SW Construction Effective Permits by County (PDF)
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South Fork of the Flathead River Originates in the South End of the Bob Marshall Wilderness and Flows Northward to Hungry Horse Reservoir
The South Fork Acclaimed as one of Montana’s most pristine and remote rivers, the Wild and Scenic South Fork of the Flathead River originates in the south end of the Bob Marshall Wilderness and flows northward to Hungry Horse Reservoir. Boats and supplies are generally packed in on mules or horses over mountain passes to reach the headwa- ters and then packed again from the take-out just above Meadow Creek Gorge, to Meadow Creek Trailhead. There are several commercial outfitters who can provide packing services or full-service floats, but plan ahead as they have limited space available. The floating season is generally from mid-June through late August. The river is Class II-III with standing river waves and shallow rocky shoals. Log jams and other hazards exist, and may change and move seasonally. Always scout from shore prior to floating into any river feature without clear passage. Due to its remoteness, the South Fork requires advanced planning and preparation. Contact the Spotted Bear Ranger Station for updated informa- tion on river and trail conditions, regulations and list of permitted outfitters. Restrictions All sections of the South Fork • Solid human waste containment and the use of fire pans and blankets is recommended. • Store your attractants in a bear resistant manner, in an approved container or vehicle, or hang. Section Specific Restrictions - Confluence with Youngs Creek to Cedar Flats - • Wilderness Section • The party size is limited to 15 people per group and 35 head of stock per party. • Use of weed free stock feed is required. • No wheeled carts or wheelbarrows. -
Butte-Silver Bow: Recreation Destination
Butte-Silver Bow: A World-Class Recreation Destination MAY 2015 Recreation Guide ENDORPHINS NOW. BREW PUBS LATER. What IPA goes best with a full suspension? What stout best compliments a hard tail? These are the kind of questions you’ll find the answers to after you conquer the nearby uncrowded Continental Divide Trail in Butte, Montana. After you saddle up, mosey up to a chair at one of our popular brewpubs and restaurants. Start your adventure at buttecvb.com. Letter from the Director/ Staff/ Board…Page 2 Policies…Page 4 Parks and Facility Reservations…Page 6 We’re on the web! Festivals and Special Events…Page 13 co.silverbow.mt.us/192/Parks-Recreation Find us on Facebook, Twitter, and Instagram! Bike Routes and Safe Biking…Page 18 Bike Route Map…Page 19 @ButteParks @ButteSilverBow @ButteParksandRec Programs…Page 21 On the cover: The 2014 Montana Folk Festival at the Original Mine Yard. Trails…Page 23 All photos by Derek Pruitt unless otherwise noted. Urban Trail Map…Page 24 Thompson Park Map…Page27 Partners…Page 31 Camps…Page 42 BUTTE RECREATION GUIDE 2015 1 A note from the director Dear citizens and visitors, Please join with me in celebrating how recreation creates a great quality of life in Butte-Silver Bow. Each of us are touched daily by recreational e appreciate the pursuits for ourselves, our children, our grandchildren, and our friends. As we walk for exercise, play sports, spectate at an event, or just W socialize with friends, these activities become a vital part of our days. opportunity to serve you Recreational activities become part of who we are and also how we celebrate community. -
The Summit Brochure with Maps.Pdf
THE SUMMIT SEELEY LAKE, MONTANA $3,800,000 | 70± ACRES LISTING AGENT: BILL MCDAVID 901 S. HIGGINS AVE., STE. 103 MISSOULA, MONTANA 59801 P: 406.542.3762 M: 406.360.3141 [email protected] THE SUMMIT SEELEY LAKE, MONTANA $3,800,000 | 70± ACRES LISTING AGENT: BILL MCDAVID 901 S. HIGGINS AVE., STE. 103 MISSOULA, MONTANA 59801 P: 406.542.3762 M: 406.360.3141 [email protected] Land… that’s where it all begins. Whether it is ranch land or family retreats, working cattle ranches, plantations, farms, estancias, timber or recreational ranches for sale, it all starts with the land. Since 1946, Hall and Hall has specialized in serving the owners and prospective owners of quality rural real estate by providing mortgage loans, appraisals, land management, auction and brokerage services