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Floodplains are intermittently flooded complex geomorphic features with positive and negative relief (Lewin & Ashworth, 2014). Negative relief consists of meso-and macro-scale elements that include accessory through-channels, tributary channels, channel margin slackwater zones, bar-shelter backwaters, contiguous channel remnants, tie channels, internal drainage channel networks, and large-scale flood basins occluded by channel-belt aggradation (Lewin & Ashworth, 2014). This negative relief is present on both braided (

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