Strata
Strata or stratum (singular) refers to layers of rock or soil with internally consistent characteristics that distinguish it from contiguous layers. Each layer is generally one of a number of parallel layers that lie one upon another, laid down by natural processes. They may extend over hundreds of thousands of square kilometers of the Earth's surface. Strata are typically seen as bands of different colored or differently structured material exposed in cliffs, road cuts, quarries, and river banks. Individual bands may vary in thickness from a few millimeters to a kilometer or more.
Formation[edit | edit source]
Strata are formed by the deposition of sediment. This process begins when the particles settle to the bottom in a body of water or on the ground surface. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation.
Classification[edit | edit source]
Strata can be classified based on their composition, origin, and texture. The primary classification is based on origin: strata formed from sediments deposited by water are called sedimentary rock strata, those formed from volcanic material are called volcanic rock strata, and those formed from the cooling of magma beneath the earth's surface are called igneous rock strata.
Importance in Geology[edit | edit source]
Strata play a crucial role in the field of geology. They provide valuable information about the geological history of a region. By studying the characteristics of strata, geologists can make inferences about the processes that shaped the earth's crust in the past. This can help in predicting future geological events and in the exploration of natural resources.
See also[edit | edit source]
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