The Interior of the Earth
Eugene C. Robertson
Explains for a general audience how seismic waves, heat flow and meteorite composition combine as indirect evidence for a layered Earth of crust, mantle and core.
link checked 17 Sept 2026The physics of the planet's interior and its fields.
8 topics · 10 curated works
No prior grounding assumed.
The Interior of the Earth
Eugene C. Robertson · 1966
Explains for a general audience how seismic waves, heat flow and meteorite composition combine as indirect evidence for a layered Earth of crust,…
+1 more at this level
Assumes you know the vocabulary.
Assessment of Geothermal Resources of the United States: 1978
L. J. Patrick Muffler · 1979
Categorises the country's geothermal energy by system type and temperature and estimates how much of it could actually reach the surface, the…
+1 more at this level
Primary sources and full treatments.
General Theory of Terrestrial Magnetism
Carl Friedrich Gauss · 1839
Applies spherical-harmonic analysis to global magnetic observations to show the Earth's field is generated internally rather than by external…
+5 more at this level
10 works
Eugene C. Robertson
Explains for a general audience how seismic waves, heat flow and meteorite composition combine as indirect evidence for a layered Earth of crust, mantle and core.
link checked 17 Sept 2026W. Jacquelyne Kious & Robert I. Tilling
Walks a general reader through the evidence — matching coastlines, magnetic stripes, earthquake belts — that persuaded geologists to accept moving plates within a single working generation.
link checked 17 Sept 2026L. J. Patrick Muffler
Categorises the country's geothermal energy by system type and temperature and estimates how much of it could actually reach the surface, the baseline resource assessment US geothermal policy still cites.
link checked 17 Sept 2026Christopher Jackson (The Royal Institution)
Shows that seismic imaging lets geologists map the magma plumbing beneath a volcano, so eruption behaviour can be read from subsurface structure rather than inferred from the surface alone.
link checked 17 Sept 2026Carl Friedrich Gauss
Applies spherical-harmonic analysis to global magnetic observations to show the Earth's field is generated internally rather than by external sources, founding geomagnetism as a mathematical science.
link checked 17 Sept 2026George Biddell Airy
Proposes that mountains are compensated by lower-density root material beneath them, explaining gravimetric anomalies unaccounted for by visible topography and founding the theory of isostasy.
link checked 17 Sept 2026Arthur Holmes
Proposes that heat from radioactive decay drives slow convection currents in the mantle, giving continental drift a physical engine three decades before plate tectonics was accepted.
link checked 17 Sept 2026Charles F. Richter
Defines earthquake size as the logarithm of the maximum trace amplitude on a standard seismometer at a fixed distance, turning a qualitative sense of an earthquake's strength into a single reproducible number.
link checked 17 Sept 2026William A. Heiskanen & Helmut Moritz
Formalises the mathematical relationship between gravity measurements and the Earth's true shape, becoming the standard reference for computing geoid models from gravimetric data.
link checked 17 Sept 2026Adam M. Dziewonski & Don L. Anderson
Fits a single set of density, seismic-velocity and attenuation profiles to a huge compilation of seismic and mass and moment-of-inertia data, giving seismology a standard reference model of Earth's interior still used as the baseline today.
link checked 17 Sept 2026