Tabetha has a mental picture of the layout of her house, also called a so when she comes home late at night she can navigate through the rooms without turning on a light. group of answer choices

Cognitive/mental map.

Explanation:

According to the information given, that Tabetha most likely has a mental map of her house, given that she can navigate through the rooms without turning on a single light. A cognitive map, as it's name implies, involves a mental representation to recall in which the individual can remember geographically any locational or enviromental information previously gathered. In this case, it's Tabetha's house, but it could very easily be her workplace, her parent's house, a club, etc.

answer; (i-o) psychologist

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)