James Montgomery
On
the last day of our exploration into the Grand Staircase Escalante National
Monument we ventured into a Hackberry Canyon, exploring millions of years of rock
formations. While walking in and around the small creek that ran through the
middle of canyon we noticed ripples in the water. Upon closer inspection we
could see the soft sand ripples at the bottom of the stream migrating slowly forward with the current. Ripples begin to form through when the water disrupts the grains of the sand on the bottom of the body of
water. The steeper, down current side of the ripple is always at the angle of repose.
What a great example of uniformitariansim. We could see modern ripples forming in a stream bed next to ripples formed in the Jurassic almost 200 million years ago.
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