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Uniontown Fault

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Formation and evolution of the <span class="search-highlight">Uniontown</span> <span class="search-highlight">fault</span> scarp. (a) Floodplain constr...
Published: 23 February 2021
Figure 9. Formation and evolution of the Uniontown fault scarp. (a) Floodplain construction and formation of alfisol surface soil until ∼ 3.5    ka ; (b) at ∼ 3.5    ka alluvium and overlying soil are folded due to subsurface faulting; (c) unit B is eroded by hillslope processes
Journal Article
Published: 23 February 2021
Bulletin of the Seismological Society of America (2021) 111 (2): 1154–1179.
...Figure 9. Formation and evolution of the Uniontown fault scarp. (a) Floodplain construction and formation of alfisol surface soil until ∼ 3.5    ka ; (b) at ∼ 3.5    ka alluvium and overlying soil are folded due to subsurface faulting; (c) unit B is eroded by hillslope processes...
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Longitudinal profiles of the Ohio River floodplain and terraces from Owensb...
Published: 23 February 2021
Figure 3. Longitudinal profiles of the Ohio River floodplain and terraces from Owensboro, Kentucky to Brookport, Illinois (city locations shown in Fig.  1 ). The upper floodplain surface is arched near Mt. Vernon, Indiana, which is directly north of the Uniontown fault (modified from Alexander
Image
(a) Google Earth image showing previously mapped bedrock <span class="search-highlight">faults</span> (solid line...
Published: 23 February 2021
Figure 13. (a) Google Earth image showing previously mapped bedrock faults (solid lines) and the new Uniontown faults identified in this research (dashed lines). White dots and gray lines are petroleum wells and cross sections shown in Figure  8 . (b) Line figure of a scaled sand‐box model
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(a) Distribution of large paleoliquefaction features within 50 km of the Un...
Published: 23 February 2021
Figure 12. (a) Distribution of large paleoliquefaction features within 50 km of the Uniontown fault. The size of the gray circle represents the scale of the paleoliquefaction feature; (b) a 0.4‐meter‐wide unweathered sill crosscutting a weathered clastic dike, near the confluence of the Black
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Deep cross sections across the floodplain scarp constructed with data from ...
Published: 23 February 2021
River channel due to over 30 m of erosion since 1965. Cross section C–C′ indicates there is another fault east of the Uniontown scarp, which is consistent with seismic profile S2. Profile F–F′ is south of the Uniontown scarp. Profile G–G′ is part of the cross section from the Uniontown and Wabash Island
Journal Article
Published: 10 October 2018
Seismological Research Letters (2018) 89 (6): 2473–2480.
..., Rutledge (2004) , Woolery (2005) , and more recently Counts et al. (2008) discovered Quaternary active deformation above other primary structures in the WVFS (e.g., Hovey Lake and Uniontown faults), suggesting that a higher resolution spatial and temporal understanding of the regional neotectonics...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1948
AAPG Bulletin (1948) 32 (2): 304.
...Donald G. Sutton The Uniontown pool in northern Union County, Kentucky, discovered in September, 1942, produces mainly from the Waltersburg, Tar Springs, and Cypress sandstones of the Chester series, Upper Mississippian system. It produces in a minor way from a sandstone of Pennsylvanian age...
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Seismic‐reflection profiles across the <span class="search-highlight">Uniontown</span> scarp (profile locations s...
Published: 23 February 2021
Figure 6. Seismic‐reflection profiles across the Uniontown scarp (profile locations shown in Fig.  4 ). Horizontal distance is in meters. All profiles show down‐to‐the‐west displacement of the bedrock surface beneath the scarp. Black lines are the bedrock surface; the black arrow at the top
Image
(a) The Wabash Valley <span class="search-highlight">fault</span> system (WVFS) and surrounding features. Thin, s...
