Geologic Framework and Glaciation of the Central Area Christopher L
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
I I I I I I I I I 1 I 1 I I I I I
I I WISCONSIN I A Summary of Cooperative Water Resources Investigations I U.S. Geological Survey and I Wisconsin Department of Natural Resources I I I I 1 I 1 I I I I I I 2000 USGS I science for a changing world I I I I I I I I I I I I I I I I I 1 I I I A SUMMARY OF COOPERATIVE WATER-RESOURCES INVESTIGATIONS U.S. GEOLOGICAL SURVEY Water Resources Division I 8505 Research Way Middleton, Wisconsin 53562 and I WISCONSIN DEPARTMENT OF NATURAL RESOURCES P.O. Box 7921 I Madison, Wisconsin 53707 I I I I I I I I i 2000 i I I I I I I I I I I I I I I I I I 1 I A Summary of Cooperative Water-Resources Investigations « U.S. Geological Survey and Wisconsin Department of Natural Resources .- "V-._.-;; , - 2000 The cooperative program of water-resources investigations between the U.S. Geological Survey and the Wisconsin Department of Natural Resources began as a continuation of cooperative programs with the various State agencies which were merged to form the Wisconsin Department of Natural Resources. These investigations involve various aspects of research, resource evaluations, and water-quantity- and water- quality-monitoring activities. This is a brief summary report of the activities and plans for the cooperative projects during the July 1999 through June 2000 fiscal year. Each project summary includes a brief description of the objectives, approach, and progress during the 2000 fiscal year, and plans for the 2001 fiscal year. -
Lexicon of Pleistocene Stratigraphic Units of Wisconsin
Lexicon of Pleistocene Stratigraphic Units of Wisconsin ON ATI RM FO K CREE MILLER 0 20 40 mi Douglas Member 0 50 km Lake ? Crab Member EDITORS C O Kent M. Syverson P P Florence Member E R Lee Clayton F Wildcat A Lake ? L L Member Nashville Member John W. Attig M S r ik be a F m n O r e R e TRADE RIVER M a M A T b David M. Mickelson e I O N FM k Pokegama m a e L r Creek Mbr M n e M b f a e f lv m m i Sy e l M Prairie b C e in Farm r r sk er e o emb lv P Member M i S ill S L rr L e A M Middle F Edgar ER M Inlet HOLY HILL V F Mbr RI Member FM Bakerville MARATHON Liberty Grove M Member FM F r Member e E b m E e PIERCE N M Two Rivers Member FM Keene U re PIERCE A o nm Hersey Member W le FM G Member E Branch River Member Kinnickinnic K H HOLY HILL Member r B Chilton e FM O Kirby Lake b IG Mbr Boundaries Member m L F e L M A Y Formation T s S F r M e H d l Member H a I o V r L i c Explanation o L n M Area of sediment deposited F e m during last part of Wisconsin O b er Glaciation, between about R 35,000 and 11,000 years M A Ozaukee before present. -
Vegetation and Fire at the Last Glacial Maximum in Tropical South America
Past Climate Variability in South America and Surrounding Regions Developments in Paleoenvironmental Research VOLUME 14 Aims and Scope: Paleoenvironmental research continues to enjoy tremendous interest and progress in the scientific community. The overall aims and scope of the Developments in Paleoenvironmental Research book series is to capture this excitement and doc- ument these developments. Volumes related to any aspect of paleoenvironmental research, encompassing any time period, are within the scope of the series. For example, relevant topics include studies focused on terrestrial, peatland, lacustrine, riverine, estuarine, and marine systems, ice cores, cave deposits, palynology, iso- topes, geochemistry, sedimentology, paleontology, etc. Methodological and taxo- nomic volumes relevant to paleoenvironmental research are also encouraged. The series will include edited volumes on a particular subject, geographic region, or time period, conference and workshop proceedings, as well as monographs. Prospective authors and/or editors should consult the series editor for more details. The series editor also welcomes any comments or suggestions for future volumes. EDITOR AND BOARD OF ADVISORS Series Editor: John P. Smol, Queen’s University, Canada Advisory Board: Keith Alverson, Intergovernmental Oceanographic Commission (IOC), UNESCO, France H. John B. Birks, University of Bergen and Bjerknes Centre for Climate Research, Norway Raymond S. Bradley, University of Massachusetts, USA Glen M. MacDonald, University of California, USA For futher -
Lake Ontario a Voice!
