The Quaternary History of the Cordilleran Ice Sheet Fringe

Total Page:16

File Type:pdf, Size:1020Kb

The Quaternary History of the Cordilleran Ice Sheet Fringe THE QUATERNARY HISTORY OF THE CORDILLERAN ICE SHEET FRINGE, ASHLEY LAKE AREA, MONTANA by Denny Lane Capps A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Science MONTANA STATE UNIVERSITY Bozeman, Montana January 2004 ©Copyright by Denny Lane Capps 2004 All Rights Reserved ii APPROVAL of a thesis submitted by Denny Lane Capps This thesis has been read by each member of the thesis committee and has been found to be satisfactory regarding content, English usage, format, citations, bibliographic style, and consistency, and is ready for submission to the College of Graduate Studies. Dr. William Locke Approved for the Department of Earth Sciences Dr. David Lageson Approved for the College of Graduate Studies Dr. Bruce McLeod iii STATEMENT OF PERMISSION TO USE In presenting this thesis in partial fulfillment of the requirements for a master’s degree at Montana State University, I agree that the Library shall make it available to borrowers under rules of the Library. If I have indicated my intention to copyright this thesis by including a copyright notice page, copying is allowable only for scholarly purposes, consistent with “fair use” as prescribed in the U.S. Copyright Law. Requests for permission for extended quotation from or reproduction of this thesis in whole or parts may be granted only by the copyright holder. Denny Lane Capps January 12th, 2004 iv ACKNOWLEDGEMENTS 1. Dr. William Locke, advisor, who was always there, introduced me to the problem and oversaw the project work 2. Dr. Kenneth Pierce, committee member, who shared his extensive field knowledge and encouragement throughout the project 3. Dr. John Montagne, committee member, who selflessly gave his time to the betterment of this thesis 4. This study was primarily funded by a generous donation of the Donald Smith Memorial Scholarship Fund 5. Jeff Deems – friend and colleague, continuous encouragement and positive criticism 6. Dr. Larry Smith – Montana Bureau of Mines and Geology – regional geologic information and encouragement 7. Gamma Family – land access, hospitality and local information 8. Scott Larson – field assistance 9. Plum Creek Timber Company – land access and aerial photos 10. Stoltz Timber Company – land access and maps 11. Flathead National Forest – especially Jane Kollmeyer, District Ranger – painless permitting and campground use 12. Dr. Sharon Eversman – MSU Department of Ecology – plant identification 13. Brist Family – land access 14. Montana DNRC - lake bathymetry v TABLE OF CONTENTS 1. INTRODUCTION..............................................................................................................................1 Problem.........................................................................................................................1 Objective.......................................................................................................................8 Study Area .................................................................................................................... 8 Regional Setting.................................................................................................... 10 Topography..................................................................................................... 10 Geology........................................................................................................... 11 Climate............................................................................................................ 15 Ice ................................................................................................................... 16 Vegetation....................................................................................................... 19 Local Setting ......................................................................................................... 19 Topography..................................................................................................... 19 Geology........................................................................................................... 20 Climate............................................................................................................ 23 Ice ................................................................................................................... 24 Vegetation....................................................................................................... 24 2. METHODS .......................................................................................................................................26 Erratics ........................................................................................................................ 26 Depositional Landforms.............................................................................................. 28 Moraines ............................................................................................................... 29 Kames ................................................................................................................... 29 Glacial Depressions .............................................................................................. 29 Erosional Landforms................................................................................................... 30 Lateral Meltwater Channels.................................................................................. 30 Direct Overflow Channels .................................................................................... 31 Weathering Rinds........................................................................................................ 32 Bog Augering.............................................................................................................. 36 Tephras.................................................................................................................. 37 Radiocarbon .......................................................................................................... 39 Ice Modeling ............................................................................................................... 40 vi TABLE OF CONTENTS - CONTINUED 3. RESULTS..........................................................................................................................................43 Erratics ........................................................................................................................ 43 Depositional Landforms.............................................................................................. 45 Moraines ............................................................................................................... 45 Kames ................................................................................................................... 47 Glacial Depressions .............................................................................................. 47 Erosional Landforms................................................................................................... 49 Lateral Meltwater Channels.................................................................................. 49 Direct Overflow Channels .................................................................................... 49 Weathering Rinds........................................................................................................ 50 Bog Augering.............................................................................................................. 52 Tephras.................................................................................................................. 52 Radiocarbon .......................................................................................................... 55 Varves ................................................................................................................... 57 Ice Modeling ............................................................................................................... 58 4. DISCUSSION ..................................................................................................................................62 Discussion of Features ................................................................................................ 62 Erratics .................................................................................................................. 62 Depositional Landforms........................................................................................ 63 Erosional Landforms............................................................................................. 65 Weathering Rinds.................................................................................................. 65 Bog Augering........................................................................................................ 66 Defining Significant Ice Margins that Created Figures .............................................. 67 Erratics .................................................................................................................. 67 Depositional Landforms........................................................................................ 70 Erosional Landforms............................................................................................. 73 Bog Augering.......................................................................................................
