Road Blog: Hole in the Ground

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A short post, since I’ve let it get so late: The next-to-last place we visited on our five-day Ice Age Floods Greatest Hits Tour was Hole in the Ground Coulee, just south of Cheney, the home of Eastern Washington University. Apparently, the area is called “Hole in the Ground” because of a 100-foot deep hole on the floor of the canyon here (one of Randy’s guidebooks says concerned locals filled it with rocks so no one would fall in).

The last stop we made, deep into the dusk, was at the site of a dry cataract not far from the site above, one of the many waterfalls that spilled flood waters south and east toward the Columbia basin when the Lake Missoula ice dams gave way far upstream.

Of course, touring the landscape created by the Big, Big Floods of Yesteryear was just part of what’s been happening the last five days. Randy and I were close during our teenage years — my shorthand for him is “my best friend from high school” — and we spent a lot of the time not filled with talk of lava flows, basalt configurations, receding cataracts, loess and loess islands, mesas, spires, potholes, craters, mima mounds, blades, benches, coulees, and the like reminiscing and catching each other up with what’s been happening in our lives.

It’s been a great five days. More pictures to come.

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