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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. -
Pathways and Mechanisms of Late Ordovician (Katian) Faunal Migrations of Laurentia and Baltica
Estonian Journal of Earth Sciences, 2015, 64, 1, 62–67 doi: 10.3176/earth.2015.11 Pathways and mechanisms of Late Ordovician (Katian) faunal migrations of Laurentia and Baltica Adriane R. Lama and Alycia L. Stigalla,b a Department of Geological Sciences, Ohio University, Athens 45701-2979, Ohio, U.S.A. b OHIO Center for Ecology and Evolutionary Studies, Ohio University, 316 Clippinger Laboratories, Athens 45701-2979, Ohio, U.S.A.; [email protected], [email protected] Received 2 July 2014, accepted 9 October 2014 Abstract. Late Ordovician strata within the Cincinnati Basin record a mass faunal migration event during the C4 and C5 depositional sequences. The geographic source region for the invaders and the paleoceanographic conditions that facilitated dispersal into the Cincinnati Basin has previously been poorly understood. Using Parsimony Analysis of Endemicity, biogeographic relationships among Laurentian and Baltic basins were analyzed for each of the C1–C5 depositional sequences to identify dispersal paths. The results support multiple dispersal pathways, including three separate dispersal events between Baltica and Laurentia. Within Laurentia, results support dispersal pathways between areas north of the Transcontinental Arch into the western Midcontinent, between the Upper Mississippi Valley into the Cincinnati Basin, and between the peri-cratonic Scoto-Appalachian Basin and the Cincinnati Basin. These results support the hypothesis that invasive taxa entered the Cincinnati Basin via multiple dispersal pathways and that the equatorial Iapetus current facilitated dispersal of organisms from Baltica to Laurentia. Within Laurentia, surface currents and large storms moving from northeast to southwest likely influenced the dispersal of organisms. Larval states were characterized for the Richmondian invaders, and most invaders were found to have had planktotrophic planktic larvae. -
A2 and B2: Upper Devonian Kellwasser Extinction Events in New York and Pennsylvania: Offshore to Onshore Transect Across the F
A2 AND B2: UPPER DEVONIAN KELLWASSER EXTINCTION EVENTS IN NEW YORK AND PENNSYLVANIA: OFFSHORE TO ONSHORE TRANSECT ACROSS THE FRASNIAN-FAMENNIAN BOUNDARY ON THE EASTERN MARGIN OF THE APPALACHIAN BASIN ANDREW M. BUSH AND J. ANDREW BEARD Geosciences & Ecology and Evolutionary Biology, University of Connecticut, Storrs, CT 06269 GORDON BAIRD Department of Geosciences, SUNY Fredonia, Fredonia, NY 14063 D. JEFFREY OVER Department of Geological Sciences, SUNY Geneseo, Geneseo, NY 14454 with contributions by KATHERINE TUSKES Department of Geological Sciences, Atmospheric, Ocean, and Earth Science, George Mason University, Manassas, VA 20110 SARAH K. BRISSON AND JALEIGH Q. PIER Geosciences & Ecology and Evolutionary Biology, University of Connecticut, Storrs, CT 06269 INTRODUCTION Earth-system perturbations caused a series of mass extinction events during the Devonian Period, including the Taghanic event in the Givetian, the Lower and Upper Kellwasser events in the Frasnian, and the Hangenberg event in the Famennian (House, 2002; Bambach, 2006). These extinctions occurred against the backdrop of orbitally forced sea-level fluctuations, the Acadian Orogeny (Averbuch et al., 2005), the expansion of plants and animals on land (Algeo et al., 1995), and ecological changes in the marine biosphere (Signor and Brett, 1984; Bambach, 1999). The Frasnian-Famennian boundary in particular represents a significant global crisis, considered one of the “big five” mass extinctions (Raup and Sepkoski, 1982) that led to the demise of the widespread and diverse Devonian -
The Classic Upper Ordovician Stratigraphy and Paleontology of the Eastern Cincinnati Arch
International Geoscience Programme Project 653 Third Annual Meeting - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett – Kyle R. Hartshorn – Allison L. Young – Cameron E. Schwalbach – Alycia L. Stigall International Geoscience Programme (IGCP) Project 653 Third Annual Meeting - 2018 - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Kyle R. Hartshorn Dry Dredgers, 6473 Jayfield Drive, Hamilton, Ohio 45011, USA ([email protected]) Allison L. Young Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Cameron E. Schwalbach 1099 Clough Pike, Batavia, OH 45103, USA ([email protected]) Alycia L. Stigall Department of Geological Sciences and OHIO Center for Ecology and Evolutionary Studies, Ohio University, 316 Clippinger Lab, Athens, Ohio 45701, USA ([email protected]) ACKNOWLEDGMENTS We extend our thanks to the many colleagues and students who have aided us in our field work, discussions, and publications, including Chris Aucoin, Ben Dattilo, Brad Deline, Rebecca Freeman, Steve Holland, T.J. Malgieri, Pat McLaughlin, Charles Mitchell, Tim Paton, Alex Ries, Tom Schramm, and James Thomka. No less gratitude goes to the many local collectors, amateurs in name only: Jack Kallmeyer, Tom Bantel, Don Bissett, Dan Cooper, Stephen Felton, Ron Fine, Rich Fuchs, Bill Heimbrock, Jerry Rush, and dozens of other Dry Dredgers. We are also grateful to David Meyer and Arnie Miller for insightful discussions of the Cincinnatian, and to Richard A. -
