South to North
wrack is the debris along the shoreline
Swanage Bay is a picturesque curved bay located on the south coast of England. It is characterized by its golden sandy beach, clear blue waters, and iconic chalk cliffs. The bay is also framed by the Purbeck Hills, offering a stunning backdrop to the coastal scenery.
A baymouth bar is a form of deposition. It is created when sediment is deposited by longshore drift and tidal currents, forming a barrier that closes off a bay or lagoon from the open ocean.
The small bay will likely interrupt the longshore current by causing it to bend around the bay. This may result in the deposition of sediment on the updrift side of the bay and erosion on the downdrift side. The bay can act as a sediment trap, reducing the sediment transport along the coast.
A spit with a sharp bend in the ocean is commonly referred to as a "hooked spit." This geographical feature forms when sediment is deposited by longshore drift, creating a protrusion that curves at the end due to the influence of prevailing currents and wave action. The bend typically directs the spit inward toward the land or into a bay.
wrack is the debris along the shoreline
Swanage is in Dorset. Swanage Bay is to the West of the Isle of Wight on the South coast.
Formation of a Barrier SpitBarrier Spits are formed by the process of Longshore Drift. What is Longshore Drift?Longshore drift, sometimes known as drifting, longshore current, LSD (not common as it typically refers to a drug) or littoral drift is the movement of sediments, most often sand, along a coast parallel to its shoreline.
Swanage bay is most famous for their land form and stacks one of them is called old harry
A bay in Dorest, on the south coast of England, United Kingdom. The town of Swanage is located within the bay and the area is a major tourist attraction.
answer is 025 785
because durston bay has been eroded more
it is likely a beaturiful places too be
Erosion and weathering by water, such as wave action and longshore drift, can create a bay by wearing away softer rock or sediments along the coastline. This process typically occurs over a long period of time, resulting in the formation of a curved indentation in the land that we recognize as a bay.
Old Harry
well from ballard point to pervil point is about 1 mile :)
Baymouth bars form across bays at the entrance, where sediment is deposited by longshore drift to create a barrier that separates the bay from the open ocean. This feature results in shallow water inside the bay and can impact navigation and water circulation within the bay.