MT Fuji lava flows violently.
Mount Pinatubo erupt violently, but does not produce lava flows. It creates massive clouds of ash and pumice.
yes it flows violently
Lava can't flow violently. Highly explosive eruptions such as the 1980 eruption of Mount St. Helens do not produce lava flows: they produce clouds of ash, gas, and pumice. Mount St. Helens has produced "quiet" lava flows at times.
Mt Fuji was pyroclastic flow in 1707-1708[ its last eruption ] their for it was a violent eruption.
Mount Fuji in Japan is an example of a stratovolcano, also known as a composite volcano. This type of volcano is characterized by its steep, conical shape and is built up by alternating layers of lava flow, ash, and volcanic rocks. Stratovolcanoes are known for their explosive eruptions and typically have a central vent or crater. Mount Fuji is the highest peak in Japan and is an iconic symbol of the country.
quikly not violently
Mount Fuji has not erupted explosively in recent history; its last eruption occurred in 1707 during the Edo period, and it primarily produced ash rather than lava flows. The eruption was characterized by phreatomagmatic activity, which involves the interaction of magma with water, leading to explosive ash clouds. However, older eruptions of Mount Fuji did include lava flows. Overall, it is primarily known for its ash emissions rather than significant lava flows in its recent activity.
YES
They have practise evacuation drills and can have certain areas where no one is allowed to live or build on as it is where the lava flow is predicted to be.
Mount Fuji typically has quiet eruptions, characterized by the slow flow of lava and minimal explosive activity. However, it has also experienced explosive eruptions in the past, with the last major eruption occurring in 1707.
Mount Fuji primarily erupts and produces basaltic to andesitic volcanic rock fragments, including tephra, pumice, and volcanic ash. The lava flows from its eruptions are typically fluid, allowing for extensive lava flow development. These materials reflect the stratovolcano's explosive and effusive eruption styles, contributing to its iconic conical shape. The volcanic activity at Mount Fuji has created a diverse range of volcanic products over its history.
Yes, Mount Fuji has the potential for pyroclastic flows, although it has not experienced such an event in recorded history. Pyroclastic flows are fast-moving currents of hot gas and volcanic matter that can occur during explosive eruptions. The last major eruption of Mount Fuji was in 1707, and while it primarily produced ash and lava flows, future eruptions could potentially generate pyroclastic flows, especially given its stratovolcano structure. Monitoring and assessment are essential for understanding the risks associated with future activity.