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----------_----------------- -
Geology in 2000 and Beyond by John C
THE EPOCH No. 32 Spring 1998 - January 2000 A Newsletter for Alumni and Students Department of Geology Website: http://www.geology.buffalo.edu The State University of New York at Buffalo E-mail: [email protected] 876 Natural Sciences Complex Telephone: (716) 645-6800, Ext. 6100 Buffalo, New York 14260-3050 Fax: (716) 645-3999 HIGHLIGHTS Geology in 2000 and Beyond By John C. Fountain, Professor & Chairman Departmental News The Fall of 1999 marked a major turning point for the Geology A Review of the Department, not because that is when I began my term as department chair but because, for the first time in five years, the department is fully staffed Last Decade . 2 again – and thus for the first time ever, our programmatic model begun under Field Camp Truck Mike Sheridan can fully be implemented. Replacement Fund . 3 When the department expanded after the formation of the SUNY system, there was one faculty member in each major area (mineralogy, petrology, Meet the NEW Faculty .. 4 structure etc.). The advantages of this model include excellent undergraduate education and a broad range of research interests. The disadvantage of this Duttweiler Geological approach is that each faculty member worked essentially alone, which is a Field Station . 7 significant disadvantage in competing for sponsored research funds. When Mike Sheridan was selected to replace Chet Langway as Chair in 1990, he began a reorganization of the department into concentrated Research News research programs. This resulted in the formation of two major programs: Paoha Island environmental geology and volcanology. While not all of our research falls How did it emerge? . -
WGBH/NOVA #4220 Making North America: Origins KIRK JOHNSON
WGBH/NOVA #4220 Making North America: Origins KIRK JOHNSON (Sant Director, Smithsonian National Museum of Natural History): North America, the land that we love: it looks pretty familiar, don’t you think? Well, think again! The ground that we walk on is full of surprises, if you know where to look. 00:25 As a geologist, the Grand Canyon is perhaps the best place in the world. Every single one of these layers tells its own story about what North America was like when that layer was deposited. So, are you ready for a little time-travelling? 00:38 I’m Kirk Johnson, the director of the Smithsonian National Museum of Natural History, and I’m taking off on the fieldtrip of a lifetime,… 00:50 Look at that rock there. That is crazy! …to find out, “How did our amazing continent get to be the way it is?” EMILY WOLIN (Geophysicist): Underneath Lake Superior, that’s about 30 miles of volcanic rock. KIRK JOHNSON: Thirty miles of volcanic rock? How did the landscape shape the creatures that lived and died here? Fourteen-foot-long fish, in Kansas. That’s what I’m telling you! 01:14 And how did we turn the rocks of our homeland… Ho-ho. Oh, man! …into riches? This thing is phenomenal. In this episode, we hunt down the clues to our continent’s epic past. 01:26 You can see new land being formed, right in front of your eyes. Why does this golf course hold the secret to the rise and fall of the Rockies? What forces nearly cracked North America in half? And is it possible that the New York City skyline… I’ve always wanted to do this. -
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. -
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 -
Justin V. Strauss Department of Earth Sciences Dartmouth College HB6105 Fairchild Hall Hanover, NH 03755 (603) 646–6954 [email protected]
Justin V. Strauss Department of Earth Sciences Dartmouth College HB6105 Fairchild Hall Hanover, NH 03755 (603) 646–6954 [email protected] Education Harvard University, Cambridge, MA PhD, Department of Earth and Planetary Sciences May 2015 MA, Department of Earth and Planetary Sciences May 2014 The Colorado College, Colorado Springs, CO BA, Department of Geology Aug. 2006 Teaching and Work Experience Dartmouth College, Department of Earth Sciences, Hanover, NH Assistant Professor Jan. 2016–present Stanford University, Department of Geological Sciences, Stanford, CA Agouron Institute Geobiology Postdoctoral Scholar July 2015 - Dec. 2015 Harvard University, Department of Earth and Planetary Sciences, Cambridge, MA Field Assistant – Dr. Francis Macdonald July 2009 - Aug. 2009 Field Assistant – Dr. Francis Macdonald May 2008 Princeton University, Department of Geosciences, Princeton, NJ Lab Technician – Dr. Adam Maloof Aug. 2007 - Dec. 2007 Field Assistant – Dr. Adam Maloof June 2007 - Aug. 2007 The Colorado College, Department of Geology, Colorado Springs, CO Paraprofessional Sept. 2006 - June 2007 Honors and Awards 2018 National Geographic Explorer 2018 American Chemical Society Doctoral New Investigator Award 2015 Agouron Institute Geobiology Postdoctoral Fellowship 2015 Geological Society of America Student Research Grant 2014 Geological Society of America Student Research Grant 2013 Star Family Prize for Excellence in Undergraduate Advising Nominee – Harvard University 2013 Bok Center Distinction in Teaching Award – Harvard University 2012 Bok Center Distinction in Teaching Award – Harvard University 2012 GACMAC 2012 Jerome Remick III Poster Award 2012 National Science Foundation Graduate Research Fellowship Recipient 2011 National Science Foundation GRFP Honorable Mention 2006 William A. Fischer Special Recognition Geosciences Award 2005 Patricia J. Buster Scholarship for Undergraduate Research 2004 Patricia J. -
Buenellus Chilhoweensis N. Sp. from the Murray Shale (Lower Cambrian Chilhowee Group) of Tennessee, the Oldest Known Trilobite from the Iapetan Margin of Laurentia
Journal of Paleontology, 92(3), 2018, p. 442–458 Copyright © 2018, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/18/0088-0906 doi: 10.1017/jpa.2017.155 Buenellus chilhoweensis n. sp. from the Murray Shale (lower Cambrian Chilhowee Group) of Tennessee, the oldest known trilobite from the Iapetan margin of Laurentia Mark Webster,1 and Steven J. Hageman2 1Department of the Geophysical Sciences, University of Chicago, 5734 South Ellis Avenue, Chicago, IL 60637 〈[email protected]〉 2Department of Geology, Appalachian State University, Boone, North Carolina 28608, USA 〈[email protected]〉 Abstract.—The Ediacaran to lower Cambrian Chilhowee Group of the southern and central Appalachians records the rift-to-drift transition of the newly formed Iapetan margin of Laurentia. Body fossils are rare within the Chilhowee Group, and correlations are based almost exclusively on lithological similarities. A critical review of previous work highlights the relatively weak biostratigraphic and radiometric age constraints on the various units within the succession. Herein, we document a newly discovered fossil-bearing locality within the Murray Shale (upper Chilhowee Group) on Chilhowee Mountain, eastern Tennessee, and formally describe a nevadioid trilobite, Buenellus chilhoweensis n. sp., from that site. This trilobite indicates that the Murray Shale is of Montezuman age (provisional Cambrian Stage 3), which is older than the Dyeran (provisional late Stage 3 to early Stage 4) age suggested by the historical (mis)identification of “Olenellus sp.” from within the unit as reported by workers more than a century ago. -
CURRICULUM VITA Dr. Robert D. Jacobi Department of Geology and Geoscience Consulting, 411 Cooke Hall Box 52 Universi
CURRICULUM VITA Dr. Robert D. Jacobi Department of Geology and Geoscience Consulting, 411 Cooke Hall Box 52 University at Buffalo Getzville, NY 14068 Buffalo, NY 14260 (716) 645-4294 rdjacobi@ buffalo.edu Education Columbia University, Ph.D. 1980 Dissertation Title: Geology of part of the terrane north of Lukes Arm Fault, north-central Newfoundland (Part I); modern submarine sediment slides and their implications (Part II), 422 p. Columbia University, M. Phil, 1974 (geology) Beloit College, B. A., 1970 (geology & music) Employment History Present-2007 Full Professor, part-time, Department of Geology, University at Buffalo Present-2012 Senior Geology Advisor, EQT, Pittsburgh, PA Present-1990 Consultant to various environmental groups and litigants such as NYS DEC, CCCC, CWVNW and such corporations as Akzo Nobel Salt, Solvay (WY), Bath Petroleum Storage, AECB (Canada), Talisman, Ansbro (Anschutz), Quest, Norse Energy 2012-2012 Co-Director, SRSI at UB 2011-2007 Director of Special Projects, Norse Energy Corporation, 2008-1997 Full Professor, full-time, Department of Geology, University at Buffalo 2005 Interim Chair, Geology Department, University at Buffalo 1997-1986 Associate Professor, Department of Geology, SUNY at Buffalo 1992-1986 Lamont-Doherty Geological Observatory of Columbia University, Adjunct Research Scientist 1990-1986 Senior Member, Undergraduate College at SUNY at Buffalo 1986-1981 Lamont-Doherty Geological Observatory of Columbia University, Visiting Research Associate 1985-1980 Assistant Professor, Department of Geological Sciences, SUNY at Buffalo 1980 Visiting Professor, Lamont-Doherty Geological Observatory of Columbia University 1979 Research Scientist, Lamont-Doherty Geological Observatory of Columbia University 1970 Instructor, Associated Colleges of the Midwest summer school at Colorado College (Colorado Springs, CO), 1968 Assistant Geologist, Texas Gulf Sulfur, Lee Creek Mine (Aurora, NC) Professional Memberships & Activities I) Memberships American Association of Petroleum Geologists Geological Society of America II) Activities A.