VOLUME III — 08 — ATLAS / CARTOGRAPHIC

GeologyThe reading of stones

Earth is a layered, slow-cooking heat engine, and the stones at our feet are its receipts. This atlas traces the science of rocks, time, and the moving plates beneath us.

PLATE 01 / 16 — INSIDE EARTH

Onion of the interior.

Earth's interior is known mostly through seismic waves. P-waves (compressional) travel through everything; S-waves (shear) cannot pass through liquids. A near-total S-wave shadow at 103°–142° from a quake locates the molten outer core.

  • Crust0–35 km · oceanic basaltic, continental granitic
  • Lithosphere~100 km · rigid; fragmented into plates
  • Asthenosphere100–410 km · plastic; allows plate motion
  • Mantle410–2,890 km · mostly silicate solid
  • Outer core2,890–5,150 km · molten Fe/Ni · generates B-field
  • Inner core5,150–6,371 km · solid Fe/Ni · ~5,400 K
crust mantle outer core inner core 0–35 km 2,890 km · ~3,400 K
PLATE 02 / 16 — PLATE TECTONICS

The moving crust.

Wegener (1912) noted the puzzle-piece fit of the Atlantic coasts. Hess (1962): the seafloor spreads. Vine, Matthews, Morley (1963): magnetic stripes record reversals. Wilson (1965): transform faults complete the picture.

Today: ~15 major + several dozen minor plates, moving 1–10 cm/yr. Three boundary types — divergent, convergent, transform — generate most of Earth's geological activity.

Three Boundary Types

DIVERGENT (mid-ocean ridge) CONVERGENT (subduction) TRANSFORM (San Andreas)
PLATE 03 / 16 — ROCK CYCLE

How rocks become rocks.

igneous sedimentary metamorphic weathering, transport melting, crystallization heat, pressure heat, pressure
  • Igneouscooled magma — basalt, granite
  • Sedimentaryaccumulated grains — sandstone, limestone, shale
  • Metamorphictransformed by heat & pressure — gneiss, schist, marble

A given mineral grain may visit each compartment several times across hundreds of millions of years. Zircons from Western Australia preserve ages back to 4.4 Ga — older than the oldest known rock.

PLATE 04 / 16 — DEEP TIME

The geologic column.

0 – 2.6 Ma
Quaternary
Pleistocene ice ages; Holocene farming.
2.6 – 66 Ma
Cenozoic
Mammals diversify; grasses; primates; us.
66 – 252 Ma
Mesozoic
Dinosaurs; Pangea breaks up; flowering plants.
252 – 541 Ma
Paleozoic
Cambrian explosion; first land plants; tetrapods.
541 Ma – 2.5 Ga
Proterozoic
Eukaryotes; oxygenation; Snowball Earth episodes.
2.5 – 4.0 Ga
Archean
Earliest stable cratons; chemoautotrophs; cyanobacteria.
4.0 – 4.54 Ga
Hadean
Magma ocean; bombardment; Moon-forming impact.
PLATE 05 / 16 — DATING

How we tell rock ages.

Two strategies: relative (this is older than that) and absolute (this is 2.45 Gyr old).

Relative dating uses superposition (Steno's law), original horizontality, cross-cutting relationships, and inclusions. Reliable for sequence; silent on years.

Absolute dating uses radioactive decay. Different isotopes for different timescales:

  • U-Pb10⁵ – 10⁹ yr (zircons)
  • Ar-Ar10⁵ – 10⁹ yr (volcanic)
  • K-Ar10⁵ – 10⁹ yr (igneous)
  • Rb-Sr10⁷ – 10⁹ yr
  • ¹⁴Cup to ~50,000 yr
  • OSLup to ~500,000 yr (sediments)

Decay law

N(t) = N0 eλt
N₀/2 — half-life N(t) time
FIG. 1
Sedimentary strata.
Geologic strata record Earth's history. The Grand Canyon's exposed layers span 1.8 billion years.
Stratified canyon

PLATE VI

Sedimentary layers expose ~2 Gyr of deposition. Each band tells of a sea, a desert, a delta.

PLATE 07 / 16 — MINERALS

5,800 known minerals.

Quartz

SiO2. Trigonal. Hardness 7. Most abundant in the continental crust.

Feldspar

(K,Na,Ca)AlSi3O8. ~60% of crust by volume.

Olivine

(Mg,Fe)2SiO4. Mantle's main mineral; gem peridot.

Pyroxene

Single-chain silicate; augite, diopside, jadeite.

Mica

Sheet silicate; biotite, muscovite. Perfect cleavage in one plane.

Calcite

CaCO3. Limestone, marble. Rhombohedral cleavage.

Halite

NaCl. Cubic. Evaporite mineral. Sets seasoning.

Diamond

C in cubic close-packing. Hardness 10. Forms ≥150 km depth.

PLATE 08 / 16 — KEY FIGURES

Who read the rocks.

James Hutton

1726–97. Deep time. "No vestige of a beginning, no prospect of an end."

