U2 Key Terms
Lesson 2.1.1 Development of Plate Tectonic Theory
Plate Tectonics
Seismology
Volcanology
Topography
Lithosphere
Gravity Anomaly
Ridge Push
Slab Pull
Mantle Convection
Asthenosphere
Continental Drift
Theory
Anomaly
Lesson 2.1.2 Seafloor Spreading
Divergence
Seafloor Spreading
Trench
Topography
Mid-Ocean Ridge
Rift
Lesson 2.1.3 Convergent Margins
Subductions
Hypocenter/Focus
Island Arc
Earthquake
Epicenter
Convergence
Oceanic Trench
Orogeny
Lesson 2.1.4 Hot Spot and Transform Boundaries
Hotspot
Rift
Volcanology
Strike-and-Slip Fault
Obsidian
Mantle Plume
Transform Fault
Lesson 2.2.1 Deformation & Metamorphism
Anticline
Axial Plane
Brittle Deformation
Ductile Deformation
Fault
Fold
Normal Fault
Reverse Fault
Syncline
Lesson 2.2.2 Earthquakes
Earthquake
Epicenter
Focus
Seismograph
Mercalli
Richter
Rupture
Magnitude
Triangulation
Liquefaction
Surface Waves
Lesson 2.2.3 Volcanos
Eruption
Lahar
Lava flow
Composite Volcano
Tephra
Tsunami
Volcano
Rupture
Shield Volcano
Supervolcano
Pyroclastic Flow
Stratovolcano
Lesson 2.1.1 Development of Plate Tectonic Theory
Plate Tectonics
Seismology
Volcanology
Topography
Lithosphere
Gravity Anomaly
Ridge Push
Slab Pull
Mantle Convection
Asthenosphere
Continental Drift
Theory
Anomaly
Lesson 2.1.2 Seafloor Spreading
Divergence
Seafloor Spreading
Trench
Topography
Mid-Ocean Ridge
Rift
Lesson 2.1.3 Convergent Margins
Subductions
Hypocenter/Focus
Island Arc
Earthquake
Epicenter
Convergence
Oceanic Trench
Orogeny
Lesson 2.1.4 Hot Spot and Transform Boundaries
Hotspot
Rift
Volcanology
Strike-and-Slip Fault
Obsidian
Mantle Plume
Transform Fault
Lesson 2.2.1 Deformation & Metamorphism
Anticline
Axial Plane
Brittle Deformation
Ductile Deformation
Fault
Fold
Normal Fault
Reverse Fault
Syncline
Lesson 2.2.2 Earthquakes
Earthquake
Epicenter
Focus
Seismograph
Mercalli
Richter
Rupture
Magnitude
Triangulation
Liquefaction
Surface Waves
Lesson 2.2.3 Volcanos
Eruption
Lahar
Lava flow
Composite Volcano
Tephra
Tsunami
Volcano
Rupture
Shield Volcano
Supervolcano
Pyroclastic Flow
Stratovolcano