Mount Rangitoto, located in New Zealand's Hauraki Gulf, primarily features basaltic lava, which is characteristic of shield volcanoes. This type of lava is low in viscosity, allowing it to flow easily and create broad, gently sloping landforms. The eruption style at Rangitoto is predominantly effusive, resulting in the formation of extensive lava fields and the unique volcanic landscape we see today.
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.
Mount Everest has no lava because it is not a volcano
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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
probably basaltic lava because the 2010 eruption was very explosive
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.
Basalt
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.
because it is.
stratovolcano