Proposed Osoyoos Airport Development – Environmental Assessment
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Okanagan Range Ecoregion
Selecting Plants for Pollinators A Guide for Gardeners, Farmers, and Land Managers In the Okanagan Range Ecoregion Keremeos and Hedley Table of CONTENTS Why Support Pollinators? 4 Getting Started 5 Okanagan range 6 Meet the Pollinators 8 Plant Traits 10 Developing Plantings 12 Farms 13 Public Lands 14 Home Landscapes 15 Plants That Attract Pollinators 16 Habitat hints 20 Habitat and Nesting requirements 21 S.H.A.R.E. 22 Checklist 22 This is one of several guides for different regions of North America. Resources and Feedback 23 We welcome your feedback to assist us in making the future guides useful. Please contact us at [email protected] 2 Selecting Plants for Pollinators Selecting Plants for Pollinators A Guide for Gardeners, Farmers, and Land Managers In the Okanagan Range Ecoregion Keremeos and Hedley A NAPPC and Pollinator Partnership Canada™ Publication Okanagan Range 3 Why support pollinators? IN THEIR 1996 BOOK, THE FORGOTTEN POLLINATORS, Buchmann and Nabhan estimated that animal pollinators are needed for the reproduction “Flowering plants of 90% of fl owering plants and one third of human food crops. Each of us depends on these industrious pollinators in a practical way to provide us with the wide range of foods we eat. In addition, pollinators are part of the across wild, intricate web that supports the biological diversity in natural ecosystems that helps sustain our quality of life. farmed and even Abundant and healthy populations of pollinators can improve fruit set and quality, and increase fruit size. In farming situations this increases production per hectare. In the wild, biodiversity increases and wildlife urban landscapes food sources increase. -
Minfile Nts 082Ese - Grand Forks
MINFILE NTS 082ESE - GRAND FORKS Original release date: 1997 Researched and compiled by: B.N. Church and L.D. Jones The Grand Forks map area, located in south-central British Columbia, contains 261 documented mineral occurrences, including 108 past producers. The map area includes the historically important Greenwood mining camp, which continues to attract exploration interest and activity. Physiographic domains include the Okanagan Highland over most of the map area, and the Selkirk Mountains to the east of Lower Arrow Lake. The map area lies in the Omineca tectonic belt, which formed in Early to Middle Jurassic time as a result of the accretion of Paleozoic and Mesozoic oceanic and arc rocks of the Slide Mountain and Quesnel terranes. These terranes were delaminated from the oceanic lithosphere and stacked against the continental margin of the North America craton. The resulting calc-alkaline plutonism created a large number of Middle Jurassic intrusions of intermediate composition. These intrude the accreted terranes and the Proterozoic pericratonic Monashee Complex. Overprinting by Cretaceous Laramide and post-Laramide Tertiary transtensional structures has complicated the geology. Paleozoic age, unconformable bedded assemblages include the Knob Hill, Attwood and Anarchist groups. Knob Hill Group is Permo-Carboniferous, and possibly as old as Devonian, and consists of massive and banded MINFILE NTS 082ESE - Grand Forks metacherts and lesser amounts of quartz chlorite schist, amphibolitic schists and gneisses, and limestone bands. The rocks have been affected by deformation and metamorphism causing recrystallization and the development of foliation, quartz sweats parallel to foliation and much deformation of individual beds. The Attwood Group is Permian and consists of black argillite, sharpstone conglomerate, greywacke, limestone lenses and metavolcanic units. -
Okanagan Ecoregional Assessment Volume 1 Report
