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 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.
Deposition is when particals are dropped of and left. Erosion is where particales are carried away
Loess is a type of sediment consisting of windblown particles, typically found in flat or gently sloping areas. It is unlikely to be found on cliffs as it requires a specific depositional environment with minimal slope for accumulation. Cliff formations are more likely to consist of harder rock types or deposits that have been eroded or weathered from the cliff face.
it is erosional
depositional
both
Erosional landforms dominate an area where the ice flows to, while depositional landforms are found where ice flows from.
Striation is typically erosional. Striations are long, narrow lines or grooves on a rock surface caused by the movement of a glacier, which acts as a powerful scouring tool that can scrape and polish the bedrock beneath it as it flows.
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.
what is the answer
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.
Erosional and depositional features along a shoreline are alike in that both are formed through the action of waves, currents, and tides. However, they differ in that erosional features involve the removal of sediment and reshaping of the coastline, while depositional features involve the accumulation of sediment and building up of the shoreline.
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.
Non-examples of loess include sand dunes, silt deposits in riverbeds, and rocky terrains. These examples do not exhibit the specific characteristics of loess, such as its fine-grained, silty composition and its unique depositional environment.
Erosional features along a shoreline are formed by the removal of sediment by natural forces like waves and currents, while depositional features are created when sediment is deposited by these forces. Both types of features shape the appearance and topography of the shoreline. Erosional features, like sea cliffs, tend to be more abrupt and steep, while depositional features, such as beaches and sandbars, are typically more gradual in slope and build up over time.