The main reason behind large clusters of people inhabiting
South, Southeast and East Asia is the chance of greater financial stability and
job opportunities. It is true that the economy of South, South east and East
Asia is on the rise. The economies of these countries are said to be growing
economies. So financial stability is high and with that comes the opportunity
of large amount of jobs. The people inhabiting these countries in numbers are
looking to take advantage of this situation and improve their living standards.
Rings or warm-core and cold-core eddies influence the intensity of storm system over the ocean because of how these rings have different measurements and impacts. Cold-core rings have diameters of about 185 mi and, viewed from above, rotate in a counterclockwise direction. While cold-core rings can be more difficult for satellites to track because their originally cool surface waters are warmed by absorption of solar radiation, which can make them almost indistinguishable thermally from surrounding surface waters. On the north side where the warm-core ring, these rings are typically 100 to 200 km (60 to 120 mi) across. These rings enclose warm waters from the Sargasso Sea located to the south and east of the Gulf Stream; hence, they are called warm-core rings. Viewed from above, these warm-core rings rotate in a clockwise direction. Because of the strong contrast in sea-surface temperatures, they are readily detected on infrared satellite images. Warm-core rings are also readily distinguished from the surrounding surface waters by their relatively low levels of biological production.
C.) Dividing
The Great Dividing Range, running just inland along Australia's eastern coast, is that continent's only significant mountain chain.
Answer:
El Salvador
Explanation:
While the majority of the republics have both the Caribbean and a Pacific coast, Belize only has a Caribbean coast and El Salvador only has a Pacific coast. Central America comprises the countries south of Mexico and up to Panama.
A) <span>the crust of the lithosphere that has fractured along plate boundaries and ridges</span>
