Robert feels lost in his biology class He wants to raise his hand and ask the teacher to explain 12 and behavior He doesn't raise his hand because he is so afraid the other students will laugh at him, call him "stupid," and talk about him after class. Robert's thinking is typical of what researchers refer to B) reversion to childhood egocentricism. how two cells that have the same genetic material can have different morphology as: A) dual processing. B) reversion to childhood egocentricism C) phobia of taking risks D) the sense of an imaginary audience

D. The sense of an imaginary audience.

Explanation:

This thinking is common with young adolescents. It is characterized by an individual imagining that a large number of people are listening or have their eyes fixated to him when talking.

This usually scares them as they get frightened trying to envisage how these ‘imaginary audience ‘ will respond to what they say or do.

answer; i believe the correct answer is enlightenment;

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)