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Cham vulcano

Unknown unknown
Cambodia, 12.1°N / 105.6°E
Stato attuale: estinto (probabilmente) (0 di 5)

Stile eruttivo tipico: non specificato
Eruzioni del vulcano Cham: None during the past 10,000 years
Less than few million years ago (Pleistocene)

Ultimi terremoti nelle vicinanze

Non terremoti recenti
Data / oraMag. / ProfonditàDistanzaUbicazione

Sfondo

There's currently no information available in the GVP database.
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Source: Smithsonian / GVP volcano information

Cham Photos

Champagne Pool  (Photo: Tom Pfeiffer)
Champagne Pool (Photo: Tom Pfeiffer)
The fountains on the lava lake are caused by degassing, the release of hot gasses that rise from the magma chambers. The gasses are the main engine of the lake, providing just the right amount of heat energy to keep the lake stable and liquid. (Photo: Tom Pfeiffer)
The fountains on the lava lake are caused by degassing, the release of hot gasses that rise from the magma chambers. The gasses are the main engine of the lake, providing...
"Lava fountains" are near-continuous gas bubbles escaping from the lava lake: they are the motor of the lake, transporting heat energy from the magma chamber to the surface and keeping the lake - underneath a thin, slvery crust - liquid and boiling where the gasses escape. (Photo: Tom Pfeiffer)
"Lava fountains" are near-continuous gas bubbles escaping from the lava lake: they are the motor of the lake, transporting heat energy from the magma chamber to the surfa...
Inside the magma chamber (by elevator!), Iceland. (Photo: mlyvers)
Inside the magma chamber (by elevator!), Iceland. (Photo: mlyvers)
 


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See also: Sentinel hub | Landsat 8
 

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