within a unique, integrated partnership structure. Our business began by cultivating long-term relationships built upon personal service and expert counsel. We have continued to grow today by being client-focused and results-oriented—because while it all starts with the land, we know it ends with you. WITH OFFICES IN: DENVER, COLORADO BOZEMAN, MONTANA EATON, COLORADO MISSOULA, MONTANA STEAMBOAT SPRINGS, COLORADO VALENTINE, NEBRASKA STERLING, COLORADO COLLEGE STATION, TEXAS SUN VALLEY, IDAHO LAREDO, TEXAS HUTCHINSON, KANSAS LUBBOCK, TEXAS BUFFALO, WYOMING MELISSA, TEXAS BILLINGS, MONTANA SOUTHEASTERN US SALES | AUCTIONS | FINANCE | APPRAISALS | MANAGEMENT © 2019 HALL AND HALL | WWW.HALLANDHALL.COM | [email protected] — 2 — EXECUTIVE SUMMARY Montana’s Seeley-Swan Valley consists of two watersheds, the Clearwater River flowing south and the Swan River flowing north off a glacial moraine divide that separates the two. -
SP114-Earthqake Map.FH10
Special Publication No. 114 MONTANA BUREAU OF MINES AND GEOLOGY Stickney et al. 2000 A Department of Montana Tech of The University of Montana Table 1. Names and parameters of Quaternary faults in western Montana. Fault Fault name Most recent Slip rate End-to-end Strike Fault type, Introduction quality for epicentral locations of pre-1995 earthquakes in northwest no. earthquake (mm/yr) length (km) (average) down direction The year 1999 marked the fortieth anniversary of the last destructive Montana is generally below that for southwest Montana. For the Montana earthquake. In contrast, the previous 40 years (19201960) same reason, many small northwest Montana earthquakes went 606 Deadman fault* <1.6 Ma <0.2 (?) 70.8 306° Normal, SW 614 Unnamed fault near Monida* <1.6 Ma <0.2 (?) 13.7 302° Normal, SW saw the occurrence of four major earthquake sequences in Montana. undetected prior to 1995. 641 Red Rock fault -------- ------ 40.7 326° Normal, NE Considering the state's history of damaging earthquakes, it is natural 641a Unnamed (north) section <1.6 Ma <0.2 (?) 14.4 337° Normal, NE that one may ponder the causes and sources of these earthquakes. The quality of seismic monitoring in northwest Montana improved 641b Timber Butte section <130 ka <0.2 (?) 9.3 327° Normal, NE In western Montana and throughout the Intermountain West, only dramatically in 1995 when the MBMG entered into a cooperative 641c Sheep Creeks section <15 ka 0.2-1.0 (?) 14.8 316° Normal, NE the very largest historic earthquakes can be ascribed to specific agreement with the Confederated Kootenai and Salish Tribes 642 Emigrant fault -------- ------ 52.0 41° Normal, NW 642a Unnamed (north) section <130 ka 0.2-1.0 (?) 12.9 21° Normal, W faults with certainty. -
Appendix 4 Brief Geologic History of the Flathead Subbasin
Appendix 4 Brief Geologic History of the Flathead Subbasin The Precambrian rocks of the Belt Supergroup that underlie the Flathead Subbasin formed from sediments deposited in and near a large but shallow sea or inland lake during the middle Proterozoic (from roughly 1,600 to 800 million years ago). This large body of water, which may have been similar to today’s Caspian Sea, occupied parts of present-day eastern Washington, the panhandle of Idaho, western Montana, and adjacent areas of Canada. Over a period of 800 million years, more than 18,000 feet of sediment accumulated from surrounding highlands. The ever-increasing load depressed the sea floor, and variations in the downwarping, combined with changes in the amount and type of sediment flowing into the basin, resulted in alternate layers of different kinds of sediment, including sand, silt, and limey mud. As the great mass of sediment accumulated, moderate heat and pressure associated with deep burial caused mild metamorphism, converting the rocks to quartzite, siltite, argillite, recrystallized limestone, and dolomite. The rocks, however, retained much of their sedimentary character; features such as ripple marks, mud cracks, salt casts, and fossil algal stromatolites are well preserved. In some areas, igneous rocks were injected into the sedimentary rocks and formed sills that today parallel the layering in the rocks. Approximately 150 million years ago the North American plate began colliding with numerous large island arcs in the Pacific. The impacts created and elevated mountain chains, forming the ancestral Rocky Mountains. Immense compressive forces persisted for some 90 million years and were enough to produce mountains several hundred miles inland from the edge of the continent. -
