Fringing reef in the context of "Bonaire"

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⭐ Core Definition: Fringing reef

A fringing reef is one of the three main types of coral reef. It is distinguished from the other main types, barrier reefs and atolls, in that it has either an entirely shallow backreef zone (lagoon) or none at all. If a fringing reef grows directly from the shoreline, then the reef flat extends to the beach and there is no backreef. In other cases (e.g., most of the Bahamas), fringing reefs may grow hundreds of yards from shore and contain extensive backreef areas within which it contains food and water. Some examples of this are Philippines, Indonesia, Timor-Leste, the western coast of Australia, the Caribbean, East Africa, and Red Sea. Charles Darwin believed that fringing reefs are the first kind of reefs to form around a landmass in a long-term reef growth process. The largest fringing coral reef in the world is the Ningaloo Reef, stretching to around 260 km (160 mi) along the coastline of Western Australia.

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👉 Fringing reef in the context of Bonaire

Bonaire is a Caribbean island in the Leeward Antilles, and is a special municipality (officially "public body") of the Netherlands. Its capital is the port of Kralendijk, on the west (leeward) coast of the island. Aruba, Bonaire and Curaçao form the ABC islands, 80 km (50 miles) off the coast of Venezuela. The islands have an arid climate that attracts visitors seeking warm, sunny weather all year round, and they lie outside the Main Development Region for tropical cyclones. Bonaire is a popular snorkeling and scuba diving destination because of its multiple shore diving sites, shipwrecks and easy access to the island's fringing reefs.

As of 1 January 2025, the island's population total 26,552 permanent residents, an increase of 10,011 since 2012. The island's total land area is 288 square kilometres (111 sq mi); it is 38.6 kilometres (24.0 mi) long from north to south, and ranges from 5–8 km (3–5 mi) wide from east to west. A short 800 metres (0.50 mi) west of Bonaire across the sea is the uninhabited islet of Klein Bonaire with a total land area of 6 km (2.3 sq mi). Klein Bonaire has low-growing vegetation including cactus, with sparse palm trees near the water and is bordered by white sandy beaches and a fringing reef. The reefs, beaches and on-island reserves located on both Bonaire and Klein Bonaire are under the protection of the Bonaire National Marine Park, and managed by STINAPA Bonaire.

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Fringing reef in the context of Gambier Islands

The Gambier Islands (French: Îles Gambier or Archipel des Gambier) are an archipelago in French Polynesia, located at the southeast terminus of the Tuamotu archipelago. They cover an area of 27.8 km or 10.7 sq mi, and are made up of the Mangareva Islands, a group of high islands remnants of a caldera along with islets on the surrounding fringing reef, and the uninhabited Temoe atoll, which is located 45 km (28 mi) south-east of the Mangareva Islands. The Gambiers are generally considered a separate island group from Tuamotu both because their culture and language (Mangarevan) are much more closely related to those of the Marquesas Islands, and because, while the Tuamotus comprise several chains of coral atolls, the Mangareva Islands are of volcanic origin with central high islands.

Administratively, the Gambier Islands are inside the commune of Gambier, which also includes several atolls in the Tuamotu Archipelago. The town hall (mairie) of the commune of Gambier is located on Mangareva, which is the largest island in the Gambier Islands group.

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Fringing reef in the context of Baker Island

Baker Island, once known as New Nantucket in the early 19th century, is a small, uninhabited atoll located just north of the Equator in the central Pacific Ocean, approximately 1,920 miles (3,090 kilometres) southwest of Honolulu. Positioned almost halfway between Hawaii and Australia, its closest neighbor is Howland Island, situated 42 mi (68 km) to the north-northwest. Both Baker and Howland Islands have been claimed as territories of the United States since 1857, though the United Kingdom regarded them as part of the British Empire between 1897 and 1936 but did not actually annex them. They were not being used when a U.S. colonization attempt was started in 1935, and the next year formal reassertion of U.S. sovereignty was issued. During World War II the Japanese Empire attacked the island, and it was evacuated and a small military base was established. The island was an important navigation beacon in the remote Pacific waters during and after World War II. In the 1970s it was made into a nature preserve and has remained so into the 21st century.

Covering an area of 0.81 sq mi (2.1 km), with 3.0 mi (4.8 km) of coastline, Baker Island experiences an equatorial climate, characterized by average temperatures around 80 °F (27 °C), minimal rainfall, persistent winds, and strong sunlight. The terrain is flat and sandy, surrounded by a narrow fringing reef. Unlike many atolls, Baker Island lacks a central lagoon, with its highest point being 26 ft (7.9 m) above sea level.

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