Comb Ridge
It was designated a National Natural Landmark in 1976 as the only North American location of tritylodont fossils. Parts of the ridge in Utah are protected as part of the Bears Ears National Monument.
Geology
The geologic formations involved in the east dipping strata of the fold include the Jurassic aged Navajo Sandstone, Kayenta Formation, Wingate Sandstone, Chinle Formation, Triassic Moenkopi Formation and Permian Organ Rock Formation. The structure is the surface expression of a deep fault along the east margin of the Monument Uplift.
History
Traces of the Ancestral Puebloan culture can be found along the southern part of the ridge where it follows Chinle Wash. The Macomb and Hayden expeditions in 1869 and 1874–1876, respectively, were the first to publish maps and descriptions of this feature. The ridge and adjacent Butler Wash were given their current names in 1884, by P. Holmann.
Numerous cliff dwellings are found along the ridge.
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Monarch Cave Ruin cliff dwelling on Comb Ridge
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Monarch Cave Ruin cliff dwelling on Comb Ridge
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House on Fire Ruin near Comb Ridge
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Procession Panel petroglyph
![](http://upload.wikimedia.org/wikipedia/commons/thumb/e/eb/WolfmanPanelUtah-AttributeAs-PhilKonstantin.jpg/389px-WolfmanPanelUtah-AttributeAs-PhilKonstantin.jpg)
![](http://upload.wikimedia.org/wikipedia/commons/thumb/0/0e/Comb_Ridge_from_US_163.jpg/464px-Comb_Ridge_from_US_163.jpg)