Pollution due to the amount of petrol burnt.
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).
Living things impact weathering and erosion by contributing to the breakdown of rocks through processes like root wedging and burrowing. Nonliving factors such as water, wind, and temperature fluctuations also play a significant role in weathering and erosion by physically breaking down and transporting rocks and sediments. Together, these factors shape the landscape over time.
Yes, weathering, erosion, and deposition are constant natural processes that occur on Earth's surface due to factors such as temperature changes, rainfall, and wind. These processes happen continuously over time, shaping landscapes and contributing to geological changes.
The vegetation source of weathering is the organic acids released by plants as they decompose. These acids can break down minerals in rocks, leading to weathering processes such as chemical weathering. The roots of plants can also physically break apart rocks, contributing to mechanical weathering.
Factors such as temperature, precipitation, type of rock, vegetation cover, and human activity can influence both chemical weathering (breakdown of rocks through chemical reactions) and mechanical weathering (physical breakdown of rocks into smaller pieces). Temperature can affect the rate of chemical reactions, while precipitation can enhance chemical weathering by providing water for reactions and mechanical weathering by contributing to erosion. Vegetation can impact weathering by producing acids that enhance chemical weathering and by roots that can cause mechanical weathering. Human activity like construction and mining can accelerate both chemical and mechanical weathering processes.
weathering is a your mp thanku
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).
Living things impact weathering and erosion by contributing to the breakdown of rocks through processes like root wedging and burrowing. Nonliving factors such as water, wind, and temperature fluctuations also play a significant role in weathering and erosion by physically breaking down and transporting rocks and sediments. Together, these factors shape the landscape over time.
Some factors that affect the rate of weathering are the type of rock, the altitude and the climate.
Some factors that affect the rate of weathering are the type of rock, the altitude and the climate.
Yes, weathering, erosion, and deposition are constant natural processes that occur on Earth's surface due to factors such as temperature changes, rainfall, and wind. These processes happen continuously over time, shaping landscapes and contributing to geological changes.
The most important factors in chemical weathering are water and carbon dioxide.THIS IS TRUE
The most important factors that determine the rate at which weathering occurs are the type of rock and the climate. Rainfall affects the rate of weathering.
The vegetation source of weathering is the organic acids released by plants as they decompose. These acids can break down minerals in rocks, leading to weathering processes such as chemical weathering. The roots of plants can also physically break apart rocks, contributing to mechanical weathering.
Factors such as temperature, precipitation, type of rock, vegetation cover, and human activity can influence both chemical weathering (breakdown of rocks through chemical reactions) and mechanical weathering (physical breakdown of rocks into smaller pieces). Temperature can affect the rate of chemical reactions, while precipitation can enhance chemical weathering by providing water for reactions and mechanical weathering by contributing to erosion. Vegetation can impact weathering by producing acids that enhance chemical weathering and by roots that can cause mechanical weathering. Human activity like construction and mining can accelerate both chemical and mechanical weathering processes.
The sources of weathering include physical factors like wind, water, and temperature changes, as well as chemical factors such as acids, oxygen, and organic compounds. Biological factors like plants, animals, and microbes can also contribute to weathering processes.
Sedimentary rocks break down due to weathering processes such as erosion, mechanical weathering (like freezing/thawing), chemical weathering (like water and acids), and biological weathering (from plants/animals). These processes weaken the rock structure and can eventually lead to the breakdown of sedimentary rocks into smaller particles.