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Southern Accent July 1953 - September 1954
Southern Adventist University KnowledgeExchange@Southern Southern Accent - Student Newspaper University Archives & Publications 1953 Southern Accent July 1953 - September 1954 Southern Missionary College Follow this and additional works at: https://knowledge.e.southern.edu/southern_accent Recommended Citation Southern Missionary College, "Southern Accent July 1953 - September 1954" (1953). Southern Accent - Student Newspaper. 33. https://knowledge.e.southern.edu/southern_accent/33 This Book is brought to you for free and open access by the University Archives & Publications at KnowledgeExchange@Southern. It has been accepted for inclusion in Southern Accent - Student Newspaper by an authorized administrator of KnowledgeExchange@Southern. For more information, please contact [email protected]. SOUTHERN msmm college UBRMV THE OUTH^^ ACCENT Souchern Missionary^ollege, Collegedale, Tennessee, July 3. 1953 o lleven SMC Graduates Ordained Young Men Ordained to M^ Kennedy Supervises Varied Gospel Ministry f. at Five Iprog am of Summer Activities Southern Union Camp Meetings fcht chapel scat Wednesday e c n ng br ngs these comn ents for once tadi week we ha\e chapel Many % r cd ch-ipel progran s ha e been '> p anned bj Dr R chard Hammill of the college rfOMffliililiins ! Thursday udenb and it d(-r e\en ng at the ball field br ngs torth to bu Id up cred cheers as a runner si des the hon e or as the umpire calls 6tr kc Three Student o^ram Comm ... and h ult) al ke mansh p of Profc share the thr II of a hon e run V d) hi\e out! ned Come th me -
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. Natural History
CHAPTER 1. NATURAL HISTORY CHAPTER 1. NATURAL HISTORY —THE WILDERNESS THAT GREETED THE FIRST SETTLERS The land one sees today traveling through northern Ohio took gone. Thus, some 14,000 years ago as the last glacier receded millions of years to form. We can see evidence of tropical sea into the Lake Erie basin, the first Native Americans arrived and reefs on the Lake Erie Islands and deep ocean sediments here in began to utilize the natural resources that these natural processes the cliffs of the Black River. Ohio was just south of the equator had produced. at that time, some 350 million years ago, and over the millennia The natural history of Sheffield encompasses all those natural has migrated northward to its present position. Mountain features and processes of the environment that greeted the Native building to the east eventually raised the sea floor from under Americans, and later the pioneers, when they first arrived in the waves and erosion by streams, and later glacial ice, began Sheffield. To be sure, the landscape was a magnificent wilderness to sculpture the land. At the same time plants and animals were to the settlers, but it needed to be “tamed” in order to support evolving and began to populate the new land once the ice was the newcomers. Ice formation on the shale bluff of the Black River north of Garfield Bridge (2005). 1 BICENTENNIAL HISTORY OF SHEFFIELD TOPOGRAPHY Regional Physiography The topography of an area is the configuration of the land Physiography refers to the physical features or landforms of surface, including its relief [vertical differences in elevation of a region. -
University of Michigan Radiocarbon Dates Xii H
[Ru)Ioc!RBo1, Vol.. 10, 1968, P. 61-114] UNIVERSITY OF MICHIGAN RADIOCARBON DATES XII H. R. CRANE and JAMES B. GRIFFIN The University of Michigan, Ann Arbor, Michigan The following is a list of dates obtained since the compilation of List XI in December 1965. The method is essentially the same as de- scribed in that list. Two C02-CS2 Geiger counter systems were used. Equipment and counting techniques have been described elsewhere (Crane, 1961). Dates and estimates of error in this list follow the practice recommended by the International Radiocarbon Dating Conferences of 1962 and 1965, in that (a) dates are computed on the basis of the Libby half-life, 5570 yr, (b) A.D. 1950 is used as the zero of the age scale, and (c) the errors quoted are the standard deviations obtained from the numbers of counts only. In previous Michigan date lists up to and in- cluding VII, we have quoted errors at least twice as great as the statisti- cal errors of counting, to take account of other errors in the over-all process. If the reader wishes to obtain a standard deviation figure which will allow ample room for the many sources of error in the dating process, we suggest doubling the figures that are given in this list. We wish to acknowledge the help of Patricia Dahlstrom in pre- paring chemical samples and David M. Griffin and Linda B. Halsey in preparing the descriptions. I. GEOLOGIC SAMPLES 9240 ± 1000 M-1291. Hosterman's Pit, Pennsylvania 7290 B.C. Charcoal from Hosterman's Pit (40° 53' 34" N Lat, 77° 26' 22" W Long), Centre Co., Pennsylvania. -
