Answer:
to show information about weather and temperature
Answer: Sand and gravel deposits.
Explanation:
Glaciation is a natural phenomenon in which the temperature of the earth drops considerably over a long period, this causes the glaciers of the poles to expand to cover large extensions of continental and oceanic terrain.
When the temperature rises again and the ice from the glaciers recedes, large deposits of sand and gravel are formed. This is because the deglazing process is slow, and the retreating glaciers remove the surface layers of the earth, therefore mineral deposits are formed. Also, the deglaciation process forms rivers and lakes that leave large deposits of sand and gravel.
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Answer:
Follows are the solution to this question:
Explanation:
Its climate dictatorships of Vancouver, as well as Winnipeg, are very different from one's different destinations. As just a marine location, Vancouver does have a fairly stable varies with temperature to Winnipeg that has an erratic pattern of sharp images. Its key aspect was its climate pattern throughout the year long. Vancouver is indeed a coastal city and therefore the effect of its water body largely regulates its freezing point. The distinction between autumn as well as winter peaks is, therefore, close to zero. Its highest warm weather is about 19°C as well as the lowest winter about 5°C, giving a roughly annual range of temperatures of 14°C.
Winnipeg, on the other hand, is a mainland internal destination. Its highest temperatures are 27°C, whereas the smallest temperatures can be -10°C. Therefore the annual range of temperatures is 37°C. So, the patterns of weather are genuinely different.
The further away the oceanic crust is from the mid-ocean ridge, the older it is. The mid-ocean ridge is where the youngest oceanic crust is.