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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.

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What type of lava does mount usu have?

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.


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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.


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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.


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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.


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