|Nickname: The Valley Isle|
Location in the state of Hawaii
|Area||727.2 sq mi (1,883 km2)|
|Area rank||2nd largest Hawaiian Island|
|Highest elevation||10,023 ft (3,055 m)|
|Pop. density||162 /sq mi (62.5 /km2)|
The island of Maui (; Hawaiian: ['m?wwi]) is the second-largest of the Hawaiian Islands at 727.2 square miles (1,883 km2) and is the 17th-largest island in the United States. Maui is part of the State of Hawaii and is the largest of Maui County's four islands, which include Moloka?i, L?na?i, and unpopulated Kaho?olawe. In 2010, Maui had a population of 144,444, third-highest of the Hawaiian Islands, behind that of O?ahu and Hawai?i Island. Kahului is the largest census-designated place (CDP) on the island with a population of 26,337 as of 2010 and is the commercial and financial hub of the island.Wailuku is the seat of Maui County and is the third-largest CDP as of 2010 . Other significant places include K?hei (including Wailea and Makena in the Kihei Town CDP, the island's second-most-populated CDP), Lahaina (including K??anapali and Kapalua in the Lahaina Town CDP), Makawao, Pukalani, P??ia, Kula, Ha?ik?, and H?na.
Native Hawaiian tradition gives the origin of the island's name in the legend of Hawai?iloa, the navigator credited with discovery of the Hawaiian Islands. According to it, Hawai?iloa named the island after his son, who in turn was named for the demigod M?ui. The earlier name of Maui was ?Ihikapalaumaewa. The Island of Maui is also called the "Valley Isle" for the large isthmus separating its northwestern and southeastern volcanic masses.
Maui's diverse landscapes are the result of a unique combination of geology, topography, and climate. Each volcanic cone in the chain of the Hawaiian Islands is built of dark, iron-rich/quartz-poor rocks, which poured out of thousands of vents as highly fluid lava over a period of millions of years. Several of the volcanoes were close enough to each other that lava flows on their flanks overlapped one another, merging into a single island. Maui is such a "volcanic doublet," formed from two shield volcanoes that overlapped one another to form an isthmus between them.
The older, western volcano has been eroded considerably and is cut by numerous drainages, forming the peaks of the West Maui Mountains (in Hawaiian, Mauna Kahalawai). Pu?u Kukui is the highest of the peaks at 5,788 feet (1,764 m). The larger, younger volcano to the east, Haleakal?, rises to more than 10,000 feet (3,000 m) above sea level, and measures 5 miles (8.0 km) from seafloor to summit.
The eastern flanks of both volcanoes are cut by deeply incised valleys and steep-sided ravines that run downslope to the rocky, windswept shoreline. The valley-like Isthmus of Maui that separates the two volcanic masses was formed by sandy erosional deposits.
Maui's last eruption (originating in Haleakal?'s Southwest Rift Zone) occurred around 1790; two of the resulting lava flows are located (1) at Cape K?na?u between ??hihi Bay and La Perouse Bay on the southwest shore of East Maui, and (2) at Makaluapuna Point on Honokahua Bay on the northwest shore of West Maui. Although considered to be dormant by volcanologists, Haleakal? is certainly capable of further eruptions.
Maui is part of a much larger unit, Maui Nui, that includes the islands of L?na?i, Kaho?olawe, Moloka?i, and the now submerged Penguin Bank. During periods of reduced sea level, including as recently as 20,000 years ago, they are joined together as a single island due to the shallowness of the channels between them.
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The climate of the Hawaiian Islands is characterized by a two-season year, tropical and uniform temperatures everywhere (except at high elevations), marked geographic differences in rainfall, high relative humidity, extensive cloud formations (except on the driest coasts and at high elevations), and dominant trade-wind flow (especially at elevations below a few thousand feet). Maui itself has a wide range of climatic conditions and weather patterns that are influenced by several different factors in the physical environment:
Maui displays a unique and diverse set of climatic conditions, each of which is specific to a loosely defined sub-region of the island. These sub-regions are defined by major physiographic features (such as mountains and valleys) and by location on the windward or leeward side of the island.
