Volcanoes are known land forms that can release ashes and lava. It actually depends on how big is the magma chamber of a volcano has but according to some scientist and volcanologist that the capacity of magma that a volcano can hold depends on its Volcanic Explosivity Index.
The exact amount of magma beneath Mount Pelée is unknown, as it varies over time and depends on the volcano's current activity level. It is estimated that there is enough magma to maintain volcanic activity and potential eruptions in the future. Monitoring techniques such as seismology and ground deformation measurements are used to better understand the volcano's magma chamber.
Basaltic magma is erupted along mid-ocean ridges because of decompression melting. As tectonic plates move apart, the pressure on the mantle decreases, causing it to melt and form basaltic magma. This magma then rises to the surface, creating new oceanic crust.
Minerals form from magma and lava through the process of crystallization. As the molten rock cools, atoms within the magma or lava arrange themselves into a crystalline structure to form solid mineral crystals. The specific minerals that form depend on factors such as the composition of the magma or lava and the cooling rate.
It is formed when hot (very hot) rocks experience a drop in surrounding pressure, or when subducted wet lithosphere is introduced into the mantle. When it "breaks out" onto the surface of the earth, we call it lava.
Mount Baker in Washington hold the highest seasonal snowfall record in the US. A total of 1,140 inches of snow or 95 feet fell during the winter of 1998 to 1999.
5,000,000 gollons
Mount Merapi, one of Indonesia's most active volcanoes, has a magma chamber that can hold approximately 10 to 20 million cubic meters of magma. This capacity can fluctuate based on geological activity and the accumulation of magma over time. The magma chamber's size and behavior contribute to the volcano's explosive eruptions, which are closely monitored by volcanologists.
Mount Unzen, located in Japan, is a stratovolcano that can hold a significant amount of magma, but exact figures are difficult to determine. The volcano has a complex history of eruptions and magma chamber dynamics, which can vary widely. Estimates suggest that its magma chamber can contain millions of cubic meters of magma, but the precise capacity can fluctuate based on geological conditions and volcanic activity. Overall, the exact volume can be challenging to quantify due to the volcano's dynamic nature.
Mount St. Helens has a magma chamber that can hold approximately 2 to 5 cubic kilometers of magma. However, the exact capacity can vary due to geological processes and the dynamics of volcanic activity. Since its major eruption in 1980, the volcano has continued to evolve, affecting the size and characteristics of its magma reservoir.
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450thousend littlers of magma the magma is a salty base and runny as it can get donot get in the path of this valcano
The 1991 eruption of Mount Pinatubo released an estimated 5 cubic kilometers of magma from underground.
The amount of weight a Sony TV mount can hold depends on the type of mount, but from what I have researched it seems that the mounts can hold up to 180 pounds.
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.
This mount can hold up to 125 pounds, and accommodates most 52" flat panel TVs.
Oshima, a volcanic island in Japan, has a magma chamber estimated to hold around 10-15 cubic kilometers of magma. This is based on studies of the island's geology and volcanic activity.