COMMONWEALTH of VIRGIN IA DEPARTMENT of CONSERVATION and ECONOMIC DEVELOPMENT DIVISION of MINERAL RESOURCES Jomes L
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Birds Rockingham County
BIRDS OF ROCKINGHAM COUNTY VIRGINIA Clair Mellinger, Editor Rockingham Bird Club o DC BIRDS OF ROCKINGHAM COUNTY VIRGINIA Clair Mellinger, Editor Rockingham Bird Club November 1998 TABLE OF CONTENTS FOREWORD AND ACKNOWLEDGEMENTS............................1 THE ENVIRONMENT....................................................................3 THE PEOPLE AND THE RECORDS........................................11 THE LOCATIONS........................................................................23 DEFINITIONS AND EXPLANATIONS......................................29 SPECIES ACCOUNTS...............................................................33 LITERATURE CITED................................................................ 113 INDEX...........................................................................................119 PHOTOGRAPHS OF THE AMERICAN GOLDFINCHES ON THE FRONT AND BACK COVER WERE GENEROUSLY PROVIDED BY JOHN TROTT. The American Goldfinch has been used as the emblem for the Rockingham Bird Club since the club’s establishment in 1973. Copyright by the Rockingham Bird Club November 1998 FOREWORD AND ACKNOWLEDGMENTS This book is the product and a publication of the Rockingham Bird Club. It is a compilation of many historical and more recent records of bird sightings in Rockingham County. The primary purpose of the book is to publish Rockingham County bird records that may otherwise be unavailable to the general public. We hope that these records will serve a variety of useful purposes. For example, we hope that it will be useful to new (and experienced) birders as a guide to when and where to look for certain species. Researchers may find records or leads to records of which they were unaware. The records may support or counterbalance ideas about the change in species distribution and abundance. It is primarily a reference book, but fifty years from now some persons may even find the book interesting to read. In the Records section we have listed some of the persons who contributed to this book. -
New River Geology
Wow! Did You Know... National Park Service Total length of the New River: 320 miles • U.S. Department of the Interior • Total size of the New River watershed: 6,965 square miles (encompasses 4,457,000 acres) New River Gorge National River • Number of dams on the New River: seven (Fields Dam in Mouth of Wilson, VA; Fries Mill Dam in Fries, VA; Byllesby Dam in Austinville, VA; Buck Dam in Carroll County, VA; Claytor Dam in Dublin, VA; Bluestone Dam in New River Geology: Hinton, WV; and Hawk’s Nest Dam in Ansted, WV) • Highest point: Snake Mountain, North Carolina at Ribbon Through Time 4,800 feet above sea level (south fork of the New River) • Lowest point: Gauley Bridge, West Virginia at 680 feet above sea level. At this point the New and Gauley Rivers join together to form the Kanawha River. • Length of New River in New River Gorge National River: 53 miles, established as a unit of the National Park Service in 1978 (encompasses over 70,000 acres) • American Heritage River: the entire New River received this national designation in 1998 • The New River drops 750 feet between Hinton and Gauley Bridge, West Virginia (around 11 feet per mile) • One of the widest sections of the river in New River Gorge National River: Sandstone Falls area, 1500 feet Stand at any overlook in the New River Gorge and • One of the narrowest sections of the river in New River look into the canyon. These panoramas of the gorge Gorge National River: Fayette Station rapid, 200 feet are where it best presents itself, where it reveals the • One of the deepest sections of the river in New River character of its natural sculpture and landscape. -
Geology of the Blue Heron Nature Preserve, Atlanta, Georgia
