A feature caused by the deposit of something else, such as a sand dune.
A tidal flat is not a depositional shoreline feature; rather, it is an intertidal area characterized by mud or sand flats that are exposed during low tide and submerged during high tide.
depositional
Depositional shoreline features are landforms created by the deposition of sediment along coastlines. Examples include barrier islands, spits, and beaches. These features are formed by the action of waves, currents, and wind carrying and depositing sediment along the shore.
It is a ridges of sediment that accumulate along the margins of river channels on floodplains.
A depositional mountain is a landform created by the accumulation of sedimentary material, such as sand, gravel, or rock fragments. It forms when these materials are deposited over time, often by processes like erosion or the movement of glaciers, rivers, or wind. As the sediment builds up, it can eventually form a mountainous feature.
An alluvial fan is a depositional feature which is formed when fast moving water comes out of a canyon, slows, and deposits the sediment it is carrying on a flat plain into a fan shaped structure.
A deferred junction is typically associated with depositional landforms. It forms when sediment is deposited at the intersection of two rivers or streams, creating a more stable junction point.
it is erosional
Eskers were formed by depositional processes. They are long, winding ridges of sand and gravel that were deposited by meltwater streams flowing in tunnels beneath glaciers during the last Ice Age.
depositional :)
the erosion zone