Statue Stories Chicago: The Public Writing Competition Give Lake Ontario a voice! Behind the Art Institute of Chicago, is the Fountain of the Great Lakes. Within the famous fountain is the wistful figure of Lake Ontario. She sits apart from her sister lakes, gazing into the distance with arms outstretched. But what does she have to say for herself? Write a Monologue! Monologos means “speaking alone” in Greek, but we all know that people who speak without thinking about their listener can be very dull indeed. Your challenge is to find a ‘voice’ for your statue and to write an engaging monologue in 350 words. Get under your statue’s skin! Look closely and develop a sense of empathy with the sculpture and imagine how it would feel. How does Lake Ontario feel about her sister lakes? Invite your listener to feel with you: create shifts in tempo and emotion, use different tenses, figures of speech and anecdotes, sensory details and even sound effects. Finding your sculpture’s voice? Write in the first person and adopt the persona of your character: What kind of vocabulary will you use - your own or that of another era/dialect? Your words will be spoken so read them aloud: use their rhythm and your sentence structure to convey emotion and urgency. Read great monologues for inspiration, for example Hamlet’s Alas Poor Yorick, or watch film monologues, like Morgan Freeman’s in The Shawshank Redemption. How will you keep people listening? Structure your monologue! How will you introduce yourself? With a greeting, a warning, a question, an order, a riddle? Grab and hold your listener’s attention from your very first line. -
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 -
The Big Chill
THE BIG CHILL Royal Saskatchewan Museum THE BIG CHILL For further information please contact: Public Programs Royal Saskatchewan Museum 2445 Albert Street Regina, Saskatchewan S4P 4W7 Email: [email protected] Website: www.royalsaskmuseum.ca © Royal Saskatchewan Museum 2012 The contents of this resource package may be reproduced for classroom use only. No portion may be duplicated for publication or sale. The following material provides teachers and students with information about the Ice Age in what is now Saskatchewan (remember, there was no such thing as Saskatchewan in those days!): • To describe Saskatchewan’s climate during the Ice Age. • To illustrate the geological effects of glaciation. • To recognize a variety of animals that lived in Saskatchewan during the Ice Age. Vocabulary advance geology climate glacier debris ice age deposit drumlin esker meltwater erratic moraine evaporation fauna retreat flora stagnant flow till fossil Laurentide Ice Sheet knob and kettle Wisconsin Glacial Period Pleistocene Epoch BACKGROUND INFORMATION Ice Ages The Ice Age or Pleistocene Epoch refers to the last two million years of our geological history when there were at least five periods of glaciation in North America. Gradual climate cooling caused huge continental ice sheets to form. Later, gradual warming caused these to melt during the interglacial periods. The last glacier began forming approximately 110,000 years ago, building until it covered all but the Cypress Hills and the Wood Mountain Plateau region of the Province. The last interglacial period started about 17,000 years ago. The ice sheet melted completely from our borders about 10,000 years ago. This last period of glaciation is called the Wisconsin Glacial Period. -
Indiana Glaciers.PM6
