Hanauma ( /ˌhɑːnəˈuːmə/ ; Hawaiian: [həˈnɔumə] ) [1] is a marine embayment formed within a tuff ring and located along the southeast coast of the Island of Oʻahu in the Hawaii Kai neighborhood of East Honolulu, in the Hawaiian Islands. [2]
Hanauma is one of the most popular tourist destinations on the Island and has suffered somewhat from overtourism. At one time, this popular tourist destination accommodated over three million visitors per year. In 1956, dynamite was used to clear portions of the reef to make room for telephone cables linking Hawaii to the west coast of the US. [3]
The prefix hana means bay in the Hawaiian language therefore the name is uma bay. There are two etymological interpretations of the second part of its name. [4] One interpretation derives it from the Hawaiian word for curve, referring to either the shape of the feature or to the shape of the indigenous canoes that were launched there. [4] Another stems from the indigenous hand-wrestling game known as "Uma". [4]
Hanauma is both a Nature Preserve and a Marine Life Conservation District (the first of several established in the State of Hawaiʻi). Reflecting changes in attitude, its name has changed over time from Hanauma Bay Beach Park to Hanauma Bay Nature Preserve. [5] Visitors are required by law to refrain from mistreating marine animals or from touching, walking, or otherwise having contact with coral heads, which appear much like large rocks on the ocean floor (here, mostly seaward of the shallow fringing reef off the beach). It is always recommended to avoid contacting coral or marine rocks as cuts to the skin can result and neglecting such wounds may bring medical problems.
About 400 species of fish are known to inhabit the bay. [6] Hanauma Bay is known for its abundance of Green sea turtles, Chelonia mydas, known as Honu. Hanauma is a nursery ground for the immature turtles, which have their nesting grounds at French Frigate Shoals. [7] It is also known for its abundance of parrotfish.
Coral bleaching due to global warming has affected the coral reefs in Hanauma. In 2014 and 2015, 47% of the corals at Hanauma Bay Nature Preserve suffered from coral bleaching, close to 10% of the corals in the nature preserve died. [8]
The Hawaiian Islands are a group of volcanoes that have risen up over a hot spot, which is a section of the Earth's surface that has exhibited volcanism for an extended period of time. Volcanic chains such as the Hawaiian Islands form as a result of the movement of a tectonic plate across fixed hot spot beneath the surface. In the case of the Hawaiian Islands, the Pacific plate has moved slowly northwestward over such a hotspot.
Approximately 3.9 million years ago, the Waiʻanae volcano created the island of Oʻahu. About 2.5 million years ago, the Koʻolau volcano breached the ocean's surface and continued to grow in elevation until about 1.7 million years ago, when it went dormant. Most of the eastern or windward portion of Oʻahu are remnants of this volcano. Most of the familiar geographic landmarks of eastern Oʻahu were created by eruptions from Koʻolau from about 500,000 to 10,000 years ago. The eastern flank of the Koʻolau volcano including the caldera slid into the sea, leaving the Koʻolau mountain range that can be seen today on the windward side of the island.
