When asked why he bought a specific automobile, Jeremy replied that is has good gas mileage, is rated one the best cars in terms of safety, and is in a moderate price range. These reasons reflect Jeremy's motives.

manifest motives

Explanation: Unlike the latent motive which describes factors that motivate individuals to do things but will find it hard admit,

Manifest motive are factors that motivates or pushes an individual to do something and they will freely admit those factors.

For example; you buy a laptop and your motive is to use it to commit crime, you won't freely admit the factors behind why you bought it; that is latent motive.

On the other hand, when you buy a laptop and the factors or reason behind your purchase is that, it will help you in your studies, you will freely admit the motive behind buying the laptop; that is manifest motive.

Jeremy freely admitted the factors that led him to buy that particular automobile, this is a good illustration of manifest motive.

aa

explanation:

literally the answer is aa. not kidding. aa is a group.

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)