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Cox Comb is not a recognised wind erosional feature, it is a LOCAL NAME given to an elongated series of ridges running along the Cottonwood Creek valley (in the Escalante National Monument - Utah), created by erosion of upwardly-pointing folded rock layers.

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Which erosional agent typically deposit hills of inspected sediments?

Wind is a common erosional agent that can deposit hills of unsorted sediments called dunes. These dunes are often found in arid or coastal regions where wind can transport and deposit sand or silt to form distinct mound-like features.


What are some surface features formed by wind erosion?

Wind erosion can create surface features such as sand dunes, ventifacts (rocks shaped by abrasion), and yardangs (elongated ridges). These features are typically found in arid or semi-arid regions where wind is a dominant erosional force.


What erosional processes modify marine structures?

Some erosional processes that modify marine structures include wave action, tidal currents, and sediment transport. These processes can slowly wear down coastlines, cliffs, and other marine features over time. Wind and precipitation can also play a role in erosional processes in marine environments.


What is the most important erosional process in the desert?

Wind erosion is typically the most important erosional process in deserts. Strong winds can pick up and transport sand and dust, leading to the formation of features like sand dunes and ventifacts in desert landscapes.


Which area is wind a major erosional agent in?

Wind is a major erosional agent in arid and semi-arid regions, such as deserts. The wind carries and deposits sand and dust particles, shaping the landscape through processes like deflation, abrasion, and sandblasting. Wind erosion is particularly prominent in areas with little vegetation to anchor the soil.