Physical weathering is the breakdown of rocks into smaller pieces by natural forces like temperature changes,water and wind without altering their chemical composition.
Erosion is the process by which soil, rock or other material is gradually worn away and transported by natural forces such as wind ,water or ice.
Exfoliation is the removal of the outer layers of a rock after repeated contraction and expansion.
The outer layers of rock expand in the day. At night the outer layers of rock contract. Repeated expansion and contraction causes the outer layers to peel off.
Scree is a collection of loose, broken rock fragments that accumulate at the base of cliffs or steep slopes.
Tributaries are the smaller streams or rivers that flow into a larger river or main water body.
Deposition is the process of settling of material where sediments,soil or rocks are added to a landform or landmass by natural agents like wind, water or ice.
A delta is a landform created at the mouth of a river where it deposits sediments as it flows into a slower-moving or standing body of water, such an ocean or lake.
Rapids are fast-flowing, turbulent sections of a river where the water flows over steep, rocky terrain.
Agents are natural forces that cause an effect or result.
Physical weathering, Chemical weathering, Biological weathering
Freeze and thaw action is a physical weathering process where water seeps into cracks in rocks, freezes, expands and eventually causes the rocks to break apart
Freeze Thaw Action occurs when water enters cracks or pores in rocks and then freezes when the temperatures drop. As water freezes, it expands and exerts pressure on the surrounding rock. Over repeated cycles of freezing and thawing,this pressure causes the rock to crack and eventually break apart into smaller pieces. This process is common in cold climates.
Chemical weathering is the breakdown of rocks through chemical reactions, often involving water, acids or oxygen, that alter that rocks mineral composition.
Carbonation is a chemical weathering process where carbon dioxide dissolves in water to form carbonic acid, which reacts with minerals such as calcium carbonate in rocks, leading to their gradual dissolution and weakening.