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  2. Neptunism - Wikipedia

    en.wikipedia.org/wiki/Neptunism

    Neptunism is a superseded scientific theory of geology proposed by Abraham Gottlob Werner (1749–1817) in the late 18th century, who proposed that rocks formed from the crystallisation of minerals in the early Earth's oceans. The theory took its name from Neptune, the ancient Roman god of the sea.

  3. Cherufe - Wikipedia

    en.wikipedia.org/wiki/Cherufe

    The Cherufe is an evil humanoid creature made of rock crystals and magma.It is said that Cherufe inhabit the magma pools found deep within Chilean volcanoes and are the source of earthquakes and volcanic eruptions. [3]

  4. Liesegang rings (geology) - Wikipedia

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

    Chemical weathering of rocks that leads to the formation of Liesegang rings typically involves the diffusion of oxygen in subterranean water into pore space containing soluble ferrous iron. [7] Liesegang rings usually cut across layers of stratification and occur in many types of rock, some of which more commonly include sandstone and chert . [ 3 ]

  5. Rock (geology) - Wikipedia

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

    The types and abundance of minerals in a rock are determined by the manner in which it was formed. Most rocks contain silicate minerals, compounds that include silica tetrahedra in their crystal lattice, and account for about one-third of all known mineral species and about 95% of the earth's crust. [6] The proportion of silica in rocks and ...

  6. Mineral evolution - Wikipedia

    en.wikipedia.org/wiki/Mineral_evolution

    Gypsum crystals formed as the water evaporated in Lake Lucero, New Mexico. Allowable combinations of elements in minerals are determined by thermodynamics; for an element to be added to a crystal at a given location, it must reduce the energy. At higher temperatures, many elements are interchangeable in minerals such as olivine. [3]

  7. Impactite - Wikipedia

    en.wikipedia.org/wiki/Impactite

    Impactite is rock created or modified by one or more impacts of a meteorite. [1] [2] Impactites are considered metamorphic rock, because their source materials were modified by the heat and pressure of the impact. [3] On Earth, impactites consist primarily of modified terrestrial material, sometimes with pieces of the original meteorite. [3]

  8. Hadean zircon - Wikipedia

    en.wikipedia.org/wiki/Hadean_zircon

    Hadean zircon is the oldest-surviving crustal material from the Earth's earliest geological time period, the Hadean eon, about 4 billion years ago. Zircon is a mineral that is commonly used for radiometric dating because it is highly resistant to chemical changes and appears in the form of small crystals or grains in most igneous and metamorphic host rocks.

  9. Enhydro agate - Wikipedia

    en.wikipedia.org/wiki/Enhydro_agate

    This is a three phase inclusion in rock crystal quartz. The solid is a black material that is of bituminous origin. The liquid encased is petroleum, and the gas bubble is methane. Enhydros are formed when water rich in silica percolates through volcanic rock, forming layers of deposited mineral. As layers build up, the mineral forms a cavity in ...