These are sea-caves. The normal weathering processes act on the cliffs, but are accelerated by the pounding action of waves and the very rapid rises in air-pressure within the cave as a large wave crashes in.
The waves also tend todrag fallen rock away to expose fresh faces to attack.
So the wind is implicated, butin creating storm-waves.
These are known as ripples. They form due to the movement of water or wind over loose sand, creating small wave-like patterns on the surface. Ripples are common on beaches, in deserts, and along the shores of rivers and lakes.
Notches are formed through the process of erosion, where the repeated action of water or wind gradually wears away rock layers to create a narrow indentation or groove. This erosion can be caused by factors like wave action on coastlines, flowing rivers, or glacial movement. Over time, the continuous abrasion of the rock surface deepens and widens the notch.
Wind action can form various landforms such as sand dunes, arches, and hoodoos through processes like erosion, transportation, and deposition. These formations result from the interactions of wind with sediment and rock over time.
Three landforms created by wind are; sand dunes, yardangs (half-teardrop shaped formations hill sized, and deflation hollows (wind swept depressions. Good examples are in death valley, California, U.S.) Wind also contributes to significant sculpting of sandstone rock including arches.
Caves do not form naturally in slate with the possible exception of sea-caves (and then would be inherently unstable) and shallow rock-shelters. Slate mines (entirely artificial) can be very extensive but these are man-made.
Erosional caves are formed by the action of water or wind.
Caves that are in the desert which are formed by wind erosion
No, wave action is caused by wind. When wind blows over the surface of a body of water, it creates friction and transfers some of its energy into the water, forming waves. So, wind is the primary driver behind wave action.
Erosional caves are formed when water dissolves and carves through soluble rock formations like limestone, creating passageways and chambers underground. Over time, the continuous flow of water erodes the rock and forms distinctive cave structures. As the water table changes and the rock continues to weather, erosional caves can further evolve and change shape.
wave cut cliffs are formed by wind and tide driven waves
Some shoreline features formed by erosion include sea cliffs, sea arches, sea caves, and wave-cut platforms. Erosion by waves, currents, and wind gradually wears away the coastline, shaping these distinctive landforms over time.
Caves are typically formed by a combination of erosion and weathering. Erosion from water, wind, and ice can wear away rock formations, while weathering processes such as chemical weathering can dissolve minerals in the rock, creating openings that can eventually form caves over time.
The height of a wind-formed wave can be affected by factors such as wind speed, duration, and fetch (distance over which the wind has blown). Stronger winds over longer distances (fetch) can create larger waves, while shorter fetch or shorter duration of wind may result in smaller waves. The interaction between wind and the ocean surface also plays a role in wave height.
The atmosphere and hydrosphere interact with wave currents. Wave currents are formed by the interactions of wind with the surface of the ocean, which is part of the hydrosphere, while the atmosphere plays a crucial role in generating and sustaining these wind patterns.
Caves are mainly the result of natural geological processes, such as the dissolution of rock by water or chemical weathering. In most cases, caves are formed in limestone or other soluble rocks where water can dissolve the rock over time, creating underground voids. Additionally, caves can also be formed by volcanic activity, glacier movements, or erosion by wind.
A desert arch is formed by the action of wind carried sand grains abrading a weakness in the rock.
A desert arch is formed by the action of wind carried sand grains abrading a weakness in the rock.