Niagara Falls And Bridal Veil Falls

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.

Largely, it is the result of erosion by water at the end of the last glacial period. The most recent glacier over North America, the Laurentide Ice Sheet, resided almost all over Canada. Eventually, the sheet melted, allowing water possessing a strong stream discharge to be released in numerous directions. One of these melt-out pathways formed the Elora Gorge.

Love Canal, a Niagra Falls, New York neighborhood, drew headline attention after newspaper sources revealed that the land had been used to bury excessive amounts of toxic waste, in the form of lye and chlorinated limestone by the landowners, Hooker Chemical Company, in the 1920s.

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.

Snow tends to fall, melt, and fall again quite often. Northern Ontario on the other hand, has a short, dry, and hot summer period. Winter is long, with frigid temperatures in the minus forties. It is not unusual for snow to fall in October and melt June. Southern Ontario is known for its tourist attractions (like Niagara Falls), professional hockey teams, polluted air, and starless sky. Northern Ontario is known for its vast wilderness, professional hockey players (like the Staal brothers), clean air, and star-filled sky. Southern Ontario is a land of opportunity. It is a place where people from all walks of life congregate to experience the wonders of the South and the rush of city life. Northern Ontario is the Land of the Midnight Sun and the Northern Lights. It is the Great White North, a rugged wilderness where one can enjoy and appreciate the peace and tranquility of Mother Nature. There is a division in Ontario that one can count in number, feel in climate, and see in attraction. Southern Ontario is a Mecca of civilization; Northern

The Niagara Escarpment AVA is a relatively new viticulture designated area. The area received the designation in 2005 and is now one of the fastest growing wine regions in New York State. This AVA is comprised of a portion of the Niagara Escarpment landform that runs from New York State through Canada into Wisconsin. (Fig. A) The escarpment has formed over time due to erosion of the rock layers. The top rock layer, dolomitic limestone, is more weather resistant causing it to erode slower and creating the escarpment landform.

Yosemite Falls is a massive waterfall system, the 5th largest in the world, and the tallest waterfall in North America. It is comprised of 3 smaller falls, which are called the Upper Fall, the Middle Cascades, and the Lower Fall. Together, they are 2,425 feet tall which is nearly equivalent to two Empire State Buildings stacked on top of one another. It is estimated that about 2,400 gallons per second flow over the falls during the Spring, which would fill a 300 cubic foot swimming pool in approximately one second. The reason the The reason the waterfall is so high above the valley floor is because the glacier that eroded the valley floor down to where it lays today eroded the surrounding rock much more rapidly than the other rivers and glaciers

Nearly 13,000 years ago, glaciers moved across the earth. In the Pacific Northwest they created many rivers, including the Columbia. The rock that the Grand Coulee Dam was built on was carved out by those glaciers creating a sturdy base of the dam. It is located in the rain-shadow of the Cascade Mountain Range in a shrub-steppe grassland, which results in very little rainfall and high temperatures. There have been many Native American tribes, including the Spokane, Sanpoli, Nespelem, Lakes, Colville and many others that have lived along the Columbia River and have relied on it for many of their day-to-day necessities (Columbia Basin Project 2015).

The Sequoia and Kings Canyon National Parks are two of the most famous national parks in the Sierra Nevada Range. The Sierra Nevada range is located in California along the North American Plate. This range sits to the right of the San Andreas Fault and the Pacific Plate. Some referred to these parks as “The Land of Giants” which turns out to fit them quite well. The parks get this name due to the huge mountains, endless canyons and the world’s largest trees they are home for (“Sequoia and Kings Canyon National Parks,” USA Today). The Sequoia National Park was founded on September 25th, 1890, making it the second oldest park in the United States, and Kings Canyon National Park was established March 4th, 1940. The two parks are adjacent to one another and stretch over approximately 865,964 acres, which a little less than 97% is woods and wilderness. These are large tourist attractions and provide a treasured experience many people value greatly in their lives. The reason it is such a treasured experience to tourists is because of the many special aspects of the park that include the Giant Forest of Sequoias as well as Mount Whitney. Mount Whitney is known for having the highest peak south of Alaska at 14,494 feet above sea level (“Sequoia and Kings Canyon National Parks,” National Geographic).

The present configuration of the Great Lakes basin is the result of the movement of massive glaciers through the mid-continent, a process that began about one million years ago. . . . Studies in the Lake Superior region indicate that a river system and valleys formed by water erosion existed before the Ice Age. The Glaciers undoubtedly scoured these valleys, widening and deepening the and radically changing the drainage of the area (Encyclopedia Britannica )

There are many ways to define Northern Ontario, however, I believe the most accurate geological definition of Northern Ontario was defined by the Ontario Census Division. Northern Ontario encompasses over a large percentage of provincial landmass, stretching from Parry Sound, north to the shores of Hudson Bay, west to the border of Manitoba and east to the border of Quebec (Map Two). Most of Northern Ontario is situated on the Canadian Shield which is characterized by a vast rocky plateau and lakes. In the video “Nine Rivers”, four men on a canoeing trip heading north to Hudson’s Bay, captured the beauty of Northern Ontario. They described the waterways that ranged from small creeks to massive bodies of moving water as an era of great

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.

Quebec is the providence in Canada, covering nearly 600,000 square miles. The notable landmasses found within Quebec include the Canadian Shield and the Appalachian Mountains. The Encyclopedia of Britannica reveals that the Canadian Shield has ice-smoothed hills, and is the most massive area containing exposed Precambrian rock (Behiels). The Appalachian Mountains are the separating feature distinguishing the Quebec’s borders from Main, Vermont, and New Hampshire (“Quebec Mountains”). The St. Lawrence River flows southwest of Lake Ontario to the northeast. Attractions involving the river include the Québec-Lévis ferry, cruises, and strolls on the Promenade Samuel-De Champlain (Quebec).

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.

In the deep valleys of western Montana, USA, one of the largest temporary lakes in the world developed during the Ice Age—glacial Lake Missoula. It was formed by meltwater ponding behind a finger of the Cordilleran Ice Sheet, which extended south into northern Idaho. The lake was about 610 m (2,000 ft) deep near this ice dam, and 305 m (1,000 ft) deep over the current city of Missoula, Montana, after which the lake and flood have been named. It had a volume of about 2,200 cubic kilometres (540 cubic miles), nearly five times the volume of Lake Erie, one of the Great Lakes that straddle the border of the US and Canada. About forty generally evenly-spaced shorelines from this lake can be seen along the nearby foothills (fig. 1). These probably