Ecosystems of British Columbia
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Gyrfalcon Falco Rusticolus
Gyrfalcon Falco rusticolus Rob Florkiewicz surveys, this area was included. Eight eyries are known from this Characteristics and Range The northern-dwelling Gyrfalcon is part of the province; however, while up to 7 of these eyries have the largest falcon in the world. It breeds mostly along the Arctic been deemed occupied in a single year, no more than 3 have been coasts of North America, Europe and Asia (Booms et al. 2008). productive at the same time. Based on these data and other Over its range, its colour varies from white through silver-grey to sightings, the British Columbia Wildlife Branch estimates the almost black; silver-grey is the most common morph in British breeding population in the province to be fewer than 20 pairs Columbia. It nests on cliff ledges at sites that are often used for (Chutter 2008). decades and where considerable amounts of guano can accumulate. Ptarmigan provide the Gyrfalcon's main prey in In British Columbia, the Gyrfalcon nests on cliff ledges on British Columbia and productivity appears dependent on mountains in alpine areas, usually adjacent to rivers or lakes. ptarmigan numbers. Large size and hunting prowess make the Occasionally, it nests on cliffs of river banks and in abandoned Gyrfalcon a popular bird with falconers, who breed and train Golden Eagle nests. them to hunt waterfowl and other game birds. Conservation and Recommendations Whilst the Gyrfalcon is Distribution, Abundance, and Habitat Most Gyrfalcons breed designated as Not at Risk nationally by COSEWIC, it is Blue-listed along the Arctic coast; however, a few breed in the northwest in British Columbia due to its small known breeding population portion of the Northern Boreal Mountains Ecoprovince of British (British Columbia Ministry of Environment 2014). -
Fraser River from Source to Mouth
FRASER RIVER FROM SOURCE TO MOUTH September 5, 2017 - 11 Days Fares Per Person: $3395 double/twin $4065 single $3210 triple > Please add 5% GST. Early Bookers: $160 discount on first 12 seats; $80 on next 8 > Experience Points: Earn 76 points from this tour. Redeem 76 points if you book by July 5. Includes Flight from Victoria to Kelowna St. John the Divine Church in Yale Coach transportation for 10 days Harrison Hot Springs pools 10 nights of accommodation & hotel taxes Copper Room music & dancing with Jones Boys Helicopter to the source of the Fraser River Fraser River Safari boat excursion Fraser River raft float trip (no white water) Paddlewheeler cruise from New Westminster Huble Homestead tour to the mouth of the Fraser River Farwell Canyon and pictographs Gulf of Georgia Cannery National Historic Site Cariboo Chilcotin Museum Transfer from New Westminster to Victoria Hat Creek Historic Ranch and roadhouse tour Knowledgeable tour director Hell’s Gate Airtram Luggage handling at hotels Alexandra Suspension Bridge 21 meals: 8 breakfasts, 9 lunches, 4 dinners Activity Level This is a unique tour with lots of activity and time outdoors while you experience many aspects of the Fraser River. The trip to the source of the Fraser requires getting in and out of a helicopter, and walking about ½ km in an alpine meadow at 2,000 metres altitude. On other days, you are boarding a large raft and two boats. Walks in- clude Farwell Canyon pictographs, Alexandra Bridge, and the boat dock to Kilby Store. This tour has activity ranging from somewhat rigorous to sedentary. -
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. -
Final Witness Statement of Bernadette Manuel May 27, 2015 (00251209
IN THE MATTER OF NATIONAL ENERGY BOARD Hearing Order OH-001-2014 Trans Mountain Pipeline ULC Application for the Trans Mountain Expansion Project WITNESS STATEMENT OF BERNADETTE WANDA MANUEL Introduction 1. My name is Bernadette Wanda Manuel, and I am a member of the Upper Nicola Band (“Upper Nicola”). 2. I was born and raised in Nicola Valley, at Spaxomin. I went to school here, and have spent the majority of my life here or in other parts of Syilx Territory. My father was the late Herb Manuel, from Spaxomin, and my mother was the late Dorothy Saddleman, from Coldwater. My paternal grandparents were Francis Saddleman, from Quilchena and Mary Jane Captain, from Coldwater. My maternal grandparents were Daniel Manuel from Spaxomin and Susan Bent, from Shulus. I also have relatives from Boston Bar. I have two brothers and one sister, and I am the third child of Herb and Dorothy Manuel. 