Department of Geology TABLE of CONTENTS
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FLOOD of AUGUST 1935 Dtf MUSKINGUM RIVER Z < 5
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Water-Supply Paper 869 FLOOD OF AUGUST 1935 dtf MUSKINGUM RIVER o O z < 5 BY i ;> ^, C. V. YOUNGQUIST AND W. B. WITH SECTIONS ON THE ASSOCIATES METEOROLOGY AND HYDROLOOT ^ ;j . » BY * V WALDO E. SMITH AND A. K. SHOWALTEK 2. Prepared in cooperation with the * ^* FEDERAL EMERGENCY ADMINISTRAflCg^ OF PUBLIC WORKS ' -o j; UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1941 jFor sale by the Superintendent of Documents, Washington, D. G. - * * « Price 40 cents (paper) CONTENTS Pag« Abstract---.--_-_-__-__-___--______.-__-_---_---_-__-_--_-__-.-_._ I Introduction.______________________________________________________ 1 Administration and personnel---_______--_-_____-__--____________-__ 3 Acknowledgments ________-________-----_--__--__-_________________ 3 Geography _ ____________________________________________________ 6 Topography, drainage, and transportation________________________ 6 Rainfall...--_---.-__-------.-_--------__..---_-----------_---- 7 Population, industry, and mineral resources_---_-__--_________--__ 8 Flood control-___-_-___-__-_-__-____-_--_-_-__--_--__.____--_- S General features of the flood-_______________________________________ 9 Damage.-__-_______--____-__--__--__-_-____--_______-____--__ IT Meteorologic and hydrologic conditions, by Waldo E. Smith____________ 19 General features of the storm.___-____-__________---_____--__--_ 19 Records of precipitation._______________________________________ 21 Antecedent -
POINT PLEASANT 1774 Prelude to the American Revolution
POINT PLEASANT 1774 Prelude to the American Revolution JOHN F WINKLER ILLUSTRATED BY PETER DENNIS © Osprey Publishing • www.ospreypublishing.com CAMPAIGN 273 POINT PLEASANT 1774 Prelude to the American Revolution JOHN F WINKLER ILLUSTRATED BY PETER DENNIS Series editor Marcus Cowper © Osprey Publishing • www.ospreypublishing.com CONTENTS INTRODUCTION 5 The strategic situation The Appalachian frontier The Ohio Indians Lord Dunmore’s Virginia CHRONOLOGY 17 OPPOSING COMMANDERS 20 Virginia commanders Indian commanders OPPOSING ARMIES 25 Virginian forces Indian forces Orders of battle OPPOSING PLANS 34 Virginian plans Indian plans THE CAMPAIGN AND BATTLE 38 From Baker’s trading post to Wakatomica From Wakatomica to Point Pleasant The battle of Point Pleasant From Point Pleasant to Fort Gower THE AFTERMATH 89 THE BATTLEFIELD TODAY 93 FURTHER READING 94 INDEX 95 © Osprey Publishing • www.ospreypublishing.com 4 British North America in1774 British North NEWFOUNDLAND Lake Superior Quebec QUEBEC ISLAND OF NOVA ST JOHN SCOTIA Montreal Fort Michilimackinac Lake St Lawrence River MASSACHUSETTS Huron Lake Lake Ontario NEW Michigan Fort Niagara HAMPSHIRE Fort Detroit Lake Erie NEW YORK Boston MASSACHUSETTS RHODE ISLAND PENNSYLVANIA New York CONNECTICUT Philadelphia Pittsburgh NEW JERSEY MARYLAND Point Pleasant DELAWARE N St Louis Ohio River VANDALIA KENTUCKY Williamsburg LOUISIANA VIRGINIA ATLANTIC OCEAN NORTH CAROLINA Forts Cities and towns SOUTH Mississippi River CAROLINA Battlefields GEORGIA Political boundary Proposed or disputed area boundary -
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. -
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. -
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 -
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 -
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. -
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.................................................... -
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................................................... -
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. -
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). -
Note: Page Numbers in Italic Refer to Illustrations, Those in Bold Type Refer to Tables
Index Note: Page numbers in italic refer to illustrations, those in bold type refer to tables. Aachen-Midi Thrust 202, 203, 233, 235 Armorican affinities 132, 283 Acadian Armorican Massif 27, 29, 148, 390 basement 36 Armorican Terrane Assemblage 10, 13, 22 Orogeny 25 drift model 27-28 accommodation cycles 257, 265 magmatic rocks 75 accommodation space 265, 277 palaeolatitudes 28 acritarchs, Malopolska Massif 93 in Rheno-Hercynian Belt 42 advection, as heat source 378, 388 separation from Avalonia 49 African-European collision 22 tectonic m61ange 39 Air complex, palaeomagnetism 23, 25 Tepl/t-Barrandian Unit 44 Albersweiler Orthogneiss 40 terminology 132 Albtal Granite 48 Terrane Collage 132 alkali basalts 158 Ashgill, glacial deposits 28, 132, 133 allochthonous units, Rheno-Hercynian Belt 38 asthenosphere, upwelling 355, 376, 377 Alps asthenospheric source, metabasites 165 collisional orogeny 370 Attendorn-Elspe Syncline 241 see also Proto-Alps augen-gneiss 68 alteration, mineralogical 159 Avalon Terrane 87 Amazonian Craton 120, 122, 123, 147 Avalonia American Antarctic Ridge 167, 168, 170 and Amazonian Craton 120 Amorphognathus tvaerensis Zone 6 brachiopods 98 amphibolite facies metamorphism 41, 43, 67, 70 and Bronovistulian 110 Brunovistulian 106 collision with Armorica 298 Desnfi dome 179 collision with Baltica 52 MGCR 223 drift model 27 Saxo-Thuringia 283, 206 extent of 10 amphibolites, Bohemian Massif 156, 158 faunas 94 anatectic gneiss 45, 389 Gondwana derivation 22 anchimetamorphic facies 324 palaeolatitude 27 Anglo-Brabant Massif