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Cotopaxi    



 

is Ecuador's highest active volcano at 5897m, located in the Eastern Cordillera. It is a stratovolcano (very similar to Mt. Fuji or Mt. Sashta) with an almost perfectly symmetrical cone, rising from a highland plain of 3800m and covered by a mighty glacier starting at a height of 5000m. The side of the cone has deep valleys scoured by lahars. The summit crater is 600m x 800m in diameter and several hundred meters deep. Its geographical location is 0.677°S and 78.43°W, some 60 km southeast of Quito and 15 km northeast of Latacunga, provincial capital of Cotopaxi province.



 

This majestic volcano forms the crown jewel of the Avenida de los Volcanes, named so rightly by Alexander von Humboldt, the German naturalist, who visited Ecuador at the beginning of the 19th century. Several active and dormant volcanoes in the Western and Eastern Cordillera dot this stretch of road leading from Quito to Riobamba.



 

 Cotopaxi has a well recorded history of explosive eruptions with lava and pyroclastic flows, which devastated often part of nearby valleys. During a battle between Incas and Spaniards in 1534, the volcano erupted and put an end to the fighting as both fled from the battle field. Eruptions in 1744 and 1768 destroyed the colonial town of Latacunga and in 1877 a huge eruption produced lahars, which reached even the Pacific oceans through the rivers, draining the valley to the west. The last recorded eruption occurred in 1904 and in 1975 the volcano awoke for a short time but did not produce any spectacular events. In the last few years fumarolic activities and sulfuric emissions increased and ice around the inside rim and on the southeastern side of the cone started to melt away.



 

Roads lead through an lava field with huge boulders, ejected from the last major eruption in 1877. That was the last big one of the volcano and many scientist think that one is due again soon as the volcano presents historically a hundred year cycle of eruptions.



 

The main danger of a huge eruption of Cotopaxi would be the ensuring flow of mud and ice from its glacier (lahars). Computer models calculated lahars of eight meters coming down by way of River Pita to the valley of Los Chillos, nowadays a main suburban area of Quito with a population of more than 100 000 people living there. In the event of a huge explosion, not much would be left from those settlement in the valley. Another major city in danger would be Latacunga to the southwest of Cotopaxi and all the small farming villages skirting the mountain. Many experts think that another eruptive stage might be coming very soon.



 

At the end of 2001 and start of 2002, fumarolic activities increased again and sulfur could be smelled strongly on top. Picture of the crater (bottom right) was taken in May of 2002, where fumaroles can be seen steaming out of the crater. At that time also snow around the crater rim melted away giving a clear view to the bottom. Beginning of 2003 a substantial increase in activity occurred which continued for the whole year. In the picture (top one) taken in November of 2003, fumaroles can be seen steaming out through the rock face of Yanasacha, which is located some two hundred meters below the summit. Another phenomenon is the accelerated loss of its glacier  due of a combination of global warming and heat from the inside of the volcano. As can be appreciated in the photo (bottom left) there is now almost an ice-free route on its southeastern side.



 

For more information of its volcanic status, click to Global Volcanism Program or to Geophysical Institute of Ecuador (Spanish).
 
  For a daytrip to Cotopaxi click here and to climb to the top..


For
more pictures of this volcano, click to our Ecuador- Images.net



 

Latest Update:

Danger alert: None
 In 2004 lesser activities observed and potential for eruptions increased.

 

 
 
 
 
 

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