sea arches and sea stacks provide evidence of weathering erosion in 3 to 5 sentences explain the roles weathering erosion play in creating these landforms
Sea arches and sea stacks are formed through the combined processes of weathering and erosion. Weathering, which includes both physical and chemical processes, weakens and breaks down the rocks along the coast. In the case of sea arches, weathering processes such as freeze-thaw action or abrasion by windblown sand create a cavity in the headland. Erosion, on the other hand, removes the weathered rock material, either by the force of waves or by the movement of water. As erosion continues, the sea arch enlarges and eventually collapses, leaving behind a sea stack. Thus, weathering weakens the rocks and erosion removes the material, resulting in the formation of sea arches and sea stacks.
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Weathering weakens rocks, while erosion removes the material. These processes work together to create sea arches and sea stacks. Weathering breaks down rocks along the coast, and erosion removes the weathered rock material. This leads to the formation of cavities in headlands that eventually collapse, forming sea arches. Over time, the continuous erosion leads to the formation of sea stacks.
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Weathering weakens rocks and erosion removes material, forming sea arches and sea stacks.
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Weathering and erosion play vital roles in the creation of sea arches and sea stacks. Weathering processes, such as freeze-thaw action or abrasion, gradually weaken and break down the rocks along the coast. This results in the formation of cavities or arches in the headlands. Erosion, driven by the force of waves or water movement, then removes the weathered rock material, further shaping and enlarging the arches. Eventually, the arches become unstable and collapse, leaving behind sea stacks. So, weathering weakens the rocks and erosion removes the material, both contributing to the formation of these distinctive coastal landforms.
