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Why is "Avulsion (river)" trending?

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Trend Analysis

  • Ranking position: #
  • Date: 2026-03-13 10:36:22

This topic has appeared in the trending rankings 1 time(s) in the past year. While it does not trend frequently, its appearance suggests a renewed or concentrated surge of public interest.

Based on Wikipedia pageviews and search interest, this topic gained significant attention on the selected date.

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Avulsion (river)

Wikipedia Overview

In sedimentary geology and fluvial geomorphology, avulsion is the process by which flow is diverted out of an established river channel and into a new course via a bifurcation, or splitting of the channel. Avulsions range from full, in which all flow is diverted from a one channel to another, to partial, in which only a portion of flow is diverted. Avulsions were once thought to occur as a result of channel slopes that are much less steep than the slope that the river could travel if it took a new course, but it is now recognized that many factors, including upstream channel planform, channel cross-sectional geometry at a bifurcation, and channel obstructions such as wood or beaver dams can also influence the rate and progression of avulsions.

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Why This Topic Is Trending

This topic has recently gained attention due to increased public interest. Search activity and Wikipedia pageviews suggest growing global engagement.


Search Interest & Related Topics

Search interest data over the past 12 months indicates that this topic periodically attracts global attention. Sudden spikes often correlate with major news events, public statements, or geopolitical developments.

Search Interest (Past 12 Months)

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