An example of refraction is when waves approach a straight shoreline at an angle. The part of the wave crest closer to shore is in shallower water and moving slower than the part away from the shore in deeper water.
The longshore transport is the process responsible for the movement of sand and sediment along the coastline. Sand and other particles are transported with the help of the longshore current and beach drift. Learn how these factors shape shorelines.
A wave-cut platform, coastal benches, or wave-cut benches is the narrow flat area often found at the base of a sea cliff or along the shoreline of a lake, bay, or sea that was created by the erosion of waves.
A sea arch is a natural arch or bridge made of stone that has been created when water wears away the underside of a rock, leaving just the top behind. They commonly form where cliffs meet the sea. Natural arches are created through the process of land, wind, or water erosion, or some combination of these methods.
A stack or sea stack is a geological landform consisting of a steep and often vertical column or columns of rock in the sea near a coast, formed by wave erosion. Stacks are formed over time by wind and water, processes of coastal geomorphology.
Barrier islands are long, narrow, offshore deposits of sand or sediment that run parallel to the coastline. They are separated from the main land by a shallow sound, bay, or lagoon and are often found in chains along the East Coast and Gulf of Mexico. The islands themselves are separated by narrow tidal inlets.
Breakwaters are structures constructed on coasts as part of coastal defense or to protect an anchorage from the effects of both weather and longshore drift.
Beach nourishment is the process of dumping or pumping sand from elsewhere onto an eroding shoreline to create a new beach or to widen the existing beach. Beach nourishment does not stop erosion, it simply gives the erosional forces (usually waves) something else to "chew on" for awhile.