Landscape Permeability for Large Carnivores in Washington: a GIS Weighted-Distance and Least-Cost Corridor Assessment
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U.Ssosi Svic
THIRTY-YEAR CLUB QGION Six U.SSosi Svic VolumeXXIIISeptember 1979 TIIIBEk LINES June -1979 VOLUME XXIII - I1JULISHED BY FWION SIX FOREST SERVICE 30-YEAR CLUB (Not published inl973) Staff Editor Carroll E. brawn Publication Region Six Forest Servjce 30-Year Club Obituaries Many - As indicated for each iypist Bunty Lilligren x XXX )OCXXX XX XXXXX XXKXXX)O(X xrAx,cc!rcxX x X XXX XX Material appearing in TIMBEJt-LflJES may not be published without express permission ofthe officers of Region SixThirty - YEAR CLUB, ForestServicepublications excepted. TAB.L OF CONTENTS A}tTICLE AND AUTHOR FRONTSPEECE Table of contents i - ii Thirty Year Club Officers,1978 7 1979 iii A word from your editor iv Greetings Fran o club tresident, Carlos T. tiTanu Brown. 1 Greetings Fran Forest Service Chief, John R. )Guire .. 2-3 Greetings Fran Regional Forester, R. E. "Dick Worthington - S Greetings Fran Station Director, Robert F. Tarrant . 6 7 I1oodman Spare that Tree . 7 In Mnoriuin and Obituaries 8-1O Notes Fran Far and Near ljJ. -lili. Sane Early History of Deschutes Nat. For.H'9)4 .0SIT1p4h - Snow, Wind and Sagebrush, Harold E Smith I8 - It.9 Cabin Lake Fire, 1915, Harold E. Smith . l9 - So Fred Groan Becomes a Forest Ranger, Jack Groom Fran the pen of "Dog Lake Ti1ey", Bob Bailey 52 51. Free Use Permit - For Personal Use, Fritz Moisio Sit. The Fort Rock Fire,1917,Harold E, Smith . 55 Christhas, 1917 Harold E. Smith 56 Hi Lo Chicamon; Hi Yu Credit, Harold E. Smith 57 - 58 A Winter Tragedy & Comments by Harold E. -
Wildlife Information for Commercial Backcountry Recreation Opportunities in the North Central Monashee Mountains
WILDLIFE INFORMATION FOR COMMERCIAL BACKCOUNTRY RECREATION OPPORTUNITIES IN THE NORTH CENTRAL MONASHEE MOUNTAINS 1.0 INTRODUCTION Amongst the wide variety of wildlife residing in the North Central Monashee Mountains are rare, threatened or endangered species as well as species of special management emphasis. Color code status has been assigned to species to indicate their vulnerability. Red listed: Includes any indigenous species or subspecies (taxa) considered to be Extirpated, Endangered, or Threatened in British Columbia. Blue listed: Includes any indigenous species or subspecies (taxa) considered to be Vulnerable in British Columbia. Special Management: Includes species which are not red or blue listed but are particularly sensitive to a variety of disturbances and require additional management emphasis. Backcountry recreation has the potential to impact wildlife and wildlife habitat, depending on the location, time of year, intensity, frequency and type of backcountry recreation activity. However, with thorough planning, impacts to wildlife from commercial backcountry recreation can be mitigated. 2.0 COMMERCIAL BACKCOUNTRY RECREATION GUIDELINES During 2000, the Ministry of Environment recognized the need for province-wide commercial backcountry recreation guidelines to address wildlife concerns and allow ministry staff to be provincially consistent in their evaluation of backcountry recreation proposals. The draft provincial guidelines are currently under review, and interim guidelines entitled Expanded Kootenay Region Interim Wildlife Guidelines for Commercial Backcountry Recreation in British Columbia (http://www.elp.gov.bc.ca/wld/comrec/crecintro.html) have been established. The guidelines will assist commercial backcountry operators and government agency staff in protecting wildlife and wildlife habitat while sustaining ecotourism and adventure travel in British Columbia. -
Physiography Geology
BRITISH COLUMBIA DEPARTMENT OF MINES HON. W. K. KIERNAN, Minister P. J. MULCAHY, Deputy Minister NOTES ON PHYSIOGRAPHY AND GEOLOGY OF (Bli BRITISH COLUMBIA b OFFICERS OF THE DEPARTMENT VICTCRIA, B.C. 1961 PHYSIOGRAPHY Physiographic divisions and names are established by the Geographic Board of Canada. Recently H. S. Bostock, of the Geological Survey of Canada, studied the physiography of the northern Cordilleran region; his report and maps are published CI I c Fig. 1. Rglief map of British Columbia. in Memoir 247 of the Geological Survey, Department of Mines and Resources, Ottawa. The divisions shown on the accompanying sketch, Figure 2, and the nomenclature used in the text are those proposed by Bostock. Most of the Province of British Columbia lies within the region of