Geology of the Blue Heron Nature Preserve, Atlanta, Georgia By naturalist L. Scott Ranger There are two stories to tell about the geology of the Blue Heron Nature Preserve: the very small scale of rocks on the ground at the preserve; and, the very large scale of both time and space of the preserve and its place on the surface of planet earth. On the ground at the preserve… The entire property—and much of this part of North Atlanta—is located on a geologic formation mapped as the button schist (POb). Unlike most geologic formation names, this really isn’t a name, but simply a description of the kind of rock that is found here. It has been called this since the early twentieth century but became more formalized in 1966 with the publishing of Michael W. Higgin’s The Geology of the Brevard Lineament Near Atlanta, Georgia as Bulletin 77 of the now defunct Georgia Geological Survey. This map locates the Blue Heron Nature Preserve in its North Atlanta setting. National Park Service (NPS) Geologic Resources Inventory (GRI) program. 2012. Unpublished Digital Geologic Map of the Northern portion of Chattahoochee River National Recreation Area, Georgia (NPS, GRD, GRI, CHAT, CHTN digital map) adapted from U.S. Geological Survey Open-File Report Series digital map by Dicken et. al. (2005). National Park Service (NPS) Geologic Resources Inventory (GRI) program. Geospatial Dataset-2188723. https://irma.nps.gov/App/Reference/Profile/2188723 National Park Service (NPS) Geologic Resources Inventory (GRI) program. 2012. Unpublished Digital Geologic Map of the Southern portion of Chattahoochee River National Recreation Area, Georgia (NPS, GRD, GRI, CHAT, CHTS digital map) adapted from a U.S. -
Open-File Report No. 2008-02-18 Phase 2 Study Of
Maryland Department of Natural Resources Resource Assessment Service MARYLAND GEOLOGICAL SURVEY Jeffrey P. Halka, Acting Director OPEN-FILE REPORT NO. 2008-02-18 PHASE 2 STUDY OF THE AREA CONTRIBUTING GROUNDWATER TO THE SPRING SUPPLYING THE A.M. POWELL STATE FISH HATCHERY, WASHINGTON COUNTY, MARYLAND by Mark T. Duigon Prepared in cooperation with the Maryland Department of Natural Resources Fisheries Service 2009 CONVERSION FACTORS AND ABBREVIATIONS The following factors may be used to convert the inch-pound units published in this report to International System (SI) units. Multiply By To obtain inch (in.) 2.54 (exact) centimeter (cm) foot (ft) 0.3048 meter (m) mile (mi) 1.609 kilometer (km) square mile (mi2) 2.590 square kilometer (km2) gallon (gal) 3.785 liter (L) cubic feet per second (ft3/s) 0.02832 cubic meters per second (m3/s) million gallons per day (Mgal/d) 3785 cubic meters per day (m3/d) ii CONTENTS Page ABSTRACT ...................................................................................................................................... 1 INTRODUCTION ............................................................................................................................ 2 Purpose and scope ....................................................................................................................... 2 Acknowledgments ....................................................................................................................... 2 HYDROLOGY AND GROUNDWATER TRACING ................................................................... -
GEOLOGIC SUMMARY of the APPALACHIAN BASIN, with REFERENCE to the SUBSURFACE DISPOSAL of RADIOACTIVE WASTE SOLUTIONS by George W
TEI-791 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY" GEOLOGIC SUMMARY OF THE APPALACHIAN BASIN, WITH;REFERENCE TO THE SUBSURFACE DISPOSAL OF RADIOACTIVE WASTE SOLUTIONS* By George W. Colton June 1961 Report TEI-791 This report is preliminary and ha^;not been edited for conformity with G^logical Survey format and nomenclature. ?1 ^Prepared on behalf of the U. S. Atomic Energy Commission. CONTENTS Abstract* .......................... 5 Introduction. ........................ 7 Purpose of report. ................... 7 Organization of report .................. 7 Location and extent of area. .............. Q Acknowledgments. .................... 10 Geologic framework. ..................... 10 Depositional framework ................. 10 Structural framework .................. llj. Stratigraphy. ........................ 17 Late Precambrian stratified sequence .......... 17 Early Cambrian clastic sequence. ............ 18 Thickness and depth ................ 22 Cambrian-Ordovician carbonate sequence ......... 23 Thickness and depth . , ........... 35 Late Ordovician clastic sequence ............ 35 Thickness and depth ................ Mi- Early Silurian clastic sequence. ............ kk Thickness and depth ................ 51 Silurian-Devonian carbonate sequence .......... 52 Thickness and depth ................ 62 Devonian classic sequence. ............... 63 Thickness and depth ................ 69 Mississippian sequence ................. 70 Thickness and depth ................ 79 Pennsylvanian sequence ................. 79 Waste -
