Okanagan Range Ecoregion
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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. -
Ecoregions with Grasslands in British Columbia, the Yukon, and Southern Ontario
83 Chapter 4 Ecoregions with Grasslands in British Columbia, the Yukon, and Southern Ontario Joseph D. Shorthouse Department of Biology, Laurentian University Sudbury, Ontario, Canada P3E 2C6 Abstract. The second largest grasslands of Canada are found in south-central British Columbia in valleys between mountain ranges and on arid mountain-side steppes or benchlands. The province contains five ecozones, with most of the grassland habitat in the Montane Cordillera Ecozone. This ecozone consists of a series of plateaux and low mountain ranges and comprises 17 ecoregions, 7 of which contain grasslands. Dominant grasses here are bunchgrasses. A few scattered grasslands are found in the Yukon in the Boreal Cordillera Ecozone within three ecoregions. Grasslands in southwestern Ontario consist of about 100 small remnants of what was once much more abundant tallgrass prairie. These grasslands grow in association with widely spaced deciduous trees and are remnants of a past prairie peninsula. Grasslands called alvars are also found on flat limestone bedrock in southern Ontario. This chapter briefly describes the physiography, climate, soils, and prominent flora of each ecoregion for the benefit of future biologists wishing to study the biota of these unique grasslands. Résumé. Les prairies du centre-sud de la Colombie-Britannique sont les deuxièmes plus vastes au Canada. Elles se trouvent dans les vallées séparant les chaînes de montagnes, et sur les steppes ou replats arides à flanc de montagne. La province renferme cinq écozones, et l’habitat de prairies se trouve principalement dans l’écozone de la cordillère alpestre. Cette écozone est constituée d’une série de plateaux et de chaînes de montagnes basses et se divise en 17 écorégions, dont 7 renferment des prairies. -
Forest District
F'INAL REPORT PEAK F'LO\ry.CULVERT DESIGN STUDY: PET{TICTOD{ FOREST DISTRICT Prepøredfor: Prepared by: Weyerhaeuser Company Limited Summit Environmental Consultants Ltd. B.C. Timberlands 174 - 100 Kalamalka Lake Road 668 St. Anne Road Vemon, B.C. VlT 7M3 Armstrong, B.C. VOE 1BO Project 042-13.00 October 2000 gl4 October 18,2000 Reference: 042-13.00 Mr. Nick Kleyn, R.P.F. Weyerhaeuser Company Limited. - B.C. Timberlands 668 St. Anne Road Armshong, B.C. VOE 1BO Dear Mr. Kleyn: Re: Peak Flow - Culvert Design Study for Penticton Forest District Summit Environmental Consultants Ltd. is pleased to provide you with two copies of the Final Report on the above-noted study. The report presents our peak flow regionalisation for the Penticton Forest District, and discusses the features, assumptions and limitations of the computer program CULVERT (Ver. 6.1) that uses the results of this regionalisation for estimating required culvert sizes. We have enjoyed working on this project, and would be pleased to provide any additional assistance you may require. Please call me at 545-3672 if you have any questions or wish to discuss any aspect ofthe report. Yours truly, Summit Environmental Consultants Ltd. Brian T. Guy, Ph.D., P.Geo., P.H. President Senior Geoscientist Enclosures: 2 copies of Final Report TABLE OF CONTENTS LETTER OF TRANSMITTAL.... .................. i TABLE OF CONTENTS.............. ................ ii LIST OF TABLES ....................iii LrsT oF FTGURES.. ................. iii LrsT oF ATTACHMENTS ............. ........... iii 1.0 rNTRODUCTrON......... ........................1 2.0 DESTGN PEAK FLOW r{YDROLOGY............ ........................3 2.1 Background ....................3 2.2 Index Flood Method..... -
MOTHS and BUTTERFLIES LEPIDOPTERA DISTRIBUTION DATA SOURCES (LEPIDOPTERA) * Detailed Distributional Information Has Been J.D
