Yes they do because of erosion and deposition
Sand is deposited on beaches by a variety of natural processes, including erosion of rocks and cliffs, wave action breaking down rocks into smaller particles, and rivers and streams carrying sediments to the coastline. These sediments are then moved along the coast by longshore drift and deposited on beaches when the energy of the waves decreases.
Both sediments and beaches are composed of a mixture of sand, silt, and gravel that has been deposited by water or wind. Sediments are the raw material that beaches are made of, as they accumulate along coastlines to form beaches through natural processes like erosion, transport, and deposition.
Erosion can lead to the formation of landforms such as valleys, canyons, and cliffs. Sediments from eroded rocks can also accumulate in new areas to form features like beaches, deltas, and sand dunes. Additionally, erosion can contribute to the shaping of riverbeds and coastlines over time.
Shale beaches are formed from the deposition of sediment form nearby shale cliffs which are eroded. The shale can also be deposited at a beach due to longshore drift.
Deposition is the process where sediments, like sand and soil, are deposited by wind, water, or ice. Over time, these sediments can build up in layers and form sedimentary rocks. Erosion and weathering play a crucial role in depositing sediments in different environments.
Beaches are found at the shoreline of rivers, lakes, and oceans. See the related link listed below for more information:
The Cliffs of Moher are mainly composed of sandstone and shale, which were deposited around 300 million years ago during the Carboniferous period. These sediments were subsequently compressed and uplifted to form the cliffs we see today.
Sediments have been transported over time through various natural processes such as erosion, weathering, and transportation by wind, water, glaciers, or gravity. These processes can move sediments from one location to another, shaping landscapes and depositing sediments in different environments. Eventually, these sediments can be compacted and cemented together to form sedimentary rocks.
Glacial deposits may form when glaciers move along mountains and break off sediments. These deposits can include a variety of sediment types such as till, moraines, and erratic boulders. As the glacier moves, it erodes and transports these sediments, eventually depositing them once the glacier melts.
Beaches: Sandy or rocky areas where waves deposit sediments. Sea cliffs: Steep, often vertical, cliffs that form as waves erode the coastline. Sea caves: Cavities formed by wave erosion in coastal cliffs. Spits: Narrow coastal landforms made of sand or gravel that extend into the sea.
Sandbars form as a result of waves depositing sand along a coastline, leading to the accumulation of sediments that rise above the water surface. They can be influenced by factors such as wave energy, currents, and the shape of the coastline.
by building up in one place for example, a river along a street flows carrying sediment and sometimes there are rocks that are placed at the end of the river. the rocks stop the river at that one point and all the sediment rushing through builds up over time in one place.