Which rocks are typically found at headlands where they erode at a slower rate?

Headlands are points of land that extend into bodies of water and are often characterized by their rugged and elevated terrain. The rocks found at these locations tend to be more resistant to erosion. Resistant rocks, such as granite or basalt, have a strong composition that allows them to withstand the erosive forces of waves, wind, and weathering over time.

These rocks are more durable and can form prominent features at the coast, contributing to the development of headlands. As weaker materials are eroded away by wave action, the resistant rocks remain intact, leading to their typical occurrence at headlands. This process creates dramatic cliffs and steep shorelines often seen in coastal landscapes.

In contrast, soft rocks, weak rocks, and loose rocks tend to erode more quickly, which usually results in the formation of low-lying beaches or areas of less dramatic coastal features rather than headlands. Understanding the relationship between rock type and erosion rates is crucial in coastal geography, particularly when examining how various formations, including headlands, are created and maintained.