Which of the following best describes the communist ideal

The Communist ideal is a classless society in which everyone works for the common good.

Explanation:

Communism is a socio-economic and political system that advocates a classless, equal and co-owned social model. Proponents of communism often see their ideas as a form of society following socialism.

This movement was aimed at replacing private ownership and the profit-based economy with at least the public ownership and control of large-scale production facilities.

As a political ideology, communism is generally considered to be the final stage of socialism. This consists of a broad group of economic and political philosophies linked to various political and intellectual movements and the work of theorists of the Industrial Revolution and the French Revolution. Communism can be said to be the opposite of capitalism, offering an alternative to the problems of the capitalist market economy and the legacy of imperialism and nationalism.

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)