Hydro Projects: Harmed Environments and Indigenous Peoples
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Chapter 4 – Project Setting
Chapter 4 – Project Setting MINAGO PROJECT i Environmental Impact Statement TABLE OF CONTENTS 4. PROJECT SETTING 4-1 4.1 Project Location 4-1 4.2 Physical Environment 4-2 4.3 Ecological Characterization 4-3 4.4 Social and Cultural Environment 4-5 LIST OF FIGURES Figure 4.1-1 Property Location Map ......................................................................................................... 4-1 Figure 4.4-1 Communities of Interest Surveyed ....................................................................................... 4-6 MINAGO PROJECT ii Environmental Impact Statement VICTORY NICKEL INC. 4. PROJECT SETTING 4.1 Project Location The Minago Nickel Property (Property) is located 485 km north-northwest of Winnipeg, Manitoba, Canada and 225 km south of Thompson, Manitoba on NTS map sheet 63J/3. The property is approximately 100 km north of Grand Rapids off Provincial Highway 6 in Manitoba. Provincial Highway 6 is a paved two-lane highway that serves as a major transportation route to northern Manitoba. The site location is shown in Figure 4.1-1. Source: Wardrop, 2006 Figure 4.1-1 Property Location Map MINAGO PROJECT 4-1 Environmental Impact Statement VICTORY NICKEL INC. 4.2 Physical Environment The Minago Project is located within the Nelson River sub-basin, which drains northeast into the southern end of the Hudson Bay. The Minago River and Hargrave River catchments, surrounding the Minago Project Site to the north, occur within the Nelson River sub-basin. The William River and Oakley Creek catchments at or surrounding the Minago Project Site to the south, occur within the Lake Winnipeg sub-basin, which flows northward into the Nelson River sub-basin. The topography in these watersheds varies between elevation 210 and 300 m.a.s.l. -
2010-2011 Annual Report
First Nations of Northern Manitoba Child and Family Services Authority CONTACT INFORMATION Head Office Box 10460 Opaskwayak, Manitoba R0B 2J0 Telephone: (204) 623-4472 Facsimile: (204) 623-4517 Winnipeg Sub-Office 206-819 Sargent Avenue Winnipeg, Manitoba R3E 0B9 Telephone: (204) 942-1842 Facsimile: (204) 942-1858 Toll Free: 1-866-512-1842 www.northernauthority.ca Thompson Sub-Office and Training Centre 76 Severn Crescent Thompson, Manitoba R8N 1M6 Telephone: (204) 778-3706 Facsimile: (204) 778-3845 7th Annual Report 2010 - 2011 First Nations of Northern Manitoba Child and Family Services Authority—Annual Report 2010-2011 16 First Nations of Northern Manitoba Child and Family Services Authority—Annual Report 2010-2011 FIRST NATION AGENCIES OF NORTHERN MANITOBA ABOUT THE NORTHERN AUTHORITY First Nation leaders negotiated with Canada and Manitoba to overcome delays in implementing the AWASIS AGENCY OF NORTHERN MANITO- Aboriginal Justice Inquiry recommendations for First Nation jurisdiction and control of child welfare. As a result, the First Nations of Northern Manitoba Child and Family Services Authority (Northern BA Authority) was established through the Child and Family Services Authorities Act, proclaimed in November 2003. Cross Lake, Barren Lands, Fox Lake, God’s Lake Narrows, God’s River, Northlands, Oxford House, Sayisi Dene, Shamattawa, Tataskweyak, War Lake & York Factory First Nations Six agencies provide services to 27 First Nation communities and people in the surrounding areas in Northern Manitoba. They are: Awasis Agency of Northern Manitoba, Cree Nation Child and Family Caring Agency, Island Lake First Nations Family Services, Kinosao Sipi Minosowin Agency, CREE NATION CHILD AND FAMILY CARING Nisichawayasihk Cree Nation FCWC and Opaskwayak Cree Nation Child and Family Services. -
Appendix 1 What We Heard from Policy Communities