mountains and plateaus, the Cordillera of Western Canada, that forms the western border of the North American Continent. The extreme northeastern comer of the Province, lying east of the Cordillera, is part of the Great Plains region. The Rocky Mountain Area extends along the eastern boundary of the Province for a distance of 400 miles, and continues northwestward for an additional 500 miles entirely within the Province. The high, rugged Rocky Mountains, averaging about 50 miles in width, are flanked on the west by a remarkably long and straight valley, known as the Rocky Mountain Trench, and occupied from south to north by the Kootenay, Columbia, Canoe, Fraser, Parsnip, Finlay, Fox, and Kechika Rivers. Of these, the first four flow into the Pacific Ocean and the second four join the Mackenzie River to flow ultimately into the Arctic Ocean. -
Gold Creek Habitat Memo
Stream & Riparian P.O. Box 15609 Resource Management Seattle, WA 98115 November 5, 2013 Kittitas Conservation Trust 205 Alaska Ave Roslyn, WA 98941-0428 Attention: Mitch Long, Project Manager David Gerth, Executive Director Subject: Gold Creek Habitat Assessment Memo PROJECT BACKGROUND The Kittitas Conservation Trust (KCT) has identified the lower 6.8 miles (mi) of Gold Creek above Keechelus Lake near Snoqualmie Pass as a candidate location for habitat restoration. The primary objectives of the Gold Creek Restoration Project (Project) are to restore perennial flow through the lower 6.8 mi of Gold Creek, and improve instream habitat for threatened Gold Creek Bull Trout (Salvelinus confluentus). The hydrologic, hydraulic, and geomorphic conditions within the project reach will be assessed to determine the causal mechanisms contributing to seasonal dewatering, and the associated impacts to Gold Creek Bull Trout. These findings will be used to develop conceptual designs that meet the primary objectives of the Project by restoring natural geomorphic processes. Existing information relevant to the Project has been reviewed and compiled to guide the assessments and conceptual design development. This information has been synthesized to describe the existing knowledge base related to the Project, and to identify key data gaps that need to be resolved to meet the objectives of the Project (NSD 2013). This technical memo describes the current hydrologic and hydraulic conditions within the Project reach, and how they contribute to seasonal dewatering in Gold Creek. PROJECT REACH Gold Creek drains a 14.3 mi2 (9,122 acre) watershed in the Cascade Mountain range, flowing for approximately 8 miles before entering Keechelus Lake near Interstate 90 (Craig 1997, Wissmar & Craig 2004, USFS 1998). -
Selkirk Mountains Grizzly Bear Recovery Area 2015 Research and Monitoring Progress Report
SELKIRK MOUNTAINS GRIZZLY BEAR RECOVERY AREA 2015 RESEARCH AND MONITORING PROGRESS REPORT PREPARED BY WAYNE F. KASWORM, ALEX WELANDER, THOMAS G. RADANDT, JUSTIN E. TEISBERG, WAYNE L. WAKKINEN, MICHAEL PROCTOR, AND CHRISTOPHER SERVHEEN 2016 UNITED STATES FISH AND WILDLIFE SERVICE GRIZZLY BEAR RECOVERY COORDINATOR'S OFFICE UNIVERSITY OF MONTANA, MAIN HALL ROOM 309 MISSOULA, MONTANA 59812 (406) 243-4903 1 Abstract: Idaho Department of Fish and Game (IDFG) captured and monitored a radio collared sample of grizzly bears in the SMGBRZ from 1983 until 2002 to determine distribution, home ranges, cause specific mortality, reproductive rates, and population trend. This effort was suspended in 2003 due to funding constraints and management decisions. In cooperation with IDFG and the Panhandle National Forest (USFS) this effort was reinitiated during 2012 with personnel from the U.S. Fish and Wildlife Service (USFWS). During 2013 the program was expanded with funding from IDFG, USFS, several sources in British Columbia (BC), and USFWS. This cooperative research and monitoring effort was expanded to involve Idaho Department of Lands, the Kalispel Tribe, the Kootenai Tribe of Idaho, and Washington Department of Fish and Wildlife in 2014 Numbers of females with cubs in the Selkirk Mountains grizzly bear recovery zone (SMGBRZ) varied from 0–4 per year and averaged 1.5 per year from 2010–15. Human caused mortality averaged 1.7 bears per year and 0.7 females per year. Ten human caused mortalities during 2010-15 include 4 females (all BC) and 6 males (one US and five BC). Human caused mortalities during 2010-15 were four adult females (one vehicle collision and three under investigation), one adult male (management), and four subadult males (two management, one mistaken identity, and one self-defense). -
