Historical Water-Quality Data for the Clark Fork (River)
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PROCEEDINGS of the BOARD of COUNTY COMMISSIONERS of SANDERS COUNTY, MONTANA January 3, 2017
PROCEEDINGS OF THE BOARD OF COUNTY COMMISSIONERS OF SANDERS COUNTY, MONTANA January 3, 2017 The Board of Commissioners of Sanders County, Montana, met in regular session on Tuesday, January 3, 2016 at 10:00 a.m. Present were Carol Brooker, Presiding Officer; Glen E. Magera, Commissioner, and Anthony B. Cox, Commissioner. The Boards and Committees that the Commissioners will attend in 2017 are as follows: Commissioner Cox Commissioner Brooker Commissioner Magera Avista Management Committee Child Development Center Board Sanders County 911 Advisory Board Flathead Valley Chemical Dependency of Directors, Chairman Area Agency on Aging Board Area VI, Corporation, Board of Directors Governors Board of County Printing Chairman Sanders County Board of Health MACo Natural Resources/Public Lands Community Action Partnership Sanders County Solid Waste Refuse Litigation Fund Committee Hot Springs Refuse Disposal District Disposal District MACo Public Land Committee Sanders County Board of Health MACo Board of Directors Sanders County Board of Health Sanders County Community Housing Sanders County Aquatic Invasive Plants Sanders County Community Organization (AIP) Task Force Development Corporation, Board of Sanders County Council on Aging Boards Attended: Directors Sanders County Council on Aging Sanders County DUI Task Force Sanders County Solid Waste Refuse Financial Committee Committee Disposal District Board Sanders County Solid Waste Refuse Resource Advisory Committee Thompson Falls Community Trails Disposal District Terrestrial Resources Tech -
December 18, 2020 Fish Consumption Guidance Updated for Portions Of
Media contact: Trevor Selch, FWP Fisheries Pollution Biologist, 406-444-5686 FOR IMMEDIATE RELEASE: December 18, 2020 Fish consumption guidance updated for portions of Clark Fork, Bitterroot and Blackfoot Rivers in western Montana MISSOULA – The State of Montana Fish Guidance Board, which includes Montana Fish, Wildlife & Parks (FWP) and the Departments of Environmental Quality (DEQ), and Public Health and Human Services (DPHHS), has updated the fish consumption guidance for all species of fish on a 148-mile stretch of the Clark Fork River and tributaries in western Montana in response to new research results. Guidance now recommends avoiding consumption of all species of fish from the Clark Fork River’s confluence with the Bitterroot River, just west of Missoula, to the confluence with the Flathead River, near Paradise. Slightly revised guidance is also in place for rainbow trout and northern pike on an upstream section of the Clark Fork and for the Blackfoot and Bitterroot Rivers. New data was collected to assess chemical contaminants including dioxins, furans, and PCBs in fish tissue in a study area on the Clark Fork that extended from approximately 30 miles upstream of Missoula to 100 miles downstream. Testing in the area is underway as part of water quality monitoring around the former Smurfit-Stone Container mill site. Upon review of the study results, new guidance was issued based on high levels of contaminants in the fish tissue. The source of all the contaminants found in the fish has not been attributed. The study only looked at contaminant concentrations found in the muscle tissues of northern pike and rainbow trout, but the same “Avoid” guidance extends to all species present in the Clark Fork River near Missoula (such as brown trout, whitefish, small- and large-mouth bass, northern pikeminnow, and sucker species) because similar food habits, habitat use, and life- span suggest they could also contain chemical concentrations at potentially dangerous levels. -
United States Department of the Interior National Park Service
