LOCATION The Hudson plains are in parts of Ontario and Manitoba. Their area is about 350 000 km squared. The west edge of the Hudson Plains is around Churchill in north Manitoba, the eastern edge is around Fort Rupert, the northern edge borders Hudson Bay and James Bay and the southern edge is near Kapuskasing, Manitoba. Moosonee and Churchill are major cities in the Hudson Plains area, and lesser known cities include Attawapiskat, Fort George, Eastmain, Fort Albany, Lake River, Winisk, Fort Severn, and Shamattawa. VEGETATION Vegetation in the Hudson Plains mostly follows latitude patterns, because of the flat nature of the land. The Hudson Plains are a merge of boreal forest and tundra. Trees are few and far between, denser in the southern, wetter area of the ecozone. In this wetter area, the variety of plants includes: tussocks of sedge, cottongrass, sphagnum moss, dwarf birch, willow shrubs, white spruce, black spruce, larch, balsam, poplar, tamarack, and Jack Pine. In the drier area, vegetation is shrubby and low-lying. It includes Lapland rosebay, crowberry, blueberry, cloudberry, reindeer moss, caribou lichen, and herbs such as arctic aven, purple saxifrage, prickly saxifrage, and lousewort. LANDFORMS The average elevation in the Hudson Plains is 120m above sea level. It is a flat lowland area. The land is made up of mineral soils, with few outcrops of underlying sandstone and shale. This land was created when the weight of glaciers depressed the Hudson Bay region and the ocean waters flooded areas up to 300 km inland from the current coastline. Then, during the retreat of the huge continental ice sheets, drainage into the Hudson Bay was blocked and lakes (Agassiz and Ojibway for example) were formed along th... ... middle of paper ... ...-ums are also common. Species of fish in streams and lakes in the Hudson Plains include northern pike, walleye, and brook trout. SUMMARY STATEMENT The Hudson Plains ecozone, in northern Ontario and parts of Manitoba and Quebec, is an area of wetlands. The climate is generally cool. The northern part of the ecozone is full of shrubs, but no trees, and areas farther south contain forests. Wet have vegetation such as moss and lichen and also some trees like willow, tamarack and black spruce. More northern, drier locations have vegetation consisting of many shrubs such as crowberry and blueberry. In the summer, the wetlands of the Hudson Plains attract millions of migratory birds, such as snow geese, Canada geese and king eider ducks. Mammals which can be found here include moose and black bear, but small mammals such as muskrats and weasels are more common.
This is a report based on three days of observations and testing in the region known as the Peterborough drumlin field. It will address a variety of regional elements, such as climate, soil, vegetation, hydrology, geomorphology, and geology. A variety of sites located on the Canadian Shield, the zone of thick glacial deposits to the south, and the transition between them will be the focus of the report. It is supplemented with previous research on the region. September 8, 1999, day one of the field study involved an area of largely granite bedrock that is part of the Canadian Shield and is the most northern point of study (see Map 2). September 9, 1999, day two, involved three main areas of study: the Bridgenorth esker (Map 3), Mark S. Burnham Park (Map 4), and the Rice Lake drumlin (Map 6). These sites are in areas of thick glacial deposits. September 10, 1999, day three, involved studying the Warsaw Caves (see Map 5) as a transition zone between Precambrian Shield rock to the north and Paleozoic rock to the south. A general map of the entire study region is provided by Map 1.
Fur trading started between the Europeans along with the Aboriginals when the most valuable beaver pelts was a substituted for metal and clothing goods such as iron knives and axis, copper kettles, blankets and trinkets. The beaver pelts were well desired by the Europeans for the reason that using this fur for headgear provided an elegant way to keep dry. However these pelts were for fashion, as men and women could be instantly noted within the social hierarchy by according to their beaver hats. It was so valuable that the sand on the floor was filtered to save every hair that has fallen off. For the Europeans, captivating advantages of the rich furs from the Indians in the New World was a major factor in generating handsome profits, and there is no other pelt exchanging business enterprise like the Hudson's Bay Company. It is the oldest venture of Canada and it inspired many by its domination in the fur trading industry during its early years. They equipped their own armies, minted its own coins and even issued its own medals. The company had controlled fully one-third of present-day Canadian territory and were thought by many as a kingdom by itself in the fur industry. They had trading posts from the very north Arctic Ocean to Hawaii and as far south as San Francisco. HBC's revenue didn't generate simply from this one way trade in furs to Europe; it also consists of large amounts of European goods to North America. These goods incorporated many other products that local people cannot construct such as gunpowder, bullets, weapons, tobacco, kettles, pots, beads, fishing hooks, needles, scissors, and so much more. The Hudson's Bay Company showed a great measure of success since its formation, but it didn't come without s...
