A Shelter Comes out the Hahn Cabin Entrapment and Fire Shelter Deployment
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Access Amendment 60 Day
317 E. Spruce Street PO Box 7274 Missoula MT 59807 406 544-9863 [email protected] October 3, 2019 Secretary, U.S. Department of Agriculture 1400 Independence Ave, SW Washington, D.C. 20250-0003 Chief, U.S. Forest Service 201 14th Street, SW Washington D.C. 20250 Secretary, U.S. Department of the Interior 1849 C Street, NW Washington, DC 20240 Director, U.S. Fish and Wildlife Service 1849 C Street, NW Washington, DC 20240 RE: 60-Day Notice of Intent to Sue under the Endangered Species Act- Idaho Panhandle National Forest, Kootenai National Forest and the Lolo National Forest You are hereby notified Alliance for the Wild Rockies, and Native Ecosystems Council (collectively Alliance) intend to file a citizen suit pursuant to the citizen suit provision of the Endangered Species Act (ESA), 16 U.S.C. § 1540(g) for violations of the ESA, 16 U.S.C. § 1531 et seq. Alliance will file the suit after the 60 day period has run unless the violations described in this notice are remedied. The names, addresses, and phone numbers of the organizations giving notice of intent to sue are as follows: Michael Garrity, Executive Director Alliance for the Wild Rockies P.O. Box 505 Helena, Montana 59624 Tel: (406) 459-5936 Dr. Sara Jane Johnson, Executive Director Native Ecosystems Council P.O. Box 125 Willow Creek, MT 59760 Tel: (406) 285-3611 The names, addresses, and phone numbers of counsel for the notifier are as follows: Kristine M. Akland, Attorney at Law Akland Law Firm, PLLC P.O. Box 7472 Missoula, MT 59807 Tel: (406) 544-9863 NOTICE OF LEGAL VIOLATION THE AGENCIES MUST COMPLETE ESA CONSULTATION FOR THE 2011 ACCESS AMENDMENTS PRIOR TO IMPLEMENTING TIMBER SALES IN THE IDAHO PANHANDLE, KOOTENAI AND LOLO NATIONAL FORESTS In November 2011, the Forest Service amended the Forest Plans of the Kootenai, Idaho Panhandle and Lolo National Forests to include wheeled motorized vehicle access and security standards. -
Oberti Resort Design Case Study
Oberti Resort Design Case Study by Phil Bamber, Kelly Chow, Jessica Lortie & Tanay Wood 1 OBERTI RESORT DESIGN: A SLIPPERY SLOPE Oberto Oberti, founder of Oberti Resort Design, is in first stages of designing a unique resort concept to add to his record. Oberti is determined to be at the forefront of the next innovative project in British Columbia by developing a new ski hill and resort in North America. The resort will operate during the summer months in order to cater to skiers and snowboarders year round. Oberti’s perplexing vision encompasses a unique mountain experience that will increase Oberti Resort Design’s market share of the ski resort industry. However, the implementation of a new ski resort is tricky due to the large project scope and implementation costs. The timing of opening the ski resort and the location of the resort will be critical to the success of the resort. Now, with financing from Japanese investors, Oberti needs to decide which direction to steer the project in to maximize the success of the new ski resort and adhere to its shareholders. This extraordinary mountain experience plans to attract 180,000 ski visits in the first year of operations, whilst maintaining a stable financial position. OBERTI RESORT DESIGN & PHEDIAS GROUP: BACKGROUND After growing up in Northern Italy within close proximity to the Alps, mountains have been a constant source of inspiration in Oberto Oberti’s life.1 Oberti’s personal mountain endeavours have stimulated curiosity and enriched his design concepts. He first started out as an architect and later established Oberti Resort Design in 2005. -
Dr. Robert D. Lawrence the Thesis Area Is Located in the Western Foothills of the North Three Major Rock Units Are Present and T