The Zoogeography of the Fishes of the Youghiogheny River System
The Zoogeographyof the Fishes of the Youghiogheny River System,Pennsylvania, Maryland and West Virginia MICHAEL L. HENDRICKS RMC-MuddyRun EcologicalLaboratory, P. 0. Box 10, Drumore,Pennsylvania 17518 JAY R. STAUFFER, JR. Universityof Maryland,Center for Environmentaland EstuarineStudies, Appalachian Environmental Laboratory,Frostburg 21532 CHARLES H. HOCUTT Universityof Maryland,Center for Environmentaland EstuarineStudies, Horn PointEnvironmental Laboratories,Cambridge 21613; andDepartment ofIchthyology and FisheriesScience, Rhodes University, Grahamstown,South Africa 6140 ABSTRACT: A total of 266 fish collectionswere made at 172 stationsin the YoughioghenyRiver drainage, the largest tributary to theMonongahela River. Collec- tionswere made usingseines, electrofishing gear, gillnets and trapnets. A comprehensiveliterature review yielded 99 speciesof fishesreported from the YoughioghenyRiver system.Six species collectedduring this survey(Amia calva, Carassiusauratus, Ericymba buccata, Notropis rubellus, Ictalurus catus and Fundulusdiaphanus) establishednew distributional records for the system, increasing the total to 105 species. Of thistotal, 78 specieswere verified either by our collections(57 species),museum records(10) or stockingrecords (11), whereas27 could not be verified.Of the 27 unverifiedspecies, 21 are expectedto occurand six are consideredmisidentifications or erroneousrecords. An additional24 speciesare expectedto have occurredhistorically in the Youghioghenyor have the potentialto do so based on theirdistribution in the -
Geology of Michigan and the Great Lakes
35133_Geo_Michigan_Cover.qxd 11/13/07 10:26 AM Page 1 “The Geology of Michigan and the Great Lakes” is written to augment any introductory earth science, environmental geology, geologic, or geographic course offering, and is designed to introduce students in Michigan and the Great Lakes to important regional geologic concepts and events. Although Michigan’s geologic past spans the Precambrian through the Holocene, much of the rock record, Pennsylvanian through Pliocene, is miss- ing. Glacial events during the Pleistocene removed these rocks. However, these same glacial events left behind a rich legacy of surficial deposits, various landscape features, lakes, and rivers. Michigan is one of the most scenic states in the nation, providing numerous recre- ational opportunities to inhabitants and visitors alike. Geology of the region has also played an important, and often controlling, role in the pattern of settlement and ongoing economic development of the state. Vital resources such as iron ore, copper, gypsum, salt, oil, and gas have greatly contributed to Michigan’s growth and industrial might. Ample supplies of high-quality water support a vibrant population and strong industrial base throughout the Great Lakes region. These water supplies are now becoming increasingly important in light of modern economic growth and population demands. This text introduces the student to the geology of Michigan and the Great Lakes region. It begins with the Precambrian basement terrains as they relate to plate tectonic events. It describes Paleozoic clastic and carbonate rocks, restricted basin salts, and Niagaran pinnacle reefs. Quaternary glacial events and the development of today’s modern landscapes are also discussed. -
Friendship Hill National Historic Site Geologic Resource Evaluation Report
National Park Service U.S. Department of the Interior Natural Resource Program Center Friendship Hill National Historic Site Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2008/022 THIS PAGE: Waterfall on Ice Pond Run, Friendship Hill NHP. ON THE COVER: Gallatin House, Friendship Hill NHP NPS Photos Friendship Hill National Historic Site Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2008/022 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 February 2008 U.S. Department of the Interior Washington, D.C. The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer- reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly- published newsletters. Views and conclusions in this report are those of the authors and do not necessarily reflect policies of the National Park Service. -
