Revision as of 03:58, 20 January 2013 edit Tillman (talk \| contribs) Autopatrolled, Extended confirmed users, Pending changes reviewers, Rollbackers 29,463 edits add photo, effects on climate, cite ← Previous edit		Revision as of 14:10, 12 March 2013 edit undo 173.66.136.60 (talk) No edit summary Next edit →
Line 29: The volcano last erupted in 1859, but its most famous activity occurred on 20 January 1835,<ref>Penland, Paige R., Gary Chandler, Liza Prado (2006), [http://books.google.com/books?id=Ver9vPkt5n4C&pg=PA189&dq=Cosig%C3%BCina&hl=cs&ei=tCauTNH2FoWSswb9mqndDQ&sa=X&oi=book_result&ct=result&resnum=1&ved=0CCcQ6AEwAA#v=onepage&q=Cosig%C3%BCina&f=false ''Lonely Planet Nicaragua & El Salvador''], Lonely Planet, Illustrated ed. p. 189, ISBN 1-74104-758-7</ref> when it produced the largest historical eruption in Nicaragua. Ash from the 1835 eruption has been found in Mexico, Costa Rica, and Jamaica. According to an analysis by [[Berkeley Earth Surface Temperature]], the 1835 eruption caused a temporary decrease in the average land temperature of Earth of about 0.75 degrees C. <ref>[http://berkeleyearth.org/pdf/berkeley-earth-press-release-july-29.pdf Berkeley Earth Releases New Analysis], 29 July 2012 </ref> ~~The volcano~~It has ~~been~~not ~~quiet~~erupted since 1859, only an instant in terms of geological time. An earthquake swarm was measured near Cosigüina in 2002, indicating that tectonic forces are still active in the region although the volcano is somewhat isolated from the line of more recently active Central American volcanoes to the northwest and southeast. The only indicators of hydrothermal activity at the volcano are intermittently observed gas bubbles in Laguna Cosigüina and a hot spring along the eastern flank of the volcano. The fairly uniform vegetation cover on the volcano’s sides also attests to a general lack of gas emissions or “hot spots” on the 872-meter-high cone. ==See also==

Cosigüina: Difference between revisions