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Chapter 1: Sequence Stratigraphy of the Glenshaw Formation
Martino, R. L., 2004, Sequence stratigraphy of the Glenshaw Formation (middle–late Pennsylvanian) in the central Appalachian basin, in J. C. Pashin and R. A. Gastaldo, eds., Sequence stratigraphy, paleoclimate, and tectonics of coal-bearing strata: AAPG Studies 1 in Geology 51, p. 1–28. Sequence Stratigraphy of the Glenshaw Formation (Middle–Late Pennsylvanian) in the Central Appalachian Basin Ronald L. Martino Department of Geology, Marshall University, Huntington, West Virginia, U.S.A. ABSTRACT he Glenshaw Formation consists predominantly of sandstones and mud- rocks with thin limestones and coals, which are thought to have accumu- T lated in alluvial, deltaic, and shallow-marine environments. Analysis of 87 Glenshaw outcrops from southern Ohio, eastern Kentucky, and southern West Vir- ginia has revealed widespread, well-developed paleosols. These paleosols are used, along with marine units and erosional disconformities, to develop a high-resolution sequence-statigraphic framework. The tops of the paleosols constitute boundaries for nine allocycles, which are interpreted as fifth-order depositional sequences. Allocycles in this framework correlate with similar allocycles described from the northern Appalachian basin. A sequence-stratigraphic model is proposed that provides a framework for in- terpreting facies architecture in terms of base-level dynamics linked to relative sea level changes. Lowered base level caused valley incision along drainage lines and sediment bypassing of interfluves, which led to development of well-drained paleo- sols. Rising base level produced valley filling by fluvioestuarine systems (lowstand systems tract/transgressive systems tract), whereas pedogenesis continued on inter- fluves. As drainage systems aggraded, the coastal plain water table rose, and in- terfluvial paleosols were onlapped by paludal and lacustrine deposits. -
Structural Geology of the Transylvania Fault Zone in Bedford County, Pennsylvania
University of Kentucky UKnowledge University of Kentucky Master's Theses Graduate School 2009 STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA Elizabeth Lauren Dodson University of Kentucky, [email protected] Right click to open a feedback form in a new tab to let us know how this document benefits ou.y Recommended Citation Dodson, Elizabeth Lauren, "STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA" (2009). University of Kentucky Master's Theses. 621. https://uknowledge.uky.edu/gradschool_theses/621 This Thesis is brought to you for free and open access by the Graduate School at UKnowledge. It has been accepted for inclusion in University of Kentucky Master's Theses by an authorized administrator of UKnowledge. For more information, please contact [email protected]. ABSTRACT OF THESIS STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA Transverse zones cross strike of thrust-belt structures as large-scale alignments of cross-strike structures. The Transylvania fault zone is a set of discontinuous right-lateral transverse faults striking at about 270º across Appalachian thrust-belt structures along 40º N latitude in Pennsylvania. Near Everett, Pennsylvania, the Breezewood fault terminates with the Ashcom thrust fault. The Everett Gap fault terminates westward with the Hartley thrust fault. Farther west, the Bedford fault extends westward to terminate against the Wills Mountain thrust fault. The rocks, deformed during the Alleghanian orogeny, are semi-independently deformed on opposite sides of the transverse fault, indicating fault movement during folding and thrusting. Palinspastic restorations of cross sections on either side of the fault zone are used to compare transverse fault displacement. -
Carboniferous Coal-Bed Gas Total Petroleum System
