the volume is 1800 mph
The shape affects the ratio of surface area to volume. The greater the surface are to volume ratio, the faster the magma will cool.
Volume does not directly affect the formation of magma. Temperature, pressure, and mineral composition are the key factors that influence magma formation.
Mount St. Helens could possibly hold up to 0.3 cubic kilometers of magma in its magma chamber. However, the exact volume can fluctuate based on various factors such as temperature, pressure, and composition of the magma.
six seconds like an orgasam
The Krakatau volcano is 813 meters above sea level.
The elevation of Mt Krakatoa, or Krakatau, is 813m or 2,667 feet.
Subduction zones, where one tectonic plate slides beneath another, tend to produce the greatest volume of magma. The intense heat and pressure created during this process can cause melting of the subducted plate, leading to significant magma production. This magma can rise to the surface and result in volcanic activity.
Subduction zones produce the greatest volume of magma due to the subduction of one tectonic plate beneath another, allowing for the melting of rock and the formation of magma. This process is associated with volcanic arcs and chains of stratovolcanoes, contributing to significant magma production.
yes, I think so. because, very large volume of magma is ejected and then magma chamber can't support the volcano above it. then the volcano begins to sink into the earth.magma chamber empties and a new collapsed depression occurs.
The Asama volcano in Japan has the potential to hold a significant amount of magma beneath its surface. Its eruptions have been known to produce voluminous lava flows and ash plumes, indicating a substantial magma storage capacity within the volcano. However, the exact volume of magma that Asama can hold is difficult to determine precisely.
Krakatoa is located in Indonesia, between the islands of Java and Sumatra in the Sunda Strait.
Krakatoa's magma chamber is estimated to be around 40 cubic kilometers in volume. This large magma chamber plays a significant role in fueling the volcanic activity and explosive eruptions of Krakatoa.