3. My Dad could speak numerous interior languages including St’at’imc, Syilx, Nlaka’pamux, and Secwepemc. He also knew and understood the Chinook language, the trade language. My father was very knowledgeable with respect to our culture and teachings, and his knowledge was sought by others. I grew up with the Syilx culture and teachings, with my father being one of my primary teachers, along with my older brother, Fabian Manuel. 4. I currently work for the Upper Nicola Band as the Cultural Heritage Project Manager. Part of my job is to ensure proponents/consultants comply with Upper Nicola laws, policies and protocols with respect to our cultural heritage, archaeological sites and environmental matters. -
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. -
Chapter Vii Table of Contents
CHAPTER VII TABLE OF CONTENTS VII. APPENDICES AND REFERENCES CITED........................................................................1 Appendix 1: Description of Vegetation Databases......................................................................1 Appendix 2: Suggested Stocking Levels......................................................................................8 Appendix 3: Known Plants of the Desolation Watershed.........................................................15 Literature Cited............................................................................................................................25 CHAPTER VII - APPENDICES & REFERENCES - DESOLATION ECOSYSTEM ANALYSIS i VII. APPENDICES AND REFERENCES CITED Appendix 1: Description of Vegetation Databases Vegetation data for the Desolation ecosystem analysis was stored in three different databases. This document serves as a data dictionary for the existing vegetation, historical vegetation, and potential natural vegetation databases, as described below: • Interpretation of aerial photography acquired in 1995, 1996, and 1997 was used to characterize existing (current) conditions. The 1996 and 1997 photography was obtained after cessation of the Bull and Summit wildfires in order to characterize post-fire conditions. The database name is: 97veg. • Interpretation of late-1930s and early-1940s photography was used to characterize historical conditions. The database name is: 39veg. • The potential natural vegetation was determined for each polygon in the analysis -
Alplains 2013 Seed Catalog P.O
ALPLAINS 2013 SEED CATALOG P.O. BOX 489, KIOWA, CO 80117-0489, U.S.A. Three ways to contact us: FAX: (303) 621-2864 (24 HRS.) email: [email protected] website: www.alplains.com Dear Growing Friends: Welcome to our 23rd annual seed catalog! The summer of 2012 was long, hot and brutal, with drought afflicting most of the U.S. Most of my botanical explorations were restricted to Idaho, Wash- ington, Oregon and northern California but even there moisture was below average. In a year like this, seeps, swales, springs, vestigial snowbanks and localized rainstorms became much more important in my search for seeding plants. On the Snake River Plains of southern Idaho and the scab- lands of eastern Washington, early bloomers such as Viola beckwithii, V. trinervata, Ranunculus glaberrimus, Ranunculus andersonii, Fritillaria pudica and Primula cusickiana put on quite a show in mid-April but many populations could not set seed. In northern Idaho, Erythronium idahoense flowered extensively, whole meadows were covered with thousands of the creamy, pendant blossoms. One of my most satisfying finds in the Hells Canyon area had to be Sedum valens. The tiny glaucous rosettes, surround- ed by a ring of red leaves, are a succulent connoisseur’s dream. Higher up, the brilliant blue spikes of Synthyris missurica punctuated the canyon walls. In southern Oregon, the brilliant red spikes of Pedicularis densiflora lit up the Siskiyou forest floor. Further north in Oregon, large populations of Erythronium elegans, Erythronium oregonum ssp. leucandrum, Erythro- nium revolutum, trilliums and sedums provided wonderful picture-taking opportunities. Eriogonum species did well despite the drought, many of them true xerics. -
Reproductive Biology of Erythronium Grandiflorum Pursh Varieties Grandiflorum and Candidum (Piper) Abrams (Liliaceae)" (1986)
