Lower Perm/An Rocks

Total Page:16

File Type:pdf, Size:1020Kb

Lower Perm/An Rocks COAL -BEARING UPPER PENNSYLVANIAN AND LOWER PERM/AN ROCKS WASHIN6TON AREA, PENNSYLVANIA Work done in cooperation with the Pennsylvania Bureau of Topographic and Geologic Survey GEOLOGICAL SURVEY PROFESSIONAL PAPER 621 Coal-Bearing Upper Pennsylvanian and Lower Permian Rocks, Washington Area, Pennsylvania Part 1. Lithofacies Part 2. Economic and Engineering Geology By HENRY L. BERRYHILL, JR., STANLEY P. SCHWEINFURTH, and BION H. KENT GEOLOGICAL SURVEY PROFESSIONAL PAPER 621 Work done in cooperation with the Pennsylvania Bureau of Topographic and Geologic Survey UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1971 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 73-608654 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract ................................................................................ 1 Stratigraphy Continued Introduction .......................................................................... 2 Pennsylvanian and Permian Systems Continued Purpose and scope of report .................................... 2 Dunkard Group ..... ........................ ................- 24 Previous work .............................................................. 3 Waynesburg Formation .............................. 24 Acknowledgments ........................................................ 3 Permian System ...................................... 25 Geography ............................................................................ 4 Dunkard Group ...................................................... 25 Location ........................................................................ 4 Washington Formation ................................ 25 Physiographic setting, topography, and drainage- 4 Greene Formation ........................................ 27 Quaternary System ........................ ............. - 29 Summary of sedimentation and paleogeography ............ 29 Part 1. Lithofacies Structure ................................................................. -. ..-. 34 Description of sedimentary rocks .................................... 5 General features .......................................................... 5 Part 2. Economic and Engineering Geology Sandstone and siltstone .............................................. 6 Economic geology .................................................................. 36 Mudstone and claystone.............................................. 11 Use of the special maps .............................................. 36 Limestone ...................................................................... 13 Commodity geology ...................................................... 36 Fossils ............................................................................ 17 Coal resources ................................... ........ i... 36 Lithofacies relations .................................................. 18 Pittsburgh coal bed ...................................... 37 Stratigraphy ........................................................................ 19 Waynesburg coal bed .................................... 38 Method of presentation .............................................. 19 Sandstone ........................................................ .. 38 History of nomenclature ............................................ 20 Limestone ................................................................ 39 Pennsylvanian System ................................................ 22 Mudstone and claystone ... .. .................. ........ 39 Conemaugh Formation ...................................... 22 Engineering geology ............................................ ................ 40 Monongahela Group ............................................ 22 Engineering properties of the rocks ........................ 40 Pittsburgh Formation ................................ 22 Movement of ground water ................................ ..... 42 Uniontown Formation ................................ 24 References cited .................................................................... 43 Pennsylvanian and Permian Systems .................... 24 Index .......................... -.. ..... ..... 45 ILLUSTRATIONS [Plates are in pocket] PLATE 1. Lithologic map of the Washington West and Washington East quadrangles, Washington area, Pennsylvania. 2. Lithologic map of the Amity quadrangle, Washington area, Pennsylvania. 3. Maps showing lithofacies and thickness of the members of the Pittsburgh and Uniontown Formations. 4. Maps showing lithofacies and thickness of the members of the Waynesburg and Washington Formations. 5-8. Maps showing thickness of: 5. Pittsburgh, Uniontown, Waynesburg, and Washington Formations. 6. Discrete sandstone in members of the Pittsburgh and Uniontown Formations. 7. Discrete sandstone in members of the Waynesburg and Washington Formations. 8. Washington, Waynesburg "A," Waynesburg, Uniontown, Sewickley, and Pittsburgh coal beds. Page FIGURE 1. Map showing location of the Washington area ....._.....................................-.................. ......................................... 4 2. Map showing area underlain by Upper Pennsylvanian and Lower Permian rocks, Appalachian basin .... 5 3. Sketch maps and cross sections showing classification of sandstone bodies by shape ........................................ 6 4. Photographs showing bedding characteristics of sandstone, siltstone, and limestone ........................................ 8 5. Sketches showing types of crossbedding in sandstone and siltstone ...................................................................... 