Mary Anning

1799–1847. Lyme Regis fossils; ichthyosaur, plesiosaur, pterosaur.

Charles Lyell

1797–1875. Uniformitarianism in Principles of Geology.

Alfred Wegener

1880–1930. Continental drift, 1912; vindicated decades later.

Inge Lehmann

1888–1993. Discovered the solid inner core via P-wave shadows, 1936.

Marie Tharp

1920–2006. Mapped the global mid-ocean ridge system.

Harry Hess

1906–69. Seafloor spreading, 1962. Trinity-launched the plate revolution.

Walter Alvarez

b. 1940. Ir anomaly; K-Pg impact hypothesis.

Plate_tectonics
PLATE 09 / 16 — TIMELINE OF GEOLOGY

The science itself.

1669

Niels Steno states stratigraphic principles.

1788

Hutton sees Siccar Point's angular unconformity.

1815

William Smith publishes the first geological map of England.

1830

Lyell's Principles — uniformitarianism.

1841

John Phillips coins Paleozoic, Mesozoic, Cenozoic.

1912

Wegener proposes continental drift.

1936

Lehmann's inner-core discovery.

1962

Hess's seafloor spreading paper.

1968

Plate tectonics synthesized — Le Pichon, Morgan, McKenzie.

1980

Alvarez et al. propose K-Pg impact.

2000

Crutzen popularizes "Anthropocene".

2024

Anthropocene formally rejected as epoch by ICS — but accepted as event.

PLATE 10 / 16 — HAZARDS

The earth moves.

Earthquakes

Mw = ⅔ log(M0) − 6.07. Largest recorded: Valdivia, Chile 1960, Mw 9.5. ~500,000 detectable per year.

Volcanoes

VEI 0–8. Tambora 1815 (VEI 7) caused "year without a summer." Yellowstone (VEI 8) last erupted 640 ka.

Tsunamis

Sumatra 2004: ~230,000 dead. Tōhoku 2011: ~20,000. Speed in deep ocean ~700 km/h.

Landslides

Rainfall, seismic shaking, slope angle, lithology. Vajont, Italy, 1963: 2,000+ dead.

Sinkholes / Karst

Dissolution of limestone/dolomite. Florida, Yucatán, China.

Impacts

Tunguska 1908, Chelyabinsk 2013. K-Pg impactor: ~10 km Chicxulub bolide, 66 Ma.

PLATE 11 / 16 — KEY RELATIONS

Quantitative geology.

Geothermal Gradient

dT/dz ≈ 25 °C/km

Surface average. ~15 °C/km in stable cratons; up to ~50 °C/km at ridges.

Gutenberg–Richter

log N = abM

Seismicity scales as power law. b ≈ 1: each unit of M reduces frequency tenfold.

Stokes for Settling

v = (g Δρ d2) / 18η

Grain settling speed in fluid. Sets sorting in sedimentary deposits.

Volcano
PLATE 12 / 16 — PULL QUOTE

"The result, therefore, of our present enquiry is, that we find no vestige of a beginning, no prospect of an end."— James Hutton, Theory of the Earth, 1788

PLATE 13 / 16 — ANTHROPOCENE

The human geological force.

Crutzen and Stoermer popularized "Anthropocene" in 2000. Twenty-three years later, after extensive debate over a candidate Global Boundary Stratotype Section and Point (GSSP), the International Commission on Stratigraphy declined to ratify it as a formal epoch. It survives as a recognized "event."

Either way the signal is unambiguous: ¹⁴C from atomic-bomb testing, plutonium isotopes, plastics, fly ash, novel radionuclides, ratios of nitrogen and phosphorus in soils. Future stratigraphers — if any — will read this layer cleanly.

PLATE 14 / 16 — FRONTIER

What's active now.

Critical minerals

Li, Co, Ni, Cu, REEs for the energy transition. Mapping deposits and recycling closed-loop.

Mantle tomography

Whole-mantle plumes (Iceland, Yellowstone) increasingly visualized. Subducted slabs traced to CMB.

InSAR & GNSS

mm-precision crustal deformation across plate boundaries; transient slow-slip events.

Snowball Earth

Cryogenian glaciations; what triggered onset and termination?

Geoengineering

Enhanced rock weathering as CDR; basalt CO₂ mineralization (CarbFix).

Mars geology

Perseverance, InSight, Tianwen-1: regolith, seismicity, ancient hydrology.

PLATE 15 / 16 — OPEN QUESTIONS

Still unresolved.

PLATE 16 / 16 — GO DEEPER

Watch & read.

PBS Eons & MinuteEarth

Plus the BBC's "Earth Story" with Aubrey Manning (1998) on YouTube — still the best long-form survey.

Watch ↗

References

  • MarshakEarth: Portrait of a Planet
  • StanleyEarth System History
  • McPheeAnnals of the Former World
  • BjornerudTimefulness (2018)
  • USGSNational Geologic Map Database
  • ICSInternational Chronostratigraphic Chart