There are different types of equilibrium in Earth Science:
Static Equilibrium: This occurs when a system is at rest and all the forces acting on it are balanced. For example, a rock sitting on the ground is in static equilibrium because the force of gravity pulling it down is balanced by the normal force exerted by the ground.
Dynamic Equilibrium: In dynamic equilibrium, there is a continuous process of change, but the overall system remains in a state of balance. An example of this is the water cycle, where the rate of evaporation is balanced by the rate of condensation and precipitation.
Review real-world applications of equilibrium, such as the role of dynamic equilibrium in maintaining environmental stability and the impact of chemical equilibrium on industrial processes.
By understanding the concept of equilibrium and its implications in Earth Science, you'll gain a deeper appreciation for the interconnectedness of natural systems and the factors that maintain their balance and stability.