AN ABSTRACT OF THE THESIS OF David Allen Jenne for the degree of Master of Science in Geology presented on March 15,1978 Title:STRUCTURAL GEOLOGY AND METAMORPHIC PETROLOGY OF THE GOLD MOUNTAIN AREA SNOHOMISH COUNTY WASHINGTON d' Abstract approved: Signature redacted for privacy. Dr. Robert D. Lawrence The thesis area is located in the western foothills of the North Cascade Mountains immediately east of Darrington, Washington. Three major rock units are present and these include, from west to east, the Darrington Phyllite, a sedimentary m1ange unit, and the Shuksan Schist.Each of these units is bounded by major faults.In the present thesis only the Darrington Phyllite and the melange unit were studied in detail. The Darrington Phyllite consists of phyllitic metapelites with very local interbedded graywacke, conglomerate, and greenschist. The phyllites contain alternating layers of quartz-albite and musco- vite-graphite.In some rocks, this compositional layering is equiva- lent to sedimentary bedding.However, in most locations,it has resulted from metamorphic processes involving the transposition of bedding and metamorphic differentiation during mimetic recrystal- lization. Greenschist is present as tectonically emplaced blocks and as very local interbeds in the phyllite.Along the western margin of the thesis area, greenschist and meta-igneous rocks have been faulted into place.These rocks probably are part of the Jumbo Mountain Complex. The interbedded greenschists contain lawsonite that has been altered to chlorite.This suggests that blueschist.-facies meta- morphism was followed by a temperature increase and greenschist- facies metamorphism. The mlange unit consists of blocks of sedimentary, meta- igneous, and metamorphic rocks in tectonic contact with a sheared pelitic matrix. -
USGS Geologic Investigation Series I-2592, Pamphlet
GEOLOGIC MAP OF THE SAUK RIVER 30- BY 60-MINUTE QUADRANGLE, WASHINGTON By R.W. Tabor, D.B. Booth, J.A. Vance, and A.B. Ford But lower, in every dip and valley, the forest is dense, of trees crowded and hugely grown, impassable with undergrowth as toughly woven as a fisherman’s net. Here and there, unnoticed until you stumble across them, are crags and bouldered screes of rock thickly clothed with thorn and creeper, invisible and deadly as a wolf trap.1 The Hollow Hills by Mary Stewart, 1973 INTRODUCTION AND Ortenburger for office and laboratory services. R.W. Tabor ACKNOWLEDGMENTS prepared the digital version of this map with considerable help from Kris Alvarez, Kathleen Duggan, Tracy Felger, Eric When Russell (1900) visited Cascade Pass in 1898, he Lehmer, Paddy McCarthy, Geoffry Phelps, Kea Umstadt, Carl began a geologic exploration which would blossom only after Wentworth, and Karen Wheeler. three-quarters of a century of growing geologic theory. The Paleontologists who helped immensely by identifying region encompassed by the Sauk River quadrangle is so struc- deformed, commonly recrystallized, and usually uninspiring turally complex that when Misch (1952) and his students fossils are Charles Blome, William Elder, Anita Harris, David began their monumental studies of the North Cascades in L. Jones, Jack W. Miller, and Kate Schindler. Chuck Blome 1948, the available geologic tools and theories were barely has been particularly helpful (see table 1). adequate to start deciphering the history. Subsequently, Bryant We thank John Whetten, Bob Zartman, and John Stacey (1955), Danner (1957), Jones (1959), Vance (1957a), Ford and his staff for unpublished U-Pb isotopic analyses (cited (1959), and Tabor (1961) sketched the fundamental outlines of in table 2). -
S That Tree Dead? Quantifying Fire-Killed Trees to Inform Salvage and Forest Management
United States Department of Agriculture Rocky Mountain Research Station Science You Can Use Bulletin SEPTEMBER 2019 | Issue 36 Is That Tree Dead? Quantifying Fire-Killed Trees to Inform Salvage and Forest Management In fire-dependent forests of the SUMMARY western United States, tree species adapt in several ways to survive Wildfires are natural disturbances in fire. In low-elevation forests that the western United States. Managing evolved with frequent, low-severity the resulting stands of dead and fire, many species have thick dying trees requires balancing bark protecting the living tissues conflicting priorities. Although these trees provide wildlife habitat and of cambium and phloem from salvage logging revenue, they also wildfires’ destructive heat. Longer, pose public safety hazards. thicker needles or those enclosed in One criticism of salvage logging is thick scales protect growing buds. that forest managers may overpredict Some tree species even shed their tree mortality and remove trees lower branches, which reduces the