Devil's Slide in Weber canyon near Croydon, Utah. Devil's slide is a created by layers of more resistant limestone that stick up above the surrounding rocks. The bed of rock are almost vertical and run up the mountain.
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Toward the top of Devil's slide the rocks are offset slight by a fault. The rocks on the lower part are offset to the left in relation to rock higher up the hill. As a kid I always wanted to take an intertube and slide down it in the winter. What can't be seen is the Weber river that is right behind the trucks. A person would have a suprise to end up in the river on a cold snowy day.
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