VOLUME Okanagan 1 Ecoregional Assessment REPORT October 2006 OKANAGAN ECOREGIONAL ASSESSMENT VOLUME 1 REPORT Okanagan Ecoregional Assessment October 2006 Prepared by Nature Conservancy of Canada The Nature Conservancy of Washington and the Washington Department of Fish and Wildlife OKANAGAN ECOREGIONAL ASSESSMENT VOLUME 1 REPORT Okanagan Ecoregional Assessment Volume 1 – Report Citation: Pryce, B., P. Iachetti, G. Wilhere, K. Ciruna, J. Floberg, R. Crawford, R. Dye, M. Fairbarns, S. Farone, S. Ford, M. Goering, M. Heiner, G. Kittel, J. Lewis, D. Nicolson, and N. Warner. 2006. Okanagan Ecoregional Assessment, Volume 1 – Report. Prepared by Nature Conservancy of Canada, The Nature Conservancy of Washington, and the Washington Department of Fish and Wildlife with support from the British Columbia Conservation Data Centre, Washington Department of Natural Resources Natural Heritage Program, and NatureServe. Nature Conservancy of Canada, Victoria, British Columbia. Cover Design: Paul Mazzucca Copyright © 2006 Nature Conservancy of Canada Vancouver, British Columbia Issued by: The Nature Conservancy of Canada Cover Photo Credits: #300 – 1205 Broad Street Methow Valley, Robin Dye; Western screech owl, Victoria, British Columbia, Canada V8W 2A4 A.M. Bezener/One Wild Earth Photography; Great Email: [email protected] basin spadefoot toad, A.M. Bezener/One Wild Earth Photography; Seton Lake, Ian Routley; Canadian Cataloguing in Publication Data: Townsends big-eared bat, Harry van Oort; Mormon metalmark, Orville Dyer; East Chopaka, ISBN 1-897386-00-1 Barbara Pryce; Mountain bluebird, Ian Routley; 1. Biological inventory and assessment – Sockeye salmon, Kristy Ciruna; Badgers, Philippe Okanagan. Verkerk; Lynx, Grant Merrill; Mountain lady’s I. Nature Conservancy of Canada. slipper, George Thornton; Long-billed curlew, Ian II. -
Great Basin Gophersnake,Pituophis Catenifer Deserticola
COSEWIC Assessment and Status Report on the Great Basin Gophersnake Pituophis catenifer deserticola in Canada THREATENED 2013 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. 2013. COSEWIC assessment and status report on the Great Basin Gophersnake Pituophis catenifer deserticola in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. xii + 53 pp. (www.registrelep-sararegistry.gc.ca/default_e.cfm). Previous report(s): COSEWIC 2002. COSEWIC assessment and status report on the Gophersnake Pituophis catenifer in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vii + 33 pp. Waye, H., and C. Shewchuk. 2002. COSEWIC status report on the Gophersnake Pituophis catenifer in Canada in COSEWIC assessment and status report on the Gophersnake Pituophis catenifer in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-33 pp. Production note: COSEWIC would like to acknowledge Lorraine Andrusiak and Mike Sarell for writing the update status report on Great Basin Gophersnake (Pituophis catenifer deserticola) in Canada, prepared under contract with Environment Canada. This report was overseen and edited by Kristiina Ovaska, Co-chair of the COSEWIC Amphibians and Reptiles Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: 819-953-3215 Fax: 819-994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Ếvaluation et Rapport de situation du COSEPAC sur la Couleuvre à nez mince du Grand Bassi (Pituophis catenifer deserticola) au Canada. -
Origins of Lake Okanagan
ORIGINSORIGINS OFOF LAKELAKE OKANAGANOKANAGAN By Murray A. Roed, PhD, PEng Information provided is primarily from a book entitled “Okanagan Geology, British Columbia” published in 2004 by the Kelowna Geology Committee. 05/12/2005 1 INTRODUCTIONINTRODUCTION z Precambrian Time – Vast granitic Continental Crust, Pangaea z Paleozoic Time – Oceanic shelf environment, major mountain building z Mesozoic Time – Island Arc archipelago, plate tectonic structure, Continental Drift, obduction, Interior Mountain Building, Massive Stream Erosion z Cenozoic Time…the valley begins 05/12/2005 2 TheThe CenozoicCenozoic EraEra (Tertiary(Tertiary andand QuaternaryQuaternary Periods)Periods) z Initiation of the Okanagan Rift System z Eocene Volcanic activity, explosive type – Knox Mountain, Mount Boucherie z Development of White Lake River System z Erosion of Highlands, Deposition onto Alberta Plains z The rise of the Rocky Mountains z Folding and Faulting in the Okanagan z Mission Creek Fault z Peneplanation of the Interior of BC 05/12/2005 3 PlateauPlateau VulcanismVulcanism z Uplift, Rifting, and Erosion, regional near- surface magma chamber. z Widespread fluid basaltic flows erupt along fractures and inundate low relief valley system (200 to 300 metres local relief) including part of the Okanagan Valley (Wrinkly Faced Cliff, Oyama). z Continued Uplift, Cooling of the Earth, High 05/12/2005Precipitation, Erosion 4 PreglacialPreglacial ValleyValley SystemSystem z Massive deep erosion along fractured and fault- bounded rocky terrain in the Canadian Cordillera and Interior Plains. z Development of major valleys; topography highly rugged with sharp bold profiles. z Incision or dissection of the Thompson Plateau and Okanagan Highland 05/12/2005 5 THETHE ICEICE AGEAGE z Ice accumulation from massive snowfall z Development of Cordilleran Ice Sheets -beginning with valley glaciers and ending with ice so thick, it overtopped mountains. -
