The Coteau Du Missouri : a Regional Study
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Interpretation of Cumberland Escarpment and Highland Rim, South-Central Tennessee and Northeast Alabama
Interpretation of Cumberland Escarpment and Highland Rim, South-Central Tennessee and Northeast Alabama GEOLOGICAL SURVEY PROFESSIONAL PAPER 524-C Interpretation of Cumberland Escarpment and Highland Rim, South-Central Tennessee and Northeast Alabama By JOHN T. HACK SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 524-C Theories of landscape origin are compared using as an example an area of gently dipping rocks that differ in their resistance to erosion UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1966 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract___________________________________________ C1 Cumberland Plateau and Highland Rim as a system in Introduction_______________________________________ 1 equilibrium______________________________________ C7 General description of area___________________________ 1 Valleys and coves of the Cumberland Escarpment___ 7 Cumberland Plateau and Highland Rim as dissected and Surficial deposits of the Highland Rim____________ 10 deformed peneplains _____________________ ,... _ _ _ _ _ _ _ _ 4 Elk River profile_______________________________ 12 Objections to the peneplain theory____________________ 5 Paint Rock Creek profile________________________ 14 Eastern Highland Rim Plateau as a modern peneplain__ 6 Conclusions________________________________________ 14 Equilibrium concept -
When the Mountain Became the Escarpment.FH11
Looking back... with Alun Hughes WHEN THE MOUNTAIN BECAME THE ESCARPMENT The Niagara Escarpment hasnt always been But Coronelli was not the first to put Niagara known by that name. Early in the 19th century it on the map. That distinction belongs to Father Louis was often referred to as the Mountain, and of course Hennepin, the Recollect priest who was the first it is still called that in Hamilton and Grimsby today. European to describe Niagara Falls from personal We in eastern Niagara have largely forgotten the observation. In his Description de la Louisiane, name, though it survives in the City of Thorolds published in 1683, five years after his visit, he speaks motto Where the Ships Climb the Mountain. of le grand Sault de Niagara, and labels it thus on the accompanying map. This is the form that So when did the name Niagara Escarpment first prevails thereafter, and it is the spelling used for Fort come into use? And what about the areas other de Niagara, established by the French at the mouth Niagara names, like Niagara Falls, Niagara River of the river in 1726. The English followed suit, and Niagara Peninsula? When did these first appear? though on many early maps (e.g. Moll 1715, I dont pretend to have definitive answers there Mitchell 1782) they use the name Great Fall of are too many sources I have not seen but I can Niagara rather than Niagara Falls. suggest some preliminary conclusions. In his Description Hennepin also refers to la The name Niagara is definitely of native origin, belle Riviere de Niagara, so the name Niagara though there is no agreement about its meaning. -
Cumulative Index North Dakota Historical Quarterly Volumes 1-11 1926 - 1944
CUMULATIVE INDEX NORTH DAKOTA HISTORICAL QUARTERLY VOLUMES 1-11 1926 - 1944 A Aiton, Arthur S., review by, 6:245 Alaska, purchase of, 6:6, 7, 15 A’Rafting on the Mississipp’ (Russell), rev. of, 3:220- 222 Albanel, Father Charles, 5:200 A-wach-ha-wa village, of the Hidatsas, 2:5, 6 Albert Lea, Minn., 1.3:25 Abandonment of the military posts, question of, Albrecht, Fred, 2:143 5:248, 249 Alderman, John, 1.1:72 Abbey Lake, 1.3:38 Aldrich, Bess Streeter, rev. of, 3:152-153; Richard, Abbott, Johnston, rev. of, 3:218-219; Lawrence, speaker, 1.1:52 speaker, 1.1:50 Aldrich, Vernice M., articles by, 1.1:49-54, 1.4:41- Abe Collins Ranch, 8:298 45; 2:30-52, 217-219; reviews by, 1.1:69-70, Abell, E. R, 2:109, 111, 113; 3:176; 9:74 1.1:70-71, 1.2:76-77, 1.2:77, 1.3:78, 1.3:78-79, Abercrombie, N.Dak., 1.3: 34, 39; 1.4:6, 7, 71; 2:54, 1.3:79, 1.3:80, 1.4:77, 1.4:77-78; 2:230, 230- 106, 251, 255; 3:173 231, 231, 231-232, 232-233, 274; 3:77, 150, Abercrombie State Park, 4:57 150-151, 151-152, 152, 152-153, 220-222, 223, Aberdeen, D.T., 1.3:57, 4:94, 96 223-224; 4:66, 66-67, 67, 148, 200, 200, 201, Abraham Lincoln, the Prairie Years (Sandburg), rev. of, 201, 202, 202, 274, 275, 275-276, 276, 277-278; 1.2:77 8:220-221; 10:208; 11:221, 221-222 Abstracts in History from Dissertations for the Degree of Alexander, Dr. -
Teacher’S Guide Teacher’S Guide Little Bighorn National Monument
