Nine-year-old Jared has one very good friend. The two boys spend a great deal of time playing one-on-one basketball, and often can be heard talking to each other about a wide range of personal topics. Compared with other boys his age, Jared's social behavior is because most boys his age .

somewhat unusual , because most boys his age typically play in large groups and do not engage in intimate discussion.

Explanation:

Nine-year-old Jared has one very good friend. The two boys spend a great deal of time playing one-on-one basketball, and often can be heard talking to each other about a wide range of personal topics. Compared with other boys his age, Jared's social behavior is somewhat unusual because most boys his age typically play in large groups and do not engage in intimate discussion.

Many nine-year-olds will have a strong desire to belong to a group and establish their place within the social order of school. As result, many will become vulnerable to peer pressure because they want to impress their peer group. It is strang to see the boys socialuze in that manner.

they all focused on themes about the inevitability of death.

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)