U.S. Geological Survey Open-File Report 2004-1272 Assessment of Appalachian Basin Oil and Gas Resources: Carboniferous Coal-bed Gas Total Petroleum System Robert C. Milici U.S. Geological Survey 956 National Center Reston, VA 20192 1 Table of Contents Abstract Introduction East Dunkard and West Dunkard Assessment units Introduction: Stratigraphy: Pottsville Formation Allegheny Group Conemaugh Group Monongahela Group Geologic Structure: Coalbed Methane Fields and Pools: Assessment Data: Coal as a source rock for CBM: Gas-In-Place Data Thermal Maturity Generation and Migration Coal as a reservoir for CBM: Porosity and Permeability Coal Bed Distribution Cumulative Coal Thickness Seals: Depth of Burial Water Production Cumulative Production Data: Pocahontas basin and Central Appalachian Shelf Assessment Units Introduction: Stratigraphy: Pocahontas Formation New River Formation Kanawha Formation 2 Lee Formation Norton Formation Gladeville Sandstone Wise Formation Harlan Formation Breathitt Formation Geologic Structure: Coalbed Methane Fields: Coal as a Source Rock for CBM Gas-in-Place Data Thermal Maturity Generation and Migration Coal as a Reservoir for CBM: Porosity and Permeability Coal Bed Distribution Cumulative Coal Thickness Seals: Depth of Burial Water Production Cumulative Production Data: Assessment Results: Appalachian Anthracite and Semi-Anthracite Assessment Unit: Pennsylvania Anthracite Introduction: Stratigraphy: Pottsville Formation Llewellyn Formation Geologic Structure: Coal as a Source Rock for CBM: Gas-In-Place-Data Thermal -
A Sequence Stratigraphic Synthesis of the Lower Pennsylvanian Pottsville Formation Encountered in Two Drill Cores in the Cahaba Synclinorium, Alabama
A sequence stratigraphic synthesis of the Lower Pennsylvanian Pottsville Formation encountered in two drill cores in the Cahaba synclinorium, Alabama by Sonnet Wilson Gomes A thesis submitted to the Graduate Faculty of Auburn University in partial fulfillment of the requirements for the Degree of Master of Science Auburn, Alabama December 8, 2012 Keywords: Pottsville Formation, Cahaba synclinorium, sequence stratigraphy, Alabama Copyright 2012 by Sonnet Wilson Gomes Approved by Ashraf Uddin, Chair, Professor of Geology Charles E. Savrda, Professor of Geology Willis E. Hames, Professor of Geology Jack C. Pashin, Director, EMD, Geological Survey of Alabama Abstract The Lower Pennsylvanian Pottsville Formation is a classic clastic wedge of the Appalachian mountain system composed of interbedded sandstone, siltstone, claystone, shale, and coal beds with orthoquartzitic conglomerate at the base. The formation developed in response to thrust and sediment loading on the convergent margin of the Laurussian craton during the Alleghanian orogeny. The greatest preserved thickness of Pennsylvanian strata, more than 2500 m (8000 ft), accumulated in the Cahaba and Coosa coalfields of the greater Black Warrior Basin. The Carboniferous coalfield, which hosts the Pottsville Formation in the greater Black Warrior Basin, occurs in large synclinoria separated by anticlinoria where Cambrian-Ordovician rocks are exposed at the surface. Eight lithofacies have been identified within two studied drill cores from the Cahaba basin on the basis of dominant rock types, color, grain size, and sedimentary structures. A transition from a tidal through delta-estuarine to fluvial environments has been identified with the aid of facies analysis. Conformable contacts indicate a gradual change in the depositional environments from delta front to the delta plain. -
Pennsylvanian, in CH Shultz Ed, the Geology of Pennsylvania
.... ~ SCALE 10 20 JO 40 501.11 i 'i I' "i' I 20 40 60 80 KM J SUSQUEHANNA ' \ -~~ '? I WAYNE r..~ \ -'\" tS: / ~ 1- Figure 10-1. Distribution of Pennsylvanian rocks at the surface (solid color) and in the subsurface (diagonal lines) (modified from Berg and others, 1980), and the location of coal fields in Pennsylvania (from Pennsylvania Geological Survey, 1992). Part II. Stratigraphy and Sedimentary Tectonics CHAPTER 10 PENNSYLVANIAN WILLIAM E. EDMUNDS INTRODUCTION Consulting Geologist The Pennsylvanian was originally named as a 263 Sassafras Street series within the Carboniferous System by H. S. Harrisburg, PA 17102 Williams (1891) for exposures in Pennsylvania and VIKTORAS W. SKEMA was later raised to a system by Chamberlin and Salis Bureau of Topographic and Geologic Survey bury (1905). It underlies about 35 percent of Pennsyl Department of Conservation and Natural vania, mostly in the Appalachian Plateaus physio Resources graphic province, but including important outliers else P. O. Box 8453 where (Figure 10-1). It is probable that Pennsylva Harrisburg, PA 17105 nian rocks originally covered the entire state, except in the southeastern source area. Pennsylvanian sedi NORMAN K. FLINT* ments were derived, principally, from southeastern University of Pittsburgh orogenic highlands along the present margin of the Department of Geology and Planetary Science North American plate. An important secondary source Pittsburgh, PA 15260 was the cratonic area to the north. Other possible sources were the Adirondack and Taconic highlands to the northeast. Pennsylvanian sedimentation took place in an elongate basin, aligned northeast to south west, receiving sediments from all directions except the west and southwest. -
