Magma is molten rock beneath the earth, usually with some trapped gasses in it. The composition of magma varies, but the most abundant compounds include:
Silica (SiO2), aluminum oxide (Al2O3), calcium oxide (CaO), sodium oxide (Na2O), magnesium oxide (MgO), potassium oxide (K2O), and iron oxide (FeO and Fe2O3). Trapped gasses, which make up a smaller proportion include water (H2O), carbon dioxide (CO2), and sulfur dioxide (SO2).
The magma that erupts at Mount Pinatubo is mainly dacitic in composition, which is a type of intermediate magma that is rich in silica. This type of magma typically leads to explosive eruptions due to its high viscosity and gas content.
An igneous intrusion is formed when molten rock (magma) is forced into preexisting rock and solidifies underground. Over time, the surrounding rock erodes away, exposing the igneous intrusion at the Earth's surface. Intrusions can take various shapes and sizes, such as dikes, sills, and laccoliths.
The size of the crystals. Large crystals mean the magma cooled slowly, small crystals are a sign that the magma was cooled quickly.
Saline.
A boulder-sized rock composed of a different type of rock than the surrounding area is the best evidence that it is an erratic. This indicates that the rock was transported from a distant location by glaciers or other geological processes.
The magma that erupts at Mount Pinatubo is mainly dacitic in composition, which is a type of intermediate magma that is rich in silica. This type of magma typically leads to explosive eruptions due to its high viscosity and gas content.
The ocean floor generally consists of basalt cooled from magma, and the overlying layers of sediment, both inorganic and organic.
A conditional statement
A conditional statement.
They became culturally different from one another.
primary
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it is a democracy and a federation
1
He was a soldier.
he IS a trusted member
never belonged