DOCSLIB.ORG

Ghost Towns and Abandoned Settlements

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Ghost Towns and Abandoned Settlements Ghost Towns and Abandoned Settlements Rumored to be under the waters of Perry Lake.) Padonia Palermo (A small population remains) Paradise (2008 estimated population of 59.) Pardee (Only the Pardee Cemetery remains. Used to be a major stop for the Pony Express.) Harlan (Small population, ruins of Main Street, and a high school gymnasium remains.) Lindsey Havana (Ruins of the Havana Stage Station and hotel remain) Hawkeye (Little remains of the townsite.) Hewins (A small population remains.) Hickory Point Hitschmann (Some old buildings still remain. Named for Pardee Butler, a farmer and preacher who was sent adrift on a raft in the Missouri River by pro-slavery men.) Pawnee Penokee (Small population remains. Route 66 Balaklava Hill Ballarat Bennettville Blue Mountain Bodie Calico Carson Hill Cerro Gordo Chambless Cherokee Chinese Camp Chloride City Coloma Darwin Deadwood (Placer County) Denny Dogtown Drawbridge Drytown Dunmovin Eagle Mountain Essex Freeman Junction Garlock Gibsonville Goffs Goler Heights Greenwater Grub Gulch Hamilton Hart Holy City Ivanpah Iowa Hill Keeler Kelso Kingston Leadfield Lexington Llano Del Rio Lookout City Ludlow Manchester (Monterey County) Mammoth City Masonic Mentryville Midland Mount Ophir New Almaden New Idria North Shore Nortonville Panamint City Picacho Pinacate Port Chicago Port Wine Providence Purissima Red Mountain Randsburg Rice Shasta Siberia Silver Lake Skidoo St. Second-smallest incorporated town in the state.) Freeport (2008 estimated population of 7) Galatia (2000 estimated population of 61.) Geary City (Only foundations remain Gem (2008 estimated population of 87.) Geneva (Little remains of the townsite.) Geuda Springs (2008 estimated population of 191.) Granada (Some ruins and abandoned building remain on what used to be Main Street.) Guilford (Few ruins and structures remains) Guittard Station (Some abandoned buildings remain. 75.) Stull (A couple of churches, some houses and the old schoolhouse remain. When the lake was completed, the town was abandoned.) Boyd (Small population and building ruins remain.) Boyd (Some abandoned buildings and ruins remain.) Brookville (2008 estimated population of 263) Buchanan Bushong (2008 estimated population of 50) Byers (2008 estimated population of 49.) Canada (Small population remains.) Carneiro (A small population remains) Castleton (Post office closed in 1957. Thomas                 Star City                                 Sulphur                                   Tempiute                                Tenabo                       Treasure City                          Tybo               Unionville                    Vernon                       Vya                White Cloud City                               Wonder New Hampshire: Beebe River Livermore Monson New Jersey: Batsto Village (a ghost town later transformed into an outdoor museum) Feltville Historic District Double Trouble Borough of Island Beach Ong's Hat Walpack Center in the Delaware Water Gap National Recreation Area Millbrook Village in the Delaware Water Gap National Recreation Area Port Elizabeth (not to be confused with Elizabethport) Raritan Landing South Cape May Whitesbog Village New Mexico: Baldy Town Blackdom Bland Cabezon Chloride Clairmont Cloverdale Cooney Dawson El Ojo Del Padre Elizabethtown Hermosa Gage Gobernador Gran Quivira (now part of the Salinas Pueblo Missions National Monument) Lake Valley Mentmore (still has post office and zip code 87319) Mogollon Mowry Old Hachita Pinos Altos (High Pines); still has some people there, located near Silver City Pittsburg Red Hill Santa Rita Shakespeare Steins Tyrone