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Transportation and Economic Potential in the Arctic Woods, K
NRC Publications Archive Archives des publications du CNRC Transportation and economic potential in the Arctic Woods, K. B.; Legget, R. F. This publication could be one of several versions: author’s original, accepted manuscript or the publisher’s version. / La version de cette publication peut être l’une des suivantes : la version prépublication de l’auteur, la version acceptée du manuscrit ou la version de l’éditeur. Publisher’s version / Version de l'éditeur: Traffic Quarterly, 14, pp. 435-458, 1960-12-01 NRC Publications Archive Record / Notice des Archives des publications du CNRC : https://nrc-publications.canada.ca/eng/view/object/?id=35ca3993-c5a1-47bc-94ba-3bbe04114bca https://publications-cnrc.canada.ca/fra/voir/objet/?id=35ca3993-c5a1-47bc-94ba-3bbe04114bca Access and use of this website and the material on it are subject to the Terms and Conditions set forth at https://nrc-publications.canada.ca/eng/copyright READ THESE TERMS AND CONDITIONS CAREFULLY BEFORE USING THIS WEBSITE. L’accès à ce site Web et l’utilisation de son contenu sont assujettis aux conditions présentées dans le site https://publications-cnrc.canada.ca/fra/droits LISEZ CES CONDITIONS ATTENTIVEMENT AVANT D’UTILISER CE SITE WEB. Questions? Contact the NRC Publications Archive team at [email protected]. If you wish to email the authors directly, please see the first page of the publication for their contact information. Vous avez des questions? Nous pouvons vous aider. Pour communiquer directement avec un auteur, consultez la première page de la revue dans laquelle son article a été publié afin de trouver ses coordonnées. -
Ecological Regions of Minnesota: Level III and IV Maps and Descriptions Denis White March 2020
Ecological Regions of Minnesota: Level III and IV maps and descriptions Denis White March 2020 (Image NOAA, Landsat, Copernicus; Presentation Google Earth) A contribution to the corpus of materials created by James Omernik and colleagues on the Ecological Regions of the United States, North America, and South America The page size for this document is 9 inches horizontal by 12 inches vertical. Table of Contents Content Page 1. Introduction 1 2. Geographic patterns in Minnesota 1 Geographic location and notable features 1 Climate 1 Elevation and topographic form, and physiography 2 Geology 2 Soils 3 Presettlement vegetation 3 Land use and land cover 4 Lakes, rivers, and watersheds; water quality 4 Flora and fauna 4 3. Methods of geographic regionalization 5 4. Development of Level IV ecoregions 6 5. Descriptions of Level III and Level IV ecoregions 7 46. Northern Glaciated Plains 8 46e. Tewaukon/BigStone Stagnation Moraine 8 46k. Prairie Coteau 8 46l. Prairie Coteau Escarpment 8 46m. Big Sioux Basin 8 46o. Minnesota River Prairie 9 47. Western Corn Belt Plains 9 47a. Loess Prairies 9 47b. Des Moines Lobe 9 47c. Eastern Iowa and Minnesota Drift Plains 9 47g. Lower St. Croix and Vermillion Valleys 10 48. Lake Agassiz Plain 10 48a. Glacial Lake Agassiz Basin 10 48b. Beach Ridges and Sand Deltas 10 48d. Lake Agassiz Plains 10 49. Northern Minnesota Wetlands 11 49a. Peatlands 11 49b. Forested Lake Plains 11 50. Northern Lakes and Forests 11 50a. Lake Superior Clay Plain 12 50b. Minnesota/Wisconsin Upland Till Plain 12 50m. Mesabi Range 12 50n. Boundary Lakes and Hills 12 50o. -
The Height of Its Womanhood': Women and Genderin Welsh Nationalism, 1847-1945
'The height of its womanhood': Women and genderin Welsh nationalism, 1847-1945 Item Type text; Dissertation-Reproduction (electronic) Authors Kreider, Jodie Alysa Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 09/10/2021 04:59:55 Link to Item http://hdl.handle.net/10150/280621 'THE HEIGHT OF ITS WOMANHOOD': WOMEN AND GENDER IN WELSH NATIONALISM, 1847-1945 by Jodie Alysa Kreider Copyright © Jodie Alysa Kreider 2004 A Dissertation Submitted to the Faculty of the DEPARTMENT OF HISTORY In Partia' Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College THE UNIVERSITY OF ARIZONA 2004 UMI Number: 3145085 Copyright 2004 by Kreider, Jodie Alysa All rights reserved. INFORMATION TO USERS The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleed-through, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. UMI UMI Microform 3145085 Copyright 2004 by ProQuest Information and Learning Company. All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. -
Description of the Herman, Barrett, Chokio, and Morris Quadrangles
