The role of a judge is different from other federal officials because a judge

bases decisions on the will of the people while other officials base decisions on the law
bases decisions on the law while other officials base decisions on the will of the people
consults other federal officials on the intent of the laws before making a case decision
consults other federal officials on the will of the people before making a case decision

The role of a judge is different from other federal officials because a judge bases decisions on the law while other officials base decisions on the will of the people

Option B

Explanation:

The federal officials hear the case and they go hand in hand with the people’s will. They actually support their people though they know the true terminology behind it. But it is not the case of a judge who takes the decision only by referring the law.

The judge stays unbiased and sticks on to the law of the court. The judge is also the finder of the exact fact by evaluating the evidence. They are supposed to comprehend the case by going through both the sides and then acquiring a conclusion with the support of reasonable evidences.

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)