10 6. Histograms showing vertical distribution of grain size in a typical sandstone-siltstone body .................... 11 7. Graph showing average composition of weathered sandstone .......................................... ........ .. ......... ....... 11 in IV CONTENTS Page FIGURE 8. Photograph showing limestone beds separated by thin layers of shaly claystone .. .................................._.... 12 9. Photograph showing laminae in limestone, probably formed by algae growing in mats ................................ 12 10. Photograph showing laminae in limestone, formed by ostracode shells arranged in layers ............................ 13 11. Photograph showing desiccation cracks in limestone ............ .......... ......_.................................. ......... ... ..... 14 12. Graph showing size distribution of insoluble residue from a limestone sample ................................................ 14 13. Photograph and sketch showing breccia-conglomerate structure in limestone .................................................... 15 14. Graph showing ratio of calcium to magnesium in 50 limestone samples ......................... .................................. 16 15. Diagram and chart showing lithofacies relations and summary of lithologic characteristics ........................ 19 16. Chart showing history and classification of the stratigraphic nomenclature for rocks in the Washington area .................................................................................................................. ... 21 17. Graphs showing average distribution of lithologic components in the Washington, Waynesburg, Uniontown, and Pittsburgh Formations .................................................................................... 23 18. Columnar Sections of the Greene Formation ........................................................................................ ....... ....... 28 19. Schematic maps showing regional paleogeographic relations during Late Pennsylvanian and Early Permian Time ......................................................................................................................................... 30 20. Schematic diagrams showing surface features of the Washington area during three consecutive stages of deposition in Late Pennsylvanian time ........................................................................ 32 21. Schematic diagrams showing surface features of the Washington area during three consecutive stages of deposition in Early Permian time .................................................................................. 33 22. Maps showing patterns of sandstone bodies ........................................-......................--. ............................................ 34 23. Maps showing thickness trends in the Waynesburg and Washington coal beds ............................................ 35 24. Graph showing results of weathering and compaction tests on a sample of silty mudstone .....-.... .............. 42 25. Schematic cross sections showing generalized movement of water in the subsurface relative to type of rock and topographic position of permeable and impermeable layers .......................................................... 43 TABLES Page TABLE 1. Stratigraphic and lithologic descriptions of rocks in the Pittsburgh and Uniontown Formations................In pocket 2. Stratigraphic and lithologic descriptions of rocks in the Waynesburg and Washington Formations1............In pocket 3. Estimated original and remaining resources of coal in the Pittsburgh coal bed and the Waynesburr coal bed in the Washington area, by quadrangle .................................................................................................................
Recommended publications
  • Geological Investigations in Ohio
    INFORMATION CIRCULAR NO. 21 GEOLOGICAL INVESTIGATIONS IN OHIO 1956 By Carolyn Farnsworth STATE OF OHIO C. William O'Neill, Governor DEPARTMENT OF NATURAL RESOURCES A. W. Marion, Director NATURAL RESOURCES COMMISSION Milton Ronsheim, Chairman John A. Slipher, Bryce Browning, Vice Chairman Secretary C. D. Blubaugh Dean L. L. Rummell Forrest G. Hall Dr. Myron T. Sturgeon A. W. Marion George Wenger DIVISION OF GEOLOGICAL SURVEY Ralph J. Bernhagen, Chief STATI OF OHIO DIPAlTMIMT 011 NATUlAL llSOUlCH DIVISION OF &EOLO&ICAL SURVEY INFORMATION CIRCULAR NO. 21 'GEOLOG·ICAL INVESTIGATIONS IN OHIO 1956 by CAROLYN FARNSWORTH COLUMBUS 1957 Blank Page CONTENTS Page Introduction 1 Project listing by author 2 Project listing by subject . 22 Economic geology 22 Aggregates . 22 Coal . • 22 Ground water 22 Iron .. 22 Oil and gas 22 Salt . 22 Sand and gravel 23 General .. 23 Geomorphology 23 Geophysics 23 Glacial geology 23 Mineralogy and petrology . 24 Clay .. 24 Coal . 24 Dolomite 24 Limestone. 24 Sandstone •• 24 Shale. 24 Till 25 Others 25 Paleontology. 25 Stratigraphy and sedimentation 26 Structural geology . 27 Miscellaneous . 27 Geographic distribution. 27 Statewide 27 Areal. \\ 28 County 29 Miscellaneous . 33 iii Blank Page I INTRODUCTION In September 1956, letters of inquiry and questionnaires were sent to all Ohio geologists on the mailing list of the Ohio Geological Survey, and to other persons who might be working on geological problems in Ohio. This publication has been compiled from the information contained on the returned forms. In most eases it is assumed that the projects listed herein will culminate in reports which will be available to the profession through scientific journals, government publications, or grad- uate school theses.
