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  2. Metasedimentary rock - Wikipedia

    en.wikipedia.org/wiki/Metasedimentary_rock

    In geology, metasedimentary rock is a type of metamorphic rock. Such a rock was first formed through the deposition and solidification of sediment. Then, the rock was buried underneath subsequent rock and was subjected to high pressures and temperatures, causing the rock to recrystallize. The overall composition of a metasedimentary rock can be ...

  3. Geology of the Himalayas - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Himalayas

    The Himalayas border the Indo-Gangetic Plain to the south, Pamir Mountains to the west in Central Asia, and the Hengduan Mountains to the east on the China–Myanmar border. From east to west the Himalayas are divided into 3 regions, Eastern Himalaya, Central Himalaya, and Western Himalaya, which collectively house several nations and states.

  4. Geology of Himachal Pradesh - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Himachal_Pradesh

    The Greater Himalayan Crystalline complex, also known as the High Himalayan Crystalline Sequence, [14] is composed of high-grade metamorphic rocks aged between Paleoproterozoic and Ordovician. [4] Over the 4.5–8 km thick layer, paragneiss , schist and orthogneiss are observed.

  5. Geology of Nepal - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Nepal

    The rocks range in age from Precambrian to Miocene. The geology is complicated due to folding, faulting, and thrusting and are largely unfossiliferous. Tectonically, the entire Lesser Himalayas consists of two sequences of rocks: allochthonous, and autochthonous-para autochthonous units; with various nappes, klippes and tectonic windows.

  6. Metasomatism - Wikipedia

    en.wikipedia.org/wiki/Metasomatism

    Metasomatism (from the Greek μετά metá "change" and σῶμα sôma "body") is the chemical alteration of a rock by hydrothermal and other fluids. [1] It is traditionally defined as metamorphism which involves a change in the chemical composition, excluding volatile components. [2]

  7. Himalayan foreland basin - Wikipedia

    en.wikipedia.org/wiki/Himalayan_foreland_basin

    The Himalayan foreland basin has been divided on the basis of modern drainage divides, [2] and subsurface topography. [7] [8] Subdivisions based on drainage divides are most commonly used, with the Indus Basin reflecting the drainage area of the Indus River, and the Ganga Basin representing the drainage area of the Ganges River.

  8. List of rock types - Wikipedia

    en.wikipedia.org/wiki/List_of_rock_types

    Dolomite (rock), also known as Dolostone – Sedimentary carbonate rock that contains a high percentage of the mineral dolomite; Evaporite – Water-soluble mineral deposit formed by evaporation from an aqueous solution; Flint – Cryptocrystalline form of the mineral quartz

  9. List of rock formations - Wikipedia

    en.wikipedia.org/wiki/List_of_rock_formations

    Metamorphic rocks are created by rocks that have been transformed into another kind of rock, usually by some combination of heat, pressure, and chemical alteration. Sedimentary rocks are created by a variety of processes but usually involving deposition, grain by grain, layer by layer, in water or, in the case of terrestrial sediments, on land ...