Since he was a year old, adrian was carefully coached by his parents so that he grew up to be a well-mannered, confident, and generous person. his parents believed in leading by example. adrian carried the values he learned at home wherever he went—to school, to college, and to his workplace. be reported these values to his children and grandchildren. the process that adrian went through is known as:

Socialization

Explanation:

From the psychology point of view, socialization refers to the process of learning social norms and acting as it is expected in a given culture.

This process takes place since when we are born and at first, our parents or principal caregivers are the ones who are mostly in charge of socialization (since they are the ones that teach us norms and how to behave) and as we grow older we can go through this process with other people/figures. Also, as we continue growing older we can transmit these values to our children or grandchildren, this entire process (which actually never stops) is called socialization.

In the example, Adrian was coached by his parents (they taught him norms and proper behaviors and who were his main caregivers) so he grew up to be a well-mannered, confident person. He kept these values and continued being led by them in the school and his workplace. Later we transmitted these values to his children and grandchildren, this is a continuous process that hasn't stopped and that has consisted in learning the social norms, therefore we can conclude this is the socialization process.

b) trade is easy because of the direct line between their major ports. bilateral trade reached 89,6 thousand million.

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)