a deposition landform is where some material is washed a shore for example sediment or metamorphic rocks/stones.
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.
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.
Erosional and depositional features along a shoreline are alike in that both are shaped by the action of waves, currents, and tides, influencing the coastal landscape. However, they differ in their formation processes: erosional features, such as cliffs and sea stacks, result from the wearing away of rock and sediment due to wave action, while depositional features, like beaches and sandbars, are formed by the accumulation of sediment transported by water. Ultimately, erosional features reflect the removal of material, whereas depositional features represent the buildup of sediment.
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.
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
a depositional mountain
A swamp
Sedimentary depositional environment
both
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.