The scarping and gouging action of the ice created depressions in the bedrock. These depressions filled with water to form the hundreds of thousands of lakes that now dot the shield.
Glaciers can alter the drainage patterns of a shield by creating valleys and basins through erosion. As glaciers move, they carve out new paths for water to flow, influencing the direction and speed of drainage. Glacial meltwater can also interact with underlying soil and rocks, affecting groundwater movement and storage.
Two factors that affect the size of glaciers are temperature and precipitation. Higher temperatures can cause glaciers to melt faster, while increased precipitation can help glaciers grow by adding more ice mass.
Although the exact amount of material transported will never be known, suffice it to say that massive amounts of soil and rock were carried away from the area of the Canadian Shield by glaciation during the most recent ice-age. The weight of the glaciers actually depressed the land surface, and scraping and gouging by rock-filled ice created thousand of depressions which are now lake basins.
Valley glaciers are narrower and longer, flowing through valleys and carving deep U-shaped valleys. Continental glaciers are wider and thicker, covering large land areas and shaping landscapes through erosion and deposition. Valley glaciers are more localized in their impact, while continental glaciers have a broader influence on the land.
Moraines are piles of rocks, soil, and debris left behind by glaciers. They can impact a landscape by creating landforms such as ridges, hills, and valleys. Moraines also play a role in shaping drainage patterns and influencing soil development in the area.
Glaciers can alter the drainage patterns of a shield by creating valleys and basins through erosion. As glaciers move, they carve out new paths for water to flow, influencing the direction and speed of drainage. Glacial meltwater can also interact with underlying soil and rocks, affecting groundwater movement and storage.
The scarping and gouging action of the ice created depressions in the bedrock. These depressions filled with water to form the hundreds of thousands of lakes that now dot the shield.
yes, it does
the effect is
Glaciers made basins and when the glaciers melted it left lots of lakes.
The shape of the Canadian Shield was cause by glaciers and ice sheets during the many glaciations which have occurred during the last 2.6 million years of the present ice age.
The Canadian shield
The Canadian shield.The Canadian shield was the area of Canada that had most of its surface scrapped up by ice age glaciers. It covers half of Canada and the glaciers that scrapped the shield also made the huge holes, that are also known as the great lakes.
Canadian Shield is the flat rock formation that covers northern ontario. It was caused my glaciers scraping the soil away.
The scientific study of glaciers and their effect on the landscape say again
melting glaciers -> flooding
Water can speed up the rate at which glaciers melt. Whether the water is acidic or not has no effect.