aren't a few dozen other great stops on each island, we just think these are the very best. Hopefully if you have only a day or two on a particular island, these lists will help you get right to the good stuff.
Hawaiian Style Star Ratings
If you've found this page you've likely wondered what all those star ratings mean around our website (and in our guidebooks) . So let's go over the basics of our rating system.
First, there are two types of ratings. Our Ratings (Hawaiian Style) and Visitor Ratings (your and fellow travelers ratings).
Each spot has a rating (1-5 stars; 5 is best):
- Avoid or Kapu
- Poor
- So-So
- Good
- Excellent
- Must SeeBy default Our Rating shows up at the top of each spot on the right. But in the event we haven't rated a spot yet, then the Visitor Ratings will show up in its place. The visitor rating also shows up further down the page, right above the comments section.
None of OUR (staff) ratings has been influenced by anyone or anything other than what you will see/experience at each spot. If we liked the place, we’ll tell you we liked it, and if we didn’t, you’re going to know about that too. You’ll know what to expect at each spot. We have found that this feature has been very useful for time-strapped travelers.
Visitor ratings are limited to one vote per person, per spot. Please be sure to cast your vote for the places you've visited and also share your thoughts in the comments section on each page.
Our guidebooks of course only contain Our Ratings. Visitor Ratings do not bear any weight in our guidebook materials.
Aloha,
John and Natasha Derrick
Hawaii Geology and Geography
So you want to know what makes a Hawaiian island? Great, you're in the right place. While every island has its own story, and we'll touch on that, only one is a living example of a Hawaiian Island in the works - the Big Island. It's the perfect specific to examine and use as an example. That said, let's take a look at the geology of the only island you can still see physically growing by day.The 'Hot Spot'
So what exactly is this 'hot spot' you hear so much about, and how does it form these beautiful islands? The answer to this question is fairly simple. The Hawaiian Islands are situated near the middle of the "Pacific Plate" on top of a 'hot spot.' This Pacific Plate is almost always moving northwestward at a rate of several centimeters per year, about the same rate as your fingernails grow. This constant northwestward movement of the Pacific Plate over a local volcanic "hot spot," or plume, has produced a series of islands, one after another in assembly line fashion. The result is a chain of volcanic islands (Hawaiian archipelago) that consists of eight major islands and 124 islets stretching from the Big Island of Hawai'i along a northwest line for 1,500 miles toward Japan and the Aleutian Islands of Alaska. In total, the islands spread across an area of 6,459 square miles. The link above shows one perspective of this chain of islands. This link shows another view of the Hawaii archipelago.
The Big Island of Hawai'i is currently the largest landmass in the Hawaiian island chain. The eight major islands at the western end of the chain are, from west to east, Ni'ihau, Hawai'i, Oahu, Moloka'i, Lana'i, Kaho'olawe, Maui, and the Big Island of Hawai'i.
Hawai'i, also the youngest island in this chain, began over a million years ago as five separate volcanoes on the ocean floor. As the five volcanoes erupted time and time again (not necessarily simultaneously but rather sequentially), they created thin new sheets of lava spread upon the old, building and building until the volcanic heads emerged from the sea. These mountains often would have flows that overlapped the other mountain's flows, and eventually the five peaks would become the single island we see today (note the diagram below). First the Kohala Mountains formed as they sat over the 'hot spot' in the plate. But as the plate shifted, so did the location of the rising magma, moving to Mauna Kea, Hualalai, Mauna Loa, and eventually Kilauea. Even now there is a new seamount, named Lo'ihi, which is also forming off the southeast coast of the Big Island. In another 50,000 years or so, it too may become the next Hawaiian island, or it may even join to become the sixth peak of the Big Island. Currently, only the volcanic remnants of Kohala are completely extinct, never to erupt again. The rest of the volcanoes on the Big Island aren't quite done yet. Consider this a history lesson that's still evolving.
The Volcanoes of the Big Island
Mauna Loa, the Big Island’s largest volcano makes up approximately 51% of the island, and most people still have a surprisingly hard time finding it when they are here. Mauna Loa means “Long Mountain” and is given this name due to its large shield shape. This shape makes it difficult to distinguish Mauna Loa as an actual mountain.
The name “shield volcano,” which is what all the islands in Hawai‘i are, comes from a perceived resemblance to the shape of a warrior’s shield. Molten lava rises from a hot spot in the earth’s crust, erupts through various vents and rifts on the surface, and proceeds to move down the gentle slopes toward the ocean, building up layer upon layer over millions of years. Kilauea Volcano, the world’s most active volcano and home to the fire-goddess, Pele, resides on the eastern slopes of Mauna Loa. At one time many believed Kilauea to be a vent of Mauna Loa, but today we know it has its own magma chamber and is completely separate from its larger cousin next door. Mauna Kea is the other major volcano on the island making up about 25% of the island’s total landmass. Mauna Kea is significantly easier to spot than Mauna Loa, often recognized in winter months by its snowy cap, hence the name Mauna Kea - meaning “White Mountain.” Reaching a total elevation of some 33,000 feet from the sea floor, of which only 13,780 (approx.) feet exist above sea level, the mountain is the highest point in the Pacific Ocean and the world’s tallest mountain from base to summit.
The Big Island’s other volcanic mountains are Hualalai in Kailua-Kona on the west side of the island and Kohala on the northwest tip of the island. Kohala is the oldest mountain on the island and shows much more geological wear than its younger counterparts. The amazing sea cliffs found in Kohala today were likely caused by a giant landslide some 200,000 years ago.
Mauna Kea and Hualalai are both considered dormant, like Haleakala on Mau'i. Chances are they will erupt again in the long-term future, though most likely to no significant degree (volume wise) as the hot spot no longer exists beneath them. Generally speaking, the only eruptions that occur beneath these dormant mountains are due to their subsidence into the ocean floor, usually a few thousand feet over time, which then heats and "pushes" any remaining magma up to the surface in the form of an eruption.
Unfortunately, while these eruptions lack volume, they can be somewhat violent and even explosive. Mauna Kea owes its steep slopes to a explosive type of eruption in the recent geologic past. Explosive eruptions often produce widespread ash deposits, which help build a steeper sided volcano like those found in the western United States. Today the physical differences between Mauna Kea (fairly steep sided due to 'recent' explosive eruptions) and Mauna Loa (still in its shield-forming stage) are very distinct. In its prime, Mauna Kea likely reached a few thousand feet higher than it does today. As previously noted, Mauna Kea remains the tallest mountain, from top to bottom, on the planet. From base to summit it towers some 33,000 feet. That's taller than Mount Everest. Plus if you consider what's subsided (sunk) into the ocean floor, which the USGS does take into account for mountain height, then the mountain is 56,000 feet tall. That's just incredible!
Mauna Loa and Kilauea are both considered active volcanoes. Mauna Loa last erupted in 1984, and is likely to erupt fairly significantly again in the near future. Since 1843, the beginning of well-documented historical data, Mauna Loa has erupted 33 times. Geologically speaking that makes it a very active volcano. Mauna Loa is by far the bulk (51%) of the Big Island and remains the world's largest (in mass) volcano. Currently, Kilauea makes all the news and steals the show, but one day in the future Mauna Loa will remind us why it's the biggest volcano on the island. Mauna Loa can erupt significant amounts of lava in a very short time frame, dwarfing Kilauea.
Kilauea, once believed to be merely a side satellite vent of Mauna Loa but now recognized as its own distinct volcano, is the world's most active volcano, erupting continuously since 1983. Between January 1983, and June 2007, nearly 600 acres of land were added to the island by lava flows from Kilauea volcano. This growth has not been without cost however. Several towns have been destroyed by Kilauea: Kapoho (1960), Kalapana (1990), and Kaimu (1990). Today the remnants of these towns struggle to survive on the flanks of the world's most active volcano. In some aspects these towns are all but abandoned except by a few.
As previously mentioned, just 18 miles off Hawai'i's southeast coast is the undersea volcano known as Lo'ihi. Lo'ihi is an actively erupting seamount that lies approximately 3,178 feet below the surface of the ocean. If and when Lo'ihi breaks above the waves, it will likely join with Kilauea (which, in theory, will be much larger by that time) and become the sixth peak in what is now Hawai'i's largest island. Don't book your hotel room just yet though: it's a good 50,000 years or more in the making.
Lava Types
As you drive around the island you can't help but notice the various lava formations and lava fields that crisscross the island. If you pay especially close attention you're likely to observe there are two distinctly different types of lava flows. Around the Kona area you'll quickly notice how clunky and jagged the lava is. In most of Hawaii Volcanoes National Park, especially at the end of Chain of Craters Road, you'll notice the lava is very smooth, pillowy, and even ropy. These two unique flow types owe their origins to two distinctly different types of lava flows, Pahoehoe and A'a.
The word Pahoehoe (pronounced Pa-hoi-hoi) rolls off the tongue in the same fashion that it flows out of the volcano. It is smooth, and as the surface cools it forms ropy swirls and smooth hills. Pahoehoe flows slowly and steadily forward using bulbous toes to lead the way. As the toe (lobe) cools, it creates a thin layer. The hot lava continues to advance by breaking through the layer. The unique cracking sound of the cooled crust popping off often bewilders first time visitors. The surface texture of pahoehoe flows can vary greatly. The viscous nature of pahoehoe makes it the perfect medium to create a variety of designs in the cooled lava.
