Saskatchewan River

Some of you in this room remember that time as children.

The dam is located about 145 kilometers southeast of Opasquiak on the banks of the Saskatchewan River.

The judge heard decades worth of research from academics, researchers, land-based educators and history from its own members.

We negotiate on your behalf.

Cul-de-sac River is its own river and it dumps into Carrot River.

And Carrot River is its own river that dumps into Saskatchewan River.

And Saskatchewan River goes through the Paw.

And then dumps into the north basin of Cedar Lake.

And then Cedar Lake dumps into Lake Winnipeg.

It is.

You can also get sturgeon.

in the Saskatchewan river.

The Algonquin tribes, as we have seen, roamed far to the west.

One branch frequented the upper Saskatchewan River.

Here the ashes of the prairie fires discoloured their moccasins and turned them black, and in consequences they were called the Blackfeet Indian.

Even when they moved to other parts of the country the name was still applied to them.

Above rise alternating slopes covered with perpetual snow and hanging glaciers, the white-blue ice of which is splintered by deep rents and dark yawning crevasses.

This mountain forms part of the continental watershed, for on the other side the melting snows finally reach the Pacific Ocean, while on the near side the snows swept into the valleys by avalanches and melted by the warmer air of lower altitudes find their way at lengths into the Saskatchewan River and Hudson Bay.

There is something wonderfully attractive about this mountain.

The pleasure grows as one continues to gaze at the immense mass.

Approaching a low ridge at the south side of the valley, suddenly there is revealed a magnificent panorama of glaciers, lakes, and mountains, unparalleled among the Canadian Rockies for its combination of grandeur and extent.

To the south, one beholds the end of an immense glacier, at the termination of which there are two great arched caverns in the ice.

From out these issue two roaring glacial streams, the source of the Saskatchewan River, or at least of its longest tributary called the Little Fork.

Lofty mountains hem in this glacier on either side, only revealing a portion of the vast nevé, which may be seen extending southward for six or seven miles.

And it was called Glass of the Sask.

And I'm like, I'm not drinking water from the Saskatchewan River.

What the fuck? Right.

But like, I got a couple of water bottles.

The track was laid, however, to a point about 50 miles west of this, and the grading done generally in an unfinished state for 30 miles further.

This was the condition of things when the contract was entered into to build 500 miles, the east end of the 500-mile contract being at station 4,660, station zero being at Brandon, and extending west to a few miles beyond the Saskatchewan River.

The spring of 1882 opened in the most unpromising manner for railroad operations, being the wettest ever known in that country.

Traffic over the St. Paul, Minneapolis and Manitoba Railroad between St. Paul and Winnipeg was entirely suspended from April 15th to the 28th, owing to the floods on the Red River at St. Vincent and Emerson, a serious blow to an early start, as on this single track depended the transportation of all supplies, men, timber, and contractors' plant, together with all track materials except ties.