Many college students study by simply repeating their notes over and over (rote rehearsal). Although this method is good for processing data into STM there are other means to effectively move material into LTM. Make sure to read the How To Study Effectively section in Chapter 8. Now, in one to two paragraphs discuss how you currently prepare for exams and how you might incorporate 4 additional techniques that are discussed in the text to your studying behavior.

Expand the scope of study to other methods

Explanation:

In some cases memorization is important for some subjects that involve how a process works. Many undergraduate studies will encourage memorization in tests for this reason but it is also important to exercise application.  Some additional tips for studying other than simple memorization are:

1. Do practice questions at the end of the chapter

2. Read additional material that is not a part of the class notes but is relevant to the chapter

3. Write a paragraph on all the the points that you picked up and cross check this with your notes

4. Engage in a discussion with people in the field to have a deeper knowledge or just a different perspective

IN conjunction with memorization and study groups these suggestions will greatly boost one's study strategies.

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)

the answer is d.index