The other type of lava is called 'A'a. 'A'a (pronounced "ah-ah") is the rough and tumble sister of pahoehoe. It rolls forth in clumps of broken lava called clinkers. The clinkers continue to pile up until the lava has cooled leaving a sharp, brittle pile of lava rock. It is difficult to find sure footing on the rubbly surface. The term 'a'a is actually said to have come from the ancient Hawaiians who would exclaim 'ah ah' as they walked over it with their bare feet. While the top of the flow may just look like a pile of rocks, underneath is a dense lava core which drives it onward. The crumbly surface clinkers are able to hitch a ride on top of the dense lava for awhile, but eventually they topple off the end and are rolled over. This process creates layers of fragments on the top and bottom of the advancing flow. It's almost like a glacier of fire.
Most of the lava that erupts in the islands begins its life as pahoehoe. Along its journey a variety of factors can make it change into 'a'a. The thickness of the lava and the resistance of the path it takes can make this change occur. The thicker the pahoehoe flow, the less resistance is required to turn it into 'a'a because it is moving so slowly. Conversely, the thinner and more free flowing the pahoehoe flow, the harder it is to encounter the amount of resistance required to turn it into 'a'a. Once a pahoehoe flow has transitioned to 'a'a, there is no going back. Pahoehoe can turn into 'a'a, but 'a'a can never turn into pahoehoe.
Two other famous volcanic by-product are Pele's hair and tears. Both formed in fountaining eruptions, Pele's hair are thin strands of volcanic glass caught in the air during a eruption. Pele's tears are solid tear-shaped glass particles formed in the same way.
Subsidence & Erosion of the Hawaiian Islands
Though the Big Island of Hawai'i may seem incredibly large compared to it's predecessors in the chain, in all likelihood it is not that much larger at all (historically speaking). Just across the 'Alenuihaha Channel sits the island of Maui and it's greatest volcano, Haleakala. Geologists suspect that at one time Haleakala was not only joined to the West Maui Mountains, like today, but also was a single landmass combined with the islands of Lana'i, Moloka'i, and Kaho'olawe -- known as Maui Nui (literally, big Maui) (view map). The submergence of Maui Nui resulted as the volcanic body moved away from the Hawaiian hot spot. The lack of volcanic upbuilding combined with continued subsidence into the ocean floor eventually sank portions of the large island into the Pacific, providing us with the four separate islands we see today.
A similar fate awaits the Big Island in due time. As the hot spot "moves away" from the island (due to the Pacific Plate carrying the islands piggyback-style off to the north west) the Big Island too will fall victim to subsidence and erosion. Eventually the Big Island will likely find itself in a similar state to that of Maui Nui. It will become separate and smaller islands as the ocean encroaches on the flanks of each separate mountain. Such is the geologic circle of life beyond the Hawaiian hot spot.
For the next few thousand years however the Big Island will remain just that, big! It continues to represent an astounding 62% of the total land area of the Hawaiian Islands. And because Mauna Loa and Kilauea are currently still active and erupting volcanoes, the island of Hawai'i is still growing. The geologic future of the island is a work in progress.
A larger version of the rendered map above can be found here: Hawaiian Islands Map (Courtesy NGDC, GLCF, and DLR).
Hawai'i, also the youngest island in this chain, began over a million years ago as five separate volcanoes on the ocean floor. As the five volcanoes erupted time and time again (not necessarily simultaneously but rather sequentially), they created thin new sheets of lava spread upon the old, building and building until the volcanic heads emerged from the sea. These mountains often would have flows that overlapped the other mountain's flows, and eventually the five peaks would become the single island we see today (note the diagram below). First the Kohala Mountains formed as they sat over the 'hot spot' in the plate. But as the plate shifted, so did the location of the rising magma, moving to Mauna Kea, Hualalai, Mauna Loa, and eventually Kilauea. Even now there is a new seamount, named Lo'ihi, which is also forming off the southeast coast of the Big Island. In another 50,000 years or so, it too may become the next Hawaiian island, or it may even join to become the sixth peak of the Big Island. Currently, only the volcanic remnants of Kohala are completely extinct, never to erupt again. The rest of the volcanoes on the Big Island aren't quite done yet. Consider this a history lesson that's still evolving.
The Volcanoes of the Big Island
Mauna Loa, the Big Island’s largest volcano makes up approximately 51% of the island, and most people still have a surprisingly hard time finding it when they are here. Mauna Loa means “Long Mountain” and is given this name due to its large shield shape. This shape makes it difficult to distinguish Mauna Loa as an actual mountain. The name “shield volcano,” which is what all the islands in Hawai‘i are, comes from a perceived resemblance to the shape of a warrior’s shield. Molten lava rises from a hot spot in the earth’s crust, erupts through various vents and rifts on the surface, and proceeds to move down the gentle slopes toward the ocean, building up layer upon layer over millions of years. Kilauea Volcano, the world’s most active volcano and home to the fire-goddess, Pele, resides on the eastern slopes of Mauna Loa. At one time many believed Kilauea to be a vent of Mauna Loa, but today we know it has its own magma chamber and is completely separate from its larger cousin next door. Mauna Kea is the other major volcano on the island making up about 25% of the island’s total landmass. Mauna Kea is significantly easier to spot than Mauna Loa, often recognized in winter months by its snowy cap, hence the name Mauna Kea - meaning “White Mountain.” Reaching a total elevation of some 33,000 feet from the sea floor, of which only 13,780 (approx.) feet exist above sea level, the mountain is the highest point in the Pacific Ocean and the world’s tallest mountain from base to summit.
The Big Island’s other volcanic mountains are Hualalai in Kailua-Kona on the west side of the island and Kohala on the northwest tip of the island. Kohala is the oldest mountain on the island and shows much more geological wear than its younger counterparts. The amazing sea cliffs found in Kohala today were likely caused by a giant landslide some 200,000 years ago.
Mauna Kea and Hualalai are both considered dormant, like Haleakala on Mau'i. Chances are they will erupt again in the long-term future, though most likely to no significant degree (volume wise) as the hot spot no longer exists beneath them. Generally speaking, the only eruptions that occur beneath these dormant mountains are due to their subsidence into the ocean floor, usually a few thousand feet over time, which then heats and "pushes" any remaining magma up to the surface in the form of an eruption.
Unfortunately, while these eruptions lack volume, they can be somewhat violent and even explosive. Mauna Kea owes its steep slopes to a explosive type of eruption in the recent geologic past. Explosive eruptions often produce widespread ash deposits, which help build a steeper sided volcano like those found in the western United States. Today the physical differences between Mauna Kea (fairly steep sided due to 'recent' explosive eruptions) and Mauna Loa (still in its shield-forming stage) are very distinct. In its prime, Mauna Kea likely reached a few thousand feet higher than it does today. As previously noted, Mauna Kea remains the tallest mountain, from top to bottom, on the planet. From base to summit it towers some 33,000 feet. That's taller than Mount Everest. Plus if you consider what's subsided (sunk) into the ocean floor, which the USGS does take into account for mountain height, then the mountain is 56,000 feet tall. That's just incredible!
Mauna Loa and Kilauea are both considered active volcanoes. Mauna Loa last erupted in 1984, and is likely to erupt fairly significantly again in the near future. Since 1843, the beginning of well-documented historical data, Mauna Loa has erupted 33 times. Geologically speaking that makes it a very active volcano. Mauna Loa is by far the bulk (51%) of the Big Island and remains the world's largest (in mass) volcano. Currently, Kilauea makes all the news and steals the show, but one day in the future Mauna Loa will remind us why it's the biggest volcano on the island. Mauna Loa can erupt significant amounts of lava in a very short time frame, dwarfing Kilauea.
Kilauea, once believed to be merely a side satellite vent of Mauna Loa but now recognized as its own distinct volcano, is the world's most active volcano, erupting continuously since 1983. Between January 1983, and June 2007, nearly 600 acres of land were added to the island by lava flows from Kilauea volcano. This growth has not been without cost however. Several towns have been destroyed by Kilauea: Kapoho (1960), Kalapana (1990), and Kaimu (1990). Today the remnants of these towns struggle to survive on the flanks of the world's most active volcano. In some aspects these towns are all but abandoned except by a few.
As previously mentioned, just 18 miles off Hawai'i's southeast coast is the undersea volcano known as Lo'ihi. Lo'ihi is an actively erupting seamount that lies approximately 3,178 feet below the surface of the ocean. If and when Lo'ihi breaks above the waves, it will likely join with Kilauea (which, in theory, will be much larger by that time) and become the sixth peak in what is now Hawai'i's largest island. Don't book your hotel room just yet though: it's a good 50,000 years or more in the making.
Lava TypesAs you drive around the island you can't help but notice the various lava formations and lava fields that crisscross the island. If you pay especially close attention you're likely to observe there are two distinctly different types of lava flows. Around the Kona area you'll quickly notice how clunky and jagged the lava is. In most of Hawaii Volcanoes National Park, especially at the end of Chain of Craters Road, you'll notice the lava is very smooth, pillowy, and even ropy. These two unique flow types owe their origins to two distinctly different types of lava flows, Pahoehoe and A'a.
The word Pahoehoe (pronounced Pa-hoi-hoi) rolls off the tongue in the same fashion that it flows out of the volcano. It is smooth, and as the surface cools it forms ropy swirls and smooth hills. Pahoehoe flows slowly and steadily forward using bulbous toes to lead the way. As the toe (lobe) cools, it creates a thin layer. The hot lava continues to advance by breaking through the layer. The unique cracking sound of the cooled crust popping off often bewilders first time visitors. The surface texture of pahoehoe flows can vary greatly. The viscous nature of pahoehoe makes it the perfect medium to create a variety of designs in the cooled lava.