Geologic Resources Inventory Ancillary Map Information Document
U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Directorate Geologic Resources Division Allegheny Portage Railroad National Historic Site and Johnstown Flood National Memorial GRI Ancillary Map Information Document Produced to accompany the Geologic Resources Inventory (GRI) Digital Geologic-GIS Data for Allegheny Portage Railroad National Historic Site and Johnstown Flood National Memorial alpo_jofl_geology.pdf Version: 5/11/2020 I Allegheny Portage Railroad National Historic Site and Johnstown Flood National Memorial Geologic Resources Inventory Map Document for Allegheny Portage Railroad National Historic Site and Johnstown Flood National Memorial Table of Contents Geologic Resourc..e..s.. .I.n..v..e..n..t.o...r.y.. .M...a..p.. .D...o..c..u..m...e...n..t............................................................................ 1 About the NPS Ge..o..l.o..g..i.c... .R..e..s..o..u...r.c..e..s.. .I.n..v..e..n...t.o..r.y.. .P...r.o..g...r.a..m............................................................... 3 GRI Digital Maps a..n...d.. .S..o..u...r.c..e.. .M...a..p.. .C...i.t.a..t.i.o...n..s.................................................................................. 5 Index Map .................................................................................................................................................................... 6 Digital Bedrock Geologic-GIS Map of Allegheny Portage Railroad National Historic Site, John..s..t..o..w...n.. .F..l.o..o...d.. .N...a..t.i.o..n..a..l. .M...e..m...o...r.i.a..l. .a..n..d... .V..i.c..i.n..i.t.y.................................................. 7 Map Unit Lis.t................................................................................................................................................................... 7 Map Unit De.s..c..r.i.p..t.io..n..s...................................................................................................................................................... 8 PNcc - Cas.s..e..l.m...a..n. -
U.S. Forest Service White Paper a Summary of the Groundwater
U.S. Forest Service White Paper A Summary of the Groundwater Resources of the Wayne National Forest Troy Thompson Eastern Region Regional Hydrogeologist August 15, 2012 A Summary of the Groundwater Resources of the Wayne National Forest SCOPE The purpose of this paper is to provide baseline hydrogeological information for assessing the potential groundwater impacts of any proposed activities on the Wayne National Forest (WNF), such as the development of tight shale formations (most notably the Utica Shale). A review of the overall risks to groundwater posed by all oil and gas activities, including tight shale formation development, and possible approaches for identifying, monitoring, and mitigating those impacts is provided as an attachment to the this paper. This review is based on a review of readily available published information on the geology and hydrogeology of the WNF area. The most significant references used are cited in this document. All conclusions are subject to change based on the discovery of new information. LAND STATUS The land within the general boundary of the Wayne National Forest within the Ohio counties comprising parts of the Athens District - Athens Unit (Athens, Hocking, Morgan, Perry, and Vinton), the Athens District - Marietta Unit (Monroe and Washington), and the Ironton District (Gallia, Jackson, Lawrence, and Scioto). SUMMARY AND CONCLUSIONS Summary of Groundwater Conditions on the Forest The essential characteristics of the groundwater system across the WNF are summarized in the bullet points below. The following sections provide more detailed information on the hydrogeology and related geology of the Forest. The geology and hydrogeology of the WNF will be fairly consistent across all districts and units. -
