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Pierce, W.G., 1997, Geologic map of the Cody 1 degree x 2 degrees quadrangle, northwestern
Wyoming: U.S. Geological Survey, Miscellaneous Geologic Investigations Map I-2500, scale 1:250000.
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in the basin are mostly exposed and relatively easy to identify, Elk Basin has long been used as a place for geology students to learn to practice
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94:. Often mapping classes are supported by the Yellowstone Bighorn Research Association, located in
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View of Elk Basin facing north along the axis of the anticline. Note strata
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with hundreds of derricks operating in it. Geologically, it is a breached
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27:to the right and left on the sides of the image.
124:Yellowstone Bighorn Research Association
54:. Most of the rocks at the surface are
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42:in the United States. It is an active
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174:Landforms of Carbon County, Montana
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50:formed by a deep subsurface thrust
16:Oil field in Wyoming, United States
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184:Landforms of Park County, Wyoming
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34:is a valley on the border of
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150:44.99722°N 108.86944°W
58:in age, including the
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194:Oil fields in Wyoming
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179:Landforms of Montana
155:44.99722; -108.86944
146: /
68:Mesaverde Formation
64:Meeteetse Formation
189:Valleys of Wyoming
96:Red Lodge, Montana
76:Frontier Formation
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92:geologic mapping
82:Teaching Geology
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60:Lance Formation
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86:As the rock
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141:108°52′10″W
168:Categories
138:44°59′50″N
102:References
72:Cody Shale
56:Cretaceous
48:anticline
44:oil field
32:Elk Basin
40:Wyoming
36:Montana
25:dipping
88:strata
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52:fault
38:and
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