The other type of lava is called 'A'a. 'A'a (pronounced "ah-ah") is the rough and tumble sister of pahoehoe. It rolls forth in clumps of broken lava called clinkers. The clinkers continue to pile up until the lava has cooled leaving a sharp, brittle pile of lava rock. It is difficult to find sure footing on the rubbly surface. The term 'a'a is actually said to have come from the ancient Hawaiians who would exclaim 'ah ah' as they walked over it with their bare feet. While the top of the flow may just look like a pile of rocks, underneath is a dense lava core which drives it onward. The crumbly surface clinkers are able to hitch a ride on top of the dense lava for awhile, but eventually they topple off the end and are rolled over. This process creates layers of fragments on the top and bottom of the advancing flow. It's almost like a glacier of fire.Most of the lava that erupts in the islands begins its life as pahoehoe. Along its journey a variety of factors can make it change into 'a'a. The thickness of the lava and the resistance of the path it takes can make this change occur. The thicker the pahoehoe flow, the less resistance is required to turn it into 'a'a because it is moving so slowly. Conversely, the thinner and more free flowing the pahoehoe flow, the harder it is to encounter the amount of resistance required to turn it into 'a'a. Once a pahoehoe flow has transitioned to 'a'a, there is no going back. Pahoehoe can turn into 'a'a, but 'a'a can never turn into pahoehoe.
Two other famous volcanic by-product are Pele's hair and tears. Both formed in fountaining eruptions, Pele's hair are thin strands of volcanic glass caught in the air during a eruption. Pele's tears are solid tear-shaped glass particles formed in the same way.
Subsidence & Erosion of the Hawaiian Islands
Though the Big Island of Hawai'i may seem incredibly large compared to it's predecessors in the chain, in all likelihood it is not that much larger at all (historically speaking). Just across the 'Alenuihaha Channel sits the island of Maui and it's greatest volcano, Haleakala. Geologists suspect that at one time Haleakala was not only joined to the West Maui Mountains, like today, but also was a single landmass combined with the islands of Lana'i, Moloka'i, and Kaho'olawe -- known as Maui Nui (literally, big Maui) (view map). The submergence of Maui Nui resulted as the volcanic body moved away from the Hawaiian hot spot. The lack of volcanic upbuilding combined with continued subsidence into the ocean floor eventually sank portions of the large island into the Pacific, providing us with the four separate islands we see today.
A similar fate awaits the Big Island in due time. As the hot spot "moves away" from the island (due to the Pacific Plate carrying the islands piggyback-style off to the north west) the Big Island too will fall victim to subsidence and erosion. Eventually the Big Island will likely find itself in a similar state to that of Maui Nui. It will become separate and smaller islands as the ocean encroaches on the flanks of each separate mountain. Such is the geologic circle of life beyond the Hawaiian hot spot.
For the next few thousand years however the Big Island will remain just that, big! It continues to represent an astounding 62% of the total land area of the Hawaiian Islands. And because Mauna Loa and Kilauea are currently still active and erupting volcanoes, the island of Hawai'i is still growing. The geologic future of the island is a work in progress.
A larger version of the rendered map above can be found here: Hawaiian Islands Map (Courtesy NGDC, GLCF, and DLR).
Brief History of Hawaii
The following is a brief history of the islands of Hawaii. Specifically this text is pulled directly from our Hawaii - Mile by Mile Guidebook. We hope it helps provide our guests with a better understanding of the islands and the people that live upon them.Birds & Seeds
Thousand of miles from the nearest continent the volcanic mountains stood somber and alone in the Pacific, void of nearly all life. Lifeless they would remain if not for the birds, the currents, and the wind. Seeds were carried by the tides that washed across the shores. Storms brought more seeds with their howling winds and rains. The birds, like the small golden plover, brought the rest.
Eventually the Hawaiian islands would be covered with extensive forest habitats, shrubbery, and grasslands. Soil and precipitation differences around the islands would cater to all kinds of plant-life. In time, the foreign species would become unique to all the world, found only in Hawai'i. Today, we call them endemic Hawaiian species like the Nene (Hawaiian goose) and silversword (which is a relative of the sunflower believe it or not). You will find them no where else on the planet. These species had thousands, if not millions, of years to develop into unique flora and fauna. And for thousands and thousands of years they were undisturbed by the ways of humans. Today, many of these species are not so lucky. The 'Akiapola'au (photo seen above) is just one example of a species that is fading fast. Most experts predict that their numbers have dwindled to between 1,000-1,500. They can be found only on the Big Island. We were very lucky to see one as recently as 2006.
Polynesian Arrival
Today most anthropologists will tell you that the original settlement of the Hawaiian islands was by Polynesians from the Marquesas Islands around 300-500 AD. This group of early settlers is today believed to be where the legend of the menehune originates. A second wave of settlement followed during the 9th and 10th centuries from Tahiti, radically changing the islands and the culture that existed there.
They came in their double-hulled canoes, some 3,500 miles south of the Big Island. Using the wind and paddle they navigated themselves in uncharted waters to the peaks of this foreign land. Arriving as early as 2,000 years ago, the Polynesians came in waves of migration bringing most everything with them they’d need to survive on the shores of Hawai'i. Banana and coconut trees, dogs, hogs, rats, and chickens came with them from thousands of miles away.
Their knowledge of the sea also provided ample seafood. Weaving, wood and stone-carving allowed them to grow crops and farm. Their population would flourish here, and by the time Europeans first made contact in 1778, their numbers were estimated at approximately 800,000 to one million. Once established, the Hawaiians had no further need to obtain supplies from their old homelands, and thus underwent centuries of isolation in what is still today the most isolated spot on the planet.
The Polynesians governed themselves by a set of rules, a kapu system with chiefs and ali'i (royalty). Their culture was strict and abundant in both mythology and lore. Their religious system was very deeply tied to nature, and there were hundreds upon thousands of gods in the system. Four main gods were especially important to the Hawaiians: Ku, Kane, Kanaloa, and Lono.
One of their most powerful deities, Pele, made her continuous presence known on the Big Island. Her home was, and still is, Kilauea’s Caldera, and her frequent eruptions are a constant reminder of her existence. She is a goddess of fire who changes form at will. A beautiful woman one minute a fireball the next, Pele is known for here fiery temper. Even today many residents hope to appease Madame Pele by placing offerings on the rim of her home. As recently as 1990, Pele made her temperament known by destroying over 200 homes along the southeast shoreline.
The Polynesians were stewards of both land and sea, guardians of all that existed here. They were careful to never over-fish the reefs or streams and to never abuse the aina (land) which so graciously supported them. They skillfully diverted water into irrigation channels to flood their taro fields, so that their staple food of poi could be produced and eaten by generation upon generation. Today these canals still criss-cross the island and taro still grows in beautiful valleys. Two of these valleys were some of the most prosperous in Hawai'i Pololu and Waipi'o, both on the northeastern Kohala coast of the Big Island. Waipi'o even today is still known for its taro fields.
European Arrival
With the sighting of great white sails on the horizon, the likes of which the Hawaiians had never seen, the islands were forever changed. Captain James Cook, one of the world’s most recognized British navigators, sailed into Waimea Bay on the island of Kaua‘i first in 1778, and then onto the Big Island at Kealakekua Bay in early 1779.
At the time of Cook’s arrival on the Big Island some 10,000 or more Hawaiians were in the midst of their makahiki celebration, a celebration that honored the god Lono. Cook arriving on his ship with white sails (similar to that of the god Lono’s flag) was likely mistaken as the god Lono and treated accordingly. During his two week stay on the Big Island, he was honored in ceremony upon ceremony. Cook and the Hawaiians entertained each other mutually with their own inventions before the famous navigator set sail away from the islands. Shortly there-after, the makahiki celebration ended, and the bay was made kapu (off-limits).
Meanwhile, a storm off-shore had damaged one of Cook’s ships. Naturally he returned to the bay expecting the same hospitality he’d received before. But many of the Hawaiians had grown tired of the sailors’ presence in the bay, and despite the fraternization that took place, one of Cook’s smaller boats was stolen. It should have ended there, but Cook instead decided to go ashore and kidnap Chief Kalaniopu'u until his boat was returned. Intentional or not, Cook was stabbed in a skirmish which left him dead at the hands of Hawaiian warriors.
Today, a white monument, stands erected at the northern end of the bay where Cook met his demise, a solemn reminder of this event. This is the only piece of land in the Hawaiian chain that remains British soil. Today the area has become most popular for its snorkeling and kayaking.
Cook’s presence forever changed the islands. Chiefs were always at war with one another in Hawai'i. Never had a single ruler controlled all the islands. But a young chief by the name of Kamehameha, a native of Kohala on the Big Island, had taken note of the Westerners weapons and set out to conquer all the islands in the Hawaiian chain: to be their first king. By 1791, he had defeated his cousin and arch-rival on the Big Island, and by 1795, he had conquered Maui, Moloka'i, Lana'i, and O'ahu. In 1810, the chief that ruled Kaua'i, seeing all that had happened with Kamehameha and his warriors island by island, pledged his loyalty to Kamehameha. With that act, Kamehameha (seen here) fulfilled the prophecy that he would become the first King of Hawai'i.
Kamehameha ruled with a tight grip. He wished to prepare the islands for increasing contact with the west - sailors, whalers, and entrepreneurs. Unfortunately Kamehameha could not prepare the islands for what would affect them the most, venereal disease. Over the next century the Hawaiian population was decimated by the likes of influenza, typhoid fever, and measles. Estimates say the population decreased by as much as 80%.
It was greed that would next change the islands. Riches were to be made of the forests of Hawai'i with the sweet smelling sandalwood, a huge commodity in the orient. Guns, boats, and even canons made their way into Hawaiian life, and for the first time the concept of owning land came into existence. In 1819, when Kamehameha died, so did the remainder of Hawaiian life. A short time later Kamehameha II, at the behest of Kamehameha I’s wife, Ka'ahumanu, broke the kapu system that had ruled the islands for generations. A year later, the missionaries arrived from Boston.
