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Metamorphic Roks

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METAMORPHIC ROCKS Metamorphic rocks are altered forms of pre-existing rocks which might have been igneous or sedimentary. The alternation may be due to either heat or pressure or by both acting together. Un er t e effect of pressure and temperature certain of the original miners are no longer stable and give place to new minerals. Quartz, e spar, and hornblende are stable under both igneous and metamorphic conditions. In addition to new minerals, new textures arise during the process of alteration or metamorphism. Rocks not altered beyond recognition include quartzite (from sandstone) and slate (from clay). Rocks altered beyond recognition include rocks known as gneisses and schists. The original rock-forming material and the names of original rocks and metamorphic rocks produced by it are given below. Mineral Original rock Metamorphic rock Sand Sandstone Quartzite Clay Shale Slate, mica-schist Calcium ...

Sedimentary rocks

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Sedimentary Rocks Sedimentary Rocks Sedimentary rocks include all rocks formed by deposition in beds or layers (strata) of the material derived from older rocks and also cover rocks formed by chemical or organic agencies. The materials may be carried by water, wind or glacier, e.g., in the case of sandstone, shale, etc. The majority of these sedimentary rocks are formed by deposition on riverbeds, or seabed and into basins or depressions on the earth's surface. The consolidation of loose sediments into hard also by deposition of cementing materials into spaces between particles of the sediments. The chief cementing materials or some mineral finely spread throughout the rock. The colour of the rock often changes on account of alteration of the original constituents due to atmospheric agencies, chiefly water. The sedimentary rocks were formed practically in the horizontal position but due to earth movements associated with earthquakes or other causes, they were tilted from the horizo...

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