Lexington Quadrangle Virginia
COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY OF THE LEXINGTON QUADRANGLE VIRGINIA KENNETH F. BICK REPORT OF INVESTIGATIONS I VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stote Geologist CHARLOTTESVI LLE, VI RGI N IA 1960 COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY OF THE LEXINGTON QUADRANGLE VIRGINIA KENNETH F. BICK REPORT OF INVESTIGATIONS I VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stote Geologist CHARLOTTESVI LLE, VI RGI N IA 1960 Couuowwoer,rn op Vtncrwre DopenrupNr op Puncnesrs exo Supptv Rrculroxn 1960 DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond. Virginia MenvrN M. SurHnnr,eNn, Director BOARD Vrcron W. Stnwenr, Petersburg, Chairtnan G. Ar,vrn MessnNnunc, Hampton, Viee'Chairman A. Pr,urvrnr BmnNn, Orange C. S. Cenrnn, Bristol ANpnpw A. Fenr,pv, Danville WonrnrrvcroN FauLKNEn, Glasgow SvoNpv F. Slter,r,, Roanoke EnwrN H. Wrr,r,, Richmond Wrr,r,renr P. Wooor,nv. Norfolk CONTENTS Pece Abstract. '"*i"#:;;;;: . : ::: , : ::.:::::::::..::::::. :.::.::::::: ::,r Z Geography 8 Purpose. 4 Previous Work. Present Work and Acknowledgements. 5 Geologic Formations. 6 Introduction. 6 Precambrian System. 6 Pedlar formation 6 Precambrian and Cambrian Systems. 6 Discussion. 6 Swift Run formation 8 Catoctin greenstone. I Unieoiformation...... ......... I Hampton(Harpers)formation. .......... I Erwin (Antietam) quartzite. Cambrian System . I0 Shady (Tomstown) dolomite 10 Rome (Waynesboro) formation.... ll Elbrook formation. 12 Conococheague limestone. l3 Ordovician System. ......., 14 Chepultepeclimestone. .......... 14 Beekmantown formatron. 14 New Market limestone. 15 Lincolnshire limestone. 16 Edinburg formation. 16 Martinsburg shale... 17 SilurianSystem. ......... 18 Clinchsandstone..... .......... 18 Clinton formation. -
25Th Annual Report to the Community
Eastern West Virginia Community Foundation 25 1995–2020 25 YEARS LOVING AND SERVING OUR COMMUNITY Silver Anniversary Report to the Community What is the Eastern West Virginia Community Foundation? • We are a 501(c)(3) nonprofit organization with a collection of 25 charitable funds established by donors to improve the quality 1995–2020 of life in the Eastern Panhandle of West Virginia. • We receive charitable gifts, work with families, individuals, businesses, other nonprofits, attorneys and estate and financial planners to devise plans to ensure a donor’s charitable contributions are used to the fullest extent and TABLE OF CONTENTS for maximum benefit. Greetings ....................................................................................3 • We place those gifts into endowed funds, manage the assets 2020 Board of Directors .........................................................3 for long-term growth, and award grants and scholarships from 25 Years of History ..................................................................4 the investment gains. Legacy Society ..........................................................................6 Accolades and Awards ............................................................6 An Anniversary to Remember ...............................................7 • We offer several types of funds to help donors achieve their Money Matters ..........................................................................8 charitable goals while also meeting community needs. 2019 Financial Snapshot .........................................................8 -
Cave Development in Strata of Ordovician-And Silurian-Devonian- Age in Highland County, Virginia
