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  2. Asthenosphere - Wikipedia

    en.wikipedia.org/wiki/Asthenosphere

    Characteristics. The asthenosphere is a part of the upper mantle just below the lithosphere that is involved in plate tectonic movement and isostatic adjustments. It is composed of peridotite, a rock containing mostly the minerals olivine and pyroxene. [2] The lithosphere-asthenosphere boundary is conventionally taken at the 1,300 °C (2,370 ...

  3. Lithosphere - Wikipedia

    en.wikipedia.org/wiki/Lithosphere

    Lithosphere. A lithosphere (from Ancient Greek λίθος (líthos) 'rocky' and σφαίρα (sphaíra) 'sphere') is the rigid, [1] outermost rocky shell of a terrestrial planet or natural satellite. On Earth, it is composed of the crust and the lithospheric mantle, the topmost portion of the upper mantle that behaves elastically on time scales ...

  4. Rock (geology) - Wikipedia

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

    Rocks are composed primarily of grains of minerals, which are crystalline solids formed from atoms chemically bonded into an orderly structure. [4]: 3 Some rocks also contain mineraloids, which are rigid, mineral-like substances, such as volcanic glass, [5]: 55, 79 that lack crystalline structure. The types and abundance of minerals in a rock ...

  5. Framestone - Wikipedia

    en.wikipedia.org/wiki/Framestone

    The in situ fossils therefore form the supporting framework of the rock, with matrix material occurring in the interstices between the fossils." [3] Lokier and Al Junaibi (2016) [4] define a framestone as "an autochthonous carbonate-dominated rock supported by a rigid organic framework developed at the time of deposition." [5]

  6. List of rock types - Wikipedia

    en.wikipedia.org/wiki/List_of_rock_types

    Claystone – Clastic sedimentary rock composed primarily of clay-sized particles. Coal – Combustible sedimentary rock composed primarily of carbon. Conglomerate – Sedimentary rock composed of smaller rock fragments. Coquina – Sedimentary rock that is composed mostly of fragments of shells.

  7. Earth's mantle - Wikipedia

    en.wikipedia.org/wiki/Earth's_mantle

    Earth's mantle is a layer of silicate rock between the crust and the outer core. It has a mass of 4.01 × 10 24 kg (8.84 × 10 24 lb) and makes up 67% of the mass of Earth. [1] It has a thickness of 2,900 kilometers (1,800 mi) [1] making up about 46% of Earth's radius and 84% of Earth's volume. It is predominantly solid but, on geologic time ...

  8. Earth's crust - Wikipedia

    en.wikipedia.org/wiki/Earth's_crust

    Earth's crust is its thick outer shell of rock, referring to less than one percent of the planet's radius and volume. It is the top component of the lithosphere, a solidified division of Earth 's layers that includes the crust and the upper part of the mantle. [1] The lithosphere is broken into tectonic plates whose motion allows heat to escape ...

  9. Boudinage - Wikipedia

    en.wikipedia.org/wiki/Boudinage

    Boudinage is a geological term for structures formed by extension, where a rigid tabular body such as hornfels, is stretched and deformed amidst less competent surroundings. [1] The competent bed begins to break up, forming sausage-shaped boudins. Boudinage is common and can occur at any scale, from microscopic to lithospheric, and can be found ...

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