A mountain formed by hardened lava.
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.
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.
A typically non-depositional environment is an area characterized by erosion rather than sediment accumulation. Examples include active river channels where strong currents transport sediment away, steep mountain slopes, and glacial environments where ice movement can remove rather than deposit material. Additionally, areas with significant weathering and high-energy conditions, such as stormy coastlines, may also not support deposition.
Loess is primarily a depositional sediment, formed from fine particles of silt that are transported by wind and then deposited when the wind's velocity decreases. It typically accumulates in thick, blanket-like layers, often in areas lacking vegetation. While loess can be subject to erosion by wind and water, its formation process is fundamentally depositional.
Any type of structure formed by deposition, example , sandbars, island - deltas, riffles ( formed across the flow, as opposed to with the flow), which is a character of most mountain streams , and form almost dam like structures.
a depositional mountain
depositional
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
both
A swamp
Sedimentary depositional environment
The depositional features from the options provided are c) delta. A delta forms at the mouth of a river where sediment is deposited as the water slows down, creating landforms. A valley is a landform shaped by erosion and does not represent a depositional feature, while an aquifer is a geological formation that can hold water but is not a depositional feature. A river, on the other hand, is a flowing body of water and not a depositional feature itself.
Erosional landforms dominate an area where the ice flows to, while depositional landforms are found where ice flows from.