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bija089 [108]
3 years ago
11

Geography-Citing relevant examples, discuss 4 benefits of possibilism on humanity

Geography
1 answer:
Eduardwww [97]3 years ago
7 0

Answer:

Hey mate.....

Explanation:

This is ur answer....

<em>Possibilist in cultural geography is the theory that the environment sets certain constraints or limitations, but culture is otherwise determined by social conditions. In cultural ecology, Marshall Sahlins used this concept in order to develop alternative approaches to the environmental determinism dominant at that time in ecological studies. Theory by Strabo in 64 BC that humans can make things happen by their own intelligence over time. Strabo cautioned against the assumption that nature and actions of humans were determined by the physical environment they inhabited. He observed that humans were the active elements in a human-environmental partnership and partnering. </em>

<em> </em>

<em>The controversy between geographical possibilism and determinism might be considered as one of (at least) three dominant epistemologic controversies of contemporary geography. The other two controversies are 1) the "debate between neopositivists and neokantians about the "exceptionalism" or the specificity of geography as a science the contention between Mackinder and Kropotkin about what is—or should be. </em>

<em>Possibilism in geography is, thus, considered as a distinct approach to geographical knowledge, directly opposed to geographical determinism.</em>

Hope it helps!

Brainliest pls!

Follow me! :)

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Briefly describe the characteristics of the four main layers of Earth. Include temperatures.
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Answer:

Crust

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Mantle

The mantle is the second layer of the earth. It is split up into two different parts, the lithosphere (which is the top part) and the asthenosphere (which is the bottom part). The lithosphere is a dense rock made out of iron and nickel, the asthenosphere is a plastic like fluid. The temperature of the lithosphere is around 300 to 500 degrees celsius, and the asthenosphere is around 4500 degrees celsius. The mantle has the biggest volume of all the layers, the volume of it is 84% of the earth. It is 1,800 miles deep or 2,900 kilometers deep. In the mantle are convection currents which make the mantle move. The lower mantle heats up and rises and cools down then gets pushed down because it is heavier. Then I keeps going on like that. The mantle grows a meter a year.

Lithosphere

The lithosphere is the top layer of the mantle. The lithosphere includes having the crust in it. It is a cooler layer because it is farther from the inner core. The lithosphere is a dense rock made out of iron and nickel. The temperature of the lithosphere is 300-500 degrees celsius. Inside the lithosphere and asthenosphere are currents, called convection currents. They make the lithosphere and asthenosphere turn round and round. So because the lithosphere is denser it is being forced down closer to the core and then heats up then forces its way back up to the top because it is less dense.

Asthenosphere

The asthenosphere is the bottom layer of the mantle. It is a plastic like liquid made up of iron and nickel. The temperature of the asthenospere is 4500 degrees celsius. It is hotter than the lithosphere because it is closer to the inner core. Inside the asthenosphere and lithosphere are currents, they are called convection currents. So because the asthenosphere is less dense or lighter than the lithosphere is forces its way up to the top and foces the lithosphere down. It then cools down then gets forced back down by a hotter substance

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Explanation:

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