Steven Dutch, Professor Emeritus, Natural and Applied Sciences, Universityof Wisconsin - Green Bay
There's a surprising amount of nice scenery in Nebraska once you get off theInterstate. The Scotts Bluff area is interesting geologically and historically.
Chimney rock was a prominent landmark for travelers on the Oregon Trail. A visitor center tells the history of the rock. | |
The rock is made of relatively soft sandstone and has eroded noticeably since it was first described. In another thousand years it will almost certainly be gone. | |
The rock is an outlier of a much more extensive series of bluffs. Pioneers used to climb the rock and carve their names in it but access now is not permitted. | |
Close up of the bluffs near Chimney rock. |
Scotts Bluff was also a prominent landmark on the Oregon Trail and is preserved as a national monument. | |
Scotts Bluff | |
The Visitor Center | |
Scotts Bluff. The Oligocene White River Group is overlain by the Miocene Arikaree Group. | |
A short drive from the Visitor center leads behind Scotts Bluff through several tunnels to an overlook. As the picture shows, weather conditions were not optimal at the overlook. | |
Sediments of the Arikaree Group | |
Although the rocks are primarily sandstone, they have a calcareous component as shown by the weathering | |
Chert lenses and nodules are also present. | |
View of Scotts Bluff from the west | |
View of Scotts Bluff from immediately southwest. | |
Left and below: Scotts Bluff is only one of a large number of bluffs carved into outliers of the Tertiary rocks. | |
Looking east from Scotts Bluff along the Platte River Valley. |
The rock units that form Scotts Bluff also form a long ridge to the south called the Wildcat hills | |
Looking north from the Wildcat hillsalong Nebraska Route 71. | |
Looking east along the south flank of the Wildcat hills |
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Created 14 July 2003, Last Update 09 June 2020