No. Andesite is an extrusive igneous rock.
plagioclase feldspar, pyroxene, horneblende (amphibole)
The mineral found in granite, andesite, gneiss, and hornfels is feldspar. It is a common mineral in these rock types and can exist in different varieties such as orthoclase, plagioclase, or potassium feldspar.
Both andesite and diorite are igneous rocks with an intermediate color index. Diorite; however, is intrusive and phaneritic, whereas andesite is aphanitic and extrusive. Andesite is said to be the extrusive equivalent of diorite. Diorite is made up of plagioclase feldspar and ferromagnesian mineral crystals, mainly amphibole. Contrarily, andesite may resemble rhyolite, meaning it presents a need for microscopic examination to see its mineral crystals. The two have a composition of plagioclase feldspar and amphibole, but it is much more difficult to detect in andesite.
The most common mineral in andesite is plagioclase feldspar, typically in the form of sodium-rich varieties like labradorite. Andesite also commonly contains other minerals such as hornblende, biotite, and pyroxene, which contribute to its overall composition. This volcanic rock is characterized by its intermediate silica content, which reflects the minerals present.
Andesite is typically classified as an igneous rock, specifically a volcanic rock, and is not categorized as either foliated or nonfoliated since those terms primarily apply to metamorphic rocks. Foliation refers to the alignment of mineral grains under pressure, which is not relevant to andesite. Instead, andesite has a fine-grained texture and can contain a mix of minerals, but it lacks the layered or banded appearance characteristic of foliated rocks.
Andesite is a type of volcanic rock that typically has a density ranging from about 2.5 to 3.0 grams per cubic centimeter (g/cm³). This density can vary based on its mineral composition and porosity. Generally, andesite is heavier than many sedimentary rocks but lighter than denser igneous rocks like basalt.
The mineral that can be found in all samples of rhyolite and andesite is typically plagioclase feldspar, which is often present in varying compositions. Rhyolite and andesite are both volcanic rocks that cool relatively quickly on the Earth's surface, leading to their fine-grained textures. While olivine and pyroxene can also be present in these rocks, plagioclase feldspar is the primary mineral characteristic of both rhyolite and andesite.
Andesite is a type of volcanic material that can appear grey or pink due to its mineral composition. Grey andesite contains a higher amount of mafic minerals like plagioclase and pyroxene, while pink andesite contains a greater proportion of felsic minerals like potassium feldspar.
Diorite and andesite are both igneous rocks, but they have different mineral compositions and origins. Diorite is a coarse-grained rock composed mostly of plagioclase feldspar and hornblende, while andesite is a fine-grained rock with a mix of plagioclase feldspar and mafic minerals like amphibole or pyroxene. Andesite typically forms from intermediate magmas in volcanic settings, while diorite forms from the slow cooling of molten rock deep beneath the Earth's surface.
Andesite rock is commonly used in construction as a decorative stone for landscaping, pathways, walls, and facades. It is also utilized as a component in the production of mineral wool insulation and as a soil amendment for gardening due to its ability to improve soil drainage. Additionally, andesite can be crushed and used as a base material in road construction and as an aggregate in concrete production.
basalt and dacite, and ranges from 57 to 63% silicon dioxide (SiO2)
dark gray, brown, greenish