Anna is confident in her ability to meet the recommended guidelines for physical activity during the next month despite being busy with a school project. from this statement we can conclude that anna has: a. high self-esteem b. high self-confidence c. high self-efficacy d. high outcome expectations e. all of the above

Option (C) is correct.

Explanation:

From the given case/scenario , we can state that Anna has High self-efficacy. According to Albert Bandura , self-efficacy is referred to as a personal judgment or opinion of, "how well an individual can execute or implement courses of action that are required in order to deal with prospective circumstance". Expectations of ones self-efficacy tends to determine whether one might be able to show coping behavior and how for long these effort are sustained when facing an obstacle.

C. High self-efficacy

Explanation:

Self-efficacy: It defines an individual's belief or faith in their tendency to achieve, whereas, motivation is constructed on the individual's wish to achieve. A person with high self-efficacy mostly considered to have high motivation and vice versa, still not a former conclusion.

Example: A student having a high level of self-efficacy in physics, then the student will feel confident enough to do difficult numerical in physics class.

Sources of self-efficacy:

1. Vicarious experiences.

2. Mastery experiences.

3. Physiological and emotional states.

4. Verbal persuasion.

it continues in business

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)