Recommended publications
  • The Cordilleran Ice Sheet 3 4 Derek B
    1 2 The cordilleran ice sheet 3 4 Derek B. Booth1, Kathy Goetz Troost1, John J. Clague2 and Richard B. Waitt3 5 6 1 Departments of Civil & Environmental Engineering and Earth & Space Sciences, University of Washington, 7 Box 352700, Seattle, WA 98195, USA (206)543-7923 Fax (206)685-3836. 8 2 Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada 9 3 U.S. Geological Survey, Cascade Volcano Observatory, Vancouver, WA, USA 10 11 12 Introduction techniques yield crude but consistent chronologies of local 13 and regional sequences of alternating glacial and nonglacial 14 The Cordilleran ice sheet, the smaller of two great continental deposits. These dates secure correlations of many widely 15 ice sheets that covered North America during Quaternary scattered exposures of lithologically similar deposits and 16 glacial periods, extended from the mountains of coastal south show clear differences among others. 17 and southeast Alaska, along the Coast Mountains of British Besides improvements in geochronology and paleoenvi- 18 Columbia, and into northern Washington and northwestern ronmental reconstruction (i.e. glacial geology), glaciology 19 Montana (Fig. 1). To the west its extent would have been provides quantitative tools for reconstructing and analyzing 20 limited by declining topography and the Pacific Ocean; to the any ice sheet with geologic data to constrain its physical form 21 east, it likely coalesced at times with the western margin of and history. Parts of the Cordilleran ice sheet, especially 22 the Laurentide ice sheet to form a continuous ice sheet over its southwestern margin during the last glaciation, are well 23 4,000 km wide.
    [Show full text]
  • Land Ice, Paleoclimate and Polar Climate Working Groups
    2019 WG Meetings Land Ice, Paleoclimate and Polar Climate Working Groups Simulating the Northern Hemisphere climate and ice sheets during the last deglaciation with CESM2.1/CISM2.1 Petrini M. & Bradley S.L February 4, 2019 Study area and scientific motivations Study area: • At Last Glacial Maximum, ~21 ka, three large ice sheets: CIS Greenland, North American, Eurasian; LIS IIS GIS BSIS FIS BIIS Ice sheet reconstruction for initial LGM boundary conditions, from BRITICE-CHRONO + Lecavalier et al., 2014. Eurasian Ice Sheet complex: Fennoscandian Ice Sheet (FIS), Barents Sea Ice Sheet (BSIS), British-Irish Ice Sheet (BIIS). North American Ice Sheet complex: Laurentide Ice Sheet (LIS), Cordilleran Ice Sheet (CIS), Innuitian Ice Sheet (IIS). Study area and scientific motivations Study area: • At Last Glacial Maximum, ~21 ka, three continental ice sheets: CIS Greenland, North American, Eurasian; • Sea level ~132±2 m lower: 76.0±6.7 Eurasian: 18.4±4.9 m SLE North American: 76.0±6.7 m SLE LIS IIS Greenland: 4.1±1.0 m SLE. f (Simms et al., 2019 QSR) GIS BSIS 4.1±1.0 FIS BIIS 18.4±4.9 Ice sheet reconstruction for initial LGM boundary conditions, from BRITICE-CHRONO + Lecavalier et al., 2014. Eurasian Ice Sheet complex: Fennoscandian Ice Sheet (FIS), Barents Sea Ice Sheet (BSIS), British-Irish Ice Sheet (BIIS). North American Ice Sheet complex: Laurentide Ice Sheet (LIS), Cordilleran Ice Sheet (CIS), Innuitian Ice Sheet (IIS). Study area and scientific motivations Study area: • At Last Glacial Maximum, ~21 ka, three continental ice sheets: CIS Greenland, North American, Eurasian; • Sea level ~132±2 m lower: Eurasian: 18.4±4.9 m SLE North American: 76.0±6.7 m SLE LIS IIS Greenland: 4.1±1.0 m SLE.
