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A list of all pages that have property "Caption" with value "Interpretive cross section of the Winslow–Henderson channel.". Since there have been only a few results, also nearby values are displayed.

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  • File:Penn carbondale 4-68.jpg  + (Figure 4-68. Diagram modified from Willman and Payne (1942) illustrating the relationship of Spring Lake Coal to adjacent units. Copyright © 1942 University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-69.jpg  + (Figure 4-69. Graphic log based on core frFigure 4-69. Graphic log based on core from Peabody Energy borehole no. 15-H7, sec. 15, T 6 N, R 8 W, Sullivan County, Indiana, the reference section for the Bucktown Coal Member of previous authors. After Willman and Payne (1942). Copyright © 1942 Illinois State Geological Survey.t © 1942 Illinois State Geological Survey.)
  • File:Penn carbondale 4-7.jpg  + (Figure 4-7. Graphic log of Indiana GeologFigure 4-7. Graphic log of Indiana Geological Survey borehole SDH-306 in sec. 2, T 2 S, R 7 W, Pike County, Indiana. Data from Hasenmueller and Ault (1991). This core is the reference section for the underlined members. © University of Illinois Board of Trustees. University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-70.jpg  + (Figure 4-70. Graphic log of part of the core from Arch Minerals borehole 57 in sec. 14, T 6 S, R 4 W, Perry County, Illinois, the type section of the Percy Limestone Member (new to this report). © University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-71.jpg  + (Figure 4-71. Graphic column at Burning Star No. 4 Mine showing the Percy Limestone Member. Modified from Palmer and Dutcher (1979). Copyright © 1979 University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-72.jpg  + (Figure 4-72. Correlations between IllinoiFigure 4-72. Correlations between Illinois and Missouri, with special reference to the Higginsville (Missouri) and Percy (Illinois) Limestone Members. Left column © University of Illinois Board of Trustees. Right column modified from Gentile and Thompson (2004). Used with permission of the Missouri Geological Survey.mission of the Missouri Geological Survey.)
  • File:Penn carbondale 4-73.jpg  + (Figure 4-73. Five well logs illustrating the Walshville channel and Walshville Member in Franklin County, southern Illinois. Well 2 is the type log for the Walshville Member. © University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-74.jpg  + (Figure 4-74. Graphic log of the Madison Coal Corp. No. 25 borehole from sec. 12, T 8 S, R 3 E, Williamson County, Illinois, the reference section for the Herrin Coal Member. © University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-75.jpg  + (Figure 4-75. Photograph illustrating the Figure 4-75. Photograph illustrating the great thickness of the Herrin Coal close to the Walshville channel. This photograph was taken circa 1915 in the Old Ben No. 9 underground mine near West Frankfort in Franklin County, Illinois. Wearing a soft cap with open-flame carbide lamp and smoking a pipe, the miner is undercutting the coal seam in preparation for drilling shot holes and blasting with black powder. Photograph donated to ISGS by the Illinois Mining Institute. to ISGS by the Illinois Mining Institute.)
  • File:Penn carbondale 4-76.jpg  + (Figure 4-76. Hand specimen of “blue band.” Photograph 2008 by Scott D. Elrick. © University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-77.jpg  + (Figure 4-77. The “blue band” at a site where the Herrin Coal is reduced to thin streaks of coal, box cut at the Francisco Mine, Gibson County, Indiana. Photograph 2010 by Scott D. Elrick. © University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-78.jpg  + (Figure 4-78. Graphic log of Freeman Coal Figure 4-78. Graphic log of Freeman Coal Company borehole No. 06-01-72 drilled in sec. 16, T 3 S, R 2 E, Jefferson County, Illinois. This core serves as a reference section for the Energy Shale and Anna Shale Members. © University of Illinois Board of Trustees. University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-79.jpg  + (Figure 4-79. Lens of Energy Shale sharply truncated by Anna Shale in the Orient No. 4 underground mine, Williamson County, Illinois. Photograph 1976 from ISGS files. The geologist is Christopher Ledvina. © University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-8.jpg  + (Figure 4-8. Graphic log of part of the Snow Hill Coal Corp. Talleydale Mine boring no. 1, a reference section for the Seelyville Coal Member. Location is in sec. 20, T 13 N, R 9 W, Vigo County, Indiana. © University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-80.jpg  + (Figure 4-80. Thin lens of Energy Shale trFigure 4-80. Thin lens of Energy Shale truncated with an angular contact by the overlying Anna Shale at the Orient No. 4 underground mine, Williamson County, Illinois. Laminations in the Energy Shale can be seen on the left side of the photograph. The knobby lower surface of the Brereton Limestone can be seen at the top of the image. Approximate height of view is 5 ft (1.5 m). Photograph 1976 from ISGS files. © University of Illinois Board of Trustees. University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-81.jpg  + (Figure 4-81. Strongly jointed, sheety Anna Shale in the roof of the Orient No. 4 underground mine, Williamson County, Illinois. Photograph 1976 from ISGS files. Brunton compass for scale. © University of Illinois Board of Trustees.)