Vinegaroon (east of La Luz, Otero County; at the mouth of La Borcita) New York: Conklingville (evacuated and used to dam the Great Sacandaga Lake) Doodletown Elko Love Canal Onoville Red House (see Allegany State Park) Tahawus North Carolina: Buffalo City Brunswick Town (former state capital) Cataloochee Diamond City Judson Mortimer Portsmouth Roanoke Colony Whitney (partially submerged by Badin Lake) North Dakota: Alfred Aurelia Bently Brisbane Charbonneau Churchs Ferry Dogtooth Fort Buford Hartland Heaton Leipzig Lonetree Melville Omeemee Petrel Sims Tagus Temple Temvik Van Hook Verendrye Wheelock Ohio: Ai Atwood Blowville Blue Ball Claylick Elk Lick (Destructed and flooded after construction of William H. Currently on private property.) Blaine (Catholic Church and former Catholic School still) Blakeman (Little remains of the townsite.) Bluff City (2008 estimated population of 73. Mary's of Aransas Salona Salt Branch Salt Flat Salt Gap Samfordyce Sanco Sandy Hills Santa Helena Santa Rita Santo Tomás Saspamco Savage Senterfitt Shafter Shafter Lake Shannon Sher-han Sherwood Signal Hill Silver Sipe Springs Sivells Bend Slide Smeltertown Smithfield Soash Spanish Fort Spurlin Starrville Sterley Sterling Steward's Mill Stiles Sulphuria Sumpter Sunnyside Sutherland Springs Swartwout Swastika Sweet Home Tarrant Tarver Tascosa Tee Pee City Tehuacana Telegraph Telico Terlingua Texana Texla Texon The Grove Theney Three Oaks Thurber Tokio Tolbert Towash Toyah Toyahvale Trickham Tucker Tuckertown Tuff Tuleta Turpentine Union Valley Unity Upland Upton Utica Vandenburg Vernal Vieja Springs Virginia City Washington-on-the-Brazos Watson Wenasco White City White Way Who'd Thought It Whon Wild Cat Bluff Williams Ranch Winkleman Wintergreen Yegua Zeirath Ziler Zorn Zella Zuehl Utah: Adventure Ajax Alunite Argyle Asay Bacchus Bingham Canyon Black Rock Blacks Fork Blue Creek Bridgeport Blue Sulphur Springs Brink Bullion Bullionville Caineville Castle Gate Castle Rock Castleton Cedar Creek Cisco Clarion Clear Lake Coal City Colton Connellsville Desert Lake Devon Dewey Diamond Dividend Dover Dragon Duncan's Retreat Dyer Eagle Eagle City Elgin Fish Springs Forest City Freed Frisco Fruita Fry Canyon Garfield Georgetown Giles Gold Hill Goodwill Grafton Grass Creek Greendale Hailstone Hale Hamblin Harper Harrisburg Hebron Heiner Hiawatha Homansville Home of Truth Ingersoll Iosepa Iron City Jackson Jerryville Johnson Keetley Kelton Kimberly Kiz Knightsville La Plata Lark Latuda Layland Lincoln Linwood Lobelia Lucin Lund Mammoth McCornick Mercur Mill Fork Miners Basin Modena Modoc Mohrland Mosida Mountain Dell Mutual National Newhouse Notom Osiris Paria Pearlytown Peerless Priesthood Camp Putney Rainbow Richardson Rockport Rockwell's Station Round Valley Royal Russian Settlement Rutherford Sage Creek Scranton Sego Sewell Silver City Silver Reef Soldier Summit Spring Canyon Standardville Stateline Stotesbury Sulphurdale Sunshine Terrace Thistle Thurmond Tonaquint Tucker Upper Kanab Upton Valley City Verdure Victor Virginius Island Vipont Wahsatch Washakie Watson Wattis Welby Westwater Widtsoe Willow Creek Willow Valley Winter Quarters Woodrow Woodside Yost Vermont: Glastenbury Lewiston Ricker Basin Smith Family Farms Somerset Virginia: Bigler's Mill Ca Ira Elko Tract Falling Creek Jamestown Lackey Lignite Potomac Rockfish Warwick Westham Washington: Ainsworth Alpine Attalia Baird Blewett Bodie Bolster Bordeaux Bossburg Chesaw Curlew Disautel Doty Dryad Elberton Fairfax Franklin Frankfort Goshen Grisdale Hanford Havillah Hot Springs Kennedy Kopiah Krain Lester Liberty Malone McCormick Melmont Molson Monohon Monte Cristo Nagrom Old Orient Osceola Pinkney City Queets Ruby City Seabeck Sheridan Sherman Skagit City Tono Torodah Trinidad Trinity Vail Walville