Imagine that you are at a party, and your best friend introduces you to a guy named david. you and your friend talk to david for an hour, and you both notice the hostile comments that he repeatedly makes about his roommate. later, you and your friend discuss your impressions of david, and you find that you disagree about him. your friend thinks that david’s comments were just good-natured joking and that he is a nice guy and a pretty funny fellow. you think that his comments were mean-spirited and that he is a hostile person. your disagreement arises because you and your friend differ in the stage of the realistic accuracy model (ram) of personality judgment.

utilization

Explanation:

Utilization stage of the Realistic Accuracy Model (RAM) of personality judgment -

The information which is detected correctly is then accurately judged by different perceivers of the information.

The point that how the perceiver uses information is very crucial  in this stage. There may be different opinions of the different perceivers which can depend on the stereotypes or the heuristics.

Thus, Both the people differ at utilization.

of what agreement it does not show

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)