In Stanley Milgram’s obedience research, the person playing the part of the “learner” was an accomplice, or , of the experiment. He was aware of the true purpose of the research, was never shocked, and was acting according to Milgram’s instructions a) confederate b) union c) associate

In Stanley Milgram’s obedience research, the person playing the part of the “learner” was an accomplice, or Confederate of the experiment.

Conclusively, we can say that in Stanley Milgram’s obedience research, the person playing the part of the “learner” was an accomplice, or Confederate of the experiment.

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a) confederate

Explanation:

Milgram's experiment was carried out to test how far people's obedience goes. For this, several men of different ages and educational levels were brought together to obey a person who was considered an authority at that time. These men did not know that they were being tested in the experiment, but they thought that an "apprentice" who would take shocks to different levels of electricity was being tested.

The experiment consisted of men giving shocks with increasing levels of electricity in the apprentice, whenever the authority ordered. The intensity of the shocks would increase to the point that it is impossible not to kill the apprentice.

What the men did not know is that the apprentice was an actor and confederate of the experimenter and that he was pretending to receive shocks.

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)