It gets deposited in a new place
A headland is formed by erosion and weathering along the coast. The softer rock and sediment of the coastline are eroded more quickly than the harder rock, creating a protruding landform. Over time, the continuous erosion and deposition processes shape the headland.
Sea cliffs: Steep rock faces along the coastline that are eroded by the constant force of waves. Sea caves: Hollowed-out spaces in coastal cliffs where waves have worn away softer rock layers. Wave-cut platforms: Flat, rocky areas at seashore level that are created by the gradual erosion of cliffs. Arch: A natural rock formation where a sea cave has eroded completely through a headland, leaving a bridge-like structure. Stack: A tall, isolated pillar of rock that is left standing as the surrounding cliff is eroded by waves.
In order to become a sedimentary rock a rock must be broken down or eroded by weathering. The sediments of the rock then go through the lithification process where they are cemented and compacted together forming a sedimentary rock.
That sounds like a sea stack. Sea stacks are tall, vertical columns of rock that form when a section of a headland is eroded by the sea, leaving a solitary pillar. They are typically found near coastlines and are a result of the continuous erosion of the surrounding rock.
A headland is a narrow strip of land that extends out into a body of water, such as an ocean or lake. Deposition at a headland occurs when sediment is deposited at the end of the headland due to wave energy decreasing and the current losing its ability to carry sediment. Erosion at a headland happens when waves and currents wear away the land, shaping the headland over time.
headland
A headland is formed by erosion and weathering along the coast. The softer rock and sediment of the coastline are eroded more quickly than the harder rock, creating a protruding landform. Over time, the continuous erosion and deposition processes shape the headland.
It is called an erection.
peninsulas are formed when waves start hitting a section of rock on the coastline that is not as easilly eroded as the rock around it. Over time it starts to stick out as a headland and if that process continues for enough years, the waves hitting the headland will start to curve around the sides and begin eroding the softer rock behind.
If eroded, deposited, compacted and cemented, it becomes clastic sedimentary rock.
When waves wash away the sides of a headland, it can eventually form a sea arch. As the waves erode the rock on both sides of the headland, a bridge of rock is left connecting the headland to the sea stack created by further erosion, forming the sea arch. Over time, the sea arch may also collapse due to continued erosion, leaving behind a standalone sea stack.
A mountain, a headland or a landscape feature.
Sea cliffs: Steep rock faces along the coastline that are eroded by the constant force of waves. Sea caves: Hollowed-out spaces in coastal cliffs where waves have worn away softer rock layers. Wave-cut platforms: Flat, rocky areas at seashore level that are created by the gradual erosion of cliffs. Arch: A natural rock formation where a sea cave has eroded completely through a headland, leaving a bridge-like structure. Stack: A tall, isolated pillar of rock that is left standing as the surrounding cliff is eroded by waves.
== == After a rock has been eroded you will find dirt,sand,rock and occcasionally silk.
In order to become a sedimentary rock a rock must be broken down or eroded by weathering. The sediments of the rock then go through the lithification process where they are cemented and compacted together forming a sedimentary rock.
Eroded rock
That sounds like a sea stack. Sea stacks are tall, vertical columns of rock that form when a section of a headland is eroded by the sea, leaving a solitary pillar. They are typically found near coastlines and are a result of the continuous erosion of the surrounding rock.