Andesite can be formed by fractional crystalization (crystals of olivine and other mafic minerals forming and falling out) of basaltic magma, or by assimilation of wall rocks into basaltic magma (hot magma melting side wall rocks and incorporating it into the magma).
Andesite can be either phaneritic or aphanitic depending on how it formed. Phaneritic andesite has larger crystals that are visible to the naked eye, suggesting slower cooling and crystallization deep within the Earth's crust. Aphanitic andesite has smaller crystals that are only visible under a microscope, indicating faster cooling at or near the Earth's surface.
Andesite is not any age in particular. Some deposites of andesite may be hundreds of millions of years old. However, since andesite is volcanic, some andesite rocks may only be minutes old.
No. It is volcanic. The plutonic equivalent of andesite is diorite.
Andesite is formed from the cooling and solidification of magma with a composition intermediate between basalt and granite. It commonly forms in volcanic settings through the partial melting of oceanic crust or the mixing of magma from different sources. The slow cooling process allows for the formation of crystals, giving andesite its characteristic texture.
No. Foliation is a term that applies to metamorphic rocks. Andesite is igneous.
Andesite can be either phaneritic or aphanitic depending on how it formed. Phaneritic andesite has larger crystals that are visible to the naked eye, suggesting slower cooling and crystallization deep within the Earth's crust. Aphanitic andesite has smaller crystals that are only visible under a microscope, indicating faster cooling at or near the Earth's surface.
Andesite typically has a light to dark gray color with a fine-grained texture, while diorite is usually darker in color with a coarse-grained texture. Additionally, andesite usually contains more silica than diorite, leading to differences in their mineral compositions and overall chemical makeup.
The rock that can be formed on the Eyjafjallajökull volcano is andesite. Andesite is an intermediate volcanic rock that is created from the cooling and solidification of magma within the volcano. It is a common rock type associated with explosive eruptions.
No. Andesite is a volcanic rock.
Felsic, high in silica. Mafic, low in silica. Intrusive, those formed underground. Extrusive, those formed above ground.
No. Andesite is an extrusive igneous rock.
Andesite is not any age in particular. Some deposites of andesite may be hundreds of millions of years old. However, since andesite is volcanic, some andesite rocks may only be minutes old.
Andesite has small crystals because it formed from lava that cooled relatively quickly at the Earth's surface, preventing larger crystals from growing. Rapid cooling does not allow enough time for the minerals to crystallize fully, resulting in smaller crystal sizes.
No. It is volcanic. The plutonic equivalent of andesite is diorite.
Yes. Andesite is an extrusive igneous rock.
Volcanic activity can form igneous rocks, such as basalt or andesite. These rocks are formed from the solidification of magma or lava ejected from a volcano.
Andesite is abundant in Leyte due to the volcanic activity in the region. Leyte is part of the Pacific Ring of Fire, a region known for its high volcanic activity, which has resulted in the widespread presence of andesite. This volcanic rock is formed from the solidification of magma beneath the Earth's surface and is commonly found in areas with past or present volcanic activity.