Level IV Ecoregions of Montana
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Montana Forest Insect and Disease Conditions and Program Highlights
R1-16-17 03/20/2016 Forest Service Northern Region Montata Department of Natural Resources and Conservation Forestry Division In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. Additionally, program information may be made available in languages other than English. To file a program discrimination complaint, complete the USDA Program Discrimination Complaint Form, AD-3027, found online at http://www.ascr.usda.gov/complaint_filing_cust.html and at any USDA office or write a letter addressed to USDA and provide in the letter all of the information requested in the form. To request a copy of the complaint form, call (866) 632-9992. Submit your completed form or letter to USDA by: (1) mail: U.S. -
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. -
MBMG 505-Jefferson-V2.FH10
GEOLOGIC MAP OF THE CENOZOIC DEPOSITS OF THE UPPER JEFFERSON VALLEY MBMG Open File Report 505 2004 Compiled and mapped by Susan M. Vuke, Walter W. Coppinger, and Bruce E. Cox This report has been reviewed for conformity with Montana Bureau of Mines and Geology’s technical and editorial standards. Partial support has been provided by the STATEMAP component of the National Cooperative Geology Mapping Program of the U.S. Geological Survey under contract Number 03HQAG0090. CENOZOIC DEPOSITS OF THE UPPER JEFFERSON VALLEY Cenozoic deposits are the focus of the Geologic Map of the upper Jefferson Valley. The map is largely a compilation of previous mapping with additional interpretations based on aerial photos and limited additional field work. Older rocks are included to show their relations to the Cenozoic deposits, but they are generalized on the map. Lithologic descriptions of the Cenozoic deposits are given in the map explanation (p. 17). References used for the map compilation are shown on p. 15. The northern and southern parts of the map are discussed separately. NORTHERN PART OF MAP AREA Quaternary deposits A variety of Quaternary deposits blanket much of the slope area of the Whitetail and Pipestone Creek valleys between the flanks of the Highland Mountains and Bull Mountain (Fig. 1). East and southeast of these Quaternary slope deposits are more isolated areas of partly cemented Pleistocene gravels on pediments. One of these gravel deposits near Red Hill (Fig. 1) yielded a late Pleistocene vertebrate assemblage including cheetah, horse, camel, and large mountain sheep. Radiocarbon dates from the lowest part of the sequence range between 10,000 and 9,000 14C yr. -
6800-Year Vegetation and Fire History in the Bitterroot Mountain Range Montana
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1995 6800-year vegetation and fire history in the Bitterroot Mountain Range Montana Anne Elizabeth Karsian The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Karsian, Anne Elizabeth, "6800-year vegetation and fire history in the Bitterroot Mountain Range Montana" (1995). Graduate Student Theses, Dissertations, & Professional Papers. 6683. https://scholarworks.umt.edu/etd/6683 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. Anne- K a r s j a n i Maureen and Mike MANSFIELD LIBRARY TheM University ontana of Permission is granted by tlie author to reproduce this material in its entirety, provided that tliis material is used for scholarly purposes and is properly cited in published works and repoits. * * Please check "Yes'' or “No “ and provide signature Yes, I grant permission ..\1 No, I do not grant permission ----- Author’s Signature Date; ' n 1 Any copying for commercial purposes or financial gain may be undertaken only with ^he author’s explicit consent. ■ Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. A 6800-YEAR VEGETATION AND FIRE HISTORY IN THE BITTERROOT MOUNTAIN RANGE, MONTANA By ANNE ELIZABETH KARSIAN Presented in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE UNIVERSHY OF MONTANA Department of Forestry 1995 Approved by: t' z o Chairperson 7 ^ ^ ^ /. -
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. -
Birding in the Missoula and Bitterroot Valleys