Showers are very common; while some of these are very heavy, the vast majority are light and brief. Even the heaviest rain showers are seldom accompanied by thunder and lightning. Throughout the lowlands in summer an overwhelming dominance of trade winds produces a drier season. At one extreme, the annual rainfall averages 17 inches (430 mm) to 20 inches (510 mm) or less in leeward coastal areas, such as the shoreline from Maalaea Bay to Kaupo, and near the summit of Haleakal?. At the other extreme, the annual average rainfall exceeds 300 inches (7,600 mm) along the lower windward slopes of Haleakal?, particularly along the H?na Highway. "Big Bog," a spot on the edge of Haleakala National Park overlooking Hana at about 5,400 feet elevation had an estimated mean annual rainfall of 404.4 inches over the 30-year period of 1978 to 2007. If the islands of the State of Hawaii did not exist, the average annual rainfall on the same patch of water would be about 25 inches (640 mm). Instead, the mountainous topography of Maui and the other islands induce an actual average of about 70 inches (1,800 mm).
In the lowlands rainfall is most likely to occur throughout the year during the night or morning hours, and least likely in mid-afternoon. The most pronounced daily variations in rainfall occur during the summer because most summer rainfall consists of trade winds showers that most often occur at night. Winter rainfall in the lowlands is the result of storm activity, which is as likely to occur in the daytime as at night. Rainfall variability is far greater during the winter, when occasional storms contribute appreciably to rainfall totals. With such wide swings in rainfall, it is inevitable that there are occasional droughts, sometimes causing economic losses. These occur when winter rains fail to produce sufficient significant rainstorms, impacting normally dry areas outside the trade winds that depend on them the most. The winter of 2011-2012 produced extreme drought on the leeward sides of Moloka'i, Maui, and Island of Hawaii.
The blend of warm tropical sunshine, varying humidity, ocean breezes and trade winds, and varying elevations create a variety of microclimates. Although the Island of Maui is small, it can feel quite different in each district resulting in a unique selection of micro-climates that are typical to each of its distinctive locations: Central Maui; leeward South Maui and West Maui; windward North Shore and East Maui; and Upcountry Maui.
Although Maui's daytime temperatures average between 75 and 90 degrees year round, evening temperatures are about 15 degrees cooler in the more humid windward areas, about 18 degrees cooler in the dryer leeward areas, and cooler yet in higher elevations.
Central Maui consists primarily of Kahului and Wailuku. Kahului is literally the center of the island, and tends to keep steady, high temperatures throughout the year. The micro-climate in Kahului can be at times muggy, but it usually feels relatively dry and is often very breezy. The Wailuku area is set closer to the West Maui Mountain range. Here, more rainfall will be found throughout the year, and higher humidity levels.
Leeward side includes South Maui (Kihei, Wailea and Makena) and West Maui (Lahaina, Kaanapali and Kapalua). These areas are typically drier, with higher daytime temperature (up to 92 degrees), and the least amount of rainfall. (An exception is the high-altitude, unpopulated West Maui summit, which boasts up to 400 inches of rainfall per year on its north and east side.)
Windward side includes the North Shore (Paia and Haiku) and East Maui (Keanae, Hana and Kipahulu). Located in the prevailing, northeast trade winds, these areas have heavier rainfall levels, which increase considerably at higher elevations.
Upcountry Maui (Makawao, Pukalani, and Kula) at the 1,700- to 4,500-foot levels, provides mild heat (70s and low 80s) during the day and cool evenings. The higher the elevation, the cooler the evenings. During Maui's winter, Upper Kula can be as cold as 40 degrees in the early morning hours, and the Haleakala summit can dip below freezing.
An exception to the normal pattern is the occasional winter "Kona storms" which bring rainfall to the South and West areas accompanied by high southwesterly winds (opposite of the prevailing trade wind direction).
Maui is a leading whale-watching center in the Hawaiian Islands due to Humpback whales wintering in the sheltered ?Au?au Channel between the islands of Maui county. The whales migrate approximately 3,500 miles (5,600 km) from Alaskan waters each autumn and spend the winter months mating and birthing in the warm waters off Maui, with most leaving by the end of April. The whales are typically sighted in pods: small groups of several adults, or groups of a mother, her calf, and a few suitors. Humpbacks are an endangered species protected by U.S. federal and Hawai?i state law. There are estimated to be about 22,000 humpbacks in the North Pacific. Although Maui's Humpback face many dangers, due to pollution, high-speed commercial vessels, and military sonar testing, their numbers have increased rapidly in recent years, estimated at 7% growth per year.
