Teaching Activities

Total Page:16

File Type:pdf, Size:1020Kb

Teaching Activities S QUAMISH RIVERS & ESTUARY Squamish Streams Around the Corner Grades: 4-7 Subject, Science, Language Arts Time required:30 –60 minutes Key Concepts: Everyday actions make a difference in watershed and estuary health.. Objectives: To identify local streams and protected areas Background: To use research, mapping and Materials interviewing skills; In British Columbia, there are many different use a variety of ways to types of protected areas. They include public Maps collect and record data; lands in networks of national, provincial and regional parks, wildlife management areas, (community & school) recreation areas, wilderness areas, ecological reserves, nature sanctuaries, greenways and Student Journals municipal parks, cultural heritage sites, heri- Pencil or pen Key Words: tage buildings and more. They also include water areas that are protected but not owned by the Streams, protected areas public but are protected by a range of fed- eral, provincial or local regulations. These types of protected areas include local areas such as water-courses (rivers, streams, lakes, Skills: ponds, wetlands) and their riparian Analysis, discussion, listing, writing/ (streamside) areas, environmentally sensitive drawing areas, and other areas of noted local impor- tance. 1 Squamish Streams Around the Corner Protected areas range in size from vast expanses of wilderness areas to tiny pockets memorabilia. of nature covering a few hectares or less. 4. Ask each group to brainstorm a list of Together, protected areas on public and places and people in their community private lands provide ways to protect natural that might be able to help them answer ecosystems such as streams as well as to the following questions about their enhance and restore local natural areas. stream: As students study their community map, • What is protected here? they will find streams nearby. Visiting these • Why is it protected? areas will increase their knowledge and may • Who or what is it protected from? lead to active involvement in caring for • How is this place protected? these streams and the organisms that live • What are the costs (monetary and there. other) of protecting this place? • What are the costs (monetary and other) of not protecting this place? Procedure: 5. Organize a walking field trip to the local 1. As a class, brainstorm as many different stream or river. On the field trip day, kinds of protected areas that might be visit the site and ask them to take their found nearby the school. Use the journals and write about: students’ list to locate all of these places • what they see, hear, feel and/or smell on a community map. Some of these at the site areas may include: rivers and streams, • how they feel visiting the site. parks and green spaces, and trails. 5. Back in class, ask students to present 2. Go to the map folder of the teacher CD their findings. The conversation might and find the map of your school. Hand center around what surprised them most out the map to students. In groups of two at the site they visited. Challenge them or three, ask them to find local to discuss the questions listed above. landmarks and then to find examples of Extensions: parks, streams/rivers, green spaces and trails on their map. 1. Ask students to write a short 3. Discuss different ways that they could sentence or poem (such as a haiku) find out more about their local stream or which sums up what they learned protected area. This might include about the stream they visited. making observations, interviewing Evaluation: people, reading newspaper clippings, Have students describe the stream or river pamphlets or historical records, nearby the school and why it is important to and studying photographs and protect it. 2 Resource: This activity has been adapted from “Protected Areas around the Corner” from Protected Areas (1995). Available from Wild BC. www.wildbc.org Taking it home: Go visit the stream or river closest to your house – can you find out its name? References: Blair Whitehead, DG (Ed.). 2002. Protected Areas: preserving our future. 2nd edition. Available from Wild BC http://www.wildbc.org Bouchard, Randy and Dorothy Kennedy. 2007.Aboriginal History of the Squamish Nation. For the Squamish Nation, Squamish. BC District of Squamish. Community Mapping data http://www.squamish.ca Golder Associates. 2007. Report on the Conceptual Management Plan for Site “A” of the Squamish Estuary. For the Squamish Nation, Squamish, BC Staniforth, Sue. 2009. Get Outdoors!: an educators guide to outdoor classrooms in parks, schoolgrounds, and other special places. Available from Wild BC www.wildbc.org 3 Source:GolderAssociates 4 Taking it Home… Name: Did You Know?? Go visit the stream or river closest to your house. What is the name of the river or stream? Local streams and rivers are important habitat for the four most common species of salmon that live in our watershed. These fish have been a traditional source of food for thousands of years to What type of fish do you think live there? local First Nations. Squamish Nation elders recalled that around 1900, the chum salmon were so thick in the Squamish River around Brackendale that it was apparently possible to “cross the water on their backs.”