    [Show full text]
  • Strophomenide and Orthotetide Silurian Brachiopods from the Baltic Region, with Particular Reference to Lithuanian Boreholes
    Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes PETRAS MUSTEIKIS and L. ROBIN M. COCKS Musteikis, P. and Cocks, L.R.M. 2004. Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes. Acta Palaeontologica Polonica 49 (3): 455–482. Epeiric seas covered the east and west parts of the old craton of Baltica in the Silurian and brachiopods formed a major part of the benthic macrofauna throughout Silurian times (Llandovery to Pridoli). The orders Strophomenida and Orthotetida are conspicuous components of the brachiopod fauna, and thus the genera and species of the superfamilies Plec− tambonitoidea, Strophomenoidea, and Chilidiopsoidea, which occur in the Silurian of Baltica are reviewed and reidentified in turn, and their individual distributions are assessed within the numerous boreholes of the East Baltic, particularly Lithua− nia, and attributed to benthic assemblages. The commonest plectambonitoids are Eoplectodonta(Eoplectodonta)(6spe− cies), Leangella (2 species), and Jonesea (2 species); rarer forms include Aegiria and Eoplectodonta (Ygerodiscus), for which the new species E. (Y.) bella is erected from the Lithuanian Wenlock. Eight strophomenoid families occur; the rare Leptaenoideidae only in Gotland (Leptaenoidea, Liljevallia). Strophomenidae are represented by Katastrophomena (4 spe− cies), and Pentlandina (2 species); Bellimurina (Cyphomenoidea) is only from Oslo and Gotland. Rafinesquinidae include widespread Leptaena (at least 11 species) and Lepidoleptaena (2 species) with Scamnomena and Crassitestella known only from Gotland and Oslo. In the Amphistrophiidae Amphistrophia is widespread, and Eoamphistrophia, Eocymostrophia, and Mesodouvillina are rare. In the Leptostrophiidae Mesoleptostrophia, Brachyprion,andProtomegastrophia are com− mon, but Eomegastrophia, Eostropheodonta, Erinostrophia,andPalaeoleptostrophia are only recorded from the west in the Baltica Silurian.
    [Show full text]
  • Geology and Coal Resources of Belmont County, Ohio
    Geology and Coal Resources of Belmont County, Ohio By HENRY L. BERRYHILL, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 380 Prepared in cooperation with the Ohio Division of Geological Survey UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEW ART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington D.C. 20402 CONTENTS Page Stratigraphy Continued Abstract. __________________________________________ 1 Pennsylvanian rocks Continued Introduction _______________________________________ 1 Conemaugh formation Continued Purpose of the study- ___________________________ 1 Description of members Continued Preparation of the report ________________________ 2 Eastern Belmont County Continued Page Acknowledgments _______________________________ 2 Connellsville sandstone member __ 14 Previous workers _______________________________ 2 Lower Pittsburgh limestone mem­ Geography- ________________________________________ 3 ber __________________________ 14 Topography and drainage.-. _________________________ 3 Bellaire sandstone member. ___ 15 Structure, _ _____________________________________ 5 Upper Pittsburgh limestone mem­ Stratigraphy _ ______________________________________ 5 ber. _______________ __________ 15 General features. _______________________________ 5 Clay overlying the Upper Pitts­ Pennsylvanian rocks ___________________________ 6 Conemaugh formation. _ _____________________ 6 burgh limestone
    [Show full text]
  • Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha)
    Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) by Richard Kissel A thesis submitted in conformity with the requirements for the degree of doctor of philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto © Copyright by Richard Kissel 2010 Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) Richard Kissel Doctor of Philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto 2010 Abstract Based on dental, cranial, and postcranial anatomy, members of the Permo-Carboniferous clade Diadectidae are generally regarded as the earliest tetrapods capable of processing high-fiber plant material; presented here is a review of diadectid morphology, phylogeny, taxonomy, and paleozoogeography. Phylogenetic analyses support the monophyly of Diadectidae within Diadectomorpha, the sister-group to Amniota, with Limnoscelis as the sister-taxon to Tseajaia + Diadectidae. Analysis of diadectid interrelationships of all known taxa for which adequate specimens and information are known—the first of its kind conducted—positions Ambedus pusillus as the sister-taxon to all other forms, with Diadectes sanmiguelensis, Orobates pabsti, Desmatodon hesperis, Diadectes absitus, and (Diadectes sideropelicus + Diadectes tenuitectes + Diasparactus zenos) representing progressively more derived taxa in a series of nested clades. In light of these results, it is recommended herein that the species Diadectes sanmiguelensis be referred to the new genus
