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What conclusion do geographers draw when they observe moraines ridge like plies of rock and debris?
Geographers draw the conclusion that moraines are the product of ice age glacial activity when they observe ridge-like piles of rock and debris. Glacial moraines are formed from the debris of rock and sediment that is carried by glaciers and then deposited when the ice melts. Moraines can vary in size shape and composition but their presence indicates the activity of a glacier in the area. Geographers may also observe the shape of the moraine which can range from a single ridge to a series of ridges as well as the size of the moraine and its elevation. By noting these characteristics geographers can draw conclusions about the past geological activity of the area.
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What conclusion do geogrphers draw when they observe moraines ridgelike piles of rock and debris?
Geographers conclude that moraines are indicators of past glacial activity. These ridgelike piles of rock and debris are formed from the accumulation of materials that glaciers have eroded and transported as they advance and retreat. The presence and characteristics of moraines can reveal information about the movement and size of glaciers, as well as the environmental conditions during the periods of glaciation.
What conclusion do geographers draw when they observe moraines and mdashridgelike piles of rock and debris a volcano erupted there chemical weathering has occurred a fault lies nearby a glacier once c?
Geographers conclude that moraines, which are ridge-like piles of rock and debris, indicate past glacial activity in the area. The presence of these formations suggests that a glacier once occupied the landscape, depositing the accumulated materials as it advanced and retreated. This observation helps researchers understand historical climatic conditions and the movement of ice in the region.
Why are moraines often fragmentary?
Moraines are often fragmentary because they are created by the accumulation of debris carried by a glacier. As the glacier moves and melts, it can deposit various sizes of rock fragments and till in a chaotic manner, leading to the fragmented appearance of the moraines. Additionally, the mixing and rearrangement of the debris by glacial processes can contribute to the irregular and broken nature of moraines.
What is a ridge or mound of debris chiefly boulders gravel sand and clay?
A ridge or mound of debris chiefly composed of boulders, gravel, sand, and clay is called a moraine. Moraines are deposited by glaciers and can be found in various formations, such as lateral moraines along the sides of glaciers or terminal moraines at the end of a glacier's advance. Moraines are important features in understanding past glacial activity.
What causes moraines to form?
Moraines are formed by the accumulation of unconsolidated rock debris, such as sand, gravel, and boulders, that have been transported and deposited by glaciers. The debris is carried along by the moving glacier and then left behind as the glacier retreats or melts, creating ridges or mounds of sediment.
What conclusion do geographers draw when they observe moraines piles of rock and debris?
No
What conclusion do geographers draw when they observe moraines- ridgelike pile of rock and debris?
A glacier once covered the area. THIS IS TRUE.GRADPOINT/NOVANET :) ;)
What conclusion do geographers draw when they observe moraines-ridgelikes piles of rock and debris?
A glacier once covered the area. THIS IS TRUE.GRADPOINT/NOVANET :) ;)
What conclusion do geogrphers draw when they observe moraines ridgelike piles of rock and debris?
Geographers conclude that moraines are indicators of past glacial activity. These ridgelike piles of rock and debris are formed from the accumulation of materials that glaciers have eroded and transported as they advance and retreat. The presence and characteristics of moraines can reveal information about the movement and size of glaciers, as well as the environmental conditions during the periods of glaciation.
What conclusion do geographers draw when they observe piles of rock and debris?
A glacier once covered the area. THIS IS TRUE.GRADPOINT/NOVANET :) ;)
What conclusion do geographers draw when they observe moraines and mdashridgelike piles of rock and debris a volcano erupted there chemical weathering has occurred a fault lies nearby a glacier once c?
Geographers conclude that moraines, which are ridge-like piles of rock and debris, indicate past glacial activity in the area. The presence of these formations suggests that a glacier once occupied the landscape, depositing the accumulated materials as it advanced and retreated. This observation helps researchers understand historical climatic conditions and the movement of ice in the region.
These moraines are ridges of rock debris formed along the sides of a moving glacier?
Terminal moraines or terminal
Ridges of debris left by melting water?
moraines
What moraines are ridges of rock debris formed in front of a moving glacier.?
Ridges of rock debris that form in front of a glacier are called terminal moraines at the point that the glacier stops moving ahead.
Why are moraines often fragmentary?
Moraines are often fragmentary because they are created by the accumulation of debris carried by a glacier. As the glacier moves and melts, it can deposit various sizes of rock fragments and till in a chaotic manner, leading to the fragmented appearance of the moraines. Additionally, the mixing and rearrangement of the debris by glacial processes can contribute to the irregular and broken nature of moraines.
Unsorted rocky debris that is formed by a melting glacier?
The accumulation of unsorted rocky debris that is formed by a melting glacier is called a moraine. There are many large moraines throughout the northern parts of North America, Europe, and Asia.
How are the four types of moraines different from each other?
The four types of moraines are lateral, medial, terminal, and ground moraines. Lateral moraines form along the sides of a glacier, medial moraines are formed when two glaciers merge and their lateral moraines combine, terminal moraines mark the furthest extent of a glacier's advance, and ground moraines are the debris left behind beneath a glacier as it retreats.