    [Show full text]
  • Jette Meadows SWDAR
    JETTE MEADOWS LANDOWNERS ASSOCIATION PHASE I Phase I-PWS ID # MT0003100 JETTE MEADOWS LANDOWNERS ASSOCIATION PHASE II Phase II-PWS ID # MT0003101 PUBLIC WATER SUPPLIES SOURCE WATER DELINEATION AND ASSESSMENT REPORTS Lake County, Montana 24 APRIL 2006 PREPARED FOR: JETTE MEADOWS LANDOWNERS ASSOCIATION PHASE I JETTE MEADOWS LANDOWNERS ASSOCIATION PHASE II PUBLIC WATER SUPPLIES Robert Gambrel, Administrative Contact Eva Gambrel, Financial Contact Clay A. Sloan, Operator PO Box 34 Polson, Montana 59860 Phone: 406/ 883-0911 or / 885-7556 PREPARED BY: MONTANA DEPARTMENT OF ENVIRONMENTAL Jette Meadows Landowners Assoc. Phase I & II SWDAR (combined) MT0003100 & MT0003101 QUALITY Source Water Protection Program Jeffrey Frank Herrick, Hydrogeologist P.O. Box 200901 Helena, Montana 59620-0901 ii Jette Meadows Landowners Assoc. Phase I & II SWDAR (combined) MT0003100 & MT0003101 iii Jette Meadows Landowners Assoc. Phase I & II SWDAR (combined) MT0003100 & MT0003101 EXECUTIVE SUMMARY This Source Water Delineation and Assessment Report was prepared under the Federal Safe Drinking Water Act and the Montana Source Water Assessment Plan. The Montana Department of Environmental Quality (DEQ) is ensuring that assessments are completed for all public water systems in Montana. The purpose of these reports is to provide information so that the public water system operator, consumers, and community citizens can begin developing strategies to protect your source of drinking water. The information that is provided includes the identification of the area most critical to maintaining safe drinking water, i.e., the Inventory Region, an inventory of potential sources of contamination within this area, and an assessment of the relative threat that these potential sources pose to the water system.
    [Show full text]
  • Advance and Retreat of Cordilleran Ice Sheets in Washington, U.S.A
    Document généré le 4 oct. 2021 19:12 Géographie physique et Quaternaire Advance and Retreat of Cordilleran Ice Sheets in Washington, U.S.A. Avancée et recul des inlandsis de la Cordillère dans l’État de Washington (É.-U.) Vorstoß und Rückzug der Kordilleren-Eisdecke in Washington State. U.S.A. Don J. Easterbrook Volume 46, numéro 1, 1992 Résumé de l'article Dans la Cordillère, les glaciations se sont produites selon des modes URI : https://id.erudit.org/iderudit/032888ar caractéristiques d'avancée et de recul : 1) dépôts fluvioglaciaires d'avancée; 2) DOI : https://doi.org/10.7202/032888ar poli glaciaire; 3) till; 4) dépôts fluvio-glaciaires de retrait au sud de Seattle, dans le sud des basses-terres de Puget, dépôts glacio-marins dans les basses-terres Aller au sommaire du numéro du nord, et eskers, terrasses fluvioglaciaires et petites moraines sur le plateau de Columbia. La datation au radiocarbone indique que les lobes de Puget et de Juan de Fuca ont avancé et reculé synchroniquement. Parmi les preuves qui Éditeur(s) nous contraignent à rejeter l'hypothèse selon laquelle un front en fusion, qui vêlait, serait à l'origine des dépôts glacio-marins, citons : 1) les nombreuses Les Presses de l'Université de Montréal datations au radiocarbone qui révèlent la mise en place simultanée de dépôts glacio-marins sur tout le territoire; 2) les dépôts issus de la fusion de la glace ISSN stagnante, intimement associés aux dépôts glacio-marins; 3) les preuves irréfutables d'une origine autre que marine des sables de Deming qui révèlent 0705-7199 (imprimé) que la Cordillère était libre de glace immédiatement avant la mise en place des 1492-143X (numérique) dépôts glacio-marins.
