The rock type you're looking for is basalt -- St. Helens contains basalt, andesite, and dacite in the form of lava flows and pyroclastic deposits.
Andesite and dacite are produced by stratovolcanoes.
A mixture of dacite (65wt% SiO2) and basaltic andesite (53wt% SiO2).
Popocat?petl produces a mixture of andesitic and dacite lava in the current cycle of activity. Andesitic, or Basaltic Andesite, is black volcanic rock that contains 55% silica. Dacite, on the other hand, is an igneous, volcanic rock that has a composition that is between Andesite and Rhyolite.
Mt St Helen's eruption of 1980 was a pyrocastic flow diverse lava, ranging from olivine basalt to andesite and dacite). The magma is believed to come from another area laterally located to the east. Magma and rock under the volcano are cool.
The material erupted in the 1980 eruption of Mount St Helens was of a composition known as dacite. Minerals common in dacite are primarily quartz, potassium feldspar, and albite. However most of the dacite from the 1980 eruption came out as ash and pumice, which are varieties of volcanic glass. Although the chemical components were there, the material cooled to quickly for the minerals to form.
Andesite and dacite are produced by stratovolcanoes.
Dacite is more felsic in composition, containing more silica.
It varies in composition, but is usually andesite, dacite, or rhyolite.
A mixture of dacite (65wt% SiO2) and basaltic andesite (53wt% SiO2).
== == Rhyolite, basalt, pumice, obsidian, andesite, dacite, tuff, welded tuff, scoria.
In some cases, yes. However the most recent eruptions have produced dacite.
== == Rhyolite, basalt, pumice, obsidian, andesite, dacite, tuff, welded tuff, scoria.
Popocat?petl produces a mixture of andesitic and dacite lava in the current cycle of activity. Andesitic, or Basaltic Andesite, is black volcanic rock that contains 55% silica. Dacite, on the other hand, is an igneous, volcanic rock that has a composition that is between Andesite and Rhyolite.
Mt St Helen's eruption of 1980 was a pyrocastic flow diverse lava, ranging from olivine basalt to andesite and dacite). The magma is believed to come from another area laterally located to the east. Magma and rock under the volcano are cool.
basalt and dacite, and ranges from 57 to 63% silicon dioxide (SiO2)
The material erupted in the 1980 eruption of Mount St Helens was of a composition known as dacite. Minerals common in dacite are primarily quartz, potassium feldspar, and albite. However most of the dacite from the 1980 eruption came out as ash and pumice, which are varieties of volcanic glass. Although the chemical components were there, the material cooled to quickly for the minerals to form.
Rhyodacite are both intermediate-felsic volcanic rocks. They form from the eruption of highly viscous silica rich magma. In terms of composition dacite is in between andesite and rhyolite while rhyodacite is in between dacite and rhyolite. They are similar rocks, generally erupting explosively but occasionally forming lava domes or very thick lava flows.