The answer is <u>"Hasty generalization".</u>
Hasty generalization is a kind of logical fallacy. A fallacy is a contention that depends on mixed up thinking. When one makes a hurried speculation, he applies a conviction to a bigger populace than he should in view of the data that he has.
For instance, if my sibling likes to eat a great deal of pizza and French fries, and he is sound, I can state that pizza and French fries are solid and don't generally make a man fat. Be that as it may, I don't have a sufficiently extensive example populace to make this case. I have summed up in light of one individual.
Since it was closer to the people the legatrative should have more power
The reason this leads to a conflict of interest, is because allowing politicians the power of redistricting creates a gateway for partisan gerrymandering, which is the act of manipulating the boundaries of an electoral constituency in order to ensure that a party wins seats in specific district.
Answer:
C. incorporates and explains both seafloor spreading and continental drift
Explanation:
The theory of plate tectonics -
According to this theory , it helps to explain briefly the bifurcations in the outermost shell of the planet earth , is referred to as the theory of plate tectonics .
The lithosphere consists of the outermost layer of the planet i.e. , the crust along with the top most portion of the layer mantle .
Exactly below the lithosphere is the second layer i.e. , asthenosphere , which consists of malleable particles of the mantle .
The theory helps to explain the process of continental drifts and seafloor spreading .
Hence ,from the given question ,
The correct answer is c.
I believe the answer is: Opening the halls of government to the citizens and abolishing the monarchy
By abolishing the monarchy, the king and nobles that held the absolute control within society started to losing their grip. This force the people to establish a new form of government which put the majority of the power to the people, hence a democracy was being chosen.