Maui is home to a large rainforest on the northeastern flanks of Haleakal?, which serves as the drainage basin for the rest of the island. The extremely difficult terrain has prevented exploitation of much of the forest.
Agricultural and coastal industrial land use has had an adverse effect on much of Maui's coastal regions. Many of Maui's extraordinary coral reefs have been damaged by pollution, run-off, and tourism, although finding sea turtles, dolphins, and Hawaii's celebrated tropical fish, is still common. Leeward Maui used to boast a vibrant dry 'cloud forest' as well but this was destroyed by human activities over the last three hundred years.
Polynesians from Tahiti and the Marquesas Islands were the original people to populate Maui. The Tahitians introduced the kapu system, a strict social order that affected all aspects of life and became the core of Hawai?ian culture. Modern Hawai?ian history began in the mid-18th century. Kamehameha I, king of the island of Hawai?i, invaded Maui in 1790 and fought the inconclusive Battle of Kepaniwai, but returned to Hawai?i to battle a rival, finally subduing Maui a few years later.
On November 26, 1778, explorer James Cook became the first European to see Maui. Cook never set foot on the island because he was unable to find a suitable landing. The first European to visit Maui was the French admiral Jean-François de Galaup, comte de Lapérouse, who landed on the shores of what is now known as La Perouse Bay on May 29, 1786. More Europeans followed: traders, whalers, loggers (e.g., of sandalwood) and missionaries. The latter began to arrive from New England in 1823, settling in Lahaina, which at that time was the capital. They clothed the natives, banned them from dancing hula, and greatly altered the culture. The missionaries taught reading and writing, created the 12-letter Hawaiian alphabet, started a printing press in Lahaina, and began writing the islands' history, which until then was transmitted orally. Ironically, the missionaries both altered and preserved the native culture. The religious work altered the culture while the literacy efforts preserved native history and language. Missionaries started the first school in Lahaina, which still exists today: Lahainaluna Mission School, which opened in 1831.
At the height of the whaling era (1843-1860), Lahaina was a major center. In one season over 400 ships visited with up to 100 anchored at one time in L?hain? Roads. Ships tended to stay for weeks rather than days, fostering extended drinking and the rise of prostitution, against which the missionaries vainly battled. Whaling declined steeply at the end of the 19th century as petroleum replaced whale oil.
Kamehameha's descendants reigned until 1872. They were followed by rulers from another ancient family of chiefs, including Queen Lili?uokalani, deposed in the 1893 when overthrow of the Kingdom of Hawaii by American business interests. One year later, the Republic of Hawaii was founded. The island was annexed by the United States in 1898 and made a territory in 1900. Hawai?i became the 50th U.S. state in 1959.
In 1937, Vibora Luviminda trade union conducted the last strike action of an ethnic nature in the Hawai?ian Islands against four Maui sugarcane plantations, demanding higher wages and the dismissal of five foremen. Manuel Fagel and nine other strike leaders were arrested, and charged with kidnapping a worker. Fagel spent four months in jail while the strike continued. Eventually, Vibora Luviminda made its point and the workers won a 15% increase in wages after 85 days on strike, but there was no written contract signed.
Maui was centrally involved in the Pacific Theater of World War II as a staging center, training base, and rest and relaxation site. At the peak in 1943-44, more than 100,000 soldiers were there. The main base of the 4th Marine Division was in Haiku. Beaches were used to practice landings and train in marine demolition and sabotage.
The island experienced rapid population growth through 2007, with K?hei one of the most rapidly growing towns in the United States (see chart, below). The island attracted many retirees, adding service providers for them to the rapidly increasing number of tourists. Population growth produced strains, including traffic congestion, housing affordability, and access to water.
Most recent years have brought droughts, resulting in the ??ao aquifer being drawn at possibly unsustainable rates above 18 million U.S. gallons (68,000 m3) per day. Recent estimates indicate that the total potential supply of potable water on Maui is around 476 million U.S. gallons (1,800,000 m3) per day, virtually all of which runs off into the ocean.
