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
A pegmatite texture in a rock is a course-grained Igneous Rock. Granite Pegmatite is a common Igneous rock
It can be described as aphanitic. This just means that the rock has very small, hard to see crystals. The crystals do not have time to grow large when they are exposed to the air so they cool quickly and remain small. If water is added to the melt, the texture can be described as glassy (like obsidian).
Coarse large grained crystals.
Well when an igneous rock cools quickly, it ends up being fine-grained, as there wasn't any time for large crystals to form. Examples include andesite, basalt, tuff, scoria, etc. Obsidian is also the result of lava cooling extremely quickly, to the point where no crystals whatsoever were able to form.
Granite is a coarse grained igneous rock without Pyroxene.
pegmatite
A pegmatite texture in a rock is a course-grained Igneous Rock. Granite Pegmatite is a common Igneous rock
fine grained
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.
pegmatite
Fine grained has larger crystals and coarse grained has smaller crystals
Fine grained has larger crystals and coarse grained has smaller crystals
Granite is a coarse grained igneous rock without Pyroxene.
The texture is really glassy, like obsidian.
Obsidian.