Birding in the Missoula and Bitterroot Valleys Five Valleys and Bitterroot Audubon Society Chapters are grassroots volunteer organizations of Montana Audubon and the National Audubon Society. We promote understanding, respect, and enjoyment of birds and the natural world through education, habitat protection, and environmental advocacy. Five Valleys Bitterroot Audubon Society Audubon Society P.O. Box 8425 P.O. Box 326 Missoula, MT 59807 Hamilton, MT 59840 www.fvaudubon.org/ www.bitterrootaudubonorg/ Montana Audubon P.O. Box 595 Helena, MT 59624 406-443-3949 www.mtaudubon.org Status W Sp Su F Bird Species of West-central Montana (most vagrants excluded) _ Harlequin Duck B r r r Relative abundance in suitable habitat by season are: _ Long-tailed Duck t r r c - common to abundant, usually found on every visit in _ Surf Scoter t r r r moderate to large numbers _ White-winged Scoter t r r r u - uncommon, usually present in low numbers but may be _ Common Goldeneye B c c c c _ missed Barrow’s Goldeneye B u c c c _ o - occasional, seen only a few times during the season, not Bufflehead B o c u c _ Hooded Merganser B o c c c present in all suitable habitat _ Common Merganser B c c c c r - rare, one to low numbers occur but not every year _ Red-breasted Merganser t o o _ Status: Ruddy Duck B c c c _ Osprey B c c c B - Direct evidence of breeding _ Bald Eagle B c c c c b - Indirect evidence of breeding _ Northern Harrier B u c c c t - No evidence of breeding _ Sharp-shinned Hawk B u u u u _ Cooper’s Hawk B u u u u Season of occurrence: _ Northern Goshawk B u u u u W - Winter, mid-November to mid-February _ Swainson’s Hawk B u u u Sp - Spring, mid-February to mid-May _ Red-tailed Hawk B c c c c Su - Summer, mid-May to mid-August _ Ferruginous Hawk t r r r F - Fall, mid-August to mid-November _ Rough-legged Hawk t c c c _ Golden Eagle B u u u u This list follows the seventh edition of the AOU check-list. -
Geological Survey
DEPARTMENT OF THE INTERIOR BULLETIN OF THE UNITED STATES GEOLOGICAL SURVEY No. 17O t, WASHINGTON GOVERNMENT PRINTING OFFICE 1900 UNITED STATES GEOLOGICAL SUKVEY CHARLES D. WALCOTT, DIRECTOR SURVEY OF THE BOUNDARY LINE BETWEEN IDAHO AND MONTANA FROM THE INTERNATIONAL BOUNDARY TO THE CREST OF THE BITTERROOT MOUNTAINS BY RICHARD TJRQUHART GOODE WASHINGTON GOVERNMENT PRINTING OFFICE 1900 CONTENTS. Page. Letter of transmittal - _. .... _..._......_....--..,.. ........... 9 Instructions ...............................1...^.......................... 11 Boundary lines.-. ....--..........---.-.--..-.-..-............-.-.-..---- 15 Account of operations ...........................-._._........... .--. 18 Latitude, longitude, base line, azimuth, and triangulation _...__.._.._..___ 21 Latitude _...-. .--.---.-... -.....-..-..........._................ 21 Longitude.........---.-..-..-..-.....-..--.. ............. ....-.-. 23 Spokane base line................J......................__._._.. 25 Azimuth .__.---.--.-.-.....___.. _..--...__.__.__.. ._._........--. 25 Triangulation ................... __........._.'......._._._.....-- 29 Transit and stadia work.................................................. 40 Monuments _. ..;......____.._._.,_._._._....__,, ._.....__. ..-..... 47 The international boundary west of the summit of the Eocky Mountains, and the Mooyie Trail monument..............................._..... 58 Financial statement ................... °........................_.i........ 63 Index ..............J..................................................... -
Abandoned-Inactive Mines on Bitterroot National Forest-Administered Land
Abandoned-Inactive Mines on Bitterroot National Forest-Administered Land Map of the Curlew Mine by Rick Schmidt in MBMG mineral property files Open-File Report MBMG 484 Phyllis A. Hargrave Catherine McDonald Michael D. Kerschen John J. Metesh Robert Wintergerst Prepared for the U.S. Department of Agriculture Forest Service-Region 1 Abandoned-Inactive Mines on Bitterroot National Forest-Administered Land Open-File Report MBMG 484 October 2003 Phyllis A. Hargrave Catherine McDonald Michael D. Kerschen John J. Metesh Robert Wintergerst Prepared for the U.S. Department of Agriculture Forest Service-Region 1 CONTENTS Page LIST OF FIGURES ........................................................... iii LIST OF TABLES ............................................................ iii 1.0 INTRODUCTION ..........................................................1 1.1 Project Objectives ....................................................1 1.2 Abandoned and Inactive Mines Defined . 2 1.3 Health and Environmental Problems at Mines . 2 1.3.1 Acid Mine Drainage ...........................................3 1.3.2 Solubilities of Selected Metals ...................................3 1.3.3 The Use of pH and SC to Identify Problems . 5 1.4 Methodology ........................................................5 1.4.1 Data Sources .................................................5 1.4.2 Pre-Field Screening............................................6 1.4.3 Field Screening ...............................................7 1.4.4 Field Methods ................................................8 -
Glacier National Park Geologic Resource Evaluation Report