that will recover from their wildfire injuries. Sharon Hood, a research chance of fire climbing into their ecologist with the Rocky Mountain crowns. Still other tree species are Research Station, has studied tree easily killed by fire but can readily mortality following wildfires to identify resprout, or their seeds survive characteristics of fire injuries that will result in tree death. Through to quickly regenerate burned her research over the past decade, areas. Collectively, these adaptive she has improved the First Order measures allow species survival in Fire Effects Model (FOFEM), a modeling tool that forest managers fire-prone areas. However, high- can use to predict tree mortality intensity wildfires can generate and subsequently plan for salvage temperatures that overwhelm a and other management activities. -
Snohomish County Hiking Guide
2015- 2016 TO OUTDOOR ADVENTURE! 30 GREAT HIKES • DRIVING DIRECTIONS MAPS • ACCOMMODATIONS • LOCAL RESOURCES photo by Scott Morris PB | www.snohomish.org www.snohomish.org | 1 SCTB Print - Hiking Guide Cover 5.5” x 8.5” - Full Color 5-2015 HIKE NAME 1 Hike subtitle ROUNDTRIP m ile ELEVATION GAIN m ile HIKING SEASON m ile MAP m ile NOTES m ile DRIVING DIRECTIONS m ile CONTACT INFO m ile Hard to imagine, but one of the finest beaches River Delta. A fairly large lagoon has developed on in all of Snohomish County is just minutes from the island where you can watch for sandpipers, downtown Everett! And this two mile long sandy osprey, kingfishers, herons, finches, ducks, and expanse was created by man, not nature. Beginning more. in the 1890s, the Army Corp of Engineers built a You won’t be able to walk around the island as the jetty just north of Port Gardiner—then commenced channel side contains no beach. But the beach to dredge a channel. The spoils along with silt and on Possession Sound is wide and smooth and you sedimentation from the Snohomish River eventually can easily walk 4 to 5 miles going from tip to tip. created an island. Sand accumulated from tidal Soak up views of the Olympic Mountains; Whidbey, influences, birds arrived and nested, and plants Camano, and Gedney Islands; and downtown Everett soon colonized the island. against a backdrop of Cascades Mountains. In the 1980s the Everett Parks and Recreation Department began providing passenger ferry service to the island. Over 50,000 folks visit this sandy gem each year. -
Lolo National Forest This Report Contains the Best Available Information at the Time of Publication
Schedule of Proposed Action (SOPA) 04/01/2018 to 06/30/2018 Lolo National Forest This report contains the best available information at the time of publication. Questions may be directed to the Project Contact. Expected Project Name Project Purpose Planning Status Decision Implementation Project Contact R1 - Northern Region, Occurring in more than one Forest (excluding Regionwide) Bob Marshall Wilderness - Recreation management In Progress: Expected:04/2015 04/2015 Debbie Mucklow Outfitter and Guide Permit - Special use management Scoping Start 03/29/2014 406-758-6464 Reissuance [email protected] CE Description: Reissuance of existing outfitter and guide permits in the Bob Marshall Wilderness Complex. Web Link: http://www.fs.usda.gov/project/?project=44827 Location: UNIT - Swan Lake Ranger District, Hungry Horse Ranger District, Lincoln Ranger District, Rocky Mountain Ranger District, Seeley Lake Ranger District, Spotted Bear Ranger District. STATE - Montana. COUNTY - Flathead, Glacier, Lewis and Clark, Missoula, Pondera, Powell, Teton. LEGAL - Not Applicable. Bob Marshall Wilderness Complex. FNF Plan Revision & NCDE - Land management planning In Progress: Expected:05/2018 06/2018 Joseph Krueger GBCS Amendment to the Lolo, Objection Period Legal Notice 406-758-5243 Helena, Lewis & Clark,and 12/14/2017 [email protected] Kootenai NFs Description: The Flathead NF is revising their forest plan and preparing an amendment providing relevant direction from the EIS NCDE Grizzly Bear Conservation Strategy into the forest plans for the Lolo, Helena, Kootenai, and Lewis & Clark *UPDATED* National Forests. Web Link: http://www.fs.usda.gov/goto/flathead/fpr Location: UNIT - Kootenai National Forest All Units, Lewis And Clark National Forest All Units, Flathead National Forest All Units, Helena National Forest All Units, Lolo National Forest All Units. -
