Auniversity has just hired additional faculty and staff. who of the following is most likely to earn the highest pay?

chemistry professor with a doctoral degree

economics graduate student teaching assistant

education lecturer with a master's degree

classics department office manager with a bachelor's degree

Chemistry professor with a doctoral degree.

Explanation:

This is the person who is most likely to earn the highest pay. There are two reasons for this. First of all, this person is a full-time professor, and not a teaching assistant, which makes his pay higher. The second reason is that this professor has the highest level of education, as he has a doctoral degree. This also warrants a higher pay compared to the other people.

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)