Question

difference between alluvial fan and cone

Answer 1

Deltas are similar to alluvial fans in shape, but are deposited in a different environment. Sediments that form deltas are transported in continuous flowing water. Delta deposits are found at the mouths of streams or rivers as they empty into lakes and oceans. ... River channels cross delta and alluvial fandeposits

Answer 2

Explanation:

An alluvial fan is an assortment of stream stores whose surface approximates a fragment of a cone that transmits downslope from the point where the stream leaves a mountaïnous zone. Alluvial fans have extraordinarily various sizes, inclines, sorts of stores and source-zone qualities. They are most across the board in the drier pieces of the world however have been contemplated likewise in muggy locales, for example, Japan, the Himalaya Mountains (Drew, 1873), and Canada (Winder, 1965), and in the Arctic districts (Hoppe and Ekman, 1964; Legget and others, 1966). [Talus cone is now and then taken to be more extreme than bone fan (see Talus Fan or Cone). A similar qualification is in some cases made with alluvial fan and cone. (editor)]

Affidavit on Alluvial Fans

Stream on alluvial fans changes from clear water to gooey mud. Water-laid silt happen essentially as sheets of dregs stored by a system of plaited streams, and as stream-channel stores. The release per unit of time Q is equivalent to the result of the width w, the mean...