A.Freezing
B.Plant Growth
C.Rain
D.Lightning
Yes, tornadoes are not a significant factor in the weathering of rocks. Tornadoes mainly cause physical erosion by moving and transporting rocks and sediment. Other factors like water, wind, and temperature fluctuations play a larger role in the chemical and mechanical weathering of rocks over time.
Which of the following is an example of chemical weathering?
Sedimentary rocks like sandstone and limestone tend to be less resistant to weathering and erosion compared to igneous or metamorphic rocks. Their softer composition and structure make them more susceptible to the effects of these processes.
The agent of weathering responsible for breaking rocks is mainly mechanical weathering. This process involves physical forces like wind, water, and ice that break down rocks into smaller pieces without changing their chemical composition. Examples of mechanical weathering include frost wedging, abrasion, and root pry.
Features such as rocks and minerals, soil composition, and landforms are most affected by weathering processes. Weathering can break down rocks and minerals, alter soil composition, and reshape landforms over time.
A.FreezingB.Plant GrowthC.RainD.LightningThe answer is B Plant Growth Because can plant growth do anything to rocks???? so its the least thing Cause freezing can break the rock ,Rain can make it into tiny pieces and lightning can break it quickly.
Yes, tornadoes are not a significant factor in the weathering of rocks. Tornadoes mainly cause physical erosion by moving and transporting rocks and sediment. Other factors like water, wind, and temperature fluctuations play a larger role in the chemical and mechanical weathering of rocks over time.
chemical reactions
Which of the following is an example of chemical weathering?
Sedimentary rocks like sandstone and limestone tend to be less resistant to weathering and erosion compared to igneous or metamorphic rocks. Their softer composition and structure make them more susceptible to the effects of these processes.
The process called weathering is responsible for the breaking up and wearing away of the Earth's rocks. The broken up rocks are then carried away by the process of erosion.
The agent of weathering responsible for breaking rocks is mainly mechanical weathering. This process involves physical forces like wind, water, and ice that break down rocks into smaller pieces without changing their chemical composition. Examples of mechanical weathering include frost wedging, abrasion, and root pry.
Features such as rocks and minerals, soil composition, and landforms are most affected by weathering processes. Weathering can break down rocks and minerals, alter soil composition, and reshape landforms over time.
Water is responsible for weathering through processes such as hydrolysis, where minerals in rocks react with water to form new minerals, and through erosion, where water physically wears down rocks and soil. Freeze-thaw cycles also contribute to weathering by causing rock fractures to expand as water freezes and thaws.
It is susceptible to chemical weathering more than other rocks from exposure to naturally acidic rainfall and groundwater.
If rocks stopped weathering, the process responsible for their breakdown and erosion would cease. This would result in a buildup of larger rocks on the beach, giving it a more rugged and rocky appearance. The beach may also experience less sand production over time since weathering is a key factor in creating sand from rocks.
The breakdown of sedimentary rocks is primarily caused by weathering processes such as physical (mechanical) weathering, chemical weathering, and biological weathering. Physical weathering involves the mechanical breakdown of rocks into smaller pieces, while chemical weathering involves the breakdown of rocks through chemical reactions. Biological weathering is the breakdown of rocks by living organisms such as plants and burrowing animals.