Christian Missionaries
In early April of 1820, the first Christian missionaries stepped off their ship from Boston to, yet again, forever change the islands. In the wake of the kapu system being destroyed, many argue the Hawaiians were a people without a religion. Ka'ahumanu and Kamehameha II both quickly became converts of Christianity. The missionaries, recognizing what had just happened in the islands, were quick to destroy many ancient alters and heiau (temples), and quickly replace them with churches (many of which still stand). Today the largest religious groups remain Roman Catholics and Protestants.
Even Pele herself was defied when Kapiolani, high chieftess to the Big Island of Hawai'i, decreed that Jehovah was her god. When Pele remained quiet, the Hawaiian people believed, and many converted. A similar event took place in the mid-1970’s, where again Pele was denounced, and in a twist of irony the volcano erupted afterwards.
However, the missionaries brought a skill to the islands that would put Hawai'i on the map as far as the rest of the world was concerned, reading and writing. Hawai'i eventually soared to have the highest literacy rates in the United States. There had been no previous written language in Hawai'i until the missionaries' arrival. Everything was passed down by word of mouth. It was for this reason the Hawaiians could recite nearly the entire Bible from memory, an astonishing feat to the missionaries that taught them.
It was the children of the missionaries' families that would ultimately make the greatest change in Hawai'i. Ideally the families would have returned home as they were supposed to have done but instead stayed on the island and began a practice no Hawaiian had ever heard of, owning land.
Western law also made its way into Hawaiian life. The Hawaiian Constitution came into existence by 1840, along with a supreme court and a parliament.
Land issues continued to be a large focus in the coming years. By 1848, land was divided into thirds - one for the royalty, one for the government, and one for the common people. Two years later foreigners could buy land outright, and that they did.
Led by the missionaries' descendent's, a great agricultural boom occurred in Hawai'i in the early 20th century, bringing more and more immigrants from Japan, China, and the Philippines to work in the growing fields of sugarcane, pineapple, and other large crops. Hawai'i became a melting pot of world cultures, faiths, and customs, which forged a new identity that still holds true today.
Oil discovered in the heart of America lead to the end of the whaling era, though whales had been so depleted in the waters off Hawai'i that the industry barely existed. Sugar was the new king of the islands, and would continue to be well on into the twentieth century. Today the industry is all but dead in the state, and the economic impact of its absence is still felt in many areas.
End of the Kingdom
With the multitude of foreign changes occurring in Hawai'i the conflict between royalty and the outsiders was bound to grow. With the U.S. military already showing a strong presence in the region (especially Pearl Harbor), it was only a matter of time before what happened, did. U.S. businessmen convinced the military that they were still U.S. citizens, and thus must be protected as such. When the businessmen seized control of the islands and took power away from Liliuokalani (the existing Queen), the military felt obligated to protect the Americans. The Republic of Hawai'i was formed. In 1898, the U.S. finally annexed Hawai'i as a territory. Sixty-one years later the voters of Hawai'i approved statehood. The Big Island, Maui (including Moloka'i and Lana'i), O'ahu, and Kau'i all became one of four counties in the 50th state of the union. Today much debate continues over what happened at the end of the 19th century.
Modern Times (On the Big Island)
The Big Island is a growing center of both education and research. Home to one of the University of Hawai'i's campuses in Hilo, the Big Island is renown for its study of astronomy, alternative energy (wind power, geothermal, etc), ocean research, and much more. Tourism is responsible for a large portion of the county's annual revenue, though various agricultural crops also make their mark - including flowers (especially orchids), macadamia nuts, and coffee. Many say the Big Island is getting bigger all the time. Perhaps it was Kamehameha’s dream, perhaps not... we'll never know for sure.
The racial, religious, and cultural background of Hawai'i has changed drastically over that time. Over the last few decades, the Hawai'i of old has reemerged bringing a great sense of pride to the remaining native Hawaiians. The hula, chant, and old ways are being reborn. The change from an agricultural hearth to a tourist destination has also now exposed Hawai'i to people the world over. A state with a population of only 1.2 million has experienced tourism numbers floating around 7 million in recent years. The influence has been both positive and negative from various points of view. Today, most of the state's residents reside on the island of Oahu, some 60% in Honolulu alone which is the 11th largest city in the United States.
A few other quick tidbits of information regarding Hawai'i's culture. If you hear the term "Hawaiian" it is in reference to someone's race only, not where they are. Hawaiian implies they have pure Hawaiian blood in their veins. Locals are typically folks who were born and raised here, but are not necessarily pure Hawaiians. A kama'aina is someone who has lived here a while but typically was not born here. Lastly, the term haole is used for all persons who are white, born here or not.
Today most anthropologists will tell you that the original settlement of the Hawaiian islands was by Polynesians from the Marquesas Islands around 300-500 AD. This group of early settlers is today believed to be where the legend of the menehune originates. A second wave of settlement followed during the 9th and 10th centuries from Tahiti, radically changing the islands and the culture that existed there.
They came in their double-hulled canoes, some 3,500 miles south of the Big Island. Using the wind and paddle they navigated themselves in uncharted waters to the peaks of this foreign land. Arriving as early as 2,000 years ago, the Polynesians came in waves of migration bringing most everything with them they’d need to survive on the shores of Hawai'i. Banana and coconut trees, dogs, hogs, rats, and chickens came with them from thousands of miles away.
Their knowledge of the sea also provided ample seafood. Weaving, wood and stone-carving allowed them to grow crops and farm. Their population would flourish here, and by the time Europeans first made contact in 1778, their numbers were estimated at approximately 800,000 to one million. Once established, the Hawaiians had no further need to obtain supplies from their old homelands, and thus underwent centuries of isolation in what is still today the most isolated spot on the planet.
The Polynesians governed themselves by a set of rules, a kapu system with chiefs and ali'i (royalty). Their culture was strict and abundant in both mythology and lore. Their religious system was very deeply tied to nature, and there were hundreds upon thousands of gods in the system. Four main gods were especially important to the Hawaiians: Ku, Kane, Kanaloa, and Lono.
One of their most powerful deities, Pele, made her continuous presence known on the Big Island. Her home was, and still is, Kilauea’s Caldera, and her frequent eruptions are a constant reminder of her existence. She is a goddess of fire who changes form at will. A beautiful woman one minute a fireball the next, Pele is known for here fiery temper. Even today many residents hope to appease Madame Pele by placing offerings on the rim of her home. As recently as 1990, Pele made her temperament known by destroying over 200 homes along the southeast shoreline.
The Polynesians were stewards of both land and sea, guardians of all that existed here. They were careful to never over-fish the reefs or streams and to never abuse the aina (land) which so graciously supported them. They skillfully diverted water into irrigation channels to flood their taro fields, so that their staple food of poi could be produced and eaten by generation upon generation. Today these canals still criss-cross the island and taro still grows in beautiful valleys. Two of these valleys were some of the most prosperous in Hawai'i Pololu and Waipi'o, both on the northeastern Kohala coast of the Big Island. Waipi'o even today is still known for its taro fields.
European Arrival
With the sighting of great white sails on the horizon, the likes of which the Hawaiians had never seen, the islands were forever changed. Captain James Cook, one of the world’s most recognized British navigators, sailed into Waimea Bay on the island of Kaua‘i first in 1778, and then onto the Big Island at Kealakekua Bay in early 1779.
At the time of Cook’s arrival on the Big Island some 10,000 or more Hawaiians were in the midst of their makahiki celebration, a celebration that honored the god Lono. Cook arriving on his ship with white sails (similar to that of the god Lono’s flag) was likely mistaken as the god Lono and treated accordingly. During his two week stay on the Big Island, he was honored in ceremony upon ceremony. Cook and the Hawaiians entertained each other mutually with their own inventions before the famous navigator set sail away from the islands. Shortly there-after, the makahiki celebration ended, and the bay was made kapu (off-limits).
Meanwhile, a storm off-shore had damaged one of Cook’s ships. Naturally he returned to the bay expecting the same hospitality he’d received before. But many of the Hawaiians had grown tired of the sailors’ presence in the bay, and despite the fraternization that took place, one of Cook’s smaller boats was stolen. It should have ended there, but Cook instead decided to go ashore and kidnap Chief Kalaniopu'u until his boat was returned. Intentional or not, Cook was stabbed in a skirmish which left him dead at the hands of Hawaiian warriors.
Today, a white monument, stands erected at the northern end of the bay where Cook met his demise, a solemn reminder of this event. This is the only piece of land in the Hawaiian chain that remains British soil. Today the area has become most popular for its snorkeling and kayaking.
Cook’s presence forever changed the islands. Chiefs were always at war with one another in Hawai'i. Never had a single ruler controlled all the islands. But a young chief by the name of Kamehameha, a native of Kohala on the Big Island, had taken note of the Westerners weapons and set out to conquer all the islands in the Hawaiian chain: to be their first king. By 1791, he had defeated his cousin and arch-rival on the Big Island, and by 1795, he had conquered Maui, Moloka'i, Lana'i, and O'ahu. In 1810, the chief that ruled Kaua'i, seeing all that had happened with Kamehameha and his warriors island by island, pledged his loyalty to Kamehameha. With that act, Kamehameha (seen here) fulfilled the prophecy that he would become the first King of Hawai'i.Kamehameha ruled with a tight grip. He wished to prepare the islands for increasing contact with the west - sailors, whalers, and entrepreneurs. Unfortunately Kamehameha could not prepare the islands for what would affect them the most, venereal disease. Over the next century the Hawaiian population was decimated by the likes of influenza, typhoid fever, and measles. Estimates say the population decreased by as much as 80%.
