What materials are deposited at the foot hill zones to form Piedmont alluvial plains
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Piedmont, in geology, landform created at the foot of a mountain (Italian: ai piede della montagne) or mountains by debris deposited by shifting streams. Such an alluvial region in a humid climate is known as a piedmont for the Piedmont district of Italy; in arid climates such a feature is called a bajada
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The Piedmont Zone has formed as a result of coalescing alluvial fans, alluvial aprons and talus deposits. The fans have differential morphologies and aggradation processes within a common climatic zone and similar litho-tectonic setting of the catchment area.
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