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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. -
Parks and Open Space Plan (PDF)
February 2010 BRC-TAG-12-5-23 The contributions of the following agencies, groups, and individuals were vital to the successful development of this Comprehensive Recreation, Parks, and Open Space Plan. They are commended for their interest in the project and for the input they provided throughout the planning process. Venango County Commissioners Timothy S. Brooks, Chair Troy A. Wood, Vice-Chair Janet D. Beichner Venango County Regional Planning Commission Judith Downs, Executive Director Project Study Committee Marilyn Black, Oil Region Alliance, Heritage Development, Vice President Judy Downs, Venango County Regional Planning Commission, Executive Director Jacob Weiland, Oil Creek State Park, Park Manager Deb Frawley, Council on Greenways and Trails Mike Henderson, Oil Region Alliance, Project Manager Jim Holden, Allegheny Valley Trails Association, President Debb Kapp, Venango County Regional Planning Commission Steve Kosak, Charitable Trust, Consultant Lori Sloss, UMPC – Employee Health Cecile Stelter, DCNR – Dept. of Forestry, District Forester David Strickland, Two Mile Run Park Advisory Board Richard Mahalic, Two Mile Run Park Director This project was fi nanced, in part, by a grant from the Community Conservation Partnership Program, Keystone Recreation, Park, and Conservation Fund, under the administration of the Pennsylvania Department of Conservation and Natural Resources, Bureau of Recreation and Conservation. Additional funding was provided by: • Oil Region Alliance of Business, Industry, and Tourism • Edith C. Justus -
Geology of the Devonian Marcellus Shale—Valley and Ridge Province
Geology of the Devonian Marcellus Shale—Valley and Ridge Province, Virginia and West Virginia— A Field Trip Guidebook for the American Association of Petroleum Geologists Eastern Section Meeting, September 28–29, 2011 Open-File Report 2012–1194 U.S. Department of the Interior U.S. Geological Survey Geology of the Devonian Marcellus Shale—Valley and Ridge Province, Virginia and West Virginia— A Field Trip Guidebook for the American Association of Petroleum Geologists Eastern Section Meeting, September 28–29, 2011 By Catherine B. Enomoto1, James L. Coleman, Jr.1, John T. Haynes2, Steven J. Whitmeyer2, Ronald R. McDowell3, J. Eric Lewis3, Tyler P. Spear3, and Christopher S. Swezey1 1U.S. Geological Survey, Reston, VA 20192 2 James Madison University, Harrisonburg, VA 22807 3 West Virginia Geological and Economic Survey, Morgantown, WV 26508 Open-File Report 2012–1194 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Ken Salazar, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. -
A Comparative Study of the Mississippian Barnett Shale, Fort Worth Basin, and Devonian Marcellus Shale, Appalachian Basin
DOE/NETL-2011/1478 A Comparative Study of the Mississippian Barnett Shale, Fort Worth Basin, and Devonian Marcellus Shale, Appalachian Basin U.S. DEPARTMENT OF ENERGY DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe upon privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. ACKNOWLEDGMENTS The authors greatly thank Daniel J. Soeder (U.S. Department of Energy) who kindly reviewed the manuscript. His criticisms, suggestions, and support significantly improved the content, and we are deeply grateful. Cover. Top left: The Barnett Shale exposed on the Llano uplift near San Saba, Texas. Top right: The Marcellus Shale exposed in the Valley and Ridge Province near Keyser, West Virginia. Photographs by Kathy R. Bruner, U.S. Department of Energy (USDOE), National Energy Technology Laboratory (NETL). Bottom: Horizontal Marcellus Shale well in Greene County, Pennsylvania producing gas at 10 million cubic feet per day at about 3,000 pounds per square inch. -
Chapter 4 GEOLOGY
Chapter 4 GEOLOGY CHAPTER 4 GEOLOGY ...................................................................................................................................... 4‐1 4.1 INTRODUCTION ................................................................................................................................................ 4‐2 4.2 BLACK SHALES ................................................................................................................................................. 4‐3 4.3 UTICA SHALE ................................................................................................................................................... 4‐6 4.3.2 Thermal Maturity and Fairways ...................................................................................................... 4‐14 4.3.3 Potential for Gas Production ............................................................................................................ 4‐14 4.4 MARCELLUS FORMATION ................................................................................................................................. 4‐15 4.4.1 Total Organic Carbon ....................................................................................................................... 4‐17 4.4.2 Thermal Maturity and Fairways ...................................................................................................... 4‐17 4.4.3 Potential for Gas Production ........................................................................................................... -
