Crystal size in these rock types is determined by their rate of cooling. Pegmatites have large crystals due to very slow cooling. Obsidian has microscopic crystals due to almost instantaneous cooling.
Pegmatite texture is a coarse-grained igneous rock texture characterized by exceptionally large crystals. These crystals can be several centimeters to several meters in size. The slow cooling of molten rock in pegmatite formations allows for the growth of such large crystals.
This is likely a pegmatite, which is a type of igneous rock known for its exceptionally large crystals. Pegmatites can contain minerals such as quartz, feldspar, and mica that have grown to substantial sizes due to the slow cooling and high concentrations of elements in the magma from which they formed. These minerals are often sought after by collectors for their impressive size and clarity.
Igneous rocks that cool quickly do not have time to form large crystals. This results in a fine-grained texture that appears smooth and may reflect light in a shiny manner. Examples of these rocks include basalt and obsidian.
Glassy textured extrusive igneous rock, such as obsidian.
Igneous rocks can have a variety of appearances. They can be glassy (obsidian), fine-grained (basalt), or coarse-grained (granite). Igneous rocks often exhibit interlocking crystals in various colors, depending on the mineral composition.
Pegmatite texture is a coarse-grained igneous rock texture characterized by exceptionally large crystals. These crystals can be several centimeters to several meters in size. The slow cooling of molten rock in pegmatite formations allows for the growth of such large crystals.
fine grained
Granite is a coarse grained igneous rock without Pyroxene.
fine grained
Actually, obsidian doesn't have grains at all. Technically obsidian is a glass, which means it has no internal structure. When geologists refer the the grain size of a rock, they mean how big the crystals that make it up are. Since obsidian has no crystals, it therefore has no grain size.
Fine grained has larger crystals and coarse grained has smaller crystals
Fine grained has larger crystals and coarse grained has smaller crystals
A pegmatite is an intrusive igneous rock comprised of coarse, interlocking mineral grains usually above three centimeters in diameter. Although very many pegmatites are granitic in composition, several hundred mineral species have been found in the most famous pegmatites worldwide, including many rare and valuable minerals. A few discovered pegmatite crystals have grown to several meters across.
Obsidian.
The black volcanic rock with small crystals is most likely basalt. Basalt is fine-grained and is commonly found in volcanic regions as a result of solidified lava flows. The small crystals are often composed of minerals such as plagioclase and pyroxene.
Obsidian has a small grain size due to its volcanic origin, which means that it cools quickly and does not have time to form large crystals. It is typically fine-grained and exhibits a glassy appearance.
This is likely a pegmatite, which is a type of igneous rock known for its exceptionally large crystals. Pegmatites can contain minerals such as quartz, feldspar, and mica that have grown to substantial sizes due to the slow cooling and high concentrations of elements in the magma from which they formed. These minerals are often sought after by collectors for their impressive size and clarity.