Sugar cane cultivation once used over 80% of the island's managed water supply. One pound of refined sugar requires one ton of water to produce. Water for sugar cultivation comes mostly from the streams of East Maui, routed through a network of tunnels and ditches hand dug by Chinese labor in the 19th century. In 2006, the town of Paia successfully petitioned the County against mixing in treated water from wells known to be contaminated with both EDB and DBCP from former pineapple cultivation in the area (Environment Hawaii, 1996). Agricultural companies have been released from all future liability for these chemicals (County of Maui, 1999). In 2009, the Office of Hawaiian Affairs and others successfully argued in court that sugar companies should reduce the amount of water they take from four streams.
In the 2000s, controversies over whether to continue rapid real-estate development, vacation rentals in which homeowners rent their homes to visitors, and Hawaii Superferry preoccupied local residents. In 2003, Corey Ryder of the Earth Foundation gave a presentation regarding the unique situation on Maui, "Hazard mitigation, safety & security", before the Maui County Council. In 2009, the county approved a 1,000-unit development in South Maui in the teeth of the financial crisis. Vacation rentals are now strictly limited, with greater enforcement than previously. Hawaii Superferry, which offered transport between Maui and Oahu, ceased operations in May 2009, ended by a court decision that required environmental studies from which Governor Linda Lingle had exempted the operator.
The major industry on Maui is tourism. Other large sectors include retail, health care, business services and government. Maui also has a significant presence in agriculture and information technology.
Maui's primary agriculture products are corn and other seeds, fruits, cattle and vegetables. Specific products include coffee, macadamia nuts, papaya, flowers and fresh pineapple. Historically, Maui's primary products were sugar and pineapple.Maui Land & Pineapple Company and Hawaiian Commercial and Sugar Company (HC&S, a subsidiary of Alexander and Baldwin Company) dominated agricultural activity. In 2016, sugar production ended. Haliimaile Pineapple Co. grows pineapple on former Maui Land & Pineapple Co. land.
In November 2014, a Maui County referendum enacted a moratorium on genetically engineered crops. Shortly thereafter Monsanto and other agribusinesses obtained a court injunction suspending the moratorium.
The Maui High Performance Computing Center (MHPCC) at the Air Force Maui Optical and Supercomputing observatory in K?hei is a United States Air Force research laboratory center that is managed by the University of Hawaii. It provides more than 10 million hours of computing time per year to the research, science and military communities.
Another promoter of high technology on the island is the Maui Research and Technology Center, also located in Kihei. The MRTC is a program of the High Technology Development Corporation (HTDC), an agency of the State of Hawaii, whose focus is to facilitate the growth of Hawaii's commercial high-technology sector.
Maui is an important center for advanced astronomical research. The Haleakala Observatory was Hawaii's first astronomical research and development facility, operating at the Maui Space Surveillance Site (MSSS) electro-optical facility. "At the 10,023-foot summit of the long dormant volcano Haleakala, operational satellite tracking facilities are co-located with a research and development facility providing superb data acquisition and communication support. The high elevation, dry climate, and freedom from light pollution offer virtually year-round observation of satellites, missiles, man-made orbital debris, and astronomical objects."
Snorkeling is one of the most popular activities on Maui. There are over 30 beaches and bays to snorkel at around the island. The Hawaiian Island of Maui has been voted "Best Island in the World" because of the nice weather environment and due to the fact that Maui has the most swimmable beaches. No matter where you are on the island of Maui, you are very close to the most beautiful beaches in the world to go snorkeling. Hawaiian Islands are known for having year round trade winds. Maui's trade winds tend to come in from the northeast, making the most popular places to snorkel on the south and west shores of Maui. Having many mountains on Maui, helps with the trade winds not being able to reach the beaches located on the south and west of the island, making the ocean water very clear and peaceful. Snorkeling is a must do when visiting the island of Maui.
One of the most popular activities in Maui is snorkeling in some of the most beautiful beaches. Many people travel thousands of miles, from all over the world to go snorkeling in Maui, Hawaii to see all different kinds of tropical fish and other wildlife. On the island of Maui, a very admired beach by both locals and tourists is Honolua Bay. Honolua Bay is located on the northwest side of the island and is in a very secluded location about 20 minutes away from any hotel or resort. A feature special to Honolua Bay is that it is a Marine Reserve, meaning that there is no fishing allowed, preserving the diversity and population of the magnificent sea-life. While snorkeling in Honolua Bay, it is very common to see a very diverse population of fish and even occasionally, sea turtles. Honolua Bay is also very popular due to the gorgeous area around the bay. The bay is surrounded by many cliffs, greenery, and very blue ocean water. Another amazing unique feature of the bay is how you get to the shore. Upon arriving, you walk through a massive forest with tons of trees, vines, birds, and a little creek, leading to the ocean.