GB 15, Sedimentology and Provenance of Carboniferous And
*8,'(%22.12 6(',0(172/2*<$1'3529(1$1&( 2)&$5%21,)(5286$1'3(50,$1 52&.62)$7+(16&2817< 6287+($67(512+,2 E\ *UHJRU\&1DGRQ (OL]DEHWK+*LHUORZVNL.RUGHVFK DQG-RVHSK36PLWK 'HSDUWPHQWRI*HRORJLFDO6FLHQFHV2KLR8QLYHUVLW\ DIVISION OF GEOLOGICAL SURVEY 4383 FOUNTAIN SQUARE DRIVE COLUMBUS, OHIO 43224-1362 (614) 265-6576 (614) 447-1918 (FAX) e-mail: [email protected] World Wide Web: http://www.dnr.state.oh.us/odnr/geo_survey/ OHIO GEOLOGY ADVISORY COUNCIL Dr. E. Scott Bair, representing Hydrogeology Mr. Mark R. Rowland, representing Environmental Geology Ms. F. Lynn Kantner, representing At-Large Citizens Dr. Mark R. Boardman, representing Higher Education Mr. David Wilder, representing Coal Mr. William M. Rike, representing Oil and Gas Mr. Ronald M. Tipton, representing Industrial Minerals SCIENTIFIC AND TECHNICAL STAFF OF THE DIVISION OF GEOLOGICAL SURVEY ADMINISTRATION (614) 265-6988 Thomas M. Berg, MS, State Geologist and Division Chief Robert G. Van Horn, MS, Assistant State Geologist and Deputy Division Chief Dennis N. Hull, MS, Assistant State Geologist and Deputy Division Chief Michael C. Hansen, PhD, Senior Geologist, Ohio Geology Editor, and Geohazards OfÀ cer Janet H. Kramer, Fiscal OfÀ cer Billie Long, Fiscal Specialist Sharon L. Stone, AD, Executive Secretary BEDROCK GEOLOGY MAPPING GROUP (614) 265-6473 CARTOGRAPHY & EDITING GROUP (614) 265-6593 Edward Mac Swinford, MS, Geologist Supervisor Edward V. Kuehnle, BA, Cartographer Supervisor Glenn E. Larsen, MS, Geologist Merrianne Hackathorn, MS, Geologist and Editor Gregory A. Schumacher, MS, Geologist Ray O. Klingbeil, AD, Cartographer Douglas L. Shrake, MS, Geologist Robert L. Stewart, Cartographer Ernie R. -
Appendix C-1: Existing Conditions
Controlling the Source Appendix C. Opportunities Identification and Evaluation Process Support Documentation C-1. Existing Conditions Supporting Information C-1.1 Geology The ALCOSAN Service Area falls within the Appalachian Plateau Physiographic Province, in the Pittsburgh Low Plateau and Waynesburg Hills Sections. The geology formations underlying the Service Area are the Casselman Formation (Pcc), Monongahela Group (Pm), Waynesburg Formation (PPw), Allegheny Formation (Pa), Glenshaw Formation (Pcg), and the Washington Formation (Pw).2 • The Casselman Formation is characterized by a few locally persistent red beds, calcareous claystones, freshwater limestones, thin sandstones, shales, siltstones, and generally thin, economically insignificant coal beds. • The Monongahela Group consists of cyclic sequences of limestone, shale, sandstone, and coal in the Uniontown and Pittsburgh Formations. • The Waynesburg Formation is divided into upper, middle and lower members, and its rocks occur in cyclic sequences with sandstone overlying Waynesburg coal. • The Allegheny Formation is composed primarily of cyclic sequences of clay shale, claystone, siltstone, sandstone, limestone, and coal. Freshwater limestone beds (commonly less than five feet thick) or calcareous claystone with limestone nodules commonly underlie the coal beds in the upper third of the formation. • The Glenshaw Formation consists of repeated sequences of sandstone, siltstone, shale, claystone (including red beds), limestone, and coal. • The Washington Formation conformably overlies the Waynesburg Formation. It is divided into an upper limestone member, middle member, and lower limestone member, all of which have cyclic rock sequences. The Washington coal is at the base of the Washington Formation. Near the top of the Glenshaw Formation are the Pittsburgh Red Beds, which are a primary source in southwest Pennsylvania for landslides. -
Allegheny Portage Railroad