It was greed that would next change the islands. Riches were to be made of the forests of Hawai'i with the sweet smelling sandalwood, a huge commodity in the orient. Guns, boats, and even canons made their way into Hawaiian life, and for the first time the concept of owning land came into existence. In 1819, when Kamehameha died, so did the remainder of Hawaiian life. A short time later Kamehameha II, at the behest of Kamehameha I’s wife, Ka'ahumanu, broke the kapu system that had ruled the islands for generations. A year later, the missionaries arrived from Boston.
Christian Missionaries
In early April of 1820, the first Christian missionaries stepped off their ship from Boston to, yet again, forever change the islands. In the wake of the kapu system being destroyed, many argue the Hawaiians were a people without a religion. Ka'ahumanu and Kamehameha II both quickly became converts of Christianity. The missionaries, recognizing what had just happened in the islands, were quick to destroy many ancient alters and heiau (temples), and quickly replace them with churches (many of which still stand). Today the largest religious groups remain Roman Catholics and Protestants.
Even Pele herself was defied when Kapiolani, high chieftess to the Big Island of Hawai'i, decreed that Jehovah was her god. When Pele remained quiet, the Hawaiian people believed, and many converted. A similar event took place in the mid-1970’s, where again Pele was denounced, and in a twist of irony the volcano erupted afterwards.
However, the missionaries brought a skill to the islands that would put Hawai'i on the map as far as the rest of the world was concerned, reading and writing. Hawai'i eventually soared to have the highest literacy rates in the United States. There had been no previous written language in Hawai'i until the missionaries' arrival. Everything was passed down by word of mouth. It was for this reason the Hawaiians could recite nearly the entire Bible from memory, an astonishing feat to the missionaries that taught them.
It was the children of the missionaries' families that would ultimately make the greatest change in Hawai'i. Ideally the families would have returned home as they were supposed to have done but instead stayed on the island and began a practice no Hawaiian had ever heard of, owning land.
Western law also made its way into Hawaiian life. The Hawaiian Constitution came into existence by 1840, along with a supreme court and a parliament.
Land issues continued to be a large focus in the coming years. By 1848, land was divided into thirds - one for the royalty, one for the government, and one for the common people. Two years later foreigners could buy land outright, and that they did.
Led by the missionaries' descendent's, a great agricultural boom occurred in Hawai'i in the early 20th century, bringing more and more immigrants from Japan, China, and the Philippines to work in the growing fields of sugarcane, pineapple, and other large crops. Hawai'i became a melting pot of world cultures, faiths, and customs, which forged a new identity that still holds true today.
Oil discovered in the heart of America lead to the end of the whaling era, though whales had been so depleted in the waters off Hawai'i that the industry barely existed. Sugar was the new king of the islands, and would continue to be well on into the twentieth century. Today the industry is all but dead in the state, and the economic impact of its absence is still felt in many areas.
End of the Kingdom
With the multitude of foreign changes occurring in Hawai'i the conflict between royalty and the outsiders was bound to grow. With the U.S. military already showing a strong presence in the region (especially Pearl Harbor), it was only a matter of time before what happened, did. U.S. businessmen convinced the military that they were still U.S. citizens, and thus must be protected as such. When the businessmen seized control of the islands and took power away from Liliuokalani (the existing Queen), the military felt obligated to protect the Americans. The Republic of Hawai'i was formed. In 1898, the U.S. finally annexed Hawai'i as a territory. Sixty-one years later the voters of Hawai'i approved statehood. The Big Island, Maui (including Moloka'i and Lana'i), O'ahu, and Kau'i all became one of four counties in the 50th state of the union. Today much debate continues over what happened at the end of the 19th century.
Modern Times (On the Big Island)
The Big Island is a growing center of both education and research. Home to one of the University of Hawai'i's campuses in Hilo, the Big Island is renown for its study of astronomy, alternative energy (wind power, geothermal, etc), ocean research, and much more. Tourism is responsible for a large portion of the county's annual revenue, though various agricultural crops also make their mark - including flowers (especially orchids), macadamia nuts, and coffee. Many say the Big Island is getting bigger all the time. Perhaps it was Kamehameha’s dream, perhaps not... we'll never know for sure.
The racial, religious, and cultural background of Hawai'i has changed drastically over that time. Over the last few decades, the Hawai'i of old has reemerged bringing a great sense of pride to the remaining native Hawaiians. The hula, chant, and old ways are being reborn. The change from an agricultural hearth to a tourist destination has also now exposed Hawai'i to people the world over. A state with a population of only 1.2 million has experienced tourism numbers floating around 7 million in recent years. The influence has been both positive and negative from various points of view. Today, most of the state's residents reside on the island of Oahu, some 60% in Honolulu alone which is the 11th largest city in the United States.
A few other quick tidbits of information regarding Hawai'i's culture. If you hear the term "Hawaiian" it is in reference to someone's race only, not where they are. Hawaiian implies they have pure Hawaiian blood in their veins. Locals are typically folks who were born and raised here, but are not necessarily pure Hawaiians. A kama'aina is someone who has lived here a while but typically was not born here. Lastly, the term haole is used for all persons who are white, born here or not.
Hawaii Weather and Climate Patterns
While it's always going to be close to impossible to predict the weather months or even weeks ahead of your vacation, you can look at past weather and climatic variables to determine what is likely to occur. Below we'll go over some of the most common concerns about Hawai'i weather. If nothing else, you'll have a general idea of what to expect. As always, be sure to check local weather through the TV stations during your stay for day to day updates. Avoid the Weather Channel's web site, they'll say it's going to rain every day. It's not.
General Weather Patterns: The best thing about Hawai'i's weather is that it is very localized. You may be driving along the island and be in a rain storm one minute and in bright sun the next. This variety of weather allows you to fully experience Hawai'i and its sun-drenched beaches, misty rainbow-filled valleys, pristine waterfalls, cool highlands, and lush mountains. The chart seen to the right here shows the distribution of precipitation annually on the islands; click the chart to enlarge it.Hawaii, like all the other major Hawaiian islands, is affected by the trade winds. These winds blow NE to ENE and are typically more prevalent in the winter months. These trade winds bring cool air to the islands from the north, often resulting in precipitation along mauka and windward areas. At times, these winds can die down and practically reverse so that a south wind blows over the islands, resulting in very hot and muggy conditions. These winds are called Kona winds.
One mistake a lot of people make when they visit Hawai'i is assuming there is a wet and/or dry season like back home, but it's not quite that simple. Granted, there are two distinct times of year and weather patterns due to the trade winds, but there is no defined "rainy season." The general point to be made is, you can't just say it's rainy in the winter and dry in the summer. We've seen it bone dry in the winter, and had flooding in the summer; each enough times to derail most short-term trends. Still, we can look at the long term trends and get a general idea of what to expect. Let's take a look.
On average, the summer months are the driest and sunniest, but they are also the most humid and warmest. The winter months usually bring more rain to the windward side of the islands, north and east, but prolonged rain storms are uncommon. Make note of the difference between the Big Island's Rainbow Falls in winter (right) and summer (left) - this is due to rainfall differences.The southern coasts of each island are the driest parts year round. Also, consider that Hawai'i is geographically and topographically one of the most diverse places you'll ever find. The weather from one side of an island to the other varies greatly over distance and the topography present. Since weather can be so unpredictable in Hawai'i, keeping a small poncho with you during hikes or other outdoor activities might be a good idea. Unless you hike into any valleys, where clouds can build up and stick around a while, you're likely only to experience rain in short spells.
Hawai'i Temperatures: Hawai'i is fortunate in that it has a mild and pleasant temperature throughout the year, the largest complaint likely being the humidity for those not used to it. There is hardly any difference between night and day temperatures year round. The occasional storm or the trade winds are the exception to the rule, but even then temperatures don't vary by much. The average high and low in the summer are around 85 and 71 respectively, while the average high and low in the winter are 78 and 62 respectively.
The temperature estimates only apply near sea level, please keep in mind that elevation changes will alter the temperatures. With every 1,000 foot climb in elevation, the temperature, on average, drops another 3.5 degrees. We strongly urge visitors to take note that certain islands have topography that changes often, as does elevation. If you plan to visit the summit's of Haleakala on Maui or Mauna Kea on the Big Island, you'll also need to prepare accordingly as temperatures between 10,000-14,000 feet can be downright cold even in the summer months. We advise against winter travel to the summits on the Big Island, as blizzards are not uncommon there. Ultimately our message is simple. Keep the topography and elevation of where you are traveling in mind and prepare accordingly. Even if you do not plan to visit the summit areas on Maui or the Big Island (or visit either of these islands at all), a light jacket might be useful in other areas around the island you're visiting where elevation is above three to four thousand feet. Jackets or light sweaters are also useful for any dawn/dusk hiking at higher elevations, like Koke'e on Kauai or Hawai'i Volcanoes Park on the Big Island.
If it's the ocean temperatures you're wondering about, rest assured you'll find warm temperatures year round. Ocean temperatures remain pretty comfortable throughout the year ranging from 80 degrees in the summer to a milder 74 in the winter.
More Information:
Be sure to check out our When to visit Hawaii page for more information about visiting each island.
For detailed information on weather forecasts, we highly recommend you check out the Hawaii Weather Today website.
Hawaii Car Rental Tips
On any island in Hawai'i (including Oahu in our honest opinion) a rental car is definitely the best option for getting around the island you're visiting and viewing all the sights we detail both here on our website and in our physical guidebooks. The rental rates in Hawai'i are some of the cheapest anywhere in the world because the competition is fierce.
