weathering is the breaking down or dissolving of rock. There are 3 types of weathering chemical, physical and mechanical.
The three sources of clay soil are weathering of rocks rich in minerals like feldspar and mica, deposition of clay particles by water or wind, and decomposition of organic material.
Possible sources of unconformities include erosion, deposition of sediment, tectonic movement that tilts or folds rock layers, and changes in sea level that expose rock layers to weathering and erosion.
Humans can impact weathering by increasing erosion through activities like deforestation, mining, and construction, which can accelerate the breakdown of rocks and soil. Pollution from industrial activities and agriculture can also contribute to chemical weathering processes by altering the composition of the atmosphere and water sources. Additionally, human activities that alter the natural landscape, such as paving over soil or changing drainage patterns, can affect the rate and intensity of weathering processes.
mechanical weathering
The three factors that affect weathering are mechanical weathering (physical breakdown of rocks), chemical weathering (chemical changes in rocks), and biological weathering (weathering caused by living organisms).
Chemical weathering of rocks on the continents & earth's interior.
Chemical weathering of rocks on the continents & earth's interior.
natural landforms such as rivers, streams, oceans. also weathering - such as rain.
The two primary sources for dissolved components in seawater are weathering of rocks on land, which releases minerals into rivers and eventually the ocean, and gases released by volcanic activity. These sources contribute ions like sodium, chloride, calcium, and magnesium to seawater.
The three sources of clay soil are weathering of rocks rich in minerals like feldspar and mica, deposition of clay particles by water or wind, and decomposition of organic material.
Possible sources of unconformities include erosion, deposition of sediment, tectonic movement that tilts or folds rock layers, and changes in sea level that expose rock layers to weathering and erosion.
Potassium enters soil through the weathering of rocks and minerals containing potassium, as well as through the decomposition of organic matter. Sources of potassium include fertilizers, plant residues, and animal manure.
mechanical weathering and chemical weathering are related because their both are types of weathering
-Mechanical weathering -Chemical weathering -Biological weathering
Physical weathering
Humans can impact weathering by increasing erosion through activities like deforestation, mining, and construction, which can accelerate the breakdown of rocks and soil. Pollution from industrial activities and agriculture can also contribute to chemical weathering processes by altering the composition of the atmosphere and water sources. Additionally, human activities that alter the natural landscape, such as paving over soil or changing drainage patterns, can affect the rate and intensity of weathering processes.
how are physical weathering and chenical weathering alike and different