Port Kelley WA (#0373)
Pasco WA BNSF Burbank bridge (#0381)
Pasco WA Snake river (#0383)
Pasco Kennewick Cable bridge (#0389)
Pasco WA BNSF Burbank bridge (#0376)
Pasco Kennewick Cable bridge (#0395)
Pasco WA BNSF Kennewick bridge (#0393)
Kennewick dusk (#0509)
Kennewick dusk (#0397)
Kennewick (#0404)
Portland Linnton rail (#0499)
Portland Linnton rail (#0501)
Sauvie Island (#0503)
Sauvie Island (#0504)
Sauvie Island floating homes (#0508)
St Helens basalt courthouse (#0509)
St Helens basalt city hall (#0511)
Rainier OR / Longview WA seaport (#0512)
Rainier OR / Longview WA seaport (#0515)
Rainier OR / Longview WA seaport (#0517)
Rainier OR / Longview WA seaport (#0518)
Longview WA Lewis and Clark bridge (#0520)
LA "Pope of Broadway" mural (#0637)
Port Kelley WA (#0370)
Port Kelley WA (#0368)
Port Kelley WA (#0372)
Port Kelley WA (#0364)
McNary Dam WA (#0409)
McNary Dam WA (#0406)
Plymouth WA (#0411)
Plymouth WA (#0410)
Umatilla Bridge (#0359)
Umatilla Bridge (#0356)
John Day Columbia Aluminum (#0426)
John Day Columbia Aluminum (#0419)
John Day dam (#0425)
John Day lava field (#0423)
Columbia Gorge rail line (#0416)
Columbia Gorge barge (#0353)
John Day dam fish ladder (#0350)
John Day dam (#0349)
John Day dam avian predation (#0346)
John Day dam avian predation (#0347)
John Day dam smolt chute (#0344)
John Day dam (#0351)
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www.ipernity.com/doc/289859/33009659/in/album/438843
We geologists will say it's an erosional feature, due to the Scabland floods, from a single thick basalt flow. The blocky, somewhat lighter part below is in the lower part of the flow, which cooled more slowly, while the more spindly buttes above are basalt that cooled from the surface and thus more quickly. The cooling fronts met in the middle of the flow, so that what looks like two flows is in fact a single flow with very different textures from the different cooling histories.
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