Wellington Weston White Bluffs West Virginia Wisconsin: Aurora Muskego Settlement Nya Upsala Ranney Ulao Wyoming: Atlantic City Bannack Benton Berlin Bessemer Bodie Bryan Calico Carbon Timber Town Fort Steele Hecla Jeffrey City Jerome Jireh Kane Lewiston Lost Springs Miner's Delight Oatman Pacific Springs Piedmont Sherman South Pass City The Duncan Tombstone Tubb Town Van Tassell Walcott . Brazil: Caraibas: Fordlandia Canada: Alberta: Alderson Alexo Allerston Allingham Altorado Amber Valley Anthracite Ardenode Ardley Bankhead Bardo Battle Bend Beazer Belloy Bindloss Bingham Buffalo Bulwark Butte Coalspur Conquerville Conrad Del Bonita Dorothy East Coulee Embarras Landing Frankburg Georgetown Harrisville Judson Kimball Kovach Legend Lille Luscar Maybutt Mercoal Mintlaw Mitford Mountain Park Nemiscam Nordegg Pakowki Pendant d'Oreille Railey Retlaw Rowley Taylorville Travers Twin River Wardlow Whiskey Gap Whitford Whitla Wimborne Windfall Winnifred Woolford Wostok Brittish Columbia: Alice Arm Allenby Alta Lake Alvin Anaconda Antler Creek Anyox Arrowhead Bamberton Barkerville Rush Barkley Valley Barnet Baynes Lake Bennett Big Bar Big Bend Birmingham Blackfoot Blakeburn Boothroyd's Boston Bar Boundary Falls Bullion Bralorne Bradian Brexton Bridge River Britannia Beach Brooklyn Butedale Camborne Camerontown Camp McKinney Cape Scott Cassidy Carmi Cascade City Cassiar Cedar City CentrevilleCherryville Circle CityClayburn Coal Creek Coalmont Cody Columbia Comaplix Copper Mountain Corbin Coryell Craigellachie Deadwood Dease Lake Derby (now rural area in Langley) Discovery Donald Duncan City Dunkeld Eagle Pass Landing East New Hazelton East Princeton Emory City Fairview Ferguson Fisherville Fort Berens (never finished construction; adjacent to Parsonville and Marysville) Fort Fraser Fort Keremeos Fort Kilmaurs Fort Kootenay Fort Rupert Fort Shepherd Fort Steele Fountain
Load more

Recommended publications
  • Upper Bridge River Valley Official Community Plan Bylaw No. Bylaw 608, 1996
    Upper Bridge River Valley Official Community Plan Bylaw No. Bylaw 608, 1996 CONSOLIDATED COPY May 2016 IMPORTANT NOTICE THIS IS AN UNOFFICIAL CONSOLIDATION OF BYLAW NO. 608 WHICH HAS BEEN PREPARED FOR CONVENIENCE ONLY. Although the Squamish-Lillooet Regional District is careful to assure the accuracy of all information presented in this consolidation, you should confirm all information before making any decisions based on it. Information can be confirmed through the SLRD Planning Department. Bylaw 608 ( Consolidated for Convenience Only) May 2016 SUMMARY OF AMENDMENTS CONSOLIDATED FOR CONVENIENCE ONLY Consolidated bylaws are consolidated for convenience only and are merely representative. Each consolidated bylaw consists of the original bylaw text and maps, together with current amendments which have been made to the original version. Copies of all bylaws (original and amendments) may be obtained from the SLRD Planning and Development Department. BY-LAW NO. DATE OF ADOPTION 1022 – 2006 Major Review of Upper Bridge River Valley OCP January 28, 2008 Rezoning a parcel of unsurveyed Crown land from Resource 1094 – 2008 October 26, 2009 Management to Industrial Tyax Real Estate Ltd. text and map amendments plus 1305 - 2014 housekeeping amendment July 28, 2014 PID 024-877-638 (Lot 5, DL 4931, Plan KAP67637, LLD) Creating a Medical Marihuana Production Facility 1309 - 2014 February 25, 2015 Development Permit Area 1440 - 2016 OCP amendments to the Tyax Staff Housing May 25, 2016 Official Community Plan Bylaw No. 608 Page 2 Bylaw 608 ( Consolidated for Convenience Only) May 2016 SQUAMISH LILLOOET REGIONAL DISTRICT BYLAW NO. 1022, 2006 A bylaw of the Squamish Lillooet Regional District to amend the Upper Bridge River Valley Official Community Plan Bylaw No.
