This sector of the Green River canyon in eastern Utah is known as Bowknot Bend because of the way the river doubles back on itself. The loop carries river rafters 14.5 kilometers (9 miles) before bringing them back to nearly the same point they started from—though on the other side of a low, narrow saddle.
The reason for the tight bends in the Green River is the same as it is for the Mississippi: River courses often wind over time when they flow across a bed of relatively soft sediment in a floodplain. Geologists assume the Green River, before its present canyon phase, once snaked across a wide valley on a bed of its own sediment and made a series of striking meander bends.
Vertical uplift of the entire landscape—by deep-seated tectonic forces related to the growth of the Rocky Mountains—caused the Green River to erode downward into the hard rocks under the valley. In the process, the present vertical-sided canyon was formed, preserving the tight loops reminiscent of an earlier time.
Bowknot was named by geologist John Wesley Powell in 1869 during one of his famous explorations of the rivers in the American West. The Green River flows south (toward the top of this image) and joins the Colorado River downstream. The combined flow of these rivers was responsible for cutting the Grand Canyon, some 325 kilometers (200 miles) away from Bowknot.
Image courtesy of NASA.