Fred FLINTstone |
Metamorphic rocks are also created from other kinds of rocks, but for them to be metamorphic they must be subjected to extreme pressure. One of these rocks is Gneiss. Pronounced like "Gneiss to meet you," or "What a Gneiss day." Gneiss can easily be distinguished by the light and dark bands which run around it. It's typically formed when granite and diorite, along with several minerals, are put under pressure. Gneiss does not break into sharp points as easily as flint does, so it has much fewer practical uses. However, Gneiss found in western Greenland is the oldest crustal rocks that we know of. These rocks are nearly 3.5 billion years old. Now those are some "gneiss" old rocks.
Igneous rocks that don't begin life as other rocks. They are formed by the cooling and crystallization of magma, and although the other rocks may be melted down again, their presence is not very apparent in igneous rocks. Pumice is one of the most distinct of the igneous rocks. It is a very porous and light rock, produced during volcanic explosions. Like flint, it can be used for several purposes, possibly even more than the sedimentary rock. It is used to make light weight concrete, to decorate a garden, and to exfoliate dead skin. When a volcano erupts, pumice will literally rain from the sky, which is what happened in the Pinatubo Eruption. This eruption was the second largest in the world and filled nearby valleys with pumice and ash that went nearly 660 feet deep.
http://www.cals.uidaho.edu/soilorders/orders.htm for a full list of the orders and a small description of each. Soil is typically distinguished by its particle size. We use the social texture diagram to do this.
Soils are another factor in Geology. There are twelve different soil orders that are used to describe the types of soil. See
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