When it cools and crystallizes into rock, the rock will be described as felsic igneous rock. Examples of felsic igneous rocks are granite, rhyolite, and pumice.
When magma crystallizes, a hard rock is formed composing of definite internal structural pattern. Such rock is called Igneous Rock.
pyroxene
Its texture.
Magma cools down about a week or so it is extremely hot about 350 degrees Fahrenheit , when it cools down it turns into crystals which are inorganic, naturally, solid, and having a atom arrangement.
They are rocks formed from magma that cools and crystallizes on the earth surface.
Gabbro forms from a magma that is rich in iron and magnesium, and poor in silica (quartz). The magma cools and crystallizes deep below the earth's surface. Gabbro is from the same kind of magma as basalt and diabase, but because it cools more slowly, it develops larger crystals.
There are two known processes by which magma ceases to exist: by volcanic eruption, or by crystallization within the crust or mantle to form a pluton. In both cases the bulk of the magma eventually cools and forms igneous rocks.
Igneous rock.
When it cools and crystallizes into rock, the rock will be described as felsic igneous rock. Examples of felsic igneous rocks are granite, rhyolite, and pumice.
When magma crystallizes, a hard rock is formed composing of definite internal structural pattern. Such rock is called Igneous Rock.
When it cools and crystallizes into rock, the rock will be described as felsic igneous rock. Examples of felsic igneous rocks are granite, rhyolite, and pumice.
pyroxene
Crystallization and cooling magma are related in the sense that cooling and crystallization occurs simultaneously. As the magma cools it crystallizes, the faster the rate of cooling the quicker crystals would develop and the slower the cooling the larger the crystals in other cases when the magma cool so rapidly crystal development may not be so prominent.
As magma cools, elements combine to form minerals.
Its texture.
Magma is molten rock, as the magma cools the minerals crystallize out of it, the slower it cools, the larger the crystals.