Old Dominion University ODU Digital Commons OES Theses and Dissertations Ocean & Earth Sciences Summer 2007 Cave Development in Strata of Ordovician-and Silurian-Devonian- Age in Highland County, Virginia Carol Ann Peterson Old Dominion University Follow this and additional works at: https://digitalcommons.odu.edu/oeas_etds Part of the Geology Commons Recommended Citation Peterson, Carol A.. "Cave Development in Strata of Ordovician-and Silurian-Devonian-Age in Highland County, Virginia" (2007). Master of Science (MS), Thesis, Ocean & Earth Sciences, Old Dominion University, DOI: 10.25777/t7pt-2404 https://digitalcommons.odu.edu/oeas_etds/20 This Thesis is brought to you for free and open access by the Ocean & Earth Sciences at ODU Digital Commons. It has been accepted for inclusion in OES Theses and Dissertations by an authorized administrator of ODU Digital Commons. For more information, please contact [email protected]. CAVE DEVELOPMENT IN STRATA OF ORDOVICIAN- AND SILURIAN-DEVONIAN-AGE IN HIGHLAND COUNTY, VIRGINIA by Carol Ann Peterson B.S. August 2002, Old Dominion University A Thesis Submitted to the Faculty of Old Dominion University in Partial Fulfillment of tine Requirement for the Degree of MASTER OF SCIENCE GEOLOGY OLD DOMINION UNIVERSITY August 2007 Approved by: ;ar (Director) Dennis A. Darby (Membes Donald J. P. Swift (Member) limes F. Coble (Member) Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ABSTRACT CAVE DEVELOPMENT IN STRATA OF ORDOVICIAN- AND SILURIAN-DEVONIAN-AGE IN HIGHLAND COUNTY, VIRGINIA Carol Ann Peterson Old Dominion University, 2007 Director: Dr. G. Richard Whittecar Picturesque Highland County, Virginia, also known as "Virginia's Little Switzerland", is characterized by high mountains, tranquil rivers, and hundreds of caves. -
2Nd International Trilobite Conference (Brock University, St. Catharines, Ontario, August 22-24, 1997) ABSTRACTS
2nd International Trilobite Conference (Brock University, St. Catharines, Ontario, August 22-24, 1997) ABSTRACTS. Characters and Parsimony. Jonathan M. Adrain, Department of Palaeontology, The Natural History Museum, London SW7 5BD, United King- dom; Gregory D. Edgecombe, Centre for Evolutionary Research, Australian Museum, 6 College Street, Sydney South, New South Wales 2000, Australia Character analysis is the single most important element of any phylogenetic study. Characters are simply criteria for comparing homologous organismic parts between taxa. Homology of organismic parts in any phylogenetic study is an a priori assumption, founded upon topological similarity through some or all stages of ontogeny. Once homolo- gies have been suggested, characters are invented by specifying bases of comparison of organismic parts from taxon to taxon within the study group. Ideally, all variation in a single homology occurring within the study group should be accounted for. Comparisons are between attributes of homologous parts, (e.g., simple presence, size of some- thing, number of something), and these attributes are referred to as character states. Study taxa are assigned member- ship in one (or more, in the case of polymorphisms) character-state for each character in the analysis. A single char- acter now implies discrete groupings of taxa, but this in itself does not constitute a phylogeny. In order to suggest or convey phylogenetic information, the historical status of each character-state, and of the the group of taxa it sug- gests, must be evaluated. That is, in the case of any two states belonging to the same character, we need to discover whether one state is primitive (broadly speaking, ancestral) or derived (representative of an evolutionary innovation) relative to the other. -
View of Valley and Ridge Structures from ?:R Stop IX
GIJIDEBOOJ< TECTONICS AND. CAMBRIAN·ORDO'IICIAN STRATIGRAPHY CENTRAL APPALACHIANS OF PENNSYLVANIA. Pifftbutgh Geological Society with the Appalachian Geological Society Septembet, 1963 TECTONICS AND CAMBRIAN -ORDOVICIAN STRATIGRAPHY in the CENTRAL APPALACHIANS OF PENNSYLVANIA FIELD CONFERENCE SPONSORS Pittsburgh Geological Society Appalachian Geological Society September 19, 20, 21, 1963 CONTENTS Page Introduction 1 Acknowledgments 2 Cambro-Ordovician Stratigraphy of Central and South-Central 3 Pennsylvania by W. R. Wagner Fold Patterns and Continuous Deformation Mechanisms of the 13 Central Pennsylvania Folded Appalachians by R. P. Nickelsen Road Log 1st day: Bedford to State College 31 2nd day: State College to Hagerstown 65 3rd day: Hagerstown to Bedford 11.5 ILLUSTRATIONS Page Wagner paper: Figure 1. Stratigraphic cross-section of Upper-Cambrian 4 in central and south-central Pennsylvania Figure 2. Stratigraphic section of St.Paul-Beekmantown 