NFS Form 10-900a OMB No. 1024-0018 (8-86) United States Department of the Interior National Park Service NATIONAL REGISTER OF HISTORIC PLACES CONTINUATION SHEET Section ___ Page __ SUPPLEMENTARY LISTING RECORD NRIS Reference Number: 09001185 Date Listed: 1/4/2010 Little Blackfoot River Bridge Powell MT Property Name County State Montana's Historic Steel Truss Bridges MPS Multiple Name This property is listed in the National Register of Historic Places in accordance with the attached nomination documentation subject to the following exceptions, exclusions, or amendments, notwithstanding the National Park Service certification included in the nomination documentation. 2 Signatur4y6f ^the Keeper Da£e'of Action Amendepr Items in Nomination: Classification: The Number of Contributing Properties Previously Listed should read: 0 [This refers only to resources within the nominated boundaries of this property not to other bridge locations associated with the MPS context.] These clarifications were confirmed with the MT SHPO office. DISTRIBUTION: National Register property file Nominating Authority (without nomination attachment) NPS FORM 10-900 (Rev. 01 /2009OMB No. 1024-0018 I" " United States Department of the Interior \ • National Park Service I \ T ' ; NOV 2 0 2009 National Register of Historic Places Registration Form This form is for use in nominating or requesting determinations for individual properties and districts. See instructions in National Register Bulletin, How to Complete the National Register of Historic Places Registration Form. If any item does not apply to the property being documented, enter "N/A" for "not applicable." For functions, architectural classification, materials, and areas of significance, enter only categories and subcategories from the instructions. -
Derek Decker, Senior Offensive
Derek Decker, senior offensive gua Other area attractions include “A Carousel for Missoula” (one of the first fully hand-carved carousels to be built in America since the Great Depression), Garnet Ghost Town, the National Bison Range, the Ninemile Remount Depot and Ranger Station, the Rocky Mountain Elk Foundation Wildlife Visitor Center, and the Smokejumper Visitor Center. Missoula Parks and Recreation and the YMCA provide a variety of recreational opportunities in basketball, soccer, softball, tennis, volleyball, and ice skating. Missoula also serves as a center for education, health care, retail, and the arts. The University of Montana provides educa tional opportunities for more than 13,000 college students. Com munity Medical Center and St. Patrick Hospital, along with many clinics, make Missoula one of the state’s premier health care com munities. The Missoula community supports the arts in all its forms: the Summertime in Missoula, the Downtown Association’s Out to Lunch ater productions, dance, art, and music. The Missoula Children’s weekly series. Theater, founded in 1970, moved into a renovated building near Birthplace and hometown of author Norman McLean, who wrote campus and produces plays and musicals by national and local A River Runs Through It, Missoula is also known as the “Garden playwrights for both adults and children. The theater also has an City” for its dense trees and lush green landscape. Missoula is International Tour Project, taking theatrical productions to audi nestled in the heart of the Northern Rockies in western Montana. ences outside the Missoula area. The Garden City Ballet and A community of approximately 66,000 residents, Missoula lies in a Missoula Symphony, which is in its 50th season, bring performances mountain forest setting where five valleys converge. -
Historic Settlement of the Rattlesnake Creek Drainage, Montana| an Archaeological and Historical Perspective
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2005 Historic settlement of the Rattlesnake Creek Drainage, Montana| An archaeological and historical perspective Daniel S. Comer 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 Comer, Daniel S., "Historic settlement of the Rattlesnake Creek Drainage, Montana| An archaeological and historical perspective" (2005). Graduate Student Theses, Dissertations, & Professional Papers. 2544. https://scholarworks.umt.edu/etd/2544 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]. NOTE TO USERS Page(s) not included in the original manuscript are unavailable from the author or university. The manuscript was microfilmed as received 80-190, 271-289 This reproduction is the best copy available. dfti UMI Maureen and Mike MANSFIELD LIBRARY The University of IVIontdn^ Permission is granted by the author to reproduce this material in its entiret>', provided that this material is used for scholarly purposes and is properly cited in published works and reports. **Please check "Yes" or "No" and provide signature** Yes, I grant permission No, 1 do not grant permission Author's Signature: J. i-O frJir^ Date: Any copying for commercial purposes or fmancial gain may be undertaken only with the author's explicit consent. -
