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Among its many influences, glaciation formed the Great Lakes and Long Island (NY state).

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What was the Wurm Glacial Period?

The Wurm Glacial Period, also known as the Last Glacial Maximum, was a period of intense glaciation that occurred about 20,000 years ago during the Pleistocene Epoch. It was characterized by extensive ice sheets covering much of North America, Europe, and Asia, leading to lower global sea levels and significant changes in climate. The Wurm Glacial Period had a major impact on the earth's landscape, shaping features like moraines, eskers, and drumlins that are still visible today.


How deep was the glacial ice that covered ny 18000 years ago?

During the last glacial period, the ice that covered New York was approximately 5,000 to 7,000 feet thick. This ice sheet, known as the Laurentide Ice Sheet, extended over much of North America and had a significant impact on the landscape and climate of the region.


Which scenario most likely formed most large lakes in North America and Europe?

Most large lakes in North America and Europe were likely formed by glacial activity during the last Ice Age. As glaciers advanced and retreated, they carved out depressions in the landscape, which later filled with water. Over time, these glacial lakes became some of the largest in the regions, including notable examples like the Great Lakes in North America. Additionally, post-glacial rebound and sedimentation further shaped the lakes we see today.


Where in the north America is the area of glacial erosion?

Canada


What are the phyisical featers for Minnesota?

A very basic overview of the landscape includes boreal (evergreen) forests in the north and northeast; plains in the extreme northwest; prairies in the west, southwest and south; glacial lakes in the north and central; and mixed hardwood forests in central, east and southeast.


How did the middle passage impact the north American trade?

it was a part of triangular trade


What geologic processes shaped much of north America?

A. Shaped much of the landscape of New England B. Left large, visible striations in the rock C. Carved out the Great Lakes


What actions did glacial ce take as it shaped North America?

Glacial ice shaped North America through processes such as erosion, transportation, and deposition. As glaciers advanced and retreated, they carved out valleys, created lakes, and sculpted mountain ranges, leaving behind distinctive landforms like U-shaped valleys and fjords. Additionally, glaciers transported sediments over vast distances, depositing them as moraines and outwash plains, which contributed to the region's diverse geological features. This glacial activity significantly influenced the landscape, ecology, and even human settlement patterns in North America.


How have glaciers affected our landscape in minnesota?

Glaciers have significantly shaped Minnesota's landscape, primarily during the last Ice Age when they advanced and retreated across the region. This glacial activity carved out the state's numerous lakes, rolling hills, and the distinctive features of the North Shore of Lake Superior. Additionally, the deposition of glacial till and sediments created fertile plains and influenced the drainage patterns of rivers and streams. Overall, glaciers have left a profound imprint on Minnesota's topography and ecology.


The general direction of continental glacial advance in the us is from north to south?

yes


How does Mexico's physical landscape affect how the area was shaped?

The physical landscape of mexico affects how the area was shaped because most of it is on the great North American Plate and it is one of the most seismically active regions in the world.


What caused the north European plain?

The North European Plain was primarily shaped by glacial processes during the last Ice Age, which ended around 10,000 years ago. As glaciers advanced and retreated, they carved out valleys and deposited sediments, creating a flat and fertile landscape. Additionally, the region's geology, consisting of sedimentary rock and loess deposits, contributed to its flat terrain. This combination of glacial activity and geological features resulted in the extensive plains seen today.