  • File:Penn carbondale 4-9.jpg  + (Figure 4-9. Composite section for west-central Illinois. After Wanless (1957), with current names and correlations to Indiana, Kentucky, and southern Illinois. © University of Illinois Board of Trustees.)
  • File:C605-Figure-31.jpg  + (Gamma-ray–neutron log from the Berry Petroleum No. 11-14 Pitcher well in Jasper County, Illinois, indicating coal in the upper part of the Effingham channel fill.)
  • File:C605-Figure-36.jpg  + (Generalized sketches illustrating oppositeGeneralized sketches illustrating opposite margins of the Leslie Cemetery channel, as exposed in surface mines in the eastern half of 9S, 4W, Warrick County, Indiana. The upper image is from Peabody’s Lynnville Mine in July 1983, representing the northern half of the channel. The lower image is from Peabody’s Eby Pit in June 1982, representing the southern half of the channel.esenting the southern half of the channel.)
  • File:C605-Figure-32.jpg  + (Graphic log of core from Richland County, Graphic log of core from Richland County, Illinois, showing filling of the Effingham channel. The core shows two upward-fining sequences, the lower having tidal rhythmites in the upper part. The borehole is ISGS No. 1 Elysium (Hazel Farm) in sec. 27, T4N, R9E (county no. 25922).) in sec. 27, T4N, R9E (county no. 25922).)
  • File:C605-Figure-06.jpg  + (Graphic logs from cores serving as type seGraphic logs from cores serving as type sections of the newly named members: (a) Energy Plus borehole no. ME-13 in sec. 31, T4S, R6E, type section of the Delafield Member. (b) Kerr-McGee borehole no. 7629-16 in sec. 29, T7S, R6E, Saline County, type section of the Galatia Member.ounty, type section of the Galatia Member.)
  • File:C605-Figure-33.jpg  + (Interpretive cross section of the Effingham channel in Richland County, Illinois, showing two stages of infilling, with local coal at the top of the lower stage.)
  • File:C605-Figure-42.jpg  + (Interpretive cross section of the Herrin Coal, Walshville channel, and Energy Shale.)
  • File:C605-Figure-48.jpg  + (Interpretive cross section of the Oraville channel.)
  • File:C605-Figure-45.jpg  + (Interpretive cross section of the Winslow-Henderson channel. BR, Brereton Limestone; HR, Herrin Coal; BH/BT, Briar Hill/Bucktown Coal; SD/AC, St. David/Alum Cave Limestone; TM, Turner Mine Shale.)
 (Interpretive cross section of the Winslow–Henderson channel.)
  • File:C605-Figure-37.jpg  + (Interpretive diagram showing sequential deInterpretive diagram showing sequential development of the Leslie Cemetery channel. (a) The Francisco channel is eroded and filled with sediment, largely sand. (b) Springfield peat accumulates in swale left by the abandoned channel. (c) Flowing water reoccupies the channel during the later stages of peat accumulation. Peat encroaches from the margins as the channel migrates laterally. (d) A marine incursion drowns the region and deposits black shale and limestone. Channel filling inverts the topography because of differential compaction.graphy because of differential compaction.)
  • File:C605-Figure-07.jpg  + (Isopach map of the Delafield Member. After Wanless et al. (1970)'"`UNIQ--ref-00000001-QINU`"'. Thicknesses are in feet.)
  • File:C605-Figure-41.jpg  + (Isopach map of the Francis Creek Shale.)
  • File:C605-Figure-38.jpg  + (Map and cross section of the Terre Haute channel. From Friedman (1960)'"`UNIQ--ref-00000001-QINU`"'. Courtesy of the Indiana Geological and Water Survey. Lines of cross section are shown on the map.)
  • File:C605-Figure-25.jpg  + (Map and cross section of the disturbance in the Dering Coal Company No. 2 Mine, Saline County, Illinois. Redrafted from field sketches by Rolf Roley and G.H. Cady in the ISGS archives.)
  • File:C605-Figure-24.jpg  + (Map and cross section of the disturbance in the Sahara No. 20 Mine, Saline County, Illinois.)
  • File:Penn carbondale 4-55 map.jpg  + (Map for Figure 4-55. Cross section of Galatia channel in Raleigh area, Saline County. © University of Illinois Board of Trustees.)
  • File:C605-Figure-08.jpg  + (Map from Potter (1962)'"`UNIQ--ref-00000006-QINU`"', showing the thickness (in feet) of sandstone between the Houchin Creek and Springfield Coals, with the Galatia channel (from Hopkins 1968'"`UNIQ--ref-00000007-QINU`"') superimposed.)
  • File:C605-Figure-30.jpg  + (Map from Potter (1962)'"`UNIQ--ref-00000001-QINU`"' showing the Effingham channel as described in this report.)