    [Show full text]
  • Horseshoe Bend Trail Rails & Trails Made Upofdeepsandand Es
    Code: GC3QN7Z Rails & Trails Written and Researched by Wayne Robinson Horseshoe Bend Trail Site Identification Nearest Community: Lillooet, B.C. Geocache Location: N 50°51.608' W 122°09.318' Ownership: Crown Land Accuracy: 4 meters Photo: Wayne Robinson Overall Difficulty: 2.5 Overall Terrain: 3 The Horseshoe Bend is located on Highway 40, along the Bridge River just south of the confluence of the Bridge Access Information and and Yalakom Rivers. This is an interesting feature marked Restrictions: by a dramatic bend within the river. The canyon walls From the Mile 0 Cairn go north 2 km and turn left on Hwy 40 and follow for are laced with hoodoos and made up of deep sand and 28 km approximately to Horseshoe Bend gravel deposits left behind by retreating glaciers. At pull off. Do not drive down old road. first glance the Horseshoe Bend looks to be a marvel of Beware of cliff edge. Watch for falling geological forces, but it is a human made feature. This rock. Caution if with children and pets. Do not walk on upper rim of Horseshoe feature is sometimes called Horseshoe Wash; this helps Bend. describe the way in which the feature was created, through hydraulic mining for gold. It is amazing that this is a mine. Parking Advice: Operations began here in the 1908 and continued off and Between trees off the road at a natural on until relatively recent times. Between 1908 and 1914 view point. over a million dollars’ worth of gold was extracted from this area (using the historic gold value of $32 per ounce).
    [Show full text]
  • British Columbia Geological Survey Geological Fieldwork 1989
    GEOLOGY AND MINERAL OCCURRENCES OF THE YALAKOM RIVER AREA* (920/1, 2, 92J/15, 16) By P. Schiarizza and R.G. Gaba, M. Coleman, Carleton University J.I. Garver, University of Washington and J.K. Glover, Consulting Geologist KEYWORDS:Regional mapping, Shulaps ophiolite, Bridge REGIONAL GEOLOGY River complex, Cadwallader Group Yalakom fault, Mission Ridge fault, Marshall Creek fault. The regional geologic setting of the Taseko-Bridge River projectarea is described by Glover et al. (1988a) and Schiarizza et al. (1989a). The distributicn and relatio~uhips of themajor tectonostratigraphic assemblages are !;urn- INTRODUCTION marized in Figures 1-6-1 ;and 1-6-2. The Yalakom River area covers about 700 square kilo- The Yalakom River area, comprisinl: the southwertem metres of mountainous terrain along the northeastern margin segment of the project area, encompasses the whole OF the of the Coast Mountains. It is centred 200 kilometres north of Shubdps ultramafic complex which is interpreted by hagel Vancouver and 35 kilometresnorthwest of Lillooet.Our (1979), Potter and Calon et a1.(19901 as a 1989 mapping provides more detailed coverageof the north- (1983, 1986) dismembered ophiolite. 'The areasouth and west (of the em and western ShulapsRange, partly mapped in 1987 Shulaps complex is underlain mainly by Cjceanic rocks cf the (Glover et al., 1988a, 1988b) and 1988 (Schiarizza et al., Permian(?)to Jurassic €!ridge Rivercomplex, and arc- 1989d, 1989b). and extends the mapping eastward to include derived volcanic and sedimentary rocksof the UpperTri %sic the eastem part of the ShulapsRange, the Yalakom and Cadwallader Group. These two assemhkgesare struclurally Bridge River valleys and the adjacent Camelsfoot Range.
