The theory that the psychological development of children repeats the history of the human race is known as the theory, proposed by mental evolution; hall recapitulation; hall mental phylogeny; cattell mental phylogeny; james physical phylogeny; munsterberg

The theory that the psychological development of children repeats the history of the human race is known as the Hall recapitulation theory, proposed by Stanley Hall.

Explanation:

G. Stanley Hall, the founder of organized psychology, was inspired by Ernst Haeckel's theories on development to propose the theory known as the theory of recapitulation, which explains that an individual goes through important developmental changes as he or she grows that follow the history of evolution of the human's body and mind.

Hall stated that until the age of eight the child should have the freedom to express natural emotions, also referred as "animal emotions" as after this stage, the individual will develop formal learning. After this, the person will also develop morals.

Hall's work is extremely important in psychology. He was the president of the American Psychological Association and was extremely interested in the education of young people.

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)