Description of the Foxburg and Clarion
DESCRIPTION OF THE FOXBURG AND CLARION By Eugene Wesley Shaw, Edwin F. Lines, and M. J. Munii.a INTRODUCTION. OUTLINE OF THE GEOGRAPHY AND GEOLOGY OF THE made up of sections of several preglacial valleys. As the APPALACHIAN PEOVINCE. LOCATION AND AREA. Foxburg and Clarion quadrangles lie within the area of SUBDIVISIONS. modified drainage, this feature will be described in detail under The Foxburg and Clarion quadrangles are in western Penn Topographically and geologically the Appalachian province the heading "Drainage," on page 2. sylvania, .mostly in Clarion County, but partly in Armstrong, is divided into two nearly equal parts by a line that follows In the southern half of the province not only do the Butler, and Venango counties. The quadrangles extend from the Allegheny Front through Pennsylvania, Maryland, and westward-flowing streams drain the Appalachian Plateau, but latitude 41° to 41° 15' and from longitude 79° 15' to 79° 45', West Virginia, and the eastern escarpment of the Cumberland many of them rise near the summits of the Blue Ridge and the line of 79° 30' being the boundary between them. (See Plateau across Virginia, Tennessee, Georgia, and Alabama. cross the Appalachian Valley as well. fig. 1.) Thus each quadrangle includes one-sixteenth of a In Pennsylvania this line passes in a northeast-southwest RELIEF, square degree of the earth's surface and measures approxi direction from southeastern New York to western Maryland, mately 17 miles from north to south by 13 miles from east to as shown in figure 2. The surface of the Appalachian Plateau is in reality made west, and the two quadrangles cover 450.12 square miles. -
LAKES of the HURON BASIN: THEIR RECORD of RUNOFF from the LAURENTIDE ICE Sheetq[
Quaterna~ ScienceReviews, Vol. 13, pp. 891-922, 1994. t Pergamon Copyright © 1995 Elsevier Science Ltd. Printed in Great Britain. All rights reserved. 0277-3791/94 $26.00 0277-3791 (94)00126-X LAKES OF THE HURON BASIN: THEIR RECORD OF RUNOFF FROM THE LAURENTIDE ICE SHEETq[ C.F. MICHAEL LEWIS,* THEODORE C. MOORE, JR,t~: DAVID K. REA, DAVID L. DETTMAN,$ ALISON M. SMITH§ and LARRY A. MAYERII *Geological Survey of Canada, Box 1006, Dartmouth, N.S., Canada B2 Y 4A2 tCenter for Great Lakes and Aquatic Sciences, University of Michigan, Ann Arbor, MI 48109, U.S.A. ::Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, U.S.A. §Department of Geology, Kent State University, Kent, 0H44242, U.S.A. IIDepartment of Geomatics and Survey Engineering, University of New Brunswick, Fredericton, N.B., Canada E3B 5A3 Abstract--The 189'000 km2 Hur°n basin is central in the catchment area °f the present Q S R Lanrentian Great Lakes that now drain via the St. Lawrence River to the North Atlantic Ocean. During deglaciation from 21-7.5 ka BP, and owing to the interactions of ice margin positions, crustal rebound and regional topography, this basin was much more widely connected hydrologi- cally, draining by various routes to the Gulf of Mexico and Atlantic Ocean, and receiving over- ~ flows from lakes impounded north and west of the Great Lakes-Hudson Bay drainage divide. /~ Early ice-marginal lakes formed by impoundment between the Laurentide Ice Sheet and the southern margin of the basin during recessions to interstadial positions at 15.5 and 13.2 ka BE In ~ ~i each of these recessions, lake drainage was initially southward to the Mississippi River and Gulf of ~ Mexico. -
Pleistbcene Lake Monongahela and the 'Carmichaels Formation'in
' j ;· ·) :; ' 1 'I ! I I ' I ! Pleistbcene Lake Monongahela and the 'Carmichaels. Formation'in' Southwest·- . Pennsylvania Pittsburgh Geological Society ·· - ~-~u F"te ld T np. l. \ · · ·. Saturday, May 2, 1998 Jack Donahue, University of Pittsburgh Brian Kirchner, University of Pittsburgh Sketch map of field trip route showing stops and road numbers. 