6.2 MULE DEER SPECIES ACCOUNT SPECIES NAME: Mule Deer (Odocoileus Hemionus)
6.2 MULE DEER SPECIES ACCOUNT SPECIES NAME: Mule Deer (Odocoileus hemionus) SPECIES CODE: M-ODHE INTRODUCTION: This document provides the background information for rating mule deer habitat values of pre-defined ecosystem units in TFL 15, south-central British Columbia. Information on mule deer habitat requirements, life requisites, and habitat / landscape use patterns has been accumulated from a variety of sources, including literature reviews, species experts, and previous inventory and mapping efforts. STATUS: Status in Canada (COSEWIC 1998): No formal designation Status in British Columbia (CDC 1999): Provincial Management List: Yellow Global Rank: S5/S4 Provincial Rank: S5/S4 Identified Wildlife (Y/N): N DISTRIBUTION: Continental Range: In North America, mule deer range covers most of the western half of the continent extending from the western coast to central North Dakota, east-central south Dakota, Nebraska, west-central Kansas, and extreme northwestern Oklahoma and Texas (Mackie et al. 1982). The northern limit approximates the tree line while the southern boundary occurs near central Mexico and through the Baja peninsula. Provincial Range: Within British Columbia, three subspecies of mule deer are identified. Mule deer (Odocoileus hemionus hemionus) are distributed throughout much of the interior, east of the coastal mountain range to the Alberta border. They are most common in the southern interior and northeastern portions of the province while remaining absent or sparse in coastal forests and northwestern British Columbia. West of the coastal range, including Vancouver island, is occupied by 2 species of black-tailed deer (O. h. columbiana and O. h. sitkensis), which inhabit coastal forests north to Glacier Bay National Park of Alaska. -
RELOCATION GUIDE 2016 - 2017 Spectacular Waterfront Homes Here’S What Our Residents Are Saying About the Cottages
Community Profile: Economy · Services · Housing Healthcare · Education · Cultural Attractions Recreation · Entertainment & Events RELOCATION GUIDE 2016 - 2017 www.SouthOkanaganRelocation.com Spectacular Waterfront Homes Here’s what our residents are saying about the Cottages. “ e setting is simply stunning, the cycling is gorgeous and safe, there are wonderful hikes to explore, and there are sh just waiting to be hooked. But what we have discovered while building at e Cottages, is the wonderful community – a caring“family” of homeowners, reminiscent of the small towns in the Maritimes where I grew up. It was the location and setting that brought us to e Cottages, but it is the 1.855.742.5555 osoyooscottages.com vibrant and welcoming community that will keep us here.” Visit our website for more details including photo galleries, home plans, video tours and more homeowner testimonials about our Visit our Display Homes » 2450 Radio Tower Road, Oliver, BC gorgeous location and homes. See website for open hours. Welcome to the South Okanagan An area of exceptional beauty and diverse ter- rain, the South Okanagan Valley is positioned at the northernmost tip of the upper Sonoran Desert system, which starts in Mexico and extends through North America as the Great Basin. Canada's only true desert is tucked into the southernmost corner of this beautiful valley, and the extraordinary habitat is home to one of North Americas most fragile ecosystems. The Okana- gan Valley was created by the retreat of massive glaciers approximately 10,000 years ago which left large deposits of gravel, silt, clay and sand behind on the bottom and sides of the valley floor. -
Eocene Paleo-Physiography and Drainage Directions, Southern Interior Plateau, British Columbia1
