That depends on the sense in which you mean silent. Pyroclastic flows are generate by explosive rather than "quiet" eruptions. However, no sound escapes the flows themselves. Their unusual acoustic properties ensure that the sound they produce remains trapped inside.
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∙ 9y agoNo, pyroclastic flows are extremely loud and can produce sounds similar to thunder or jet engines as they travel down the volcano at high speeds. They are formed from superheated volcanic gases, ash, and rocks that move swiftly down the volcano's slopes, often reaching speeds of over 100 km/h.
Pyroclastic flow typically occurs during a violent eruption.
No. A "quiet" eruption will produce lava flows. Pyroclastic flows generally result from explosive eruptions.
No, pyroclastic flows typically occur during explosive volcanic eruptions when hot gas and volcanic particles travel rapidly down the side of the volcano. Quiet eruptions, such as lava flows, do not produce pyroclastic flows.
Pyroclastic flow
No. A pyroclastic flow can move at well over 100 mph.
Pyroclastic flow typically occurs during a violent eruption.
No. Pyroclastic flows are characteristic of explosive eruptions.
Mount Etna has had both explosive and "quiet" eruptions and has produced lava flows, lava fountains, and pyroclastic flows.
No. A "quiet" eruption will produce lava flows. Pyroclastic flows generally result from explosive eruptions.
No, pyroclastic flows typically occur during explosive volcanic eruptions when hot gas and volcanic particles travel rapidly down the side of the volcano. Quiet eruptions, such as lava flows, do not produce pyroclastic flows.
Pyroclastic flow.
Pyroclastic flow
an explosive volcano will usually have a pyroclastic flow
No. A pyroclastic flow can move at well over 100 mph.
The pyroclastic flow from the volcano devastated the surrounding area, burying everything in its path under a blanket of ash and hot gases.
the volcano that has pyroclastic flow in addition to liquid lava is the composite or stratovolcano.
Pyroclastic flow is gas that result from water mixing with loose material on the steep sides of a volcano.