!!! Wow, that is a lot of fish! 5 S QUAMISH RIVERS & ESTUARY Watershed Food Fest Background: Grades: K-7 Today most of our food comes off the Subject, Science, Language farm, often from far outside our own watershed. However, there are many Arts; Social Studies plants and animals that grow, often wild, in our watersheds. Time required:30 minutes re- search; 60 minutes cooking & First Nation peoples make use of these foods to sustain their culture. Plants eating that grow wild naturally are called “native plants.” These plants are Key Concepts: adapted to live in a particular biogeo- climatic zone. Plants that have been Everyday actions make a introduced to an area but then self- difference in watershed and seed are “naturalized” plants. These estuary health. plants can also be “wild” foods of a watershed. Objectives: In British Columbia, we can look at It is expected that the student Materials will: foods that First Nations peoples tradi- Learn about a variety of foods tionally used to gain an understanding Research materials that grow in their watershed of what foods are native to watersheds (native and non-native); in British Columbia. While the tradi- Native Plant foods Appreciate the importance of tional aboriginal diet of the Coastal water and watersheds in lifestyle peoples relied heavily on protein: fish, Local food samples choices; shellfish, and sea mammals, coastal peoples also have extensive knowl- Key Words: edge of native plants, using over 200 Decision-making; sustainability; native species for food, medicine and other plants; First Nations purposes. In the Squamish watershed, the Skills: Squamish First Nation have been har- discussion; research; communication; vesting and eating native foods for well over 4,000 years. They have an expression: “when the tide is out… the table is set.” This refers to how 6 Watershed Food Fest Background continued: diet was replaced by animal fats and oils. important the food fishery is to their Plants that provided edible roots, rhizomes, traditional diet. This continues to be true and bulbs were scarce and often seasonal. today. Sometimes however, these products would be soaked overnight in water to plump them Traditionally, the Squamish First Nation ate up prior to eating. animal foods such as chum and Coho salmon (dried and fresh), herring spawn, Today, we have growing and living in our clams, deer, goat, or other game animals as watersheds a rich diversity of foods. Some the mainstay of their diet. However, greens foods are native plants and animals, while (shoots, stalks, young plants) and other some have been introduced to our vegetable dishes were eaten daily and watersheds from elsewhere. We can learn provided necessary vitamins and minerals. about our local ecosystems and traditional Greens such as roots and bulbs were often customs using foods as a teaching tool. This prepared in steaming pits. Pit ovens can is a powerful way to learn about your retain heat for several hours before cooling watershed. and are very efficient for preparing large quantities of foods. People also prepared Teaching Note: foods such as soups and stews with meat or Please use caution if exploring your fish and vegetable combination using watershed for native plants and be sure baskets and more recently kettles or pots. plants are identified as edible and safe to Drying berries and other fruits was an handle. Some native plants are extremely important way to preserve them for later use. sensitive to disturbance: do not disturb Sometimes berries would be cooked first sensitive sites. and then dried into berry “cakes.” People ate dried berries and berry cakes such as the Procedure: way modern people eat raisins or other dried 1. Explain that today we can eat foods fruit. from around the world. However, in our own watersheds there is an The basic types of food plants gathered and amazing diversity of plant and prepared fall into several categories: fruits animal life. (especially berries), green vegetables 2. Brainstorm with students the names (sprouts, leaves, seaweeds), mushrooms, of plants, animals and foods that underground parts of plants (roots, bulbs, grow or could be harvested from rhizomes) and cambium from certain trees. their community. You could ask One component of the traditional aboriginal them if they have gone to a local diet that was in short supply: carbohydrates. Farmers Market: what did they see or In many areas, due to the lack of food what did their family buy there? sources for carbohydrates, this part of the 3. Make a list of these foods. Be sure to remember seasonal foods and native plants that may be an important local food.
