Eastern Mojave Vegetation | Utah Highway 261, San Juan County, Utah |
Edited by Tom Schweich |
The Moqui Dugway ia a steep, partially paved road (UT RT 261) with a series of tight switchbacks that climbs up and over Cedar Mesa north of Mexican Hat, UT. There are panoramic views of the Valley of the Gods and the canyons of the San Juan River at various pullouts along the road. The road is cut into the Halgaito Formation (first switchback at the base of the mesa) and Cedar Mesa Sandstones of the Permian Cutler Group. Large-scale cross stratification and reddish interdune deposits, including permineralized roots in the Cedar Mesa Sandstone can be examined at several of the pullouts. The Raplee anticline, a smaller, en echelon fold in the eastern limb of the Monument Upwarp is also visible to the south along the San Juan River. | ||
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Junction: Utah Highway 95 | |
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Moki Dugway.
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Pullout at a switchback about 2/3 of the way to the top. | |
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Locations: Moki Dugway. |
Moki DugwayNear this location are paleosol collection sites in the Permian Halgaito Shale and Cedar Mesa formation used by Retallack in his 2009 study of greenhouse crises of the past 300 million years. Retallack used stomatal index data for fossil Ginko and related leaves as a proxy for past CO2 spikes and paleosol chemical data as proxies for temperature and humidity changes. These data show that global warming due to CO2 rise is a not a unique event in earth history and that the magnitude of the coming anthropogenic greenhouse pales in comparison with past greenhouse spikes at times of global mass extinctions. | |
Junction: Valley of the Gods Road | ||
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View of Cedar Mesa and Moki Dugway. | |
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Junction: US Highway 163 | |
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Date and time this article was prepared: 12/9/2024 7:38:02 PM |