There is no *serious* bus service on the islands, excluding Oahu, and taxi services are both expensive and illogical for sight-seeing purposes. Mopeds and bikes can be a practical alternative for day excursions along the drier south coastlines, but generally are not as useful in other parts of the island, especially where long distances and/or rain storms may prevail between locations you'll want to see.
Ultimately, your best bet is to get a rental for your stay on any island, especially Maui, Kauai, and the Big Island. Below are some tips when acquiring your rental car:
1.) SUV, 4x4, or car, which do you need? For years we've heard debate about what vehicle best suites the needs of folks visiting the islands. There are rumors, especially on the Big Island, that you MUST have a 4x4 to visit the island; it's just not true. In fact, a 4x4 on any island is almost a complete waste of money. We'll tell you why in the next paragraph. In fact, of ALL the places listed on our website and of ALL the places written about in our guidebooks, the ONLY place you will need a 4x4 to reach is the summit of Mauna Kea on the Big Island of Hawaii. Every other location we describe has either a drivable road, a trail available for access, or is kapu (off limits). Save yourself money and rent a regular car.
OK, just so we're thorough, we want to make sure you know the real policies regarding any "off-roading," including 4x4 rentals. This is specifically meant for visitors to the Big Island, though it's applicable state wide. While policies and regulations about where you can and cannot go in a rental are always changing, we can tell you this: currently there is NO rental agency that allows off-roading on the Big Island (or any other island) without severe risks. A little research might lead you to one of the few Big Island companies (Harper's being the most prominent) allowing visitors to drive on Saddle Road and to the summit of Mauna Kea. However there is some fuzziness about how much off-roading you can do with these rentals. We can promise you they are all very strict about damage and will check the car very thoroughly, including with mirrors under the car, when you return it. If you are on any other island, it doesn't matter who you rent from or what you rent (including a Hummer). If you off-road, you are technically violating your rental agreement. If you violate your rental agreement, you void ALL your insurance (no matter who it's with; including rental insurance you're using from back home). We've heard horror stories of how folks have to pay off their ENTIRE rental because they damaged it or got it stuck somewhere off-roading. And you cannot leave the state before you settle all debts. Don't make a costly mistake - stay legal and stay on the roads!
2.) We recommend you book your rental online as many rental companies have online specials. Booking your rental together with a flight and/or accommodation will also save you money.
3.) Book as far in advance as possible. Depending on when you travel the rates may increase or decrease according to demand from other travelers. We always figure that planning ahead on this never hurts.
4.) When possible, rent two, three, five day, or week long packages as these are generally priced lower than any other.
5.) At the rental counter you'll be given three options in regards to refueling the vehicle. Two are good deals and one is not. You can choose to prepay for a tank of gas, usually at a special (lower) rate, which allows you to return it with any amount of fuel in the tank. Or you can choose to refuel before you return the car at the going rate for gas at stations near the airport. The final option is the most expensive option, to return the car and let the rental agency refuel it for you. Just be warned that their refueling rate is significantly higher than the going rate for gasoline at stations (up to two dollars more!).
So which option is best for you? Here's the benefits of each option, and some price estimates to go along.
If you choose the prepay option you'll be charged at the counter for a full tank of gas. The rates that most rental agencies charge per gallon are typically only pennies cheaper than the going rate on the island, but it's still a way to save some money. Of course you are not reimbursed for what fuel remains in the tank when you return the car. So if you return the car with a half tank of gas then you paid for something you didn't use. The prepay option is ideal for people who don't want to worry about refueling their car on the way back to the airport or who think they'll return the car nearly empty.
The other option you have is to refuel the car yourself before you drive back to the airport. This can be the cheapest alternative for many folks because you leave with a "free" tank of gas at the time of your rental, and you're only responsible for filling the tank back up when you return. Ultimately you pay only for what you used on the island. This is the best option if you plan to do a lot of driving on the island and have the time to refuel on your way to the airport. Just keep in mind that gas stations are only allowed to get so close to airports for security reasons, so make sure you top the car off when you return it.
The last option we do not recommend because it's the most expensive. If you don't prepay for your fuel, and you return the vehicle with a half tank, the rental company will charge you a much higher rate to refuel the car once back in their possession. The rate is usually criminal, and thus we highly advise you not to choose this option unless you absolutely have to.
6.) As far as insurance goes, expect to hear the sales pitch telling you it's needed. We can almost hear the statistics now on Hawai'i roads and accident costs. Don't let the rental folks talk you into anything you don't need. Consider the following: The rental insurance they want to sell you is temporary insurance, but the fact is, you might very well already have it. Check with your insurance agent for your personal vehicles to see if you're covered. If you do already have rental insurance, you can save a bundle by avoiding this cost. Second, check with the credit card company you make the purchase with, as they may also provide you protection as a cardholder. Just be sure to clarify with your credit card company what they cover and what the limits are. We should also refer back to Tip #1 here. If you do off-road, any insurance you do have (regardless of who it's with) is void - even your own insurance will only cover you for what's legal by the rental agreement.
7.) Speaking of credit cards, expect to pay with one. Some companies may accept checks, but they definitely won't accept cash. Also, don't just assume if you book ahead of time that you've paid all the fees associated with the rental. Occasionally additional fees will be charged at the time of the rental, one of which we detail next.
8.) The "under age" curse of renting in Hawai'i. This is one of the biggest and most despised surprises to all renters under the age of 25. Welcome honeymooner's! Yeah right!. In Hawai'i you are obligated by law to pay an "underage" fee for the 'risk' the rental companies must take to insure you to drive on the island. This fee can be as much as $25-$75 a day or more and quickly adds up. Also as far as we know, if you're under 21, you can't even rent a vehicle on Hawai'i.
9.) If your car breaks down while on Hawai'i be sure to call the 800 number provided with your rental package. If you fail to call them first in the event of an emergency, your expenses may not be covered. After you call them, call your own insurance to see if they'll cover any costs the rental agency won't (like a blown tire, etc).
10.) If you arrive and are told the model you reserved is not available, or isn't what you were looking for, you'll have the opportunity to "upgrade/downgrade" accordingly. This could be a bait and switch tactic, or they may just be overstocked on larger models, so be careful. If you're good at negotiating you might be able to get a larger vehicle at a really good rate, so don't feel shy about pressing them for the better vehicle at the same rate you already paid. After all, it's their fault for not having your model. Usually you'll be given the upgrade at the same rate, but if not, definitely argue it. If all else fails, cancel your rental with them and go to a competitor. If they actually let you walk away from the desk empty-handed you're probably better at another company anyway.
11.) Be prepared to wait once you arrive (up to two hours), the lines at most rental counters can be long and require patience. Some folks like to use the split-up tactic of having one individual head for the rental counter as soon as they get off the plane while the other waits for the luggage. This used to work fairly well, but since more and more folks are doing it - it's 50/50 now. Plus, if you land right after another large flight, you can count on waiting even longer. But relax, you're in Hawai'i now!
OK, just so we're thorough, we want to make sure you know the real policies regarding any "off-roading," including 4x4 rentals. This is specifically meant for visitors to the Big Island, though it's applicable state wide. While policies and regulations about where you can and cannot go in a rental are always changing, we can tell you this: currently there is NO rental agency that allows off-roading on the Big Island (or any other island) without severe risks. A little research might lead you to one of the few Big Island companies (Harper's being the most prominent) allowing visitors to drive on Saddle Road and to the summit of Mauna Kea. However there is some fuzziness about how much off-roading you can do with these rentals. We can promise you they are all very strict about damage and will check the car very thoroughly, including with mirrors under the car, when you return it. If you are on any other island, it doesn't matter who you rent from or what you rent (including a Hummer). If you off-road, you are technically violating your rental agreement. If you violate your rental agreement, you void ALL your insurance (no matter who it's with; including rental insurance you're using from back home). We've heard horror stories of how folks have to pay off their ENTIRE rental because they damaged it or got it stuck somewhere off-roading. And you cannot leave the state before you settle all debts. Don't make a costly mistake - stay legal and stay on the roads!
2.) We recommend you book your rental online as many rental companies have online specials. Booking your rental together with a flight and/or accommodation will also save you money.
3.) Book as far in advance as possible. Depending on when you travel the rates may increase or decrease according to demand from other travelers. We always figure that planning ahead on this never hurts.
4.) When possible, rent two, three, five day, or week long packages as these are generally priced lower than any other.
5.) At the rental counter you'll be given three options in regards to refueling the vehicle. Two are good deals and one is not. You can choose to prepay for a tank of gas, usually at a special (lower) rate, which allows you to return it with any amount of fuel in the tank. Or you can choose to refuel before you return the car at the going rate for gas at stations near the airport. The final option is the most expensive option, to return the car and let the rental agency refuel it for you. Just be warned that their refueling rate is significantly higher than the going rate for gasoline at stations (up to two dollars more!).
So which option is best for you? Here's the benefits of each option, and some price estimates to go along.
If you choose the prepay option you'll be charged at the counter for a full tank of gas. The rates that most rental agencies charge per gallon are typically only pennies cheaper than the going rate on the island, but it's still a way to save some money. Of course you are not reimbursed for what fuel remains in the tank when you return the car. So if you return the car with a half tank of gas then you paid for something you didn't use. The prepay option is ideal for people who don't want to worry about refueling their car on the way back to the airport or who think they'll return the car nearly empty.