Recommended publications
  • Washington Division of Geology and Earth Resources Open File Report
    l 122 EARTHQUAKES AND SEISMOLOGY - LEGAL ASPECTS OPEN FILE REPORT 92-2 EARTHQUAKES AND Ludwin, R. S.; Malone, S. D.; Crosson, R. EARTHQUAKES AND SEISMOLOGY - LEGAL S.; Qamar, A. I., 1991, Washington SEISMOLOGY - 1946 EVENT ASPECTS eanhquak:es, 1985. Clague, J. J., 1989, Research on eanh- Ludwin, R. S.; Qamar, A. I., 1991, Reeval­ Perkins, J. B.; Moy, Kenneth, 1989, Llabil­ quak:e-induced ground failures in south­ uation of the 19th century Washington ity of local government for earthquake western British Columbia [abstract). and Oregon eanhquake catalog using hazards and losses-A guide to the law Evans, S. G., 1989, The 1946 Mount Colo­ original accounts-The moderate sized and its impacts in the States of Califor­ nel Foster rock avalanches and auoci­ earthquake of May l, 1882 [abstract). nia, Alaska, Utah, and Washington; ated displacement wave, Vancouver Is­ Final repon. Maley, Richard, 1986, Strong motion accel­ land, British Columbia. erograph stations in Oregon and Wash­ Hasegawa, H. S.; Rogers, G. C., 1978, EARTHQUAKES AND ington (April 1986). Appendix C Quantification of the magnitude 7.3, SEISMOLOGY - NETWORKS Malone, S. D., 1991, The HAWK seismic British Columbia earthquake of June 23, AND CATALOGS data acquisition and analysis system 1946. [abstract). Berg, J. W., Jr.; Baker, C. D., 1963, Oregon Hodgson, E. A., 1946, British Columbia eanhquak:es, 1841 through 1958 [ab­ Milne, W. G., 1953, Seismological investi­ earthquake, June 23, 1946. gations in British Columbia (abstract). stract). Hodgson, J. H.; Milne, W. G., 1951, Direc­ Chan, W.W., 1988, Network and array anal­ Munro, P. S.; Halliday, R. J.; Shannon, W.
    [Show full text]
  • Squamish Estuary
    OCEAN WATCH | Howe Sound Edition SPECIES AND HABITATS Squamish Estuary AUTHOR Edith B. Tobe, Registered Professional What is happening in Biologist, Squamish River Watershed Society REVIEWER the Squamish Estuary? Gary Williams, M.Sc., R.P.Bio, Professional Wetland Scientist, GL Williams and Associates Ltd. The Squamish Estuary is situated at the head of Howe Sound, one of the southernmost fjords in British Columbia, where the Squamish River drains over 3,650 square kilometers of coastal rainforest into the ocean. An estuary is formed when fresh water mixes with marine waters to create a brackish tidally influenced zone. Estuaries are one of the most productive ecosystems on the planet, providing habitat for fisheries, waterfowl, and wildlife. There have been many anthropomorphic impacts to the Squamish Estuary since it was settled first by First Nations and later by Europeans and other cultures. The impacts have included urbanization, diking and logging and resulted in loss of habitat, changes to hydrology, and introduction of con- tamination. Figure 1. The brownfield site, a former log sort in the central Estuary, is the location of current restoration efforts. (Photo: Colin Bates, June 2015) Squamish Estuary | Page 123 OCEAN WATCH | Howe Sound Edition SPECIES AND HABITATS Organizations such as the Squamish River Water- lish tidal channels, mud flats and sedge marshes on shed Society (SRWS) have been working for close to the site. In 2015, efforts included removal of a large 20 years on re-establishing the estuary to its origin- amount of wood waste, grading the site, and trans- al function by reconnecting tidal channels, installing planting Lyngbye’s sedge (Carex lyngbyei), the dom- culverts, planting aquatic and terrestrial vegetation, inant grassy plant in the estuary and in many Pacific and creating wildlife habitat for aquatic and terrestrial coastal marshes.
