Me!
mikai is ready for his test in science. he gets nine hours of sleep the night before the test and wakes up to have a breakfast of yogurt and fruit. he walks into the classroom and takes a seat at the back of the class so he can be alone and avoid distractions. what can mikai do to improve his test-taking strategy?
a. eat more at breakfast and have something like pancakes.
b. drink coffee or soda with breakfast so he is more alert.
c. get less sleep; nine hours will make him too groggy.
d. sit in the front of the class or down the middle row.

D. Sit in the front of the class or down the middle row.

Explanation:

if she/he sat in the back she/he could easily get distracted and the teacher would not notice and she/he could also be raising her/his hand and could be not noticed. It would be better to sit more in front because the teacher can catch him/her sidetracked and can get him/her back and track.

I hope this helped.

~Aubrie~

world bank is the correct answer.

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)