Till is an unsorted sediment deposited directly from the melting glacial ice; stream action is not involved.

Name: Till is an unsorted sediment deposited directly from the melting glacial ice; stream action is not involved.
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Till is a glacial deposit that is formed from melted ice sheets or glaciers. It consists of unsorted sediments like rocks, gravels, sand, and clay that are deposited directly by the melting water of the ice. Stream action is not involved in the formation of till deposits.

Till Is an Unsorted Sediment Deposited Directly from the Melting