Correct option is C
The correct answer is: (c), B and E only
Landforms associated with depositional activity typically result from the deposition of sediment by various agents such as water, wind, ice, or gravity.
Eskers and wave-built platforms are examples of landforms formed through depositional activity.
Eskers are long, winding ridges of sediment deposited by meltwater streams flowing within or beneath glaciers.
Wave-built platforms are gently sloping areas of sediment deposited by wave action along coastlines.
Barrier beaches and loess are examples of landforms formed through deposition.
Barrier beaches are long, narrow ridges of sand deposited parallel to the coastline by wave action.
while loess is a wind-deposited sediment consisting of fine particles such as silt and clay.
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Sea caves are geological formations formed by the erosive action of waves pounding against coastal rock formations over extended periods of time. These caves typically occur along rocky coastlines and are commonly found in areas with softer rock types such as limestone, sandstone, or shale.
A caldera is a large, basin-shaped depression formed by the collapse of the summit of a volcano following a massive eruption.
A playa is a flat, dry lakebed or basin that periodically fills with water, typically after rainfall or snowmelt, and then evaporates, leaving behind a layer of sediment or salt. Playas are commonly found in arid and semi-arid regions around the world and are characterized by their flat topography and lack of surface vegetation.
A meander is a winding, looping curve or bend in a river's course. It is a common feature found in rivers and streams, especially in their middle and lower reaches. Meanders form as a result of erosional and depositional processes acting on the river's channel and floodplain over time.
Arches are formed through the erosive action of natural forces, particularly water and wind. In regions with sedimentary rock layers that are horizontally stratified, erosion gradually wears away softer rock layers, leaving behind harder, more resistant layers.
A plunge pool is a geological feature formed by the erosive action of water, typically in the form of a waterfall or cascading stream. It is a basin or depression carved into the bedrock by the force of falling water and sediment transported by the water. Plunge pools are commonly found at the base of waterfalls and are characterized by their deep, circular or elliptical shape.