    [Show full text]
  • Historical Development and Problems Within the Pennsylvanian Nomenclature of Ohio.1
    Historical Development and Problems Within the Pennsylvanian Nomenclature of Ohio.1 GLENN E. LARSEN, OHIO Department of Natural Resources, Division of Geological Survey, Fountain Sq., Bldg. B, Columbus, OH 43224 ABSTRACT. An analysis of the historical development of the Pennsylvanian stratigraphic nomenclature, as used in Ohio, has helped define and clarify problems inherent in Ohio's stratigraphic nomenclature. Resolution of such problems facilitates further development of a useful stratigraphy and philosophy for mapping. Investigations of Pennsylvanian-age rocks in Ohio began as early as 1819- From 1858 to 1893, investigations by Newberry, I. C. White, and Orton established the stratigraphic framework upon which the present-day nomenclature is based. During the 1950s, the cyclothem concept was used to classify and correlate Pennsylvanian lithologic units. This classification led to a proliferation of stratigraphic terms, as almost every lithologic type was named and designated as a member of a cyclothem. By the early 1960s, cyclothems were considered invalid as a lithostratigraphic classification. Currently, Pennsylvanian nomenclature of Ohio, as used by the Ohio Division of Geological Survey, consists of four groups containing 123 named beds, with no formal formations or members. In accordance with the 1983 North American Stratigraphic code, the Ohio Division of Geological Survey considers all nomenclature below group rank as informal. OHIO J. SCI. 91 (1): 69-76, 1991 INTRODUCTION DISCUSSION Understanding the historical development of Pennsyl- The Early 1800s vanian stratigraphy in Ohio is important to the Ohio The earliest known references to Pennsylvanian-age Division of Geological Survey (OGS). Such an under- rocks in Ohio are found in Atwater's (1819) report on standing of Pennsylvanian stratigraphy helps define Belmont County, and an article by Granger (1821) on plant stratigraphic nomenclatural problems in order to make fossils collected near Zanesville, Muskingum County.
    [Show full text]
  • Presented by Title Before the Society, December £9, 1906)
    BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA Vol. 18, pp. 29-178 April 9,1907 CARBONIFEROUS OF THE APPALACHIAN BASIN * BY JOHN J. STEVENSON (Presented by title before the Society, December £9, 1906) CONTENTS Page Monongahela formation ............................................................................................... 30 Correlation ............................................................................................................... 30 East from the Alleghenies................................................................................... 45 Broad Top ........................................................................................................ 46 Maryland ......................................................................................................... 46 West from the Allegheny mountains, in Pennsylvania............................ 47 The First and Second bituminous basins............................................. 47 The Blairsville-Conncllsville basin............................................................ 60 The Greensburg basin.................................................................................. 64 The Lisbon-Irwin basin................................................................................ 54 The Waynesburg basin................................................................................ 58 The western basins in Pennsylvania....................................................... 60 The northern panhandle of W est Virginia....................................................
