Ash, cinders and bombs only come from explosive eruptions because quiet eruptions really only spew thin lava, not thick and sticky lava like explosive ones. The thick lava can get caught inside the pipe leading to the vent, which can cause more and more pressure to build up. When the volcano's side gives in, or when the lava finally gets to the vent, it ends up exploding, making ash, cinders and bombs.
because the geysers crash through the valleys and create layers of thin cinder cones that land through assofoniam clinbitchers
just because & to make you ask questions
Ash and cinders are formed from lava that is blown apart explosively. If lava is not ejected explosively it will either flow away from the vent, fill a lava lake, or pile up into a lava dome.
Paricutin produced mildly explosive eruptions, as is typical of cinder cone volcanoes.
Kilauea is a shield volcano fed by gas-poor basaltic magma. It is the gas in the magma that makes eruptions explosive. Kilauea has occasionally produced explosive eruptions when magma cam in contact with water.
Explosive and non-explosive eruptions form different types of rock. Explosive eruptions tend to have fragmented rocks composed of cinders, ash, and pumice. Non-explosive eruptions usually produce lava flows, which tend to cool as solid sheets or channels of rock.
Sheild volcanoes generally erupt "quietly."
It is an explosive volcano. Mount Rainier is a stratovolcano, characterized by layers of ash from explosive eruptions and cooled lava flows from effusive eruptions. The high viscosity and gas content of its magma are the reason for its explosive nature.
It requires an explosive force to hurl and fragment the molten rock like that. Non explosive eruptions extrude rock more "gently".
Yes. The Yellowstone volcano has produced several VEI-8 eruptions, the most explosive level of eruption possible.
Cinder cones are small and steep-sloped, composed of volcanic cinders, and have mildly explosive eruptions. Shield volcanoes are large and shallow-sloped with very runny lava and generally non-explosive eruptions.
Paricutin produced mildly explosive eruptions, as is typical of cinder cone volcanoes.
Kilauea is a shield volcano fed by gas-poor basaltic magma. It is the gas in the magma that makes eruptions explosive. Kilauea has occasionally produced explosive eruptions when magma cam in contact with water.
Explosive and non-explosive eruptions form different types of rock. Explosive eruptions tend to have fragmented rocks composed of cinders, ash, and pumice. Non-explosive eruptions usually produce lava flows, which tend to cool as solid sheets or channels of rock.
Sheild volcanoes generally erupt "quietly."
A: it can have explosive eruptions
During a quiet eruption lava flows from vents, setting fire to, and then burying, everything in its path. During an explosive eruption, a volcano can belch out hot clouds of deadly gases as well as ash, cinders, and bombs
Explosive eruptions will produce pyroclastic rocks such as scoria, pumice, and tuff.
Generally not. Explosive eruptions may happen occasionally, but most eruptions are effusive.
No. A supervolcano is a volcano that is capable of producing extremely large explosive eruptions. Kilauea is a shield volcano. Most of its eruptions are non-explosive or only mildly explosive.