A2 and B2: Upper Devonian Kellwasser Extinction Events in New York and Pennsylvania: Offshore to Onshore Transect Across the F
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Fractured Shale Gas Potential in New York
FRACTURED SHALE GAS POTENTIAL IN NEW YORK David G. HILL and Tracy E. LOMBARDI TICORA Geosciences, Inc., Arvada, Colorado, USA John P. MARTIN New York State Energy Research and Development Authority, Albany, New York, USA ABSTRACT In 1821, a shallow well drilled in the Devonian age shale ushered in a new era for the United States when natural gas was produced, transported and sold to local establishments in the town of Fredonia, New York. Following this discovery, hundreds of shallow shale wells were drilled along the Lake Erie shoreline and eventually several shale gas fields were established southeastward from the lake in the late 1800’s. Since the mid 1900’s, approximately 100 wells have been drilled in New York to test the fractured shale potential of the Devonian and Silurian age shales. With so few wells drilled over the past century, the true potential of fractured shale reservoirs has not been thoroughly assessed, and there may be a substantial resource. While the resource for shale gas in New York is large, ranging from 163-313 trillion cubic feet (Tcf) and the history of production dates back over 180 years, it has not been a major contributor to natural gas production in New York. A review of the history and research conducted on the shales shows that the resource in New York is poorly understood and has not been adequately tested. Other shales such as the Silurian and Ordovician Utica Shale may also hold promise as new commercial shale gas reservoirs. Experience developing shale gas plays in the past 20 years has demonstrated that every shale play is unique. -
Mapping Potential Geologic Hazards for Proposed Highway Construction Projects in Pennsylvania: Route 15 in Lycoming County
Mapping Potential Geologic Hazards for Proposed Highway Construction Projects in Pennsylvania: Route 15 in Lycoming County By Stuart O. Reese, P.G. Pennsylvania Geological Survey 3240 Schoolhouse Road Middletown, PA 17057 Telephone: (717) 702-2028 Fax: (717) 702-2065 email: [email protected] INTRODUCTION acidic drainage from uncovered Marcellus Shale (a black shale with approximately 3 percent sulfur) that had to be mitigated. The current project is situated in north-central Pennsyl- Recently, the Pennsylvania Geological Survey has vania in the Deep Valleys section of the Appalachian Plateaus worked on behalf of the Pennsylvania Department of Trans- portation (PennDOT) to develop maps for specific highway physiographic province in Lycoming County, Pennsylvania. construction projects. The purpose of these maps is to identify Section C41 of U.S. Route 15 is located from north of Trout potential geologic hazards such as landslides, sinkholes, min- Run to the Village of Buttonwood in the “Steam Valley” eralization, historic deep mines, acid drainage, and ground- area of Cogan House and Lewis Townships. The improved water conditions. Map layers have included aerial imagery, highway corridor will become part of Interstate 99, the Appa- digital elevation model (DEM) datasets, digital raster graphics lachian Thruway. This requires an upgrade of the 4 1/2 mile (DRGs), bedrock units and their contacts, surficial and struc- Steam Valley section (C41) to a four-lane limited access high- tural geology features, mapped landslides, glacial boundaries, way that meets current design standards comparable to adja- and water well locations. Possible issues are described in cent sections of U.S. 15. Construction is estimated to begin in the accompanying poster for the proposed construction zones fall 2007 (pending the availability of funds). -
(Late Devonian) Boundary Within the Foreknobs Formation, Maryland and West Virginia
