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Lake C. W. McConaughy

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Journal Article
Published: 01 January 2004
Environmental & Engineering Geoscience (2004) 10 (1): 69–90.
...R. M. JOECKEL; R. F. DIFFENDAL, JR. Abstract Lake C. W. McConaughy, a 63-year-old manmade reservoir in the North Platte Valley of western Nebraska, is the largest standing body of water in the state. From the time that Kingsley Dam was completed in 1941 until the present day (2004), many geomorphic...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2005
GSA Bulletin (2005) 117 (3-4): 436–449.
... for this study because they exhibit a well-developed, well-preserved joint surface morphology ( Sheldon, 1912 ; Parker, 1942 ; Engelder and Geiser, 1980 ). The best examples are found within the Ithaca Formation (Genesee Group) in the Finger Lakes District of New York ( McConaughy and Engelder, 2001...
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Journal Article
Journal: Paleobiology
Published: 26 July 2018
Paleobiology (2018) 44 (3): 546–559.
... . Holocene paleoenvironments in southeastern Minnesota—chasing the prairie-forest ecotone . Palaeogeography, Palaeoclimatology, Palaeoecology 177 : 103 – 122 . Behrensmeyer , A. K. , R. W. Hook , C. E. Badgley , J. A. Boy , R. E. Chapman , P. Dodson , R. A. Gastaldo...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 2009
AAPG Bulletin (2009) 93 (7): 857–889.
... – 502 . Holzhausen , G. R. , 1989 , Origin of sheet structures: 1. Morphology and boundary conditions : Engineering Geology , v.  27 , p.  225 – 278 , doi: 10.1016/0013-7952(89)90035-5 . Hopkins , CW. , R. L. Rosen , and D. G. Hill , 1998 , Characterization...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 2005
AAPG Bulletin (2005) 89 (11): 1433–1449.
... lenses in the lower Palaeozoic sedimentary rocks in northern Estonia : Oil Shale , v. 11 , p. 100 . Krushin , J. T. , 1997 , Seal capacity of non-smectite shale , in R. C. Surdam , ed., Seals, traps, and the petroleum system: AAPG Memoir 67 , p. 31 – 67 . Lambe , T. W...
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Journal Article
Journal: AAPG Bulletin
Published: 15 April 2021
AAPG Bulletin (2021) 105 (4): 669–694.
.... , 1996 , Petroleum geochemistry and geology , 2nd ed. : New York , W. H. Freeman and Company , 743 p . Hunter , C. D. , and D. M. Young , 1953 , Relationship of natural gas occurrence and production in eastern Kentucky (Big Sandy gas field) to joints and fractures in Devonian...
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Journal Article
Published: 01 January 2005
Journal of Paleontology (2005) 79 (1): 185–199.
.... Soderstrom , K. W. Hilu , C. S. Campbell , and M. E. Barkworth (eds.), Grass Systematics and Evolution . Smithsonian Institution Press , Washington, D.C . Beauvois , P. de . 1812 . Essai Agrostographie . Paris , 495 p. Berry , E. W. 1928a . Fossil nutlets...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 2014
AAPG Bulletin (2014) 98 (1): 67–117.
..., Lake Bonney-1, Caroline-1, Burrungle-1, Viewbank-1, Hungerford-1, Kalangadoo-1, Troas-1ST1, Geltwood Beach-1, and Chama-1a. The solid lines correspond to the physically constrained normal compaction trends (NCTs) (i.e., Δ t 0 ≈ 196 μs ft –1 and C = 56 μs ft –1 ), whereas the dashed lines...
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Series: Geological Society, London, Special Publications
Published: 01 January 2004
DOI: 10.1144/GSL.SP.2004.231.01.09
EISBN: 9781862394797
... to Alleghanian folds. Note ENE and E-W joints remain consistent in orientation across the Finger Lakes District. Fig. 2. Generalized Upper Devonian stratigraphie columns of the Lake Erie and Finger Lakes districts. Our work was stimulated by industry reports from both the Appalachian (e.g. Kubik...
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Series: Geological Society, London, Special Publications
Published: 17 July 2020
DOI: 10.1144/SP496-2019-7
EISBN: 9781786205315
... (shear). Failure angle for a tensile failure surface with respect to the maximum principal compressive stress ( σ 1 ) is approximately 0° ( Fig. 1 ). In many cases tensile fractures display plumose markings and other fractographic features (e.g. Bahat & Engelder 1984 ; Hancock 1985 ; McConaughy...
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Series: GSA Field Guide
Published: 01 January 2011
DOI: 10.1130/2011.0020(02)
EISBN: 9780813756202
... ( McConaughy and Engelder, 1999 ). In general, the surfaces are not as planar as seen in outcrops of black shale in the Finger Lakes District, New York. Like the J 1 joints in the Snook quarry at Antis Fort, these joints form normal to bedding. When bedding is rotated to horizontal, the J 1 joints return...
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Series: Geological Society, London, Special Publications
Published: 01 January 2004
DOI: 10.1144/GSL.SP.2004.231.01.17
EISBN: 9781862394797
... and concretions (e.g. McConaughy & Engelder 1999 ), this black shale was devoid of internal structures at the time of joint propagation. We examine orientation data collected by Hägen (1997) from this ENE joint set within the Finger Lakes District of New York State. A scardine, placed on the pavement...
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