LITTLE BIGHORN NATIONAL MONUMENT TEACHER’S GUIDE TEACHER’S GUIDE LITTLE BIGHORN NATIONAL MONUMENT INTRODUCTION The purpose of this Teacher’s Guide is to provide teachers grades K-12 information and activities concerning Plains Indian Life-ways, the events surrounding the Battle of the Little Bighorn, the Personalities involved and the Impact of the Battle. The information provided can be modified to fit most ages. Unit One: PERSONALITIES Unit Two: PLAINS INDIAN LIFE-WAYS Unit Three: CLASH OF CULTURES Unit Four: THE CAMPAIGN OF 1876 Unit Five: BATTLE OF THE LITTLE BIGHORN Unit Six: IMPACT OF THE BATTLE In 1879 the land where The Battle of the Little Bighorn occurred was designated Custer Battlefield National Cemetery in order to protect the bodies of the men buried on the field of battle. With this designation, the land fell under the control of the United States War Department. It would remain under their control until 1940, when the land was turned over to the National Park Service. Custer Battlefield National Monument was established by Congress in 1946. The name was changed to Little Bighorn National Monument in 1991. This area was once the homeland of the Crow Indians who by the 1870s had been displaced by the Lakota and Cheyenne. The park consists of 765 acres on the east boundary of the Little Bighorn River: the larger north- ern section is known as Custer Battlefield, the smaller Reno-Benteen Battlefield is located on the bluffs over-looking the river five miles to the south. The park lies within the Crow Indian Reservation in southeastern Montana, one mile east of I-90. -
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. -
A Historical Geography of Lake Kampeska in the City of Watertown, South Dakota Joanita M
South Dakota State University Open PRAIRIE: Open Public Research Access Institutional Repository and Information Exchange Geography Faculty Publications Department of Geography 2007 A Historical Geography of Lake Kampeska in the City of Watertown, South Dakota Joanita M. Kant South Dakota State University, [email protected] Follow this and additional works at: https://openprairie.sdstate.edu/geo_pubs Part of the Physical and Environmental Geography Commons Recommended Citation Kant, Joanita M., "A Historical Geography of Lake Kampeska in the City of Watertown, South Dakota" (2007). Geography Faculty Publications. 2. https://openprairie.sdstate.edu/geo_pubs/2 This Article is brought to you for free and open access by the Department of Geography at Open PRAIRIE: Open Public Research Access Institutional Repository and Information Exchange. It has been accepted for inclusion in Geography Faculty Publications by an authorized administrator of Open PRAIRIE: Open Public Research Access Institutional Repository and Information Exchange. For more information, please contact [email protected]. i A Historical Geography of Lake Kampeska in the City of Watertown, South Dakota 2007 by Joanita Kant copyright ii “Never forget that a small group of thoughtful, committed citizens can change the world. Indeed, it is the only thing that ever has.” Margaret Meade i ABSTRACT Many alterations in the hydrology of Lake Kampeska began with the arrival of masses of Anglo settlers in the 1870s. Why the lake has been altered is a complex issue linked to various natural physical processes which would have occurred even without the introduction of those settlers into the ecosystem. Those processes include weather, climate, sedimentation rates, lakebank erosion, chemical and mineral transport from soils, and flooding, among others. -
The Abyssal Giant Pockmarks of the Black Bahama Escarpment: Relations Between Structures, fluids and Carbonate Physiography” by Thibault Cavailhes Et Al
Solid Earth Discuss., https://doi.org/10.5194/se-2020-11-RC2, 2020 SED © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Interactive comment Interactive comment on “The abyssal giant pockmarks of the Black Bahama Escarpment: Relations between structures, fluids and carbonate physiography” by Thibault Cavailhes et al. Charles Paull (Referee) [email protected] Received and published: 10 April 2020 The manuscript describes a series of ∼circular depressions at the base of the Bahama Escarpment. These are curious features and their discovery may ultimately merit pub- lication. However, the manuscript more closely resembles a first draft, rather than a Printer-friendly version polished work. As is, the existing draft is too poorly written to fully follow many of the arguments in detail. Part of may be attributed to the challenge of writing in a second Discussion paper language. I have made some suggestions as to how to begin to sharpen the word- ing, but it is an incomplete effort. There are also a number of science related points C1 (also indicate below) that need to be considered before this could be recommended for publication. SED Why are these depressions called pockmarks from the outset? What is actually ob- served are approximately circular depressions. The term ‘pockmark’ has evolved to Interactive imply that the depression was somehow physically excavated by seepage, not phys- comment ical collapse. Moreover, it is not commonly been used in carbonate settings. The manuscript also refers to other similar depressions that have been previously been called plunge pools. This is yet another mechanism for surface erosion. -
