The Hydrology of Tree-Like Figures on the Desert
I came across this aerial photo by National Geographic and was compelled to post on the hydrology of how such a stunning river would develop. Dendritic drainage structures originate from sheet flow – downslope movement of water as a thin sheet – which converges or diverges on an uneven surface. Where convergence occurs the water develops more power (mass x velocity), which mobilizes sediments. This erosion deepens the channels, concentrating even more water and new rills develop as water flows into the deepening rill. The watershed boundary seen between the main branches of this stream will eventually close in to … Read More