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Clipperton Island

Atoll in the eastern Pacific Ocean

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Clipperton was documented by French merchant-explorers in 1711 and formally claimed as part of the French protectorate of Tahiti in 1858. Despite this, American guano miners began working the island in the early 1890s. As interest in the island grew, Mexico asserted a claim to the island based upon Spanish records from the 1520s that may have identified the island. Mexico established a small military colony on the island in 1905. During the Mexican Revolution, contact with the mainland became infrequent, most of the colonists died, and lighthouse keeper Victoriano Álvarez instituted a short, brutal reign as "king" of the island. Eleven survivors were rescued in 1917 and Clipperton was abandoned.

The dispute between Mexico and France over Clipperton was taken to binding international arbitration in 1909. Victor Emmanuel III, King of Italy, was chosen as arbitrator and decided in 1931 that the island was French territory. Despite the ruling, Clipperton remained largely uninhabited until 1944 when the U.S. Navy established a weather station on the island to support its war efforts in the Pacific. France protested and, as concerns about Japanese activity in the eastern Pacific waned, the U.S. abandoned the site in late 1945.

Since the end of World War II, Clipperton has primarily been the site for scientific expeditions to study the island's wildlife and marine life, including its significant masked and brown booby colonies. It has also hosted climate scientists and amateur radio DX-peditions. Plans to develop the island for trade and tourism have been considered, but none have been enacted and the island remains mostly uninhabited, with periodic visits from the French Navy.

Geography

The coral island is located at 10°18′N 109°13′W / 10.300°N 109.217°W in the East Pacific, 1,080 km (583 nmi) southwest of Mexico, 2,424 km (1,309 nmi) west of Nicaragua, 2,545 km (1,374 nmi) west of Costa Rica, and 2,390 km (1,290 nmi) northwest of the Galápagos Islands in Ecuador. The nearest land is Socorro Island, about 945 km (510 nmi) to the northwest in the Revillagigedo Archipelago. The nearest French-owned island is Hiva Oa in the Marquesas Islands of French Polynesia, which is about 3,300 km (1,781 nmi) southwest of Clipperton.

Despite its proximity to North America, Clipperton is often considered one of the eastern-most points of Oceania because it is part of the French Indo-Pacific, and its marine fauna are similar to those of Hawaii and Kiribati's Line Islands—Clipperton lies on Eastern Tropical Pacific migration paths. The island is the only emerged part of the East Pacific Rise, as well as the only feature in the Clipperton fracture zone that breaks the ocean's surface, and it is one of the few islands in the Pacific that lacks an underwater archipelagic apron.

The atoll is low-lying and largely barren, with some scattered grasses, and a few clumps of coconut palms (Cocos nucifera). The land ring surrounding the lagoon measures 1.7 square kilometres (0.66 mi2) in area with an average elevation of 2 m (6.6 ft), although a small volcanic outcropping, referred to as Clipperton Rock (Rocher de Clipperton), rises to 29 m (95 ft) on its southeast side. The surrounding 3.7-square-kilometre (1.4 mi2) reef hosts an abundance of corals and is partly exposed at low tide. In 2001 a geodetic marker was placed to evaluate if the land is rising or sinking.

Clipperton Rock is the remains of the island's now extinct volcano's rim; because it includes this rocky outcropping, Clipperton is not a true atoll and is sometimes referred to as a 'near-atoll'. The surrounding reef in combination with the weather makes landing on the island difficult and anchoring offshore hazardous for larger ships; in the 1940s American ships reported active problems in this regard.

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