The coastal topography and features related to the type of rock in that area are related to the type of rock (geology) in that area. I visited many places to gather information on hypothesis 1. All of them are digitally recorded on the geological map of Pulpek Island. It is also used as a location map (see M1 for details). * Man O War Cove * Lulworth Cove * North Swanage Bay * South Swanage Bay * Reusing Points * North Studland Beach * South Studland Beach * Sandbanks * Durdle Door * Stairway Hole * Old Harry's Rocks We have a single sheet of paper We recorded the collection using the information of each area
Geology management over the coastal topography of the Swanage area can have a significant impact on many coastal areas. This is because the rock formations and structures of the rock affect the coastal topography and the various processes that occur may affect the formation of the topography. Starting from the Swanage area, you can see that the Swanage area is the Atlantic Ocean. This means that there are hard rocks and soft rock bands on the coast. In other words, since rocks have different hardnesses, the rocks are eroded at different speeds, resulting in different landscapes.
There are two main types of coastal formation. One is erosion and the other is sedimentation. Although they clearly show different terrain, each type may contain specific features of other terrain. In general, eroded beaches are coasts with little or no sediments, while sedimentary coasts are characterized by long sediments. In these coastal areas, both temporal and geographical changes may occur. The eroded coast often shows high rise and steep terrain. They often occur at the leading edge of the lithosphere plate and the West Coast of the Americas is a good example of that. Glacier activities may also lead to erosive coasts such as the northern New England and Scandinavian countries. Normally these coasts are occupied by exposed rocky areas, steep hilly areas, high altitude places near the coast.