a least 1,530 degrees
The viscosity of magma affects its ability to flow. For Krakatoa, the magma was characterized by high viscosity due to its high silica content, causing pressure buildup leading to explosive volcanic eruptions. The high viscosity of the magma at Krakatoa contributed to the violent nature of its eruptions in 1883.
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'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.
Krakatoa volcano typically has mafic magma, which is low in silica content and high in magnesium and iron. This type of magma tends to be more fluid and can lead to explosive eruptions due to the rapid release of gases.
Krakatoa is silica-rich, meaning it contains a high amount of silicon dioxide (silica) in its composition. This high silica content is associated with explosive volcanic eruptions due to the interaction between silica and magma.
Three Million gallons of magma
The viscosity of magma affects its ability to flow. For Krakatoa, the magma was characterized by high viscosity due to its high silica content, causing pressure buildup leading to explosive volcanic eruptions. The high viscosity of the magma at Krakatoa contributed to the violent nature of its eruptions in 1883.
the volume is 1800 mph
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'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.
Krakatoa volcano typically has mafic magma, which is low in silica content and high in magnesium and iron. This type of magma tends to be more fluid and can lead to explosive eruptions due to the rapid release of gases.
Everyone near the mountain died from the magma
Krakatoa is silica-rich, meaning it contains a high amount of silicon dioxide (silica) in its composition. This high silica content is associated with explosive volcanic eruptions due to the interaction between silica and magma.
It is a Strato Volcano.
no it does not
Krakatoa was a volcanic island. In 1883 that volcano produced a colossal eruption. This eruption drained about 10 cubic kilometers of magma from the magma chamber. The island collapsed into the space left behind, forming a depression called a caldera.
at least 1,530 degrees