The Mission Mountains Tribal Wilderness
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1995 A Confluence of sovereignty and conformity : the Mission Mountains Tribal Wilderness Diane L. Krahe 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 Krahe, Diane L., "A Confluence of sovereignty and conformity : the Mission Mountains Tribal Wilderness" (1995). Graduate Student Theses, Dissertations, & Professional Papers. 8956. https://scholarworks.umt.edu/etd/8956 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]. A CONFLUENCE OF SOVEREIGNTY AND CONFORMITY: THE MISSION MOUNTAINS TRIBAL WILDERNESS by Diane L Krahe BA Bridgewater College, 1986 presented in partial fulfillment of the requirements for the degree of Master of Science The University of Montana 1995 Approved by; Chairperson Dean, Graduate School Date UMI Number: EP39757 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMT OiSiMflAtion Pubiishrig UMI EP39757 Published by ProQuest LLC (2013). Copyright in the Dissertation held by the Author. -
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. -
Big Sky Area Sustainable Watershed Stewardship Plan
Big Sky Area Sustainable Watershed Stewardship Plan January 26, 2018 BIG SKY AREA SUSTAINABLE WATERSHED STEWARDSHIP PLAN Prepared by Jeff Dunn, Watershed Hydrologist Troy Benn, Water Resources Engineer Zac Collins, GIS Analyst And Karen Filipovich, Facilitator and Analyst Gary Ingman, Water Resources Scientist, Headwaters Hydrology Prepared for And Big Sky Sustainable Water Solutions Forum Big Sky, MT January 26, 2018 PO Box 160513 Big Sky, MT 59716 Over 2016-2017, the Gallatin River Task Force hosted a collaborative stakeholder driven effort to develop the Big Sky Area Sustainable Watershed Stewardship Plan. The Gallatin River Task Force (Task Force) is a nonprofit organization headquartered in Big Sky, with a focus on protecting and improving the health of the Upper Gallatin River and its tributaries. I would like to take this opportunity to thank the many entities and individuals involved in this effort. The main funders of plan development included the Big Sky Resort Area Tax District, and Gallatin and Madison Counties. Initial seed funding was provided by the Big Sky Water and Sewer District, Lone Mountain Land Company, and the Yellowstone Club. Thank you to the stakeholders and their representative organizations that contributed time, energy, and brain power to become educated in water issues in the Big Sky Community, roll up their sleeves and spend countless hours developing creative solutions to complex water issues. Thank you to the many member of the public who provided input by attending stakeholder and public meetings or taking our survey. Implementation of this plan will ensure that the ecological health of our treasured river systems are enhanced and protected as our community and region continue to grow in residential and visitor population. -
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). -
In Re Yellowstone Mountain Club: Equitable Subordination to Police Inequitable Conduct by Non-Insider Creditors Marina Montes
NORTH CAROLINA BANKING INSTITUTE Volume 14 | Issue 1 Article 20 2010 In Re Yellowstone Mountain Club: Equitable Subordination to Police Inequitable Conduct by Non-Insider Creditors Marina Montes Follow this and additional works at: http://scholarship.law.unc.edu/ncbi Part of the Banking and Finance Law Commons Recommended Citation Marina Montes, In Re Yellowstone Mountain Club: Equitable Subordination to Police Inequitable Conduct by Non-Insider Creditors, 14 N.C. Banking Inst. 495 (2010). Available at: http://scholarship.law.unc.edu/ncbi/vol14/iss1/20 This Notes is brought to you for free and open access by Carolina Law Scholarship Repository. It has been accepted for inclusion in North Carolina Banking Institute by an authorized administrator of Carolina Law Scholarship Repository. For more information, please contact [email protected]. In re Yellowstone Mountain Club: Equitable Subordination to Police Inequitable Conduct by Non-Insider Creditors I. INTRODUCTION [C]reditors who cause debtors' financial ruin should