The boyd family has twins, markus and valeria, both of whom have been identified with emotional and behavior disorders. mr. and mrs. boyd as well as mrs. williams, the grandmother, have begun meeting twice each month at the community center with other families. during these meetings, the families share information about local resources; ideas and suggestions for dealing with behavior, social, and academic issues; and strategies for coping on a day to day basis. this is an example of:

parent-support group

Explanation:

According to my research on studies conducted by various sociologists, I can say that based on the information provided within the question this is an example of a parent-support group. This is a type of group within a community in which the parents of the community gather together and discuss important issues regarding the community and it's inhabitants including their children. Just like what is going on in this situation.

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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)

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