Typical eruption style
: unspecifiedCham volcano eruptions
: None during the past 10,000 years
Less than few million years ago (Pleistocene)
No recent earthquakes
|Time||Mag. / Depth||Distance||Location|
There's currently no information available in the GVP database.
---Source: Smithsonian / GVP volcano information
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...
"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)
Descending into the magma chamber of Thrihnukagigur volcano, Iceland (Photo: Janka)
Volcanic massif of Chambe, Mulanje mountain, Malawi (Photo: WNomad)
See also: Sentinel hub
| Landsat 8