Chapter 1. Natural History
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Land Resource Regions and Major Land Resource Areas in New York
R L NS Land Resource Regions and Major Land Resource Areas in New York State Land Resource Regions and Major Land Resource Areas of the United States, the Caribbean, and the Pacific Basin MLRA Explorer Custom Report L - Lake State Fruit, Truck Crop, and Dairy Region 101 - Ontario-Erie Plain and Finger Lakes Region M - Central Feed Grains and Livestock Region 111E - Indiana and Ohio Till Plain, Eastern Part 111B - Indiana and Ohio Till Plain, Northeastern Part R - Northeastern Forage and Forest Region 144B - New England and Eastern New York Upland, Northern Part 144A - New England and Eastern New York Upland, Southern Part 143 - Northeastern Mountains 142 - St. Lawrence-Champlain Plain 141 - Tughill Plateau 140 - Glaciated Allegheny Plateau and Catskill Mountains 139 - Lake Erie Glaciated Plateau Major Land Resource Regions Custom Report Page 1 Data Source: USDA Agriculture Handbook 296 (2006) 03/26/08 http://soils.usda.gov/MLRAExplorer L - Lake State Fruit, Truck Crop, and Dairy Region Figure L-1: Location of Land Resource Region L LRR Overview This region (shown in fig. L-1) is in Michigan (59 percent), New York (22 percent), Ohio (10 percent), Indiana (8 percent), and Illinois (1 percent). A very small part is in Pennsylvania. The region makes up 45,715 square miles (118,460 square kilometers). Typically, the land surface is a nearly level to gently sloping glaciated plain (fig. L-2). The average annual precipitation is typically 30 to 41 inches (760 to 1,040 millimeters), but it is 61 inches (1,550 millimeters) in the part of the region east of Lake Erie. -
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 -
Lorain, Ohio: a Study in Urban Geography*
THE OHIO JOURNAL OF SCIENCE VOL. XXXV MAY, 1935 No. 3 LORAIN, OHIO: A STUDY IN URBAN GEOGRAPHY* R. B. FROST, Oberlin College TABLE OF CONTENTS PAGE INTRODUCTION 140 PART I. THE NATURAL ENVIRONMENT A. REGIONAL ASPECTS 1. Lake Erie and the Great Lakes Chain 142 2. The Lake Plain 143 (a) Geological Section 3. Appalachian Plateau 145 (a) Northern Glaciated Section (b) Unglaciated Section 4. Climate and Aboriginal Forest Cover 146 B. SITE CHARACTERISTICS 1. Black River and its Estuary 148 2. Lake Erie Shoreline 150 PART II. SEQUENT STAGES OF HUMAN OCCUPANCE (1755-1894) A. THE LANDSCAPE DURING THE INDIAN PERIOD 1. Indian Occupance 151 2. Indian Removal 152 B. THE LANDSCAPE DURING THE PIONEER PERIOD 1. Interim Period 153 2. Village Birth 154 3. Pioneer Developments 155 C. LANDSCAPE DURING THE PERIOD OF GROWTH 1. Agri-functional Character of the Village 158 2. Durand Survey 159 3. Village Extensions 160 4. Population Increase 160 D. A DECADENT VILLAGE 1. Effects of Railroad Expansion on Charleston 161 2. Decline of Population 162 3. Trade Decline 162 4. Persistence of Certain Industries 164 *Publication of this paper is made possible by a grant-in-aid from the trustees of the Research Fund of the Ohio Academy of Science. 139 140 R. B. FROST Vol. XXXV E. THE LANDSCAPE OF THE EARLY INDUSTRIAL PERIOD: A REVIVAL 1. Functional Changes 166 PART III. MODERN LANDSCAPE (1894-1932) A. RECENT GROWTH AND EXTENSION OF LORAIN 1. Landscape Characteristics 173 2. Present Plan 176 B. ELEMENTS OF THE CULTURAL LANDSCAPE 1. Heavy Industrial 182 2. -
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. -
Middle Devonian Formations in the Subsurface of Northwestern Ohio
STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 SCIENTIFIC AND TECHNICAL STAFF OF THE OHIO DIVISION OF GEOLOGICAL SURVEY ADMINISTRATIVE SECTION Horace R. Collins, State Geologist and Di v ision Chief David K. Webb, Jr., Geologist and Assistant Chief Eleanor J. Hyle, Secretary Jean S. Brown, Geologist and Editor Pauline Smyth, Geologist Betty B. Baber, Geologist REGIONAL GEOLOGY SECTION SUBSURFACE GEOLOGY SECTION Richard A. Struble, Geologist and Section Head William J. Buschman, Jr., Geologist and Section Head Richard M. Delong, Geologist Michael J. Clifford, Geologist G. William Kalb, Geochemist Adriaan J anssens, Geologist Douglas L. Kohout, Geologis t Frederick B. Safford, Geologist David A. Stith, Geologist Jam es Wooten, Geologist Aide Joel D. Vormelker, Geologist Aide Barbara J. Adams, Clerk· Typist B. Margalene Crammer, Clerk PUBLICATIONS SECTION LAKE ERIE SECTION Harold J. Fl inc, Cartographer and Section Head Charles E. Herdendorf, Geologist and Sectwn Head James A. Brown, Cartographer Lawrence L. Braidech, Geologist Donald R. Camburn, Cartovapher Walter R. Lemke, Boat Captain Philip J. Celnar, Cartographer David B. Gruet, Geologist Aide Jean J. Miller, Photocopy Composer Jean R. Ludwig, Clerk- Typist STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 GEOLOGY SERVES OHIO CONTENTS Page Introduction . 1 Previous investigations .. .. .. .. .. .. .. .. .. 1 Study methods . 4 Detroit River Group . .. .. .. ... .. ... .. .. .. .. .. .. .. ... .. 6 Sylvania Sandstone .......................... -
