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Painting Courtesy of Monte Dolack May of 1805 . . .
When Dinosaurs Wandered the Area . . . Same Layer, Different Location . . . When the coast was located farther to the west, the sea would have been somewhat deeper here. As a result of this deeper environment, this would have been a time when smaller particles such as silts, and clays were deposited here. Those materials make up the layer known as the Marias River Shale shown in the photo of the Eagle Creek area below as well as on the painting. ![]() Mountain Building (and the subsequent erosion) to the west of here provided an abundant source for the sands, silts, and clays deposited in this part of central Montana. The rock layers seen along the river tilt gently to the east, so as travelers move downriver (eastward), they see increasingly younger rock layers along the river. Source: The book entitled "Montana’s Wild and Scenic Upper Missouri River" by Glenn Monahan and Chanler Biggs. Term: fluctuating |
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*More about the geology of the White Cliffs |
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More about the book |
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Next picture of the week |
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Earth Science Teacher at Helena High School |