A. appropriate; persons familiar with group members are allowed self-help membership. B. appropriate; self-help groups are not professional and therefore are open to public knowledge. C. inappropriate, most self-help groups have a rule of confidentiality. D. inappropriate: the student should not have been allowed to attend the group.

A student nurse attends a self-help group as part of a class assignment. While there the student recognizes a family friend. Upon returning home, the student talks about the friend's attendance with the family. The student's actions can be described as...

C. Inappropriate; most self-help groups have a rule of confidentiality

Explanation:

HWhen it comes to self-help group, it is always believed that, there is a good degree of confidentiality such that, any issues shared among the self-help members will be kept "secret"

Thus, it is in appropriate for the student nurse to talk about the attendance of the friends with, the family.

The reason why confidentiality is considered important among self-help group members is because, it allows them to pour their hearts out, and such "secret" is best kept safe rather than let people outside the group know except the owner of the stories, that is the person involve, actually grant the permission of the story going public.

the psychological impact of incarceration

explanation:

a brief interference with a person's freedom of movement with a duration that can be measured in minute.

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)