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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. -
Riding the Kettle Valley Railway
BC Ballast Riding the Kettle Valley Railway Story and photos by Chuck Haney BC Ballast ith chains lubed, tires topped In past cycling trips to the backroads and off with air, and water in the trails of Colorado, Utah, and Oregon, Mike packs, another two-wheeled and I seemed destined to follow a dubious Wadventure was set in motion as the morning pattern of unpredictable weather leading sunlight began to filter through thick stands to various misadventures from incessant of coniferous forest. The cool of the morn- rain, wind, or even snow mucking up our ing air slowly dissipated to the warmth of planned itinerary. Throw in car troubles, a lengthy June summer day. Ravens called tow trucks, raccoons setting off car alarms out to each other from opposing sides of in the middle of the night in a full camp- the trail, their squawking banter and the ground, and getting lost, and it seemed we gravel ballast crunched constantly below had been through it all. But for this particu- our tires. This was the soundtrack of our lar trip, the skies remained clear, the winds first day of riding. In south central British were calm, and even annoying things like Columbia, mighty locomotives were once mosquitoes stayed mostly at bay. the undeniable kings of the Kettle Valley. Our British Columbia adventure on I’m once again paired up with Adventure the KVR began near the remote town of Cyclist editor, Mike Deme, for a cycling Westbridge, which is small enough to be view of the rapids below. For the first excursion in a far-flung location. -
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. -
Large Creekfront Acreage Less Than an Hour from Kelowna
® Large Creekfront Acreage Less Than an Hour from Kelowna Sam Hodson Personal Real Estate Corporation www.landquest.com [email protected] (604) 809-2616 ® Marketing British Columbia to the World® “The Source” for Oceanfront, Lakefront, Islands, Ranches, Resorts & Land in British Columbia www.landquest.com www.landquest.com Large Creekfront Acreage Less Than an Hour from Kelowna PROPERTY DETAILS As you drive up Wilkinson Creek FSR Road you’ll see that the property takes in both the north and south side of the valley, with large flat sections with Listing Number: 20242 excellent views on the top of each ridge. The entire Price: $1,995,000 valley bottom is flat and usable with over 2.5 km of creek frontage on Wilkinson Creek. There are Taxes (2020): $7,462.23 literally dozens of potential building sites near the creek for your backcountry getaway. The views Size: 1,655 acres from the upper sections of the property look out over the Kettle River Valley to the south and are Zoning: None quite spectacular. DESCRIPTION Keep in mind this property is located in an area with no zoning, so subdivision, multiple cabins, RV This impressive 1,655 acre property is located sites are all good options for a savvy investor. This less than 70 km from downtown Kelowna and a is one of the largest private land holdings in close 20-minute drive to Big White Ski Resort. After proximity to the Okanagan and your opportunity to turning off Highway 33 acreage begins 1.35 km up take advantage of an emerging trend within British Wilkinson Creek FSR Road and runs along both Columbia with soaring RV popularity and desire sides of the road for the next 3 km to the north for wide open spaces. -
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. -
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. -
Kettle River Watershed Analysis Midway, British Columbia to Stream Headwaters
1 Kettle River watershed analysis Midway, British Columbia to stream headwaters Robert Maciak, Trevor Ford, Jenn Schroeder 2 Table of Contents Introduction p. 3 Watershed Description p. 4-10 Issues concerning quality p. 10-13 Issues concerning quantity p. 14-16 Recommendations p. 16 Monitoring strategies p. 18-20 Summary p. 21 References p. 21-22 3 Introduction The Kettle River flows from its headwaters in the Christian Valley, located in the Southern Interior of British Columbia, Canada to the Columbia River in Washington State, USA. We have chosen the drainage upstream of Midway, BC as our sample segment. This is an ideal location for analysis for several reasons: First, the headwaters are located in this area, as are two notable tributaries, the West Kettle River and Boundary Creek; second, the Kettle is a trans-boundary river shared by both Canadian and American riparians and Midway, British Columbia is where the river first crosses the border, making it an important point internationally; third, there are a variety of land use and water quality issues; and finally, Environment Canada has available data sets for the Kettle River at Midway from 1972 to present (BWP Consulting, 2003). Before crossing into the United States, the Kettle River’s resources affect both local riparians as well as visitors. The primary value of the river is irrigation for agricultural purposes. Although, water quality in the river is reported to be excellent, there are concerns of high fluoride levels and increasing levels of fecal coli form (BC Ministry of Environment, 1996). During the summer months the Kettle is used widely by locals and visitors alike for recreational purposes. -
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. -
Geology and Thermal History of an Area Near Okanagan Lake, Southern British Columbia
GEOLOGY AND THERMAL HISTORY OF AN AREA NEAR OKANAGAN LAKE, SOUTHERN BRITISH COLUMBIA. by Gary Allan Medford B.Sc.(Hon.) McGill University 1968 M.Sc. McGill University 1970 A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in the Department of Geological Sciences We accept thi.s thesis as conforming to the required standard. THE UNIVERSITY OF BRITISH COLUMBIA January, 1976 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the Head of my Department or by his representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Depa rtment The University of British Columbia Vancouver 8, Canada Date i ABSTRACT Five phases of deformation are recognized in Shuswap (Monashee Group) gneiss in an area east of Okanagan Lake, southern British Columbia.. The first is delineated by north trending mesoscopic structures. The second comprises a south closing megascopic synform with a horizontal ESE axial direction. This structure has in turn been coaxially refolded into a more open phase 3 synform. The second deformation was associated with extensive introduction of synkinematic quartz monzonite and granodiorite that comprises much of the area, and culminated with amphibolite grade metamorphism. Phase 3 deformation was followed by extensive local recrystal1ization and meta• somatism which destroyed earlier fabric elements of the gneisses.