Rock (geology): Difference between revisions
Jump to navigation
Jump to search
imported>Nereo Preto (Stub of an important article) |
imported>Todd Coles (categories, bold title) |
||
| Line 1: | Line 1: | ||
In [[geology]], a rock is an aggregate of [[mineral|minerals]]. Rocks constitute the [[lithosphere]], that is, the part of our planet below the [[soil]]. | In [[geology]], a '''rock''' is an aggregate of [[mineral|minerals]]. Rocks constitute the [[lithosphere]], that is, the part of our planet below the [[soil]]. | ||
==Classification== | ==Classification== | ||
| Line 7: | Line 7: | ||
# ''Igneous rocks'' are formed from the solidification of melts, i.e., [[magma|magmas]] or [[lava|lavas]]. When an igneous rock is formed within the [[crust]], it is called an ''intrusive rock''. ''Subvolcanic rocks'' are formed within the crust, but very close to the surface, and exhibite textures similar to those of volcanic rocks. Finally, igneous rocks formed from the solidification of lavas, either on dry land or under the sea, are called ''volcanic rocks''. | # ''Igneous rocks'' are formed from the solidification of melts, i.e., [[magma|magmas]] or [[lava|lavas]]. When an igneous rock is formed within the [[crust]], it is called an ''intrusive rock''. ''Subvolcanic rocks'' are formed within the crust, but very close to the surface, and exhibite textures similar to those of volcanic rocks. Finally, igneous rocks formed from the solidification of lavas, either on dry land or under the sea, are called ''volcanic rocks''. | ||
# ''Metamorphic rocks'' are formed within the crust by the textural and mineralogical modification of a previous rock, under high pressure and/or high temperature conditions. | # ''Metamorphic rocks'' are formed within the crust by the textural and mineralogical modification of a previous rock, under high pressure and/or high temperature conditions. | ||
[[category:CZ Live]] | |||
[[category:Earth Sciences Workgroup]] | |||
Revision as of 09:11, 1 August 2007
In geology, a rock is an aggregate of minerals. Rocks constitute the lithosphere, that is, the part of our planet below the soil.
Classification
Rocks can be classified based on their origin. There are thus three main groups of rocks:
- Sedimentary rocks are formed at the earth's surface by sedimentation of fragments of previously existing rocks, or by chemical precipitation. Most sedimentary rocks are marine.
- Igneous rocks are formed from the solidification of melts, i.e., magmas or lavas. When an igneous rock is formed within the crust, it is called an intrusive rock. Subvolcanic rocks are formed within the crust, but very close to the surface, and exhibite textures similar to those of volcanic rocks. Finally, igneous rocks formed from the solidification of lavas, either on dry land or under the sea, are called volcanic rocks.
- Metamorphic rocks are formed within the crust by the textural and mineralogical modification of a previous rock, under high pressure and/or high temperature conditions.