Uranium-Lead Age Constraints and Structural Analysis
Uranium-Lead Age Constraints and Structural Analysis for the Ruddock Creek Zinc-Lead Deposit: Insight into the Tectonic Evolution of the Neoproterozoic Metalliferous Windermere Supergroup, Northern Monashee Mountains, Southern British Columbia (NTS 082M) L.M. Theny, Simon Fraser University, Burnaby, BC, [email protected] H.D. Gibson, Simon Fraser University, Burnaby, BC J.L. Crowley, Boise State University, Boise, ID Theny, L.M., Gibson, H.D. and Crowley, J.L. (2015): Uranium-lead age constraints and structural analysis for the Ruddock Creek zinc- lead deposit: insight into the tectonic evolution of the Neoproterozoic metalliferous Windermere Supergroup, northern Monashee Moun- tains, southern British Columbia (NTS 082M); in Geoscience BC Summary of Activities 2014, Geoscience BC, Report 2015-1, p. 151– 164. Introduction syenite gneiss and syenite gneiss occur as concordant lay- ers within the calcsilicate gneiss. Pegmatite and granitoid The Ruddock Creek property (Figure 1) is situated within intrusions account for approximately 50% of the overall the Windermere Supergroup of the northern Monashee outcrop (Fyles, 1970; Scammell, 1993; Höy, 2001). The Mountains of British Columbia. Structurally, the Ruddock metasedimentary rocks are thought to belong to the Creek property is interpreted to reside within the base of the Windermere Supergroup (Scammell, 1993), which is an Selkirk allochthon, in the immediate hanging wall of the important stratigraphic succession in the North American Monashee décollement, a crustal-scale, thrust-sense duc- Cordillera interpreted to have been originally deposited tile shear zone. Crustal thickening associated with poly- along the rifted western margin of Laurentia during Neo- phase deformation involved at least three episodes of proterozoic time (Gabrielse, 1972; Stewart, 1972, 1976; superposed folding of rocks in the region and two prograde Burchfield and Davis, 1975; Stewart and Suczek, 1977; metamorphic events (Fyles, 1970; Scammell and Brown, Monger and Price, 1979; Eisbacher, 1981; Scammell and 1990; Scammell, 1993; Höy, 2001). -
CANADA's MOUNTAIN Rocky Mountain Goats
CANADA'S MOUNTAIN Rocky Mountain Goats CANADA'S MOUNTAIN PLAYGROUNDS BANFF • JASPER • WATERTON LAKES • YOHO KOOTENAY ° GLACIER • MOUNT REVELSTOKE The National Parks of Canada ANADA'S NATIONAL PARKS are areas The National Parks of Canada may, for C of outstanding beauty and interest that purposes of description, be grouped in three have been set apart by the Federal Govern main divisions—the scenic and recreational ment for public use. They were established parks in the mountains of Western Canada; the to maintain the primitive beauty of the land scenic, recreational, wild animals, and historic scape, to conserve the native wildlife of the parks of the Prairie Provinces; and the scenic, country, and to preserve sites of national his recreational, and historic parks of Eastern Can toric interest. As recreational areas they pro ada. In these pages will be found descriptions vide ideal surroundings for the enjoyment of of the national parks in the first group—areas outdoor life, and now rank among Canada's which lie within the great mountain regions outstanding tourist attractions. of Alberta and British Columbia. Canada's National Park system teas estab * * * lished in 1SS5, when a small area surrounding mineral hot springs at Banff in the Rocky This publication is compiled in co-operation Mountains was reserved as a public posses with the National Parks Branch, Department sion. From this beginning has been developed of Northern Affairs and National Resources. the great chain of national playgrounds note Additional information concerning these parks stretching across Canada from the Selkirk may be obtained from the Park Superintend Mountains in British Columbia to the Atlantic ents, or from the Canadian Government Travel Coast of Nova Scotia. -
The Effects of Linear Developments on Wildlife
