A meander. <-------NovaNet
wrong your answer miss or mister novanet
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The absolutely best answer is "a delta " cause a delta is a n accumulation of sediment formed where a stream enters a lake or ocean....:-)hismejohn
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.
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.
A depositional mountain is a landform created by the accumulation of sedimentary material, such as sand, gravel, or rock fragments. It forms when these materials are deposited over time, often by processes like erosion or the movement of glaciers, rivers, or wind. As the sediment builds up, it can eventually form a mountainous feature.
We call this a delta since it is somewhat shaped liked a D or triangle.
Cross-bedding refers to inclined layers in sedimentary rock that were formed as a result of wind or water driven ripples or dunes in the original depositional environment.
No. A delta forms when a stream enters a standing body of water, usually the ocean. Those conditions do not exist on Mount St Helens.
A point bar is a depositional feature found on the inside bend of a meandering river, characterized by coarser sediment accumulation due to decreased water velocity. In contrast, a channel bar forms in the middle of a river channel and is composed of sediment deposited within the active channel due to changes in flow velocity or sediment supply.
A characteristic is a feature that has different forms in a population
water
A good example would be the ones in Death Valley, California. An alluvial fan is basically a fan-like structure formed from the mouth of a flattened and spread out stream (it looks like a fan).
It is dissolved (-;
It is dissolved (-;