215 Eocene paleo-physiography and drainage directions, southern Interior Plateau, British Columbia1 Selina Tribe Abstract: A map of reconstructed Eocene physiography and drainage directions is presented for the southern Interior Plateau region, British Columbia south of 53°N. Eocene landforms are inferred from the distribution and depositional paleoenvironment of Eocene rocks and from crosscutting relationships between regional-scale geomorphology and bedrock geology of known age. Eocene drainage directions are inferred from physiography, relief, and base level elevations of the sub-Eocene unconformity and the documented distribution, provenance, and paleocurrents of early Cenozoic fluvial sediments. The Eocene landscape of the southern Interior Plateau resembled its modern counterpart, with highlands, plains, and deeply incised drainages, except regional drainage was to the north. An anabranching valley system trending west and northwest from Quesnel and Shuswap Highlands, across the Cariboo Plateau to the Fraser River valley, contained north-flowing streams from Eocene to early Quaternary time. Other valleys dating back at least to Middle Eocene time include the North Thompson valley south of Clearwater, Thompson valley from Kamloops to Spences Bridge, the valley containing Nicola Lake, Bridge River valley, and Okanagan Lake valley. During the early Cenozoic, highlands existed where the Coast Mountains are today. Southward drainage along the modern Fraser, Chilcotin, and Thompson River valleys was established after the Late Miocene. Résumé : Cet article présente une carte reconstituée de la géographie physique et des directions de drainage, à l’Éocène, pour la région du plateau intérieur de la Colombie-Britannique, au sud du 53e parallèle Nord. Les formes de terrain à l’Éocène sont déduites de la distribution et du paléoenvironnement de déposition des roches de l’Éocène et à partir de relations de recoupement entre la géomorphologie à l’échelle régionale et la géologie du socle, d’âge connu. -
1 Christian Valley Geology
358000m.E. 360000 362000 364000 366000 368000 370000 372000 374000 376000 378000 380000 382000 384000 386000 388000 390000m.E. Big White Mountain Pm CPa 5512000m.N. Pm GEOSCIENCE BC MAP 2017-10 5510000m.N. Jgd GEOLOGY of the 5410000 Goatskin Creek CHRISTIAN VALLEY MAP SHEET KTg 5408000 Eg Pk NTS 082E/10 Mount 5408000 Arthurs SCALE 1:50 000 Qal 0 1 2 3 4 5 5406000 Pk Copper Kettle Creek Ec KILOMETRES Geology and Compilation by Trygve Höy 5406000 GRANBY Pk Cartography by Wayne Jackaman PROVINCIAL Extent of mapping by HÖy and DeFields, 2017 5404000 R e n d e l l C r e e k PARK LEGEND CENOZOIC QUATERNARY ID: 12663 Epm K/Ar 56.3 Qal Alluvium, sand, gravel, till 5404000 Pw MIOCENE/PLIOCENE E R 5402000 Pk KALLIS FORMATION: plateau basalt; black to dark green, fine-grained; locally olivine phyric Pk1 Conglomerate, sandstone, shale Cochrane Creek Mount EOCENE Tanner Ec CORYELL: undifferentiated syenite and monzonite T EL R IV Eg T 5402000 mJg KTg PENTICTON GROUP (Ep): K E Epm MARRON FORMATION: alkali basalt, trachyte; locally amygdaloidal, vesicular or porphyritic; well-banded mafic tuff, blocky tephra; minor black or red shale or slate 5400000 Epm1 UPPER MARRON: basalt Epk KETTLE RIVER FORMATION: basal conglomerate, overlain by feldspathic grit, conglomerate, siltstone and rare shale or argillite; typically light coloured and well bedded 5400000 Trapping Creek Eg Porphyritic granite; coarse-grained with commonly large, pink euhedral K-feldspar crystals Mount Cochrane EOCENE/CRETACEOUS? Pk 5498000 KTg Granite, locally K-feldspar porphyritic; medium -
A National Ecological Framework for Canada
A NATIONAL ECOLOGICAL FRAMEWORK FOR CANADA Written and compiled by: Ecological Stratification Working Group Centre for Land and Biological State of the Environment Directorate Resources Research Environment Conservation Service Research Branch Environment Canada Agriculture and Agri-Food Canada ---- Copies of this report and maps available from: Canadian Soil Information System (CanSIS) Centre for Land and Biological Resources Research Research Branch, Agriculture and Agri-Food Canada Ottawa, ON KIA OC6 State of the Environment Directorate Environmental Conservation Service Environment Canada Hull, PQ KIA OH3 Printed and digital copies of the six regional ecodistrict and ecoregion maps at scale of 1:2 million (Atlantic Provinces #CASOlO; Quebec #CASOll; Ontario #CAS012; Manitoba, Saskatchewan, and Alberta #CAS013; British Columbia and Yukon Territory #CASOI4; and the Northwest Territories #CASOI5); and associated databases are available from Canadian Soil Information System (CanSIS), address as above. co Minister of Supply and Services Canada 1996 Cat. No. A42-65/1996E ISBN 0-662-24107-X Egalement disponible en fran91is sous Ie titre Cadrc ecologiqllc national po"r Ie Canada Bibliographic Citation: Ecological Stratification Working Group. 