    [Show full text]
  • Level IV Ecoregions of Montana
    DRAFT 2 Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and quantity of environmental resources; they are designed to serve as a spatial framework for the research, assessment, management, and monitoring of ecosystems and ecosystem components. By recognizing the spatial differences in the capacities and potentials of ecosystems, ecoregions stratify the environment by its Ecoregions of Montana probable response to disturbance (Bryce and others, 1999). These general purpose regions are critical for Second Edition structuring and implementing ecosystem management strategies across federal agencies, state agencies, and nongovernment organizations that are responsible for different types of resources within the same 116° 115° 114° 113° 112° 111° 110° 109° 108° 107° 106° 105° 104° geographical areas (Omernik and others, 2000). ° 49° The approach used to compile this map is based on the premise that ecological regions can be identified 49 BRITISH COLUMBIA 42d through the analysis of the spatial patterns and the composition of biotic and abiotic phenomena that affect ALBERTA SASKATCHEWAN 42k or reflect differences in ecosystem quality and integrity (Wiken, 1986; Omernik, 1987, 1995). These 15d CANADA 15h 41b 42q 42n sa 17r ATE S phenomena include geology, physiography, vegetation, climate, soils, land use, wildlife, and hydrology. u F 41a 42l UNITED ST n l Plentywood a a 42n 42r 42m Scobey c th 42r o e The relative importance of each characteristic varies from one ecological region to another regardless of o a 42r K d R e i 42r 17r the hierarchical level. A Roman numeral hierarchical scheme has been adopted for different levels of k v a 41c e r Fresno 15h L 42i 42b 42d ecological regions.
    [Show full text]
  • Animating the Temporal Progression of Cordilleran Deglaciation and Vegetation Succession in the Pacific Northwest During the Late Quaternary Period
    Western Washington University Western CEDAR Scholars Week 2017 - Poster Presentations May 17th, 9:00 AM - 12:00 PM Animating the Temporal Progression of Cordilleran Deglaciation and Vegetation Succession in the Pacific Northwest during the late Quaternary Period Henry Haro Western Washington University Follow this and additional works at: https://cedar.wwu.edu/scholwk Part of the Environmental Studies Commons, and the Higher Education Commons Haro, Henry, "Animating the Temporal Progression of Cordilleran Deglaciation and Vegetation Succession in the Pacific Northwest during the late Quaternary Period" (2017). Scholars Week. 20. https://cedar.wwu.edu/scholwk/2017/Day_one/20 This Event is brought to you for free and open access by the Conferences and Events at Western CEDAR. It has been accepted for inclusion in Scholars Week by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. Animating the Temporal Progression of Cordilleran Deglaciation in the Pacific Northwest during the late Quaternary Period Henry Haro – 2017 The Cordilleran Ice Sheet Sequential Progression of Cordilleran Retreat The topography of the Pacific Northwest, its fjords, inland waterways and islands, are a result of an extended period of glaciation and glacial retreat. This retreat influenced the physical features and the resulting succession of vegetation that led to the landscape we see today. Despite this importance of the Cordilleran ice sheet and the large volume of research on the topic, there lacks a good detailed animation of the movement of the entire ice sheet from the last glacial maximum to the present day. In this study, I used spatial data of the glacial extent at different periods of time during the Quaternary period to model and animate the movement of the Cordilleran ice sheet as it retreated from 18,000 BCE to 10,000 BCE.
    [Show full text]
  • Climate Investigations Using Ice Sheet and Mass Balance Models with Emphasis on North American Glaciation Sean David Birkel
    The University of Maine DigitalCommons@UMaine Electronic Theses and Dissertations Fogler Library 2010 Climate Investigations Using Ice Sheet and Mass Balance Models with Emphasis on North American Glaciation Sean David Birkel Follow this and additional works at: http://digitalcommons.library.umaine.edu/etd Part of the Glaciology Commons Recommended Citation Birkel, Sean David, "Climate Investigations Using Ice Sheet and Mass Balance Models with Emphasis on North American Glaciation" (2010). Electronic Theses and Dissertations. 97. http://digitalcommons.library.umaine.edu/etd/97 This Open-Access Dissertation is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of DigitalCommons@UMaine. CLIMATE INVESTIGATIONS USING ICE SHEET AND MASS BALANCE MODELS WITH EMPHASIS ON NORTH AMERICAN GLACIATION By Sean David Birkel B.S. University of Maine, 2002 M.S. University of Maine, 2004 A THESIS Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy (in Earth Sciences) The Graduate School The University of Maine December, 2010 Advisory Committee: Peter O. Koons, Professor of Earth Sciences, Advisor George H. Denton, Libra Professor of Earth Sciences, Co-advisor Fei Chai, Professor of Oceanography James L. Fastook, Professor of Computer Science Brenda L. Hall, Professor of Earth Science Terrence J. Hughes, Professor Emeritus of Earth Science ©2010 Sean David Birkel All Rights Reserved iii CLIMATE INVESTIGATIONS USING ICE SHEET AND MASS BALANCE MODELS WITH EMPHASIS ON NORTH AMERICAN GLACIATION By Sean D. Birkel Thesis Advisor: Dr. Peter O. Koons An Abstract of the Dissertation Presented in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy (in Earth Sciences) December, 2010 This dissertation describes the application of the University of Maine Ice Sheet Model (UM-ISM) and Environmental Change Model (UM-ECM) to understanding mechanisms of ice-sheet/climate integration during ice ages.
