Basic freedoms in the United States:

A. can never be diminished under the Constitution.
B. must be balanced against competing interests, such as national security.
C. have vanished in the modern era.
D. are absolute; no restrictions are allowed.

B. must be balanced against competing interests, such as national security.

Explanation:

While the basic freedom in the US, is to grant each and every citizen the liberty to do as they wishes within the content of the law and constitution, the civil right is the action government should take to curb the excess or those acts that may jeopardize the freedom of others.

Hence, Civil liberties is defined as the protection of US citizens or minority against government actions. For example, the First Amendment of the Bill of Rights guarantees citizens the right to practice whatever religion they please.

However, Civil rights, on the contrary, is expressed to be the positive actions or measures the government should take to create and enable equal conditions for all Americans.

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)

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explanation:

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