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the parent rock of obsidian is magma, because it is made from quickly-cooling magma after a volcanic eruption.
Obsidian
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.
Granite, rhyolite, obsidian, basalt, pumice, gabbro, diorite; all examples of igneous rock that by definition forms from the cooling of molten rock.
Glassy textured extrusive igneous rock, such as obsidian.
Igneoous rock is made from cooling of magma. Obsidian is a classic example of igneous rock.
the parent rock of obsidian is magma, because it is made from quickly-cooling magma after a volcanic eruption.
obsidian
Obsidian
Granite is a rock, whereas obsidian is a type of glass formed by cooling lava.
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.
Obsidian is an glassy, extrusive, igneous rock that is found in areas that have experienced rhyolitic eruptions. Obsidian is formed when the rhyolitic lava comes into contact with water. This quick-cooling results in the glassy texture of obsidian.
Obsidian is an extrusive igneous rock, formed from rapidly cooling lava.
Obsidian, or "volcanic glass," is made when molten rock comes out of a volcano and cools so quickly that no crystalline structure has time to form. This makes obsidian an extrusive igneous rock. The cooling occurs right at the surface.
Granite, rhyolite, obsidian, basalt, pumice, gabbro, diorite; all examples of igneous rock that by definition forms from the cooling of molten rock.
Obsidian is a rock that is essentially natural glass. Obsidian is formed by high volcanic heat and very fast cooling (So that crystallization has no time to occur).
Obsidian is a glassy rock formed from rapid cooling of acidic magma.