The tort of intentional infliction of emotional distress: a. requires proof of conduct that exceeds all bounds of decency. b. is a property tort. c. is the same as the tort of false imprisonment. d. requires proof of some physical harm before there can be recovery.

a. requires proof of conduct that exceeds all bounds of decency.

Explanation:

"Tort of intentional infliction of emotional distress" is a term used to refer to an offense where a person has been extremely offended in order to develop an emotional distress form by someone who intentionally or recklessly behaved extremely outrageously. Based on this, we can conclude that the tort of intentional infliction of emotional distress requires proof of conduct that exceeds all limits of decency.

"choosing is refusing" means individuals face an opportunity cost with each decision they make. economists state that every decision involves trade-offs. opportunity cost is the least desirable alternative given up as a result of a decision.

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)