Roy was sitting in class when he realized that he had stopped listening to his instructor's lecture and started day dreaming. he only stopped paying attention for a few minutes, but the instructor had already moved on to a new topic. it would be most appropriate for roy to

refocus his attention on the lecture and start actively taking notes again.

Explanation:

Roy need to stop daydreaming and draw back his focus to the lecture otherwise he will have a lot to catch up on and may end up being lost completely when she tries to study in the future which may effect his grade.

It will be hard to try to study something that he didn't understand whilst he was in the classroom.

answer; i believe its   (india); this is the correct answer; /// good luck

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)