Appendix 1 What we heard from policy communities Background In the Terms of Reference issued by the Minister of Conservation on September 1 2011, the Clean Environment Commission was asked to “hear evidence from Manitobans regarding the impacts of Lake Winnipeg regulation since the project was put into commercial use by Manitoba Hydro on August 1, 1976.” Over the period of approximately one month (January 12, 2015 to February 18, 2015), the Clean Environment Commission (CEC) attended 17 communities surrounding Lake Winnipeg.1 They also held two evening public sessions in Winnipeg and received a number of written submissions from the public.2 The CEC heard from many residents and users around the Lake including: cottage owners, permanent residents, Indigenous people, agricultural farmers, commercial and subsistence fishermen, and people and organizations from the tourism and recreation industry. There is disagreement in terms of the implications of Lake Winnipeg Regulation on Lake Winnipeg. Manitoba Hydro argues that its effects are generally either positive, benign or insignificant. Others take the position that LWR in conjunction with other Hydro activities has adverse and ongoing effect on the Lake. Among the prominent concerns are: • Lack of confidence in Manitoba Hydro, the Province and the CEC Hearing process on LWR • Lack of transparency of Manitoba Hydro and Manitoba Government operations of LWR • Lack of meaningful ongoing engagement • Sense of exclusion by upstream, downstream and Indigenous people • A sense that Manitoba hydro -
Directory – Indigenous Organizations in Manitoba
Indigenous Organizations in Manitoba A directory of groups and programs organized by or for First Nations, Inuit and Metis people Community Development Corporation Manual I 1 INDIGENOUS ORGANIZATIONS IN MANITOBA A Directory of Groups and Programs Organized by or for First Nations, Inuit and Metis People Compiled, edited and printed by Indigenous Inclusion Directorate Manitoba Education and Training and Indigenous Relations Manitoba Indigenous and Municipal Relations ________________________________________________________________ INTRODUCTION The directory of Indigenous organizations is designed as a useful reference and resource book to help people locate appropriate organizations and services. The directory also serves as a means of improving communications among people. The idea for the directory arose from the desire to make information about Indigenous organizations more available to the public. This directory was first published in 1975 and has grown from 16 pages in the first edition to more than 100 pages in the current edition. The directory reflects the vitality and diversity of Indigenous cultural traditions, organizations, and enterprises. The editorial committee has made every effort to present accurate and up-to-date listings, with fax numbers, email addresses and websites included whenever possible. If you see any errors or omissions, or if you have updated information on any of the programs and services included in this directory, please call, fax or write to the Indigenous Relations, using the contact information on the -
Petition to List US Populations of Lake Sturgeon (Acipenser Fulvescens)
Petition to List U.S. Populations of Lake Sturgeon (Acipenser fulvescens) as Endangered or Threatened under the Endangered Species Act May 14, 2018 NOTICE OF PETITION Submitted to U.S. Fish and Wildlife Service on May 14, 2018: Gary Frazer, USFWS Assistant Director, [email protected] Charles Traxler, Assistant Regional Director, Region 3, [email protected] Georgia Parham, Endangered Species, Region 3, [email protected] Mike Oetker, Deputy Regional Director, Region 4, [email protected] Allan Brown, Assistant Regional Director, Region 4, [email protected] Wendi Weber, Regional Director, Region 5, [email protected] Deborah Rocque, Deputy Regional Director, Region 5, [email protected] Noreen Walsh, Regional Director, Region 6, [email protected] Matt Hogan, Deputy Regional Director, Region 6, [email protected] Petitioner Center for Biological Diversity formally requests that the U.S. Fish and Wildlife Service (“USFWS”) list the lake sturgeon (Acipenser fulvescens) in the United States as a threatened species under the federal Endangered Species Act (“ESA”), 16 U.S.C. §§1531-1544. Alternatively, the Center requests that the USFWS define and list distinct population segments of lake sturgeon in the U.S. as threatened or endangered. Lake sturgeon populations in Minnesota, Lake Superior, Missouri River, Ohio River, Arkansas-White River and lower Mississippi River may warrant endangered status. Lake sturgeon populations in Lake Michigan and the upper Mississippi River basin may warrant threatened status. Lake sturgeon in the central and eastern Great Lakes (Lake Huron, Lake Erie, Lake Ontario and the St. Lawrence River basin) seem to be part of a larger population that is more widespread. -
Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a Foundation in Northern Manitoba
Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba Karla Zubrycki Dimple Roy Hisham Osman Kimberly Lewtas Geoffrey Gunn Richard Grosshans © 2014 The International Institute for Sustainable Development © 2016 International Institute for Sustainable Development | IISD.org November 2016 Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba © 2016 International Institute for Sustainable Development Published by the International Institute for Sustainable Development International Institute for Sustainable Development The International Institute for Sustainable Development (IISD) is one Head Office of the world’s leading centres of research and innovation. The Institute provides practical solutions to the growing challenges and opportunities of 111 Lombard Avenue, Suite 325 integrating environmental and social priorities with economic development. Winnipeg, Manitoba We report on international negotiations and share knowledge gained Canada R3B 0T4 through collaborative projects, resulting in more rigorous research, stronger global networks, and better engagement among researchers, citizens, Tel: +1 (204) 958-7700 businesses and policy-makers. Website: www.iisd.org Twitter: @IISD_news IISD is registered as a charitable organization in Canada and has 501(c)(3) status in the United States. IISD receives core operating support from the Government of Canada, provided through the International Development Research Centre (IDRC) and from the Province -
Sub-‐Agreement Holders – Community List
Sub-Agreement Holders – Community List Sub-Agreement Holders Abbr. Address E&T Coordinator Phone # Fax # Garden Hill First Nation GHFN Island Lake, MB R0B 0T0 Elsie Monias 204-456-2085 204-456-9315 Keewatin Tribal Council KTC 23 Nickel Rd, Thompson, MB R8N 0Y4 Aggie Weenusk 204-677-0399 204-677-0257 Manto Sipi Cree Nation MSCN God's River, MB R0B 0N0 Bradley Ross 204-366-2011 204-366-2282 Marcel Colomb First Nation MCFN Lynn Lake, MB R0B 0W0 Noreena Dumas 204-356-2439 204-356-2330 Mathias Colomb Cree Nation MCCN Pukatawagon, MB R0B 1G0 Flora Bighetty 204-533-2244 204-553-2029 Misipawistik Cree Nation MCN'G Box 500 Grand Rapids, MB R0C 1E0 Melina Ferland 204-639- 204-639-2503 2491/2535 Mosakahiken Cree Nation MCN'M Moose Lake, MB R0B 0Y0 Georgina Sanderson 204-678-2169 204-678-2210 Norway House Cree Nation NHCN Norway House, MB R0B 1B0 Tony Scribe 204-359-6296 204-359-6262 Opaskwayak Cree Nation OCN Box 10880 The Pas, MB R0B 2J0 Joshua Brown 204-627-7181 204-623-5316 Pimicikamak Cree Nation PCN Cross Lake, MB R0B 0J0 Christopher Ross 204-676-2218 204-676-2117 Red Sucker Lake First Nation RSLFN Red Sucker Lake, MB R0B 1H0 Hilda Harper 204-469-5042 204-469-5966 Sapotaweyak Cree Nation SCN Pelican Rapids, MB R0B 1L0 Clayton Audy 204-587-2012 204-587-2072 Shamattawa First Nation SFN Shamattawa, MB R0B 1K0 Jemima Anderson 204-565-2041 204-565-2606 St. Theresa Point First Nation STPFN St. Theresa Point, MB R0B 1J0 Curtis McDougall 204-462-2106 204-462-2646 Tataskweyak Cree Nation TCN Split Lake, MB R0B 1P0 Yvonne Wastasecoot 204-342-2951 204-342-2664 -
Weekly Update #7 – February 21, 2020
Water Level & Flow Update for the Lower Nelson River Weekly Update # 7 February 21, 2020 Lower Nelson River (Split Lake to Hudson Bay) Water up and impoundment has not started at Keeyask (planned to begin in February). Flows on the Nelson River are high as heavy Fall rainfall in the southern parts of the watershed flows north on its way to Hudson Bay - this will continue all winter. Hydro system flows to Split Lake and the Lower Nelson River come from 2 sources – Lake Winnipeg (LW) outflows through Kelsey generating station (at 3115 cms or 110,000 cfs) and Churchill River Diversion (CRD), through Notigi control structure (960 cms or 33,900 cfs)-see map. These combined flows (of 4,075 cms or 143,900 cfs) have been relatively