DESCRIPTION OF THE HERMAN, BARRETT, CHOKIO, AND MORRIS QUADRANGLES. By Frederick W. Sardesoii. INTRODUCTION, general trend northeastward, reach an altitude of 2,000 feet, Winnipeg, which discharges through Nelson River into Hud GENERAL RELATIONS. and the Mesabi Range stands 2,200 feet above the sea. son Bay. Northeastern Minnesota and a little of northern Although they reach an altitude of 2,000 feet in places along Wisconsin are drained into Lake Superior, part of the St. The area here described lies between parallels 46° 30' and their western margin and in the Turtle Mountains plateau on Lawrence system. The rest of Minnesota, except the extreme 46° and meridians 95° 45' and 96° 15' and includes the the international boundary, the Glaciated Plains elsewhere lie southwest corner, the greater part of Wisconsin, and the Herman, Barrett, Chokio, and Morris quadrangles, comprising considerably lower. In North Dakota and South Dakota and eastern two-thirds of Iowa are drained directly into the upper 834.83 square miles. It is in western Minnesota and includes eastern Nebraska their surface slopes in general eastward to Mississippi, and the remainder of the region mapped in figure the greater part of Grant and Stevens counties and small adja a level of about 1,000 feet along the Missouri and to consider 2 is drained into the Mississippi through the Missouri. The cent parts of Douglas, Pope, and Big Stone counties. (See ably less in the valley of Red River. In the area east of this State of Minnesota lies in part of each of the four drainage fig. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
By Nevin M. Fenneman DEPARTMENT of GEOLOGY, UNIVERSITY of CINCINNATI Communicated by W
GEOLOGY: N. M. FENNEMAN 17 PHYSIOGRAPHIC SUBDIVISION OF THE UNITED STATES By Nevin M. Fenneman DEPARTMENT OF GEOLOGY, UNIVERSITY OF CINCINNATI Communicated by W. M. Davis, November 24, 1916 Various attempts at subdivision of the United States into physio- graphic provinces have been made, beginning with- that of Powell.' The Association of American Geographers, recognizing the fundamental importance of this problem, appointed a committee in 1915 to prepare a suitable map of physiographic divisions. The committee consists of Messrs. M. R. Campbell and F. E. Matthes of the U. S. Geological Survey and Professors Eliot Blackwelder, D. W. Johnson, and Nevin M. Fenneman (chairman). The map herewith presented and the ac- companying table of divisions constitute the report of that committee. The same map on a larger scale (120 miles to the inch) will be found in Volume VI of the Annals of the Association of American Geographers, accompanying a paper by the writer on the Physiographic Divisions of the United States. In that paper are given the nature of the bound- ary lines and those characteristics of the several units which are believed to justify their recognition as such. Though the above-named com- mittee is not directly responsible for the statements there made, many of them represent the results of the committee's conferences. The paper as a whole is believed to represent fairly well the views of the committee, though in form the greater part of it is a revision of a former publication.2 The basis of division shown on this map, here reproduced, is physio- graphic or, as might be said in Europe, morphologic. -
FIGURE 4 Map Showing Physiographic Provinces and Sections of the Eastern United States (From Fenneman 1938)
nagement of Central Hardwood Forests The Central Hardwood Region 7 PHYSIOGRAPHY ardwood region is situated in an area that, in the main part, is th the Appalachian system and, except for the northwestern rglaciated (Fig. 4). The primary physiographic regions of the oods are the Blue Ridge, Ridge and Valley, Appalachian Plateaus, md, Ozark Plateau, and Ouachita provinces (Fenneman 1938). Ridge is the easternmost province in the central hardwood region 1 the south in northern Georgia and extends into southeastern Through Virginia, the Blue Ridge narrows to form a prominent the name "Blue Ridge." The highest elevations in the eastern occur in the Blue Ridge section of western North Carolina. Mount le Black Mountains just northeast of Asheville rises to a height of ~ sea level and, like many of the tallest peaks in the Appalachians, rith a relic spruce-fir forest. tely north and west of the Blue Ridge is the Ridge and Valley xtends from central Pennsylvania in the north to northern Georgia . The Ouachita Mountains of Arkansas, Oklahoma, and Missouri pographically to the Ridge and ValleyProvince, and several authors I I I o 125 250 :hey are part of a common feature, part of which is buried in 11 500 miles bama and Mississippi (King 1950; Petersen et al. 1980; Hubler ITI2TI CENTRAL HARDWOOD REGION dge and Valley section is very old and geologically complex, having I faulted, folded, and eroded. The ridges are long and narrow with ..-.~/ s through Pennsylvania, western Maryland, and West Virginia (Fig. /_. } iden southward to form the valley of the Shenandoah in Virginia essee farther south. -
