Final answer:
A drumlin is a depositional landform created by the accumulation and shaping of unconsolidated glacial debris by glaciers.
Step-by-step explanation:
In the context of glaciation deposition, a drumlin is represented as a depositional landform. Drumlins are streamlined, elongated hills of unconsolidated glacial debris, or till, that are deposited and shaped by the advancing or retreating glaciers. They provide clues about the direction of ice movement during the time of their formation. Because drumlins are formed from material that has been picked up and then deposited by a glacier rather than being carved out by it, they are specifically associated with depositional processes.