Sioux Falls, 1877-1880
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Great Plains Quarterly Great Plains Studies, Center for 2004 A Dakota Boomtown: Sioux Falls, 1877-1880 Gary D. Olsen Augustana College - Sioux Falls Follow this and additional works at: https://digitalcommons.unl.edu/greatplainsquarterly Part of the Other International and Area Studies Commons Olsen, Gary D., "A Dakota Boomtown: Sioux Falls, 1877-1880" (2004). Great Plains Quarterly. 268. https://digitalcommons.unl.edu/greatplainsquarterly/268 This Article is brought to you for free and open access by the Great Plains Studies, Center for at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Great Plains Quarterly by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. A DAKOTA BOOMTOWN SIOUX FALLS, 1877 .. 1880 GARY D. OLSON The "Dakota boom" is a label historians have claiming of land by immigrant and American almost universally adopted to describe the would, be farm owners in the plains of Dakota period of settlement in Dakota Territory be, Territory and adjacent areas. Less well known tween the years 1878 and 1887. The term is the impact this rapid, large,scale settling of "boom" has been applied to this period largely the land had on the rise and growth of townsites because of the volume of land claimed and the aspiring to become prosperous ci ties. We know rapid increase in Dakota Territory's popula, the rural landscape changed as sod houses and tion that occurred during those years. Most dugouts were erected, fields plowed, and trees accounts of this time period have treated the planted. -
To Prairie Preserves
This document is made available electronically by the Minnesota Legislative Reference Library as part of an ongoing digital archiving project. http://www.leg.state.mn.us/lrl/lrl.asp (Funding for document digitization was provided, in part, by a grant from the Minnesota Historical & Cultural Heritage Program.) A GUIDE TO MINNESOTA PRAIRIES By Keith M. Wendt Maps By Judith M. Ja.cobi· Editorial Assistance By Karen A. Schmitz Art and Photo Credits:•Thorn_as ·Arter, p. 14 (bottom left); Kathy Bolin, ·p: 14 (top); Dan Metz, pp. 60, 62; Minnesota Departme'nt of Natural Resources, pp. '35 1 39, 65; U.S. Department of Agriculture, p. -47; Keith Wendt, cover, pp~ 14 (right), 32, 44; Vera Wohg, PP· 22, 43, 4a. · · ..·.' The Natural Heritage Program Minnesota Department of Natural Resources Box 6, Centennial Office Building . ,. St. Paul; MN 55155 ©Copyright 1984, State of Minnesota, Department of Natural Resource.s CONTENTS PREFACE .......................................... Page 3 INTRODUCTION .................................... Page 5 MINNESOTA PRAIRIE TYPES ........................... Page 6 PROTECTION STATUS OF MINNESOTA PRAIRIES ............ Page 12 DIRECTORY OF PRAIRIE PRESERVES BY REGION ............ Page 15 Blufflands . Page 18 Southern Oak Barrens . Page 22 Minnesota River Valley ............................. Page 26 Coteau des Prairies . Page 32 Blue Hills . Page 40 Mississippi River Sand Plains ......................... Page 44 Red River Valley . Page 48 Aspen Parkland ................................... Page 62 REFERENCES ..................................... Page 66 INDEX TO PRAIRIE PRESERVES ......................... Page 70 2 PREFACE innesota has established an outstanding system of tallgrass prairie preserves. No state M in the Upper Midwest surpasses Minnesota in terms of acreage and variety of tallgrass prairie protected. Over 45,000 acres of native prairie are protected on a wide variety of landforms that span the 400 mile length of the state from its southeast to northwest corner. -
Status of Mineral Resource Information for the Standing Rock Indian Reservation, North Dakota and South Dakota