    [Show full text]
  • Behavior of the James Lobe, South Dakota During Termination I
    Behavior of the James Lobe, South Dakota during Termination I A dissertation submitted to the Graduate School of the University of Cincinnati in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY in the Department of Geology of the McMicken College of Arts and Sciences by Stephanie L. Heath MSc., University of Maine BSc., University of Maine July 18, 2019 Dissertation Committee: Dr. Thomas V. Lowell Dr. Aaron Diefendorf Dr. Aaron Putnam Dr. Dylan Ward i ABSTRACT The Laurentide Ice Sheet was the largest ice sheet of the last glacial period that terminated in an extensive terrestrial margin. This dissertation aims to assess the possible linkages between the behavior of the southern Laurentide margin and sea surface temperature in the adjacent North Atlantic Ocean. Toward this end, a new chronology for the westernmost lobe of the Southern Laurentide is developed and compared to the existing paradigm of southern Laurentide behavior during the last glacial period. Heath et al., (2018) address the question of whether the terrestrial lobes of the southern Laurentide Ice Sheet margin advanced during periods of decreased sea surface temperature in the North Atlantic. This study establishes the pattern of asynchronous behavior between eastern and western sectors of the southern Laurentide margin and identifies a chronologic gap in the western sector. This is the first comprehensive review of the southern Laurentide margin since Denton and Hughes (1981) and Mickelson and Colgan (2003). The results of Heath et al., (2018) also revealed the lack of chronologic data from the Lobe, South Dakota, the westernmost lobe of the southern Laurentide margin.
    [Show full text]
  • Article Is Available Online USA, 2004
    The Cryosphere, 10, 639–664, 2016 www.the-cryosphere.net/10/639/2016/ doi:10.5194/tc-10-639-2016 © Author(s) 2016. CC Attribution 3.0 License. Numerical simulations of the Cordilleran ice sheet through the last glacial cycle Julien Seguinot1,2,3, Irina Rogozhina3,4, Arjen P. Stroeven2, Martin Margold2, and Johan Kleman2 1Laboratory of Hydraulics, Hydrology and Glaciology, ETH Zürich, Zürich, Switzerland 2Department of Physical Geography and the Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden 3Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany 4Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany Correspondence to: Julien Seguinot ([email protected]) Received: 21 June 2015 – Published in The Cryosphere Discuss.: 7 August 2015 Revised: 2 February 2016 – Accepted: 19 February 2016 – Published: 16 March 2016 Abstract. After more than a century of geological research, 1 Introduction the Cordilleran ice sheet of North America remains among the least understood in terms of its former extent, volume, and dynamics. Because of the mountainous topography on During the last glacial cycle, glaciers and ice caps of the which the ice sheet formed, geological studies have often had North American Cordillera have been more extensive than only local or regional relevance and shown such a complexity today. At the Last Glacial Maximum (LGM), a continuous that ice-sheet-wide spatial reconstructions of advance and re- blanket of ice, the Cordilleran ice sheet (Dawson, 1888), treat patterns are lacking. Here we use a numerical ice sheet stretched from the Alaska Range in the north to the North model calibrated against field-based evidence to attempt a Cascades in the south (Fig.1).