The Frasnian-Famennian (Late Devonian) boundary within the Foreknobs Formation, Maryland and West Virginia GEORGE R. McGHEE, JR. Department of Geological Sciences, University of Rochester, Rochester, New York 14627 ABSTRACT The approximate position of the Frasnian-Famennian (Late De- vonian) boundary is determined within the Foreknobs Formation along the Allegheny Front in Maryland and West Virginia by utiliz- ing the time ranges of the articulate brachiopods Athryis angelica Hall, Cyrtospirifer sulcifer (Hall), and members of the Atrypidae. INTRODUCTION The age of strata previously called the "Chemung Formation" along the Allegheny Front in Maryland and West Virginia (Fig. 1) has been of interest to Devonian wokers for some time. Recent at- tempts to resolve this problem include the works of Dennison (1970, 1971) and Curry (1975). New paleontological contribu- tions to the resolution of time relations within the Greenland Gap Group ("Chemung Formation") are the object of this paper, which is an outgrowth of a much larger ecological analysis of Late Devo- nian benthic marine fauna as preserved in the central Appalachians (McGhee, 1975, 1976). STRATIGRAPHIC SETTING The following is a condensation and summary of the evolution of Upper Devonian stratigraphic nomenclatural usage in the study Figure 1. Location map of study area, showing positions of the mea- area; for a more complete and thorough discussion, the reader is sured sections used in this study (after Dennison, 1970). referred to Dennison (1970) and Kirchgessner (1973). The Chemung Formation was originally designated by James lower Cohocton Stage." Elsewhere, concerning the upper limit of Hall (1839) from Chemung Narrows in south-central New York. -
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, By GEORGE V. COHEE, ROBERT G. BATES, and WILNA B. WRIGHT CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1294-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 35 cents (paper cover) CONTENTS Listing of nomenclatural changes- --- ----- - - ---- -- -- -- ------ --- Ortega Quartzite and the Big Rock and Jawbone Conglomerate Members of the Kiawa Mountain Formation, Tusas Mountains, New Mexico, by Fred Barker---------------------------------------------------- Reasons for abandonment of the Portage Group, by Wallace de Witt, Jr-- Tlevak Basalt, west coast of Prince of Wales Island, southeastern Alaska, by G. Donald Eberlein and Michael Churkin, Jr Formations of the Bisbee Group, Empire Mountains quadrangle, Pima County, Arizona, by Tommy L. Finnell---------------------------- Glance Conglomerate- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - Willow Canyon Formation ....................................... Apache Canyon Formation-- ................................... Shellenberger Canyon Formation- - --__----- ---- -- -- -- ----------- Turney Ranch Formation---- ------- ------ -- -- -- ---- ------ ----- Age--_------------------------------------------------------- Pantano Formation, by Tommy L. Finnell----------_----------------- -
Assessing the Petroleum Geology and Future Development of the Clendenin Gas Field in Kanawha County, West Virginia
Assessing the Petroleum Geology and Future Development of the Clendenin Gas Field in Kanawha County, West Virginia By: Jonathan Prevatte August 2020 Director of Thesis: Donald W. Neal Major Department: Geological Sciences Petroleum is one of the main sources for energy production in the US and is therefore important for the continuation of economic growth. Future development of petroleum resources in the US to meet supply demands is equally important. Understanding the controls on petroleum production will help in determining where and how to development these resources for maximum production. West Virginia is home to many gas fields and is underlain by one of the more prominent gas producing shales, the Marcellus Shale. The Clendenin Gas Field in Kanawha County is one of the historical gas producing areas found in West Virginia. This assessment is focused on the Devonian strata throughout the field including the Marcellus Shale. Using available geophysical logs, production