The other option you have is to refuel the car yourself before you drive back to the airport. This can be the cheapest alternative for many folks because you leave with a "free" tank of gas at the time of your rental, and you're only responsible for filling the tank back up when you return. Ultimately you pay only for what you used on the island. This is the best option if you plan to do a lot of driving on the island and have the time to refuel on your way to the airport. Just keep in mind that gas stations are only allowed to get so close to airports for security reasons, so make sure you top the car off when you return it.
The last option we do not recommend because it's the most expensive. If you don't prepay for your fuel, and you return the vehicle with a half tank, the rental company will charge you a much higher rate to refuel the car once back in their possession. The rate is usually criminal, and thus we highly advise you not to choose this option unless you absolutely have to.
6.) As far as insurance goes, expect to hear the sales pitch telling you it's needed. We can almost hear the statistics now on Hawai'i roads and accident costs. Don't let the rental folks talk you into anything you don't need. Consider the following: The rental insurance they want to sell you is temporary insurance, but the fact is, you might very well already have it. Check with your insurance agent for your personal vehicles to see if you're covered. If you do already have rental insurance, you can save a bundle by avoiding this cost. Second, check with the credit card company you make the purchase with, as they may also provide you protection as a cardholder. Just be sure to clarify with your credit card company what they cover and what the limits are. We should also refer back to Tip #1 here. If you do off-road, any insurance you do have (regardless of who it's with) is void - even your own insurance will only cover you for what's legal by the rental agreement.
7.) Speaking of credit cards, expect to pay with one. Some companies may accept checks, but they definitely won't accept cash. Also, don't just assume if you book ahead of time that you've paid all the fees associated with the rental. Occasionally additional fees will be charged at the time of the rental, one of which we detail next.
8.) The "under age" curse of renting in Hawai'i. This is one of the biggest and most despised surprises to all renters under the age of 25. Welcome honeymooner's! Yeah right!. In Hawai'i you are obligated by law to pay an "underage" fee for the 'risk' the rental companies must take to insure you to drive on the island. This fee can be as much as $25-$75 a day or more and quickly adds up. Also as far as we know, if you're under 21, you can't even rent a vehicle on Hawai'i.
9.) If your car breaks down while on Hawai'i be sure to call the 800 number provided with your rental package. If you fail to call them first in the event of an emergency, your expenses may not be covered. After you call them, call your own insurance to see if they'll cover any costs the rental agency won't (like a blown tire, etc).
10.) If you arrive and are told the model you reserved is not available, or isn't what you were looking for, you'll have the opportunity to "upgrade/downgrade" accordingly. This could be a bait and switch tactic, or they may just be overstocked on larger models, so be careful. If you're good at negotiating you might be able to get a larger vehicle at a really good rate, so don't feel shy about pressing them for the better vehicle at the same rate you already paid. After all, it's their fault for not having your model. Usually you'll be given the upgrade at the same rate, but if not, definitely argue it. If all else fails, cancel your rental with them and go to a competitor. If they actually let you walk away from the desk empty-handed you're probably better at another company anyway.
11.) Be prepared to wait once you arrive (up to two hours), the lines at most rental counters can be long and require patience. Some folks like to use the split-up tactic of having one individual head for the rental counter as soon as they get off the plane while the other waits for the luggage. This used to work fairly well, but since more and more folks are doing it - it's 50/50 now. Plus, if you land right after another large flight, you can count on waiting even longer. But relax, you're in Hawai'i now!
Hawaii Safety and Hazards
The islands of Hawaii could each easily be described as paradise. But even paradise has its hazards and we'd be foolish not to at least educate you on a few of them. Please make sure you and those who travel with you know about these hazards. Our statements below are rather candid because we want you to know the truth about the place you are visiting. This isn't Disneyland; it is often wild, rough, and natural law prevails out here. The more you know, the better prepared you are to avoid the hazards of our beautiful islands. We've made this short section a chapter in all of our recent guidebooks, and that should show how much emphasis we put on this subject.
Wildlife, Plants, & Insects (All Islands)For the most part you are very safe on the Hawaiian Islands from all animal and plant life. There are no large predators or snakes, and there are few plants that will cause irritation when hiking (no poison oak/ivy for example). However, other hazards still exist.
The main culprit we've come across in the animal world is actually an insect, the centipede (seen here). In Hawai'i these aggressive insects carry quite a punch and getting bit or stung by one is not what you want during your visit to the islands. The resorts usually spray for them very well, but be careful with any shoes left outside during the night, etc. Another insect that gets a lot of attention is the Cane Spider. But it's mostly hype. The brown cane spider is mostly feared due to its appearance (size). It is about the size of a can of tuna; that includes its long legs. Typically it will run versus defend, and the bite of a cane spider is rarely dangerous. None-the-less, we wanted to give it a mention.
There are also scorpions on the drier sides of the islands, but they usually stay out of sight. Mosquitoes typically frequent the wetter sides of the islands, so prepare accordingly. Geckos are nothing to be worried about; they're the cute lizards that actually keep the bug population somewhat under control here. On the Big Island, the other cute, but pesky, resident is the coqui tree frog (seen here). Especially prevalent on the Hilo/Puna side of the island, they will likely be music to your ears the first night. By the fifth night you'll probably understand why they spray for them.The many edible plants and fruits of Hawai'i also create a hazard. Many visitors believe that they can pop just about anything in their mouths for a taste in Hawai'i, not so. Many plants here are poisonous and no fruits or plants should be eaten unless you absolutely know for sure it is safe. Remember that many plants will have similar looking fruits.
The Sun (All Islands)
The sun - A UV index of near 14+ every day speaks for itself. We recommend at least 15+ sun block in Hawai'i at all times. Don't ruin your visit by trying to get that tropical tan. The tan will be gone within a month of your return home, the memory of the burns will last a lot longer.
Streams, Rivers, & Pools (All Islands)
Our primary message here is short and sweet. Pay attention to the flow of the stream where you are and be aware of the weather inland. Streams and rivers can change flow rates and heights very quickly in the islands. Flash flooding is a regular occurrence in some places. One good rain, even far inland from where you are, can cause a stream to rise substantially. If you're crossing any streams or rock hopping, pay close attention to the weather and the water levels. Anytime you are crossing a stream or river where it empties into the ocean, we also advise crossing inland a bit. Dangerous rip currents can form in the ocean at the mouth of a river or stream. Hiking poles may be extremely useful for any crossings you do make, as they provide an extra set of limbs to help you keep your balance.
If you go swimming, make sure you don't swallow any water, and try and cover up any open wounds you have so that water can't get in them. In Hawaii leptospirosis can be found in water contaminated by animal droppings, and you do not want to get mixed up with the likes of this disease. It causes flu-like symptoms and in rare cases death.Ocean Life & The Beach (All Islands)
If you've ever been to the beach then you likely already know about the hazards of the ocean. Rip currents, sharp coral, large waves, surf, and various creatures are just a few. The most notable sea-creatures to watch out for on the Big Island are coral, jellyfish (Portuguese Man-of-War), and sea urchin's. If you plan to swim, snorkel, or scuba dive on the island, make sure to do your homework and become fully educated on the hazards of the ocean here.
Volcano Area Hazards (Big Island and portions of Maui)
The first thought that comes to mind when you hear about Hawai'i volcano danger is probably the lava hazards. In reality the 2000 degree Fahrenheit lava probably poses the least amount of danger to the sensible person. Hawai'i Volcanoes National Park and the surrounding Volcano area of the Big Island are subject to a number of hazards that are easy to overlook or just aren't something you'd expect without prior knowledge of the area. While this is mostly applicable to the Big Island, Maui is no exception providing it has many areas covered with recent (geologically speaking) lava flows as well - especially in South Maui. Let's go over a few of these hazards.
Hiking on Lava: Around the Big Island and especially at the end of Chain of Craters Road you will have the opportunity to hike over lava. You may have made note on our Hawaii Geology page, that there are two types of lava, pahoehoe and a'a flows. You also likely know that trying to walk over a'a is a fool's errand. The only lava flows that are traversable are hardened pahoehoe flows like those found at the end of Chain of Craters Road.
Currently this is the only location you can also safely approach active flows (when they are present). The dangers involved in crossing lava, even pahoehoe lava, are primarily due to the razor-like sharpness of the hardened lava. Even the pahoehoe flows are as sharp as glass, and you can easily cut yourself (especially your hands) in the event of a fall. Extreme care and/or precautions should be taken when hiking over lava. Long pants and gloves are always a good idea. The heat produced by the sun on top of the black asphalt-like lava surface deters many visitors from wearing long pants, but don't risk the injury. The pahoehoe surface is smooth but can contain all sorts of variations in the surface that can catch your foot or cause you to stumble. It is also important you remain keenly aware of the texture of the flows you are walking across, as shallow lava tubes can cave in, dropping you a few inches (or more) below the surface. If you plan to make any lengthy hikes, also be sure to bring adequate amounts of water as dehydration can occur quickly on the shade-less black lava surface.
Viewing Active Lava Flows: As a continuation of the above hazard and warning, we again encourage all visitors to be prepared for any hiking they do on hardened flows out to see active flows. When approaching active flows your body will only let you get so close before the heat forces you to stand back, but use common sense and don't attempt to get any closer than you must to view the lava safely. Lava temperatures average around 2000 degrees Fahrenheit. Do not attempt to cross any active flow up slope as active flows are often concealed in lava tubes beneath the surface, and you do not want to find one by mistake.
Do not cross any National Park boundary ropes in the park, as they are in place for your protection. The park service is fairly liberal about how close they will allow people to get to lava flows; so traversing beyond the boundaries they've set up is extremely dangerous. Usually the roped off areas are near the lava entry point into the ocean. Violent explosions, deadly steam plumes, and gases make this a treacherous area to be near. Furthermore, all lava benches are roped off for the same reason. Lava benches can easily collapse at any time spelling certain catastrophe for anyone on the bench at the time. Just two days before writing this article a 45 acre bench collapsed in a single night; yes, 45 ACRES!