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1986 Reproductive biology of Erythronium grandiflorum Pursh arietiesv grandiflorum and candidum (Piper) Abrams (Liliaceae) Jane K. Fritz-Sheridan The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Fritz-Sheridan, Jane K., "Reproductive biology of Erythronium grandiflorum Pursh varieties grandiflorum and candidum (Piper) Abrams (Liliaceae)" (1986). Graduate Student Theses, Dissertations, & Professional Papers. 7403. https://scholarworks.umt.edu/etd/7403 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. COPYRIGHT ACT OF 1976 Th is is an unpublished manuscript in which copyright sub s is t s . Any FURTHER REPRINTING OF ITS CONTENTS MUST BE APPROVED BY THE AUTHOR. Ma n s fie ld L ibrary U n iv e r s it y of Montana Date : 1 98-6 REPRODUCTIVE BIOLOGY OF ER'iTHRONtUM GRANDIFLORUM PURSH VARIETIES GRANDtFLORUM m o CANDIDUM (PIPER) ABRAMS (LILIACEAE) by Jane K. Fritz-Sheridan B. S ., Michigan State U n iv e rs ity , 1972 M. S., University of Montana, 1981 Presented in partial fulfillment of the requirements for the degree of Master of Arts U n iv e rs ity of Montana 1906 Approved by ïhairm^, B^ard of Examiners D^n, Graduate SC^^I /f, Date UMI Number: EP38204 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction Is dependent upon the quality of the copy submitted. -
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. -
Mkwal'ts Conservancy Management Plan
Mkwal’ts Conservancy Management Plan ConservancyProtected Area] March 2012 Cover photo: Shore of Lillooet Lake at the mouth of Ure Creek. Photo credit: Liz Scroggins Mkwal’ts Conservancy Management Plan ii Acknowledgements The Lil’wat Nation and BC Parks have jointly prepared this management plan. The management planning process was coordinated by Harriet VanWart, Referral Coordinator, and Lucinda Phillips, Director, Land and Resources Department of the Lil’wat Nation and by Vicki Haberl, Planning Section Head, South Coast Region, BC Parks. Tracy Howlett, GIS Manager for the Lil’wat Nation Land and Resources Department, prepared all of the maps. Liz Scroggins of Scroggins Consulting prepared management plan drafts for review by Lil’wat Nation and BC Parks, under contract to Lil’wat Nation. The planning team extends special thanks to Johnny Jones and Lex Joseph of the Lil’wat Nation for their input on culturally significant features and for their review of the management plan documents. Additional thanks are also extended to Jennie Aikman, BC Parks Planner for the Ministry of Environment, for providing support to the planning process. The Lil’wat Nation and Ministry of Environment would like to thank those who took the time to provide comments on this conservancy management plan. iii Table of Contents Acknowledgements............................................................................................................... iii 1.0 Introduction ...............................................................................................................1 -
Late Prehistoric Cultural Horizons on the Canadian Plateau
LATE PREHISTORIC CULTURAL HORIZONS ON THE CANADIAN PLATEAU Department of Archaeology Thomas H. Richards Simon Fraser University Michael K. Rousseau Publication Number 16 1987 Archaeology Press Simon Fraser University Burnaby, B.C. PUBLICATIONS COMMITTEE Roy L. Carlson (Chairman) Knut R. Fladmark Brian Hayden Philip M. Hobler Jack D. Nance Erie Nelson All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording or any information storage and retrieval system, without permission in writing from the publisher. ISBN 0-86491-077-0 PRINTED IN CANADA The Department of Archaeology publishes papers and monographs which relate to its teaching and research interests. Communications concerning publications should be directed to the Chairman of the Publications Committee. © Copyright 1987 Department of Archaeology Simon Fraser University Late Prehistoric Cultural Horizons on the Canadian Plateau by Thomas H. Richards and Michael K. Rousseau Department of Archaeology Simon Fraser University Publication Number 16 1987 Burnaby, British Columbia We respectfully dedicate this volume to the memory of CHARLES E. BORDEN (1905-1978) the father of British Columbia archaeology. 11 TABLE OF CONTENTS Page Acknowledgements.................................................................................................................................vii List of Figures.....................................................................................................................................iv