data, and historic well records obtained from the West Virginia Geologic and Economic Survey (WVGES), cross-sections, isopach maps, and structure contour maps were created to give a visual representation of the subsurface geology across the field. Construction of the cross-sections and maps in conjunction with production and well record data aided in the identification of controls influencing production throughout the field. Applying the findings of this assessment to future production may reduce costs and improve yields of future petroleum wells. Results of this study indicate several options should be considered when planning for future production wells within the field. Target areas include the areas to the east of the field where formations tend to thicken. -
Appalachian Bedrock Geology
Bedrock References (updated November 21, 1998) Alger, W.C., 1986, Petrography of the Upper Devonian sequence east of Elkins, West Virginia: Unpublished M.S. Thesis, West Virginia Univeristy, Morgantown, WV, 168 p. On file(Y/N):y Read?(Y/N):n X-ref(Y/N):n/a Applicability(0,low,m,high):m-h Arkle, T., 1974, Stratigraphy of the Pennsylvanian and Permian systems of the central Appalachians: Geological Society of America Special Paper 148, p. 5-29. Avary, K.L., ed., 1979, Devonian clastics in West Virginia and Maryland, Field Trip Guide, Oct. 3-5, 1979: West Virginia Geological and Economic Survey, 100 p. (Guidebook for Eastern Section meeting of AAPG) (this is the original field trip across sections on US 33, Call No. W 551.72 D498 in Colson Library, WV Collection) Barrell, S.M., 1986, Stratigraphy and depositional environments of Upper Devonian rocks in east central West Virginia and adjacent Virginia: Unpublished M.S. Thesis, University of North Carolina at Chapel Hill, 113 p. On file(Y/N):y Read?(Y/N):n X-ref(Y/N):n/a Applicability(0,low,m,high):m-h Barrell, S.M., and Dennison, J.M., 1986, Northwest-southeast stratigraphic cross-section of Devonian Catsill Delta in east-central West Virginia and adjacent Virginia: Appalachian Basin Industrial Associates, Program Fall Meeting October 16-17, 1986, Pittsburgh, Pennsylvania, v. 11, p. 7-32. Beardsley, R.W. and Cable, M.S., 1983, Overview of the evolution ofthe Appalachian basin: Northeastern Geology, v. 5, p. 137-145. On file(Y/N):y Read?(Y/N):n X-ref(Y/N):n/a Applicability(0,low,m,high):l-m Berger, P.S., Perry, W.J., and Wheeler, R.L., 1979, Three-stage model of brittle deformation in central Appalachians: Southeastern Geology, v. -
Xsec A-A Sht1of2 Layout FINAL V
U.S. DEPARTMENT OF THE INTERIOR SCIENTIFIC INVESTIGATIONS MAP 3425 U.S. GEOLOGICAL SURVEY (SHEET 1 OF 2) Explanatory pamphlet accompanies map A Ontario Allegheny Lowlands Plateau province province SEVERNE WATKINS-BEAVER LODI POINT FIRTREE DAMS ALPINE VAN ETTEN ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE GLENORA SYNCLINE UNNAMED COHOCTON CORBETT POINT ENFIELD CAYUTA SYNCLINE SYNCLINE SYNCLINE SYNCLINE SYNCLINE Bend in section Bend in section Bend in section New York W SE Oatka Genesee NW SE Canisteo NW SW Pennsylvania Black Creek River Canaseraga River Tuscarora Creek Creek Creek FEET MILES 0 10 20 30 40 50 60 70 80 90 3,000 1 2 3 4 5 6 William Duchscherer, Jr. E.F. Blair and Associates NYS Natural Gas Company E.F. Blair and Associates Bowdoin Storage Service Inc. NYS Natural Gas Company No. 1 J. Klotzbach No. 1 L. Tyler No. 1 Albert McClurg No. 1 Arthur N. Kennedy No. 1 Hubbard No. 1 Robert Olin API No. 31-037-05117 API No. 31-037-04593 API No. 31-051-04552 API No. 31-051-04630 API No. 31-101-21496 API No. 31-101-03924 Genesee Co., New York Genesee Co., New York Livingston Co., New York Livingston Co., New York Steuben Co., New York Steuben Co., New York Perrysburg Formation Dunkirk Dunkirk Shale Shale 2,000 Member Wiscoy Sandstone Member Java Perrysburg West River Shale, Nunda Wiscoy Sandstone Member Formation Formation Genundewa Sandstone Member unnamed Pipe Creek 0 Pipe Creek shale member Limestone, Penn Member Shale Member Shale Member Perrysburg Yan Shale, and rmation Formation 0 Dun West River Shale, Java Fo kirk -
