Geology And Lithology

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Geology and Lithology of la Sierra de Guadarrama What is Geology and Lithology? Geology is the science that studies the origin and formation of the earth and the materials that compose them and Lithology is the science that studies of the rocks in an environment. Types and Characteristics of the Rocks: There are lots of types of rocks that the geologists studies, in Sierra de Guadarrama there are some type of rocks like: plutonics, metamorphics, sedimentaries and dykes rocks. Also the most antique rocks are the gneiss, marble and schist (Those are Metamorphic Rocks). Plutonics Rocks: Plutonics rocks are igneous rocks that had been melt at a deep distance. The most common type of plutonic rock is the granite. The granite of the Sierra de…show more content…
In Sierra de Guadarrama these rocks are 30 km underground and at a temperature of 750ºC The gneiss is a metamorphic rock due to the high temperatures and pressures in the interior of the earth's surfaces, it’s composed of quartz, feldspar and mica. The genesis is one of the most important rock in Sierra de Guadarrama due to its antiquity of 450 million years…show more content…
This pieces can be of multiple sizes and are carried by wind, water. In la Sierra de Guadarrama there are three types of Sedimentaries Rocks: marl, limestone and dolomite. Marl or also known as marlstone is a mudstone that contain a high variation of clays and silt. The limestone is a sedimentary rock that is practically composed of calcite, it is the 10% of all sedimentary rocks and it is white but the clay, sand and dust it can change the colours of the rocks. Dolomite or dolostone is a carbonate rock that is mainly composed of Calcium Magnesium Carbonate. This rocks can be found in the bottom of valleys, like in La Pinilla del Valle, that is totally exposed because the erosion that the rain caused. It is also found in the southeast slope in Sierra de Guadarrama Dyke Rocks: Dyke rocks origin inside of the terrestrial surface, because of the solidification from magma that goes up through cracks or breaches to the exterior. It is basically a igneous rock that extend from the interior of the earth's surface into the exterior and then fall over other rocks forming vertical tall walls. The process would

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