Abstract

Floodwaters from the Assiniboine River are typically diverted to Lake Manitoba and then Lake St. Martin to save the City of Winnipeg and Portage la Prairie from flooding. The four Indigenous communities living Lake St. Martin basin experienced many negative impacts, including long-term displacement after the 2011 flood. Data analysis of historical water levels of Lake Manitoba and Lake St. Martin were conducted to understand the impact of control structures and water levels. Satellite imagery allowed geographic information system (GIS) raster analysis of the shoreline change of Lake St. Martin before and after the 2011 super flood. From 1986 to 2010, the Lake St. Martin area increased slightly by approximately 0.63% but in 2011 the lake area increased by 13%. 11,000 acres were lost mainly around Lake St. Martin First Nation (LSMFN) reserve and the Little Saskatchewan First Nation, as a result and many houses and other buildings (churches, band offices, etc.) flooded in these communities. The shoreline change analysis showed that, in particular, the west and north shoreline of Lake St. Martin lost its beaches and lakefront properties, to become swampland after the 2011 flood. Thousands of Indigenous people were displaced for eight years, as the community could only start to rebuild its infrastructure and houses on higher ground after a government settlement was reached.

Highlights

  • Floods are forces of nature, which humans are powerless to stop, floodwaters can be diverted (Thompson, 2015)

  • The 2011 flood in Manitoba was nicknamed the “super flood”, due to the extremely high water levels on the Assiniboine River leading to high levels in Lake Manitoba and Lake St

  • The historical water levels flowing to Lake Manitoba and Lake St

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Summary

Introduction

Floods are forces of nature, which humans are powerless to stop, floodwaters can be diverted (Thompson, 2015). Upstream dams and water control structures create further vulnerabilities as evident from the higher number of displaced Indigenous communities than settler communities (Ballard & Thompson, 2013; Thompson, Ballard, & Martin, 2014). This water diversion resulted in the long term evacuation of entire communities, including Lake St. Martin First Nation (LSMFN), Little Saskatchewan First Nation and Dauphin River First Nation (Manitoba Infrastructure, 2018). The 2011 flood in Manitoba was nicknamed the “super flood”, due to the extremely high water levels on the Assiniboine River leading to high levels in Lake Manitoba and Lake St. Martin, causing long-term negative impacts.

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