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What is Hay 2016 ContinentalSlope about?

The continental slope is the steep transition from continental platforms to ocean basins, first defined by Rollin D. Salisbury in 1907. Its configuration varies significantly based on geological factors, including passive and active margins, sediment supply, and tectonic activity. Understanding the continental slope is crucial for marine geology, as it influences sediment deposition and erosion processes.

Author

Muhammad Rafli

Language

EN