The Great Lakes in North America, including Lake Superior, Lake Michigan, Lake Huron, Lake Erie, and Lake Ontario, were formed by glacial erosion during the last Ice Age. These lowlands were carved out by the movement of glaciers, creating the wide and deep basins that now hold the Great Lakes.
When the mountains got eroded, sediments broke off, and rolled down the mountain into the lowlands, that were oceans at the time, and the pressure from all the rocks fused them together, making it a sheet of sedimentary rock.
They would be scoured and eroded, eventually get deposited at the base of the glacier when it recedes as terminal moraine
The choices for this question are either a: U cross-Valley Profile, Y Cross-Valley Profile, V cross-valley profile, or S Cross Valley Profile.The answer to this question is a: U cross-valley profile is typical of canyons and valleys eroded by alpine or valley glaciers.
Glacially eroded valleys are normally U-shaped.
The Great Lakes in North America, including Lake Superior, Lake Michigan, Lake Huron, Lake Erie, and Lake Ontario, were formed by glacial erosion during the last Ice Age. These lowlands were carved out by the movement of glaciers, creating the wide and deep basins that now hold the Great Lakes.
the erosion of the shield regions created the rest of each continent. rivers and glaciers carried eroded material, called sediment, intoancient seas. there, it accumulated into thickbeds that slowly solidified intosedimentry rock.
No, it is they that are eroded by such things as rain, rivers and glaciers.
Till
Glaciers and rivers transport eroded rock material (sediment), that can form new sedimentary rock after deposition.
Glaciers have helped form Long Island in the sense that millions of years ago, the glaciers eroded the block of land that is now known as Long Island.
There are three lowland regions surrounding the shield: the Interior Plains, the Great Lakes-St.Lawrence Lowlands, and the Hudson Bay-Artic Lowlands. The bedrock under these lowlands is formed mainly of sediments eroded from the Shield. The sediments were laid down in the seas that existed at various times millions of years ago. As the rock particles collected, the weight of the upper layers compressed the lower layers into sedimentary rocks.
When the mountains got eroded, sediments broke off, and rolled down the mountain into the lowlands, that were oceans at the time, and the pressure from all the rocks fused them together, making it a sheet of sedimentary rock.
Glaciers eroded valleys, and when the ice melted, the valleys were flooded, and became fjords.
Sediments are deposited at the bottom of lakes, rivers, seas, and other large bodies of water, as well as certain depressions or basins on land. After being covered with additional layers of sediment, they could undergo the processes of sedimentary rock formation. Eventually, however, they could once again be subjected to weathering and erosion.
They would be scoured and eroded, eventually get deposited at the base of the glacier when it recedes as terminal moraine
The choices for this question are either a: U cross-Valley Profile, Y Cross-Valley Profile, V cross-valley profile, or S Cross Valley Profile.The answer to this question is a: U cross-valley profile is typical of canyons and valleys eroded by alpine or valley glaciers.