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.
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 plain is a flat landform that is created by the deposition of sediment carried by rivers, wind, or glaciers over time. This type of plain typically has a gentle slope and is formed by the accumulation of materials such as sand, silt, and clay. Depositional plains are often found near sources of water, such as rivers or coastlines.
Volcanoes are different from other mountains because they are built by deposits (magma), whereas other mountains are built by erosion. Volcanoes have lava, whereas other depositional mountains do not, even though they may have hot spots.
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.