rock (geology)

Examples of intrusive igneous rocks are diabase, diorite, gabbro, granite, pegmatite, and peridotite. The conditions required to form a metamorphic rock are very specific. It is made of minerals (which are crystalline), or other mineral-like substances. Igneous rocks are formed when molten magma cools, either above or below the surface. Rocks are classified according to characteristics such as mineral and chemical composition, permeability, texture of the constituent particles, and particle size. San Francisco, a truly unique city characterized by its proximity to the Pacific Ocean and amazingly steep hills, along with its many different neighborhoods with many different personalities, is the home that inspired and fostered the hippie counterculture movement in the 1960s as well as the famous Gold Rush era miners that began in 1849. Igneous rock (derived from the Latin word igneus, meaning of fire, from ignis meaning fire) is formed through the cooling and solidification of magma or lava. Where both heat and pressure play a role, the mechanism is termed regional metamorphism. Badlands National Park—Distance Learning: Layers of Sedimentary Rock, The National Mall—Virtual Field Trip of Washington, D.C. Igneous rocks are subdivided into two categories: intrusive (emplaced in the crust), and extrusive (extruded onto the surface of the land or ocean bottom), in which case the cooling molten material is called lava. Caring for the sustainability and enjoyment of your parks. Others, like this large rock that was dropped as a glacier melted, are as large as, or larger than, small cars. Typically, the melting of rocks is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. If a media asset is downloadable, a download button appears in the corner of the media viewer. The metamorphic rocks are formed when existing rocks are subjected to such large pressures and temperatures that they are transformed—something that occurs, for example, when continental plates collide. Join our community of educators and receive the latest information on National Geographic's resources for you and your students. Most shales (the lithified version of clay) contain some silt. These three classes, in turn, are subdivided into numerous groups and types on the basis of various factors, the most important of which are chemical, mineralogical, and textural attributes.
petroleum, natural gas, salt or even water) from the earth. Diagenesis is, as previously explained, the process of forming sedimentary rock by compaction and natural cementation of grains, or crystallization from water or solutions, or recrystallization. From Simple English Wikipedia, the free encyclopedia,, Creative Commons Attribution/Share-Alike License. Some rocks are made of the shells of once-living animals, or of compressed pieces of plants. Sedimentary rocks are generally stratified—i.e., they have layering. You cannot download interactives. The common textural terms used for rock types with respect to the size of the grains or crystals, are given in the Table. That means the Earth's crust is made of rock.

Igneous rock, or magmatic rock, is one of the three main rock types. Apparent (effective, or net) porosity is the proportion of void space that excludes the sealed-off pores. Depending on the type of close-packing of the grains, porosity can be substantial. The mining of rocks for their metals has been one of the most important things in human advancement. The audio, illustrations, photos, and videos are credited beneath the media asset, except for promotional images, which generally link to another page that contains the media credit. A rock is a naturally occurring solid. Rocks: Igneous, Metamorphic and Sedimentary. Total porosity encompasses all the void space, including those pores that are interconnected to the surface of the sample as well as those that are sealed off by natural cement or other obstructions.

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