Olivia and her teenage daughter, natalie, are arguing again about whether natalie should go to a family gathering this sunday or attend an outing with her friends. olivia and her daughter argue about this topic every week. this time, olivia turns to her daughter and says, "ok, if it is that important that you go out with jenna sunday, then i can agree this time around." olivia is using what conflict handling style? accommodation controlling collaboration avoidance

Olivia and her teenage daughter, Natalie, are arguing again about whether Natalie should go to a family gathering this Sunday or attend an outing with her friends. Olivia and her daughter argue about this topic every week. This time, Olivia turns to her daughter and says, "Ok, if it is that important that you go out with Jenna Sunday, then I can agree this time around." Olivia is using accommodation, conflict handling style.

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)

the article must be ratified by three-fourths (38) of states within a proscribed deadline.

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