Earth science

Rocks and plate tectonics

Rock cycle, earthquakes, volcanoes, plate boundaries.

Basics

Rock cycle

Igneous: cooled magma. Sedimentary: particles, precipitation, compaction. Metamorphic: recrystallized by heat and pressure. Weathering, erosion, and melting link them.

Plate tectonics

Lithospheric plates move over the asthenosphere. Divergent: rifts and ridges, new crust. Convergent: subduction or collision mountains. Transform: side-by-side slip. Most quakes and volcanoes hug boundaries.

Earthquakes

Elastic rebound: a fault slips. P waves (compressional, faster) then S waves (shear, not through liquid) then surface waves (most damage). Focus is inside; epicenter is above it.

Formulas

Density

ρ = m / V

Crust is lighter than mantle; oceanic (basaltic) crust is denser than continental (granitic) crust.

Symbols

  • ρ density
  • m mass
  • V volume

Moment magnitude (idea)

M_w ∝ log₁₀ (μ A D)

Uses rigidity, fault area, and slip. Better than Richter for large events.

Symbols

  • μ rigidity
  • A fault area
  • D average slip

Key table

Crust Continental ~30–70 km, oceanic ~5–10 km
Age of Earth about 4.54 billion years
Outer core Liquid Fe–Ni — S-wave shadow, geodynamo

In this field