The unthreatening travelogue of Coast was built on the assumption that its audience would listen to just about anything as a helicopter-mounted camera produced a seemingly endless pan of the British Isles shoreline Cliffs!
Is it the massive shoreline cliffs or the teeming shore life that survives the relentless churning of our continents?
Measuring historical shoreline change and cliff retreat is an essential aspect of understanding the long-term geomorphic evolution of any coastal system.
This paper deals with investigation of the shoreline changes and cliff retreat along the 34 km section of the Black Sea coast at Shabla Municipality (Northeast Bulgaria).
Results for rates of shoreline change and cliff retreat were verified with preliminary field measurement studies and cross-checked with existing hydrodynamics, geology and geomorphology of the coast of Shabla Municipality.
Along the 1,100 miles (1,800 km) of shoreline, red sandstone cliffs average about 20 feet (6 metres) in height but occasionally exceed 50 feet (15 metres).
The course of the Columbia changed over the millennia, and from the kayak it's easy to trace the slow flattening of the Oregon shoreline from forested cliffs to marshland and sandbars.
Much of the shoreline includes high cliffs with alternating pocket beaches.
This cape consists of gently folded limestone, forming a rocky shoreline with low cliffs and numerous deep incisions along fault lines or abraded mylonitic rocks (Scheffers and Kelletat 2005).
