Volcán Tolimán
Encyclopedia
Tolimán is a stratovolcano
in Guatemala
, on the southern shores of Lago de Atitlán
. The volcano has an elevation of 3,158 m
(10,361 ft
) and was formed near the southern margin of the Pleistocene
Atitlán III caldera. The top of the volcano has a shallow crater and its flanks are covered with the thick remains of ancient lavas flows that emerged from vents in the volcano's flanks. A parasitic lava dome
, known as Cerro de Oro, was formed on the volcano's northern flank, which may have erupted a few thousand years ago.
Stratovolcano
A stratovolcano, also known as a composite volcano, is a tall, conical volcano built up by many layers of hardened lava, tephra, pumice, and volcanic ash. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile and periodic, explosive eruptions...
in Guatemala
Guatemala
Guatemala is a country in Central America bordered by Mexico to the north and west, the Pacific Ocean to the southwest, Belize to the northeast, the Caribbean to the east, and Honduras and El Salvador to the southeast...
, on the southern shores of Lago de Atitlán
Lago de Atitlán
Lake Atitlán is a large endorheic lake in the Guatemalan Highlands. Atitlan is recognized to be the deepest lake in Central America with maximum depth about 340 meters. The lake is shaped by deep escarpments which surround it and by three volcanos on its southern flank...
. The volcano has an elevation of 3,158 m
M
M is the thirteenth letter of the basic modern Latin alphabet.-History:The letter M is derived from the Phoenician Mem, via the Greek Mu . Semitic Mem probably originally pictured water...
(10,361 ft
Ft
Ft or ft. may mean:* Foot , a unit of distance or length* Hungarian forint, the currency of Hungary* Fair Trade, the principle to give a fair price when trading* Fort, a fortified place, especially in place names...
) and was formed near the southern margin of the Pleistocene
Pleistocene
The Pleistocene is the epoch from 2,588,000 to 11,700 years BP that spans the world's recent period of repeated glaciations. The name pleistocene is derived from the Greek and ....
Atitlán III caldera. The top of the volcano has a shallow crater and its flanks are covered with the thick remains of ancient lavas flows that emerged from vents in the volcano's flanks. A parasitic lava dome
Lava dome
|250px|thumb|right|Image of the [[rhyolitic]] lava dome of [[Chaitén Volcano]] during its 2008–2009 eruption.In volcanology, a lava dome is a roughly circular mound-shaped protrusion resulting from the slow extrusion of viscous lava from a volcano...
, known as Cerro de Oro, was formed on the volcano's northern flank, which may have erupted a few thousand years ago.