    [Show full text]
  • British Columbia Geological Survey Geological Fieldwork 1987
    GEOLOGY OF THE NOAXE CREEK MAP AREA* (920/02) By J. K. Glover, P. Schiarizza and J. I. Garver KEYWORDS: Regional geology, Noaxe Creek, Warner Pass, The '&aughton 'kough: Marine sedimentary strata of he BridgeRiver terrane, Cadwallader terrane, Tyaughton Middle Jurassic to Lower Cretaceous Relay Mountain GrrNugl trough. Yalakom fault, Shulaps ultramafic complex, wrench and the mid-Cretaceous Taqlor Creek and Jackass Mountain faults. groups (Jeletzky and Tipper, 1968). An Upper Cretaceous succession, which comprises her- INTRODUCTION ally discontinuous, nonmarine basinal deposits that grade up into continental volcanicarcrelated rocks, overlies theo13e: The Noaxe Creek map area lies 200 kilometres north of marine strata of the the Tyaughton trough with local pro- Vancouver on the eastern margin of the Coast Mountains, nounced angular unconformity (Glover and Schiarizra, and covers an area of 1000 squarekilometres within the 1987). Chilcotin Range. The topography and vegetation vary from The BridgeRiver terraneand Tyaughton trough are alpine tosubalpine in thewest, southeast and northeast, thought to have been offset from their correlatives to thc: where elevations range up to 2850 metres, to rolling tree- south, the tiozameen Group andMethow basin, by at leas170 covered ridges with intervening broad river valleys in the kilometres of right-lateral strike-slip movement along the central part of the area. north-trending Fraser - Straight Creek fanlt system during Approximately 70 per cent of the area, mostly north of Late Cretaceous (?) and Early Tertiary time (Monger, 19U). Tyaughton and Noaxe creeks, was mapped at ascale of Earlier, post-Albian fragmentation of the Tyaughton-Methow 120 000 by a four-person field crew duringthe 1987 season.
    [Show full text]
  • Examining Precontact Inuit Gender Complexity and Its
    EXAMINING PRECONTACT INUIT GENDER COMPLEXITY AND ITS DISCURSIVE POTENTIAL FOR LGBTQ2S+ AND DECOLONIZATION MOVEMENTS by Meghan Walley B.A. McGill University, 2014 A thesis submitted to the School of Graduate Studies In partial fulfillment of the requirements for the degree of Master of Arts Department of Archaeology Memorial University of Newfoundland May 2018 St. John’s, Newfoundland and Labrador 0 ABSTRACT Anthropological literature and oral testimony assert that Inuit gender did not traditionally fit within a binary framework. Men’s and women’s social roles were not wholly determined by their bodies, there were mediatory roles between masculine and feminine identities, and role-swapping was—and continues to be—widespread. However, archaeologists have largely neglected Inuit gender diversity as an area of research. This thesis has two primary objectives: 1) to explore the potential impacts of presenting queer narratives of the Inuit past through a series of interviews that were conducted with Lesbian Gay Bisexual Transgender Queer/Questioning and Two-Spirit (LGBTQ2S+) Inuit and 2) to consider ways in which archaeological materials articulate with and convey a multiplicity of gender expressions specific to pre-contact Inuit identity. This work encourages archaeologists to look beyond categories that have been constructed and naturalized within white settler spheres, and to replace them with ontologically appropriate histories that incorporate a range of Inuit voices. I ACKNOWLEDGEMENTS First and foremost, qujannamiik/nakummek to all of the Inuit who participated in interviews, spoke to me about my work, and provided me with vital feedback. My research would be nothing without your input. I also wish to thank Safe Alliance for helping me identify interview participants, particularly Denise Cole, one of its founding members, who has provided me with invaluable insights, and who does remarkable work that will continue to motivate and inform my own.