Exhibit 5 Town of Barton Geology and Seismicity Report Sections
GEOLOGY AND SEISMICITY REPORT SNYDER E1-A WELL TOWN OF BARTON TIOGA COUNTY, NEW YORK Prepared for: Couch White, LLP 540 Broadway P.O. Box 22222 Albany, New York 12201 Prepared by: Continental Placer Inc. II Winners Circle Albany, New York 12205 July 25, 2017 Table of Contents 1.0 EXECUTIVE SUMMARY............................................................................................................. 1 2.0 INTRODUCTION ........................................................................................................................... 2 2.1 Depositional Sequences and General Stratigraphic Sequence ................................................ 2 2.1.1 Upper Devonian Lithologies ........................................................................................................ 4 2.1.2 Marcellus-Hamilton ..................................................................................................................... 4 2.1.3 Tristates-Onondaga ...................................................................................................................... 4 2.1.4 Helderberg .................................................................................................................................... 4 2.1.5 Oneida-Clinton-Salina ................................................................................................................. 4 2.1.6 Black River-Trenton-Utica-Frankfort .......................................................................................... 5 2.1.7 Potsdam-Beekmantown .............................................................................................................. -
Geologic Cross Section C–C' Through the Appalachian Basin from Erie
Geologic Cross Section C–C’ Through the Appalachian Basin From Erie County, North-Central Ohio, to the Valley and Ridge Province, Bedford County, South-Central Pennsylvania By Robert T. Ryder, Michael H. Trippi, Christopher S. Swezey, Robert D. Crangle, Jr., Rebecca S. Hope, Elisabeth L. Rowan, and Erika E. Lentz Scientific Investigations Map 3172 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 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 To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Ryder, R.T., Trippi, M.H., Swezey, C.S. Crangle, R.D., Jr., Hope, R.S., Rowan, E.L., and Lentz, E.E., 2012, Geologic cross section C–C’ through the Appalachian basin from Erie County, north-central Ohio, to the Valley and Ridge province, Bedford County, south-central Pennsylvania: U.S. Geological Survey Scientific Investigations Map 3172, 2 sheets, 70-p. -
Figure 3A. Major Geologic Formations in West Virginia. Allegheney And
82° 81° 80° 79° 78° EXPLANATION West Virginia county boundaries A West Virginia Geology by map unit Quaternary Modern Reservoirs Qal Alluvium Permian or Pennsylvanian Period LTP d Dunkard Group LTP c Conemaugh Group LTP m Monongahela Group 0 25 50 MILES LTP a Allegheny Formation PENNSYLVANIA LTP pv Pottsville Group 0 25 50 KILOMETERS LTP k Kanawha Formation 40° LTP nr New River Formation LTP p Pocahontas Formation Mississippian Period Mmc Mauch Chunk Group Mbp Bluestone and Princeton Formations Ce Obrr Omc Mh Hinton Formation Obps Dmn Bluefield Formation Dbh Otbr Mbf MARYLAND LTP pv Osp Mg Greenbrier Group Smc Axis of Obs Mmp Maccrady and Pocono, undivided Burning Springs LTP a Mmc St Ce Mmcc Maccrady Formation anticline LTP d Om Dh Cwy Mp Pocono Group Qal Dhs Ch Devonian Period Mp Dohl LTP c Dmu Middle and Upper Devonian, undivided Obps Cw Dhs Hampshire Formation LTP m Dmn OHIO Ct Dch Chemung Group Omc Obs Dch Dbh Dbh Brailler and Harrell, undivided Stw Cwy LTP pv Ca Db Brallier Formation Obrr Cc 39° CPCc Dh Harrell Shale St Dmb Millboro Shale Mmc Dhs Dmt Mahantango Formation Do LTP d Ojo Dm Marcellus Formation Dmn Onondaga Group Om Lower Devonian, undivided LTP k Dhl Dohl Do Oriskany Sandstone Dmt Ot Dhl Helderberg Group LTP m VIRGINIA Qal Obr Silurian Period Dch Smc Om Stw Tonoloway, Wills Creek, and Williamsport Formations LTP c Dmb Sct Lower Silurian, undivided LTP a Smc McKenzie Formation and Clinton Group Dhl Stw Ojo Mbf Db St Tuscarora Sandstone Ordovician Period Ojo Juniata and Oswego Formations Dohl Mg Om Martinsburg Formation LTP nr Otbr Ordovician--Trenton and Black River, undivided 38° Mmcc Ot Trenton Group LTP k WEST VIRGINIA Obr Black River Group Omc Ordovician, middle calcareous units Mp Db Osp St. -
CONNECTING to COLLECTIONS PENNSYLVANIA a Five-Year Preservation Plan for Pennsylvania PROJECT OVERVIEW