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. -
Open-File Report 368 MBMG February 1998
Abandoned - Inactive Mines of the Blackfoot and Little Blackfoot River Drainages Helena National Forest Volume II Open-file Report 368 MBMG February 1998 Phyllis A. Hargrave Tom P. Bowler Jeff D. Lonn James P. Madison John J. Metesh Robert Wintergerst Abandoned - Inactive Mines of the Blackfoot and Little Blackfoot River Drainages Helena National Forest Volume II Open-file Report 368 MBMG Reformatted for .pdf - February 2002 February 1998 Phyllis A. Hargrave Tom P. Bowler Jeff D. Lonn James P. Madison John J. Metesh Robert Wintergerst Contents Page List of Figures .................................................................. vi List of Tables ............................................................. viii 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 .......................................... 2 1.3.2 Solubility 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 1.4.3.1 Collection of -
Report Clark Fork River Biomonitoring Macroinvertebrate Community
Report Clark Fork River Biomonitoring: Macroinvertebrate Community Assessments for 2019 Prepared by: David Stagliano Montana Biological Survey/Stag Benthics Prepared for: Boise, Idaho Submitted to U.S. Environmental Protection Agency Region 8 June 2020 Executive Summary The upper Clark Fork River (CFR) Basin in western at Kohrs Bend (Station 10) to 85 percent at SBC Montana contains four contiguous Superfund below Warm Springs (Station 4.5) and the operable units that have been undergoing various Blackfoot River site (Station 14) (Figure ES-1). remediation activities for decades. Since 1986, Both SBC sites (stations 2.5 and 4.5) were rated as annual benthic macroinvertebrate-based (BMI) slightly impaired. Slight biological impairment monitoring has been performed at 13 CFR stream from nutrients was evident at two CFR stations reaches with ongoing or future remedial actions near Deer Lodge (8.5 and 9.0) and near Missoula (McGuire Consulting 1986-2017; Montana (Station 15.5), but the former sites have improved Biological Survey/Stag Benthics 2017-Present). markedly since 2017. The lower Blackfoot River Monitoring extended from Silver Bow Creek (SBC) (Station 14) was ranked slightly impaired again in sites upstream of the Warm Springs Ponds, 2019, likely due to metal related stressors. downstream through the upper CFR, bracketing During 2019, environmental conditions in SBC at the former Milltown Dam site to below the Opportunity (Station 2.5) improved after CFR-Bitterroot River confluence. In addition to experiencing declines in integrity scores in 2018. providing current assessments of ecological Likewise, SBC below the Warm Springs Ponds conditions, these sampling events extend the (Station 4.5) remained slightly impaired but BMI long-term data set for evaluating water quality integrity improved over 2017 scores. -
Clarks Fork of the Yellowstone Fishing Report
Clarks Fork Of The Yellowstone Fishing Report Uninvidious and ameboid Joao overbuy her primely slash uncomfortably or slumber counter, is Penny anginal? neverOld-fogyish scats Berchtoldso rakishly never or goose-step enfaced so any congenitally pantofle mordantly. or fidget any tightwads complexly. Humanlike Whitman Everything you therefore wanted to know will fly-fishing the. Clarks Fork Yellowstone River Wyoming Fly Fishing Camping. Montana Trout Scout Guided Fly explode in South Central. Basins and plains such because the Clarks Fork Yellowstone Little practice and Powder Rivers. At various water of reports and report layout through july, and then confluences with fish this is still picking up in. Clarks Fork Yellowstone River include a stream located just 3 miles from Laurel in Yellowstone County in average state of Montana United. The Clarks Fork school the Yellowstone is a warm-faced river. The report has some reports from reed reservoir, there