Sherwood Mine Is in Fluvial Rocks of the Eocene Sanpoil Volcanics (Waggoner, 1990, Geol
Okanogan Tough Nut (434) ALTERNATE NAMES DISTRICT COUNTY Okanogan 0 • PRIMARY QUADRANGLE SCALE 1h x 1° QUAD 1° X 2° QUAD Conconully East 1:24,000 Oroville Okanogan LATITUDE LONGITUDE SECTION, TOWNSHIP, AND RANGE 48° 34' 46.84" N 119° 44' 55.56" w NWl/4 sec. 31, 36N, 25E, elev. 3,200 ft LOCATION: elev. 3,200 ft HOST ROCK: NAME LITHOLOGY AGE metamorphic complex of Conconully schist pre-Jurassic ASSOCIATED IGNEOUS ROCK: DESCRIPTION AGE Conconully pluton Cretaceous COMMODIDES ORE MINERALS NON-ORE MINERALS Ag galena pyrite, quartz Pb chalcopyrite Cu sphalerite Zn DEPOSIT TYPE MINERALIZATION AGE vein Cretaceous? PRODUCTION: Production prior to 1901 was valued at $9,000 (Moen, 1973). TECTONIC SETTING: The Triassic sediments were deposited along an active margin associated with an island arc. The Conconully pluton is a directionless, post-tectonic body that was intruded into a major structural zone (Stoffel, K. L., OGER, 1990, oral commun.). ORE CONTROLS: The quartz vein is in quartz-mica schist is 3-10 ft wide, strikes N25W, and dips 60SW (Moen, 1973, p. 28). GEOLOGIC SETTING: The vein is in quartz-mica schist of the metamorphic complex of Conconully near the contact • with the Conconully pluton of Cretaceous age (Stoffel, 1990, geol. map). COMMENTS: The mine was developed by a 50-ft inclined shaft and a 250-ft adit with a 40-ft winze (Moen, 1973, p. 28). REFERENCES Huntting, M. T., 1956, Inventory of Washington minerals-Part II, Metallic minerals: Washington Division of Mines and Geology Bulletin 37, v. 1, 428 p.; v. 2, 67 p. Jones, E. -
The Mountaineer 1978
THE' MOUNTAINEER THE MOUNTAINEER 1978 Published July, 1979 Cover: Mountain Hemlock (Ramona Hammerly) 2 The Mountaineer (USPS 366-700) EDITORIAL COMMITTEE Mary Nysether, Managing Editor; Verna Ness, Production Editor; Christa Lewis, Assistant Editor; Herb Belanger, Don Brooks, Mary Leberg, Mariann Schmitt, Laura Swan, Cindy Vollmer, Mary Jane Ware. Writing, graphics and photographs should be submitted to the Editor, The Mountaineer, at the address below, before Janu ary 15, 1980 for consideration. Photographs should be black and white prints, at least 5x7 inches, with caption and photographer's name on back. Manuscripts should be typed double-spaced, with at least 1 Y2 inch margins, and include wri ter's name, address and phone number. Graphics should have caption and artist's name on back. Manuscripts cannot be re turned. Properly identified photographs and graphics will be returned about July. Copyright @1979 by The Mountaineers. Entered as second class matter April 8, 1922, at Post Office, Seattle, Washington, and additional offices under the act of March 3, 1879. Published monthly, except July, when semi monthly, by The Mountaineers, 719 Pike Street, Seattle, Washington 98101. 3 THE MOUNTAINEERS Purposes To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanent form the history and traditions of this region; To preserve by the encouragement of protective legislation or otherwise the natural beauty of Northwest America; Tomake expeditions into these regions in fulfillment of the above purposes; To encourage a spirit of good fellowship among all lovers of out door life. t � ----..:::::- -""°"'� ---������0wiw.=-- --- Firs at Excelsior Pass, North Cascades. Susan Marsh 4 Black-capped chickadee. -
Reprint 8. Emplacement of the Twin Sisters Dunite, Washington
STATE OF WASHINGTON ALBERT D. ROSELLINI, Governor Department of Conservation EARL COE, Director DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTIING, Supervisor Reprint No. 8 EMPLACEMENT OF THE TWIN SISTERS DUNITE, WASHINGTON By DONAL M. RAGAN Reprinted from American Journal 0£ Science, vol. 261, June 1963, p. 549-565 1963 [AMERICA N JoURNAL OF SCIENCE, VOL. 261, JUNE 1963, P. 549-565) EMPLACEMENT OF THE TWIN SISTERS DUNITE, WASHINGTON DONAL M. RAGAN Geology Department, University of Alaska, College, Alaska ABSTRACT. The large, elliptical, 36-square-mile Twin Sisters duuite and two smaller dunite bodies are located along a northwest-trending, nearly vertical fault and are intru· sive into several thrust plates and locally into the unconformably overlying Swauk forma tion. The time of