Phaneritic rock has visible identifiable crystal grains. Aphanitic rock has crystal grains that are too small to be visible with the naked eye. In igneous rock, the difference is due to the amount of time spent in cooling. Long term cooling of magma underground leads to large crystals, rapid cooling of lava above ground leads to small crystal texture.
Granite is a phaneritic rock. Phaneritic rocks are coarse-grained, and they have visible crystals. Other phaneritic rocks include diorite, gabbro, and periodite. These rocks are also intrusive because they cool slowly.
And their texture, which can be aphanitic, phaneritic, glassy, or porphyritic. mineral composition and crystal texture
Glassy igneous rocks cool the fastest. The most likely had more nucleation. Pegmatic cooled the slowest, which is why its crystals are larger than 1 cm. Phaneritic is the next slowest in cooling. Porphyritic has slow then rapid cooling, while aphanitic igneous rocks also have rapid cooling.
These are igneous rocks that are too fine textured to an extent that there mineral grains or crystalline texture cannot be seen or distinguished with the necked or unaided eyes. They appear or occur as a whole single massive crystalline extrusive body of Igneous origin. Example is Obsidian.
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It is glassy.
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.
*fine-grained *coarse-grained
Granite is a phaneritic rock. Phaneritic rocks are coarse-grained, and they have visible crystals. Other phaneritic rocks include diorite, gabbro, and periodite. These rocks are also intrusive because they cool slowly.
Phaneritic texture refers to igneous rocks that have large, visible crystals, typically formed from slow cooling of magma beneath the Earth's surface. In contrast, aphanitic texture describes rocks with small, fine-grained crystals that are not easily visible to the naked eye, indicating rapid cooling of lava at or near the surface. The size of the crystals in these textures provides insights into the cooling history and environment of the rock formation.
Porphryitic igneous rock is composed of phenocrysts embedded in a finer matrix.
By definition, yes. In contrast, aphanitic rocks do not have visible crystals.
No, not all lava crystallizes to form igneous rocks with phaneritic textures. Phaneritic textures are characterized by large, visible crystals, which form when magma cools slowly beneath the Earth's surface. Lava that cools quickly on the Earth's surface forms igneous rocks with aphanitic textures, characterized by fine-grained or glassy structures.
And their texture, which can be aphanitic, phaneritic, glassy, or porphyritic. mineral composition and crystal texture
Rhyolite may be aphanitic or porphyritic.
No, diorite has a coarse-grained texture, which means its crystals are large enough to be visible without a microscope. Aphanitic rocks have a fine-grained texture where the crystals are too small to be seen with the naked eye.
The size of crystals formed when magma cools slowly, such as in the case of granite, is referred to as "phaneritic." In this process, larger crystals can develop because the slow cooling allows more time for the atoms to arrange themselves into a crystalline structure. This contrasts with "aphanitic" textures, where rapid cooling results in smaller, less visible crystals.