"Mark is a member of a small tribe in New Guinea. The majority of people in his group fish for sustenance and share their catch with all the other members. Most of the people in his culture are very similar in their values, norms, and outlook on life. Mark steals from another member of his tribe. He will probably receive which type of social realignment?

- Mark will be shamed in front of the entire tribe.

Explanation:

As per the question, the kind of social realignment that Mark would probably receive includes 'being shamed before the entire tribe' as he 'steals the values, outlook, or norms on life from another member of his tribe'. Since Mark denied to conform to the beliefs or values perpetuated by the majority, he would be subject to humiliation and shame before the entire tribe in order to realign or bring him back to accept the culture or belief propagated by the majority of people in the tribe. Therefore, 'being ashamed in the public' would be the most likely social realignment he would receive.

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)

b. have a great