Community Wildfire Protection Plan (CWPP) 2021 for FLATHEAD
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Montana Official 2018-2019 Visitor Guide
KALISPELL MONTANA OFFICIAL 2018-2019 VISITOR GUIDE #DISCOVERKALISPELL 888-888-2308 DISCOVERKALISPELL.COM DISCOVER KALISPELL TABLE OF CONTENTS 4 DISCOVER KALISPELL 6 GETTING HERE 7 GLACIER NATIONAL PARK 10 DAY HIKES 11 SCENIC DRIVES 12 WILD & SCENIC 14 QUICK PICKS 23 FAMILY TIME 24 FLATHEAD LAKE 25 EVENTS 26 LODGING 28 EAT & DRINK 32 LOCAL FLAVOR 35 CULTURE 37 SHOPPING 39 PLAN A MEETING 41 COMMUNITY 44 RESOURCES CONNECTING WITH KALISPELL To help with your trip planning or to answer questions during your visit: Kalispell Visitor Information Center Photo: Tom Robertson, Foys To Blacktail Trails Robertson, Foys To Photo: Tom 15 Depot Park, Kalispell, MT 59901 406-758-2811or 888-888-2308 DiscoverKalispellMontana @visit_Kalispell DiscoverKalispellMontana Discover Kalispell View mobile friendly guide or request a mailed copy at: WWW.DISCOVERKALISPELL.COM Cover Photo: Tyrel Johnson, Glacier Park Boat Company’s Morning Eagle on Lake Josephine www.discoverkalispell.com | 888-888-2308 3 DISCOVER KALISPELL WELCOME TO KALISPELL Photos: Tom Robertson, Kalispell Chamber, Mike Chilcoat Robertson, Kalispell Chamber, Photos: Tom here the spirit of Northwest Montana lives. Where the mighty mountains of the Crown of the Continent soar. Where the cold, clear Flathead River snakes from wild lands in Glacier National Park and the Bob WMarshall Wilderness to the largest freshwater lake in the west. Where you can plan ahead for a trip of wonder—or let each new moment lead your adventures. Follow the open road to see what’s at the very end. Lay out the map and chart a course to its furthest corner. Or explore the galleries, museums, and shops in historic downtown Kalispell—and maybe let the bakery tempt you into an unexpected sweet treat. -
Coram Experimental Forest
United States Department of Agriculture Coram Experimental Forest Service Forest: 50 Years of Rocky Mountain Research Station General Technical Research in a Western Report RMRS-GTR-37 September 1999 Larch Forest Raymond C. Shearer Madelyn M. Kempf Abstract Shearer, Raymond C.; Kempf, Madelyn M. 1999. Coram Experimental Forest: 50 years of research in a western larch forest. Gen. Tech. Rep. RMRS-GTR-37. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 66 p. This publication will enrich public understanding about the important contributions to science made at this and other outdoor laboratories. Coram, and other long-range research sites, provide scientific knowledge to assist resource professionals with the development of sound land management principles. This knowledge ensures healthy, sustainable, and productive ecosystems while meeting social and economic needs. Major research at Coram includes the regeneration of young forests and the interaction of flora, fauna, and water to a wide range of forest treatments. Ongoing studies include: • cone and seed development and dispersal • natural and artificial regeneration after harvest cuttings • effects of stand culture treatment on forest development • insect and disease interactions • effects of the amount of wood harvest on site productivity • influence of silvicultural practices on watershed, esthetics, and wildlife values The Coram Experimental Forest is used cooperatively by Federal, university, and private scientists. About 340 ha of the forest are designated as the Coram Research Natural Area where virgin conditions are permanently maintained for research and monitoring. Coram, designated a Biosphere Reserve in 1976, is part of an international network that is devoted to the conservation of nature and scientific research in the service of humans. -
Outstandingly Remarkable Values Assessment