The Hanauma Crater was created about 32,000 years ago during the Honolulu volcanic series, the latest (and perhaps final) round of volcanic activity to occur on Oʻahu. [9] Tens of thousands of years ago, a series of volcanic vents opened along the southeast shoreline of Oʻahu. Unlike the gentle lava flows currently building the island of Hawaiʻi, the late-stage eruptions on Oʻahu were most often short-lived violent explosions. The volcanic vents that formed Hanauma Crater opened on the sea floor. Upwelling magma vaporized the ocean water and steam explosions blew the magma into fine ash. The explosions built cones or rings of ash, which solidified into tuff. The eruptions shattered the sea floor—coral reef and basalt—and scattered pieces that are now embedded in the tuff. Wave erosion eventually cut through the low, southeast wall of the crater, forming the current bay. [2]
Due to the lack of fresh water in the vicinity, the area was not inhabited, although archeologists have found fishing tools and other indications of human presence there. [4] The bay was used as a recreational area by aliʻi (Hawaiian nobility), including King Kamehameha and Queen Ka‘ahumanu, who fished, entertained visitors, and sponsored games there. [3] It was also used as a layover and as a navigational lookout point, since the waters between Oʻahu and Molokaʻi are at times difficult. [3]
Hanauma Bay was purchased from the Bernice Pauahi Bishop estate by the City and County of Honolulu, and subsequently opened for public use. It was initially a favorite fishing and picnic spot for residents who were willing to travel out to the bay. In the 1930s the road along Hanauma Bay's corner of Oahu was paved and a few other amenities provided that made it easier to visit the beach and reef. After the 1941 attack on Pearl Harbor, barbed wire was placed at the beach and a bunker was constructed for use by sentries. [4] The Bay area reopened after the war and became even more visitor friendly after blasting in the reef for a transoceanic cable provided room for swimming. Hawaii-themed films and television shows, including Blue Hawaii , Paradise, Hawaiian Style , Tora! Tora! Tora! , Hawaii Five-O , and Magnum, P.I. , shot footage at the bay. [10]
In 1967, it was set apart by the State division of Fish and Game as a Marine Protected Area, a term used generically to describe any marine area that had some or all of its resources protected. In Hanauma Bay's case everything became protected, from the fish to the reef, to the sand itself. A volunteer group set up a booth at the beach and began teaching visitors about conservation of the reef and fish who lived there. More changes in the 1970s by the City cleared more area in the reef for swimming, made an additional parking lot, and shipped in white sand from the North Shore, leaving Hanauma Bay increasingly more attractive to visitors.
By the late 1980s, the bay had become a major attraction on Oahu. Tourists were brought in by the busload and sometimes as many as 13,000 visitors descended on the beach in one day. Most were uneducated about the fragile marine ecosystem and, unwittingly, "these crowds stirred up sediment, disturbed and trampled the coral and algae, dropped trash, fed the fish and left a slick of suntan lotion on the bay's surface." [11] Consequently, the beautiful multicolored coral reef closest to the beach died; only its blackened skeleton is visible today.
By 1990, overuse of the beach and surrounding area was a real problem, with visitors walking on the reef, swarming the surrounding areas, parking on the grass and on the sides of the road. Commercial filming was banned during that year. [10] Measures were taken to limit use and so visitor access was limited to the parking lot, and when it was full everyone after was turned away. In 1997, the city of Honolulu levied an entrance fee on non-residents of the state, leading to a class action lawsuit by a visitor, which was settled in favor of the city during 2004. [12] [13] Then in August 2002 the Marine Education Center was opened at the entrance to the bay, where still today new visitors must watch a short film and receive instruction about conservation of the Bay's resources. Upon watching the film, visitors are allowed to sign a form and skip any subsequent film if they should return within the following 365 days.
Prior to 2020, Hanauma Bay saw an average of 3,000 visitors a day, with peak days reaching up to 10,000, or about 1 million per year – the majority of them being tourists. [14] One of the largest threats to the bay is the approximately 412 lb (187 kg) of sunscreen that was deposited into Hanauma Bay every day. [15] Sunscreen containing oxybenzone and octinoxate has been banned from the Hawaiian islands due to the deadly effects it has on coral reefs; however, sunscreens that do not have those harsh chemicals still have an effect on the reef's survival. [16] The National Centers for Coastal Ocean Science (NCCOS) has found from oceanographic models that it takes approximately 50 hours for sunscreen deposited in a single day to be cycled out of Hanauma Bay. [17] Hanauma Bay received sunscreen that would take two days to get rid of, but since the Bay never closed, the reef would not have the necessary time to recover. The COVID-19 pandemic caused the state park to see record lows, with this they also discovered the rehabilitation of the Hanauma Bay reef. The reservation system has implemented limits it to 1000 visitors per day, and the park is closed on Mondays and Tuesdays as well as holidays to give the fish a break from all the people disturbing their feeding, breeding, and other natural cycles that allow the reef to process the damage done by sunscreen pollution. [14] The park has since been limited to 720 guests per day and requires online reservations for all non-residents. [18] Upon entry, first-time visitors are required to watch a 9-minute video about the bay, its history, its delicate ecosystem, and how to sustainably visit the Bay, causing as minimal damage to the area as possible.
