Quilotoa: Difference between revisions

From Citizendium
Jump to navigation Jump to search
imported>Joe Quick
mNo edit summary
imported>Joe Quick
No edit summary
Line 1: Line 1:
{{subpages}}
{{subpages}}
{{Image|Laguna Quilotoa.jpg|right|350px|Laguna Quilotoa (Lake Quilotoa).}}
'''Quilotoa''' is a [[dacite|dacitic]] [[volcano]] located in the [[Cordillera Occidental (Ecuador)|Western Cordillera]] of the [[Ecuador]]ian [[Andes]]. It erupted most recently in about 1280 AD, causing large [[pyroclastic flow]]s, [[lahar]]s that reached as far as the [[Pacific Ocean|Pacific]] coast, and ash-fall deposits that covered much of present-day northern Ecuador. The eruption caused a significant disruption in the agricultural livelihoods of the pre-Columbian peoples of the region. Today, the volcano is best known for the deep [[crater lake]] within its caldera, drawing large numbers of domestic and international [[tourism|tourists]].
'''Quilotoa''' is a [[dacite|dacitic]] [[volcano]] located in the [[Cordillera Occidental (Ecuador)|Western Cordillera]] of the [[Ecuador]]ian [[Andes]]. It erupted most recently in about 1280 AD, causing large [[pyroclastic flow]]s, [[lahar]]s that reached as far as the [[Pacific Ocean|Pacific]] coast, and ash-fall deposits that covered much of present-day northern Ecuador. The eruption caused a significant disruption in the agricultural livelihoods of the pre-Columbian peoples of the region. Today, the volcano is best known for the deep [[crater lake]] within its caldera, drawing large numbers of domestic and international [[tourism|tourists]].

Revision as of 16:56, 12 September 2020

This article is a stub and thus not approved.
Main Article
Discussion
Definition [?]
Related Articles  [?]
Bibliography  [?]
External Links  [?]
Citable Version  [?]
 
This editable Main Article is under development and subject to a disclaimer.
(CC) Photo: Joe Quick
Laguna Quilotoa (Lake Quilotoa).

Quilotoa is a dacitic volcano located in the Western Cordillera of the Ecuadorian Andes. It erupted most recently in about 1280 AD, causing large pyroclastic flows, lahars that reached as far as the Pacific coast, and ash-fall deposits that covered much of present-day northern Ecuador. The eruption caused a significant disruption in the agricultural livelihoods of the pre-Columbian peoples of the region. Today, the volcano is best known for the deep crater lake within its caldera, drawing large numbers of domestic and international tourists.