Formation of Enderbite and Basaltic Trachyandesite

Enderbite

Basaltic Trachyandesite

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Formation

Charnockite is an intrusive igneous rock which is very hard and is formed due to weathering of existing rocks.

Basaltic Trachandesite is a fine-grained, hard rock that forms when bits of lava shoot out of volcanoes.

Composition

Mineral Content

Amphibole, Biotite, Feldspar, Hornblade, Micas, Muscovite or Illite, Olivine, Plagioclase, Pyroxene, Quartz

Olivine, Plagioclase, Pyroxene

Compound Content

Aluminium Oxide, CaO, Iron(III) Oxide, FeO, Potassium Oxide, MgO, MnO, Sodium Oxide, Phosphorus Pentoxide, Silicon Dioxide, Titanium Dioxide

Transformation

Metamorphism

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Types of Metamorphism

Contact Metamorphism, Impact Metamorphism

Contact Metamorphism

Weathering

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Types of Weathering

Biological Weathering, Chemical Weathering

Biological Weathering

Erosion

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Types of Erosion

Glacier Erosion, Sea Erosion, Water Erosion, Wind Erosion

Enderbite and Basaltic Trachyandesite Formation

Formation of rocks is a long process and hence, Enderbite and Basaltic Trachyandesite 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 Enderbite and Basaltic Trachyandesite, composition of Enderbite and Basaltic Trachyandesite and their transformation.