constant since early December. The Nelson’s flow downstream of Keeyask is 4,480 cms ( or 158,200 cfs) (measured at As of February 19, Lower Nelson River lake and Limestone GS). forebay levels are: • Split Lake 168.35 m (or 552.3 ft) Nelson River flow depends on Lake Winnipeg Water level: • Clark Lake 167.94 m (or 551.0 ft ) Lake Winnipeg outflows are largely controlled by the • Gull Lake 156.17 m (or 512.4 ft ) Jenpeg Generating Station (upstream of Kelsey Jenpeg• Stephens Lake 139.76 m (or 458.5 ft) Generating Station). These flows are maximized every • Long Spruce forebay 110.90 m (or 361.2 ft ) winter to allow as much water as possible to flow out of • Limestone forebay 85.07 m (or 279.1 ft) Lake Winnipeg to fuel generating stations on the Nelson River to meet heating demands by Manitobans. -
Convergent Margin Magmatism in the Central Andes and Its Near Antipodes in Western Indonesia: Spatiotemporal and Geochemical Considerations
AN ABSTRACT OF THE DISSERTATION OF Morgan J. Salisbury for the degree of Doctor of Philosophy in Geology presented on June 3, 2011. Title: Convergent Margin Magmatism in the Central Andes and its Near Antipodes in Western Indonesia: Spatiotemporal and Geochemical Considerations Abstract approved: ________________________________________________________________________ Adam J.R. Kent This dissertation combines volcanological research of three convergent continental margins. Chapters 1 and 5 are general introductions and conclusions, respectively. Chapter 2 examines the spatiotemporal development of the Altiplano-Puna volcanic complex in the Lípez region of southwest Bolivia, a locus of a major Neogene ignimbrite flare- up, yet the least studied portion of the Altiplano-Puna volcanic complex of the Central Andes. New mapping and laser-fusion 40Ar/39Ar dating of sanidine and biotite from 56 locations, coupled with paleomagnetic data, refine the timing and volumes of ignimbrite emplacement in Bolivia and northern Chile to reveal that monotonous intermediate volcanism was prodigious and episodic throughout the complex. 40Ar/39Ar age determinations of 13 ignimbrites from northern Chile previously dated by the K-Ar method improve the overall temporal resolution of Altiplano-Puna volcanic complex development. Together with new and updated volume estimates, the new age determinations demonstrate a distinct onset of Altiplano-Puna volcanic complex ignimbrite volcanism with modest output rates beginning ~11 Ma, an episodic middle phase with the highest eruption rates between 8 and 3 Ma, followed by a general decline in volcanic output. The cyclic nature of individual caldera complexes and the spatiotemporal pattern of the volcanic field as a whole are consistent with both incremental construction of plutons as well as a composite Cordilleran batholith. -
A Freshwater Classification of the Mackenzie River Basin
A Freshwater Classification of the Mackenzie River Basin Mike Palmer, Jonathan Higgins and Evelyn Gah Abstract The NWT Protected Areas Strategy (NWT-PAS) aims to protect special natural and cultural areas and core representative areas within each ecoregion of the NWT to help protect the NWT’s biodiversity and cultural landscapes. To date the NWT-PAS has focused its efforts primarily on terrestrial biodiversity, and has identified areas, which capture only limited aspects of freshwater biodiversity and the ecological processes necessary to sustain it. However, freshwater is a critical ecological component and physical force in the NWT. To evaluate to what extent freshwater biodiversity is represented within protected areas, the NWT-PAS Science Team completed a spatially comprehensive freshwater classification to represent broad ecological and environmental patterns. In conservation science, the underlying idea of using ecosystems, often referred to as the coarse-filter, is that by protecting the environmental features and patterns that are representative of a region, most species and natural communities, and the ecological processes that support them, will also be protected. In areas such as the NWT where species data are sparse, the coarse-filter approach is the primary tool for representing biodiversity in regional conservation planning. The classification includes the Mackenzie River Basin and several watersheds in the adjacent Queen Elizabeth drainage basin so as to cover the ecoregions identified in the NWT-PAS Mackenzie Valley Five-Year Action Plan (NWT PAS Secretariat 2003). The approach taken is a simplified version of the hierarchical classification methods outlined by Higgins and others (2005) by using abiotic attributes to characterize the dominant regional environmental patterns that influence freshwater ecosystem characteristics, and their ecological patterns and processes. -