    [Show full text]
  • Community Risk Assessment
    COMMUNITY RISK ASSESSMENT Squamish-Lillooet Regional District Abstract This Community Risk Assessment is a component of the SLRD Comprehensive Emergency Management Plan. A Community Risk Assessment is the foundation for any local authority emergency management program. It informs risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflects their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property. SLRD Emergency Program [email protected] Version: 1.0 Published: January, 2021 SLRD Community Risk Assessment SLRD Emergency Management Program Executive Summary This Community Risk Assessment (CRA) is a component of the Squamish-Lillooet Regional District (SLRD) Comprehensive Emergency Management Plan and presents a survey and analysis of known hazards, risks and related community vulnerabilities in the SLRD. The purpose of a CRA is to: • Consider all known hazards that may trigger a risk event and impact communities of the SLRD; • Identify what would trigger a risk event to occur; and • Determine what the potential impact would be if the risk event did occur. The results of the CRA inform risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflect their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property.
    [Show full text]
  • Where the Rivers Meet The
    Natural Hazards in Squamish 1 District of Squamish Where the Rivers Meet the Sea Lessons from the Past HIGHWAY 99 Official Community Plan Adopted 2010 SQUAMISH RIVER The District of Squamish is located at the head of Howe Several conclusions can be drawn from the flood history in VER Schedule D1 YE RI CHEEKE Sound where 5 rivers converge. These mountain rivers, Squamish: FLOOD AND DEBRIS FLOW fed by glaciers, snowmelt and precipitation, descend HAZARD AREAS from their steep mountain tops carrying water, sediment, 1. All the rivers in Squamish pose a risk of flooding. All have Levette Legend Lake and on occasion, rocks and other debris. When these fast Evans Cr B Debris Flow Hazard Area r Brohm Lake o h caused multiple and damaging floods in the past. m Riv Flood Hazard Area !!! e r Dykes flowing rivers reach the gently sloping valley, they tend to Parks and Ecological Reserves Paradise Valley Rd 2. Damaging floods have also occurred as a result of coastal Indian Reserves Boundaries slow down and spread out, and leave sediment behind. Evans hazard zones Lake The terms alluvial fan and floodplain are used to describe inundation. Source: Cheekye River Terrain Hazard and Land Use Study, March 1993 HAZARD ZONES 1. Alluvial fan hazard zone - level 1 (high) the riparian areas along these lower river reaches. 4 2. Alluvial fan hazard zone - level 2 (intermediate) 3. The flood risk in Squamish has strong seasonal variations. Most C 6 H 3 Cat E 3 3. Alluvial fan hazard zone - level 3 (moderate) ER E Lake s Cr IV K Evan R E 5 Y 4.
    [Show full text]
  • Flow Hydraulics, Bedforms and Macroturbulence of Squamish River Estuary, British Columbia
    FLOW HYDRAULICS, BEDFORMS AND MACROTURBULENCE OF SQUAMISH RIVER ESTUARY, BRITISH COLUMBIA C. Scott Babakaiff B.Sc. University of British Columbia 1991 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE in the Department of Geography OC. Scott Babakaiff Simon Fraser University December 1993 All rights reserved. This work may not be reproduced in whole or in part, by photocopy or other means, without permission of the author. APPROVAL Name: Scott Curtis Babakaiff Degree: Master of Science Title of Thesis: Row Hydraulics, Bedforms And Macroturbulence Of Squamish River Estuary, British Columbia Examining Committee: Chair: A.C.B. Roberts, Associate Professor L. Lesack Assistant Professor Mr. K.' Re,HydroloBst Northwest Hydraulics Dr. M.A. Church, Professor Department of Geography University of British Columbia External Examiner Date Approved: December 6.1993 i i PARTIAL COPYRIGHT LICENSE I hereby grant to Simon Fraser University the right to lend my thesis, project or extended essay (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further agree that permission for multiple copying of this work for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying or publication of this work for financial gain shall not be allowed without my written permission. Title of Thesis/Project/Extended Essay Flow Hydraulics, Bedforms And Macroturbulence Of Sauamish River Estuary.