not be allowed to use the courts as their collection agents. The United States courts should not be enforcers for loan sharks. The Bankruptcy Code currently gives courts that power to equitably subordinate creditors who act improperly. But... it is applied inconsistently. Equitable subordination provides bankruptcy courts with the authority to place the first lien position of a self-enriching secured creditor in an inferior position to that of other secured or unsecured creditors.2 Historically, bankruptcy judges have been reluctant to use their power to subordinate3 a secured creditor's unjust claims in circumstances where they are not• • fiduciaries.5 For purposes of this Case Comment, a non-insider refers to any creditor that does not have fiduciary obligations. -
Kootenai Lodge Kootenai Lodge
ALL 2004 F COMPLIMENTARY FLATFLATHHEADEAD NORTHWEST MONTANA...THE LAST BEST PLACE LIVING ̄ The history and romance of... Kootenai Lodge KALISPELL • WHITEFISH • BIGFORK • LAKESIDE • POLSON • COLUMBIA FALLS • GLACIER KOOTENAI LODGE The magical Kootenai Lodge is reflected in a tranquil Swan Lake. A STORYBOOK PLACE Photos and text by Kay Bjork ou arrive at Kootenai Lodge and peer curiously through an iron gate adorned with graceful swan silhouettes. The Y drive meanders down into the luscious green estate where towering pines stand like sentinels over the log buildings that line the shores of a glittery Swan Lake. FLATHEAD LIVING Fall 2004 www.flatheadliving.com 79 At the main lodge you enter another gate– KOOTENAI LODGE this one small and inviting, like one you would expect in a secret garden. You im- mediately feel safe and quieted in the court- yard that leads to the grand main lodge. Whimsical etchings created by Charlie Russell in a bygone era are lit up by bright afternoon sun – salamander, turtle and a noble Indian headdress. You are tempted to take off your shoes so that you can feel the curve and dip of the salamander and the warm cement on your feet. You swing the heavy double door open and the latch clinks with the thud of the door behind you. Twirling to take in the im- mense room, warmed by the red-hued larch logs and accented by the soft grey of un- peeled cedar, you imagine the delicious sound of music and laughter in this party place. You turn in a circle, slowly now, to take in the scope of this huge room: the walk- in fireplace, antique wicker furniture, a dozen animal mounts, and a Steinway grand piano. -
Montana — One Landscape for People and Wildlife
2020 TRAVEL GUIDE REDISCOVERMT.COM YOUR LOCAL GUIDE FOR THINGS TO DO IN MONTANA LEE NEWSPAPERS OF MONTANA Montana — One Landscape for People and Wildlife License plate image: “The Great Bear” by Monte Dolack. More at www.dolack.com. Save vital habitat. Put a bear on your car! ontanans have always prized open space. It allows both people and wildlife to thrive Mhere. Nothing embodies wild Montana like our state animal, the grizzly bear. Vital Ground protects key habitat, connecting wild strongholds so grizzlies, other wildlife and people have room to roam. You can help Montana’s one landscape stay open and wild for future generations! Support Montana’s wildlife and open space. Select a Vital Ground specialty license plate when you renew your vehicle registration. The Vital Ground Foundation • 20 Fort Missoula Rd., Missoula, MT 59804 • [email protected] • www.vitalground.org • 406-549-8650 REDISCOVER MONTANA N EW S National forest Wilderness area and/or national wildlife refuge National park Indian reservation Glacier Missouri Glacier Missouri Country Central River Country Central River Country Country Country Country Southwest Southwest Country Southeast Country Southeast Yellowstone Country Yellowstone Country Country Country CONTENTS GLACIER 3 COUNTRY REDISCOVER MONTANA RM S PRING/SUMMER 2015 YELLOWSTONE 8 COUNTRY SOUTHWEST 19 COUNTRY SOUTHEAST COUNTRY Lee Newspapers of Montana 26 rediscovermt.com CENTRAL 38 COUNTRY MISSOURI RIVER 45 COUNTRY SPRING/SUMMER 2020 REDISCOVER MONTANA 1 ABOUT THIS SECTION Rediscover Montana is a publication of Lee NewspapersABOUT of Montana THIS — SECTION ABOUTThe Billings THIS Gazette, SECTION Missoulian, Rediscover Montana is a publication Montana Standard, Helena Independent of Lee Newspapers of Montana — RediscoverRecord MontanaABOUT and Ravalli is THIS a publication Republic.