Claim status
A global empty interior does not match the wave observations
In the record
Modern seismic studies of Earth’s interior
Testable
Direct P and S arrivals across angular distance
Method
Angular distance converted to spherical surface arc
DEEP TIME / CASE FILE

Hollow Earth: a 36° seismic shadow zone

The nominal direct P-wave shadow extends from 104° to 140° from an earthquake: a 36° band, not evidence of an empty planet.

Earthquakes send signals through regions no borehole reaches. Some stations receive strong arrivals while others lie in a shadow. The missing signal is information about the material that changed its path.

Run the calculation
A fossil skull with geological drawings and red investigation threadsEvery thread starts somewhere.
01 / THE CLAIM

An unseen interior is declared empty

Hollow-Earth claims replace the planet’s deep material with a large empty space. Surface caves are real, but a local cavity and a planet-scale void make very different predictions for waves travelling through the interior.

02 / THE CASE

Different waves reveal different materials

Compressional P waves pass through solids and liquids. Shear S waves do not pass through the liquid outer core. The changed wave paths, rather than simply an absent arrival, help identify the core’s physical state.

USGS describes a nominal direct P-wave shadow between angular distances of 104° and 140° from the earthquake. Refraction at the core changes the paths. A station in that band can still record other seismic phases: this is not a claim that its entire seismogram is blank.

Earth’s interior is layered, with crust and mantle over a liquid outer core and a solid inner core. A large central vacuum would need to reproduce the observed transmitted, refracted and reflected signals together, not only point to one missing direct arrival.

03 / THE COMPUTATION

Put the shadow band on a surface-distance scale

For a spherical radius R, an angular separation θ corresponds to a surface arc s = Rθπ/180. The calculator converts the nominal shadow boundaries into kilometres and locates a chosen station by angular distance.

These are distances around the surface from the epicentre, not lengths of the bent paths inside Earth and not predicted arrival times. Move the station control to compare an angle before, within or beyond the direct P-wave shadow. Boundary values are reference markers, not a detailed earthquake travel-time solution.

RUN THE NUMBERS

Locate a station relative to the P-wave shadow

Enter the epicentre-to-station angle. Surface arc distance is not the wave’s underground path length.

Calculation inputs
°

The nominal direct P-wave shadow is between 104° and 140°. Greater angle means greater surface separation.

Epicentre-to-station surface arc13,343km

Surface arc on the mean-radius sphere; not a seismic ray path.

104° shadow boundary11,564 km

Nominal near edge of the direct P-wave shadow.

140° shadow boundary15,567 km

Nominal far edge of the direct P-wave shadow.

Angular width of the shadow band36 °

The difference between the two reference boundary angles.

Working tape
  1. Radius × π ÷ 1806,371.0084 × 0.017453 = 111.195073
  2. Station angle × kilometres per degree120 × 111.195073 = 13,343.40879
  3. Near boundary surface arc104 × 111.195073 = 11,564.287618
  4. Far boundary surface arc140 × 111.195073 = 15,567.310255
  5. Far angle − near angle140 − 104 = 36
  6. Angular width × kilometres per degree36 × 111.195073 = 4,003.022637
04 / THE FINDING

The shadow is a material boundary, not an entrance

The 104°–140° reference interval spans 36° of angular distance. At the selected mean Earth radius it covers roughly 4,003 km of surface arc. The tool places the interval on a scale; the seismic observations supply its physical interpretation.

A missing direct P arrival alone does not prove a void. The pattern across P waves, S waves and other phases supports a differentiated interior and a liquid outer core. It does not support extrapolating small caves into a hollow planet.

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