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  2. Igneous rock - Wikipedia

    en.wikipedia.org/wiki/Igneous_rock

    Igneous rock (igneous from Latin igneus 'fiery'), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rocks are formed through the cooling and solidification of magma or lava. The magma can be derived from partial melts of existing rocks in either a planet's mantle or crust.

  3. List of rock formations - Wikipedia

    en.wikipedia.org/wiki/List_of_rock_formations

    Rock formations are usually the result of weathering and erosion sculpting the existing rock. The term rock formation can also refer to specific sedimentary strata or other rock unit in stratigraphic and petrologic studies. A rock structure can be created in any rock type or combination: Igneous rocks are created when molten rock cools and ...

  4. List of rock types - Wikipedia

    en.wikipedia.org/wiki/List_of_rock_types

    Tephriphonolite – Type of igneous rock – A volcanic rock with a composition between phonotephrite and phonolite; Tephrite – Igneous, volcanic rock – A silica-undersaturated volcanic rock; Tonalite – Igneous rock – A plagioclase-dominant granitoid; Trachyandesite – Extrusive igneous rock – An alkaline intermediate volcanic rock

  5. Rock (geology) - Wikipedia

    en.wikipedia.org/wiki/Rock_(geology)

    Metamorphic rocks are formed by subjecting any rock type—sedimentary rock, igneous rock or another older metamorphic rock—to different temperature and pressure conditions than those in which the original rock was formed. This process is called metamorphism, meaning to "change in form". The result is a profound change in physical properties ...

  6. Rock cycle - Wikipedia

    en.wikipedia.org/wiki/Rock_cycle

    This diamond is a mineral from within an igneous or metamorphic rock that formed at high temperature and pressure. The rock cycle is a basic concept in geology that describes transitions through geologic time among the three main rock types: sedimentary, metamorphic, and igneous.

  7. Igneous textures - Wikipedia

    en.wikipedia.org/wiki/Igneous_textures

    Phaneritic (phaner = visible) textures are typical of intrusive igneous rocks, these rocks crystallized slowly below Earth's surface. As magma cools slowly the minerals have time to grow and form large crystals. The minerals in a phaneritic igneous rock are sufficiently large to see each individual crystal with the naked eye.

  8. Stratigraphic column - Wikipedia

    en.wikipedia.org/wiki/Stratigraphic_column

    “The differences between rock unit types and fossils observed within the rock determine how these rocks are grouped for diagramming purposes. The column displays what types of rocks these units are composed of in two ways. The unit name itself reveals to geologists the rock type. and displays the relative thickness of the rock units”. [6]

  9. Plutonism - Wikipedia

    en.wikipedia.org/wiki/Plutonism

    Plutonism is the geologic theory that the igneous rocks forming the Earth originated from intrusive magmatic activity, with a continuing gradual process of weathering and erosion wearing away rocks, which were then deposited on the sea bed, re-formed into layers of sedimentary rock by heat and pressure, and raised again.