1995. A National Ecological Framework for Canada. Agriculture and Agri-Food Canada, Research Branch, Centre for Land and Biological Resources Research and Environment Canada, State of the Environment Directorate, Ecozone Analysis Branch, Ottawa/Hull. Report and national map at 1:7500 000 scale. TABLE OF CONTENTS Preface iv Acknowledgemenl<; v 1. Ecolo~cal Re~onalization in Canada 1 2. Methodology. .. .. 2 Map COlnpilation . .. 2 Levels of Generalization. .. 2 Ecozones 2 Ecoregions . 4 Ecodistricts 4 Data Integration. .. 6 3. The Ecological Framework 8 4. Applications of the Framework 8 Reporting Applications. -
Biogeography of Behr's Hairstreak in the South Okanagan
St. John, D., and S. Desjardins. 2003. Biogeography of Behr’s hairstreak (Satyrium behrii columbia McDunnough 1944) in the South Okanagan. Part 1: inventory survey and mapping. Part 2: mark recapture study. Unpublished report. Okanagan University College, Kelowna, British Columbia. 18 pp. Biogeography of Behr’s Hairstreak, Satyrium behrii columbia (McDunnough 1944) in the South Okanagan (Analysis of data collected in 2003 and earlier) PART 1. Inventory Survey and Mapping Introduction Behr’s Hairstreak (Satyrium behrii W. H. Edwards, 1870) is confined to the south Okanagan Valley of British Columbia in Canada(Guppy & Shepard, 2001). Kondla (2003) estimates the Canadian distribution at less than 1% of the global distribution of this species. The species ranges south to southern California, northern Arizona and New Mexico, and an outlier population is found in northwest Texas. From about the middle of Oregon, north to British Columbia, the species’ range narrows to a thin band terminating in British Columbia south of Penticton. This range follows the eastern boundaries of the Oregon and South Cascades Ecogeographic Provinces into Washington state, and parallels the course of the Columbia eastward to Spokane County, and northward along Okanagan river system into BC (Opler, 1999, Pyle 2002). The subspecies Satyrium behrii columbia(McDunnough,1944) is the taxon found in BC and throughout Cascadia(Pyle, 2002). The type locality is at Fairview near Oliver (Guppy & Shepard, 2001). In Cascadia, including BC, antelope brush (Purshia tridentata (Pursh)) is the only known larval foodplant of Behr’s Hairstreak (Guppy & Shepard 2001, Shepard 2000, Pyle 2002). Previous field work indicates that yarrow (Achillea millefolium L.) is the most widely utilized nectar source. -
Athabasca Airport Committee Athabasca County Thursday, October 4, 2018 - 9:30 A.M
A G E N D A Athabasca Airport Committee Athabasca County Thursday, October 4, 2018 - 9:30 a.m. County Office - Chambers Athabasca Airport Committee Athabasca County Thursday, October 4, 2018 - 9:30 a.m. Page 1. CALL TO ORDER 2. APPROVAL OF AGENDA 2.1 October 4, 2018, Airport Committee 3. APPROVAL OF MINUTES 3.1 July 5, 2018, Airport Committee Minutes 3 - 6 4. BUSINESS ARISING FROM THE MINUTES 4.1 2018 Fly-In BBQ Summary 7 4.2 Runway Markings Update 8 5. FINANCIAL 5.1 September 30, 2018 9 6. NEW BUSINESS 6.1 Budget 2019-2021 10 - 13 6.2 Lease Agreement 14 6.3 Husky Energy Wells 15 - 17 6.4 Fuel Sales and Movement 18 - 20 6.5 Lease Extension 21 - 22 6.6 6.7 7. INFORMATION 7.1 Manager's Report 23 7.2 AAMA Newsletters 24 - 49 7.3 8. IN CAMERA ITEMS 8.1 9. NEXT MEETING 9.1 January 10, 2019 10. ADJOURNMENT Page 2 of 49 AGENDA ITEM # 3.1 Athabasca Airport Committee Meeting Athabasca County July 05, 2018 - 9:30 AM Council Chambers PRESENT: Chair Brent Murray; Members Christi Bilsky, Dwayne Rawson, Derrick Woytovicz, Kevin Haines (alternate), Health Safety & Facilities Coordinator Norm De Wet; and Recording Secretary Iryna Kennedy. ABSENT: Member Travais Johnson. CALL TO ORDER: Chair Murray called the meeting to order at 9:30 a.m. APPROVAL OF AGENDA: July 5, 2018, Athabasca Airport Agenda Resolution Moved by Member Haines that the agenda be adopted, as AP 18-15 amended, with the following additions: 6.3 - AAMA Seminar 6.4 - Runway Markings.