1 Dr. Bernhard Peucker-Ehrenbrink
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution
Graduate Theses, Dissertations, and Problem Reports 2020 Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution Mark D. Swift West Virginia University, [email protected] Follow this and additional works at: https://researchrepository.wvu.edu/etd Part of the Geomorphology Commons Recommended Citation Swift, Mark D., "Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution" (2020). Graduate Theses, Dissertations, and Problem Reports. 7542. https://researchrepository.wvu.edu/etd/7542 This Thesis is protected by copyright and/or related rights. It has been brought to you by the The Research Repository @ WVU with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you must obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in WVU Graduate Theses, Dissertations, and Problem Reports collection by an authorized administrator of The Research Repository @ WVU. For more information, please contact [email protected]. Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution Mark D. Swift Thesis Submitted to the Eberly College of Arts and Sciences at West Virginia University in partial fulfillment of the requirements for the degree of Master of Arts in Geography Jamison Conley, Ph.D., Co-Chair J. Steven Kite, Ph.D., Co-Chair Nicolas Zegre, Ph.D. Department of Geology and Geography Morgantown, West Virginia 2020 Keywords: landscape evolution, knickzone, southwest Pennsylvania Copyright 2020 Mark D. -
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. -
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 -
DEPT. of EARTH SCIENCES B.Sc. Theses – by Author (Page 1 of 17)
BROCK UNIVERSITY – DEPT. OF EARTH SCIENCES B.Sc. Theses – by Author (page 1 of 17) Abu Hassan, R. Composition of Glacial and Post-Glacial Sediments in 20 Mile Creek, near Jordan Harbour, 1986. Aichele, S. Sub-watershed Study of the Upper Twelve Mile Creek: background conditions of stream water quality and chemistry, 2005. Ainslie, A. Volcanism and Hydrothermal Activity - McAras Brook, Nova Scotia, 1986. Ainsworth, B.H. The Sedimentation and Stratigraphy of the Walkerton Clay Banks, 1978. Allen, J. Stratigraphy and Sedimentology of the Dundee Member, Sarnia-Lambton Townships, Southern Ontario, Canada, 1988. Alley, D. Rock Particle Transport Distances in the Norwood Esker , 1972. Alther, G. The Effects of a Farmyard on the Geochemistry of Nearby Streams, 1973. Anderson, M. Structure, Petrography and Chemistry of A Zones Migmatite Complex, Bancroft Region, Ontario: Relationship to Uraniferous Pegmatites, 1981. Anderson, R.J. Environmental Effects on an Emanometric Survey, 1977. Arbour, J. Determination of the Runoff Response Functions for the Soper Creek Basin, Ontario, 1973. Artinian, D. J. A Petrological and Geochemical Study of the Catherine Sills: Catherine TWP. Timiskaming District, Ontario, 1980. Atherton, P.G. Hydrology and Sediment Distribution in the Fifteen, Sixteen and Twenty Mile Creeks, 1975. Atherton, P.J. Some Engineering Properties of Three Glacio-Lacustrine Deposits in the Niagara Peninsula , 1972. Atkinson, D. A Textural and Petrological Study of Igneous Rocks of Uncertain Origin from the Adel Lake - Klob Lake Area, Northern Ontario, 1985. Atkinson, J. Petrofabric Analysis Using the Quantimet Image Analysis Computer, 1972. Axtmann, M. Interpretation of Point-Dilution Experiments in a single fracture involving a new technique using a Conductivity Electrode, 1996. -
Synoptic Taxonomy of Major Fossil Groups
APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida -
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. -
Distribution of Cogenetic Iron and Clay Deposits in the Central Appalachian Region
DISTRIBUTION OF COGENETIC IRON AND CLAY DEPOSITS IN THE CENTRAL APPALACHIAN REGION by Mary Karandosovski McGuire B.S. Geology, The Pennsylvania State University, 1973 Submitted to the Graduate Faculty of Kenneth P. Dietrich School of Arts and Sciences in partial fulfillment of the requirements for the degree of Master of Science University of Pittsburgh 2012 UNIVERSITY OF PITTSBURGH DIETRICH SCHOOL OF ARTS AND SCIENCES This thesis was presented by Mary Karandosovski McGuire It was defended on March 30, 2012 and approved by Daniel Bain, Associate Professor, Faculty Charles Jones, Lecturer, Faculty Thesis Director: Thomas H. Anderson, Professor Emeritus, Faculty ii Copyright © by Mary K. McGuire 2012 iii DISTRIBUTION OF COGENETIC IRON AND CLAY DEPOSITS IN THE CENTRAL APPALACHIAN REGION Mary K. McGuire, M.S. University of Pittsburgh, 2012 Maps of more than 500 abandoned iron mines, 350 early iron furnaces, and numerous clay mines in the central part of the Appalachian region reveal the distribution and close association of siderite-limonite bearing ores and clay deposits. The deposits crop out from Lancaster County, Pennsylvania to Scioto County, Ohio, a distance of more than 300 miles. The geologic settings of the deposits are diverse. In the Valley and Ridge Province and Piedmont Province, mineralization follows structures such as major sub-horizontal thrust faults (e.g. Martic) and steep thrust faults, (e. g. Path Valley), that juxtapose carbonate units against other rocks. Carbonate units within the Plateau Province also contain economic deposits of iron ores and clay. The ores are commonly siderite and limonite principally in the form of nodules and other irregular masses in clayey, calcareous beds. -
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).