6 rocks in central Pennsylvania and nearby Maryland Nickelsen paper: Figure 1. Geologic map of Pennsylvania 15 Figure 2. Structural lithic units and Size-Orders of folds 18 in central Pennsylvania Figure 3. Camera lucida sketches of cleavage and folds 23 Figure 4. Schematic drawing of rotational movements in 27 flexure folds Road Log: Figure 1. Route of Field Trip 30 Figure 2. Stratigraphic column for route of Field Trip 34 Figure 3. Cross-section of Martin, Miller and Rankey wells- 41 Stops I and II Figure 4. Map and cross-sections in sinking Valley area- 55 Stop III Figure 5. Panorama view of Valley and Ridge structures from ?:r Stop IX Figure 6. Camera lucida sketch of sedimentary features in ?6 contorted shale - Stop X Figure 7- Cleavage and bedding relationship at Stop XI ?9 Figure 8. -
“A People Who Have Not the Pride to Record Their History Will Not Long
STATE HISTORIC PRESERVATION OFFICE i “A people who have not the pride to record their History will not long have virtues to make History worth recording; and Introduction no people who At the rear of Old Main at Bethany College, the sun shines through are indifferent an arcade. This passageway is filled with students today, just as it was more than a hundred years ago, as shown in a c.1885 photograph. to their past During my several visits to this college, I have lingered here enjoying the light and the student activity. It reminds me that we are part of the past need hope to as well as today. People can connect to historic resources through their make their character and setting as well as the stories they tell and the memories they make. future great.” The National Register of Historic Places recognizes historic re- sources such as Old Main. In 2000, the State Historic Preservation Office Virgil A. Lewis, first published Historic West Virginia which provided brief descriptions noted historian of our state’s National Register listings. This second edition adds approx- Mason County, imately 265 new listings, including the Huntington home of Civil Rights West Virginia activist Memphis Tennessee Garrison, the New River Gorge Bridge, Camp Caesar in Webster County, Fort Mill Ridge in Hampshire County, the Ananias Pitsenbarger Farm in Pendleton County and the Nuttallburg Coal Mining Complex in Fayette County. Each reveals the richness of our past and celebrates the stories and accomplishments of our citizens. I hope you enjoy and learn from Historic West Virginia. -
Geologic Controls on the Morphology of the Chattooga River
Geologic Controls on the Morphology of the Chattooga River Scott E. Brame Geological Sciences Clemson University Clemson, SC 29634 and Robert D. Hatcher, Jr. Earth and Planetary Sciences and Science Alliance Center of Excellence University of Tennessee Knoxville, TN 37996–1410 Abstract The East fork of the Wild and Scenic Chattooga River drains the south side of Whiteside Mountain in North Carolina and flows in a predominant southwesterly direction following the predominant joint direction, and to a much lesser extent the foliation, until it turns sharply to the southeast becoming part of the Savannah River system and flows to the Atlantic Ocean. Paralleling the northeast to southwest trend is the Brevard fault zone and two other river systems, the Chauga River in South Carolina and the Chattahoochee River in Georgia. The Chauga follows a pattern similar to that of the Chattooga, turning sharply to the southeast after flowing predominantly to the southwest from its headwaters. The locations that mark the abrupt turn of the flow of the Chattooga and Chauga Rivers from the southwest to the southeast are likely the result of stream piracy as proposed by Acker and Hatcher. The upper sections of the Chattooga and Chauga represent an extension of the Dahlonega Plateau with a topographic surface that has a maximum elevation of approximately 1600 feet. The 1600’ surface is a piedmont surface at the base of the Blue Ridge. Differential erosion along northeast- and northwest-trending joint sets has exerted a powerful control on the development of the landscape. The northwest-trending joint sets have encouraged headward erosion and breaching of the Dahlonega Plateau surface resulting in stream capture of both the Chattooga and Chauga watersheds by the Savannah River system.