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Île Saint-Paul
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Île Saint-Paul
Île Saint-Paul (French pronunciation: [il sɛ̃ pɔl], "Saint Paul Island") is an island forming part of the French Southern and Antarctic Lands (French: Terres australes et antarctiques françaises, TAAF) in the Indian Ocean, with an area of 6 km2 (2.3 sq mi; 1,500 acres). The island is located about 90 km (56 mi) south of the larger Île Amsterdam 55 km2 (21 sq mi), 1,300 kilometres (810 mi) northeast of the Kerguelen Islands, and 3,000 km (1,900 mi) southeast of Réunion.
It is an important breeding site for seabirds. A scientific research cabin on the island is used for scientific or ecological short campaigns, but there is no permanent population. It is under the authority of a senior administrator on Réunion.
Île Saint-Paul is a volcanic island with a triangular shape that measures no more than 5 km (3.1 mi) at its widest point. It is the top of an active volcano; the volcano last erupted in 1793 (from its SW flank), and is rocky with steep cliffs on the east side. The thin stretch of rock that used to close off the crater collapsed in 1780, admitting the sea through a 100 m (330 ft) channel; the entrance is only a few meters deep, thus allowing only very small ships or boats to enter the crater. The interior basin, 1 km (0.62 mi) wide and 50 m (160 ft) deep, is surrounded by steep walls up to 270 m (890 ft) high. There are active thermal springs.
The island is antipodal of Cheyenne County, Colorado, one of the few places in the continental United States with a non-oceanic antipode.
The island is located on the mainly under sea Amsterdam-Saint Paul Plateau which is of volcanic hotspot origin, with the currently active Amsterdam-Saint Paul hotspot believed to be located close to the island. The aphyric (no phenocrysts) basalts found on Saint Paul are distinct from other basalts found to date on the Amsterdam-Saint Paul Plateau, being mildly alkalic, incompatible element-enriched and highly fractionated. The island is no more than 400,000 years old and was formed by magma that was a simple binary mixture between upper mantle and the Amsterdam-Saint Paul hotspot plume.
Île Saint-Paul was first discovered in 1559 by the Portuguese. The island was mapped, described in detail and recorded in paintings by members of the crew of the nau São Paulo, among them Father Manuel Álvares and the chemist Henrique Dias. Álvares and Dias correctly calculated the latitude as 38° South. The ship was commanded by Rui Melo da Câmara and was part of the Portuguese India Armada commanded by Jorge de Sousa. The São Paulo, which also carried women and had sailed from Europe and stopped in Brazil, would be the subject of a dramatic and moving story of survival after it sank south of Sumatra.
The next confirmed sighting was made by Dutchman Harwick Claesz de Hillegom on 19 April 1618. There were further sightings of the island through the 17th century. One of the first detailed descriptions of it, and possibly the first landing, was made in December 1696 by Willem de Vlamingh.
In sailing-ship days captains would occasionally use the island as a check on their navigation before heading north. Saint-Paul was occasionally visited by explorers, fishermen, and sealers in the 18th and 19th centuries, among which was the American sealer General Gates, which called at the island in April 1819. George William Robinson, an American sealer, was left on the island to hunt seals, and stayed there for 23 months until the General Gates returned for him in March 1821. Robinson subsequently returned to Saint-Paul in 1826 to gather sealskin, sailing from Hobart aboard his own vessel, the schooner Hunter.
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Île Saint-Paul AI simulator
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Île Saint-Paul
Île Saint-Paul (French pronunciation: [il sɛ̃ pɔl], "Saint Paul Island") is an island forming part of the French Southern and Antarctic Lands (French: Terres australes et antarctiques françaises, TAAF) in the Indian Ocean, with an area of 6 km2 (2.3 sq mi; 1,500 acres). The island is located about 90 km (56 mi) south of the larger Île Amsterdam 55 km2 (21 sq mi), 1,300 kilometres (810 mi) northeast of the Kerguelen Islands, and 3,000 km (1,900 mi) southeast of Réunion.
It is an important breeding site for seabirds. A scientific research cabin on the island is used for scientific or ecological short campaigns, but there is no permanent population. It is under the authority of a senior administrator on Réunion.
Île Saint-Paul is a volcanic island with a triangular shape that measures no more than 5 km (3.1 mi) at its widest point. It is the top of an active volcano; the volcano last erupted in 1793 (from its SW flank), and is rocky with steep cliffs on the east side. The thin stretch of rock that used to close off the crater collapsed in 1780, admitting the sea through a 100 m (330 ft) channel; the entrance is only a few meters deep, thus allowing only very small ships or boats to enter the crater. The interior basin, 1 km (0.62 mi) wide and 50 m (160 ft) deep, is surrounded by steep walls up to 270 m (890 ft) high. There are active thermal springs.
The island is antipodal of Cheyenne County, Colorado, one of the few places in the continental United States with a non-oceanic antipode.
The island is located on the mainly under sea Amsterdam-Saint Paul Plateau which is of volcanic hotspot origin, with the currently active Amsterdam-Saint Paul hotspot believed to be located close to the island. The aphyric (no phenocrysts) basalts found on Saint Paul are distinct from other basalts found to date on the Amsterdam-Saint Paul Plateau, being mildly alkalic, incompatible element-enriched and highly fractionated. The island is no more than 400,000 years old and was formed by magma that was a simple binary mixture between upper mantle and the Amsterdam-Saint Paul hotspot plume.
Île Saint-Paul was first discovered in 1559 by the Portuguese. The island was mapped, described in detail and recorded in paintings by members of the crew of the nau São Paulo, among them Father Manuel Álvares and the chemist Henrique Dias. Álvares and Dias correctly calculated the latitude as 38° South. The ship was commanded by Rui Melo da Câmara and was part of the Portuguese India Armada commanded by Jorge de Sousa. The São Paulo, which also carried women and had sailed from Europe and stopped in Brazil, would be the subject of a dramatic and moving story of survival after it sank south of Sumatra.
The next confirmed sighting was made by Dutchman Harwick Claesz de Hillegom on 19 April 1618. There were further sightings of the island through the 17th century. One of the first detailed descriptions of it, and possibly the first landing, was made in December 1696 by Willem de Vlamingh.
In sailing-ship days captains would occasionally use the island as a check on their navigation before heading north. Saint-Paul was occasionally visited by explorers, fishermen, and sealers in the 18th and 19th centuries, among which was the American sealer General Gates, which called at the island in April 1819. George William Robinson, an American sealer, was left on the island to hunt seals, and stayed there for 23 months until the General Gates returned for him in March 1821. Robinson subsequently returned to Saint-Paul in 1826 to gather sealskin, sailing from Hobart aboard his own vessel, the schooner Hunter.