    [Show full text]
  • Atlantic Walrus Odobenus Rosmarus Rosmarus
    COSEWIC Assessment and Update Status Report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada SPECIAL CONCERN 2006 COSEWIC COSEPAC COMMITTEE ON THE STATUS OF COMITÉ SUR LA SITUATION ENDANGERED WILDLIFE DES ESPÈCES EN PÉRIL IN CANADA AU CANADA COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC 2006. COSEWIC assessment and update status report on the Atlantic walrus Odobenus rosmarus rosmarus in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. ix + 65 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Previous reports: COSEWIC 2000. COSEWIC assessment and status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vi + 23 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Richard, P. 1987. COSEWIC status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-23 pp. Production note: COSEWIC would like to acknowledge D.B. Stewart for writing the status report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada, prepared under contract with Environment Canada, overseen and edited by Andrew Trites, Co-chair, COSEWIC Marine Mammals Species Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: (819) 997-4991 / (819) 953-3215 Fax: (819) 994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Évaluation et Rapport de situation du COSEPAC sur la situation du morse de l'Atlantique (Odobenus rosmarus rosmarus) au Canada – Mise à jour.
    [Show full text]
  • Electoral Area Directors Committee Agenda December 4, 2019; 10:30 AM Pemberton Community Church - Meeting Room 7420 Dogwood St., Pemberton, BC
    Electoral Area Directors Committee Agenda December 4, 2019; 10:30 AM Pemberton Community Church - Meeting Room 7420 Dogwood St., Pemberton, BC Item Item of Business and Page Number Page 1. Call to Order by the Corporate Officer We would like to recognize that this meeting is being held on the Traditional Territory of the Líl’wat Nation. 1.1. Election of 2020 Electoral Area Directors Committee Chair 1.2. Election of 2020 Electoral Area Directors Committee Vice-Chair 2. Approval of Agenda 3. Electoral Area Directors Committee Closed Meeting THAT the Committee close the meeting to the public under the authority of Section 90(1)() of the Community Charter. 4. Rise & Report from the Closed Electoral Area Directors Committee Meeting 5. Consent Agenda (Voting rule on each item may vary; unanimous vote required) Items appearing on the consent agenda which present a conflict of interest for Committee Members must be removed from the Consent Agenda and considered separately. Any items to be debated or voted against must be removed from the Consent Agenda and considered separately. THAT the resolutions set out in the Consent Agenda be approved, and those Consent Agenda items which do not have resolutions related thereto be received. 5.1 Approval and Receipt of Minutes 5.1.1. Electoral Area Directors Committee Meeting Draft 5 - 10 Minutes of November 13, 2019 THAT the Electoral Area Directors Committee Meeting Minutes of November 13, 2019 be approved as circulated. 5.2 Staff Reports & Other Business Item Item of Business and Page Number Page 5.2.1. November 2019 Select Funds Report 11 - 15 6.
