Monthly Archives: October 2013

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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Road Blog: Palouse

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Columbia River at Wallula Gap, shot from Twin Sisters.

Tuesday, Randy and I started out in Kennewick, Washington, made our way to the Columbia River, then south to a landmark called Twin Sisters — a sort of double volcanic spire on the east bank of the river (and in native stories, what’s left of sisters who were thwarted in their salmon fishing then turned to stone by Coyote). Part of the attraction of the Twin Sisters is what you see from there: the Wallula Gap, where the Columbia flows through an opening eroded through the Horse Heaven Hills then enlarged by the Big Floods.

From there we made our way over to the Snake River country, the town of Kahlotus and Devil’s Canyon, yet another landscape wrought by the ice age floods. We stopped in the town of Washtucna for a hot dog and a double cappuccino, then headed to Palouse Falls.

The Palouse is an extensive area of steeply rolling hills, mostly treeless, much of it planted in wheat, made up mostly of ancient wind-blown soil (or loess, pronounced “less” in approximation of its German origin) that’s as much as 200 feet deep. (That’s a shot of a recently plowed field below, looking south toward the Snake River.)

Palouse Falls is another one of those places that recounts a chapter of the flood epoch. The Palouse River flows through gorges excavated by the ice age floods and falls into a “plunge pool” dug out by the gigantic volume of water that came rushing through 15,000 years ago or so.

From the falls, we cruised back through Clarkston, Washington, and Lewiston, Idaho, to Randy’s house in the town of Orofino, population 3,000 and some, seat of Clearwater County. More geoimagery tomorrow.

Conclusion of the foregoing.

Road Blog: Palouse

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Road Blog: Potholes

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Potholes, as in Potholes Coulee, part of the recently mentioned channeled scablands of eastern Washington. This was today’s main event, hiking up the one branch of the coulee — which I’ll describe as a valley about a little more than a mile and a half from west to east, surrounded on both the north and south by 300 foot rock walls. I’ll call it a valley, but it was actually an outlet for the big ice age floods that roared from northwestern Montana into the Columbia River basin.

The picture above (click for a larger version) is the north wall of this part of the coulee, which had waterfalls every few hundred yards. The wall consists of multiple layers of basalt from lava flows that occurred over a span of millions of years. That columnar structure high atop the wall (it is actually called a colonnade) and signifies the lower layer of a flow and one that cooled slowly compared to the irregularly fractured section above (called entablature). The lighter rock below is basalt from an earlier flow that spent some time underwater when a lake filled part of this valley.

At least that’s what I’ve absorbed over the last few days. And here’s a more scientifically grounded partial explanation, if you’re interested.

Me? I’m done. More later.

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Road Blog: Extreme Geology

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That’s Washington state Highway 155, headed north from Coulee City toward Grand Coulee Dam. We got a gray, cool to cold day with a little autumn rain thrown in. The landscape is huge and surprising. To the right in this picture are basalt cliffs formed from successive lave flows over millions of years and then violently gouged out by the repeated great floods that poured through this region during the ice age. I heard an estimate somewhere today that about 520 cubic miles of water — cubic miles — came pouring across this part of eastern Washington in 48 hours. That’s a little less than the volume of Lake Michigan, which counts as a big lake in my book, discharged over a weekend. In the left of this picture in Banks Lake, a big reservoir created as part of the Bureau of Reclamation’s massive World War II era plumbing of this area. The huge mesa-like shape in the left distance is Steamboat Rock, once an island at the foot of an immense waterfall upstream. (Click the picture above for a larger image.)

Started: Moses Lake, Washington (7:15 a.m.)
McDonald’s breakfast to go
North on Washington 17 through Soap Lake
Stopped at Lenore Lake
Hiked up through canyon to Lenore Coulee and Great Blade
North on Washington 17 to Dry Falls State Park
Hiked up through notch in Umatilla Rock
Stopped at visitors center
Stopped in Coulee City; lunch at Last Stand restaurant and saloon
North on Washington 155 to Grand Coulee Dam
Stopped at Crown Point, overlooking dam and town, hiked to Candy Point
Stopped at dam visitors center
West on Washington 174 to Washington 17
South on Washington 17 to Washington 172
West of Washington 172 to U.S. 2
U.S. 2 to Wenatchee, Washington
Arrived: 7:30 p.m.

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Road Blog: Scablands

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The scablands–that’s what they call big pieces of eastern Washington, where I spent the day with one of my oldest friends, Randy Robinson. Roughly speaking, the scablands are the extensive rocky breaks in the rolling countryside in this part of the state. Mesas, tiered benches of basalt from ancient lava flows, gravel ridges, craters, the random distribution of huge boulders across the landscape. They’ve come to be known as the channeled scablands because of a reinterpretation of the regional geology in the 1920s that proposed that a flood of unimaginable proportions — set loose by the collapse of a colossal ice dam in western Montana, which in turn led to the sudden outflow of a huge mountain lake — scoured and sculpted the land maybe 15,000 years ago.

Anyway, that’s a summary of what Randy told me today, and we’ve got two or three or four more days of scabland hiking and sight-seeing ahead. (Where did the term scablands come from? I’m running it down — I find several references in the 1880s that apply that term to this part of Washington; I also found one possible reference from 1630s Britain that may indicate there’s an older and more general meaning of the term.

The picture above: One of our stops, a spot called Twin Lakes, west of Spokane. The challenge with this countryside is capturing something so big in any sort of meaningful way. Anyway

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Scorebook: Oakland 1, Detroit 0

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In just 10 hours or so, the A’s and Tigers will be back on the field, this time in Detroit, to continue their playoff series. It hardly seems possible, because Saturday night’s game in Oakland, the game the A’s won 1-0 in the bottom of the ninth, barely seems over. The epic tension of the game, the pitching, the crazy enthusiasm of the crowd (yeah, the Coliseum looks great with those third-deck tarps taken off and all those seats filled with fans), and the A’s finally breaking through to get a run home. Anyway, that’s all I’m going to say on the matter for now. Here’s Kate’s scorecard for Game 2–Tigers up above, A’s below (click the pages for bigger images).

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