LAND by the LAKES Nearshore Terrestrial Ecosystems
State of the Lakes Ecosystem Conference 1996 Background Paper THE LAND BY THE LAKES Nearshore Terrestrial Ecosystems Ron Reid Bobolink Enterprises Washago, Ontario Canada Karen Holland U.S. Environmental Protection Agency Chicago, Illinois U.S.A. October 1997 ISBN 0-662-26033-3 EPA 905-R-97-015c Cat. No. En40-11/35-3-1997E ii The Land by the Lakes—SOLEC 96 Table of Contents Acknowledgments ................................................................. v 1. Overview of the Land by the Lakes .................................................. 1 1.1 Introduction ............................................................ 1 1.2 Report Structure ......................................................... 2 1.3 Conclusion ............................................................. 2 1.4 Key Observations ........................................................ 3 1.5 Moving Forward ......................................................... 5 2. The Ecoregional Context .......................................................... 6 2.1 Why Consider Ecoregional Context? .......................................... 6 2.2 Classification Systems for Great Lakes Ecoregions ............................... 7 3. Where Land and Water Meet ....................................................... 9 3.1 Changing Shapes and Structures ............................................. 9 3.1.1 Crustal Tilting ................................................. 10 3.1.2 Climate ....................................................... 10 3.1.3 Erosion ...................................................... -
The Geology of Ohio—The Precambrian
No. 13 OHIOGeoFacts DEPARTMENT OF NATURAL RESOURCES • DIVISION OF GEOLOGICAL SURVEY THE GEOLOGY OF OHIO—THE PRECAMBRIAN Precambrian time (all of geologic time before the Cambrian Pe- million years ago a continent to the east collided with North America, riod) began when the Earth became a solid entity about 4.5 billion resulting in extensive crustal compression and development of a years ago and ended when the Cambrian Period began, about 570 mountain range that geologists call the Grenville Mountains. What million years ago. “Precambrian” is actually an informal term used is thought to be the zone of continental collision, known as a suture by geologists. This long period of time is divided formally into two zone, is located in eastern Ohio and is called the Coshocton Zone. eons—the Archeozoic (greater than 2.5 billion years ago) and the As these continents collided along a 3,000-mile-long line, stretch- Proterozoic (2.5 billion to 570 million years ago). Despite the immense ing perhaps from Sweden to Mexico, rocks were folded, twisted, span of time it represents, the Precambrian is the most poorly known metamorphosed, and thrust westward across part of the rift zone of the geologic subdivisions in Ohio, in part because Precambrian in western Ohio. This north-south-oriented, 30-mile-wide zone of rocks are nowhere exposed in the state. These primarily crystalline east-dipping, imbricated thrust slices is called the Grenville Front igneous and metamorphic rocks are deeply buried beneath younger Tectonic Zone and marks the westward limit of the Grenville Moun- Paleozoic sedimentary rocks at depths ranging from about 2,500 feet tains. -
Ohio Division of Geological Survey Great Lakes Geologic Mapping Coalition Publications Updated March 2020
