Research comparing the effectiveness of psychotherapists who received training in a number of different areas (psychology, psychiatry, counseling, social work) has demonstrated psychologists and psychiatrists tend to be more effective than counselors and social workers clinical psychologists tend to be more effective than psychiatrists psychiatrists tend to be more effective than clinical and counseling psychologists no reliable association exists concerning therapists professional training and effectiveness

no reliable association exists concerning therapists' professional training and effectiveness

Explanation:

Psychotherapy is designed based on the assumption that the problems which exist within the patient is caused by underlying unconscious thought that influence the patient's behavior.

The problem is that we can't really have a method to proof whether the diagnosis that the therapists made is correct. This make psychotherapy has notoriously low rate of success (only around 26.5%)

answer:   c.

it was not against the chinese government.

explanation:

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)