Plate Tectonics: The Earth's outer shell is divided into several large and small plates that float on the semi-fluid asthenosphere. These plates are in constant motion, either moving apart, colliding, or sliding past each other.
Divergent Boundaries: Where plates move away from each other, leading to the formation of new oceanic crust and rift valleys.
Convergent Boundaries: Where plates move towards each other, resulting in subduction zones, volcanic activity, and the formation of mountain ranges.
Transform Boundaries: Where plates slide past each other, causing earthquakes along faults such as the San Andreas Fault in California.
Earthquakes: Sudden shaking of the ground caused by the release of energy along faults. The focus is the point within the Earth where the earthquake starts, while the epicenter is the point on the Earth's surface directly above the focus.
Volcanism: The eruption of molten rock, ash, and gases from the Earth's interior onto the surface. Volcanoes can form at convergent boundaries, divergent boundaries, and hot spots.
Learn about the specific geological features and events associated with each type of plate boundary, including the types of mountains, volcanoes, and seismic activity that occur at each boundary.
Develop and use models to illustrate that energy at the macroscopic scale can be accounted for as either motions of particles or energy stored in fields.