The textbook answer would be granitic or rhyolitic lava. In reality composite volcanoes are highly variable, erupting the full range from basaltic to rhyolitic (granitic) materal and everything in between includin andesite and dacite. One composite volcano in Africa erupts unique carbonatite lava.
Pahoehoe is the most common lave for a composite volcano
A compostie volcano has an overall slope- 30 - 40 degrees.
the composite volcano has a alternating lava and ash eruptions
Composite volcanoes have very steep sides
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composite volcanoes
Cinder-Cone Volcanoes and Composite Volcanoes
Most composite volcanoes are comprised of Andesitic lava. Andesetic lava has an intermediate silica content compared to granitic with a high silica content and basaltic with a low silica content.
Three types of volcanoes are Cinder Cone Volcanoes, Shield Volcanoes and Composite Volcanoes.
it has mafic and felsic duhhhhh
There are four main types of volcanoes. These include shield volcanoes, cinder cones, composite volcanoes, and lava domes.
Composite volcanoes usually do not erupt mafic material. Intermediate material is the most common. The mafic material they do erupt is usually basalt.
No. Composite volcanoes erupt mostly ash and pumice.
Shield Volcanoes are made out of running lava. Not composite.
Aa and pahoehoe lavas are both basaltic in composition. The lava from composite volcanoes is likely to be granitic.
composite volcanoes
Cinder-Cone Volcanoes and Composite Volcanoes
Most composite volcanoes are comprised of Andesitic lava. Andesetic lava has an intermediate silica content compared to granitic with a high silica content and basaltic with a low silica content.
Three landforms that can be created from ash are cinder cone volcanoes, composite volcanoes, and shield volcanoes. Lava plateaus can also be formed.
Three types of volcanoes are Cinder Cone Volcanoes, Shield Volcanoes and Composite Volcanoes.
Compared with the lava in composite volcanoes, hawaiian lava has a slow silica content, is runny, and erupts at a higher temperature.