The Saskatchewan River Watershed Flows

Wikapedia.org says that The lake is shared by the province of Ontario to the north in Canada, the states of Minnesota to the west, Wisconsin and Michigan to the south in the United States. It is generally considered the largest freshwater lake in the world by surface area. It is the world's third-largest freshwater lake by volume and the largest by volume in North America.

The Mississippi River is one of the world’s major river systems not only in size, but in habitat diversity as well. It is the third longest river in North America. It flows 2,350 miles from its source at Lake Itasca through the center of the United States to the Gulf of Mexico.

This photo was taken more than 100 years later and quite a bit further upstream, just south-east of St. Clair and Spadina. There, the brook runs through the Nordheimer Ravine, named after the family who used to own the land. Samuel Nordheimer made his fortune importing pianos and then married Edith Boulton of the super-crazy-important Boultons: one of the first families to move here when the city was founded, they were leaders of the Family Compact and the people who built the Grange. In the 1870s, the newlywed Nordheimers built a mansion on the hill overlooking the ravine and damned the brook at this spot to create a little pond and waterfall.

Running water moves sediment in the processes of erosion and deposition, causing different types of landforms. As you can tell in the picture above, Michigan’s topography plays a huge role on where the faster and slower flowing rivers are located and the transportation of the materials in the water depends on the speed of the rivers. Erosion is the breaking down of those materials by the agent, water. The water can erode the channel laterally and vertically, in the end, making the channel wider and deeper. There are different types of erosion: hydraulic action, corrasion, corrosion, cavitation, and attrition. Hydraulic action (above on the right) takes place at rapids and waterfalls because the force of the water removes rock particles from the bed and banks of the river. A great example of this in Michigan is Canyon Falls on the Sturgeon River. At the waterfall, the water is rushing at a high velocity, especially in the spring, causing rock particles to move downstream, creating a wider and deeper river. Eventually the rivers velocity begins to decrease and particles start to deposit. This could also occur because lack of precipitation or an increase in evaporation. The deposition of materials at different locations of the river that they began changes the shape of the river, and effects Michigan as a whole in the end. The particles can travel all the way to the mouth of the river, in this case, Lake Superior, causing

The Wabigoon – English River in Ontario has been contaminated with mercury for about 40 years now and the government has not approached this issue that affects most of the people of Grassy Narrows First Nation. A majority of the community has mercury poisoning, which could be fatal. Additionally, residents are forced to continue to consume contaminated food. In the 1970s, the government let the river to naturally recover itself and said that it would be better than any attempts to clean it, however, it has only gotten worse. Now, the government says that they do not want to attempt to clean the water until they are completely sure that it will not make the situation worse. Recently, scientists have suggested several solutions that have been successful in the past, but it is still unknown as to when the government will clean the water.

The Red Deer River is a major tributary of the South Saskatchewan. Lake Diefenbaker is Saskatchewan was created as a reservoir when the Gardiner and Qu’Appelle dams were created to slow the river flow. Those dams create 19% of the power generated by SaskPower. While the river flows north through Saskatoon it will join up with the North Saskatchewan River creating the Saskatchewan River. It joins at the Saskatchewan River Forks.

The San Luis Rey River Watershed in southern California encompasses 562 square miles of land and is the third largest watershed in the San Diego region. San Luis Rey river is a small tidal wetland where fresh river water meets the coastal salt water. The San Luis Rey River Watershed is located in northern San Diego Country and is bordered to the north by the Santa Margarita River Water and to the south by the Carlsbad and San Dieguito River Watersheds. Major water bodies in the watershed is Lake Henshaw and the San Luis Rey River.

Ontario's many lakes, rivers, and streams played a central role in the province's history and development. For Aboriginal peoples and the early European settlers, the lakes and rivers were a means of transportation and a source of food. Waterways determined the patterns of settlement as well as the patterns of industrialization. More than 80% of Ontarians get their drinking water from the lakes. The Great Lakes and St. Lawrence River Basin supports nearly more than 75% of Canada’s manufacturing, and a third of the country's employment in agriculture and food processing.

A separate tributary of Buffalo Creek, known as Stony Run, lies upstream from Conley Run. Since it is located in a dense wooded area with little to no agricultural interference, Stony Run has experienced very little degradation in comparison to Conley Run. However, Stony Run also shares a number of similar physical characteristics with Conley Run, such as discharge, watershed area, elevation and slope. Therefore, it will serve as a reference stream for this study.

There is a great deal of interest to determine the current state and temporal/spatial variations of the water quality of the Athabasca River, particularly below Fort McMurray. Such an understanding of Athabasca River water quality (particularly dissolved oxygen, DO) is crucial due to its broad range of influences, for example, on aquatic ecosystem and neighboring communities. Canadian Council of Resource and Environment Ministers CCREM (1987) suggested a DO guideline of 6.5 mg/L or greater for the protection of adult

Croix, Herbert and Kennetcook Rivers in the Minas Basin, and the Salmon River in Truro.

The Howe Sound to Whistler region has further been shaped by both fluvial and mass wastage processes. There are many river systems in this area that have been created to shed the water from this U-shaped valley. These river systems are in various stages of age ranging from youth to maturity. There are also man made drainage systems to allow water to flow from areas where rivers haven't formed down to the water's edge. With Howe Sound being a U shaped valley, this area is prone to rockslides and landslides.

The Au Gres River drains approximately 245 square miles. The river starts in Ogemaw County and flows south to its discharge into Lake Huron, similar to the Rifle River. The upper sections of the river flows through forested land; and agricultural land becomes more apparent as you reach Iosco County.

The Genesee River and its watershed is a major tributary to Lake Ontario. The river originates in the Allegheny Plateau in the town of Ulysses, Potter County, Pennsylvania, about fifteen miles south of the New York State border (GFLRPC, 2004). The river flows north through Allegheny, Livingston, and Monroe Counties and forming a portion of two borders between Livingston County and Wyoming or Monroe Counties. Letchworth State Park runs along the Genesee River encapsulating 14,350 acres of the watershed and contains the “Grand Canyon of the East” a gorge 550 feet deep and six miles long.

Landscape description: The Cedar River Watershed covers 90,638 acres and is owned by the City of Seattle (seattle.gov). It is mainly managed to support and provide clean drinking water to 1.4 million people in the Seattle area (seattle.gov). The watershed is generally divided into the lower region and the upper region (see maps 2 and 3) (seattle.gov).