Rock (geology)

From Citizendium, the Citizens' Compendium
Jump to: navigation, search
This article is a stub and thus not approved.
Main Article
Talk
Related Articles  [?]
Bibliography  [?]
External Links  [?]
Citable Version  [?]
 
This editable Main Article is under development and not meant to be cited; by editing it you can help to improve it towards a future approved, citable version. These unapproved articles are subject to a disclaimer.

In geology, a rock is a natural aggregate of minerals. Rocks constitute the lithosphere, that is, the part of our planet below the soil.

Classification

Hand sample of a sedimentary rock. This sample comes from the Carnian (Upper Triassic) of the Dolomites, and is better described as a oolitic/bioclastic grainstone, a kind of carbonate rock. The small spheres in the rock are oolites, all other elements are fossils. Among others, brachiopods, molluscs and echinoderm fragments are recognizable in this picture. It is typical of many carbonate rocks to be composed mainly by fossil shells.

Rocks can be classified based on their origin. There are thus three main groups of rocks:

  1. 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.
  2. 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.
  3. 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.

Sedimentary rocks

Sedimentary rocks are produced at the earth's surface, or after a relatively shallow burial, mostly through two processes: by lithification of fragments of a pre-existing rock, or by chemical precipitation from a supersaturated solution. The rocks produced by the first of these processes are called clastic, and those produced by precipitation, chemical sedimentary rocks. Petroleum and bitumen are also considered sedimentary rocks, produced by the accumulation and diagenesis of organic matter.

Clastic rocks

Chemical rocks

Most chemical rocks are produced by precipitation of calcium carbonate from seawater supersaturated with respect to CaCO3. This process is responsible for the formation of most limestones.

Chemical Sedimentary Rocks:

Igneous rocks

Metamorphic rocks