emplacement was post-Paleocene, and definitely later than the main Cretaceous orogeny. The Twin Sisters mass is composed of a virtually unaltered, coarse-grained enstatite· bearing dunite, with accessory amounts of chromite and chromium diopside. Every section displays abundant evidence of cataclasis, including granulation and bending of mineral grains, and translation bands in olivine. Completely identical textures have recrystallized. These recrystallized cataclastic features now consist of fine-grained, unstrained olivine mosaic zones surrounding and embaying large, strained porphyroclasts. Locally thin mosaic zones cut single, large crystals. The translation bands have recrystallized into bandlike forms with irregular, sutured boundaries. This recrystallization is thought to have taken place at moderate temperatures. Serpentinites are marginal to and gradational with the large Twin Sisters mass and one exposed smaller body. The width of this nalTOW marginal zone is essentially the same for both the large and the small, and is thus independent of the size of the mass. -
PM2.5 2017 Exceptional Events in Libby Due to Wildfires
PM2.5 2017 Exceptional Events in Libby due to Wildfires Source: CIRA and NOAA. These data are preliminary and not operational. Prepared by: Montana DEQ February 2019 Contents 1. Summary ............................................................................................................................................... 3 2. Conceptual Model ................................................................................................................................. 6 3. Comparison to Historical Data .............................................................................................................. 7 4. Clear Causal Relationship .................................................................................................................... 10 Tuesday, August 08, 2017 .............................................................................................................. 10 Wednesday, August 09, 2017 ........................................................................................................ 17 Thursday, August 10, 2017 ............................................................................................................ 23 Friday, August 11, 2017 ................................................................................................................. 28 Monday, September 04, 2017 ....................................................................................................... 33 Tuesday, September 05, 2017 ...................................................................................................... -
Mineral Properties
State of Washington ARTHUR B. LANGLIE, Governor Department of Conservation and Development ED DAVIS, Director DIVISION OF GEOLOGY HAROLD E. CULVER, Supervisor Report of Investigations No. 6 INVENTORY OF MINERAL PROPERTIES IN Snohomish County, Washington By W. A. BROUGHTON OLYMPIA STATE PRINTING PLANT 1942 For sale by Depa.rtment of Conservation and Development, Olympia, Washington. Price, 25 Cents. CONTENTS Page Introduct_ion ................................................. 5 Lode mining properties by districts . 7 Darrington Mining District. 7 General features . 7 Mines ............................ :. 7 Prospects . 8 Glacier Peak Mining District. H General features . 11 Prospects ................................. : ......... 11 Granite Falls Mining District. 12 General features . 12 Mines ................. ............................. 13 Prospects ............... ........................... 13 Index Mining District .................................... 13 General features . 13 Mines ....................... , ....................... 14 Prospects ........... ..................... ............ 16 Monte Cristo Mining District. 19 General features . • . 19 Mines ............................................... 20 Prospects . 22 Silver Creek Mining District. 27 General features . 27 Mines ................................................ 28 Prospects . 29 Silverton Mining District ...... .. ........................ 39 General features . 39 Mines ............................................... 39 Prospects . 40 Sultan Mining District. ... 46