Cotopaxi is a stratovolcano in the Andes Mountains, located about 28 km (17 mi) south of Quito, Ecuador, South America. It is the second highest summit in the country, reaching a height of 5,897 m (19,347 ft) and is one of the highest active volcanoes in the world. (Claims that Cotopaxi is the highest active volcano in the world are incorrect.
Since 1738, Cotopaxi has erupted more than 50 times, resulting in the creation of numerous valleys formed by lahars (mudflows) around the volcano.Cotopaxi is clearly visible on the skyline from Quito[3] and is part of the chain of volcanoes around the Pacific plate known as the Pacific Ring of Fire. It has an almost symmetrical cone that rises from a highland plain of about 3,800 metres (12,500 ft), with a width at its base of about 23 kilometres (14 mi). It has one of the few equatorial glaciers in the world, which starts at the height of 5,000 metres (16,400 ft). At its summit, Cotopaxi has a 800 X 550 m wide crater which is 250 m deep. The crater consists of two concentric crater rims, the outer one being partly free of snow and irregular in shape. The crater interior is covered with ice cornices and rather flat. The highest point is on the outer rim of the crater on the north side.Cotopaxi's most violent eruptions in historical times occurred in the years 1742, 1744, 1768, and 1877. The 1744 and 1768 events destroyed the colonial town of Latacunga. In the 26 June 1877 eruption, pyroclastic flows descended all sides of the mountain melting the entire ice cap, with lahars traveling more than 100 km into the Pacific Ocean and western Amazon basin draining the valley. The city of Latacunga was again leveled completely due to the lahar deposits.
There was a major eruption from 1903 through 1904, and minor activity persisted until at least 1940 and possibly 1942. (Note that direct observations of minor eruptions can be difficult because of bad weather, hence the uncertainty about the 1942 "eruption.") The same source also reported increased thermal/seismic, non-eruptive activity in 1975 and 2002. In the most recent case of increased activity, fumarolic activity and sulfuric emissions increased and ice around the inside and on the southeastern side of the cone started to melt. However, no actual eruption was observed.
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