Outstandingly Remarkable Values Assessment of the Flathead River System Flathead National Forest Glacier National Park January 2013 Notes and Disclaimers to Reviewers: The U.S. Department of Agriculture (USDA) and U.S. Department of the Interior (USDI) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W., Washington, D.C. 20250-9410, or call (800) 795-3272 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity provider and employer. Data Accuracy – The Park Service and Forest Service uses the most current and complete data available. Geographic information system (GIS) data and product accuracy may vary. They may be developed from sources of differing accuracy, accurate only at certain scales based on modeling or interpretation, incomplete while being create or revised, etc. Using GIS products for purposes other than those for which they were created, may yield inaccurate or misleading results. The Forest Service reserves the right to correct, update, modify, or replace GIS products without notification. If a map contains contours, these contours were generated and filtered using the Digital Elevation Model (DEM) files. -
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. -
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. -
Voices of Our Lake
Voices of Our Lake i Funders & Supporters This project was made possible by the generous support of: Cadeau Foundation Whitefish Community Foundation WLI Members Authorship & Citation Whitefish Lake Institute, 2018.Voices of Our Lake. Whitefish, MT Copyright Whitefish Lake Institute, Whitefish, MT 2018 Front & Back Cover Photos gravityshots.com, Whitefish, MT Layout & Design eBizServices, Whitefish, MT Printing Towne Printer, Kalispell. MT Disclaimer: The views expressed in the vignettes are those of the authors and do not necessarily represent the views of the Whitefish Lake Institute staff, board, committee members, or membership. Photo courtesy gravityshots.com ii Voices of Our Lake Photo courtesy gravityshots.com founded the Whitefish Lake Institute (WLI) in 2005 to give Whitefish Lake a voice. Its muted waters were undergoing increasing pressure and it needed I better understanding. After all, the lake provides a beautiful backdrop to our community while being a major economic driver. WLI’s role is to define the underpinnings of this lake-based ecosystem and to develop methods we can employ to manage and care for it. Through the years, WLI and project partnershave amassed a solid baseline awareness of the water quality and food web that shape the lake and local streams. In 2015, we compiled that information in one narrative—the Whitefish Area Water Resources Report: A Status of the Whitefish Lake Watershed and Surrounding area. This report and all its supporting re- sources are available at www.whitefishlake.org. Photo courtesy Whitefish Lake Institute In the report, the lake’s voice becomes clearer, revealing a unique record of trends and patterns – the result of natural forces and human actions that operate at time scales ranging from minutes to decades. -
2003 GTSR Avalanche Program Report
Flathead Avalanche Center 2013-2014 Annual Report FLATHEAD AVALANCHE CENTER 2013-2014 ANNUAL REPORT Erich Peitzsch, Interim Director and Avalanche Specialist, Flathead National Forest 1 Flathead Avalanche Center 2013-2014 Annual Report Table of Contents Background ................................................................................................................................................................... 4 Website ......................................................................................................................................................................... 5 Media ............................................................................................................................................................................ 9 Weather, Snowpack, and Avalanche Summary ............................................................................................................ 9 Incidents ...................................................................................................................................................................... 16 Education .................................................................................................................................................................... 20 Finances ...................................................................................................................................................................... 21 Observations .............................................................................................................................................................. -