How the Ice Age Shaped Indiana Jerry Wilson Published by Wilstar Media, www.wilstar.com Indianapolis, Indiana 1 Previiously published as The Topography of Indiana: Ice Age Legacy, © 1988 by Jerry Wilson. Second Edition Copyright © 2008 by Jerry Wilson ALL RIGHTS RESERVED 2 For Aaron and Shana and In Memory of Donna 3 Introduction During the time that I have been a science teacher I have tried to enlist in my students the desire to understand and the ability to reason. Logical reasoning is the surest way to overcome the unknown. The best aid to reasoning effectively is having the knowledge and an understanding of the things that have previ- ously been determined or discovered by others. Having an understanding of the reasons things are the way they are and how they got that way can help an individual to utilize his or her resources more effectively. I want my students to realize that changes that have taken place on the earth in the past have had an effect on them. Why are some towns in Indiana subject to flooding, whereas others are not? Why are cemeteries built on old beach fronts in Northwest Indiana? Why would it be easier to dig a basement in Valparaiso than in Bloomington? These things are a direct result of the glaciers that advanced southward over Indiana during the last Ice Age. The history of the land upon which we live is fascinating. Why are there large granite boulders nested in some of the fields of northern Indiana since Indiana has no granite bedrock? They are known as glacial erratics, or dropstones, and were formed in Canada or the upper Midwest hundreds of millions of years ago. -
St. Louis River Natural Area to the DULUTH NATURAL AREAS PROGRAM DATE: 3/7/19
NOMINATION OF THE St. Louis River Natural Area TO THE DULUTH NATURAL AREAS PROGRAM DATE: 3/7/19 Nominated by: City of Duluth Parks & Recreation Division This report was produced by the Minnesota Land Trust under contract to the City of Duluth and funded by U.S. Environmental Protection Agency Great Lakes Restoration Initiative grant number GL00E02202. Many organizations and individuals participated in a variety of ways as collaborators to the report. St. Louis River Natural Area Nomination DRAFT 3/7/19 Table of Contents Executive Summary ..................................................................................................................... iii Introduction ................................................................................................................................1 Eligibility ......................................................................................................................................2 − Land Ownership ......................................................................................................................... 2 − Scientific Criteria ........................................................................................................................ 3 References ................................................................................................................................. 10 Figures .......................................................................................................................................12 Appendices ................................................................................................................................36 -
The Geomorphology and Alluvial History of Matzhiwin Creek, a Small Tributary of the Red Deer River in Southern Alberta
(3x mm awmsraais UNIVERSITY OF ALBERTA RELEASE FORM NAME OF AUTHOR: Mark Barling TITLE OF THESIS: The geomorphology and alluvial history of Matzhiwin Creek, a small tributary of the Red Deer River in southern Alberta. DEGREE: Master of Science YEAR THIS DEGREE PRESENTED: Fall 1995 Permission is hereby granted to the University of Alberta Library to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. The author reserves all other publication and other rights in association with the copyright in the thesis, and except as hereinbefore provided neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatever without the author's prior written permission. UNIVERSITY OF ALBERTA The geomorphology and alluvial history of Matzhiwin Creek, a small tributary of the Red Deer River in southern Alberta. By Mark Bariing A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfilment of the requirements for the degree of Master of Science. Department of Geography Edmonton, Alberta Fall 1995 UNIVERSITY OF ALBERTA FACULTY OF GRADUATE STUDIES AND RESEARCH The undersigned certify that they have read, and recommend to the Faculty of Graduate Studies and Research for acceptance, a thesis entitled THE GEOMORPHOLOGY AND ALLUVIAL HISTORY OF MATZHIWIN CREEK, A SMALL TRIBUTARY OF THE . RED DEER RIVER IN SOUTHERN ALBERTA submitted by MARK BARLING in partial fulfilment of the requirements for the degree of MASTER OF SCIENCE. Abstract This study examines the postglacial alluvial chronologies of some of the rivers and creeks in central and southern Alberta. -
