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  2. Laterite - Wikipedia

    en.wikipedia.org/wiki/Laterite

    The mineralogical and chemical compositions of laterites are dependent on their parent rocks. [6]: 6 Laterites consist mainly of quartz, zircon, and oxides of titanium, iron, tin, aluminum and manganese, which remain during the course of weathering. [6]: 7 Quartz is the most abundant relic mineral from the parent rock. [6]: 7

  3. Major soil deposits of India - Wikipedia

    en.wikipedia.org/wiki/Major_soil_deposits_of_India

    Laterite soils are formed from chemical decomposition of rocks. soils mainly contain iron oxide which gives them characteristic pink or red color. These soils are found in Central,Eastern and Southern India. These are residual soils is formed from basalt and have high specific gravity. These soils are mostly composed as calcite depositions.

  4. List of rock types - Wikipedia

    en.wikipedia.org/wiki/List_of_rock_types

    The following is a list of rock types recognized by geologists.There is no agreed number of specific types of rock. Any unique combination of chemical composition, mineralogy, grain size, texture, or other distinguishing characteristics can describe a rock type.

  5. Angadipuram Laterite - Wikipedia

    en.wikipedia.org/wiki/Angadipuram_Laterite

    Angadippuram Laterite is a notified National Geo-heritage Monument [1] [2] [3] in Angadippuram town in Malappuram district in the southern Indian state of Kerala, India.The special significance of Angadippuram to laterites is that it was here that Dr. Francis Buchanan-Hamilton, a professional surgeon, gave the first account of this rock type, in his report of 1807, as "indurated clay", ideally ...

  6. Saprolite - Wikipedia

    en.wikipedia.org/wiki/Saprolite

    A represents soil; B represents laterite, a regolith; C represents saprolite, a less-weathered regolith; beneath C is bedrock. Saprolite is a chemically weathered rock. Saprolites form in the lower zones of soil profiles and represent deep weathering of the bedrock surface. In most outcrops, its color comes from ferric compounds.

  7. Lateritic nickel ore deposits - Wikipedia

    en.wikipedia.org/wiki/Lateritic_nickel_ore_deposits

    Typical nickel laterite ore deposits are very large tonnage, low-grade deposits located close to the surface.They are typically in the range of 20 million tonnes and upwards (this being a contained resource of 200,000 tonnes of nickel at 1%) with some examples approaching a billion tonnes of material.

  8. Geology of Cambodia - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Cambodia

    The geology of Cambodia is the study of the nation's rocks, minerals, water and landforms. Cambodia's ancient geologic history in the Precambrian is poorly understood. The region experienced tectonic activity and low-grade metamorphic rock formation throughout the Paleozoic , which a shift to marine conditions and fossil formation during the ...

  9. Oxisol - Wikipedia

    en.wikipedia.org/wiki/Oxisol

    Oxisols are a soil order in USDA soil taxonomy, best known for their occurrence in tropical rain forest within 25 degrees north and south of the Equator. In the World Reference Base for Soil Resources (WRB), [1] they belong mainly to the ferralsols, but some are plinthosols or nitisols. Some oxisols have been previously classified as laterite ...