179 r4e Sel.Ie Vernon Speers J\ 51 -- ·-· -· y Cree·k • ' Grays Mile Landing Introduction The Carmichaels Formation is a Pleistocene unit of lacustrine clay, silt, and sand matrix containing subangular to well-rounded, cobble- to boulder-sized, typically sandstone clasts. The Carmichaels was deposited at the bottom of Lake . Monongahela, a standing body of water formed by the glacial damming of the pre-Pleistocene Pittsburgh River system, the drainage of which included those of the modem Monongahela, Allegheny and Beaver Rivers (Figures la, 1b and 2). The unit occurs as a series of terraces along these rivers and their tributaries in western Pennsylvania and northern West Virginia. Carmichaels Formation terraces within the Monongahela River's drainage basin can be grouped by elevation into two distinct levels which have been interpreted as representing two different glacial damming events: -900-970 It representing illinoian glaciation, and -1000-1100 It pre-illinoian (Figures 3 and 4) (Marine, 1997; Jacobson, et al., 1988; White, 1896). These age constraints are tenuous, based primarily on correlation with outwash gravel trains and drift and on measurement of remanent paleomagnetism in Carmichaels sediments at widely scattered localities; Utey will most likely require revision based on the results of future studies. In addition, a lower terrace, not composed of the Carmichaels Formation, occurs at -920-970 It and is interpreted as being Wisconsinan in age (Marine, 1997; White, 1896). -
Contents List of Illustrations
STATE OF MICHIGAN Deltas..................................................................... 41 MICHIGAN GEOLOGICAL AND BIOLOGICAL SURVEY Distributaries.......................................................... 42 Lake deposits ........................................................ 42 Publication 12. Geological Series 9. CHAPTER IV. Physical Geography (Continued). .......44 GEOLOGICAL REPORT ON WAYNE COUNTY Surface drainage..........................................................44 BY Stream development ............................................. 44 W. H. SHERZER. Drainage systems.................................................. 45 Lakes, ponds, swamps and drains ........................ 54 PUBLISHED AS A PART OF THE ANNUAL REPORT OF THE Soils and subsoils. .......................................................55 BOARD OF GEOLOGICAL SURVEY FOR 1911. General characteristics.......................................... 55 LANSING, MICHIGAN Clay soils ............................................................... 55 WYNKOOP HALLENBECK CRAWFORD CO., STATE PRINTERS Sand and gravel soils ............................................ 56 1913 Loam...................................................................... 57 Silt.......................................................................... 58 Contents Muck ...................................................................... 58 Amelioration of soils .............................................. 59 CHAPTER I. Geographical and Historical CHAPTER V. Physical geography (Continued)..........61 -
Geoscenario Resources—Glaciers
Geoscenario Resources—Glaciers: Geologist Task Now that you have explored as a team the general story of how glaciers shaped the midwestern and northeastern United States, it is time for each of you to dive into more specialized information. The geologist focuses on regional features shaped by glaciers and how they formed. Add helpful details to your notes for Geoscenario Team Questions. Then work together and combine all the information to successfully present your story of glaciers. Questions for the Geologist to Consider • What geological features in this region were formed by glaciers? • What is the geological story of how the features were formed? Information Over a period of 10,000 years (100,000–110,000 years ago), the temperature dropped about 17°C, and the most recent glacial period began (evidence from oxygen ratios and foraminifera data). Around 20,000–35,000 years ago, the Laurentide (or Wisconsin) Ice Sheet covered most of Canada and a large portion of the northern United States. The massive ice sheet scraped away layers of earth materials as it pushed southward. Geologists look for clues today that help them determine the path and rate of glacial movement. The Great Lakes A glacier pushing poorly sorted glacial till in front of it. The glacial till forms a fill basins that the glaciers carved. In other areas, moraine. © iStockphoto/cotesebastien exposed rock displays scrape marks created by advancing ice carrying rocks and debris, called glacial till. Piles of glacial till form landmarks like moraines. Even huge boulders can be carried by glaciers. When geologists spot a boulder in an unexpected place, called an erratic, they often suspect a glacier carried it there.