because when sea water crashes onto them they ware away due to salt erosion
A line of cliffs formed by displacement along a fault is known as a fault scarp.
cataract
White cliffs can be found in various locations around the world, but some of the most well-known examples include the White Cliffs of Dover in England, the White Cliffs of Rügen in Germany, and the White Cliffs of Møn in Denmark.
Relict boundary is a boundary that has ceased to function, but its imprint can still be detected on the cultural landscape An example would be East and West Berlin.
Fjords.
Relic cliffs are cliffs that used to be active (Eroded) when the sea reached the raised beach beneath it. (Higher sea levels) Now these cliffs are relict because they receive no erosion and have vegetation on them.
The mountains which are formed by by the blocks earth's crust or rock-bed developed by the tensional forces and faulting are known as Relict Mountains.It is also known as Block mountains.
Dover (white cliffs)
Relict Gull was created in 1931.
They are best formed in dry climates.
it is formed by erosion <3
caves, and cliffs
Cliffs can be formed by various processes, including erosion. Erosion slowly wears away the rock, leading to the formation of steep cliffs over time. Additionally, factors such as weathering, tectonic activity, and sea level changes can also contribute to the formation of cliffs.
Dry Climate
Weathered cliffs are formed as natural rain storms or snow and ice cause parts of the cliffs to break off and fall. This weathering also includes erosion caused by water passing from the top of the cliff to the bottom.
Sri Lankan relict ant was created in 1893.
A line of cliffs formed by displacement along a fault is known as a fault scarp.