mechanical weathering breaks it down into gradual sloped hills
I dont know :d !!
I dont know :d !!
Factors that affect the rate of mechanical weathering include temperature fluctuations, presence of water, wind intensity, type of rock or mineral composition, and presence of vegetation or organisms that can contribute to physical breakdown of rocks.
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).
The rates of mechanical weathering does not affect anything since the chemical properties remain unchanged. Only chemical weathering affects the chemical properties of an object.
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.
Climate can affect rates of mechanical weathering by influencing the frequency of freeze-thaw cycles and differential heating of rocks, leading to physical breakdown. In contrast, climate can influence rates of chemical weathering by determining the availability of water and temperature for chemical reactions which can break down minerals. Both types of weathering are related as they work together to break down rocks - mechanical weathering initiates the process by breaking rocks into smaller pieces which exposes more surface area for chemical weathering to act upon.
When rocks are broken down without any change to their chemical compositions it is mechanical weathering. Causes of mechanical weathering are Freezing and melting of water, Abrasion, when the rock is weather by an abrasive agent such as wind and sand, and exfoliation occurs when a rock is brought to the surface.
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.
Weathering can continue to affect the rounded rock by breaking it down into smaller pieces through processes such as mechanical weathering (e.g., erosion by wind and water) and chemical weathering (e.g., acidic rain dissolving minerals). Over time, the rounded rock can be further worn down and its surface features changed by these weathering processes.
Climate affects mechanical weathering by influencing the rate of freeze-thaw cycles, which can break down rocks through repeated expansion and contraction. In terms of chemical weathering, climate can impact the presence of water, temperature, and type of vegetation, all of which contribute to the breakdown of rocks through chemical reactions. Warmer and wetter climates generally promote more rapid chemical weathering processes.
Climate can affect rates of mechanical weathering by influencing temperature fluctuations, precipitation levels, and the frequency of freeze-thaw cycles. Chemical weathering, on the other hand, is influenced by factors such as the presence of water, oxygen, and acids in the environment. The two types of weathering are related in that they often work together to break down rocks: mechanical weathering weakens the rock's structure, making it more susceptible to chemical weathering, which further breaks down the rock's minerals.