    [Show full text]
  • Squamish/ Mamquam River Survey
    DISTRICT OF SQUAMISH REPORT TO: Council FOR: Regular Meeting of Council PRESENTED: September 18, 2007 FILE: COMDEV SUBJECT: Award of Squamish and Mamquam River Studies Recommendation: THAT Council award the Research and Survey components of the Squamish & Mamquam River Studies to Kerr Wood Leidal and Associates at a price not to exceed $64,872 plus GST; AND FURTHER THAT Council implore the Province to recognize the urgent need for the remainder of the work to be completed, the historical role of the Province in performing this work and request funding for the remainder of the study from Province. CAO Recommendation: THAT the report from Community Development be approved. K. Anema, CAO 1. Purpose: This report is intended to authorize the award the Squamish and Mamquam River Studies. 2. Time Critical: Flood hazard protection is one of Council’s highest priorities. This assignment is intended to undertake the river surveys that are needed to assess the current level of protection afforded by the existing dykes and then determine what, if any, measures are needed to achieve the 200 year standard of protection. 3. Background: The flood of record for the Squamish River occurred in October of 2003. The subsequent analysis of that flood suggested that the existing dykes on the Squamish and Mamquam Rivers may not be providing protection from the provincially accepted, 200 year design storm. Of further concern is aggradation or sediment build-up of the river bed. This may have the effect of further reducing the level of protection afforded by the dykes. In order to determine the current level of protection and thereby establish what, if any, upgrading is necessary a survey of the floodplain must first be undertaken.
    [Show full text]
  • Seismic Hazards of Western Washington and Selected Adjacent Areas­ Bibliography and Index, 1988-1991
    LIBRARY DEPT. OF NATURAL RESOURCES GEOLOGY & EARTH RESOURCES DIVISION OLYMPIA, WA. 98504-7007 SEISMIC HAZARDS OF WESTERN WASHINGTON AND SELECTED ADJACENT AREAS­ BIBLIOGRAPHY AND INDEX, 1988-1991 compiled by Connie J. Manson WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 92-2 Supported l:,y the National Earthquake Hazards Reduction Program through U.S. Geological Survey Agreement no. 14-08-0001-A0509. February 1992 -, WASHINGTON STATE DEPARTMENT OF Natural Resources Brian Boyle - Commissioner of Public Lands Art Stearns - Supervisor Division of Geology and Earth Resources . Raymond Lasmanis, State Geologist SEISMIC HAZARDS OF WESTERN WASHINGTON AND SELECTED ADJACENT AREAS­ BIBLIOGRAPHY AND INDEX, 1988-1991 compiled by Connie J. Manson WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 92-2 Sllpported 1,y tlu! National Earthqll/JU Hazards Reduction Program lhro11gh U.S. Geological SllrVey Agreement no. J4..()8-000J-AOS09. February 1992 l Contents Introduction . 1 Bibliography . 3 Index ............................................. 79 iii Seismic Hazards of Western Washington and Selected Adjacent Areas-Bibliography and Index, 1988-1991 compiled by Connie J. Manson Introduction This work continues the previous seismic hazards bibliography (Manson, 1988). Like that work, this includes all citations pertinent to the study of earthquake hazards in western Washington and the metropolitan Portland, Oregon, area that were received by the Washing­ ton Division of Geology and Earth Resources Library from September 1988 through Septem­ ber 1991. Studies that could shed light on the causes and(or) effects of earthquakes in western Wash­ ington and adjacent areas have been included. Thus, the bibliography emphasizes the seis­ mology, paleoseismology, geophysics, and earthquake-related hazards of the targeted geo­ graphic areas and includes studies of structural geology and tectonics, glacial geology, geochronology, slope stability, soil mechanics, and other pertinent subjects.
