wo important classifications of weathering processes exist - physical and chemical weathering. Mechanical or physical weatheringinvolves the breakdown of rocks and soils through direct contact with atmospheric conditions, such as heat, water, ice and pressure. The second classification, chemical weathering, involves the direct effect of atmospheric chemicals or biologically produced chemicals (also known as biological weathering) in the breakdown of rocks, soils and minerals.[1]
The materials left over after the rock breaks down combined with organic material creates soil. The mineral content of the soil is determined by the parent material, thus a soil derived from a single rock type can often be deficient in one or more minerals for good fertility, while a soil weathered from a mix of rock types (as in glacial, aeolian or alluvial sediments) often makes more fertile soil.
When any type of rock undergoes weathering, it usually forms sedimentary rock. Weathering breaks down existing rocks into smaller pieces that get deposited and compressed to form sedimentary rocks over time.
Ice wedging is a form of mechanical weathering.
The two main types of weathering are mechanical weathering and chemical weathering. Mechanical weathering involves physically breaking down rocks into smaller pieces, while chemical weathering involves the alteration of rock composition through chemical reactions.
The two kinds of weathering are mechanical weathering, which breaks down rocks into smaller pieces without changing their chemical composition, and chemical weathering, which alters the chemical composition of rocks through processes like oxidation or dissolution.
Weathering is the process of breaking down and wearing away rocks, minerals, and soil through exposure to the elements such as wind, water, and temperature changes.
Two forms of mechanical weathering are frost heaving and plant root wedging. All forms of mechanical weathering result in the breakage of rock into smaller size particles.
Mountains and Valleys.
Ice live
Wind and rain
weathering results in the disintegration of rocks on a large scale. then these rocks break-up and forms soil and the soil forms the soil profile.
The weathering of asteroids. Fe2SiO4 + hn > Fe + FeSiO3 + O Forms a metallic crust.
Soil form by weathering of rocks...:)
The 2 kinds of weathering are the Mechanical or Physical Weathering and the Mechanical Weathering.
acid rain is one.
It is called weathering.
When any type of rock undergoes weathering, it usually forms sedimentary rock. Weathering breaks down existing rocks into smaller pieces that get deposited and compressed to form sedimentary rocks over time.
weathering occurs faster in warm and rainy climate. the rate of which soil forms depends on the climate and type of rock. so soil formation is faster when weathering is quicker too.