USGS Geologic Investigations Series I-2720, Pamphlet
A Tapestry of Time and Terrain Pamphlet to accompany Geologic Investigations Series I–2720 U.S. Department of the Interior U.S. Geological Survey This page left intentionally blank A Tapestry of Time and Terrain By José F. Vigil, Richard J. Pike, and David G. Howell Pamphlet to accompany Geologic Investigations Series I–2720 U.S. Department of the Interior Bruce Babbitt, Secretary U.S. Geological Survey Charles G. Groat, Director Any use of trade, product, or firm names in this publica- tion is for descriptive purposes only and does not imply endorsement by the U.S. Government. United States Government Printing Office: 2000 Reprinted with minor corrections: 2008 For additional copies please contact: USGS Information Services Box 25286 Denver, CO 80225 For more information about the USGS and its products: Telephone: 1–888–ASK–USGS World Wide Web: http://www.usgs.gov/ Text edited by Jane Ciener Layout and design by Stephen L. Scott Manuscript approved for publication, February 24, 2000 2 Introduction are given in Thelin and Pike (1991). Systematic descriptions of the terrain features shown on this tapestry, as well as the Through computer processing and enhancement, we have geology on which they developed, are available in Thornbury brought together two existing images of the lower 48 states of (1965), Hunt (1974), and other references on geomorphology, the United States (U.S.) into a single digital tapestry. Woven the science of surface processes and their resulting landscapes into the fabric of this new map are data from previous U.S. (Graf, 1987; Bloom, 1997; Easterbrook, 1998). Geological Survey (USGS) maps that depict the topography and geology of the United States in separate formats. -
Library Research for Water Resources March 5, 2020 Emily C
Library Research for Water Resources March 5, 2020 Emily C. Wild, Chemistry, Geosciences and Environmental Studies Librarian [email protected] 609-258-5484 http://digitalcollections.archives.nysed.gov/index.php/Det http://digitalcollections.archives.nysed.gov/i ail/objects/46309 ndex.php/Detail/objects/4197 Overview Session Information & Questions : 1. My Past Presentations & Bio 2. What is Hydrology? 3. Who is a Hydrologist? 4. What does a Hydrologist Research? 5. What does this water map mean? The opening of the first section of the Erie Canal http://digitalcollections.archives.nysed.gov/index.php/D 6. Is there oil/gas/mining in my etail/objects/9566 watershed? H2O/day: 64 ounces to 7. What are your most frequently half your asked questions? bodyweight 8. How do I become a Hydrologist? Past GPO Sessions Use the Internet Archive WayBackMachine https://archive.org/web/ January 2020 – “Introduction to Geosciences Library Research https://www.fdlp.gov/introduction-to-geosciences-library-research March 2018 - "U.S. Geological Survey (USGS) Library Materials for Natural Hazards (and Land Change)” https://www.fdlp.gov/usgs-library-materials-for-natural-hazards March 2018 - "USGS Library Materials for Water Resources Information" https://www.fdlp.gov/usgs-library-materials-for-water- resources-information March 2018 - "USGS Library Materials for Earth's Age" https://www.fdlp.gov/usgs-library-materials-for-earth-s-age September 2017 - "USGS Library - Indexes, Catalogs, and Other Bibliographic Tools, A day in the life of a reference librarian” -
Contents Tables ABSTRACT