    [Show full text]
  • The Mamquam River Floodplain Restoration Project
    Background Information: The Mamquam River Floodplain Restoration Project The Mamquam River Floodplain Restoration project is being undertaken in The partnership with the Squamish River Watershed Society, Fisheries and Oceans Mamquam Canada, District of Squamish, and Squamish Nation. Funding support has been River is received from the Pacific Salmon Commission, B.C. Ministry of Transportation, important Pacific Salmon Foundation, Canadian Hydro Development Corporation. The coho and Squamish River Watershed Society and the local community are working closely Chinook to provide future working plans for conservation of these important floodplain salmon lands. habitat. 2005 The Mamquam River is an important coho, pink, chum and Chinook salmon producing tributary within the Squamish River watershed. The Squamish River estuary, lying at the head of Howe Sound, was formed at the confluences of the Mamquam and Squamish Rivers and historically supported a large complex wetland with interconnected tidally influenced sloughs and channels. These diverse habitats provided exceptional quality habitat for many salmonid species particularly coho, pink, chum and Chinook salmon. Dyking in the early twentieth century confined the Mamquam River and Squamish Rivers to relatively narrow corridors isolated from most of their historic floodplain The building lands. Internal drainages remain in some of the undeveloped portions of these of dykes on isolated floodplain areas but suffer from reduced flows and poor connections to the viable salmon populations in adjacent habitats. One such drainage is Loggers Lane Mamquam & Creek. Loggers Lane Creek was originally a river channel of the Mamquam River Squamish but was isolated following a giant storm in 1921 after which the dyke was built.
    [Show full text]
  • Mamquam River Stranding Sensitivity Mapping and Method for Estimating Fish Stranding
    Mamquam River Stranding Sensitivity Mapping and Method for Estimating Fish Stranding K.L.C. Munn, G.C. Dare, H.D. Klassen Fisheries and Oceans Canada Pacific Region Ecosystem Management Branch 200-401 Burrard Street Vancouver, British Columbia V6C 3S4 2016 Canadian Manuscript Report of Fisheries and Aquatic Sciences 3102 Canadian Manuscript Report of Fisheries and Aquatic Sciences Manuscript reports contain scientific and technical information that contributes to existing knowledge but which deals with national or regional problems. Distribution is restricted to institutions or individuals located in particular regions of Canada. However, no restriction is placed on subject matter, and the series reflects the broad interests and policies of Fisheries and Oceans Canada, namely, fisheries and aquatic sciences. Manuscript reports may be cited as full publications. The correct citation appears above the abstract of each report. Each report is abstracted in the data base Aquatic Sciences and Fisheries Abstracts. Manuscript reports are produced regionally but are numbered nationally. Requests for individual reports will be filled by the issuing establishment listed on the front cover and title page. Numbers 1-900 in this series were issued as Manuscript Reports (Biological Series) of the Biological Board of Canada, and subsequent to 1937 when the name of the Board was changed by Act of Parliament, as Manuscript Reports (Biological Series) of the Fisheries Research Board of Canada. Numbers 1426 - 1550 were issued as Department of Fisheries and Environment, Fisheries and Marine Service Manuscript Reports. The current series name was changed with report number 1551. Rapport manuscrit canadien des sciences halieutiques et aquatiques Les rapports manuscrits contiennent des renseignements scientifiques et techniques qui constituent une contribution aux connaissances actuelles, mais qui traitent de problèmes nationaux ou régionaux.
    [Show full text]
  • Cheakamus River Watershed Action Plan
    CHEAKAMUS RIVER WATERSHED ACTION PLAN FINAL November 14, 2017 Administrative Update July 21, 2020 The Fish & Wildlife Compensation Program is a partnership between BC Hydro, the Province of B.C., Fisheries and Oceans Canada, First Nations and Public Stakeholders to conserve and enhance fish and wildlife impacted by BC Hydro dams. The Fish & Wildlife Compensation Program is conserving and enhancing fish and wildlife impacted by BC Hydro dam construction in this watershed. Top row from left: Cheakamus Dam and powerhouse. Bottom row from left: Squamish River Powerhouse (Credit BC Hydro). Cover photos: Coho fry (Credit iStock) and Roosevelt Elk (Credit iStock). The Fish & Wildlife Compensation Program (FWCP) is a partnership between BC Hydro, the Province of BC, Fisheries and Oceans Canada, First Nations and Public Stakeholders to conserve and enhance fish and wildlife impacted by BC Hydro dams. The FWCP funds projects within its mandate to conserve and enhance fish and wildlife in 14 watersheds that make up its Coastal Region. Learn more about the Fish & Wildlife Compensation Program, projects underway now, and how you can apply for a grant at fwcp.ca. Subscribe to our free email updates and annual newsletter at www.fwcp.ca/subscribe. Contact us anytime at [email protected]. 2 Cheakamus River Action Plan EXECUTIVE SUMMARY: CHEAKAMUS RIVER WATERSHED The Fish & Wildlife Compensation Program is a partnership between BC Hydro, the Province of B.C., Fisheries and Oceans Canada, First Nations and Public Stakeholders to conserve and enhance fish and wildlife impacted by BC Hydro dams. This Action Plan builds on the Fish & Wildlife Compensation Program’s (FWCP’s) strategic objectives, and is an update to the previous FWCP Watershed and Action Plans.
