Smaller floods have more variations in channel size, quantity, and topography. It also created more meandering/braided streams. The big floods had fewer variations and focus more on the main channel wiping out most of the topography. We saw overbank flows and that contributed to new channel developments through avulsions or chute dissection. Bankfull flows were also present when there was higher discharges. Through flows contributed to the base flow of many river channels we created. Hyporehic flows made the biggest difference in the beginning because the flume wasn't fully saturated but after that, It helped with through flow and creating new channels. A role that the recession limb flow played was that when discharge decreased It created more distinct channels and braided more than before.