Maui | Tourism Sight

The island of Maui 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.[4] Maui is part of the State of Hawaiʻi and is the largest of Maui County's four islands, bigger than Molokaʻi, Lānaʻi, and unpopulated Kahoʻolawe. In 2010, Maui had a population of 144,444, third-highest of the Hawaiian Islands, behind that of Oʻahu and Hawaiʻi 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.[5] Wailuku is the seat of Maui County and is the third-largest CDP as of 2010. Other significant places include Kīhei (including Wailea and Makena in the Kihei Town CDP, which is the second-most-populated CDP in Maui); Lahaina (including Kāʻanapali and Kapalua in the Lahaina Town CDP); Makawao; Pāʻia; Kula; Haʻikū; and Hāna.
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.
Looking into the Haleakalā crater
A beach in Maui, Hawaii
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). Puʻu Kukui is the highest of the peaks at 5,788 feet (1,764 m). The larger, younger volcano to the east, Haleakalā, rises to more than 10,000 feet (3,000 m) above sea level, and measures 5 miles (8.0 km) from seafloor to summit, making it one of the world's tallest mountains.
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 Haleakalā's Southwest Rift Zone) occurred around 1790; two of the resulting lava flows are located (1) at Cape Kīnaʻu between ʻĀhihi 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, Haleakalā is certainly capable of further eruptions.
Maui is part of a much larger unit, Maui Nui, that includes the islands of Lānaʻi, Kahoʻolawe, Molokaʻi, 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.
Showers are very common; while some of these are very heavy, the vast majority are light and brief — a sudden sprinkle of rain and it's over. 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 Haleakalā. At the other extreme, the annual average rainfall exceeds 300 inches (7,600 mm) along the lower windward slopes of Haleakalā, particularly along the Hāna Highway. 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 actual average is about 70 inches (1,800 mm). Thus, the islands extract from the air that passes over them about 45 inches (1,100 mm) of rainfall that otherwise would not fall. The mountainous topography of Maui and the other islands is responsible for this added water bonus.
Kahikinui coastline near Kaupo
Daily variations in rainfall
In the lowlands, throughout the year, rainfall is most likely to occur during the night or morning hours, and is least likely to occur 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. The real drought years are the ones where the winter rains fail, with too few significant rainstorms. Droughts hit hardest in the normally dry areas that depend on winter storms for their rainfall and receive little rain from the trade wind showers. The winter of 2011-2012 has had extreme drought on the leeward sides of Moloka'i, Maui, and Island of Hawaii.
Maui is a leading whale-watching center in the Hawaiian Islands due to Humpback whales wintering in the sheltered ʻAuʻau 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 Hawaiʻi state law. There are estimated to be about 10,000 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 Haleakalā, 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, runoff, and tourism, although finding sea turtles, dolphins, and Hawai'i'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, were the original peoples to populate Maui. The Tahitians introduced the kapu system, a strict social order that affected all aspects of life and became the core of Hawaiian culture. Modern Hawaiian history began in the mid-18th century. King Kamehameha I, king of Hawaii's "Big Island," invaded Maui in 1790 and fought the inconclusive Battle of Kepaniwai, but returned to Hawaii to battle a rival, finally subduing Maui a few years later.

On November 26, 1778, explorer Captain 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 La Pérouse, 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.[12] 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.
Japanese laborers on Maui harvesting sugar cane in 1885.
At the height of the whaling era (1843–1860), Lahaina was a major whaling center with anchorage in Lāhainā Roads; in one season over 400 ships visited Lahaina with 100 berthed at one time. Ships tended to stay for weeks rather than days, which explains the drinking and prostitution in the town at that time, 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 Liliuokalani who ruled in 1893 when the monarchy was overthrown. 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. Hawaii became the 50th U.S. state in 1959.
In 1937, Vibora Luviminda trades union conducted the last labor strike of an ethnic nature in the Hawaiian 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 for rest and relaxation. 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 (e.g., in Kīhei) were used to practice landings and train in marine demolition and sabotage.
The island experienced rapid population growth through 2007, when Kīhei was one of the most rapidly growing towns in the United States (see chart, below). The island attracted many retirees and many others came to provide services to them and to the rapidly increasing number of tourists. Population growth produced its usual strains, including traffic congestion, housing affordability, and access to water.

Most recent years have brought droughts and the ʻĪao aquifer is being drawn from rates above 18 million U.S. gallons (68,000 m3) per day, possibly more than the aquifer can sustain. 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, many times greater than any foreseeable demand.

Sugar cane cultivation once used over 80% of the island's water supply (The Water Development Plan of Maui, 1992 – Present?). One pound of refined sugar requires one ton of water to produce.[citation needed] Water for sugar cultivation comes mostly from the streams of East Maui, routed though 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 1974, Emil Tedeschi of the Napa Valley winegrower family of Calistoga, California, established the first and only Hawaiian commercial winery, the Tedeschi Winery at Ulupalakua Ranch.
In the 2000s, controversies over whether to continue rapid real-estate development, so-called "vacation rentals" in which homeowners rent their homes to visitors, and Hawaii Superferry preoccupied local residents. In 2003, Corey Ryder of the Earth Foundation presented regarding the unique situation on Maui in "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.