Volcanic Gases & Vog: Where hot lava meets the sea, and especially at the source of the eruption, the volcano produces a deadly concoction of gases. In fact, it's estimated Kilauea puts out about 2,500 tons of sulfur dioxide a day. Enough of those fumes can kill someone almost instantly, (as if you needed another reason to stay behind those barriers the park service puts up). Even far away from the sources of these sulfur dioxide plumes visitors can experience another type of gas, Vog.Vog is a mixture of the sulfur dioxide gas, water vapor, carbon dioxide, dust, and other airborne particles. Vog exists in fairly high amounts all around the volcano area and can even wrap around the island into Kailua-Kona depending on trade wind activity. Hilo, Puna, Kohala, and the Hamakua coast are usually vog-free. Vog affects different people in different ways. Visitors with asthma and respiratory troubles will have the most problems. In our experiences with vog we've been mostly unaffected by it. It's unpleasant to smell, but it has never had any adverse affects on us. We have though, on a few occasions, experienced especially heavy vog settle upon us near the end of Chain of Craters Road (usually coming from Pu'u O'o up the pali, “cliff”) when the trade winds were blowing light. Usually this causes coughing and a burning sensation in the eyes, nose, and mouth. If possible, avoid areas where you notice a lot of vog. Usually you can see it in the air like a low cloud moving south down the coastline from the volcano (can you make it out in the photo here?). If you are caught in thick vog, try and get out of it as quickly as possible. You can call 808-885-7143 for a vog index update.
If you want more information on vog, hiking over, and viewing lava safely, please consult the park rangers inside Hawai'i Volcanoes National Park.
General Sightseeing
There are many locations on Hawai'i that are private property and we, to our best efforts, have attempted to avoid the use of such properties. If a trail says it's closed, it's closed. If you see a sign that says “Kapu” then it's off-limits. Don't explore places you're not sure about - waterfalls, pools, trails, caves, lava tubes, etc. You likely wouldn't want people exploring your backyard at home, so be mindful and respectful of residents here. Your courtesy will be greatly appreciated.
Hazards YOU Pose
It may or may not surprise you, but one of Hawai'i's greatest hazards is us, humans. If you refer to the history of Hawaii page you'll learn about Hawai'i's endemic species, or species found ONLY in Hawai'i. Thus as visitors to these islands we must remember that we ourselves are one of the greatest hazards to the rare and endangered species that live here, and only here. There are a few general guidelines to follow while on the islands.
1.) As a general rule it is best to stay away from all wildlife. In fact, you should know it's illegal to feed or touch them. That means no feeding the geese (Nene), no touching the turtles (Honu), and no swimming with the dolphins. These three issues are something we hear and witness a lot of in Hawai'i. It seems innocent enough, but consider the consequences of your casual interaction with these creatures. Nene no longer fear our cars and are being killed off at an alarming rate. The touch of a human can deliver deadly infections to the honu as it basks in the sun or swims in a shallow pool.
2.) Kapu means kapu (off-limits). Many areas that are now deemed as ecologically or culturally fragile have been made kapu (off-limits) by the government. Sensitive places include lava tubes, caves, burial grounds, heiaus (temples), etc. Please show ho'ihi (respect) for the laws that protect these beautiful and fragile places.3.) Remember that trails and roads exist for a reason. It's easy to get off the beaten path and do a bit of exploring, but remember that just off that beaten path in Hawai'i could be the home to a variety of animals and plants you might not be aware of.
4.) Don't take the lava rocks or sand home with you; it's actually even illegal to sell black sand in Hawaii. You're sure to hear the legend of Pele cursing all those who take her 'children' away from the islands. If that won't stop you, know that local airport screener's will likely confiscate any they find in your luggage.
If you follow these tips we can guarantee you that the Aloha you show will be most appreciated by all, people and animals alike. Mahalo nui!
Hawaii Waterfalls
The Hawaiian Islands are home to some of the world's most beautiful waterfalls. Below we've included links to several of the best waterfalls on the islands, most of which you can actually see without a tour or helicopter (all falls visible from the air only are noted).
On the list of falls below, we've included the height of the falls when possible, a rank (out of 5 stars), noted if it's a seasonal falls (dry in summer), and included any additional access information as necessary. If you discover a falls we've mistakenly left off this list, by all means please contact us and we'll make sure it's added. We've also broken the falls down individually by island if you'd prefer to view them that way: Maui Waterfalls, Kauai Waterfalls, and Big Island of Hawaii Waterfalls. Oahu waterfalls will be coming soon.
**Click the name any falls below for more information.
BIG ISLAND WATERFALLSRainbow Falls
----Height: Approx. 80ft | Season: Varies in flow | Access: Next to parking lot | Rating:
----Height: Approx. 80ft | Season: Varies in flow | Access: Next to parking lot | Rating:
Umauma Falls (Inside Garden - requires admission charge)
----Height: Approx. 40ft per fall (tiered) | Season: Year round | Access: Via Overlook | Rating:
----Height: Approx. 40ft per fall (tiered) | Season: Year round | Access: Via Overlook | Rating:
Hi'ilawe Falls (Visible only from within Waipio Valley)
----Height: 1200-1600ft | Season: Year round | Access: Via valley road | Rating:
----Height: 1200-1600ft | Season: Year round | Access: Via valley road | Rating:
Wai'ilikahi Falls (Visible only from within remote Waimanu Valley)
----Height: Approx. 1080ft | Season: Year round | Access: Via difficult trail/helicopter tour | Rating:
----Height: Approx. 1080ft | Season: Year round | Access: Via difficult trail/helicopter tour | Rating:
Onomea Falls (Inside Garden - requires admission charge)
----Height: Approx. 20-30ft (tiered) | Season: Year round | Access: Along trail in garden | Rating:
----Height: Approx. 20-30ft (tiered) | Season: Year round | Access: Along trail in garden | Rating:
MAUI WATERFALLSHelele'ike'oha (Blue Angel) Falls [KAPU]
----Height: Approx. 100ft | Season: Dec-April | Access: None (Private Property) | Rating:
----Height: Approx. 100ft | Season: Dec-April | Access: None (Private Property) | Rating:
Upper Hanawi Falls
----Height: Approx. 35ft | Season: Dec-April | Access: Visible from Hwy | Rating:
----Height: Approx. 35ft | Season: Dec-April | Access: Visible from Hwy | Rating:
Lower Puohokamoa Falls (Closed in late 2007)
----Height: Approx. 160ft | Season: Dec-April | Access: NA (Now Closed) | Rating:
----Height: Approx. 160ft | Season: Dec-April | Access: NA (Now Closed) | Rating:
'Ohe'o Gulch Falls (7 Sacred Pools)
----Height: Approx. 10-30ft | Season: Year round | Access: Via short trail | Rating:
----Height: Approx. 10-30ft | Season: Year round | Access: Via short trail | Rating:
Upper Puohokamoa Falls - Clearly visible from overlook within the 'Garden of Eden' (admission required)
----Height: Approx. 40ft | Season: Year round | Access: Via Overlook | Rating:
----Height: Approx. 40ft | Season: Year round | Access: Via Overlook | Rating:
Upper Waikani (Three Bears) Falls
----Height: Approx. 70ft | Season: Varies | Access: Visible from Hwy | Rating:
----Height: Approx. 70ft | Season: Varies | Access: Visible from Hwy | Rating:
Waimoku Falls
----Height: Approx. 400ft | Season: Year round | Access: Two miles along trail | Rating:
----Height: Approx. 400ft | Season: Year round | Access: Two miles along trail | Rating:
KAUAI WATERFALLSManawaiopuna Falls (via Helicopter only)
----Height: Approx. 360ft | Season: Year round | Access: Via helicopter | Rating:
----Height: Approx. 360ft | Season: Year round | Access: Via helicopter | Rating:
Wailua Falls
----Height: Approx. 80ft | Season: Year round | Access: Visible from overlook | Rating:
----Height: Approx. 80ft | Season: Year round | Access: Visible from overlook | Rating:
Waipo'o Falls
----Height: Approx. 800ft | Season: Usually year round | Access: Visible from overlooks | Rating:
----Height: Approx. 800ft | Season: Usually year round | Access: Visible from overlooks | Rating:
Kalihiwai Falls
----Height: Approx. 60ft | Season: Usually year round | Access: Via difficult hike or quick view from bridge | Rating:
----Height: Approx. 60ft | Season: Usually year round | Access: Via difficult hike or quick view from bridge | Rating:
Hawaii Gardens
The Hawaiian Islands are home to some of the worlds most beautiful gardens, arboretums, and landscapes. Below we've included links to several of the best gardens on the islands, most of which require admission, but at a price worth paying.
On the list of gardens below, we've included the admission price when possible, a rank (out of 5 stars), general location, and included any additional information as necessary. If you discover a garden we've mistakenly left off this list, by all means please contact us and we'll make sure it's added.
BIG ISLAND GARDENSMAUI GARDENS
KAUAI GARDENSNational Tropical Botanical Garden
----Admission: $35/adult (Allerton), $20/adult (McBryde) | Location: South Kauai | Rating:
----Admission: $35/adult (Allerton), $20/adult (McBryde) | Location: South Kauai | Rating:
Best time to travel to Hawaii
A question we hear frequently is "What's the best time to travel to Hawaii?" or "When should I visit Hawaii?" This question is typically followed by "What’s the weather like in Hawaii?" You can learn about the general weather conditions on our