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lava + pyroclastic flow mainly
Soufriere Hills volcano in Montserrat has primarily experienced explosive eruptions. These eruptions are characterized by the ejection of ash, gas, and pyroclastic material from the volcano. However, there have been periods of effusive eruptions as well, where lava flows have been released from the volcano.
Pyroclastic debris is usually produced by stratovolcanoes. However, shield volcanoes occasionally produce pryoclastic material in phreatomagmatic eruptions, which involve water interacting with magma.
The area surrounding a volcano which is in danger of eruptions, dangerous gasses, seismic activity, high temperatures, landslides/slips, lahars and pyroclastic flows etc.
In one sense, you can divide volcanic eruptions into two general types: "red" eruptions and "gray" eruptions. "Red" eruptions are generally nonexplosive or mildly explosive. These eruptions produce flows or fountains of glowing red lava. The lava flows can be destructive, but they generally move slowly, so "red" eruptions rarely cause a significant loss of life. "Gray" eruptions ares explosive. They produce clouds of hot ash and rock. Some of these clouds race down the slopes of a volcano as pyroclastic flows, burning everything in their path. These flows along with other hazards make "gray" eruptions extremely dangerous.
a Pyroclastic Shield Volcano. Basically a shield volcano covered in pyroclastic debris from earlier eruptions.
Explosive eruptions will produce pyroclastic rocks such as scoria, pumice, and tuff.
the Rabaul caldera is a Pyroclastic shield volcano. A pyroclastic shield volcano is basically a shield volcano, but made up of pyroclastic debris from earlier eruptions. Rabaul caldera is found in New Britain in Papua new Guinea.
lava + pyroclastic flow mainly
Soufriere Hills volcano in Montserrat has primarily experienced explosive eruptions. These eruptions are characterized by the ejection of ash, gas, and pyroclastic material from the volcano. However, there have been periods of effusive eruptions as well, where lava flows have been released from the volcano.
Generally not. Most eruptions in Hawaii are effusive.
are also known as Strato volcanoes. They are the most common type of volcano, and are formed by explosive eruptions of pyroclastic material followed by a quiet outpouring of lava.
Pyroclastic debris is usually produced by stratovolcanoes. However, shield volcanoes occasionally produce pryoclastic material in phreatomagmatic eruptions, which involve water interacting with magma.
The area surrounding a volcano which is in danger of eruptions, dangerous gasses, seismic activity, high temperatures, landslides/slips, lahars and pyroclastic flows etc.
an explosive volcano will usually have a pyroclastic flow
Generally not. Explosive eruptions may happen occasionally, but most eruptions are effusive.
Tuff is deposited by pyroclastic flows, which are almost always associated with stratovolcanoes. Cinder cones are somewhat explosive in their eruptions, but not enough to produce pyroclastic deposits.