    [Show full text]
  • Bridge River Newsletter – Fall 2020
    Bridge River Hydroelectric System Projects update—Fall 2020 We’re working to renew the Bridge River electricity system which is about 300 kilometres north of Vancouver in the Bridge River System Traditional Territory of the St’át’imc Nation. Carpenter Reservoir The system consists of the La Joie Dam and Powerhouse La Joie Dam (Downton Reservoir), Bridge 1 and 2 Powerhouses (Terzaghi Terzaghi Dam Dam and Carpenter Reservoir) and Seton Dam and Powerhouse Downton Reservoir (Seton Lake). Bridge 2 Powerhouse Bridge 1 Powerhouse Lillooet Seton Lake We’re making significant investment in these 55 to 70 year- Seton Dam and Anderson Lake Powerhouse old facilities, whose proximity to the Lower Mainland helps us operate the electrical system more efficiently. This includes British Columbia a number of projects in the region. 6.2 MI 10 KM Update: Bridge River 2 Generating Station Upgrade – Units 7 and 8 99 We’ve begun upgrades on units 7 and 8 at the Bridge River 2 (BR2) generating station. Our main contractor, Voith, is on site and focussed on the pre-assembly work for both units, with unit 7 completed in July and unit 8 expected to be completed in September. Most major components have now arrived on site and the project is on track to meet its 2021 targeted completion date. As we prepare to enter the next phase of the project, we’ll ramp up site activity, which will result in an increased number of workers from major contractors and BC Hydro Construction Services. Employees and contractors will continue to follow all Provincial and Federal requirements around social distancing and self-isolation.
    [Show full text]
  • Pumice from Haylmore, Bridge River, British Columbia*
    PUMICE FROM HAYLMORE, BRIDGE RIVER, BRITISH COLUMBIA* Loursp SrovnNs SrevnNsoN, V ictoria, Briti.sh Columbi'a. Alsrnlcr Dacite pumice of Recent age near llaylmore's placer mine, Bridge River district, British Columbia, is highly vesicular and also shows pronounced fluidal structure. The p'urnice is vitrophyric; the volcanic glass of the groundmass has a refractive index of 1.497. The principal phenocrysts are plagioclase feldspars (AbzoAnao)characterized by an abundance of glass inclusions. Possible modes of origin of the inclusions are discussed. A chemical analysis of the pumice and the calculated norm are given. Pumice forms a widespread blanket over much of the Bridge River area of western British Columbia, and its occurrence has been briefly noted in reports of the Canadian Geological Survey. Early in 1946 KAMLOOPS PACIF, C OCEAN "-'t-.. SCALE OF MILES Frc. 1. Index map of British Columbia showing location of llaylmore. Bralorne mine constructed a new wood road across the Hurley River near its confluencewith the Bridge River, exposing an excellent cross- section of the pumice on the west side of the Hurley River, adjacent to the placer workings of William Haylmore (Fig. 1). The pumice rests,on stream boulders and silty gravels of Recent age, and grades upward into the soil. The Bridge River pumice bed is remarkably uniform, and * Presented December 27,1946, at tlle annual meeting of the Mineralogical Society of America held in Chicago, Ill. 548 LOA ISE STEV ENS STEV ENSON the Haylmore exposureseems to be a typical section. It is unique, how- ever, in that part of the section shows stratified silty sand overlying the pumice, a sequencenot heretofore recorded.
    [Show full text]
  • Wildsafebc Squamish-Lillooet Regional District Annual Report
    WildSafeBC Annual Report 2020 Squamish-Lillooet Regional District Prepared by: Devin Pawluk, WildSafeBC Squamish-Lillooet Regional District Coordinator 0 WildSafeBC Squamish-Lillooet Regional District 2020 Annual Report Executive Summary This report describes the activities of the WildSafeBC Squamish-Lillooet Regional District (SLRD) Program between May 1st and November 30th, 2020. This program is new to the SLRD and complements the work being doing in the Bear Smart Communities of the District of Squamish and the Resort Municipality of Whistler. The SLRD consists of four member municipalities (District of Lillooet, Village of Pemberton, Resort Municipality of Whistler, District of Squamish) and four unincorporated rural Electoral Areas (A, B, C, D) (Figure 1 and Figure 2). While Squamish and Whistler have their own education programs, there was a recognized need for a human-wildlife conflict reduction education in the rural areas and smaller communities. The WildSafeBC SLRD Program focused on the communities of Britannia Beach, Furry Creek, Squamish Valley, Pemberton Meadows, and Lillooet. The SLRD is located within the traditional territories of the Líl'wat, Squamish, St'at'imc, Stó:lō, Tsleil-Waututh, Nlaka'pamux, Tsilhqot'in, and Secwepemc Nations. Pemberton serves as the approximate geographic center of the region and hosts the SLRD office. This season was unusual in that there were several reports of grizzly bears in both Squamish and Whistler. In addition, near Lillooet there were three separate incidents where people were attacked by either a black bear, grizzly bear, or a cougar. Black bears remain the most commonly reported species for the area followed by cougars and coyote.
