Ecoregions of North Dakota and South Dakota Hydrography, and Land Use Pattern
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Summary Report of the Geological Survey for the Calendar Year 1911
5 GEORGE V. SESSIONAL PAPER No. 26 A. 1915 SUMMARY REPORT OK THE GEOLOGICAL SURVEY DEPARTMENT OF MINES FOR THE CALENDAR YEAR 1914 PRINTED BY ORDER OF PARLIAMENT. OTTAWA PRTNTKD BY J. i»k L TAOHE, PRINTER TO THE KING'S MOST EXCELLENT IfAJESTS [No. 26—1915] [No , 15031 5 GEORGE V. SESSIONAL PAPER No. 26 A. 1915 To Field Marshal, Hit Hoi/al Highness Prince Arthur William Patrick Albert, Duke of Connaught and of Strath-earn, K.G., K.T., K.P., etc., etc., etc., Governor General and Commander in Chief of the Dominion of Canada. May it Please Youb Royal Highness.,— The undersigned has the honour to lay before Your Royal Highness— in com- pliance with t>-7 Edward YIT, chapter 29, section IS— the Summary Report of the operations of the Geological Survey during the calendar year 1914. LOUIS CODERRK, Minister of Mines. 5 GEORGE V. SESSIONAL PAPER No. 26 A. 1915 To the Hon. Louis Codebrk, M.P., Minister of Mines, Ottawa. Sir,—I have the honour to transmit, herewith, my summary report of the opera- tions of the Geological Survey for the calendar year 1914, which includes the report* of the various officials on the work accomplished by them. I have the honour to be, sir, Your obedient servant, R. G. MrCOXXFI.L, Deputy Minister, Department of Mines. B . SESSIONAL PAPER No. 28 A. 1915 5 GEORGE V. CONTENTS. Paok. 1 DIRECTORS REPORT REPORTS FROM GEOLOGICAL DIVISION Cairncs Yukon : D. D. Exploration in southwestern "" ^ D. MacKenzie '\ Graham island. B.C.: J. M 37 B.C. -
Souris R1ve.R Investigation
INTERNATIONAL JOINT COMMISSION REPORT ON THE SOURIS R1VE.R INVESTIGATION OTTAWA - WASHINGTON 1940 OTTAWA EDMOND CLOUTIER PRINTER TO THE KING'S MOST EXCELLENT MAJESTY 1941 INTERNATIONAT, JOINT COMMISSION OTTAWA - WASHINGTON CAKADA UNITEDSTATES Cllarles Stewrt, Chnirmun A. 0. Stanley, Chairman (korge 11'. Kytc Roger B. McWhorter .J. E. I'erradt R. Walton Moore Lawrence ,J. Burpee, Secretary Jesse B. Ellis, Secretary REFERENCE Under date of January 15, 1940, the following Reference was communicated by the Governments of the United States and Canada to the Commission: '' I have the honour to inform you that the Governments of Canada and the United States have agreed to refer to the International Joint Commission, underthe provisions of Article 9 of theBoundary Waters Treaty, 1909, for investigation, report, and recommendation, the following questions with respect to the waters of the Souris (Mouse) River and its tributaries whichcross the InternationalBoundary from the Province of Saskatchewanto the State of NorthDakota and from the Stat'e of NorthDakota to the Province of Manitoba:- " Question 1 In order to secure the interests of the inhabitants of Canada and the United States in the Souris (Mouse) River drainage basin, what apportion- ment shouldbe made of the waters of the Souris(Mouse) River and ita tributaries,the waters of whichcross theinternational boundary, to the Province of Saskatchewan,the State of North Dakota, and the Province of Manitoba? " Question ,$! What methods of control and operation would be feasible and desirable in -
Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region. -
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. -
Archeological and Bioarcheological Resources of the Northern Plains Edited by George C
Tri-Services Cultural Resources Research Center USACERL Special Report 97/2 December 1996 U.S. Department of Defense Legacy Resource Management Program U.S. Army Corps of Engineers Construction Engineering Research Laboratory Archeological and Bioarcheological Resources of the Northern Plains edited by George C. Frison and Robert C. Mainfort, with contributions by George C. Frison, Dennis L. Toom, Michael L. Gregg, John Williams, Laura L. Scheiber, George W. Gill, James C. Miller, Julie E. Francis, Robert C. Mainfort, David Schwab, L. Adrien Hannus, Peter Winham, David Walter, David Meyer, Paul R. Picha, and David G. Stanley A Volume in the Central and Northern Plains Archeological Overview Arkansas Archeological Survey Research Series No. 47 1996 Arkansas Archeological Survey Fayetteville, Arkansas 1996 Library of Congress Cataloging-in-Publication Data Archeological and bioarcheological resources of the Northern Plains/ edited by George C. Frison and Robert C. Mainfort; with contributions by George C. Frison [et al.] p. cm. — (Arkansas Archeological Survey research series; no. 47 (USACERL special report; 97/2) “A volume in the Central and Northern Plains archeological overview.” Includes bibliographical references and index. ISBN 1-56349-078-1 (alk. paper) 1. Indians of North America—Great Plains—Antiquities. 