Methane in Pennsylvania Water Wells Unrelated to Marcellus Shale Fracturing Lisa J
Methane in Pennsylvania water wells unrelated to Marcellus shale fracturing Lisa J. Molofsky of existing gas wells. The correlation of methane concentra- John A. Connor tions with elevation indicates that, on a regional level, elevat- Shahla K. Farhat ed methane concentrations in groundwater are a function of GSI Environmental Inc. geologic features, rather than shale gas development. Houston Technical literature and historical publications confirm the presence of methane gas in natural seeps and water wells Albert S. Wylie Jr. in this region for many decades, long before shale gas drill- Tom Wagner ing operations were initiated in 2006. Cabot Oil & Gas Corp. Potential sources of this naturally occurring methane in- Pittsburgh clude thermogenic gas-charged sandstones in the Catskill formation, which are tapped by most water wells in this re- Results from more than 1,700 water wells sampled and test- gion. These sandstones exhibit an extensive network of frac- ed prior to proposed gas drilling in Susquehanna County, tures, joints, and faults that serve as principle conduits of Pa., show methane to be ubiquitous in shallow groundwater, groundwater flow and potential pathways for the movement with a clear correlation of methane concentrations with sur- of shallow-sourced dissolved methane. face topography. Biogenic methane, which is produced by the natural de- Specifically, water wells located in lowland valley areas composition of organic material within thick valley alluvium exhibit significantly higher dissolved methane levels than and glacial drift deposits in the area, may also be found in wa- water wells in upland areas, with no relation to proximity ter wells that draw water from shallower sediment deposits. -
Geochemical and Mineralogical Sampling of the Devonian Shales in the Broadtop Synclinorium, Appalachian Basin, in Virginia, West Virginia, Maryland, and Pennsylvania
Geochemical and Mineralogical Sampling of the Devonian Shales in the Broadtop Synclinorium, Appalachian Basin, in Virginia, West Virginia, Maryland, and Pennsylvania By Catherine B. Enomoto, James L. Coleman, Jr., Christopher S. Swezey, Patrick W. Niemeyer, and Frank T. Dulong Open-File Report 2015–1061 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2015 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner Suggested citation: Enomoto, C.B., Coleman, J.L., Jr., Swezey, C.S., Niemeyer, P.W., and Dulong, F.T., 2015, Geochemical and mineralogical sampling of the Devonian shales in the Broadtop synclinorium, Appalachian basin, in Virginia, West Virginia, Maryland, and Pennsylvania: U.S. Geological Survey Open-File Report 2015‒1061, 32 p., 5 pls., 1 appendix, http://dx.doi.org/10.3133/ofr20151061. ISSN 2331-1258 (online). Contents Abstract ..................................................................................................................................................................... -
Eastern Section American Association of Petroleum Geologists 46Th Annual Meeting Morgantown, West Virginia September 24-27, 2017
Eastern Section American Association of Petroleum Geologists 46th Annual Meeting Morgantown, West Virginia September 24-27, 2017 Program with Abstracts Hosted by: Appalachian Geological Society West Virginia University Department of Geology and Geography With support from the West Virginia Geological and Economic Survey Meeting Sponsors We appreciate your support! Marcellus Level Meeting Sponsors Utica Level Rogersville Level We appreciate your support! Eastern Section American Association of Petroleum Geologists 46th Annual Meeting Morgantown, West Virginia September 24-27, 2017 Program with Abstracts Hosted by: Appalachian Geological Society West Virginia University Department of Geology and Geography With support from the West Virginia Geological and Economic Survey Cover photo used with permission from Jacob Everhart, Canary, LLC Contents Welcome………………………………………………………………………………………………………………………………………1 2017 Meeting Organizing Committee……………………………………………………………………………….1 Eastern Section AAPG Officers………………………………………………………………………………………….2 Appalachian Geological Society Officers……………………………………………………………………………2 General Information…………………………………………………………………………………………………………………….3 Registration Hours……………………………………………………………………………………………………………3 Parking………………………………………………………………………………………………………………………….