Along the left point is the "Toilet Bowl", a natural spa tub that gently rises and falls with the tide. However, water in the Toilet Bowl can rise and fall with greater intensity during inclement weather conditions, and has caused injuries. Because of that, The Bowl has been permanently closed. [19]
Oahu is the most populated and third-largest of the Hawaiian Islands. The island of Oahu and the Northwestern Hawaiian Islands constitute the City and County of Honolulu. The state capital, Honolulu, is on Oahu's southeast coast. In 2021, Oahu had a population of 995,638, up from 953,207 in 2010.
Kāneʻohe Bay, at 45 km2 (17 sq mi), is the largest sheltered body of water in the main Hawaiian Islands. This reef-dominated embayment constitutes a significant scenic and recreational feature along the northeast coast of the Island of Oʻahu. The largest population center on Kāneʻohe Bay is the town of Kāneʻohe.
Makapuʻu is the extreme eastern end of the Island of Oʻahu in the Hawaiian Islands, comprising the remnant of a ridge that rises 647 feet (197 m) above the sea. The cliff at Makapuʻu Point forms the eastern tip and is the site of a prominent lighthouse. The place name of this area, meaning "bulging eye" in Hawaiian, is thought to derive from the name of an image said to have been located in a cave here called Keanaokeakuapōloli. The entire area is quite scenic and a panoramic view is presented at the lookout on Kalanianaole Highway where the roadway surmounts the cliff just before turning south towards leeward Oʻahu and Honolulu.
Diamond Head is a volcanic tuff cone on the Hawaiian island of Oʻahu. It is known to Hawaiians as Lēʻahi, which is most likely derived from lae plus ʻahi (tuna) because the shape of the ridgeline resembles the shape of a tuna's dorsal fin. Its English name was given by British sailors in the 19th century, who named it for the calcite crystals on the adjacent beach.
Hawaiʻi Kai, also known as Maunalua or Koko Marina, is a largely residential area located in the City & County of Honolulu, in the East Honolulu CDP, on the island of Oʻahu. Hawaiʻi Kai is the largest of several communities at the eastern end of the island. The area was largely developed by Henry J. Kaiser around the ancient Maunalua fishpond and wetlands area known as Kuapā. Hawaiʻi Kai or Koko Marina was dredged from Kuapā Pond starting around 1959. Dredging not only transformed the shallow coastal inlet and wetlands into a marine embayment, but was accompanied by considerable filling and clearing of the pond margins. In 1961, Kaiser-Aetna entered into a lease agreement with the land owner, the Bernice Pauahi Bishop Estate, to develop the 521 acre (2.11 km2) fishpond into residential tracts with a marina and channels separated by fingers of land and islands upon which house lots and commercial properties would be laid out and developed. Nearly all of the low-lying lands surrounding the marina have since been developed, and neighborhoods now extend back into the several valleys and up the separating ridges.
Located about 2,300 miles (3,680 km) from the nearest continental shore, the Hawaiian Islands are the most isolated group of islands on the planet. The plant and animal life of the Hawaiian archipelago is the result of early, very infrequent colonizations of arriving species and the slow evolution of those species—in isolation from the rest of the world's flora and fauna—over a period of at least 5 million years. As a consequence, Hawai'i is home to a large number of endemic species. The radiation of species described by Charles Darwin in the Galapagos Islands which was critical to the formulation of his theory of evolution is far exceeded in the more isolated Hawaiian Islands.
The following is an alphabetical list of articles related to the U.S. state of Hawaii:
Jeremy Harris is an American politician who served as The 11th Mayor of Honolulu, Hawaii from 1994 to 2005. A biologist by training, Harris started his political career as a delegate to the 1978 Hawaiʻi State Constitutional Convention. While Harris served as chief executive of the City & County of Honolulu, the city was named "America's Greatest City" by the official American governance journal, Governing Magazine. Harris is the founder of the China-U.S. Conference of Mayors and Business Leaders and the Japan-American Conference of Mayors and Chamber of Commerce Presidents. He lives in Kalihi Valley on the island of O'ahu.
Koʻolau Range is a name given to the dormant fragmented remnant of the eastern or windward shield volcano of the Hawaiian island of Oʻahu. It was designated a National Natural Landmark in 1972.
Nuʻuanu Pali is a section of the windward cliff of the Koʻolau mountain located at the head of Nuʻuanu Valley on the island of Oʻahu. It has a panoramic view of the windward (northeast) coast of Oʻahu. The Pali Highway connecting Kailua/Kāneʻohe with downtown Honolulu runs through the Nuʻuanu Pali Tunnels bored into the cliffside.
