Graded Bedding 

Graded bedding is a layering in sedimentary rocks that is characterized by a decrease in grain size from the bottom to the top of the layer. This is in contrast to normal bedding, which is characterized by relatively uniform grain sizes throughout the layer. Graded bedding forms when sediment is deposited in a location where the energy of the depositing fluid (such as water or wind) decreases over ________ ______ __________ _________ __________ ___ _____ _________ __________ __________ ______ _____.
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