National Park Service U.S. Department of the Interior Geologic Resources Division Denver, Colorado Glacier National Park Geologic Resource Evaluation Report Glacier National Park Geologic Resource Evaluation Geologic Resources Division Denver, Colorado U.S. Department of the Interior Washington, DC Table of Contents List of Figures .............................................................................................................. iv Executive Summary ...................................................................................................... 1 Introduction ................................................................................................................... 3 Purpose of the Geologic Resource Evaluation Program ............................................................................................3 Geologic Setting .........................................................................................................................................................3 Glacial Setting ............................................................................................................................................................4 Geologic Issues............................................................................................................. 9 Economic Resources..................................................................................................................................................9 Mining Issues..............................................................................................................................................................9 -
Experience the Nez Perce Trail
Lolo, Montana, to the Big Hole National Battlefield, Montana, through the Bitterroot Valley Experience the Nez Perce Trail Bitterroot River © Jerry Bauer 1 The Nez Perce (Nee-Me-Poo) National Historic Trail Designated by Congress in 1986, the entire Nez Perce National Historic Trail stretches 1,170 miles from the Wallowa Valley of eastern Oregon to the plains of north-central Montana. This segment of the Nez Perce National Historic Trail from Lolo, Montana, to the Big Hole Battlefield, Montana through the Bitterroot Valley is one of eight available tours (complete list on page 35). These are available at Forest Service offices and other federal and local visitor centers along the route. As you travel this historic trail, you will see highway signs marking the official Auto Tour route. Each Mainstream Auto Tour route stays on all-weather roads passable for all types of vehicles. Adventurous and Rugged Routes are an alternative for those seeking the most authentic historic route. They are often on gravel or dirt roads, so plan ahead. Check weather and road conditions before embarking on your journey. Call 511 for road condition reports on major routes. For road condition information on Adventurous and Rugged routes inquire locally. 3 Experience the Nez Perce Trail How do I get there? Mainstream Traveler (Passable for all types of vehicles.) This Auto Tour begins at Fort Fizzle, 4.6 miles west of Lolo Montana. Lolo is located approximately 7 miles south For most travelers this will be the appropriate route. of Missoula, Montana. The roads are generally paved and won’t pose a challenge for typical cars, campers with trailers, and RVs. -
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 -
Surrounded by Mountains
Surrounded by Mountains he Gallatin Valley is one of the most picturesque and Rockies into the jagged peaks we see today. Over the last 50 Geo-Facts: agriculturally productive valleys in Montana. From million years, western Montana experienced several phases of • From the summit of Sacagawea Peak (9,596 ft.) in the northern here, you can see four prominent Montana mountain regional extension and block-faulting, resulting in the creation Bridger Range, you can see even more ranges in a spectacular Tranges: the Bridger Range (east), Gallatin Range (south), of modern Basin-and-Range topography. The crest of the 360o panorama of southwest Montana. Spanish Peaks (southwest), and the Big Belt Mountains Bridger Range arch slowly down-dropped one earthquake at a • A pluton is an intrusive igneous rock body that crystallized from (north). Each range has its own unique geology and topography. time to form the modern Gallatin Valley. Thick layers of mid- magma slowly cooling below the surface of the Earth. Its name The high peaks of the Gallatin Range are carved from volcanic and late Cenozoic sedimentary rocks and more recent stream comes from Pluto, the Roman god of the underworld. rocks and volcanic-derived mudflows that erupted during the deposits have been deposited in the Gallatin Valley, producing • One of the richest gold strikes in Montana history was made at Eocene, approximately 45 million years ago. The Spanish Peaks the fertile landscape that Native Americans called the “Valley of Confederate Gulch in the Big Belt Mountains in 1864. Miners expose metamorphic rocks that date back to the Earth’s early Flowers” – the Gallatin Valley.