Key Formulas & Equations
Core Concepts
Plate Tectonics
Earth's lithosphere is divided into rigid plates that move over the asthenosphere. Divergent boundaries create new crust (mid-ocean ridges); convergent boundaries destroy crust (subduction zones); transform boundaries slide past each other (San Andreas). Driven by mantle convection.
The Rock Cycle
Rocks transform between three types: igneous (cooled magma/lava), sedimentary (compacted sediments), and metamorphic (altered by heat/pressure). Weathering breaks rocks to erosion → deposition → lithification → sedimentary rock. Subduction → melting → igneous rock.
Geologic Time Scale
Earth's 4.6-billion-year history divided into eons, eras, periods, and epochs. Hadean (4.6-4.0 Ga), Archean (4.0-2.5 Ga), Proterozoic (2.5 Ga-541 Ma), Phanerozoic (541 Ma-present). Fossil record, radiometric dating, and stratigraphy establish the timeline.
Mineral Properties
Minerals are naturally occurring inorganic solids with definite chemical composition and crystalline structure. Identified by hardness (Mohs scale), luster, cleavage, fracture, streak, crystal form, specific gravity, and other diagnostic properties.
Seismology & Earth's Interior
Seismic waves reveal Earth's layered structure: crust (5-70 km), mantle (2,900 km), outer core (liquid Fe-Ni, 2,200 km), inner core (solid Fe-Ni, 1,200 km). P-waves travel through solids and liquids; S-waves only through solids. Shadow zones prove the liquid outer core.
Fossils & Stratigraphy
Fossils are preserved remains or traces of ancient life. Principle of superposition: in undisturbed strata, older layers are below younger ones. Index fossils (short-lived, widespread species) correlate rock layers across regions. Unconformities represent gaps in the geologic record.
Worked Examples
Example 1: Radiometric Dating
Problem: A volcanic rock has 25% of original ⁴⁰K remaining. If t₁/₂ = 1.25 billion years, how old is the rock?
Step 1: N/N₀ = (1/2)^(t/t₁/₂) → 0.25 = (1/2)^(t/1.25)
Step 2: 0.25 = (1/2)² → t/1.25 = 2
Step 3: t = 2 × 1.25 = 2.5 billion years
Answer: The rock is 2.5 billion years old.
Example 2: Porosity
Problem: A sandstone sample has total volume 200 cm³ and pore volume 40 cm³. Find the porosity.
Step 1: n = V_voids / V_total × 100%
Step 2: n = 40 / 200 × 100 = 20%
Answer: The porosity is 20%.
Example 3: Plate Velocity
Problem: Magnetic anomalies show oceanic crust 300 km from a ridge is 10 million years old. Find the spreading rate.
Step 1: v = d/t = 300 km / 10,000,000 yr
Step 2: v = 0.03 km/yr = 3 cm/yr
Answer: The seafloor spreads at 3 cm per year on each side of the ridge.
Example 4: Stress Calculation
Problem: A force of 50,000 N acts on a rock cross-section of 2 m². Calculate the stress.
Step 1: σ = F/A = 50,000/2 = 25,000 Pa
Step 2: σ = 25 kPa
Answer: The stress is 25 kilopascals.
Practice Problems
Problem 1
What percentage of a radioactive element remains after 3 half-lives?
Answer: (1/2)³ = 1/8 = 12.5%
Problem 2
A mineral scratches fluorite (hardness 4) but not apatite (hardness 5). What is its Mohs hardness?
Answer: Between 4 and 5 (approximately 4.5)
Problem 3
Calculate the density of a rock sample with mass 270 g and volume 100 cm³.
Answer: ρ = 270/100 = 2.7 g/cm³
Problem 4
A seismic wave travels 1,000 km in 200 seconds. What is its velocity?
Answer: v = 1,000/200 = 5 km/s (typical P-wave in mantle)
Problem 5
What is the specific gravity of quartz with density 2.65 g/cm³?
Answer: SG = 2.65/1.0 = 2.65
Problem 6
A glacier accumulates 5 m of ice/year but melts 3 m/year. What is the net mass balance?
Answer: B = 5 - 3 = +2 m/year (advancing glacier)