STATE OF MICHIGAN Table 2. Annual precipitation for the years 1940 to 1949, Ironwood, Michigan. .........................................................7 PROGRESS REPORT NUMBER FOURTEEN Table 3. Monthly normal precipitation and mean temperatures, Ground-Water Resources of the Glacial Ironwood, Michigan. .........................................................7 Deposits, Bessemer Area, Michigan Table 4. Annual pumpage for Bessemer municipal supply. ..11 1950 Table 5. Complete chemical analysis of water from Bessemer’s new production well 2* (Parts per million)...13 by E. A. Brown and W. T. Stuart Table 6. Partial chemical analysis of ground water in the Bessemer area (Parts per million)..................................16 Prepared in cooperation with The United States Department of the Interior Geological Survey ABSTRACT June, 1951 This report is based on an investigation of the ground- water resources in the vicinity of Bessemer in the Contents western part of the northern peninsula of Michigan, made by the Geological Survey of the United States ABSTRACT....................................................................... 1 Department of the Interior in cooperation with the INTRODUCTION............................................................... 2 Geological Survey Division of the Michigan Department of Conservation. The area studied in detail covers about ACKNOWLEDGMENTS................................................ 3 60 square miles within a 4.5-mile radius of Bessemer, PERSONNEL ............................................................... -
Development and Evaluation of Bankfull Hydraulic Geometry Relationships for the Physiographic Regions of the United States1
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION AMERICAN WATER RESOURCES ASSOCIATION DEVELOPMENT AND EVALUATION OF BANKFULL HYDRAULIC GEOMETRY RELATIONSHIPS FOR THE PHYSIOGRAPHIC REGIONS OF THE UNITED STATES1 Katrin Bieger, Hendrik Rathjens, Peter M. Allen, and Jeffrey G. Arnold2 ABSTRACT: Bankfull hydraulic geometry relationships are used to estimate channel dimensions for streamflow simulation models, which require channel geometry data as input parameters. Often, one nationwide curve is used across the entire United States (U.S.) (e.g., in Soil and Water Assessment Tool), even though studies have shown that the use of regional curves can improve the reliability of predictions considerably. In this study, regional regression equations predicting bankfull width, depth, and cross-sectional area as a function of drain- age area are developed for the Physiographic Divisions and Provinces of the U.S. and compared to a nationwide equation. Results show that the regional curves at division level are more reliable than the nationwide curve. Reliability of the curves depends largely on the number of observations per region and how well the sample represents the population. Regional regression equations at province level yield even better results than the division-level models, but because of small sample sizes, the development of meaningful regression models is not possible in some provinces. Results also show that drainage area is a less reliable predictor of bankfull channel dimensions than bankfull discharge. It is likely that the regional curves can be improved using multiple regres- sion models to incorporate additional explanatory variables. (KEY TERMS: streams; fluvial geomorphology; bankfull discharge; nationwide and regional regression equa- tions; hydrologic modeling.) Bieger, Katrin, Hendrik Rathjens, Peter M. -
The White Man's Grave: a Visit to Sierra Leone, in 1834, Volume I
This is a reproduction of a library book that was digitized by Google as part of an ongoing effort to preserve the information in books and make it universally accessible. https://books.google.com 7*M 7. 1 I THE WHITE MAN'S GRAVE. VOL. I. LONDON : PRINTED BY 8AMUEL BENTLEY, Dorset Street, Fleet Street. THE WHITE MAN'S GRAVE: A VISIT 10 SIERRA LEONE, in 1834. BY F. HARRISON RANKIN. It is quite customary to ask in the morning, how many died last night . M. A. Falconbridgb. IN TWO VOLUMES. VOL. I. LONDON : RICHARD BENTLEY, NEW BURLINGTON STREET. (successor to henry colburn.) 1836. TO THE HON. W. H. MACAULEY, CHIEF JUDGE OF THE HIGH COURT OF MIXED COMMISSION AT SIERRA LEONE, " THESE VOLUMES ARE OFFERED, SEEKING A " BRIEF IMMORTALITY " TOR THE MEMORY OF SCENES TO WHICH HIS FRIENDSHIP AND HOSPITALITY GAVE ADDITIONAL INTEREST. "sO-xrvc^:- 0x^- ^%zjxst~ /to 6 f ^tn^^/^ Xj<yr^ Jo yt-*fiwL (zcwetp ^ 'fas o^cx. 4 > PREFACE. Majesty, moving in royal progresses, is preceded by a graduated line of peers. The noblest follow in the wake of the less noble, and the latest creations place them selves before the titles of ancient date. The etiquette of books enforces the same rule. The last portion written, fa cetiously named the Preface, takes its station in front of the volume, and claims the first notice of the reader ; whence it may occasionally chance to be mistaken by exoterics and the uninitiated for the first-born, mid to enjoy a respect due to its subsequent but elder brethren.