Ballard Cliff, Chalk cliff in Studland, England
Ballard Cliff is a chalk cliff at the northern end of Swanage Bay featuring tall white rock formations that rise sharply from the shore. The base exposes layers of softer sediment that contrast with the hard chalk above.
The cliff experienced major landslides in the late 1990s and early 2000s that created visible white diagonal lines across its face. These rock movements reshaped the appearance of the slope and continue to change slowly.
The cliff stands as part of the Jurassic Coast UNESCO World Heritage Site, representing millions of years of geological processes along the English coastline.
The best way to reach it is via the South West Coast Path, a established trail with clear viewpoints along the way. The route offers good views from above and also connects to the beach below for exploration from different angles.
A rotational landslide revealed a section of soft blue-grey clay that remains exposed today. This exposed layer makes it particularly valuable for geology students and researchers studying coastal erosion patterns.
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