Maui is a well known destination for windsurfing. Kanaha Beach Park is a very well-known windsurfing spot and may have stand-up paddle boarders or surfers if there are waves and no wind. Windsurfing has evolved on Maui since the early 1980s when it was recognized as an ideal location to test equipment and publicize the sport.
One of the most popular sports in Hawaii. Ho'okipa Beach Park is one of Maui's most famous surfing and windsurfing spots. Other famous or frequently surfed areas include Slaughterhouse Beach, Honolua Bay, Pe'ahi (Jaws), and Fleming Beach. The north side of Maui absorbs the most swell during the winter season and the south and west in the summer time. Due to island blocking, summer south swells tend to be weak and rare.
One of the newest sports on Maui is Kiteboarding/Surfing. Kanaha Beach Park is where beginner, intermediate and advanced Kiters gather. It is known as Kite Beach. Kiters share the water with Windsurfers who have dominated the area since the early 1980s. Since 2008 there has been an explosion in the number of Kiters mostly due to advances in equipment and safety.
The H?na Highway runs along the east coast of Maui, curving around mountains and passing by black sand beaches and waterfalls. Haleakal? National Park is home to Haleakal?, a dormant volcano. Snorkeling can be done at almost any beach along the Maui coast. Surfing and windsurfing are also popular on Maui.
The main tourist areas are West Maui (K??anapali, Lahaina, N?pili-Honok?wai, Kahana, Napili, Kapalua) and South Maui (K?hei, Wailea-M?kena). The main port of call for cruise ships is located in Kahului. There are also smaller ports located at Lahaina Harbor (located in Lahaina) and Ma?alaea Harbor (located between Lahaina and Kihei). Lahaina is one of the main attractions on the island with an entire street of shops and restaurants which leads to a wharf where many set out for a sunset cruise or whale watching journey. Known locally as Lahainatown, it has a long and diverse history from its Hawaiian population beginnings to the arrival of travelers and settlers and its use as a significant whaling port.
Maui County welcomed 2,207,826 tourists in 2004 rising to 2,639,929 in 2007 with total tourist expenditures north of US$3.5 billion for the Island of Maui alone. While the island of O?ahu is most popular with Japanese tourists, the Island of Maui appeals to visitors mostly from the U.S. mainland and Canada: in 2005, there were 2,003,492 domestic arrivals on the island, compared to 260,184 international arrivals.
While winning many travel industry awards as Best Island In The World in recent years concerns have been raised by locals and environmentalists about the overdevelopment of Maui. A number of activist groups, including Save Makena have gone as far as taking the government to court to protect the rights of local citizens.
Throughout 2008 Maui suffered a major loss in tourism compounded by the spring bankruptcies of Aloha Airlines and ATA Airlines. The pullout in May of the second of three Norwegian Cruise Line ships also hurt. Pacific Business News reported a $166 million loss in revenue for Maui tourism businesses.
The Maui Public Bus Transit System is a county-funded program that provides transportation around the island for nominal fares.
Three airports provide air service to Maui:
There are two hospitals on the island of Maui. The first, Maui Memorial Medical Center, is the only acute care hospital in Maui County. It is centrally located in the town of Wailuku approximately 4 miles from Kahului Airport. The second, Kula Hospital, is a critical access hospital located on the southern half on the island in the rural town of Kula. Kula Hospital, along with Lanai Community Hospital (which is located in Maui County but on the neighboring island of Lanai), are affiliates of Maui Memorial Medical Center. All three hospitals are open 24/7 for emergency access. Although not technically a hospital or emergency room, Hana Health Clinic (or Hana Medical Center), located in the remote town of Hana on the southeastern side of the island, works in cooperation with American Medical Response and Maui Memorial Medical Center to stabilize and transport patients with emergent medical conditions. It too is open 24/7 for urgent care and emergency access.
Maui is twinned with: