One of the main reasons why social class may not be completely reliable in predicting the preferences and tastes of americans is that:

One of the main reasons why social class may not be completely reliable in predicting the preferences and tastes of Americans is that "huge range of income call themselves middle class".

A social class is a gathering of individuals of comparable status, usually sharing equivalent levels of influence and riches. In human science, social classes portray one type of social stratification. At the point when a general public is sorted out by social classes, rather than by standings, it is hypothetically workable for individuals to achieve a higher status than the status with which they began. This development is conceivable in light of the fact that social classes are not founded on birth but rather on components, for example, instruction and expert achievement.

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)