    [Show full text]
  • Summerfield and Woodsfield Quadrangles, Ohio
    DEPARTMENT OF THE INTERIOR ALBERT B. FALL, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Bulletin 720 ECONOMIC GEOLOGY OF THE SUMMERFIELD AND WOODSFIELD QUADRANGLES, OHIO WITH DESCRIPTIONS OF COAL AND OTHER MINERAL RESOURCES EXCEPT OIL AND GAS BY D. DALE CONDIT WASHINGTON GOVERNMENT PRINTING OFFICE 1923 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 30 CENTS PER COPY CONTENTS. Bibliography............................................................. 6 Introduction. ^........................................................... 7 i Abstract of report.............................................:....... 7 Field and office work................................................. 7 Acknowledgments.................................................... 8 Geography .................../...................................... ..... 8 Location............................................................ 8 Topographic features................................................... 9 Drainage........................................................ 9 Relief and land forms...............:........... '. ................. 10 Agricultural and commercial conditions................................ 11 Transportation facilities........................................... 11 Railroads.................................................... 11 New railroad routes........................................... 11 Highways...................................................
    [Show full text]
  • Section 4.2.2.2
    4.0 ENVIRONMENTAL IMPACT ANALYSIS 4.1 GEOLOGY 4.1.1 Existing Resources 4.1.1.1 Geologic Setting The proposed LX Project is located entirely in the Kanawha Section of the Appalachian Plateaus physiographic province. The Appalachian Plateaus consist primarily of Pennsylvanian and Permian layered deposits, with Quaternary Alluvium overlying most geologic formations (USGS, 2015a). Elevations along the project range from 455 feet to 1,500 feet above mean sea level (USGS, 2015b). Topography in the project area ranges from relatively flat-lying rocks and rolling hills to steep slopes, with a local relief of up to several hundred feet (West Virginia Geological and Economic Survey [WVGES], 2004a; Greene County Government, 2013; ODNR, 2014a). The proposed RXE Project Grayson CS is located in the region known as the Eastern Kentucky Coal Field (Kentucky Geological Survey [KGS], 2012a), in an area of Quaternary alluvium composed of sand, silt, clay, and gravel created by floodplain deposits of present day streams. The thickness of the alluvium ranges from 0 to 60 feet (Whittington and Ferm, 1967). The proposed RXE Project Means CS is located within the Lexington Plains Section of the Interior Low Plateaus physiographic province (USGS, 2015a), in a region known as The Knobs, that consists of hundreds of isolated, steep-sloping, cone-shaped hills (KGS, 2012b). The nearest knob, Kashs Knob, is approximately one-quarter mile north of the proposed compressor station site (USGS, 1975). The USDA Soil Conservation Survey (SCS) County soil survey information indicates there are restrictive layers (potentially shallow bedrock) within the upper five feet of the ground surface at both CS locations (USDA SCS, 1974 and 1983).
    [Show full text]
  • Detroit River Group in the Michigan Basin
    GEOLOGICAL SURVEY CIRCULAR 133 September 1951 DETROIT RIVER GROUP IN THE MICHIGAN BASIN By Kenneth K. Landes UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Washington, D. C. Free on application to the Geological Survey, Washington 25, D. C. CONTENTS Page Page Introduction............................ ^ Amherstburg formation................. 7 Nomenclature of the Detroit River Structural geology...................... 14 group................................ i Geologic history ....................... ^4 Detroit River group..................... 3 Economic geology...................... 19 Lucas formation....................... 3 Reference cited........................ 21 ILLUSTRATIONS Figure 1. Location of wells and cross sections used in the study .......................... ii 2. Correlation chart . ..................................... 2 3. Cross sections A-«kf to 3-G1 inclusive . ......................;.............. 4 4. Facies map of basal part of Dundee formation. ................................. 5 5. Aggregate thickness of salt beds in the Lucas formation. ........................ 8 6. Thickness map of Lucas formation. ........................................... 10 7. Thickness map of Amherstburg formation (including Sylvania sandstone member. 11 8. Lime stone/dolomite facies map of Amherstburg formation ...................... 13 9. Thickness of Sylvania sandstone member of Amherstburg formation.............. 15 10. Boundary of the Bois Blanc formation in southwestern Michigan.
