In the research presented in the textbook, people who were asked to provide examples rated themselves as more assertive than people who were asked to provide examples.

The correct answer is:

Assertive - unassertive

In the research presented in the textbook, people who were asked to provide assertive examples rated themselves as more assertive than people who were asked to provide unassertive examples.

Explanation:

According to the research paper Ease of Retrieval as Information: Another Look at the Availability Heuristic published by the Journal of Personality and Social Psychology, human behavior is conditioned depending on the different considerations that can be taken into account about a certain situation.

During the study it was possible to observe how for the individuals that were asked to provide examples about assertive behaviors, their own perception was described as a more assertive one, while on the other side individuals who were asked to describe unassertive situations described themselves in an unassertive conception.

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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)