A mesa is a landform typically created by the erosional action of rivers over geological time scales. This process involves the wearing away of rock layers through hydraulic action, abrasion, and the transportation of sediment, eventually resulting in a flat-topped, steep-sided structure. Below is an explanation of why a mesa is the correct answer relative to the options provided:
Thus, a mesa is directly attributable to the erosional action of rivers, making it the correct answer.