Rather than get mad at her roommate for spending too much time in the bathroom, Anita decided to come up with some ideas so each of them can use the bathroom when they need to. Anita’s conflict management style would be described as .

cooperative

Explanation:Conflict management is the process for handling disputes and disagreements between two or multiple parties. The goal of this system is to minimize the negative factors that are influencing the conflict and encourage all participants to come to an agreement. Successful conflict management results in a mutually beneficial outcome that's agreed upon by each party.

conflict is a normal and natural part of any workplace, it can lead to absenteeism, lost productivity, and mental health issues. At the same time, conflict can be a motivator that generates new ideas and innovation as well as leads to increased flexibility and a better understanding of working relationships.

Cooperative conflict systems (sometimes also termed mutual gains, interest-based, and win/win) are grounded in a win/win or positive mutual outcome perspective--for one party to win the other party's needs and goals must also be considered, with the net result that both parties maximize their outcomes.

cooperative.

Explanation:

The way people deals with conflicts or disagreements are different and I must say having a good conflict management style is one of the traits or qualities of good leadership.

How people solve conflicts cases or disagreements are based on several factors that are reasonable to them. One of the conflicts management style that was introduced by Lewin is the Cooperative management styles.

Simply put, cooperative management styles is a kind of solving disagreement based on mutual agreement. Anita deciding to give out some ideas so each of them can use the bathroom when they need to is a kind of cooperative management style.

a is the final ! : )

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)