Published: 23 February 2021
Figure 1. (a) The Wabash Valley fault system (WVFS) and surrounding features. Thin, solid lines are mapped bedrock faults, and the dashed ellipse is the approximate extent of the WVFS. The RCFZ and FAFC are the Rough Creek fault zone and the Fluorspar Area fault complex, respectively. Thick
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1929
AAPG Bulletin (1929) 13 (10): 1301–1315.
... below Uniontown, Kentucky, at the Middle and Lower Highlands Reefs. It extends farther southwest, rising more than 100 feet to Grundy Knob on the south. 1 Farther north, the West Franklin formation, which is well developed in the high river bluff at Merom, Indiana, is exposed a short distance...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 April 2002
AAPG Bulletin (2002) 86 (4): 653–670.
... by imbricated Devonian Tully-Helderberg rocks thrust inward toward a depressed axial low. New data from wells at North Summit show that the core of the Chestnut Ridge anticline is not filled with imbricated reservoir rocks but that the reservoir is deformed into a series of faulted folds. Gas was trapped...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1948
AAPG Bulletin (1948) 32 (11): 2063–2082.
... and south and at right angles to the Shawneetown-Rough Creek fault, the south end of the field being 4 1 2 miles north of the fault. West of the Hitesville anticline is a broad shallow syncline bordered on the west by the Uniontown anticline and fault ( Fig. 2 ). Fig. 2. —Regional map...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1943
AAPG Bulletin (1943) 27 (6): 814–821.
... per day, and the general average seems to be approximately 500 barrels. This discovery led to the drilling of numerous wildcat wells in Henderson and Union counties. As a result, new pools were discovered at Uniontown in Union County, and the Wathen pool was discovered a few miles southwest...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1938
AAPG Bulletin (1938) 22 (2): 175–188.
... Geological Survey. 3 In West Virginia the Ridgeley sandstone member of the Oriskany ( Fig. 1 ) is correlative with the Oriskany sand of the driller and is the main producing member of this series. Recently, commercial gas has been produced near Uniontown, Fayette County, Pennsylvania, near the crest...
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Journal Article
Published: 01 December 2013
Journal of Sedimentary Research (2013) 83 (12): 1114–1129.
... was performed using stratigraphic data from the Pennsylvanian succession containing floodplain limestones of the Stewart Quadrangle of Athens County in Ohio (USA). Limestone volumes for six limestone units (Upper Pittsburgh, Fishpot, Sewickley, Benwood/Arnoldsburg, Uniontown, and Waynesburg limestones) were...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1941
AAPG Bulletin (1941) 25 (8): 1563–1574.
... and on the eastern flanks, particularly in West Virginia and Pennsylvania, there has been relatively little exploration. At Uniontown, Pennsylvania (well No. 21), commercial amounts of gas have been developed on the Chestnut Ridge anticline from the Oriskany and overlying Onondaga chert beds. In well No. 23...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1955
AAPG Bulletin (1955) 39 (3): 317–328.
... Run anticline the “Oriskany” was encountered in wells at a depth of approximately 3,000 feet. The major structural elements of the area are complex folds; no mappable faults were recognized in the area west of the North Mountain fault, which lies about 11 miles southeast of the Bergton-Crab Run...
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Journal Article
Published: 01 June 2005
Bulletin of the Seismological Society of America (2005) 95 (3): 1193–1201.
... . Hildenbrand , T. G. , and D. Ravat ( 1997 ). Geophysical setting of the Wabash Valley Fault System , Seism. Res. Lett. 68 , 567 – 585 . Johnson , W. D. , and R. L. Norris ( 1976 ). Geologic map of parts of the Uniontown and Wabash Island quadrancles, Union and Henderson Counties...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1948
AAPG Bulletin (1948) 32 (1): 34–51.
... for March, 1947, was 755 barrels of oil. Cumulative production of the field to April 1, 1947, was 489,865 barrels of oil. The limits of the field now appear to be fairly well defined. A normal fault, downthrown on the west with 250-300 feet displacement, delimits the west side of the field. The Powell’s...
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