Sediment Records of the Influence of River Damming on the Dynamics Of
HOL0010.1177/0959683616670465The HoloceneDuboc et al. 670465research-article2016 Research paper The Holocene 2017, Vol. 27(5) 712 –725 Sediment records of the influence of river © The Author(s) 2016 Reprints and permissions: sagepub.co.uk/journalsPermissions.nav damming on the dynamics of the Nelson DOI:https://doi.org/10.1177/0959683616670465 10.1177/0959683616670465 and Churchill Rivers, western Hudson Bay, journals.sagepub.com/home/hol Canada, during the last centuries Quentin Duboc,1,2 Guillaume St-Onge1,2 and Patrick Lajeunesse3 Abstract Two gravity cores (778 and 780) sampled at the Nelson River mouth and one (776) at the Churchill River mouth in western Hudson Bay, Canada, were analyzed in order to identify the impact of dam construction on hydrology and sedimentary regime of both rivers. Another core (772) was sampled offshore and used as a reference core without a direct river influence. Core chronology was established using 14C and 210Pb measurements. Cores 778 and 780 show greater variability than the others, and the physical, chemical, magnetic, and sedimentological properties measured on these cores reveal the presence of several hyperpycnites, indicating the occurrence of hyperpycnal flows associated with floods of the Nelson River. These hyperpycnal flows were probably caused by ice-jam formation, which can increase both the flow and the sediment concentration following the breaching of such natural dams. However, these hyperpycnites are only observed in the lower parts of cores 778 and 780. It was not possible to establish a precise chronology because of the remobilization of sediments by the floods. Nevertheless, some modern 14C ages suggest that this change in sedimentary regime is recent and could be concurrent with the dam construction on the Nelson River, which allows a continuous control of its flow since the 1960s. -
Lake Agassiz: a Chapter in Glacial Geology
Journal of the Minnesota Academy of Science Volume 2 Number 4 Article 5 1883 Lake Agassiz: A Chapter in Glacial Geology Warren Upham Follow this and additional works at: https://digitalcommons.morris.umn.edu/jmas Part of the Geology Commons, and the Glaciology Commons Recommended Citation Upham, W. (1883). Lake Agassiz: A Chapter in Glacial Geology. Journal of the Minnesota Academy of Science, Vol. 2 No.4, 290-314. Retrieved from https://digitalcommons.morris.umn.edu/jmas/vol2/iss4/5 This Article is brought to you for free and open access by the Journals at University of Minnesota Morris Digital Well. It has been accepted for inclusion in Journal of the Minnesota Academy of Science by an authorized editor of University of Minnesota Morris Digital Well. For more information, please contact [email protected]. LAK;E AGASSIZ : A . CHAPTER IN GLACIAL GEOLOGY. BY WARREN tTPIUM• • In tha last ol the geological ages a "'lery cold climate cov~ (!red the north part of our continent wfth ice. Every year the snowfall was greater than could be melted away in sum mer; and its depth gradually increased till its lower portion Was changed to compact ice by the pressure of its weight. This pressure also caused the "'last sheet of ice to moYe slowly outward. from the region of its greatest thickness toward its margin. Our reasons for believing that there has been such a wonderful glacial period, are abundant and must convince anyone who gi"'les attention to them. The surfaces of the bed-rock at the quarries in this city, on Nicollet island and beside the Mississippi farther east, bear fine scratches and markings, called stn:m, like those which are found beneath the glaciers of the Alps.