Welkom is actually the second-largest city in the province of FREE STATE in South Africa, located about 140 kilometres northeast of the provincial capital, Bloemfontein.
Th province was formerly known as the Orange Free State before the year 1995. Interestingly, it is the only one of the four original provinces of South Africa which did not undergo border changes, excluding the reincorporation of Bantustans.
Answer:
the answer is D
Explanation:
before the spanish invaded it they carry desease that the natives were unknown with many died as well as the leader of the aztac empire
The combination of the weathering and erosion of the stream bank and the cutting into the bedrock from the velocity of the stream combine to make a "stream valley".
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What is stream valley?</h3>
A stream valley is an earthen dip where water is present at its lowest point. These valleys are the result of erosion, which is the transfer of decomposed rock or soil from one location to another.
The formation of stream valley is given below-
- The typically V-shaped stream valley is changed to a U-shaped valley because the U-shape offers the flowing glacier the least amount of frictional resistance.
- Because a glacier's cross section and viscosity are substantially greater than those of a river, its route has fewer and wider bends.
To know more about characteristics of weathering, here
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Answer:
Normal faults are <u>associated with tensional tectonic force.</u>
Explanation:
A Fault , in geology represents a planar fracture in a rock , there can be large faults , which are formed by the action of the tectonic forces , even the rapid movement of these tectonic plates on any active fault can lead to an earthquake.
There are two types of fault possible ,
Normal fault and Reverse fault.
In a normal fault , the hanging wall moves in downward direction with respect to the footwall , and , in reverse faults, the footwall moves in downward direction with respect to the hanging wall.
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