Igneous rock
Igneous rock is one of the three main rock types, the others being sedimentary and metamorphic rock.
Igneous rocks are rocks formed from molten magma. The material is made liquid by the heat inside the Earth's mantle.
When magma comes out onto the surface of the Earth, it is called lava. Lava cools down to form rocks such as tuff and basalt. Intrusive rocks are made when the magma slowly cools to form rocks under the surface. Granite is one of these.
The word 'igneous' derives from the Latin word Ignis which is called fire in English.
Geological significance
The upper 16 km (10 miles) of the Earth's crust is composed of about 95% igneous rocks with only a thin, widespread covering of sedimentary and metamorphic rocks.[1]
Igneous rocks are geologically important because:
- their absolute ages may be determined from various forms of radiometric dating. This gives information about the dating of adjacent non-igneous geological strata;
- their features are usually characteristic of a specific tectonic environment (see plate tectonics);
- in some special circumstances they host important mineral deposits (ores): for example, tungsten, tin, and uranium are commonly associated with granites and diorites, whereas ores of chromium and platinum are commonly associated with gabbros.
Two types
Igneous rock occurs in two ways.
- Igneous rock formed from magma that has become solid inside the earth is called intrusive igneous rock. Examples of intrusive igneous rock types are gabbro, diorite, and granite.
- Igneous rock formed from lava that has become solid on the outside of the Earth is called extrusive igneous rock. This can happen because of the eruption of a volcano. Some extrusive igneous rock types are basalt, andesite, rhyolite, tuff, obsidian, and pumice.
Magma is made from my bhosda temperature fluid substance. Temperatures of most magmas are in the range 700 plutonic), or forced out to the surface (extrusion or volcanic) as lava, or blown out in exposions which include rock pieces (tephra).
Magma is made up of atoms and molecules of melted minerals. When magma cools the atoms and molecules rearrange to form mineral grains. Rock forms when mineral grains (often crystals) grow together. Granite, diorite, gabbro and basalt are a few types of igneous rock. Quartz is one of the chief minerals produced by igneous action; it is made of silica (SiO2), the most common molecule in igneous minerals. Some examples of igneous volcanic rock are pumice, obsidian (volcanic glass), and scoria and much more.
Minerals
Most of the minerals that make up igneous rock are of these types:[2]p12
Chemical make-up
Igneous rocks can be classified according to their chemistry. The main types are:
- Mafic: a silicate mineral or igneous rock which is rich in magnesium and iron.
- Felsic: silicate minerals, magma, and igneous rocks which are rich in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium.
The first six minerals in the list are silicates. Oxides are mostly of iron.
Igneous Rock Media
Volcanic eruptions of lava are major sources of igneous rocks. (Mayon volcano in the Philippines, erupting in 2009)
Natural columns of igneous rock separated from each other by columnar joints, in Madeira
Igneous rock illustration with English text and labels of a magma chamber as well as explanation of the meanings of the extrusive and intrusive types. Has better phrasing than
- Igneous rock eng text.jpg, which it is based on.
Basic types of intrusions: Template:Olist*
Extrusive igneous rock is made from lava released by volcanoes
Sample of basalt (an extrusive igneous rock), found in Massachusetts
Close-up of granite (an intrusive igneous rock) exposed in Chennai, India
Gabbro specimen showing phaneritic texture, from Rock Creek Canyon, eastern Sierra Nevada, California
Basic classification scheme for igneous rocks based on their mineral composition. If the approximate volume fractions of minerals in the rock are known, the rock name and silica content can be read off the diagram. This is not an exact method, because the classification of igneous rocks also depends on other components, yet in most cases it is a good first guess.
Total alkali versus silica classification scheme (TAS) as proposed in Le Maitre's 2002 Igneous Rocks – A classification and glossary of terms Blue area is roughly where alkaline rocks plot; yellow area is where subalkaline rocks plot.
Related pages
References
- ↑ Klein, Cornelis and Cornelius S. Hurlbut, Jr. 1985. Manual of mineralogy, Wiley, 20th ed, p275 ISBN 0-471-80580-7
- ↑ Smith P. 1900. Volcanoes: a planetary perspective. Oxford.