    [Show full text]
  • Planning Record Index for the Flathead National Forest 2018 Land Management Plan and NCDE Grizzly Bear Amendments
    Planning Record Index for the Flathead National Forest 2018 Land Management Plan and NCDE Grizzly Bear Amendments Exhibit Author Description 00001 Flathead National Forest Public Involvement List of Meetings September 2013 to May 2015 00002 Chip Weber (forest supervisor, Flathead letter inviting Confederated Salish and Kootenai Tribes resource managers to meet with Flathead National Forest National Forest) planning team 00003 consultation record of meeting Jan. 21, 2015, with Confederated Salish and Kootenai Tribes 00004 Meridian Institute Flathead National Forest Plan Revision Middle Fork and South Fork Geographic Area Meeting – Mapping Management Areas Draft Summary 00005 Meridian Institute Flathead National Forest Plan Revision Swan Valley and Salish Mountains Geographic Area Meeting – Mapping Management Areas Draft Summary 00006 Meridian Institute Flathead National Forest Plan Revision Hungry Horse and North Fork Geographic Area Meeting – Mapping Management Areas Draft Summary 00007 Meridian Institute Flathead National Forest Stakeholder Collaboration Forest-Wide Meeting – Mapping Management Areas Draft Summary 00008 Meridian Institute Flathead National Forest Plan Revision - Salish Mountains Geographic Area Meeting Draft Summary 00009 Meridian Institute Flathead National Forest Plan Revision - Swan Valley Geographic Area Meeting Draft Summary 00010 Meridian Institute Flathead National Forest Plan Revision - Hungry Horse, Middle Fork, and South Fork - Geographic Areas Meeting - Draft Summary 00011 Meridian Institute Flathead National
    [Show full text]
  • Quaternary and Late Tertiary of Montana: Climate, Glaciation, Stratigraphy, and Vertebrate Fossils
    QUATERNARY AND LATE TERTIARY OF MONTANA: CLIMATE, GLACIATION, STRATIGRAPHY, AND VERTEBRATE FOSSILS Larry N. Smith,1 Christopher L. Hill,2 and Jon Reiten3 1Department of Geological Engineering, Montana Tech, Butte, Montana 2Department of Geosciences and Department of Anthropology, Boise State University, Idaho 3Montana Bureau of Mines and Geology, Billings, Montana 1. INTRODUCTION by incision on timescales of <10 ka to ~2 Ma. Much of the response can be associated with Quaternary cli- The landscape of Montana displays the Quaternary mate changes, whereas tectonic tilting and uplift may record of multiple glaciations in the mountainous areas, be locally signifi cant. incursion of two continental ice sheets from the north and northeast, and stream incision in both the glaciated The landscape of Montana is a result of mountain and unglaciated terrain. Both mountain and continental and continental glaciation, fl uvial incision and sta- glaciers covered about one-third of the State during the bility, and hillslope retreat. The Quaternary geologic last glaciation, between about 21 ka* and 14 ka. Ages of history, deposits, and landforms of Montana were glacial advances into the State during the last glaciation dominated by glaciation in the mountains of western are sparse, but suggest that the continental glacier in and central Montana and across the northern part of the eastern part of the State may have advanced earlier the central and eastern Plains (fi gs. 1, 2). Fundamental and retreated later than in western Montana.* The pre- to the landscape were the valley glaciers and ice caps last glacial Quaternary stratigraphy of the intermontane in the western mountains and Yellowstone, and the valleys is less well known.
    [Show full text]
  • GW Atlas Book.Book
    Montana Ground-Water Assessment Atlas 2 Ground-Water Resources of the Flathead Lake Area: Flathead, Lake, Missoula, and Sanders Counties, Montana Part A*—Descriptive Overview and Water-Quality Data by John I. LaFave Larry N. Smith Thomas W. Patton *The atlas is published in two parts: Part A contains a descriptive overview of the study area, along with water-quality data and an illustrated glossary to introduce and explain many specialized terms used in the text; Part B contains the 11 maps referenced in this document. The maps offer expanded discussions about many aspects of the hydrogeology of the Flathead Lake area. Parts A and B are published separately and each map in Part B is also available individually. iv Ground-Water Assessment Atlas 2 Front Cover: Flathead Lake and the valley to the north are featured in this north–northeast-looking, low-oblique photograph. Formed by glacial damming of the Flathead River during the last ice age, Flathead Lake is 30 miles long and 12 to 14 miles wide. The small city of Kalispell is barely discernible north–northwest of the lake. Kal- ispell is a center for tourism, trade, and the production of livestock, grain, fruit, timber, and aluminum. The Flathead River drains into Flathead Lake, forming a conspicuous delta in the northeast part of the lake. South- west of Kalispell are the small Foy Lakes; Whitefish Lake is to the north. Near the top center of the photograph are Glacier National Park and Lake McDonald. Image courtesy of Earth Science and Image Analysis Laboratory, NASA Johnson Space Center (http://eol.jsc.nasa.gov).
    [Show full text]