Formation of Oolite and Pseudotachylite

Oolite

Pseudotachylite

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Formation

Mineral Content

Compound Content

Metamorphism

Types of Metamorphism

Weathering

Types of Weathering

Erosion

Types of Erosion

Oolites form when layers of calcite are deposited around a sand grain or fossil piece and are rolled around in calm water, which makes them round.

Calcite, Chert, Clay, Dolomite, Quartz, Sand, Silt

Aluminium Oxide, Ca, NaCl, CaO, Iron(III) Oxide, FeO, MgO

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Biological Weathering, Chemical Weathering, Mechanical Weathering

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Chemical Erosion, Coastal Erosion

Due to change in environmental conditions, rocks are heated and pressurized deep inside the Earth's surface. Pseudotachylite is formed from the extreme heat caused by magma or by the intense collisions and friction of tectonic plates.

Iron Oxides, Pyroxene, Quartz, Stishovite, Sulfides

Carbon Dioxide, Silicon Dioxide, Sulfur Dioxide, Sulphur

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Burial Metamorphism, Cataclastic Metamorphism, Contact Metamorphism

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Oolite and Pseudotachylite Formation

Formation of rocks is a long process and hence, Oolite and Pseudotachylite formation sounds very interesting. According to the formation, all rocks are divided into :Igneous Rocks, Sedimentary Rocks and Metamorphic Rocks. Igneous rocks form by crystallization of magma or lava. The magma is made up of various components of pre-existing rocks which have been subjected to melting either at subduction zones or within the Earth's mantle. Igneous rocks are generally seen at mid ocean ridges or in intra-plate hotspots. Sedimentary rocks are formed when sediments accumulate gradually. As the sediments are buried they get compacted as more and more material is deposited on top. Eventually the sediments become so dense that they form a rock. Metamorphic rocks are rocks which once existed as igneous or sedimentary rocks but have been subjected to varying degrees of pressure and heat within the Earth's crust. Get to know all about formation of Oolite and Pseudotachylite, composition of Oolite and Pseudotachylite and their transformation.