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Lecture

Seacliff and wave.docx

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Department
Geology
Course
GEOL 2207
Professor
B.Ward
Semester
Summer

Description
Seacliff and wave-cut platforms, Santa Barbara  Cliff formed by erosion of waves  Sediments on the below the beach are sediments from the cliff  Dissolution – affects more rocks with CaCO3 – chalk, limestone, etc – subject to chemical break down Ex. Kits and Jericho Beaches Wave Refraction  Waves refraction concentrates energy on headlands (points from the shore) (convergence  erosion and deposited in the bays) and may
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