Answer:
The traditional beliefs led to sparsely population is explained below in details.
Explanation:
A custom is a belief or practice established down within an organization or society with figurative meaning or particular importance with roots in the past.
A basic source of population increase that addresses this rural-to-urban transformation states that as nations urbanize and industrialize, household size typically reduces and incomes traditionally improve. Though this may not be correct in all circumstances, it is a general belief that is compatible across cultural lines.
Answer:
Non Linear
Explanation:
This appears to be a quadratic equation, not a linear.
Linear equations can be represented by the following:
Y=mx+b
Ax+By=C
Y-y1=m(x-x1)
This equation can't be represented as ANY of these. It is, however, able to be converted to the standard form of quadratic equations.
Answer:
Only the stratosphere contains enough air for living things to breathe. True Or False?
its true
This geological process is called Mantle drag .
What is Mantle drag?
According to the first driving mechanism, known as mantle drag, plate motion is the consequence of viscous drag brought on by the lateral motion of the tops of mantle convection cells in the asthenosphere on the base of the lithosphere . Convection cells would thus be mostly absent beneath continents, rising beneath oceanic ridges, and dropping beneath trenches. This idea states that the oceanic lithosphere would be in a state of tension at the ocean ridges and compression at the trenches.
Due to their connection to accretive and destructive plate boundaries, the horizontal widths of the convection cells causing mantle drag would be projected to be around half an ocean's breadth, or 3000 km.
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Answer:
-high
-low
-stronger
Explanation:
A lot of factors determines the generation and movement of wind. However, winds tend to blow from areas of high atmospheric pressure to areas of low atmospheric pressure, and the greater the difference between the high and the low pressure areas, the stronger the wind.
These factors include Coriolis effect, trade winds, energy from the sun, differences in local temperature.