North korea and south korea both received from other nations during the korean war. which countries intervened?
a) the united states supported north korea; japan supported south korea.
b) china supported north korea; the united states supported south korea.
c) germany supported north korea; france supported south korea.
eliminate
d) vietnam supported north korea; china supported south korea.

North Korea and South Korea both received help from other nations during the Korean War. China supported North Korea; the United States supported South Korea are the countries intervened.

Option B

Explanation:

The Korean is the war fought between North Korea and the South Korea. It led to the split of Korea, eventually forming North and South Korea. This war was aided by some countries taking sides and supporting both of the parties.

North Korea was backed by People’s Republic of China and the South Korea was backed by United Nations, which was also supported by United States of America. The war led to an end in 1953 which lead to the split of two nations.

the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)