by the wind over millliion of years and it breaks down
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 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.
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
Mountains can become shorter over time due to processes like erosion, weathering, and tectonic activity. Erosion from factors such as water, wind, and ice can wear down the surface of mountains, while weathering breaks down the rocks that make up the mountains. Tectonic processes like plate movement can also cause mountains to slowly erode and decrease in height.
Mountains can get smaller due to various natural processes such as erosion, weathering, and tectonic activity. Wind, water, and ice can erode the rock and reduce the height of mountains over time. Additionally, tectonic forces can cause mountains to slowly decrease in height as the Earth's crust moves and adjusts.
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 and erosion
Weathering is the breaking down of rocks, soil, and minerals. Mountains are broken down by harsh weather and turned into stone, sand, and eventually soil.
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.
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
Mountains can become shorter over time due to processes like erosion, weathering, and tectonic activity. Erosion from factors such as water, wind, and ice can wear down the surface of mountains, while weathering breaks down the rocks that make up the mountains. Tectonic processes like plate movement can also cause mountains to slowly erode and decrease in height.
The Appalachian Mountains are belived to have been the highest mountains on earth roughfly 466 million years ago. The mountains are divided onto a series of ranges, with the individual mountains averaginf from a height of 3,000 feet (900 m). The highest of the group is Mount Mitchell at a height of 6,684 feet, (2,037 m)
Mountains can get smaller due to various natural processes such as erosion, weathering, and tectonic activity. Wind, water, and ice can erode the rock and reduce the height of mountains over time. Additionally, tectonic forces can cause mountains to slowly decrease in height as the Earth's crust moves and adjusts.
Older fold mountains have undergone millions of years of erosion processes like weathering and sedimentation, which have worn down their peaks and reduced their height. In contrast, younger fold mountains are still being uplifted by tectonic forces, so they have not experienced as much erosion and retain their height.
The two primary processes responsible for the decrease in height of the Appalachian Mountains are erosion and weathering. Erosion, driven by water, ice, and wind, gradually wears down the mountain surfaces, while weathering breaks down rocks into smaller particles. These processes have been ongoing for millions of years, leading to the gradual reduction of the mountains' elevation. Additionally, tectonic activity has diminished over time, contributing to the overall stability and erosion of the range.
Shape. Erosion would change the shape of the tops of the mountains. It may also change in height a little, too.
The tallest mountains on Earth are formed by the collision of tectonic plates. This collision forces rock layers to be pushed upward, creating towering mountain ranges such as the Himalayas and the Andes. Additionally, the process of erosion and weathering over millions of years can also contribute to the height of these mountains.