CONNECTING TO COLLECTIONS PENNSYLVANIA a five-year preservation plan for Pennsylvania PROJECT OVERVIEW Imagining Our Future: Preserving Pennsylvania’s Collections, published in August 2009, includes an in-depth analysis of conditions and needs at Pennsylvania’s collecting institutions, a detailed preservation plan to improve collections care throughout the state, and a five-year implementation timetable (2010-2015). The analysis concludes that many of Pennsylvania’s most important historic holdings must be considered at risk. Millions of items comprise these collections, and the financial resources available to care for them are limited and shrinking. Pennsylvania is a state vibrant with world-class art museums, libraries, historic sites. Arts and culture play a substantial role in creating business, jobs, and bringing revenue into the state and stewardship of its artifacts is too important —to the state, to the people, to the history of country—to be ignored. This call to action is a rallying cry for all future generations of Pennsylvanians. With generous support from the Institute of Museum and Library Services, and in close partnership with three leading preservation organizations, the Pennsylvania Historical and Museum Commission (PHMC), the Pennsylvania Federation of Museums and Historical Organizations (PFMHO), and LYRASIS, the Conservation Center for Arts & Historic Artifacts organized and led the assessment and planning process. The project was capably guided by a Task Force with representatives from the Office of (PA) Commonwealth Libraries, the Western Pennsylvania Museum Council, the Pennsylvania Caucus of the Mid- Atlantic Regional Archives Conference, Pennsylvania State University, the Philadelphia Area Consortium of Special Collections Libraries, the University of Pittsburgh, and Carnegie Mellon University. -
Late Devonian and Early Mississippian Distal Basin-Margin Sedimentation of Northern Ohio1
Late Devonian and Early Mississippian Distal Basin-Margin Sedimentation of Northern Ohio1 THOMAS L. LEWIS, Department of Geological Sciences, Cleveland State University, Cleveland, OH 44115 ABSTRACT. Clastic sediments, derived from southeastern, eastern and northeastern sources, prograded west- ward into a shallow basin at the northwestern margin of the Appalachian Basin in Late Devonian and Early Mississippian time. The western and northwestern boundary of the basin was the submerged Cincinnati Arch. The marine clastic wedges provided a northwest paleoslope and a distal, gentle shelf-edge margin that controlled directional emplacement of coarse elastics. Rising sea levels coupled with differences in sedimen- tation rates and localized soft-sediment deformation within the basin help explain some features of the Bedford and Berea Formations. The presence of sand-filled mudcracks and flat-topped symmetrical ripple marks in the Berea Formation attest to very shallow water deposition and local subaerial exposure at the time of emplacement of part of the formation. Absence of thick, channel-form deposits eastward suggests loss of section during emergence. OHIO J. SCI. 88 (1): 23-39, 1988 INTRODUCTION The Bedford Formation (Newberry 1870) is the most The Ohio Shale, Bedford, and Berea Formations of lithologically varied formation of the group. It is com- northern Ohio are clastic units which record prograda- prised of gray and red mudshales, siltstone, and very tional and transgressional events during Late Devonian fine-grained sandstone. The Bedford Formation thins and Early Mississippian time. The sequence of sediments both to the east and west and reaches its maximum is characterized by (1) gray mudshale, clayshale, siltstone, thickness in the Cleveland area. -
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 -
University of Michigan University Library
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY , THE UNIVERSITY OF MICHIGAN VOL. XWI, No. 11, pp. 241-263 (2 pk., 5 figs.) OCTOBER9, 1962 A MISSISSIPPIAN FLORA FROM NORTHEASTERN UTAH AND ITS FAUNAL AND STRATIGRAPHIC RELATIONS BY CHESTER A. ARNOLD and WALTER SADLICK Published with aid from the Edward Pulteney Wright and Jean Davies Wright Expendable Trust Fund MUSEUM OF PfiEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Director: LEWISB. KELLUM The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan. VOLS.11-XV. Parts of volumes may be obtained if available. VOLUMEXVI 1. Two Late Pleistocene Faunas from Southwestern Kansas, by Claude W. Hibbard and Dwight W. Taylor. Pages 1-223, with 16 plates. 2. North American Genera of the Devonian Rugose Coral Family Digonophylli- dae, by Erwin C. Stumm. Pages 225-243, with 6 plates. 3. Notes on Jaekelocystis hartleyi and Pseudocrinjtes gordoni, two Rhombi- feran Cystoids Described by Charles Schuchert in 1903, by Robert V. Kesling. Pages 245-273, with 8 plates. 4. Corals of the Traverse Group of Michigan. Part VI, Cladopora, Striatopora, and Thamnopora, by Erwin C.