Sediments are usually formed from matter which falls to the bottom of oceans and lakes. The matter includes tiny pieces of other rocks, and dead animals, plants and microorganisms. Also, inorganic chemicals may be precipitated from solution in the water.
Sedimentary rocks cover 75–80% of the Earth's land area, but they make up only 5% of the Earth's crust. The relative abundances of the different types of sedimentary rocks are:
Consolidation[change | edit source]
Squeezed and compressed over time, the sediments become 'consolidated' (made solid) into layers of rock.
Otherwise, rocks may have the water squeezed out, yet remain for long periods with their character unchanged. There are many quarries of unconsolidated deposits where sand and pebbles are removed for the construction industry. Such quarries may be taking out sand which has lasted as sand since the Jurassic period. But consolidated sand, sandstone, can be a very hard rock.
Consolidated rocks may be changed some more, by water seeping through, or by heat and extreme pressure.
Types of sedimentary rock[change | edit source]
Sediments are formed by three processes: 1. Solids swept down from the land. 2. Bits & pieces laid down in water, e.g. shells. 3. Chemicals in solution, which may be precipitated. These sedimentary processes – weathering, transportation, and deposition – reach three final end products: quartz sand, shale (from clay), and limestone (CaCO3). Most sedimentary rocks are variations on this general pattern.
Chalk, limestone, and dolomite are all basically made from calcium carbonate. This comes from a mixture of minerals and pieces of animals (especially animal shells). They are mostly formed in oceans. Shales, sandstones, and conglomerates are all clastic rocks. They are made from pieces of other rocks. The pieces may have come from erosion by water, ice or wind. Coal is made from ancient plants; oil and natural gas is also organic in origin.
Sedimentary rocks may be found anywhere on Earth. When sedimentary rocks are heated and squeezed, they become metamorphic rocks. Igneous rocks have a volcanic origin. Over a very long time, rocks get recycled, in two ways. When marine sediments are raised above sea level, they get weathered, and the pieces carried down to the sea. On a much longer time-scale continental plates may collide. Then one plate goes under the other (is subducted), and all its material is recycled, emerging much later.
Relevant pages[change | edit source]
Footnotes[change | edit source]
- "Sediment and Sedimentary Rocks." .
References[change | edit source]
- Blatt, Harvey and Tracy, Robert J. 1996. Petrology: igneous, sedimentary and metamorphic, Freeman, 2nd Ed. ISBN 0-7167-2438-3
- Folk R.L. 1965. Petrology of sedimentary rocks PDF version. Austin: Hemphill’s Bookstore. 2nd ed. 1981, ISBN 0-914696-14-9
- Basic sedimentary rock classification
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