Koko Head is the headland that defines the eastern side of Maunalua Bay along the southeastern side of the Island of Oahu in Hawaii. On its western slope is the community of Portlock, a part of Hawaiʻi Kai. Koko Head is an ancient tuff cone that is somewhat dwarfed by its neighboring tuff cone, Koko Crater, with its peak, Kohelepelepe, rising to 1208 ft or 368 m. Koko Head itself has three significant depressions or old vents, the largest of which forms the well-known Hanauma Bay. Koko Head's last eruption was 3,000-5,000 years ago and it is part of the Honolulu Volcanics.
Hālona Blowhole is a rock formation and a blowhole on the island of Oahu, Hawaii off of Hanauma Bay at Hālona Point overlooking the Pacific Ocean. In Hawaiian hālona means "lookout".
The 2006 Kīholo Bay earthquake occurred on October 15 at 07:07:49 local time with a magnitude of 6.7 and a maximum Mercalli intensity of VIII (Severe). The shock was centered 21 kilometers (13 mi) southwest of Puakō and 21 km (13 mi) north of Kailua-Kona, Hawaiʻi, just offshore of the Kona Airport, at a depth of 38.2 km (23.7 mi). It produced several aftershocks, including one that measured a magnitude of 6.1 seven minutes after the main shock. The Pacific Tsunami Warning Center measured a nondestructive tsunami of 4 in (100 mm) on the coast of the Big Island.
Sandy Beach, also referred to as "Sandy's" and known to Hawaiians as Wāwāmalu, is a beach on the southeastern shore of Oʻahu in Hawaii. It is known for its excellent bodyboarding and bodysurfing opportunities due to its peaky shore break and consistent barrels. Consequently, Sandy Beach has one of the highest incidences of water related spinal cord injuries in Hawaii, earning it the infamous nickname, "break-neck" beach. The water is especially dangerous during high surf, when powerful waves break over shallow sand and slabs of underwater lava rock. In certain conditions, strong rip currents are also present. The beach park is located between Hanauma Bay Nature Preserve to the west and Makapuʻu Point to the east along Kalanianaʻole Highway.
Koko Crater is an extinct tuff cone located on the Hawaiian island of Oʻahu near Hawaiʻi Kai. It is northeast of Hanauma Bay and south of the Koʻolau Range.
Maunalua Bay is a bay in the southeast of Honolulu, the capital of Hawaiʻi. The bay extends about 6.3 miles from the southern tip of Diamond Head, the Black Point, also called Kūpikipikiʻō, in the west to Portlock Point, also known as Kawaihoa Point, to the east.
Molokini is a crescent-shaped, partially submerged volcanic crater which forms a small, uninhabited islet located in ʻAlalākeiki Channel between the islands of Maui and Kahoʻolawe, within Maui County in Hawaiʻi. It is the remains of one of the seven Pleistocene epoch volcanoes that formed the prehistoric Maui Nui island, during the Quaternary Period of the Cenozoic Era.
Kaʻena Ridge, also referred to as the Kaʻena Volcano, is a submerged remnant of an ancient shield volcano that is to the north of and once comprised the northern section of the Hawaiian Island of Oʻahu.
The Honolulu Volcanics are a group of volcanoes which form a volcanic field on the island of Oʻahu, Hawaiʻi, more specifically in that island's southeastern sector and in the city of Honolulu from Pearl Harbor to the Mokapu Peninsula. It is part of the rejuvenated stage of Hawaiian volcanic activity, which occurred after the main stage of volcanic activity that on Oʻahu built the Koʻolau volcano. These volcanoes formed through dominantly explosive eruptions and gave rise to cinder cones, lava flows, tuff cones and volcanic islands. Among these are well known landmarks such as Diamond Head and Punchbowl Crater.
Kahauloa Crater is a tuff cone located in Hawaii. It sits between Koko Crater and Hanauma Bay. The Koko Head Shooting Complex operates in its crater.
This article incorporates public domain material from Hanauma Bay, Oahu, Hawaii. National Aeronautics and Space Administration.
Many locals grew up playing in the now-closed Toilet Bowl at Oahu's Hanauma Bay, where the high numbers of visitors have led to a proportionately high injury rate.