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 reshape the drainage patterns of a shield by eroding the landscape and creating new channels for water flow. As glaciers advance and retreat, they can leave behind moraines and other landforms that affect how water drains across the shield. Melting glaciers can also increase water flow, leading to changes in drainage patterns.
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.
The case in question: eyjafjallajokull is a glacier. It is on a volcano, which is a shield volcano. A shield volcano has gentle sides. This defines a shield volcano. I hope this answers your question.
Some of the environmental problems faced by the Canadian Shield include acid rain pollution causing damage to its lakes and forests, mining activities leading to deforestation and water contamination, and climate change impacting its fragile ecosystems and wildlife habitats. Additionally, improper waste disposal and industrial activities can also have detrimental effects on the region's environment.
I do not know for sure but I had to research this a little bit and I believe that the land can be very mountainous at some points because it is partially a part of the Canadian Shield but that it can turn into valleys at some parts.... I would definitely not describe it as being plains such as Saskatchewan.... just so you have an idea. ;) hope this helped =)
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 reshape the drainage patterns of a shield by eroding the landscape and creating new channels for water flow. As glaciers advance and retreat, they can leave behind moraines and other landforms that affect how water drains across the shield. Melting glaciers can also increase water flow, leading to changes in drainage patterns.
The primary force that had the greatest effect on the drainage of the Canadian Shield area is glaciation. During the last Ice Age, massive glaciers sculpted the landscape, carving out valleys, lakes, and river systems. As the glaciers retreated, they left behind a network of lakes and rivers, significantly influencing the hydrology and drainage patterns of the region. This glacial activity has had a lasting impact on the topography and water flow of the Canadian Shield.
yes, it does
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.
they were formed when the lakes were frozen in the glaciers. Then as they resided, the clay belts were formed.
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.
Yes, lava can flow from a shield volcano. Shield volcanoes are typically characterized by low-viscosity lava that flows easily over long distances, creating broad, gentle slopes. The lava flows from shield volcanoes are generally not explosive and occur as a result of the slow accumulation and drainage of magma.
The Ice Age significantly shaped the Canadian Shield through extensive glaciation, which carved and eroded the landscape, creating features like valleys, lakes, and rugged terrain. The massive glaciers scraped away softer rock layers, exposing the ancient Precambrian rocks that form the Shield today. As glaciers retreated, they left behind deposits of sediments and created numerous freshwater lakes, influencing the region's ecology and hydrology. This geological activity also contributed to the rich mineral resources found in the Shield, making it a crucial area for mining.