Parent material, in soil science, means the underlying bedrock from which soil horizons form. Soils typically get a great deal of structure and minerals from their parent material. Soil science deals with soil as a natural resource on the surface of the earth including soil formation, classification and mapping; physical, chemical, biological, and fertility properties of soils per se; and these properties in relation to the use and management of soils. ... This article is about the type of rock. ...
Parentmaterial, in soil science, means the underlying geological material (generally bedrock or a superficial or drift deposit) in which soil horizons form.
Parentmaterials are made up of consolidated or unconsolidated mineral material that has undergone some degree of physical or chemical weathering.
Parentmaterial is classified by its last means of transport.
Parentmaterial is the unconsolidated mass or soil material from which a soil forms.
The parentmaterial determines to a great extent the physical and chemical composition of a soil, but the composition is also influenced by climate, relief, living organisms, and length of time.
Two distinct kinds of parentmaterial are typical in Scotland County: glacial till, which is material transported by a glacier, and loess, material transported by wind.
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