When geographers observe moraines, they can conclude that glaciers once extended to that location and deposited the moraine material. The size, shape, and distribution of the moraines can provide insights into the past behavior of the glaciers, such as their extent and direction of flow. Studying moraines can also help geographers understand past climate conditions and how they have changed over time.
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.
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.
Well, Geographers! :)
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.
ground moraines
No
A glacier once covered the area.
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.
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.
A glacier once covered the area. THIS IS TRUE.GRADPOINT/NOVANET :) ;)
A glacier once covered the area. THIS IS TRUE.GRADPOINT/NOVANET :) ;)
It means to observe or conclude some thing about your experiment.
It means to observe or conclude some thing about your experiment.
A glacier once covered the area. THIS IS TRUE.GRADPOINT/NOVANET :) ;)
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.
inductive logic.
Ground moraines are located at the base of the glacier.