Final answer:
The Plate Tectonics lab explores the interactions and geologic events at convergent, divergent, and transform plate boundaries, which are crucial in shaping Earth's surface.
Step-by-step explanation:
Objective of the Plate Tectonics Lab
The purpose of the Plate Tectonics lab is to investigate interactions between continental and oceanic plates at convergent, divergent, and transform boundaries. These interactions are studied to understand the geologic events that occur at different types of plate boundaries and how they have shaped Earth's surface over millions of years.
Hypothesis Predictions
For Location One, at a convergent boundary between two continental plates, it is predicted that earthquakes and mountains will be observed. At Location Two, a divergent boundary between continental plates, earthquakes, faults, and seafloor spreading are expected. For Location Three, at a transform boundary between continental plates, earthquakes and faults are anticipated. In the case of oceanic plates at a convergent boundary (Location Four), earthquakes and island chains may occur. At a divergent boundary between oceanic plates (Location Five), earthquakes, volcanoes, and seafloor spreading can be predicted. Location Six, with oceanic plates at a transform boundary, is expected to showcase earthquakes and faults.
Test and Outcome Variables
Test variable (independent variable): Type of plate boundary (convergent, divergent, transform)
Outcome variable (dependent variable): Geologic events observed (earthquakes, faults, seafloor spreading, etc.)
Conclusion of Plate Tectonics Lab
Divergent boundaries are typically associated with seafloor spreading, earthquakes, and occasional volcanic activity. Convergent boundaries can show a wide array of features including mountain formation, creation of volcanic island arcs, and various earthquake depths. Transform boundaries are characterized by earthquakes occurring as the plates slide past one another.
These tectonic interactions have also caused significant changes to Earth's topography over millions of years, shaping the mountains, oceans, and landforms we see today.