MOTHS AND BUTTERFLIES LEPIDOPTERA DISTRIBUTION DATA SOURCES (LEPIDOPTERA) * Detailed distributional information has been J.D. Lafontaine published for only a few groups of Lepidoptera in western Biological Resources Program, Agriculture and Agri-food Canada. Scott (1986) gives good distribution maps for Canada butterflies in North America but these are generalized shade Central Experimental Farm Ottawa, Ontario K1A 0C6 maps that give no detail within the Montane Cordillera Ecozone. A series of memoirs on the Inchworms (family and Geometridae) of Canada by McGuffin (1967, 1972, 1977, 1981, 1987) and Bolte (1990) cover about 3/4 of the Canadian J.T. Troubridge fauna and include dot maps for most species. A long term project on the “Forest Lepidoptera of Canada” resulted in a Pacific Agri-Food Research Centre (Agassiz) four volume series on Lepidoptera that feed on trees in Agriculture and Agri-Food Canada Canada and these also give dot maps for most species Box 1000, Agassiz, B.C. V0M 1A0 (McGugan, 1958; Prentice, 1962, 1963, 1965). Dot maps for three groups of Cutworm Moths (Family Noctuidae): the subfamily Plusiinae (Lafontaine and Poole, 1991), the subfamilies Cuculliinae and Psaphidinae (Poole, 1995), and ABSTRACT the tribe Noctuini (subfamily Noctuinae) (Lafontaine, 1998) have also been published. Most fascicles in The Moths of The Montane Cordillera Ecozone of British Columbia America North of Mexico series (e.g. Ferguson, 1971-72, and southwestern Alberta supports a diverse fauna with over 1978; Franclemont, 1973; Hodges, 1971, 1986; Lafontaine, 2,000 species of butterflies and moths (Order Lepidoptera) 1987; Munroe, 1972-74, 1976; Neunzig, 1986, 1990, 1997) recorded to date. -
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. -
National Park System: a Screening Level Assessment
Environment Canada Parks Canada Environnement Canada Parcs Canada Edited by: Daniel Scott Adaptation & Impacts Research Group, Environment Canada and Roger Suffling School of Planning, University of Waterloo May 2000 Climate change and Canada’s national park system: A screening level assessment Le Changement climatique et le réseau des parcs nationaux du Canada : une évaluation préliminaire This report was prepared for Parks Canada, Department of Canadian Heritage by the Adaptation & Impacts Research Group, Environment Canada and the Faculty of Environmental Studies, University of Waterloo. The views expressed in the report are those of the study team and do not necessarily represent the opinions of Parks Canada or Environment Canada. Catalogue No.: En56-155/2000E ISBN: 0-662-28976-5 This publication is available in PDF format through the Adaptation and Impacts Research Group, Environment Canada web site < www1.tor.ec.gc.ca/airg > and available in Canada from the following Environment Canada office: Inquiry Centre 351 St. Joseph Boulevard Hull, Quebec K1A 0H3 Telephone: (819) 997-2800 or 1-800-668-6767 Fax: (819) 953-2225 Email: [email protected] i Climate change and Canada’s national park system: A screening level assessment Le Changement climatique et le réseau des parcs nationaux du Canada : une évaluation préliminaire Project Leads and Editors: Dr. Daniel Scott1 and Dr. Roger Suffling2 1 Adaptation and Impacts Research Group, Environment Canada c/o the Faculty of Environmental Studies, University of Waterloo Waterloo, Ontario N2L 3G1 519-888-4567 ext. 5497 [email protected] 2 School of Planning Faculty of Environmental Studies, University of Waterloo Waterloo, Ontario N2L 3G1 Research Team: Derek Armitage - Ph.D. -
Integrating Biophysical and Eco-Cultural Fire in Canada Doi: 10.4996/Fireecology.0701074 Page 74
Fire Ecology Volume 7, Issue 1, 2011 White et al.: Integrating Biophysical and Eco-Cultural Fire in Canada doi: 10.4996/fireecology.0701074 Page 74 FORUM ARTICLE BURNING AT THE EDGE: INTEGRATING BIOPHYSICAL AND ECO-CULTURAL FIRE PROCESSES IN CANADA’S PARKS AND PROTECTED AREAS Clifford A. White1*, Daniel D.B. Perrakis2, Victor G. Kafka3, and Timothy Ennis4 1Parks Canada Agency, P.O. Box 900, Banff National Park, Banff, Alberta, Canada T1L 1K2 2 British Columbia Ministry of Natural Resource Operations, Wildfire Management Branch, P.O. Box 9502 Station Provincial Government Victoria, British Columbia, Canada V8W 9C1 3Parks Canada Agency, Ecosystem Conservation Service, 3 passage du Chien d’Or, C.P. 6060, Haute-Ville, Québec, Province of Québec, Canada G1R 4V7 4 Nature Conservancy of Canada, 200-825 Broughton Street, Victoria, British Columbia, Canada V8W 1E5 *Corresponding author: Tel.: 001-403-760-0203; e-mail: [email protected] ABSTRACT Currently, high intensity, large-area lightning fires that burn during droughts dominate Canada’s fire regimes. However, studies from several disciplines clearly show that hu- mans historically ignited burns within this matrix of large fires. Two approaches for fire research and management have arisen from this pattern: a “large-fire biophysical para- digm” related to lightning-ignited fires, and an “eco-cultural paradigm” related to human- caused burning. Working at the edge between biophysically driven fires and eco-cultural burns, and their associated management and research paradigms, presents unique chal- lenges to land managers. We proceed by describing fire frequency trends across Canada, and how an interaction between changing climatic and cultural factors may provide better causal explanations for observed patterns than either group of factors alone. -
