Tree roots can grow in cracks of rocks and break the rocks. The rocks of mountains
change due to many kinds of weathering.
Chemical weathering is when chemicals such as chemicals excreted from plants wear away at the earth's surface. Mechanical weathering is when natural forces wear away at the earth's surface such as rock.
Mechanical weathering typically occurs more quickly than chemical weathering. Mechanical weathering involves the physical breakdown of rocks into smaller pieces, while chemical weathering involves the alteration of rocks through chemical reactions. Factors such as temperature, precipitation, and rock composition can influence the rate of weathering.
Weathering involves ways that rocks break down without changes to their chemical state. Weathering involves mechanical forces e.g. wind and rainfall rather than chemical energy in disintegration or rocks.
There are several types of rock weathering: chemical (oxidation, chemical reaction to acidic fluids), mechanical (frost wedging, water hydraulics), and biological (plant root growth, burrowing by animals, plant secretions). Technically, any process that results in a diminution or reduction in rock size is classified as a weathering process. Therefore, the answer to the question would be 'yes'.
Both mechanical weathering (physically breaking rock into smaller pieces) and chemical weathering (chemically changing and even dissolving rock) result in rock layers being broken down. Water can be involved in both - freezing and then thawing lead to mechanical breaking by cracking rock, dissolving can lead to leaching chemical components of the rock, possibly weakening it and leading to pitting of the surface, for example. Also they both can break down some rocks faster than other rocks.
Both are mechanical, physical changes, involving the removal of surface material by the action of wind or water. But both can also involve chemical changes which would tend to change the rate of erosion or weathering - for example, acidic rain might cause limestone to weather faster than neutral rain water would.
Rock hardness affects the rate of weathering because softer rocks weather more quickly than harder rocks. Soft rocks are more easily broken down by chemical or mechanical weathering processes, while hard rocks are more resistant to weathering due to their strong mineral structure.
Weathering involves ways that rocks break down without changes to their chemical state. Weathering involves mechanical forces e.g. wind and rainfall rather than chemical energy in disintegration or rocks.
Rock is far more resistant to weathering (erosion) than sand.
During mechanical weathering, the physical breakdown of rocks occurs without changing their mineral composition. The rock may break into smaller pieces, but the minerals that make up the rock remain the same.
Mechanical (or physical) weathering is where physical forces (abrasion, exfoliation, frost action, root wedging) break the rock into smaller pieces but the composition of the rock is fundamentally unchanged. in other terms: Mechanical weathering is the process of erosion where larger rocks are broken down into smaller rocks without changing any of its chemical nature. The rocks are basically crashed by physical breakdown, rather than chemical. :)
Erosion due to wind-blown sand is a physical weathering process rather than a chemical weathering process. This type of erosion involves the mechanical breakdown and transportation of rock and sediment particles by wind action, rather than chemical alteration of the material.