Fan splay
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Fan splay
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A crevasse splay is a sedimentary fluvial deposit which forms when a stream breaks its natural or artificial levees and deposits sediment on a floodplain. A breach that forms a crevasse splay deposits sediments in similar pattern to an alluvial fan deposit. Once the levee has been breached the water flows out of its channel. As the water spreads onto the flood plain sediments will start to fall o… WebFansly - @PrismSplay Follow Prism @PrismSplay 1.9K Likes 5.9K Followers 22 Photos 27 Videos Glitter-bender, roller-skating, kinkromancer, Unicorn Goddess. Real handful. Horny Tip Jar! Horny Tip Jar! 1 month 5 Holes Holes 1 month 10 Additional Plans Hornies Hornies 1 month 20 Additional Plans Rainboners Rainboners 1 month 35 Additional Plans
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WebAug 1, 2024 · Our data integrate with regional structural information of the Tanlu fault zone; we suggested that the Tanlu fault zone has an eastwards-fan splay pattern geometric feature in its northern part. Accordingly, we further restore the ancient tectonic configuration of eastern Asia before the Tanlu fault zone initiation. WebCrevasse splays: If a stream avulses out of its channel by breaking its levee, the main flow of a stream can be diverted out of the channel and into the adjacent flood plain. As it does, the flow will expand and slow, dropping its load, as in a normal flood, but in this case, much more (and coarser) sediment will be transported to the flood plain.
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