Answer:
Colonials would want to build their settlemesnt by the sea so they could use ships as transportation or for trading. They would also want to build near mountains so they could be protected or not want to build by mountains so they wouldn't have to travel over them for expansion reasons or also trading.
Hope I could help
Pull factors can be better climate, food, resources, jobs
Answer:
Yes, it would import wool
Explanation:
Autarka will import wool from the neighboring country because the country has a comparative advantage in the production of wool and hence wool from the country will be cheaper than what is obtainable in Autarka, Autarka should concentrate in the production of a good they have comparative advantage over the neighboring country in producing and export such good to the neighboring country and import wool.
Explanation:
Satellite image of the Piqiang Fault, a northwest trending left-lateral strike-slip fault in the Taklamakan Desert south of the Tian Shan Mountains, China (40.3°N, 77.7°E)
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In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within the Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as subduction zones or transform faults.[1] Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep.[2]
A fault plane is the plane that represents the fracture surface of a fault. A fault trace or fault line is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault.[3][4]
A fault zone is a cluster of parallel faults.[5][6] However, the term is also used for the zone of crushed rock along a single fault.[7] Prolonged motion along closely spaced faults can blur the distinction, as the rock between the faults is converted to fault-bound lenses of rock and then progressively crushed.[8]
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