2. Indians of North America—Anthropometry—Great Plains. 3. Great Plains—Antiquities. I. Frison, George C. II. Mainfort, Robert C. III. Arkansas Archeological Survey. IV. Series. V. Series: USA-CERL special report: N-97/2. E78.G73A74 1996 96-44361 978’.01—dc21 CIP Abstract The 12,000 years of human occupation in the Northwestern Great Plains states of Montana, Wyoming, North Dakota, and South Dakota is reviewed here. -
1 a Film by Roger J. Kuhns What Was It Like in Door County Wisconsin 425 Million Years Ago? What
a film by Roger J. Kuhns www.rogerjameskuhns.com What was it like in Door County Wisconsin 425 million years ago? What has gone on in the geologic and biologic past beneath our feet? What are the changes we’re experiencing now? What might the future hold for our land, water, environment and communities? “Escarpment” is the natural history story of Eastern Wisconsin and the Niagara Escarpment region of the Great Lakes. The film was shot on location along the entire length of the Niagara Escarpment, with a Door County focus. It is a fast-paced fun voyage through billions of years of Eastern Wisconsin geologic and biologic past. The film reconstructs ecosystems that existed when the dolomitic rocks of the Niagara Escarpment were formed, considers if dinosaurs ever walked in what is now Door County, follows the path of glaciers, and many other major events in our rich geologic past. Locations around the world are featured to show what Eastern Wisconsin was like in the past. Animated sequences are used to illustrate parts of the story. The film helps to inform, enlighten, and guide us towards being better stewards of the land, and takes a glimpse of what a sustainable future might look like. In the spirit of Discovery Channel and National Geographic films, geologist and sustainologist Roger Kuhns produced this film for all ages. Kuhns has worked on the Niagara Escarpment and Great Lakes geology and ecology during the course of his career. FILM: Escarpment GENRE: Science / Nature / Travel PRODUCED BY: Roger J. Kuhns RUN TIME: 1 hour 33 minutes PRODUCTION: musicTOears Press CONTACT INFO: [email protected] / 860-910-8525 AVAILABLE AT: www.rogerjameskuhns.com MOVIE TRAILER: https://www.youtube.com/watch?v=YAyRp7VYFWs 1 2017-2018 Reviews from viewers of a film by Roger J. -
Historic Overview
Updated Reconnaissance Level Survey of Historic Resources Town of Amherst HISTORIC OVERVIEW LOCATION The Town of Amherst lies in northern Erie County, New York. It is bordered by Niagara County to the north, the Erie County towns of Clarence to the east, Cheektowaga to the south, and Tonawanda to the west. The total area of Amherst is approximately 53 square miles. ENVIRONMENTAL SETTING The natural environmental setting influenced prehistoric and historic settlement patterns in the Town of Amherst. The town lies within the Erie‐Ontario Lake Plain physiographic province, described as a nearly level lowland plain with few prominent topographic features. The area is underlain by Onondaga limestone dating to the Late Devonian period. Later glaciations shaped much of the western New York topography, including that of Amherst. One of the most prominent topographic features in the relatively featureless province is the Onondaga Escarpment, an east‐west trending hard limestone bedrock formation that lies in the southern portion of the Town of Amherst. The Onondaga Escarpment proved resistant to the effects of glacial scouring and it forms the southern boundary of a large basin once occupied by the shallow glacial Lake Tonawanda. Lake Tonawanda eventually receded leaving behind wetlands and deposits of clay and sand throughout much of northern Amherst (Owens et al. 1986:2). The most important drainages in the Town of Amherst are Tonawanda Creek, Ransom Creek, and Ellicott Creek. Tonawanda Creek forms the northern boundary between Amherst and Niagara County. It flows in a western direction and drains much of the eastern and Northern portions of Amherst. -
Landform Regions of Iowa — 2000