GWAA 2 Map06 Geol Map.FH10
Montana Bureau of Mines and Geology Ground-Water Assessment Atlas No. 2, Part B, Map 6 A Department of Montana Tech of The University of Montana December 2004 114o R19W 48o30 R20W R21W Qal Qal T32N R22W Qgta Ybe Qgt 114o 37 30 R23W Qao Qgo R24W Qgt Qao o Ybe Qgt 48 30 Qgo Qgt Ybe Qgo Qgt T32N Ybe Tk Qgt Qgt Qls Ybe Qaf Qgo Qao Qaf Qgta Ybe Qgo Qgt Ybe Key to Symbols Qal Ybe Qal Qao Qal Qgt Qaf Qgt Contact, dashed where approximate Qgo Ybe Qgt Ybe Qls Qgo Qlk Ybe Qls Stream 71 Ybe Qgt 82 Qgt W Qls Qgoo h Qls Road Ybe Tk 70 it Qgo Qaf e Qgta Qgo 81 Township boundary, section boundary Ybe f Qgta Qgo i 21a s 83 28 Tk h Tk 21 T31N Population center Qgl L 23 22 Qls Qgt 69 a 27 Marsh Ybe Qgt Ybe k Qgta 24 e Qgo 26 25 Qgo Qgt Qgt Qgoo Lake or reservoir Ybe Qls Qlk 84 Qgo T31N Qal Qgt Tk Qgt Qgt 5 Location where geologic notes were recorded, photographs taken, and/or a vertical Qlk Qal Qaf section was described. Qgt Ybe Qal Qgo Qlk Ybe Qgt Qgt Ybe Ybe Qgo GLACIOFLUVIAL CHANNEL - Channelized depressions recognized from aerial Qgo Qgo Qgt Qal photographs and topographic expression; associated with deposits of glacial outwash Ybe in some areas; multiple types of channels are represented: ice-marginal channels: Ybe Qgt Qgt Qgi Qaf Qgo Qgta Qgo Qgo Qgi irregular linear erosional channels formed by channelized flow next to, or partially Qgo Ybe 73 Qgo Qgl Tk beneath the lateral margins of glaciers; commonly form notches, meander loops, and Qlk 74 Qgt Qgt Ybe Qgt Qgo some integrated drainage networks in bedrock or till that then may have become modern streams; some contain series of internally drained depressions (pools formed Qgt 66 Qgo Qgl Qgt Qgi Qal Qaf Qgo by scour). -
Flathead and Lincoln Counties Montana
USE ON IRRIGATED AREAS and Part ll: MAPS SHOWING IRRIGAlED ArEAs IN COLORS DESIGNATING THe SOURCES OF SUPPLY lItIJifMilCl ",,,J "lACO/" fJo""tJ. .., M."Ir""G • nnw., SlIATE ENGINEER'S 4fFJtE WATER RE SOURCE S SURVEY FLATHEAD AND LINCOLN COUNTIES MONTANA Part I History of Land and Water Use on I rrigated Areas MONTANA < ~ I , I • Published by STATE ENGINEER'S OFFICE Helena, Montana June, 1965 STATE ENGINEER'S OFFICE Everett V. Darlinton .......___ .................. __ .... ____ .............. __ .......... State Engineer Director of \Vater Hesoun:es, Ground and Surface "Vater Hans L. Bille_______ _______ ___ __________________________ ______________ __________ Assistant State Engineer Water Hesources Survey and Publication of County Heports Miller J-Jansen ___________________________________________________________________ _________ Deputy State Engineer CO-OPERATING AGENCIES STATE WATER CONSERVATION BOARD Governor Tim M_ Babcock.. __ _______ _ ______ ___ __________ __ ______ Chairman C. J-I. HaymondO _________ __ ___ . ____ . ___ ______ .Vi ce Chairman and Secretary Everett V. Darlinton ___ _ _______ ___ ____ . _____ ___ __ _____ __ _____ M ember H . J. SawteIL. ____ __ _ ________ ... _______ __ . _____ Member Wi lbur White. __ _ ___ .____ ... ______ Member A. D. McDermott __________ . __ _ ........... ___ .. Director Donald D. Sullivan.___ ___ _ __________ Acting Chief Engineer °Hetired from Board on January 8, 1965 MONTANA STATE AGRICULTURAL EXPERlMENT STATION C. C. Bowman, ] rrigation Engineer and Consultant, Bozeman ~ 3 REPOR T ER PRTG. a SUPPLY co . June, 1965 Honorable Tim M. Bahcock Governor of Montana Capitol Building Helena, Montana Dear Governor Babcock: Submitted herewith is a consolidated report on the \Vater Resources Survey of Flathead and Lincoln CO llnties, Montana. -
