magma or lava controls most texture in igneous rock
Igneous rocks are identified by first looking at the color index. Felsic igneous rocks contain mostly potassium feldspar. Intermediate igneous rocks contain mostly plagioclase feldspar. Mafic igneous rocks contain pyroxene, olivine, and plagioclase feldspar. Ultra mafic igneous rocks contain mostly olivine. Then igneous rocks are identified based on texture. For example, the texture of igneous rocks can be aphanitic, pegmatitic, phaneritic, glassy, vesicular, etc.
False. Igneous rocks are primarily classified by their origin (intrusive or extrusive) and their mineral composition, rather than their texture or shape. Texture can be a characteristic used to further describe igneous rocks, but it is not a primary method of classification.
Rocks with an aphanitic texture have fine-grained crystals that are too small to be seen by the naked eye. Common igneous rocks with this texture include basalt, andesite, and rhyolite. These rocks cool quickly at the Earth's surface, preventing larger crystals from forming.
Igneous rocks are not always thin and brittle. They can vary widely in thickness and texture, depending on their formation process. Intrusive igneous rocks, like granite, are often coarse-grained and can be quite thick, while extrusive rocks, such as basalt, can be thin and more fragile but also vary in strength. The characteristics of igneous rocks are influenced by factors such as cooling rate and mineral composition.
Granite, diorite, and gabbro are examples of igneous rocks that do not have a glassy texture. These rocks are formed from slowly cooled magma underground, allowing time for crystals to grow, giving them a coarse-grained appearance.
Phaneritic is the texture of igneous rocks. These types of rocks crystallized slowly.
Crystalline texture.
Obsidian
Igneous rocks are identified by first looking at the color index. Felsic igneous rocks contain mostly potassium feldspar. Intermediate igneous rocks contain mostly plagioclase feldspar. Mafic igneous rocks contain pyroxene, olivine, and plagioclase feldspar. Ultra mafic igneous rocks contain mostly olivine. Then igneous rocks are identified based on texture. For example, the texture of igneous rocks can be aphanitic, pegmatitic, phaneritic, glassy, vesicular, etc.
yes
False. Igneous rocks are primarily classified by their origin (intrusive or extrusive) and their mineral composition, rather than their texture or shape. Texture can be a characteristic used to further describe igneous rocks, but it is not a primary method of classification.
The relationship between an igneous rock's texture and where it was formed is that the texture depends on whether or not the rock is an extrusive rock or an intrusive rock. Those two different types of classifications for rocks tell you what the texture will be. For example, Intrusive rocks have a coarse-grained texture like granite and extrusive rocks have a fine-grained texture like basalt.
Course grained texture.
Correct, porphyritic texture is typically associated with igneous rocks and is not a common feature of sedimentary rocks. It is characterized by larger crystals, known as phenocrysts, surrounded by a fine-grained or glassy matrix. Sedimentary rocks are formed through the accumulation and lithification of sediments, which do not typically undergo the same crystallization processes as igneous rocks.
Rocks with an aphanitic texture have fine-grained crystals that are too small to be seen by the naked eye. Common igneous rocks with this texture include basalt, andesite, and rhyolite. These rocks cool quickly at the Earth's surface, preventing larger crystals from forming.
Igneous rocks are not always thin and brittle. They can vary widely in thickness and texture, depending on their formation process. Intrusive igneous rocks, like granite, are often coarse-grained and can be quite thick, while extrusive rocks, such as basalt, can be thin and more fragile but also vary in strength. The characteristics of igneous rocks are influenced by factors such as cooling rate and mineral composition.
These are extrusive igneous rocks with an aphanitic texture.