….3 Maps………………………………………………………………………………………………………………………………..3 Exhibits……………………………………………………………………………………………………………………….……3 Presenters and Judges Room……………………………………………………………………………………..….…3 Presenters, Judges and Session Chairs Breakfast and Information……………………………………3 -
Figure 2 (Pdf)
South North West East West East West East West East Eastern Kentucky Central West Virginia Eastern and Central Ohio Western and Central Pennsylvania Western and Central New York Age Stratigraphy from: Repetski and others (2008) Stratigraphy from: Ryder and others (2008, 2009) Stratigraphy from: Ryder and others (2008, 2009, 2010) Stratigraphy from: Berg and others (1983); Ryder and others (2010) Stratigraphy from: Repetski and others (2008) Era System Series (Ma) Valley Valley Rome Trough Rome Trough Rome Trough and Ridge Bedford Shale and Ridge Cleveland Member Venango Group Catskill Formation 359.2 Upper Devonian strata, undivided Ohio Shale Ohio Three Lick Bed Chagrin Shale equivalent rocks Chagrin Shale Bradford Group Foreknobs Formation Perrysburg Formation Shale Dunkirk Shale Member Huron Member of Ohio Shale Huron Member Elk Group Scherr Formation Upper Dunkirk Shale Java Formation Angola Shale Member Olentangy Shale (upper) Java Formation Java Formation Angola Shale Member West Falls West Falls Brallier Formation West Falls Angola Shale Member Formation Rhinestreet Shale Member Rhinestreet Shale Member of the Formation Rhinestreet Shale Member Formation Rhinestreet Shale Member Upper Devonian strata, undivided West Falls Formation 385.3 Sonyea and Genesee Formations, undivided Sonyea and Genesee Formations, undivided Sonyea and Genesee Formations, undivided Tully Limestone Tully Limestone Tully Limestone Mahantango Formation Mahantango Formation Moscow, Ludlowville, and Skaneateles Shales, undivided Hamilton Olentangy Shale (lower) -
Regional Stratigraphy and Petroleum Systems of the Appalachian Basin, North America
U.S. DEPARTMENT OF THE INTERIOR GEOLOGIC INVESTIGATIONS SERIES U.S. GEOLOGICAL SURVEY MAP I–2768 SOUTHWEST NORTHEAST 85° W 80° W 75° W INTRODUCTION In addition to the major packages of siliciclastic rocks, there are two minor packages Age 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 General Age of siliciclastic rocks that were deposited at approximately 480 to 475 million years North North Although more than 100 years of research have gone into deciphering the ago (St. Peter Sandstone) and at approximately 389 to 387 million years ago (million Features (million Periods Epochs American American East- North- North- Central Eastern Western Eastern South- South- Central North- Northern Western South- East- South- South- North- North- North- Southern Western West- East- Sequences Sequence Periods 45° N 45° N Paleozoic stratigraphy of the Appalachian Basin of North America, it remains a (Oriskany Sandstone). These two minor packages of siliciclastic rocks are present years central east west Tenn. Tenn. Va. Ky. west east W.Va. west W.Va. Md. east central west east east west central Ontario N.Y. central central Boundaries (Interpreted years Lake challenge to visualize the basin stratigraphy on a regional scale and to describe within predominantly carbonate strata and they are not associated with significant Series Stages Huron Events) ago) WISCONSIN stratigraphic relations within the basin. Similar difficulties exist for visualizing and fining-upwards or coarsening-upwards trends. Furthermore, these siliciclastic rocks ago) Ala. Ala. Ga. W.Va. W.Va. W.Va.