Jumbo Glacier Mountain Resort Municipality
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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). -
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. -
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. -
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 -
Publications of the Washington Division of Geology and Earth
Publications of the Washington Division of Geology RESOURCES and Earth Resources May 18, 2011 NATURAL Many of our publications are sold through the Washington State Department of Printing (see p. 3) TABLE OF CONTENTS How to Obtain Publications ...........................................................3 Contact Us ......................................................................................3 Geology Links ................................................................................3 Annual Reports .............................................................................4 Bulletins .........................................................................................6 Digital Reports ...............................................................................8 Field Trip Guides ...........................................................................9 Geologic Maps ...............................................................................9 Information Circulars ...................................................................13 Open File Reports ........................................................................17 Reports of Investigations .............................................................30 Resource Maps .............................................................................31 Topographic Maps .......................................................................32 Reprints ........................................................................................33 Miscellaneous Reports -
Washington Geologic Newsletter
,, A PUBLICATION OF THE WASHINGTON STATE DIVISION OF MINES AND GEOLOGY WASHINGTON GEOLOGIC NEWSLETTER JULY 1973 BERT L. COLE VOLUME 1 - NUMBER 3 COMMISSIONER Of PUBLIC LANDS DON LEE FRASER , SUPERVISOR VAUGHN E. LIVINGSTON, JR ., STATE GEOLOGIST DEPARTMENT Of NATURAL RESOURCES DIVISION Of MINES AND GEOLOGY DEPARTMENT OF NATURAL RESOURCES, DIVISION OF MINES AND GEOLOGY, OLYMPIA WASHINGTON , 9850-4 FIRST KNOWN ACTIVE FAULT IN WASHINGTON By Robert J • Carson l/ A post-glacial fault has been discovered across the fault scarp. Gene Visser used his 19 miles north of Shelton in north-central front-end loader to dig through glacial drift Mason County; it is believed to be the first to the volcanic bedrock. The fault crosses known surface expression of an active fault an old railroad grade built when the area was in the State of Washington. The fault lies logged in the 19201s. Stumps on the scarp are halfway between Hood Canal and Lake Cush up to at Ieast 137 years o Id, so major move man, and 5 miles north of Hoodsport. The ment on the fault probably occurred before fault has offset the east end of Saddle Moun the 19th century. The Saddle Mountain fault tain, a local name given to the ridge between strikes north to northeast, dips steeply ( about Price Lake and Lilliwaup swamp. Movement 75°) to the east, and is downthrown on the of the Saddle Mountain fault has taken place west. The scarp can be traced almost 1 mi le since deglaciation of the southern Puget Low from near the east end of Price Lake to just land, about 13,000 years ago. -
Summits on the Air USA (W7W)
Summits on the Air U.S.A. (W7W) Association Reference Manual (ARM) Document Reference S39.1 Issue number 2.0 Date of issue 01-Dec-2016 Participation start date 01-July-2009 Authorised Date 08-Jul-2009 obo SOTA Management Team Association Manager Darryl Holman, WW7D, [email protected] Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Summits on the Air – ARM for USA W7W-Washington Table of contents Change Control ................................................................................................................... 4 Disclaimer ........................................................................................................................... 5 Copyright Notices ............................................................................................................... 5 1.0 Association Reference Data .......................................................................................... 6 2.1 Program Derivation ....................................................................................................... 7 2.2 General Information ...................................................................................................... 7 2.3 Final Access, Activation Zone, and Operating Location Explained ............................. 8 2.4 Rights of Way and Access Issues ................................................................................ -
A Shelter Comes out the Hahn Cabin Entrapment and Fire Shelter Deployment
A Shelter Comes Out The Hahn Cabin Entrapment and Fire Shelter Deployment Rice Ridge Fire Facilitated Learning Analysis September 12, 2017 This photo was taken from the gravel bar on Youngs Creek on the afternoon of Sept. 12, 2017, by one of the two firefighters who used this gravel bar as a safety zone when the approaching Rice Ridge Fire surrounded and engulfed them with embers and smoke. 0 Contents 1. Summary………………………………………………………………………………………………. 2 2. Narrative………………………………………………………………………………………………. 3 3. Discussion Points A. Safety Zone……………………………………………………………………………… 12 B. Deploying the Fire Shelter………………………………………………………… 12 C. Lookout(s)……………………………………………………………………………….. 13 D. Structure Protection Plan………………………………………………………… 13 E. The Big Picture………………………………………………………………………….. 14 F. The Safety “Margin”………………………………………………………………….. 14 G. Roles/Responsibilities, Delegation and Communication…………… 17 4. Timeline………………………………………………………………………………………………… 18 5. Conclusion…………………………………………………………………………………………….. 19 6. FLA Team Members……………………………………………………………………………..… 19 7. Appendix – Photos of Fire Shelter After Deployment…………………………….. 20 1 National Wildfire Coordinating Group Definitions Entrapment – A situation where personnel are unexpectedly caught in a fire behavior-related, life- threatening position where planned Escape Routes or Safety Zones are absent, inadequate, or compromised. An entrapment may or may not include deployment of a fire shelter for its intended purpose. These situations may or may not result in injury. They include “near misses.” Fire Shelter Deployment – Removing a fire shelter from its case and unfolding it to use as protection against heat, smoke, and burning embers. 1. Summary Two Spotted Bear Ranger District firefighters on the Flathead National Forest were flown into the Bob Marshall Wilderness to implement a Point/Zone Protection Strategy for the Forest’s historic Hahn Cabin, located within the northern portion of the Rice Ridge Fire.