  • File:C605-Figure-39.jpg  + (Map of the Illinois Basin showing channels and gray shale wedges affecting the Murphysboro, Colchester, Herrin, Baker, and Danville Coals.)
  • File:C605-Figure-01.jpg  + (Map of the Illinois Basin showing the exteMap of the Illinois Basin showing the extent of Pennsylvanian rocks, thickness of the Springfield Coal, and channels interrupting the coal. From Finley et al. (2005)'"`UNIQ--ref-00000001-QINU`"'. Straight lines separating polygons are artifacts of mapping protocol in original.artifacts of mapping protocol in original.)
  • File:C605-Figure-35.jpg  + (Map of the Leslie Cemetery channel prepared for this study, using information from boreholes and mines. Lines of section for Figure 36 and Plate 6 are shown.)
  • File:C605-Plate-01.jpg  + (Map of the southeastern part of the Illinois Basin showing the thickness of the Springfield Coal, channels that affect the coal, and major structural features)
  • File:C605-Figure-43.jpg  + (Map showing the Walshville channel and sulfur content of the Herrin Coal. After Treworgy et al. (2000)'"`UNIQ--ref-00000001-QINU`"'. The four named areas of low-sulfur coal are all associated with thick Energy Shale adjacent to the channel.)
  • File:C605-Figure-44.jpg  + (Map showing the Winslow–Henderson channel.)
  • File:C605-Figure-10.jpg  + (Map showing the thickness and mined areas of the Springfield Coal throughout Illinois. After Treworgy et al. (1999)'"`UNIQ--ref-00000001-QINU`"'. Straight lines separating polygons are artifacts of mapping protocol in original.)
  • File:C605-Figure-14.jpg  + (Map showing the thickness of the Dykersburg Member in the vicinity of Galatia channel in southeastern Illinois. From Treworgy et al. (1999)'"`UNIQ--ref-00000001-QINU`"'.)
  • File:C605-Figure-47.jpg  + (Map showing the thickness of the Murphysboro Coal near the Oraville channel in Jackson and Perry Counties, southwestern Illinois. From Jacobson (1983)'"`UNIQ--ref-00000001-QINU`"')
  • File:C605-Figure-34.jpg  + (Maps of the Leslie Cemetery channel. (a) RMaps of the Leslie Cemetery channel. (a) Regional map showing the relationship to other channels. (b) Map of the northern part of the Leslie Cemetery channel, with the thickness of the Folsomville Member. From Eggert (1984), The Leslie Cemetery and Francisco distributary fluvial channels in the Petersburg Formation (Pennsylvanian) of Gibson County, Indiana, U.S.A., in R.A. Rahmani and R.M. Flores, eds., Sedimentology of coal and coal-bearing sequences: International Association of Sedimentologists, Special Publication 7 p. 311, 313. Copyright © 1984 The International Association of Sedimentologists.rnational Association of Sedimentologists.)
  • File:C605-Figure-18.jpg  + (Photograph of an upright tree stump, rooted at the top of the coal and encased in mudstone of the Dykersburg Member, at American Coal’s Galatia Mine in Saline County, Illinois.)
  • File:C605-Figure-29.jpg  + (Photograph of interlaminated carbonaceous shale and bright to dull coal close to the margin of the Sullivan channel in the Oaktown Mine in Knox County, Indiana.)
  • File:C605-Figure-28.jpg  + (Photograph of interlaminated carbonaceous shale and bright to dull coal close to the margin of the Sullivan channel in the Oaktown Mine in Knox County, Indiana.)
  • File:C605-Figure-19.jpg  + (Photograph of “rolls” at the top of the SpPhotograph of “rolls” at the top of the Springfield Coal, filled with Dykersburg sediments, at American Coal’s Millennium Mine in Saline County, Illinois. Ragged splaying of coal layers at the margins of rolls evokes fibrous peat layers ripped out by strong currents.peat layers ripped out by strong currents.)
  • File:C605-Figure-15.jpg  + (Photograph showing rhythmic lamination in Photograph showing rhythmic lamination in sandy facies of the Dykersburg Member in American Coal’s Millennium Mine, Saline County, Illinois. Enlarged view at right. Reprinted from Palaeogeography, Palaeoclimatology, Palaeoecology, v. 487, p. 74, W.A. DiMichele, S.D. Elrick, and W.J. Nelson, Vegetational zonation in a swamp forest, Middle Pennsylvanian, Illinois Basin, U.S.A., indicates niche differentiation in a wetland plant community. Copyright 2017, with permission from Elsevier.right 2017, with permission from Elsevier.)
  • File:C605-Figure-16.jpg  + (Photograph showing rhythmic lamination in sandy facies of the Dykersburg Member in the Millennium Mine, with lamination offlapping the top of the coal. Sediment thus was deposited in a wedge, prograding from left to right.)