aa lava
Lava, ash, smoke, and rock
The San Cristóbal volcano in Nicaragua primarily erupts andesitic lava flows, which produce blocky lava fragments. These lava flows are intermediate in silica content and tend to be viscous, resulting in slower and more explosive eruptions.
Tinakula typically erupts basaltic lava, which is low in viscosity and can flow more easily compared to other types of lava. This type of lava often results in gentle to moderately explosive eruptions.
Shield volcanoes will erupt basaltic lava. Cinder cones erupt basaltic lava or basaltic andesite lava. Stratovolcanoes often erupt andesite lava, but may erupt basaltic or rhyolitic lava and all intermediate types as well.
Different types of lava result in different types of volcanic eruptions. Basaltic lava, which is low in viscosity, typically leads to effusive eruptions characterized by gentle flows. Andesitic or dacitic lava, with higher viscosity, can cause explosive eruptions with pyroclastic flows and ash clouds. Rhyolitic lava, the most viscous type, tends to form dome eruptions with slow-moving lava flows and explosive activity.
Lava, ash, smoke, and rock
Kilauea generally produces lava flows and lava fountains. Its current activity has also involved the formation of lava lakes. All of the lava involved is basaltic.
Igneous Rock
Lava
The San Cristóbal volcano in Nicaragua primarily erupts andesitic lava flows, which produce blocky lava fragments. These lava flows are intermediate in silica content and tend to be viscous, resulting in slower and more explosive eruptions.
Tinakula typically erupts basaltic lava, which is low in viscosity and can flow more easily compared to other types of lava. This type of lava often results in gentle to moderately explosive eruptions.
lots of pineapples
Shield volcanoes will erupt basaltic lava. Cinder cones erupt basaltic lava or basaltic andesite lava. Stratovolcanoes often erupt andesite lava, but may erupt basaltic or rhyolitic lava and all intermediate types as well.
It is called Lava
a shield volcano
Eyjafjallajökull Volcano produces basaltic and andesitic lava. The eruption in 2010 resulted in the release of both types of lava, creating a mix of volcanic products.
Different types of lava result in different types of volcanic eruptions. Basaltic lava, which is low in viscosity, typically leads to effusive eruptions characterized by gentle flows. Andesitic or dacitic lava, with higher viscosity, can cause explosive eruptions with pyroclastic flows and ash clouds. Rhyolitic lava, the most viscous type, tends to form dome eruptions with slow-moving lava flows and explosive activity.