That is correct.
No. Obsidian is formed by the very rapid cooling of lava which means that crystals do not have time to form.
Large grains of intrusive rock that cool down slowly are called phaneritic. This indicates that the individual mineral grains are visible to the naked eye. Examples of phaneritic rocks include granite and diorite.
Obsidian, which is volcanic glass, is a good example.
no texture
Red sandstone is a type of sedimentary rock composed primarily of sand-sized minerals or rock grains. Sandstone belongs to the mineral group of silicates, which are minerals that contain silicon and oxygen atoms.
Glassy textuered rocks, such as Obsidian.
Granite has large mineral grains compared to obsidian, basalt, and pumice. Granite is an intrusive igneous rock that forms deep within the Earth's crust, allowing for the growth of large mineral crystals due to slow cooling. Obsidian, basalt, and pumice are extrusive igneous rocks that cool quickly at the Earth's surface, resulting in smaller mineral grains or a glassy texture.
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.
No. Obsidian is formed by the very rapid cooling of lava which means that crystals do not have time to form.
All rock does not contain mineral crystals. Obsidian, or volcanic glass, in particular is a rock that has cooled so quickly from lava that mineral crystals were not able to form.
Molten rock contains liquified minerals, some solid mineral grains, and dissolved gasses.
Fine grains of rocks are referred to as "clasts." The word "clast" comes from the Greek word "klastos," meaning "broken."
Rocks are for the most part composed of one or more minerals. Obsidian is an exception because the mineral solution (lava) did not have time to form mineral crystals because of very rapid cooling. However, most obsidian will still contain some mineral crystals or crystal inclusions.
The slower the rate of cooling the larger the size of the crystals that can develop.
A rock with long flat mineral grains is likely to be schist. Schist is a metamorphic rock characterized by its foliated texture, with mineral grains aligned in a parallel fashion, giving it a distinct layered appearance.
Large grains of intrusive rock that cool down slowly are called phaneritic. This indicates that the individual mineral grains are visible to the naked eye. Examples of phaneritic rocks include granite and diorite.
No. Sandstone is not a mineral, it is a rock type.