Bibliography Rec# 5. LeBlanc, R. 1991. The aversive conditioning of a roadside habituated grizzly bear within Banff Park: progress report 1991. 6 pp. road impacts/ grizzly bear/ Ursus arctos/ Banff National Park/ aversive conditions/ Icefields Parkway. Rec# 10. Forman, R.T.T. 1983. Corridors in a landscape: their ecological structure and function. Ekologia 2 (4):375-87. corridors/ landscape/ width. Rec# 11. McLellan, B.N. 1989. Dymanics of a grizzly bear population during a period of industrial resource extraction. III Natality and rate of increase. Can. J. Zool. Vol. 67 :1865-1868. reproductive rate/ grizzly bear/ Ursus arctos/ British Columbia/ gas exploration/ timber harvest. Rec# 14. McLellan, B.N. 1989. Dynamics of a grizzly bear population during a period of industrial resource extraction. II.Mortality rates and causes of death. Can. J. Zool. Vol. 67 :1861-1864. British Columbia/ grizzly bear/ Ursus arctos/ mortality rate/ hunting/ outdoor recreation/ gas exploration/ timber harvest. Rec# 15. Miller, S.D., Schoen, J. 1993. The Brown Bear in Alaska . brown bear/ grizzly bear/ Ursus arctos middendorfi/ Ursus arctos horribilis/ population density/ distribution/ legal status/ human-bear interactions/ management/ education. Rec# 16. Archibald, W.R., Ellis, R., Hamilton, A.N. 1987. Responses of grizzly bears to logging truck traffic in the Kimsquit River valley, British Columbia. Int. Conf. Bear Res. and Manage. 7:251-7. grizzly bear/ Ursus / arctos/ roads/ traffic/ logging/ displacement/ disturbance/ carnivore/ BC/ individual disruption / habitat displacement / habitat disruption / social / filter-barrier. Rec# 20. Kasworm, W.F., Manley, T.L. 1990. Road and trail influences on grizzly bears and black bears in northwest Montana. -
UNIVERSITY of CALGARY Estimating Extreme Snow
UNIVERSITY OF CALGARY Estimating Extreme Snow Avalanche Runout for the Columbia Mountains and Fernie Area of British Columbia, Canada by: Katherine S. Johnston A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DEPARTMENT OF CIVIL ENGINEERING CALGARY, ALBERTA AUGUST, 2011 ©Katherine S. Johnston 2011 ABSTRACT Extreme snow avalanche runout is typically estimated using a combination of historical and vegetation records as well as statistical and dynamic models. The two classes of statistical models (α – β and runout ratio) are based on estimating runout distance past the β-point, which is generally defined as the point where the avalanche slope incline first decreases to 10°. The parameters for these models vary from mountain range to mountain range. In Canada, α – β and runout ratio parameters have been published for the Rocky and Purcell Mountains and for the British Columbia Coastal mountains. Despite active development, no suitable tall avalanche path model parameters have been published for the Columbia Mountains or for the Lizard Range area around Fernie, BC. Using a dataset of 70 avalanche paths, statistical model parameters have been derived for these regions. In addition, the correlation between extreme and average snowfall values and avalanche runout is explored. iii ACKNOWLEDGEMENTS Thank you to Bruce Jamieson for giving me the opportunity to work on this project, and for coordinating the financial support for this project. His thoughtful advice, numerous reviews, and inspirational leadership have helped make this a fantastic experience. My thanks to Alan Jones for providing numerous hours of guidance, mentoring, and thoughtful discussion throughout this project, and for facilitating data acquisition from outside sources. -
Asturica Augusta
Today, as yesterday, communication and mobility are essential in the configuration of landscapes, understood as cultural creations. The dense networks of roads that nowadays crisscross Europe have a historical depth whose roots lie in its ancient roads. Under the might of Rome, a network of roads was designed for the first time that was capable of linking points very far apart and of organizing the lands they traversed. They represent some of the Empire’s landscapes and are testimony to the ways in which highly diverse regions were integrated under one single power: Integration Water and land: Integration Roads of conquest The rural world of the limits ports and trade of the mountains Roads of conquest The initial course of the roads was often marked by the Rome army in its advance. Their role as an instrument of control over conquered lands was a constant, with soldiers, orders, magistrates, embassies and emperors all moving along them. Alesia is undoubtedly one of the most emblematic landscapes of the war waged by Rome’s legions against the peoples that inhabited Europe. Its material remains and the famous account by Caesar, the Gallic Wars, have meant that Alesia has been recognized for two centuries now as a symbol of the expansion of Rome and the resistance of local communities. Alesia is the famous battle between Julius Caesar and Vercingetorix, the Roman army against the Gaulish tribes. The siege of Alesia took place in 52 BC, but its location was not actually discovered until the 19th century thanks to archeological research! Located on the site of the battle itself, in the centre of France, in Burgundy, in the village of Alise-Sainte-Reine, the MuseoParc Alesia opened its doors in 2012 in order to provide the key to understanding this historical event and the historical context, in order to make history accessible to the greatest number of people. -