    [Show full text]
  • “Salmon on the Rough Edge of Canada and Beyond”
    “Salmon on the Rough Edge of Canada and Beyond” A Squamish Thanksgiving By Matt Foy Located in south-western British Columbia, Canada, the Squamish River is a large glacial fed watershed. The brawling mountain river, with its major tributaries such as the Elaho, Cheakamus, Ashlu, and Mamquam Rivers drains from the rugged terrain of the BC Coast mountains into the head of Howe Sound, part of the Salish Sea. Once known for its prolific runs of pink salmon these runs were decimated during the late- twentieth century. This is a story about their remarkable recovery and some of the people who worked hard to see pink salmon return to this beautiful mountain domain. As summer slid into fall, the phenomenal pink salmon run to the Squamish River was just winding down. The run of 2013 had exceeded all expectations, and such an abundance of pink salmon had not been observed in over fifty years, since the memorable return of 1963. For many people, the 2013 return would seem to have come out of nowhere but many other people understood the hard work and dedication that had led to this remarkable recovery. In that season of giving thanks, it seems fitting to reflect back on the path that has led from the last great run of 1963 to the years when pink salmon were almost absent from the Squamish River watershed, to the fall of 2013, one of great abundance to be celebrated and remembered. Upper Howe Sound, Squamish, BC, Canada Photo: Courtesy Ruth Hartnup Boom and Bust The growth decades of the 1950’s through the 1970’s were not kind to pink salmon populations around the Strait of Georgia.
    [Show full text]
  • Influence of a Large Debris Flow Fan on the Late Holocene Evolution of Squamish River, Southwest British Columbia, Canada
    Canadian Journal of Earth Sciences Influence of a large debris flow fan on the late Holocene evolution of Squamish River, southwest British Columbia, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2017-0150.R2 Manuscript Type: Article Date Submitted by the Author: 02-Jan-2018 Complete List of Authors: Fath, Jared; University of Alberta, Renewable Resources Clague, John J.; Dept of Earth Sciences, Friele, Pierre;Draft Cordilleran Geoscience Is the invited manuscript for consideration in a Special N/A Issue? : Quaternary geology, Alluvial fans, Fan-impounded lakes, Squamish River, Keyword: Cheekye Fan https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 48 Canadian Journal of Earth Sciences 1 Influence of a large debris flow fan on the late Holocene evolution of Squamish River, southwest British Columbia, Canada 1 2 3 4 Jared Fatha,c *, [email protected] Draft 5 John J. Claguea,*, [email protected] 6 Pierre Frieleb, [email protected] 7 8 a Department of Earth Sciences, Simon Fraser University, 8888 University Drive, Burnaby, 9 BC, V5A 1S6 10 b Cordilleran Geoscience, PO Box 612, Squamish, BC, V0N 3G0 11 c Presently at Department of Renewable Resources, University of Alberta, Edmonton 12 *Corresponding author 13 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 48 2 1 Abstract 2 Cheekye Fan is a large paraglacial debris flow fan in southwest British Columbia. It owes its 3 origin to the collapse of Mount Garibaldi, a volcano that erupted in contact with glacier ice 4 near the end of the Pleistocene Epoch. The fan extended across Howe Sound, isolating a 5 freshwater lake upstream of the fan from a fjord downstream of it.
    [Show full text]