Who finna answer all of that
<span>Supreme Court cases come in three varieties. Least numerous are the "original jurisdiction" actions, brought by one state against another, or between states and the federal government. The Constitution also empowers the Court to hear "all Cases affecting Ambassadors, other public Ministers and Consuls."</span><span>
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Answer: republican or dictatorships
Explanation:
Answer:
The answer is D.
Each side was able to gain land during the war. It went back and forth for a long time. The south invaded the north all the way up to the Chinese border until China decided to aid North Korea and pushed the south back down to its land. It went on like this for some time until finally the war stopped and the border between the north and the south stayed the same. The area between the border is called "No Man's Land" because not a single man has stepped foot there since the war ended. There are land mines there and who knows what kind of animals live in between the borders of North and South Korea.
Because of the fluctuation.
In most ocean regions, wind-driven circulation, which has been the focus of discussions so far, does not reach below the first kilometer of the oceans. The renewal of the waters below this depth is achieved by currents that are guided by differences in density produced by effects of temperature (thermals) or salinity (halinos). The associated circulation is therefore referred to as the thermohaline circulation. Since these movements are mostly quite slow, it is very unlikely to use direct current meters (current meters); they are usually estimated by the distribution of the physical properties of the water and the application of geostrophy.
The driving force of thermohaline circulation is the formation of water bodies. Water bodies with well-defined salinity and temperature characteristics are created in specific regions by surface processes; they then sink and slowly mix with other bodies of water as they move. The two main processes for the formation of water bodies are deep convection and subduction. Both are linked to the dynamics of the mixing layer on the surface of the ocean; thus, it is necessary to first discuss thermohaline aspects of the surface ocean first.