THE HISTORY AND GEOLOGY OF THE ALLEGHENY PORTAGE RAILROAD BLAIR AND CAMBRIA COUNTIES, PENNSYLVANIA May 11, 2002 Guidebook for the PITTSBURGH GEOLOGICAL SOCIETY Field Trip Saturday, May 11, 2002 THE HISTORY AND GEOLOGY OF THE ALLEGHENY PORTAGE RAILROAD, BLAIR AND CAMBRIA COUNTIES, PENNSYLVANIA Trip leader: John A. Harper, Pennsylvania Geological Survey For additional copies of this field trip guidebook, contact: Pittsburgh Geological Society PO Box 58172 Pittsburgh, PA 15209 TABLE OF CONTENTS Page Introduction .................................................................................................................................1 Historical Perspective .................................................................................................................2 The Pennsylvania Mainline Canal System .....................................................................2 A Tunnel Through The Mountain ...................................................................................5 The Advantage Of Railroads ..........................................................................................6 Construction (Finally!!!) .................................................................................................8 Railroad Bed .......................................................................................................9 Railroad Tracks ...................................................................................................9 Ropes .................................................................................................................10 -
FTG-9: What The
What the H!? Paleozoic Stratigraphy Exposed Regional Stratigraphy and Structure in the Central Appalachians from the Ordovician to the Pennsylvanian as seen in new outcrops along US 48 (“Corridor H”) and other locations Pre-Meeting Field Trip Guide for the 46th Annual Meeting Eastern Section of the American Association of Petroleum Geologists (ESAAPG) Morgantown, West Virginia September 24 and 25, 2017 Field Trip Leaders and Authors Paula J. Hunt1, Ronald R. McDowell1, B. Mitch Blake, Jr.1, Jaime Toro2, Philip A Dinterman1 1 West Virginia Geological and Economic Survey, 1 Mont Chateau Rd., Morgantown, WV 26508 2 Department of Geology and Geography, West Virginia University, PO Box 6300, Morgantown, WV 26506 CoverImages Top:Tonolowayroadcutforeground,quarrybackgroundalongUS48 Middle(lefttoright):SenecaRocks,“Dragon’sTongue,”PaleoseismitesinSpechtyKopfFormation (Dintermanforscale) Bottom(lefttoright):US48(“CorridorH”),OldReedsville/MartinsburgquarryonUS33,FieldTrip RouteonGeologicMap PhotosinthisreportweretakenbyWVGESpersonnelunlessnotedotherwise. West Virginia Geological and Economic Survey Mont Chateau Research Center 1 Mont Chateau Road • Morgantown, WV 26508-8079 304.594.2331 • fax: 304.594.2575 www.wvges.org • [email protected] 39q39’30” N, 79q50’57” W Suggested citation: Hunt, P.J., R.R. McDowell, B.M. Blake, Jr., J. Toro, and P.A. Dinterman, 2017, What the H!? Paleozoic Stratigraphy Exposed,Pre-Meeting Field Trip Guide for the 46th Annual Meeting, Eastern Section of the American Association of Petroleum Geologists -
Geology of the Pennsylvania Coal Regions
CHAPTER 2. GEOLOGY OF THE PENNSYLVANIA COAL REGIONS Roger J. Hornberger, Caroline M. Loop, Keith B. C. Brady, Nathan A. Houtz The geology of the Anthracite and Bituminous Coal Regions of Pennsylvania is fundamental to most of the contents of this book. Since most of the coal ash placement sites described in this book are in the anthracite coal fields, the geology of the Anthracite Region is emphasized. However, the significant differences and similarities between the anthracite and bituminous regions, in their regional-scale physiography and local-scale topography, geologic structure, stratigraphy and hydrogeology will be briefly discussed in this chapter. 2.1 PHYSIOGRAPHY AND TOPOGRAPHY Pennsylvania’s Anthracite Region is located in the Valley and Ridge Province of the Appalachian Mountains as shown on Figure 2.1. The Valley and Ridge Province and other provinces and sections of the Appalachian Highlands were described in Fenneman (1938) and delineated on a U.S. Geological Survey Map by Fenneman and Johnson (1946). The province extends for a distance of 1200 miles from the St. Lawrence Lowland to Alabama, according to Thornbury (1965) who calls it the Ridge and Valley Province. This province is generally divided into three sections: a northern section also known as the Hudson-Champlain section; a middle section reaching from the Delaware River to the New River in southern Virginia; and a southern section from southern Virginia to the end of the highlands in Alabama. The width of the Valley and Ridge Province ranges from about 20 miles in New York near the Hudson River to about 80 miles wide in central Pennsylvania between Williamsport and Harrisburg, according to Hunt (1974) and Thornbury (1965).