LANDFORM REGIONS OF IOWA LANDFORM REGIONS2000 OF IOWA — 2000 0 20 40 60 miles 0 20 40 60 miles 0 40 80 kilometers 0 40 80 kilometers 327 Trowbridge Hall Iowa Department of NaturalIowa City, Resources Iowa 52242-1319 Geological Survey Bureau 109 Trowbridge Hallwww.iowageologicalsurvey.org Iowa City, Iowa 52242-1319 319-335-1575 Hydroscience & Engineering www.igsb.uiowa.edu Printed on recycled paper A landscape is a collection of shapes or landforms. LANDFORM REGIONS In Iowa, these shapes are composed of earth materials OF IOWA derived from glacial, wind, river, and marine environments of the geologic past. This map is a guide to seeing the state’s remarkably diverse landscapes and www.iowageologicalsurvey.org landform features. 319-335-1575 The Des Moines Lobe Southern Iowa Drift Plain Paleozoic Plateau The last glacier to enter Iowa advanced in a series of surges This region is dominated by glacial deposits left by ice Narrow valleys deeply carved into sedimentary rock beginning just 15,000 years ago and reached its southern sheets that extended south into Missouri over 500,000 of Paleozoic age and a near-absence of glacial deposits limit, the site of modern-day Des Moines, 14,000 years years ago. The deposits were carved by deepening define this scenic region. Fossil-bearing strata originated ago. By 12,000 years ago, the ice sheet was gone, leaving episodes of stream erosion so that only a horizon line as sediment on tropical sea floors between 300 and 550 behind a poorly drained landscape of pebbly deposits of hill summits marks the once-continuous glacial plain. -
Characterization of Ecoregions of Idaho
1 0 . C o l u m b i a P l a t e a u 1 3 . C e n t r a l B a s i n a n d R a n g e Ecoregion 10 is an arid grassland and sagebrush steppe that is surrounded by moister, predominantly forested, mountainous ecoregions. It is Ecoregion 13 is internally-drained and composed of north-trending, fault-block ranges and intervening, drier basins. It is vast and includes parts underlain by thick basalt. In the east, where precipitation is greater, deep loess soils have been extensively cultivated for wheat. of Nevada, Utah, California, and Idaho. In Idaho, sagebrush grassland, saltbush–greasewood, mountain brush, and woodland occur; forests are absent unlike in the cooler, wetter, more rugged Ecoregion 19. Grazing is widespread. Cropland is less common than in Ecoregions 12 and 80. Ecoregions of Idaho The unforested hills and plateaus of the Dissected Loess Uplands ecoregion are cut by the canyons of Ecoregion 10l and are disjunct. 10f Pure grasslands dominate lower elevations. Mountain brush grows on higher, moister sites. Grazing and farming have eliminated The arid Shadscale-Dominated Saline Basins ecoregion is nearly flat, internally-drained, and has light-colored alkaline soils that are Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and America into 15 ecological regions. Level II divides the continent into 52 regions Literature Cited: much of the original plant cover. Nevertheless, Ecoregion 10f is not as suited to farming as Ecoregions 10h and 10j because it has thinner soils. -
CONTEXT DOCUMENT on the FUR TRADE of NORTHEASTERN
CONTEXT DOCUMENT on the FUR TRADE OF NORTHEASTERN NORTH DAKOTA (Ecozone #16) 1738-1861 by Lauren W. Ritterbush April 1991 FUR TRADE IN NORTHEASTERN NORTH DAKOTA {ECOZONE #16). 1738-1861 The fur trade was the commercia1l medium through which the earliest Euroamerican intrusions into North America were made. Tl;ns world wide enterprise led to the first encounters between Euroamericar:is and Native Americans. These contacts led to the opening of l1ndian lands to Euroamericans and associated developments. This is especial,ly true for the h,istory of North Dakota. It was a fur trader, Pierre Gaultier de Varennes, Sieur de la Ve--endrye, and his men that were the first Euroamericans to set foot in 1738 on the lar;ids later designated part of the state of North Dakota. Others followed in the latter part of the ,eighteenth and first half of the nineteenth century. The documents these fur traders left behind are the earliest knowr:i written records pertaining to the region. These ,records tell much about the ear,ly commerce of the region that tied it to world markets, about the indigenous popu,lations living in the area at the time, and the environment of the region before major changes caused by overhunting, agriculture, and urban development were made. Trade along the lower Red River, as well as along, the Misso1.:1ri River, was the first organized E uroamerican commerce within the area that became North Dakota. Fortunately, a fair number of written documents pertainir.1g to the fur trade of northeastern North 0akota have been located and preserved for study.