Erosional landforms are formed through a variety of erosional processes including weathering, decay, chemical reactions, and water. Erosion occurs when surface material is removed from the Earth’s surface by any natural process. Pediments and Pediplains Gently inclined rocky floors close to the mountains at their foot with or without a thin cover of debris, are

Wind is caused by the uneven heating of the air by the Sun, the irregularities of the Earth’s surface, and rotation of the Earth. The desert floors get heated up too much and too quickly because of being dry and barren. The heated floors heat up the air directly above them and result in upward

Landforms are formed by vast quantities of sand, gravel and debris which are carried by water. Depositional landforms include beaches, spits and bars. These three form during two different depositional processes. Beaches form as water carrying sediment comes to rest at the coastline; however, spits and bars (which are very similar) form due to sediment

Generally, the caves that extend into the cliff beyond the level of highest high tides are called sea caves. The sea caves can be classified as overhanging and underhanging caves, the former being those whose roofs overlie than their openings and the latter being those whose roof and opening line up. Sea caves are formed

There are different types of coasts which are defined by the type of bedrock. Low sedimentary coasts are ones which are formed over plain sedimentary rocks. The coasts are usually smooth with occasional incursions of water in the form of lagoons and tidal creeks. Low sedimentary coasts may have a few scattered islands that have