Bonita believes we learn about the mind mainly by using logic and intuition; miguel believes it would be better to measure the activity of the brain. bonita is following the philosophy of , while miguel is following the philosophy of
a. aristotle; locke
b. plato; aristotle
c. descartes; plato
d. james; locke

d. Descartes; Plato.

Explanation:

For Descartes, the mind operates under two principles: intuition and deduction. The first is the simple observation and the second implies a consecutive order of ideas that implies a conclusion. That's the way kwonledge is build.

Plato, on the other hand, considers that knowledge is something we have already met before the soul were trapped into the body. In this case is not necessary a method to reach knowledge -like Descartes proposed- all we need is to observe the nature and then remember. Thats why would be enough for Miguel to measure and investigate what happens within the mind.

the president has the power to appoint federal judges, ambassadors, and other "principal officers” of the united states, subject to senate confirmation of such appointments.

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)