    [Show full text]
  • The Geology of Switzerland Township, Monroe County, Ohio1
    THE OHIO JOURNAL OF SCIENCE VOL. LIU JANUARY, 1953 No. 1 THE GEOLOGY OF SWITZERLAND TOWNSHIP, MONROE COUNTY, OHIO1 THOMAS ARKLE, JR.2 Ohio Department of Natural Resources, Division of Geological Survey, Columbus 10 The aim of this report is twofold. It is primarily an attempt to summarize the geologic events that transpired in the past as interpreted from the exposed rocks in Switzerland Township, the Ohio River valley, and in the broader region of Ohio, West Virginia, and Pennsylvania. Secondly, this report summarizes the structural and economic geology of Switzerland Township and immediate environs. HISTORY AND ECONOMIC SETTING OF SWITZERLAND TOWNSHIP In April 1819, ten German and Swiss families embarked on a flat boat on the Aar River enroute to Berne, Switzerland, and thence on the Rhine to Antwerp, Belgium. After 48 days aboard the Eugenius, a French vessel bound for New York, they landed at Amboy, New Jersey. Six families purchased teams for the overland trek to Wheeling, West Virginia. At the mouth of Captina Creek at the present site of Powhatan Point, Ohio, they found two Pennsylvania Dutch men who informed them that there was plenty of government land in Monroe County, Ohio. On September 15, Father Tischer and part of his band continued down river 15 miles to Bare's Landing, Ohio Township, and the remainder settled in the hills above Powhatan Point. Switzerland Township, an area of about 28 square miles, was organized by the latter group January 1, 1827. These early settlers selected a small portion of the maturely dissected Allegheny Plateau (fig. 1) as the site for their new home.
    [Show full text]
  • Xerox University Microfilms
    information t o u s e r s This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1.The sign or "target” for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image. You will find a good image of the page in the adjacent frame. 3. When a map, drawing or chart, etc., was part of the material being photographed the photographer followed a definite method in "sectioning" the material. It is customary to begin photoing at the upper left hand corner of a large sheet and to continue photoing from left to right in equal sections with a small overlap. If necessary, sectioning is continued again - beginning below the first row and continuing on until complete. 4. The majority of usefs indicate that the textual content is of greatest value, however, a somewhat higher quality reproduction could be made from "photographs" if essential to the understanding of the dissertation.
    [Show full text]
  • Table of Contents Page 4.0 Characterization of Regional And
    Table of Contents Page 4.0 Characterization of Regional and Local Geology, Hydrogeology, and Hydrology 4-1 4.1 Physiography 4-1 4.2 Regional Geology 4-1 4.2.1 Pennsylvanian System 4-2 4.2.1.1 Conemaugh Group 4-2 4.2.1.2 Monongahela Group 4-2 4.2.2 Permian System – Dunkard Group 4-3 4.2.2.1 Waynesburg Formation 4-3 4.2.2.2 Washington Formation 4-4 4.2.2.3 Greene Formation 4-5 4.2.3 Quaternary System 4-6 4.2.4 Coal Resources 4-6 4.3 Structural Geology 4-7 4.3.1 Appalachian Plateaus Physiographic Province 4-7 4.3.2 Prototypical Area of the Pittsburgh Low Plateau Section 4-7 4.3.3 Joint Systems 4-8 4.3.4 Lineaments 4-8 4.3.5 Very Low Frequency Survey 4-9 4.4 Soils 4-10 4.4.1 Washington County Soil Survey 4-10 4.4.2 Colluvial Deposits 4-12 4.5 Hydrogeology 4-12 4.5.1 General 4-12 4.5.2 Aquifer Characteristics 4-13 4.5.3 Washington County Hydrogeology 4-14 4.6 Hydrology 4-14 4.6.1 Drainage Basin Characteristics 4-14 4.6.2 Upper Ohio – Wheeling Watershed 4-14 4.7 Climatology 4-15 4.0 Characterization of Regional and Local Geology, Hydrogeology, and Hydrology 4.1 Physiography The study area is situated within the Appalachian Plateaus Physiographic Province, a region that extends from Alabama into New York. The Appalachian Plateaus Physiographic Province in Pennsylvania is currently divided into seven sections based on characteristic geomorphic features unique to each.
    [Show full text]