STATUS OF MINERAL RESOURCE INFORMATION FOR THE STANDING ROCK INDIAN RESERVATION, NORTH DAKOTA AND SOUTH DAKOTA By Lee R. Rice Richard Bretz U.S. Bureau of Mines South Dakota Geological Survey Administrative Report BIA-41 1978 CONTENTS SUMMARY AND CONCLUSIONS ................................................. 1 INTRODUCTION ................................................................ 1 Previous Work ............................................................. 2 Land Status................................................................ 2 Map Coverage ............................................................. 3 Physiography .............................................................. 3 GEOLOGY ..................................................................... 4 General ................................................................... 4 Stratigraphy ............................................................... 4 Outcropping Rock Units ............................................... 4 Subsurface Rock Units ................................................. 5 Structure.................................................................. 5 GEOPHYSICS ................................................................... 6 MINERAL RESOURCES .......................................................... 6 General ................................................................... 6 Energy Resources........................................................... 6 Lignite ............................................................. 6 General -
Updating Boundaries for Large Water Bodies of the Coteau Des Prairies Using Landsat 8
UPDATING BOUNDARIES FOR LARGE WATER BODIES OF THE COTEAU DES PRAIRIES USING LANDSAT 8 South Dakota State University Landsat 8 drawing. Credit: NASA Department of Geography – Bruce V. Millett A BSTRACT M ETHODS R E S U L T S / C ONCLUSIONS Large lakes and wetland boundaries of the Coteau des Prairies and There were three main data elements used to create this map. The assembly of the map components began with coordinate system. surrounding region have changed since the National Wetlands 1. Digital Elevation Model All map coverages were projected to USA Contiguous Albers Equal Inventory (NWI) dataset was developed approximately 30 years ago. 2. National Wetlands Inventory Area Conic USGS version. This was further customized adjusting the Landsat 8, a NASA and USGS collaboration, acquires global moderate- 3. Landsat 8 data. Central Meridian to: -97.5°, Standard Parallel 1 to 29.5°, Standard resolution measurements in the visible, near-infrared, short wave, and Parallel 2 to 45.5°, and the Latitude of Origin to 23.0°. thermal infrared. Boundary limits for large water bodies were updated using 2016 Landsat 8 imagery with less than ten percent cloud cover. The mosaicked 1/3 arc-second DEM resulted in a cell resolution 10 Unsupervised and supervised classification methods were used to 1. Digital Elevation Model meters. extract water features from Landsat 8 imagery using ArcGIS Pro Imagery tools. Extracted polygon features were manually edited and • 30 National Elevation Dataset Clipped NWI data provided a total of 1,652,089 basins within the study overlaid with the NWI dataset. A final map was created by overlaying (NED) 1/3 arc-second DEMs area. -
Fishes of South Dakota
MISCELLANEOUS PUBLICATIONS MUSEUM OF ZOOLOGY, UNIVERSITY OF MICHIGAN, NO. 119 Fishes of South Dakota REEVE M. BAILEY AND MARVIN 0. ALLUM South Dakota State College ANN ARBOR MUSEUM OF ZOOLOGY, UNIVERSITY OF MICHIGAN JUNE 5, 1962 MISCELLANEOUS PUBLICATIONS MUSEUM OF ZOOLOGY, UNIVERSITY 01; MICHIGAN The publications of the Museum of Zoology, University of Michigan, consist of two series-the Occasional Papers and the Miscellaneous Publications. Both series were founded by Dr. Bryant Walker, Mr. Bradshaw H. Swales, and Dr. W. W. Newcomb. The Occasional Papers, publication of which was begun in 1913, serve as a medium for original studies based principally upon the collections in the Museum. They are issued separately. When a sufficient number of pages has been printed to make a volume, a title page, table of contents, and an index are supplied to libraries and indi- viduals on the mailing list for the series. The Miscellaneous Publications, which include papers on field and museum tech- niques, monographic studies, and other contributions not within the scope of the Occasional Papers, are published separately. It is not intended that they be grouped into volumes. Each number has a title page and, when necessary, a table of contents. A conlplete list of publications on Birds, Fishes, Insects, Mammals, Mollusks, and Reptiles and Amphibians is available. Address inquiries to the Director, Museum of Zoology, Ann Arbor, Michigan No. 13. Studies of the fishes of the order Cyprinodontes. By CARL L. HUBBS. (1924) 23 pp., 4 pls. ............................................. No. 15. A check-list of the fishes of the Great Lakes and tributary waters, with nomenclatorial notes and analytical keys.