in the Canadian Shield there are many types of living organisms living in it, such as moose, black bears, grizzly bears, wolves, foxes, beavers, minks, martens, wolverines, lynxes, wood buffalo, woodland caribou, shrews, weasels and hares, these animals live here because they can find enough food, water and shelter in the Canadian Shield
Great Lakes Region. This region includes lakes Superior, Michigan, Huron, Ontario, & Erie as well as surrounding
Chapter 1: Regions of Canada describe regionalism and how it divides countries, specifically Canada, naturally into six regions: British Columbia, Western Canada, Territorial North, Ontario, Quebec, and Atlantic Canada. These regions have been divided in a manner that correlates ‘like spaces’ in regards to human and physical geography (Bone, p.6) along with Canada’s historical development. The second key feature of chapter 1 describes Canada’s faultlines and they’re affects on Canada’s regional divide. There are four faultlines within Canada that reciprocate tensions that are mostly solved by being “soft” through negotiation and discussion (according to John Ralston Saul, Bone, p. 10). Bone places a great focus on these faultlines, which include: centralist/decentralist, Aboriginal/Non-Aboriginal, French/English Canadians, and newcomer/old-timer. “Canada’s heterogeneous nature often forms the basis of regional quarrels” (Bone, p. 11) particularly for the centralist/decentralist faultline. English/French speaking Canadians focus on Quebec and sovereignty, while the Aboriginal/Non-Aboriginal faultline deals with land claims, settlement and colonized peoples. Newcomers/old-timers refer to immigrants and settlers of Canada. The core/periphery model is a key concept that is commonly referred to throughout the text. It depicts the core as concentrations of power/wealth/population, with the periphery/hinterland as the weakly developed, resource based area.
Lake Erie is one of the first of the Great Lakes formed by the glaciers receding between 1 and 12,600 million years ago. Lake Erie borders New York, Pennsylvania, Ohio, Michigan and Canadian Province, Ontario. Lake Erie is about 241 miles long, about 57 miles wide and has about 871 miles of shoreline. The length of Ohio's shoreline is about 312 miles. It has three basins: the western which averages about 24 feet, central which averages 60 feet and eastern basin. The eastern basin averages about 80 feet with a maximum depth are 210 feet which make it the deepest. The water surface area is about 9,910 square miles and the volume is about 116 cubic miles. The Detroit River water flow makes up
Mississippi has a variety of different soils .The three general soils are 1) the river flood plain, known as the Delta, 2) a loess region, or bands of soils formed in windblown material that adjoins the Delta, and 3) Coastal Plain. The Mississippi Delta is better for growing row crop, while the loess and Coastal Plain region are better for animal production and forestry. The loess and Coastal Plain regions are divided based on similar soils, geology, climate, water resources, and land use called Major Land Resource Areas. The Mississippi Delta’s soil comes from sediments left by flooding various rivers in the region, rather than being a typical Delta formed by the mouth of a river. In the Delta most of the land is farmed, with three-fourths of the cropland to the north. Controlling surface water and drainage are major soil management issues. In the Delta soils are naturally diverse because of their alluvial origin. Particle sizes within the sediment decrease as distance from the originating stream increase. Another factor in Delta soil formation us surface water movement over time, because soils that formed under standing water have different properties than soils formed under moving water. Soils with large amounts of clay particles have unique features. When the soil is dry, small round aggregates form at the surface that look like shotgun buckshot, which is where the popular name for Delta clay soils “buckshot” came from. Soils with large clay content have very slow water filtration rates; this has led to significant aquaculture and rice production in the region. When floodwaters receded in the Delta, strong winds blew some of the dry sediment left by flooded river to the adjacent uplands to form the loess areas. Because of eas...
5 Narratives of the Indian Wars 1675-1699, edited by Charles H. Lincoln, Ph.D: A World Wide Web Site Containing Information About the Biology, History, and Geology of New England's Largest River (http://www.bio.umass.edu/biology/conn.river/), University of Massachusetts, Amherst.
The region's wildlife is also unique. In the winter, hoofed animals such as mule deer and bighorn sheep migrate down from the mountains into the warmer valleys. White-tailed deer, cottontails, jackrabbits, badgers and muskrats are seen throughout the seasons.
The climate of the tundra is characterized by harsh winters. The average temperature in the tundra area is about –27 degrees. But what is even worse are the long night. At nights the lowest temperture recorded was –67.36 degrees. There are even times in the year when the sun doesn’t come up for days. In the tundra we have little snow and even less rainfall. The rainfall is about a quarter inch in a yearly rainfall. Even though the tundra’s winters are long a harsh there summers are the shortest season of all. Do to the terrible weather and climate in the tundra their animals and plant life is very limited.
Endangered Plants and Animals of Oregon, by the Agriculture Experiment Station at Oregon State University.
Temperate grassland biomes can be found in North America, Africa, the pampas of South America and many parts of Eurasia. Grass is the main plant in Temperate Grassland biomes, trees and shrubs are rare to see in this type of biome. Temperate grasslands also have an extremely high abundance of wildlife. The wildlife living in this biome includes bison and pronghorn sheep, but mainly the animals most affected were the cattle and horses that lived on the surrounding farms.
are mainly based in plains and lowlands of some kind. The Low Arctic Tundra is
The Niagara River is the river which connects two great lakes together and is located in Ontario, Canada. It connects Lake Ontario to Lake Erie. A landform which is located around here, that you may be familiar with, is the Welland Canal which is used so that ships can bypass the falls. The Welland Canal first opened in 1829, and this version of the Canal was dug by hand. The Canal has been widened and deepened over time, and the last alteration to it was made in 1959. It is run by the St. Lawrence Seaway Management Corporation, and has allowed ships to bypass the amazing Niagara Falls that are found in the Niagara River, as well as the rapids on the river. (1)
"Step 1. Characterizations of the Watershed." Forest Service: 17 pars. Viewed 7 Nov. 2002. <http://www.fs.fed.us/r2/psicc/spl/south_platte_web/step_1.htm>.