    [Show full text]
  • Alaskan Analogues and Eastern Uncertainties: Reconstructing Thule Inuit Interaction Networks in the Eastern North American Arctic
    T. Max Friesen Department of Anthropology University of Toronto, Canada Alaskan Analogues and Eastern Uncertainties: Reconstructing Thule Inuit Interaction Networks in the Eastern North American Arctic Introduction Thule archaeology has made great strides over the past several decades. Much has been learned about variability in social organization, settlement patterns, technology, subsistence, and even less visible archaeological phenomena such as gender roles and world view. However, a number of areas remain unclear, one of them being the issue of interaction within and between Thule regional groups. As is the case with all other cultural entities, the Thule tradition in the central Arctic can only be understood fully if the broadest scale of interregional interaction is taken into account. Of course, some attention has been paid to interaction, particularly in the form of trade, with copper, iron, ivory, and other exotic materials commonly reported from Thule sites; and aspects of interac- tion have been used to explain phenomena as diverse as the original Thule mi- gration (McGhee 2000) and the eventual collapse of Classic Thule (Whitridge 1999a). Less attention has been paid to the issue of how interregional systems of interaction operated at a broader scale, although McCartney (1988, 1991), Savelle (2000), and Whitridge (1999a, 1999b, 2002) have made important con- tributions in this area. This paper attempts to build on these previous studies, and in particular McCartney’s (1991) consideration of Thule interaction, in two steps. First, it will consider existing information on Thule interaction in relation to the ethnographic record of Northwest Alaska, which is usually considered the best analogue for understanding the Thule archaeological record.
    [Show full text]
  • The Late Wisconsinan and Holocene Record of Walrus (Odobenus Rosmarus) from North America: a Review with New Data from Arctic and Atlantic Canada ARTHUR S
    ARCTIC VOL. 52, NO. 2 (JUNE 1999) P. 160–181 The Late Wisconsinan and Holocene Record of Walrus (Odobenus rosmarus) from North America: A Review with New Data from Arctic and Atlantic Canada ARTHUR S. DYKE,1 JAMES HOOPER,2 C. RICHARD HARINGTON3 and JAMES M. SAVELLE4 (Received 30 March 1998; accepted in revised form 20 October 1998) ABSTRACT. The Late Wisconsinan and Holocene record of the Atlantic walrus is known from numerous collections of bones and tusks from Arctic Canada and south to North Carolina, as well as from many archaeological sites in the Arctic and Subarctic. In contrast, the Pacific walrus has no dated Late Wisconsinan or early Holocene record in North America, and it may have been displaced into the northwest Pacific at Last Glacial Maximum (LGM). The Atlantic walrus rapidly exploited newly deglaciated territory, moving northward from its LGM refugium and reaching the Bay of Fundy by 12800 B.P., the Grand Banks by 12500 B.P., southern Labrador by 11 500 B.P., and the central Canadian Arctic Archipelago (CAA) by 9700 B.P. Its southern range limit may have retracted to the Bay of Fundy by ca. 7500 B.P. Within the CAA, walrus remains cluster in two main age groups: 9700 to 8500 B.P. and 5000 to 4/3000 B.P. This pattern strongly resembles the distribution of bowhead whale radiocarbon ages from the same area, which suggests a common control by sea-ice conditions. Walrus remains occur in Indian culture archaeological sites as old as 7500 B.P. and, in some cases (Namu, British Columbia, and Mackinac Island, Michigan), they evidently represent long-distance human transport.
    [Show full text]