Matches in DBpedia 2016-04 for { ?s ?p "Little Manitou Lake is a small saltwater lake about 100 kilometres south-east of Saskatoon, Canada. The lake was formed by receding glaciers during the most recent ice age. It is fed by underground springs, and has a mineral content high in sodium, magnesium and potassium salts due to it being a terminal lake. The salt content of the water (180 g/L) gives it a density about half of that of the Dead Sea (300-400 ppt), allowing bathers to float easily."@en }
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- Little_Manitou_Lake_(Saskatchewan) abstract "Little Manitou Lake is a small saltwater lake about 100 kilometres south-east of Saskatoon, Canada. The lake was formed by receding glaciers during the most recent ice age. It is fed by underground springs, and has a mineral content high in sodium, magnesium and potassium salts due to it being a terminal lake. The salt content of the water (180 g/L) gives it a density about half of that of the Dead Sea (300-400 ppt), allowing bathers to float easily.".
- Q6650824 abstract "Little Manitou Lake is a small saltwater lake about 100 kilometres south-east of Saskatoon, Canada. The lake was formed by receding glaciers during the most recent ice age. It is fed by underground springs, and has a mineral content high in sodium, magnesium and potassium salts due to it being a terminal lake. The salt content of the water (180 g/L) gives it a density about half of that of the Dead Sea (300-400 ppt), allowing bathers to float easily.".
- Little_Manitou_Lake_(Saskatchewan) comment "Little Manitou Lake is a small saltwater lake about 100 kilometres south-east of Saskatoon, Canada. The lake was formed by receding glaciers during the most recent ice age. It is fed by underground springs, and has a mineral content high in sodium, magnesium and potassium salts due to it being a terminal lake. The salt content of the water (180 g/L) gives it a density about half of that of the Dead Sea (300-400 ppt), allowing bathers to float easily.".
- Q6650824 comment "Little Manitou Lake is a small saltwater lake about 100 kilometres south-east of Saskatoon, Canada. The lake was formed by receding glaciers during the most recent ice age. It is fed by underground springs, and has a mineral content high in sodium, magnesium and potassium salts due to it being a terminal lake. The salt content of the water (180 g/L) gives it a density about half of that of the Dead Sea (300-400 ppt), allowing bathers to float easily.".