Publication: [1608] Petrology and depositional environments of the Fountain and Ingleside Formations, Owl Canyon, Colorado

Documented Paleocurrents

Total Items: 5

#		Continental Area	Stratigraphic Level	Total Records	Period	Latitude	Longitude	Tectonic Plate	Deposition Environment	Paleocurrent Type	Lithology	Formation
1	Data RefID #20182 [Rec № 1608] Petrology and depositional environments of the Fountain and Ingleside Formations, Owl Canyon, Colorado Fredrickson, J. A. Masters thesis, University of Wyoming, 1979, « Missing Vol »	North American	Upper Carboniferous (Pennsylvanian)	5	26832	40.75	-105.33	North American	Subaerial (Eolian)	Crossbedding	Sandstone
2	Data RefID #20183 [Rec № 1608] Petrology and depositional environments of the Fountain and Ingleside Formations, Owl Canyon, Colorado Fredrickson, J. A. Masters thesis, University of Wyoming, 1979, « Missing Vol »	North American	Upper Carboniferous (Pennsylvanian)	5	26832	40.73	-105.27	North American	Subaerial (Eolian)	Crossbedding	Sandstone
3	Data RefID #20184 [Rec № 1608] Petrology and depositional environments of the Fountain and Ingleside Formations, Owl Canyon, Colorado Fredrickson, J. A. Masters thesis, University of Wyoming, 1979, « Missing Vol »	North American	Upper Carboniferous (Pennsylvanian)	5	26832	40.72	-105.31	North American	Subaerial (Eolian)	Crossbedding	Sandstone
4	Data RefID #20185 [Rec № 1608] Petrology and depositional environments of the Fountain and Ingleside Formations, Owl Canyon, Colorado Fredrickson, J. A. Masters thesis, University of Wyoming, 1979, « Missing Vol »	North American	Upper Carboniferous (Pennsylvanian)	5	26832	40.74	-105.25	North American	Subaerial (Eolian)	Crossbedding	Sandstone
5	Data RefID #20186 [Rec № 1608] Petrology and depositional environments of the Fountain and Ingleside Formations, Owl Canyon, Colorado Fredrickson, J. A. Masters thesis, University of Wyoming, 1979, « Missing Vol »	North American	Upper Carboniferous (Pennsylvanian)	5	26832	40.7	-105.29	North American	Subaerial (Eolian)	Crossbedding	Sandstone