Constraints on Lake Agassiz Discharge Through the Late-Glacial Champlain Sea (St
Quaternary Science Reviews xxx (2011) 1e10 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Constraints on Lake Agassiz discharge through the late-glacial Champlain Sea (St. Lawrence Lowlands, Canada) using salinity proxies and an estuarine circulation model Brandon Katz a, Raymond G. Najjar a,*, Thomas Cronin b, John Rayburn c, Michael E. Mann a a Department of Meteorology, 503 Walker Building, The Pennsylvania State University, University Park, PA 16802, USA b United States Geological Survey, 926A National Center, 12201 Sunrise Valley Drive, Reston, VA 20192, USA c Department of Geological Sciences, State University of New York at New Paltz, 1 Hawk Drive, New Paltz, NY 12561, USA article info abstract Article history: During the last deglaciation, abrupt freshwater discharge events from proglacial lakes in North America, Received 30 January 2011 such as glacial Lake Agassiz, are believed to have drained into the North Atlantic Ocean, causing large Received in revised form shifts in climate by weakening the formation of North Atlantic Deep Water and decreasing ocean heat 25 July 2011 transport to high northern latitudes. These discharges were caused by changes in lake drainage outlets, Accepted 5 August 2011 but the duration, magnitude and routing of discharge events, factors which govern the climatic response Available online xxx to freshwater forcing, are poorly known. Abrupt discharges, called floods, are typically assumed to last months to a year, whereas more gradual discharges, called routing events, occur over centuries. Here we Keywords: Champlain sea use estuarine modeling to evaluate freshwater discharge from Lake Agassiz and other North American Proglacial lakes proglacial lakes into the North Atlantic Ocean through the St. -
Bildnachweis
Bildnachweis Im Bildnachweis verwendete Abkürzungen: With permission from the Geological Society of Ame- rica l – links; m – Mitte; o – oben; r – rechts; u – unten 4.65; 6.52; 6.183; 8.7 Bilder ohne Nachweisangaben stammen vom Autor. Die Autoren der Bildquellen werden in den Bildunterschriften With permission from the Society for Sedimentary genannt; die bibliographischen Angaben sind in der Literaturlis- Geology (SEPM) te aufgeführt. Viele Autoren/Autorinnen und Verlage/Institutio- 6.2ul; 6.14; 6.16 nen haben ihre Einwilligung zur Reproduktion von Abbildungen gegeben. Dafür sei hier herzlich gedankt. Für die nachfolgend With permission from the American Association for aufgeführten Abbildungen haben ihre Zustimmung gegeben: the Advancement of Science (AAAS) Box Eisbohrkerne Dr; 2.8l; 2.8r; 2.13u; 2.29; 2.38l; Box Die With permission from Elsevier Hockey-Stick-Diskussion B; 4.65l; 4.53; 4.88mr; Box Tuning 2.64; 3.5; 4.6; 4.9; 4.16l; 4.22ol; 4.23; 4.40o; 4.40u; 4.50; E; 5.21l; 5.49; 5.57; 5.58u; 5.61; 5.64l; 5.64r; 5.68; 5.86; 4.70ul; 4.70ur; 4.86; 4.88ul; Box Tuning A; 4.95; 4.96; 4.97; 5.99; 5.100l; 5.100r; 5.118; 5.119; 5.123; 5.125; 5.141; 5.158r; 4.98; 5.12; 5.14r; 5.23ol; 5.24l; 5.24r; 5.25; 5.54r; 5.55; 5.56; 5.167l; 5.167r; 5.177m; 5.177u; 5.180; 6.43r; 6.86; 6.99l; 6.99r; 5.65; 5.67; 5.70; 5.71o; 5.71ul; 5.71um; 5.72; 5.73; 5.77l; 5.79o; 6.144; 6.145; 6.148; 6.149; 6.160; 6.162; 7.18; 7.19u; 7.38; 5.80; 5.82; 5.88; 5.94; 5.94ul; 5.95; 5.108l; 5.111l; 5.116; 5.117; 7.40ur; 8.19; 9.9; 9.16; 9.17; 10.8 5.126; 5.128u; 5.147o; 5.147u;