Answer:
Democracy.
Explanation:
In the period of Ancient Greece there were many city-states established, that had different forms of government. The most peculiar one was created in Athens, known to us as democracy. With many reforms introduced by Cleisthenes, Solon and others, Athenians created a system inside which the people had authority and possibility to govern themselves through certain institutions such as Ecclesia. Of course, Athenian democracy differed from modern democracy as a lot of people didn't had the right to participate in public life.
Answer:
Group polarization has always been a thing, whether it be by class or political lean it is the way it is, no country is without strife, eventually tensions amount to the point the government can't contain it and has to get involved. I believe an American civil war is a possibility but unlikely, and probably not in our lifetime.
Explanation:
Answer: The Constitution improved greatly on the Articles of Confederation by creating an appropriately strong federal government, with provisions for protections of freedom.
Improved strengths of the federal government:
1. Creation of an executive branch of federal government, where the Articles just had a legislature.
2. Creation of a federal court system, with a Supreme Court that has final say (Articles of Confederation only allowed state courts)
3. Congress was divided into two bodies to allow for representation for both small and large states. Congress was granted powers to regulate interstate commerce, levy taxes, and print money.
Protections of freedom:
The Constitution includes the Bill of Rights. This outlines individual rights, and also reserves some rights to the states, so it protects from a tyrannical federal government.
The correct answer is - Passive.
The passive continental margins are transitional zones between the oceanic and continental crust, lithosphere, and it is not an active plate margin. This type of margins form from sedimentation over an ancient rift, which has now become a transitional lithosphere. This type of margins can be found further away from the ocean ridges, but also away from the active continental margins. The east coast of North America is a nice example of a passive continental margin. It has all the characteristics of it. It is made out of sediments, it is a transitional zone between continental and oceanic lithosphere, it is far away from the mid-ocean ridge from one side, and the active continental margins on the other side.
