Miravalles
 | Ten artykuł od 2022-07 wymaga zweryfikowania podanych informacji. |
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| Państwo | |
|---|---|
| Pasmo | |
| Wysokość | 2028 m n.p.m. |
Położenie na mapie Kostaryki  (c) Eric Gaba (user Sting) for Wikimedia Commons using GEBCO_2021 Grid data, CC BY-SA 4.0 | |
 10°44′54″N 85°09′10″W/10,748333 -85,152778 | |
Miravalles – wulkan w Kostaryce położony w paśmie górskim Cordillera de Guanacaste. Osiąga wysokość 2028 m n.p.m. Jedyna historyczna erupcja miała miejsce w 1946.
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Costa Rica relief location map.jpg
(c) Eric Gaba (user Sting) for Wikimedia Commons using GEBCO_2021 Grid data, CC BY-SA 4.0
Blank relief map of Costa Rica for geo-location purpose.
Note : The Isla del Coco, out of the map, is not shown.
Scale : 1:1,856,000 (accuracy : 464 m)
(c) Eric Gaba (user Sting) for Wikimedia Commons using GEBCO_2021 Grid data, CC BY-SA 4.0
Blank relief map of Costa Rica for geo-location purpose.
Note : The Isla del Coco, out of the map, is not shown.
Scale : 1:1,856,000 (accuracy : 464 m)
U+25B2.svg
Black up-pointing triangle ▲, U+25B2 from Unicode-Block Geometric Shapes (25A0–25FF)
Black up-pointing triangle ▲, U+25B2 from Unicode-Block Geometric Shapes (25A0–25FF)
Miravalles volcano.jpg
Miravalles volcano rises above a thermal area on its SW flank. The 2028-m-high andesitic stratovolcano is one of five post-caldera cones constructed along a NE-trending line within the Pleistocene 15 x 20 km Miravalles caldera. Morphologically youthful lava flows cover the western and SW flanks of the volcano. The only reported historical eruptive activity was a small steam explosion in 1946, although high heat flow remains, and a producing geothermal field is located within the caldera.
Miravalles volcano rises above a thermal area on its SW flank. The 2028-m-high andesitic stratovolcano is one of five post-caldera cones constructed along a NE-trending line within the Pleistocene 15 x 20 km Miravalles caldera. Morphologically youthful lava flows cover the western and SW flanks of the volcano. The only reported historical eruptive activity was a small steam explosion in 1946, although high heat flow remains, and a producing geothermal field is located within the caldera.