Mount Eyjafjallajökull primarily erupts basaltic lava, which is characterized by its low viscosity and fluid nature. This type of lava allows for relatively gentle eruptions, though the volcano is also known for its explosive activity due to the interaction of lava with water from the glacier that covers it. The eruptions can produce both lava flows and ash clouds, impacting air travel significantly during its notable eruption in 2010.
Mount Usu in Japan typically erupts with andesitic lava, which is a type of intermediate lava with a higher silica content compared to basaltic lava. Andesitic lava flows tend to be slower-moving and more viscous than basaltic lava.
The lava that formed Mount Fuji is primarily composed of dacite and andesite, which are intermediate in composition between basaltic and rhyolitic lava. This type of lava is viscous and flows relatively slowly, contributing to the steep slopes of Mount Fuji.
Mount Shasta primarily produces andesitic lava, which is a type of intermediate lava characterized by a medium viscosity and silica content. This type of lava typically results in eruptions that produce a combination of lava flows and explosive eruptions.
Mount Rainier is composed primarily of andesite lava, which is an intermediate type of lava that has a higher silica content compared to basaltic lava. This type of lava is more viscous, leading to explosive eruptions and the formation of volcanic cones like Mount Rainier.
Mount Pelée in Martinique is known for producing andesitic lava, a type of lava that is thicker and more viscous than the basaltic lava typically seen in shield volcanoes. This means that eruptions at Mount Pelée tend to be more explosive and can produce pyroclastic flows that travel quickly down the volcano's slopes.
probably basaltic lava because the 2010 eruption was very explosive
Eyjafjallajokull volcano in Iceland produces andesitic lava, which is a type of intermediate lava that is typically more viscous than basaltic lava. This can lead to explosive eruptions as gases get trapped within the molten rock before being released.
Mount Everest has no lava because it is not a volcano
Eyjafjallajokull is a volcano that recently spewed out ash, particles, and lava. The volcano is on Iceland.
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Mount Usu in Japan typically erupts with andesitic lava, which is a type of intermediate lava with a higher silica content compared to basaltic lava. Andesitic lava flows tend to be slower-moving and more viscous than basaltic lava.
it has metomorphic as rock and touchy lava
Mount Eyjafjallajokull was formed through a series of volcanic eruptions over thousands of years, building up layers of lava, ash, and volcanic rocks. These eruptions occurred along a fault line in the Earth's crust, allowing magma to reach the surface and create the mountain that we see today.
just no
Mount St. Augustine is a stratovolcano and lava domes
The Type of Lava that is really, really hot and could kill lots of people
Mt. Vesuvius produces felsic lava in a pyroclastic explosion.