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  1. en.wikipedia.org › wiki › Red_soilRed soil - Wikipedia

    Red soil is a type of soil that typically develops in warm, temperate, and humid climates and comprise approximately 13% of Earth's soils. It contains thin organic and organic-mineral layers of highly leached soil resting on a red layer of alluvium .

  2. 4 days ago · Red soil is a type of soil that is characterized by its reddish color. It is also known as Terra Rossa, which is Italian for "red earth." Red soil is found in areas where the climate is warm and humid, such as in tropical and subtropical regions. It is usually fertile and good for agriculture.

  3. Red soil, Any of a group of soils that develop in a warm, temperate, moist climate under deciduous or mixed forests and that have thin organic and organic-mineral layers overlying a yellowish-brown leached layer resting on an illuvial (see illuviation) red layer. Red soils generally form from.

  4. Red soil is known as reddish clay minerals and is primarily composed of iron (hydro)oxides coated on soil particles. This type of soil tends to form in warm, temperate, humid climates, and in regions covered with deciduous or mixed forests.

  5. Red soils encompass various soil types such as ultisols, alfisols, and oxisols, characterized by their distinctive reddish color resulting from high iron content. The reddish color of red soils can range from reddish brown to reddish yellow.

  6. May 26, 2022 · Each soil has unique properties, nutrients, and minerals, and different things can grow in different soils. Red soil is one of those 70,000 kinds of soil. The reason it is called red soil is for its red color. The red color comes from un-hydrated iron oxides and is rich in iron and aluminum.

  7. en.wikipedia.org › wiki › UltisolUltisol - Wikipedia

    Ultisol, commonly known as red clay soil, is one of twelve soil orders in the United States Department of Agriculture soil taxonomy. The word "Ultisol" is derived from "ultimate", because Ultisols were seen as the ultimate product of continuous weathering of minerals in a humid, temperate climate without new soil formation via ...