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Photographer’s Note

This is a very different image given the unusual mix of colors in one pallete, but I am hoping you will appreciate it once you read abit about it. We visited the Palouse Prairie region of eastern Washington this week and viewed the amazing landscape from Steptoe Butte on two successive days.

The peculiar and picturesque silt dunes which characterize the Palouse Prairie were formed during the ice ages. Blown in from the glacial outwash plains to the west and south, the Palouse hills consist of more or less random humps and hollows. The steepest slopes, which may reach 50% slope, face the northeast. The highly productive soil ranges from 5 to 130 cm deep. Large areas of level land are rare.

Steptoe Butte itself is a quartzite island jutting out of the silty loess of the Palouse hills. The rock that forms the butte is over 400 million years old. Steptoe Butte is currently recognized as a National Natural Landmark because of its unique geological value. It is named in honor of Colonel Edward Steptoe. Elevation: 3,612 feet (1,101 m), approximately 1,000 feet (300 m) above the surrounding countryside.

Both my wife and I have prairie / farming roots so scenes like this brought back many fond memories and was an enriching experience for us. I only wished I could have pressed a little button somewhere and scrolled these views through the four seasons of the year! Needless to say, in Palouse Wheat Is King! Enjoy.

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Additional Photos by Gerald Neufeld (gneufeld) Gold Star Critiquer/Gold Star Workshop Editor/Gold Note Writer [C: 1668 W: 102 N: 3572] (15519)
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