Gracie was recently hired by a detective agency after rounds of pre-employment testing and interviews. The pre-employment testing showed that she had a high ability to gather information regarding crimes, filter out unwanted information, and draw the right conclusions to strengthen her case. We can say that the pre-employment tests revealed that Gracie is good at

inductive reasoning                                      

Explanation:

Inductive reasoning is defined as a phenomenon in which an individual makes generalized decisions just after witnessing and observing the repeated instances related to something. Inductive reasoning begins with different observations and then moves backward to specific theories and generalizations. It is based on different logical processes and therefore is involved in various application, for example, forecasting, prediction, etc.

In reference to the question above, Gracie is good at inductive reasoning.

what are the answer choices?

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)