Link to ODGS Publications Ohio Division of Geological Survey Great Lakes Geologic Mapping Coalition Publications Updated March 2020 2019 Aden, Douglas, 2019, Karst in the Lilley Formation, Peebles 7.5-minute quadrangle, Ohio, in Thorleifson, L. H., ed., Geologic Mapping Forum 2019 Abstracts: Minnesota Geological Survey Open-File Report 19-1, p. 4–5. Aden, D. J., 2019, Surficial geology of the Gnadenhutten quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000. Aden, D. J., 2019, Surficial geology of the New Philadelphia quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000. Aden, D. J., 2019, Surficial geology of the Tippecanoe quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000. Aden, D. J., 2019, Surficial geology of the Uhrichsville quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000. Aden, D. J., and Parrick, B. D., 2018, Karst of northern portions of the Peebles and Jaybird 7.5-minute quadrangles, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey Open-File Report 2018-3, 40 p., 44 map tiles. Nash, T. A., 2019, Surficial geology of the Antrim quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000. Nash, T. A., 2019, Surficial geology of the Birmingham quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000. -
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. -
New Map of the Surficial Geology of the Lorain and Put-In-Bay 30 X 60 Minute Quadrangles, Ohio by Edward M
177 New Map of the Surficial Geology of the Lorain and Put-in-Bay 30 x 60 Minute Quadrangles, Ohio By Edward M. Swinford, Richard R. Pavey, and Glenn E. Larsen Ohio Department of Natural Resources Division of Geological Survey 2045 Morse Road Bldg. C-1 Columbus, OH 43229 Telephone: (614) 265-6473 e-mail: [email protected] ABSTRACT can be queried on the basis of material types and thick- nesses for rapid generation of derivative maps. Potential queries for derivative maps might include isolating clay A map depicting the surficial geology of the Lo- and silt deposits for the identification of potential geohaz- rain and Put-in-Bay 30 x 60 minute (1:100,000-scale) ards, identifying sand and gravel deposits for aggregate quadrangles has been produced by the Ohio Department exploration, or depicting areas of thick glacial till for the of Natural Resources, Division of Geological Survey. identification of potentially favorable solid-waste disposal Existing surficial maps at various scales document the sites. Mapping was partially funded by the U.S. Geologi- uppermost surficial lithology of the area. The new map cal Survey, National Cooperative Geological Mapping depicts underlying lithologies from the surface down to Program, STATEMAP component. Digital compilation bedrock for use in geotechnical studies, land-use plan- was made possible by funding from the Central Great ning, and mineral exploration. To produce the new map, Lakes Geologic Mapping Coalition. surficial deposits were mapped at 1:24,000 scale to create thirty-six 7.5-minute quadrangles, which were compiled digitally using GS technology and converted into a INTRODUCTION full-color, print-on-demand, 1:100,000-scale, surficial- geology map. -
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. -
Description of the Niagara Quadrangle
DESCRIPTION OF THE NIAGARA QUADRANGLE. By E. M. Kindle and F. B. Taylor.a INTRODUCTION. different altitudes, but as a whole it is distinctly higher than by broad valleys opening northwestward. Across northwestern GENERAL RELATIONS. the surrounding areas and is in general bounded by well-marked Pennsylvania and southwestern New York it is abrupt and escarpments. i nearly straight and its crest is about 1000 feet higher than, and The Niagara quadrangle lies between parallels 43° and 43° In the region of the lower Great Lakes the Glaciated Plains 4 or 5 miles back from the narrow plain bordering Lake Erie. 30' and meridians 78° 30' and 79° and includes the Wilson, province is divided into the Erie, Huron, and Ontario plains From Cattaraugus Creek eastward the scarp is rather less Olcott, Tonawanda, and Lockport 15-minute quadrangles. It and the Laurentian Plateau. (See fig. 2.) The Erie plain abrupt, though higher, and is broken by deep, narrow valleys thus covers one-fourth of a square degree of the earth's sur extending well back into the plateau, so that it appears as a line face, an area, in that latitude, of 870.9 square miles, of which of northward-facing steep-sided promontories jutting out into approximately the northern third, or about 293 square miles, the Erie plain. East of Auburn it merges into the Onondaga lies in Lake Ontario. The map of the Niagara quadrangle shows escarpment. also along its west side a strip from 3 to 6 miles wide comprising The Erie plain extends along the base of the Portage escarp Niagara River and a small area in Canada.