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Q97 (CAPF/2019) Geography › World Physical Geography › Weathering and erosion Answer Verified

The gently sloping accumulation of coarse alluvium deposits by a braided stream is known as

Result
Your answer: —  Â·  Correct: B
Explanation

The correct answer is Option B: alluvial fan.

In geomorphology, an alluvial fan is a cone-shaped or fan-shaped deposit of sediment formed where a stream leaves a mountain range and flows into a flatter plain. This change in gradient causes the stream to lose energy and deposit its load.

  • Key Characteristics: The deposits typically consist of coarse alluvium (sand and gravel). The landform is described as a gently sloping accumulation.
  • Association with Braided Streams: The streams flowing across alluvial fans are almost always braided (consisting of multiple interconnecting channels) due to the high sediment supply and variable discharge.

Why other options are incorrect:

  • Sand bar (Option A): A sand bar (or braid bar) is a temporary ridge of sediment within a river channel. While braided streams contain sand bars, the term "gently sloping accumulation" refers to the broader landform (the fan) created by the stream, not the bars inside it.
  • Bajada (Option C): A bajada is a continuous apron of sediment formed by the merging of multiple adjacent alluvial fans.
  • Diaras (Option D): This is a regional term used in India for flood-prone islands or land located between river channels.
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