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Tolimán vulcano

Stratovolcano 3158 m / 10,361 ft
Guatemala, 14.61°N / -91.19°W
Stato attuale: normal or dormant (1 di 5)

Show interactive Map
Stile eruttivo tipico: non specificato
Eruzioni del vulcano Tolimán: unknown, no recent eruptions

Latest nearby earthquakes

Data / oraMag. / ProfonditàDistanzaUbicazione
Sat, 27 Feb 2021 (GMT) (3 Terremoti)
27 feb 2021 14:12 (GMT -6) (27 Feb 2021 20:12:19 GMT)
4.0

86 km - Più
130 kmSanta Lucrecia del Valle, 18 km a sud ovest da Tapachula, Chiapas, Messico
27 feb 2021 04:43 (GMT -6) (27 Feb 2021 10:43:50 GMT)
4.6

25 km - Più
139 kmNorth Pacific Ocean, 90 km a sud ovest da Retalhuleu, Guatemala
27 feb 2021 04:27 (GMT -6) (27 Feb 2021 10:27:39 GMT)
5.0

18 km - Più
135 kmNorth Pacific Ocean, 87 km a sud ovest da Retalhuleu, Guatemala
Fri, 26 Feb 2021 (GMT) (1 terremoto)
26 feb 2021 15:46 (GMT -6) (26 Feb 2021 21:46:23 GMT)
3.8

34 km - Più
90 kmNorth Pacific Ocean, 29 km a sud da La Gomera, Escuintla, Guatemala
Tue, 23 Feb 2021 (GMT) (1 terremoto)
23 feb 2021 07:38 (GMT -6) (23 Feb 2021 13:38:41 GMT)
3.7

1 km - Più
68 kmMunicipio de Amatitlan, 27 km a sud da Città del Guatemala, Municipio de Guatemala

Sfondo

Volcán Tolimán is a large andesitic stratovolcano that rises above the south shore of Lake Atitlán. Tolimán was constructed within the Pleistocene Atitlán III caldera, near its inferred southern margin. A shallow elliptical crater truncates the summit, and a minor subsidiary peak to the SSW also has a shallow crater. In contrast to the tephra-covered surface of its twin volcano to the south, Volcán Atitlán, the surface of Tolimán is draped by prominent thick lava flows. Many of the flows were erupted from vents on the volcano's flanks and form a highly irregular shoreline on the south side of Lake Atitlán. No historical eruptions are known from Tolimán. However, a lava flow that entered Lake Atitlán from the parasitic lava dome of Cerro de Oro on the northern flank was considered by Newhall et al. (1987) to be less than a few thousand years old based on the thickness of sediment accumulated on the sublacustral part of the flow.
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Smithsonian / GVP volcano information


See also: Sentinel hub | Landsat 8

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