Rapids
Basaltic columns formed during cooling of a basaltic lava flow lie along the bank of the Fall River near Chester, Idaho. The rapids are caused by a restriction formed as the river cut through the basalt flow. This photo was taken near the bridge where US 20 crosses the river.
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Uploaded on October 13, 2019
Taken on August 18, 2019
Rapids
Basaltic columns formed during cooling of a basaltic lava flow lie along the bank of the Fall River near Chester, Idaho. The rapids are caused by a restriction formed as the river cut through the basalt flow. This photo was taken near the bridge where US 20 crosses the river.
1,331
views
41
faves
0
comments
Uploaded on October 13, 2019
Taken on August 18, 2019