BLOODVEIN RIVER a Canadian Heritage River Ten-Year Monitoring Report: 2008 – 2018
BLOODVEIN RIVER A Canadian Heritage River Ten-year Monitoring Report: 2008 – 2018 Prepared by Manitoba Conservation and Climate Parks and Protected Spaces Branch with Ontario Parks, The Ministry of the Environment, Conservation and Parks for The Canadian Heritage Rivers System June 2020 Acknowledgements This report was prepared with contributions from numerous individuals and organizations including but not limited to: • Yan Cong and Myra Ramos, Travel Manitoba • Suyoko Tsukamoto, Manitoba Sport, Culture and Heritage Historic Resources Branch • Sung Joon Kim, Mark Lee, and Tara Wiess, Manitoba Sustainable Development Water Science & Watershed Management Section • Daniel Rheault, Manitoba Sustainable Development Water Quality Management Section • Bloodvein River, Little Grand Rapids, Pikangikum and Lac Seul First Nations, who conducted a review of this report and/or collaborated on past research projects that contributed to information included in this report • The Pimachiowin Aki Corporation • The Manitoba Métis Federation • Jill Taylor-Hollings, Department of Anthropology, Lakehead University. EXECUTIVE SUMMARY The Bloodvein River is part of a network of rivers and lakes across northern Manitoba and Ontario, which were created by glaciers scouring the earth as they receded over 11,000 years ago. Indigenous Peoples have been living along the river corridor for thousands of years and today it flows through the Anishinaabe traditional territories of Lac Seul, Pikangikum, Little Grand Rapids, and Bloodvein River First Nations. On the basis of its strong natural and human heritage values, the western (Manitoba) portion of the Bloodvein was nominated to the Canadian Heritage Rivers System (CHRS) in 1984 and the eastern (Ontario) portion nominated in 1986. The CHRS requires that a detailed monitoring report be prepared every 10 years from designation to confirm that Bloodvein River : A Canadian Heritage River | i Table of Contents Acknowledgements ......................................................
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