Skeletonized Microfossils from the Lower–Middle Cambrian Transition of the Cantabrian Mountains, Northern Spain
Skeletonized microfossils from the Lower–Middle Cambrian transition of the Cantabrian Mountains, northern Spain SÉBASTIEN CLAUSEN and J. JAVIER ÁLVARO Clausen, S. and Álvaro, J.J. 2006. Skeletonized microfossils from the Lower–Middle Cambrian transition of the Cantabrian Mountains, northern Spain. Acta Palaeontologica Polonica 51 (2): 223–238. Two different assemblages of skeletonized microfossils are recorded in bioclastic shoals that cross the Lower–Middle Cambrian boundary in the Esla nappe, Cantabrian Mountains. The uppermost Lower Cambrian sedimentary rocks repre− sent a ramp with ooid−bioclastic shoals that allowed development of protected archaeocyathan−microbial reefs. The shoals yield abundant debris of tube−shelled microfossils, such as hyoliths and hyolithelminths (Torellella), and trilobites. The overlying erosive unconformity marks the disappearance of archaeocyaths and the Iberian Lower–Middle Cambrian boundary. A different assemblage occurs in the overlying glauconitic limestone associated with development of widespread low−relief bioclastic shoals. Their lowermost part is rich in hyoliths, hexactinellid, and heteractinid sponge spicules (Eiffelia), chancelloriid sclerites (at least six form species of Allonnia, Archiasterella, and Chancelloria), cambroclaves (Parazhijinites), probable eoconchariids (Cantabria labyrinthica gen. et sp. nov.), sclerites of uncertain af− finity (Holoplicatella margarita gen. et sp. nov.), echinoderm ossicles and trilobites. Although both bioclastic shoal com− plexes represent similar high−energy conditions, the unconformity at the Lower–Middle Cambrian boundary marks a drastic replacement of microfossil assemblages. This change may represent a real community replacement from hyolithelminth−phosphatic tubular shells to CES (chancelloriid−echinoderm−sponge) meadows. This replacement coin− cides with the immigration event based on trilobites previously reported across the boundary, although the partial infor− mation available from originally carbonate skeletons is also affected by taphonomic bias. -
UPPER YAKIMA RIVER Geographic Response Plan
Northwest Area Committee JUNE 2017 UPPER YAKIMA RIVER Geographic Response Plan (YAKU-GRP) UPPER YAKIMA RIVER GRP JUNE 2017 UPPER YAKIMA RIVER Geographic Response Plan (YAKU-GRP) June 2017 2 UPPER YAKIMA RIVER GRP JUNE 2017 Spill Response Contact Sheet Required Notifications for Oil Spills & Hazardous Substance Releases Federal Notification - National Response Center (800) 424-8802* State Notification - Washington Emergency Management Division (800) 258-5990* - Other Contact Numbers - U.S. Coast Guard Washington State Sector Puget Sound (206) 217-6200 Dept Archaeology & Historic Preservation (360) 586-3065 - Emergency / Watchstander (206) 217-6001* Dept of Ecology - Command Center (206) 217-6002* - Headquarters (Lacey) (360) 407-6000 - Incident Management (206) 217-6214 - Central Regional Office (Union Gap) (509) 575-2490 13th Coast Guard District (800) 982-8813 Dept of Fish and Wildlife (360) 902-2200 National Strike Force (252) 331-6000 - Emergency HPA Assistance (360) 902-2537* - Pacific Strike Team (415) 883-3311 - Oil Spill Team (360) 534-8233* Dept of Health (800) 525-0127 U.S. Environmental Protection Agency - Drinking Water (800) 521-0323 Region 10 – Spill Response (206) 553-1263* Dept of Natural Resources (360) 902-1064 - Washington Ops Office (360) 753-9437 - After normal business hours (360) 556-3921 - RCRA / CERCLA Hotline (800) 424-9346 Dept of Transportation (360) 705-7000 - Public Affairs (206) 553-1203 State Parks & Recreation Commission (360) 902-8613 State Patrol - District 3 (509) 575-2320* National Oceanic Atmospheric Administration State Patrol - District 6 (509) 682-8090* Scientific Support Coordinator (206) 526-6829 Weather (NWS Pendleton) (541) 276-7832 Tribal Contacts Confederated Tribes of the Yakama Nation (509) 865-5121 Other Federal Agencies U.S.