Alluvial fans are landforms that develop at the base of mountainous regions where streams and rivers transfer sediment to the valley floor. These landforms are characterized by their fan-like shape and the presence of a braided stream channel.
Alluvial fans are landforms that develop at the base of mountainous regions where streams and rivers transfer sediment to the valley floor. These landforms are characterized by their fan-like shape and the presence of a braided stream channel.