Want this question answered?
Granite
Their texture could be formed from slow-cooling magma, from mineral precipitation and crystallization in pockets or fractures, or from recrystallization during metamorphism.
No. Obsidian is formed by the very rapid cooling of lava which means that crystals do not have time to form.
Rock
This is due to the rate of cooling - a slower rate of cooling results in large mineral grains because the molecules had time to maneuver into a crystalline lattice. A faster rate of cooling results in smaller mineral grains because the molecules were locked into place faster and therefore couldn't form the crystalline lattice structures before getting stuck.
Slow cooling of igneous rocks typically forms large crystal grains. This is because slow cooling allows more time for mineral grains to grow, resulting in larger crystals. Examples of rocks formed through slow cooling and having large crystal grains include granite and gabbro.
Sedimentary Rocks
This is as a result of difference in the rate of cooling of the Igneous rocks.
When water combines with mineral grains, the grains become larger. The increase in size of mineral grains strains the rock material and weakens it.
The slower the rate of cooling the larger the size of the crystals that can develop.
Quartz and mica. Clay minerals come from decomposing feldspars.
Mineral grains are crystals or pieces of crystals that vary widely in chemicalcomposition