"if a response is followed by a pleasurable consequence, it will tend to be repeated. if a response is followed by an unpleasant consequence, it will tend not to be repeated." this is a statement of

Thorndike's law of effect

Explanation:

Thorndike's law of effect states that if the reponse to an action is pleasurable the person tries to keep doing the same action to receive pleasure.

If a person gets displeasure from an action's response then the person will stop doing that action.

For example, if a child gets candy from their parent after getting good grades, the child will try obtain good grades in the next test in order to recieve the plesurable response of receiving candy.

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)