You are a university student, but you also wait tables at a restaurant. One evening, one of your professors happens to come in for a meal (awkwardly, on a first date!). Use role theory to describe the interaction (and possible role conflict) that ensues.

According to the role theory each scenario or environment stablishes certain roles in society, each person takes. In this case the student and teacher know how to behave according to the roles in an academic context. The scenario and social context changes and it can cause akwardness because the roles under they related are changed because of the situation.

Explanation:

The interaction teacher student, located each one under a specific role. The interaction changes according to the social context. They both may feel unconfortable because the change of scenary

The teacher is having an intimate moment in which being around a student may not be the ideal situation for neither. But it is a matter of stablishing the roles of the actual context.

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)

answer; adjusting and adapting to a culture other than one's own;