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What is Tronto River Geomorphology Study about?

The document summarizes the Late Pleistocene and Holocene evolution of the Tronto River valley in central eastern Italy. During the Late Pleistocene, the river had a braided pattern and deposited thick gravel deposits. During the Holocene, sea level rise and decreasing sediment load led to incision and formation of meander belts at different elevations. In the early Holocene, a beach extended 4 km inland at the river mouth. Human activities beginning around 3000-2000 years ago ended river incision and initi

Author

Elkhan Baihaqy

Language

EN