Are the use of psychological, sociological, and anthropological factors to determine how the market is segmented by the propensity of groups within the market (and their reasons. to make a particular decision about a product, person, ideology, or otherwise hold an attitude or use a medium.

Psychographics.

Explanation:

As the exercise describes, psychographics is a method which determines how the market is segmented by different groups within it. It's a qualitative methodology used to describe consumers on psychological attributes, like the exercise says: the reasons about making particular decisions about a product, a person, an ideology or otherwise hold an attitude or use a medium.

i dont believe in religion. lets all be peace

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)