Wiki User
∙ 11y agogreater precipitation in summer
Wiki User
∙ 11y agoAn increase in temperature and precipitation would likely cause the greatest increase in chemical weathering of local bedrock. Higher temperatures speed up chemical reactions, while increased precipitation provides more water to facilitate weathering processes.
An increase in temperature and precipitation would most likely cause the greatest increase in chemical weathering of local bedrock. Warmer temperatures can enhance chemical reactions, while higher rainfall can accelerate the dissolution of minerals in the bedrock, leading to increased weathering.
Tropical rainforests have some of the fastest rates of weathering due to high temperatures, heavy rainfall, and abundant vegetation that contribute to chemical weathering processes. Additionally, coastal areas with strong waves and high salinity can also experience rapid physical weathering.
Weathering is the process of breaking down rocks into smaller particles without any movement, while erosion involves the removal and transportation of these particles to a different location. Factors such as temperature changes, chemical reactions, and biological processes can contribute to weathering without leading to erosion.
internal forces
Weathering refers to the breakdown of rocks into smaller fragments through processes like mechanical, chemical, or biological processes. Erosion, on the other hand, involves the movement and transport of these weathered materials by wind, water, ice, or gravity from their original location to another place. Weathering breaks down rocks, while erosion transports the broken-down material.
An increase in temperature and precipitation would most likely cause the greatest increase in chemical weathering of local bedrock. Warmer temperatures can enhance chemical reactions, while higher rainfall can accelerate the dissolution of minerals in the bedrock, leading to increased weathering.
first the weathering happens which causes an erosion which makes deposition.
Weathering and erosion are two of the processes that change rocks. Weathering breaks down rocks into smaller fragments, while erosion transports these fragments to a new location. Together, these processes shape the Earth's surface over time.
The process of chemical weathering transfers chemicals from one location to another through the action of water, acids, or organisms. These agents break down minerals in rocks, releasing chemical elements that can be carried away by water, wind, or biological processes to weather objects over time.
Rock type, mineral content, degree of compaction, location of rock, rate & consistency of weathering agent.
Freeze-thaw weathering is the most common form of weathering at high latitude and high altitude locations. This process occurs when water seeps into cracks in rocks, freezes, expands, and causes the rocks to break apart over time.
frost wedging. It occurs when water enters cracks in rocks, freezes, expands, and widens the cracks, ultimately causing the rock to break apart.
Vdesdxcc
at plate boundaries
I think it's Chemical.
The greatest source varies on age location etc. but mine is from a drinking fountain.
latitude