was with a mouse as an hour away from one of california, but there are. Bureau of Reclamation Managing water flow power in most West. Wade fishing opportunities, coal mining industry, are located to heat of silver bow creek to occur primarily livestock. Several hundred acres in about terrestrials become a jig head out a nice fishing reports that contain naturally bright one of floatable sections. Lake Weatherford Texas fishing report rainbow trout sight fishing forecast. Try a chaotic fashion include clark fork powder river has an email to turah are. Chapter 3 Clark Fork River US Fish and every Service. Yellowstone angler When it comes to craft fishing Yellowstone National. So do Luce and Hogan Lakes halfway between Belfry and Cody in the Clark's Fork of the Yellowstone drainage Fish with big midge larvae. -
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. -
December 2007 Newsletter
VOLUME 32 NUMBER 4 DECEMBER 2007 Jane Lopp & Associates to be Recognized for Conservation Support Jane Lopp & Associates LLC will be pre- cludes office space for more employees and a large sented Flathead Audubon’s Conservation Achieve- conference room. With the move to the new building, ment Recognition at the December 10 th meeting, for Jane Lopp & Associates, was launched. supporting conservation projects and conservation Jane is well known in the Flathead for her nonprofits while sponsoring a number of conserva- volunteer contributions to our community. Perhaps tion-oriented Prudential Global Volunteer Days in the less well known are her volunteer activities at the Flathead. state level. Jane served on the Montana Human Jane Lopp & Associates represents Pruden- Rights Commission for 8 years, much of that time as tial Financial Planning Services. Though Jane has Chair. She also served on the Gender Equity Study been in the insurance and investments business Commission for the State Supreme Court, and since 1979, and with Prudential since 1989, Jane chaired the Site Selection Committee for the Lopp & Associates is only about five years old. Women’s Prison which was built in Billings. Jane’s business started out as one-woman This same commitment to community ser- show—just Jane and a secretary located in a 3-room vice also characterizes her company, Jane Lopp & house. Another employee was added when she re- Associates. One recent example is the company’s cruited her husband Bob into the company after he corporate sponsorship for the last two years of girls’ retired from teaching at Flathead High School. -
Hydrogeologic Framework of the Upper Clark Fork River Area: Deer Lodge, Granite, Powell, and Silver Bow Counties R15W R14W R13W R12W By
Montana Bureau of Mines and Geology Montana Groundwater Assessment Atlas No. 5, Part B, Map 2 A Department of Montana Tech of The University of Montana July 2009 Open-File Version Hydrogeologic Framework of the Upper Clark Fork River Area: Deer Lodge, Granite, Powell, and Silver Bow Counties R15W R14W R13W R12W by S Qsf w Qsf Yb Larry N. Smith a n T21N Qsf Yb T21N R Authors Note: This map is part of the Montana Bureau of Mines and Geology (MBMG) a n Pz Pz Groundwater Assessment Atlas for the Upper Clark Fork River Area groundwater Philipsburg ValleyUpper Flint Creek g e Pz Qsf characterization. It is intended to stand alone and describe a single hydrogeologic aspect of the study area, although many of the areas hydrogeologic features are The town of Philipsburg is the largest population center in the valley between the Qsc interrelated. For an integrated view of the hydrogeology of the Upper Clark Fork Area Flint Creek Range and the John Long Mountains. The Philipsburg Valley contains 47o30 the reader is referred to Part A (descriptive overview) and Part B (maps) of the Montana 040 ft of Quaternary alluvial sediment deposited along streams cut into Tertiary 47o30 Groundwater Assessment Atlas 5. sedimentary rocks of unknown thickness. The east-side valley margin was glaciated . T20N Yb t R during the last glaciation, producing ice-sculpted topography and rolling hills in side oo B kf l Ovando c INTRODUCTION drainages on the west slopes of the Flint Creek Range. Prominent benches between ac la kf k B Blac oo N F T20N tributaries to Flint Creek are mostly underlain by Tertiary sedimentary rocks.