Search results
Results from the WOW.Com Content Network
Cotopaxi is among the highest active volcanoes in the world. Cotopaxi is known to have erupted 87 times, resulting in the creation of numerous valleys formed by lahars (mudflows) around the volcano. [2] An ongoing eruption began on 21 October 2022. [3]
The Cotopaxi volcano (meaning 'smooth neck of the moon' in Quechua; Quechua q'oto 'throat' + Aymara phakhsi 'moon') that lends its name to the park is located within its boundaries, together with two others: the dormant Rumiñawi volcano to its north-west and the historical Sincholagua volcano (last major eruption: 1877) to the south-east.
Volcanic block at Cotopaxi volcano, Ecuador. A volcanic block is a fragment of rock that measures more than 64 mm (2.5 in) in diameter and is erupted in a solid condition. Blocks are formed from material from previous eruptions or from country rock and are therefore mostly accessory or
Cotopaxi is an 1862 oil painting by American artist Frederic Edwin Church, a member of the Hudson River School. The painting depicts Cotopaxi , an active volcano that is also the second highest peak in modern-day Ecuador , spewing smoke and ash across a colorful sunrise. [ 1 ]
Map of a north-south sea-parallel pattern of rock ages in western Colombia. This pattern is a result of the Andean orogeny. Tectonic blocks of continental crust that had separated from northwestern South America in the Jurassic re-joined the continent in the Late Cretaceous by colliding obliquely with it. [6]
This Ecuador location article is a stub. You can help Wikipedia by expanding it.
Cotopaxi (Spanish pronunciation: [kotoˈpaksi]) is one of the provinces of Ecuador. The capital is Latacunga . The province contains the Cotopaxi volcano, an intermittent volcano with a height of 19,347 feet (5,897 m).
In 2015, researchers found that the volcano's structure bore patterns of magnetic striping on either side, indicating that the volcano is likely a hybrid of a mid-ocean ridge and a shield volcano. Geologic data also indicated that Tamu Massif formed at the junction of three mid-ocean ridges, which was a highly unusual occurrence.