Flathead Wild and Scenic River CRMP Botany & Geology Fact Sheet
Flathead Wild and Scenic River CRMP Botany & Geology Fact Sheet Introduction The Three Forks of the Flathead River were designated a Wild and Scenic River (WSR) in 1976 and are a component of the National Wild and Scenic Rivers System. A total of 219 miles of the Flathead River are included in the designation. The free-flowing conditions and water quality of designated wild and scenic rivers are to be protected and enhanced. BOTANY Botanical resources on the three forks of the Flathead are considered one of its Outstandingly Remarkable Values (ORVs). Therefore, review of baseline conditions, potential threats to resources, and future management and monitoring objectives will be integral to the ongoing Comprehensive River Management Plan (CRMP) process. High Quality Riparian Habitat The Three Forks of the Flathead River occur within one of the largest intact ecosystems in the lower 48 states where natural processes such as fire, flooding, plant succession, wildlife migration, and predator-prey dynamics shape the landscape and its wildlife. A full complement of native plant and wildlife species is present in the river corridor, which is a significant value at both a regional and national scale. Management and Regulatory Framework The Forest has one designated wild and scenic river, the Flathead River. Its three forks—the South Fork, Middle Fork, and North Fork—Wild and Scenic river corridors extend 0.25 miles (roughly 1,300 feet) on each side of the river. Public Law 94-486 established the Three Forks of the Flathead as a Wild and Scenic -
Abandoned-Inactive Mines of the Flathead National Forest-Administered Land
Abandoned-Inactive Mines of the Flathead National Forest-Administered Land Montana Bureau of Mines and Geology Open-file Report 462 Catherine McDonald Phyllis A. Hargrave Michael D. Kerschen John J. Metesh Robert Wintergerst Prepared for the U.S. Department of Agriculture Forest Service-Region 1 Abandoned-Inactive Mines on Flathead National Forest-Administered Land Open-File Report MBMG 462 July 2002 Catherine McDonald Phyllis A. Hargrave 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........................................................... iv LIST OF TABLES............................................................ iv 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 1.4.3.1 Collection -
TRAILS of the PAST: Historical Overview of the Flathead National Forest, Montana, 1800-1960
TRAILS OF THE PAST: Historical Overview of the Flathead National Forest, Montana, 1800-1960 By Kathryn L. McKay Historian 1994 Final report of a Historic Overview prepared under agreement with the United States, Flathead National Forest, Kalispell, Montana (Contract #43-0385-3-0363). Submitted in fulfillment of agreement by Kathryn L. McKay, Consulting Historian, 491 Eckelberry Dr., Columbia Falls, Montana, 59912. TABLE OF CONTENTS Introduction Acknowledgements Previous Work Methodology Physical Environment Abbreviations Used in Text Introduction The Fur Trade Introduction The Fur Trade Missionary Activity and Early Exploration Introduction Missionary Activity Railroad Surveys International Boundary Surveys Other Early Explorations Mining Introduction Oil Fields Coal Deposits Placer and Lode Mining General Prospector's Life Placer and Lode Mining in the Flathead Settlement and Agriculture Introduction Settlement Up to 1871 1871-1891 1891 to World War II World War II to Present Forest Reserves Introduction Forested Land on the Public Domain up to 1891 Creation of the Forest Reserves GLO Administration of the Forest Reserves, 1898-1905 Forest Supervisors and Rangers on the Flathead and Lewis & Clarke Forest Reserves, 1898-1905 Forest Service Administration, 1905-1960 Introduction Qualifications of Early Forest Service Workers Daily Work of Early Forest Service Employees Forest Service Food Winter Work Families Injuries Special-Use Permits Forestry Research and Education World Wars Administrative Sites Boundaries Northern Pacific Railroad