Yes
Actually, weathering does not reduce the height of a mountain...erosion does. The rate of mountain erosion depends on the nature of the mountain material rate of weathering and the climate primarily. Some disappear in thousands of years or less while other take millions of years to go.If orogenic-isostatic uplift is faster than the weathering/erosion rate, then there will be mountain growth instead of height loss.(c) http://answers.yahoo.com/question/index?qid=20070807161730AAtVNtr@maybdeleon.follow me )Rate This Answer
Rain water seeps into cracks and weak spots in the rock. When the water freezes, it expands as it turns into ice. It is the ice that forces the cracks to widen, and could cause rocks and boulders to come away and plunge down the mountain side. Scree shoots are another example of weathering.
Weathering breaks down rocks on a mountain into smaller pieces through processes like freeze-thaw cycles and chemical reactions. Erosion then transports these smaller pieces downhill through agents like water, wind, or ice, gradually wearing away the mountain over time. Together, weathering and erosion can reshape and reduce the size of a mountain.
Weathering breaks down rock into smaller pieces through processes like freeze-thaw cycles and chemical reactions. This weakens the rock, making it more susceptible to erosion by processes like wind and water. Over millions of years, this continuous cycle of weathering and erosion can slowly wear down mountains, reducing their height.
Weathering breaks down rocks into smaller particles, while erosion transports these particles, including gravel, away from the mountain. Sediment is the accumulation of these particles at the base of the mountain. So both weathering and erosion contribute to reducing mountains to gravel over time.
Actually, weathering does not reduce the height of a mountain...erosion does. The rate of mountain erosion depends on the nature of the mountain material rate of weathering and the climate primarily. Some disappear in thousands of years or less while other take millions of years to go.If orogenic-isostatic uplift is faster than the weathering/erosion rate, then there will be mountain growth instead of height loss.(c) http://answers.yahoo.com/question/index?qid=20070807161730AAtVNtr@maybdeleon.follow me )Rate This Answer
Rain water seeps into cracks and weak spots in the rock. When the water freezes, it expands as it turns into ice. It is the ice that forces the cracks to widen, and could cause rocks and boulders to come away and plunge down the mountain side. Scree shoots are another example of weathering.
Weathering breaks down rocks on a mountain into smaller pieces through processes like freeze-thaw cycles and chemical reactions. Erosion then transports these smaller pieces downhill through agents like water, wind, or ice, gradually wearing away the mountain over time. Together, weathering and erosion can reshape and reduce the size of a mountain.
Weathering breaks down rock into smaller pieces through processes like freeze-thaw cycles and chemical reactions. This weakens the rock, making it more susceptible to erosion by processes like wind and water. Over millions of years, this continuous cycle of weathering and erosion can slowly wear down mountains, reducing their height.
the way the turtle mountain was created was by weathering.
Weathering breaks down rocks into smaller particles, while erosion transports these particles, including gravel, away from the mountain. Sediment is the accumulation of these particles at the base of the mountain. So both weathering and erosion contribute to reducing mountains to gravel over time.
Weathering, erosion, and deposition will gradually break down and reshape the mountain range over time. Weathering will weaken rocks, erosion will transport the material downhill, and deposition will deposit the material in lower-lying areas. This process will eventually lead to the overall reduction in the height and size of the mountain range.
Over time, mountains can erode due to factors like weathering and tectonic activity, which can gradually reduce their height and steepness. As a mountain erodes, it may eventually be classified as a hill based on its elevation and slope characteristics.
Various weathering processes such as freeze-thaw cycles, erosion by water and wind, and chemical weathering can break down a mountain into gravel over time. These processes gradually weaken the rock, causing it to fracture and eventually disintegrate into smaller pieces.
The effect of weathering is to reduce the volume of the igneous rock.
Weathering breaks down rocks and sediments on the surface of mountains, weakening their structure over time. This makes the mountains more susceptible to erosion by natural forces such as wind, water, and ice, which gradually wear away the rock material and reduce the height of the mountains.
Weathering breaks down rocks into smaller particles over time, which are carried away by erosion. This process weakens the structure of mountains, leading to the gradual reduction of their height. Additionally, weathering creates space for plants to grow, which can further break down rocks and contribute to the erosion process.