Earth Science Review Bullets
Continental Drift & Plate Tectonics
Alfred Wegener: proposed Continental Drift (continents once in , later split)
Key evidence: matching coastlines, fossil distribution (Glossopteris, Lystrosaurus), glacial striations, coal in polar regions, rock/mountain belts (Caledonian–Appalachian)
Replaced by Plate Tectonics (lithosphere broken into major/minor plates)
Abraham Ortelius: early atlas hinting at continental fit
Seafloor Spreading & Magnetic Reversals
Harry Hess (SONAR mapping) → new oceanic crust forms at mid-ocean ridges, oldest near trenches
Plate Boundaries
Divergent: plates move apart → mid-ocean ridges, rift valleys
Convergent: plates collide → subduction zones, volcanic arcs, mountain ranges
Transform: plates slide past → strike-slip faults (conservative)
Major & Minor Plates (examples)
Pacific (largest), North American, Eurasian, African, Indo-Australian, Antarctic, South American
Minor: Philippine Sea, Nazca, Arabian, Caribbean, Juan de Fuca, Somali
Earth’s Internal Structure
Crust (continental, oceanic)
Mantle: lithosphere (rigid) over asthenosphere (plastic; convection)
Core: outer (liquid Fe-Ni) vs. inner (solid Fe-Ni)
Discontinuities: (crust–mantle), Gutenberg (mantle–outer core), Lehmann (outer–inner core)
Earthquake Basics
Sudden rock rupture along faults; studied by seismology (seismograph)
Focus energy (magnitude: Richter) vs. surface effects (intensity: Mercalli)
Pacific Ring of Fire: belt of quakes & volcanoes
Fault Types
Normal (extension), Reverse/Thrust (compression), Strike-Slip (lateral), Oblique, Horst & Graben blocks
Volcano Classification
Shield: broad, fluid lava (e.g.
)Composite/Stratovolcano: steep, explosive (e.g.
)Cinder Cone: small, single-vent, short-lived
Lava Dome: viscous plug
Activity: Active (erupting/likely), Dormant ( yr silence), Extinct (> yr, no signs)
Weathering, Erosion & Deposition
Physical: temperature changes, frost-wedging, abrasion, biotic action, salt crystallization
Chemical: dissolution, oxidation; forms sediments
Erosion agents: water, wind, gravity, ice, organisms
Deposition: settling of transported material
Endogenic vs. Exogenic Processes
Endogenic (internal): diastrophism, orogeny, epeirogeny, volcanism, plutonism
Exogenic (external): weathering, erosion, mass wasting, driven by solar energy & gravity
Uniformitarianism: present processes = key to past; Catastrophism: sudden, rare events
Hydrosphere & Water Cycle
97.5% ocean (saline water); 2.5% freshwater (1.7 glaciers, 0.77% readily consumable)
Processes: evaporation → condensation → precipitation → runoff/infiltration → storage
Reverse osmosis: desalination method
Biogeochemical Cycles (core points)
Oxygen: produced by photosynthesis (plants, phytoplankton)
Carbon: exchange among atmosphere, biosphere, oceans; human emissions raise carbon dioxide
Geological Time & Supercontinents
Supercontinent sequence: Valbara (3.6 billion years ago), Ur (3.1 billion years ago), Kenorland (2.6 billion years ago), Columbia/Luna (1.8 Billion years ago), Rodinia (1.1 years ago), Pannotia (600-540 million years ago), Pangaea (300 years ago)
Geological Time Scale: eons → eras → periods → epochs; established via stratigraphy & fossil records
Atmosphere Layers (bottom ↑)
Troposphere (weather): Extends from surface to ≈8−15 km≈8−15 km; temperature decreases with altitude from an average of 15∘C15∘C at the surface to −55∘C−55∘C at the tropopause.
Stratosphere (ozone): Extends from ≈15−50 km≈15−50 km
Mesosphere: Extends from ≈50−85 km≈50−85 km
Thermosphere (ionosphere): Extends from ≈85−600 km≈85−600 km
Exosphere: Extends from ≈>600 km≈>600 km outwards
Key Institutions & Tools
PHIVOLCS: monitors Philippine volcanism & earthquakes (est. Sept 17 1984)
SONAR & GPS(Global Positioning System: map seafloor, track plate motion