Article Is Available On- Anderson, E
Hydrol. Earth Syst. Sci., 25, 2513–2541, 2021 https://doi.org/10.5194/hess-25-2513-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. The spatial extent of hydrological and landscape changes across the mountains and prairies of Canada in the Mackenzie and Nelson River basins based on data from a warm-season time window Paul H. Whitfield1,2,3, Philip D. A. Kraaijenbrink4, Kevin R. Shook1, and John W. Pomeroy1 1Centre for Hydrology, University of Saskatchewan, Saskatoon, SK, S7N 1K2, Canada 2Department of Earth Sciences, Simon Fraser University, Burnaby, BC, Canada 3Environment and Climate Change Canada, Vancouver, BC, Canada 4Geosciences, Utrecht University, Utrecht, the Netherlands Correspondence: Paul H. Whitfield (paul.h.whitfi[email protected]) Received: 24 November 2020 – Discussion started: 4 January 2021 Revised: 30 March 2021 – Accepted: 8 April 2021 – Published: 18 May 2021 Abstract. East of the Continental Divide in the cold inte- separating the Canadian Rockies and other mountain ranges rior of Western Canada, the Mackenzie and Nelson River in the west from the poorly defined drainage basins in the basins have some of the world’s most extreme and variable east and north. Three specific areas of change were iden- climates, and the warming climate is changing the landscape, tified: (i) in the mountains and cold taiga-covered subarc- vegetation, cryosphere, and hydrology. Available data consist tic, streamflow and greenness were increasing while wetness of streamflow records from a large number (395) of natu- and snowcover were decreasing, (ii) in the forested Boreal ral (unmanaged) gauged basins, where flow may be peren- Plains, particularly in the mountainous west, streamflows nial or temporary, collected either year-round or during only and greenness were decreasing but wetness and snowcover the warm season, for a different series of years between were not changing, and (iii) in the semi-arid to sub-humid 1910 and 2012. -
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. -
The Amazing Race How Does Agriculture Make Regions Unique?
Learning Sources PROJECT Agriculture Project-Based Learning and Teaching Series The Amazing Race How does agriculture make regions unique? www.albertamilk.com/teacher-resources/ PROJECT Agriculture Learning Source: The Amazing Race 1 ©Alberta Milk 2017 Permission is granted to make copies of any or all parts of this resource for educational, not-for-profit use only. Readers should be aware that Internet websites offered as citations and/or sources for further information may have changed or disappeared between the time this was written and when it is read. Teachers are cautioned that all websites listed in this resource should be checked for appropriateness and suitability before being provided to, or used with, students. Every effort has been made to acknowledge sources used in the PROJECT Agriculture resources. In the event of questions arising as to the use of any material, we will be pleased to make the necessary corrections in future printings. Please contact Patricia Shields-Ramsay at InPraxis Learning at 780.421.7163. This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License. To view a copy of this license, visit http:// creativecommons.org/licenses/by-nc-sa/4.0/ or send a letter to Creative Commons, PO Box 1866, Mountain View, CA 94042, USA. 2 PROJECT Agriculture Learning Source: The Amazing Race Learning Source: The Amazing Race Cross Country Canada How do geographers define a region? Regions are areas that share common characteristics. They are identified by the natural features or geographic characteristics that an area shares. Regions are often named by the main physical or geographic feature. -
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.