because they can carry on
Water and wind can shape Earth's landscape through erosion, weathering, and deposition. Water can carve out valleys and canyons through its flow, while wind can create sand dunes and sculpt rock formations through abrasion. Over time, these processes can significantly alter the topography of the land.
Wind can erode and reshape a mountain by carrying away loose rock and soil, forming features like ridges and valleys. Water can also erode a mountain through processes like erosion, weathering, and sediment transport, creating features like rivers, waterfalls, and canyons. Together, wind and water can significantly alter the shape and appearance of a mountain over time.
Rock characteristics such as mineral composition and porosity can influence the rate of weathering. Climatic factors like temperature fluctuations and precipitation levels can also have a significant impact on the rate of weathering.
Erosion gradually wears down rock and soil through processes such as wind, water, and ice. This can lead to the formation of new landforms, like valleys, and the reshaping of existing ones, such as cliffs. Over time, erosion can significantly alter the topography and appearance of a landscape, creating unique features like canyons and deltas.
Some examples of slow changes on Earth's surface include erosion of rock formations by wind and water, the gradual shifting of tectonic plates resulting in the formation of mountains, and the weathering of rocks through exposure to the elements over time. These processes can take thousands to millions of years to significantly alter the landscape.
Rock chemistry, and size. Temperature and wind.
Water and wind can shape Earth's landscape through erosion, weathering, and deposition. Water can carve out valleys and canyons through its flow, while wind can create sand dunes and sculpt rock formations through abrasion. Over time, these processes can significantly alter the topography of the land.
mechanical weathering (by wind or water or perhaps tenacious plant roots or human activities)
Wind can erode and reshape a mountain by carrying away loose rock and soil, forming features like ridges and valleys. Water can also erode a mountain through processes like erosion, weathering, and sediment transport, creating features like rivers, waterfalls, and canyons. Together, wind and water can significantly alter the shape and appearance of a mountain over time.
windmills and wind energy
The speed required to move a rock with wind depends on the rock's size, shape, and weight. Generally, wind speeds of at least 20-30 miles per hour are needed to significantly move small rocks, while larger rocks may require much stronger winds exceeding 40-50 miles per hour.
Rock characteristics such as mineral composition and porosity can influence the rate of weathering. Climatic factors like temperature fluctuations and precipitation levels can also have a significant impact on the rate of weathering.
Erosion gradually wears down rock and soil through processes such as wind, water, and ice. This can lead to the formation of new landforms, like valleys, and the reshaping of existing ones, such as cliffs. Over time, erosion can significantly alter the topography and appearance of a landscape, creating unique features like canyons and deltas.
Some examples of slow changes on Earth's surface include erosion of rock formations by wind and water, the gradual shifting of tectonic plates resulting in the formation of mountains, and the weathering of rocks through exposure to the elements over time. These processes can take thousands to millions of years to significantly alter the landscape.
A reduction in surface wind speed will have a minor effect on the Coriolis force. The Coriolis force is primarily influenced by the Earth's rotation and the object's velocity, not the speed of the wind. Therefore, a decrease in wind speed will not significantly alter the Coriolis force.
Wind and glaciers abrade rock with their brute force.
The steps involved in breaking down mountain rock is called weathering. Weathering takes place naturally and is caused by wind, rain, ice, snow, and rivers. This breaks rocks into large pieces that continue to break down.