August 1886 Charleston Earthquake, USA

1. Status: INSIDE TSW

TSW Window: 1886-08-25T12:53:35Z to 1886-09-02T12:53:35Z

Syzygy Time: 1886-08-29T12:53:35Z

Perigee Time: 1886-08-29T09:00:00Z

Sublunar Latitude: 9.1890481514°

Sublunar Longitude: -13.4356380357°

TSB Lower Latitude: -5.8110°

TSB Upper Latitude: 24.1890°

Radial Stress

Syzygy: 7.9634970776 kPa

Perigee: 7.964682962 kPa

Coulomb Stress

Syzygy: 4.7780982466 kPa

Perigee: 4.7788097772 kPa

Target Faults

Indonesian Arc / Papua New Guinea, Philippine Plate / Mexico / Caribbean/ Red Sea Rift

Alignments

Perigee In Tsw: Yes

Perihelion In Tsw: No

Mars In Tsw: No

Venus In Tsw: Yes

Super Tsw: Yes

Countries in High Seismic Zone

  • Indonesia
  • Ecuador
  • Mexico
  • Brazil
  • Solomon Islands
  • Tiwan
  • Philippines
  • Saudi Arabia
  • Thailand
  • Papua New Guinea
  • Sudan
  • Vietnam

The August 31, 1886, Charleston Earthquake (M_w approx 7.0–7.3) stands as one of the most significant intraplate events in North American history. Our data reveals that this disaster occurred during a Super TSW (Tidal Stress Window) with nearly perfect synchronization between the Moon’s phase and its distance to Earth.

2. The 1886 Super-Alignment

The alignment on the day of the earthquake was exceptionally tight:

  • Syzygy-Perigee Sync: The Moon reached Perigee at 09:00 UTC and Syzygy (New Moon) at 12:53 UTC—a gap of less than 4 hours.
  • Stress Intensity: Our data shows a Coulomb Stress of 4.77 kPa. For a stable continental region like South Carolina, where faults are under constant but slow-moving regional stress, this tidal pulse acted as a potent mechanical trigger.
  • Venus Influence: Our data notes Venus in TSW: Yes. In some planetary-tidal models, the gravitational influence of Venus (Earth’s closest planet) can slightly modulate the Earth-Moon tidal envelope, adding an extra layer of complexity to the stress window.
  • The “Tidal Nudge”: Because intraplate faults accumulate strain very slowly, they can remain at a “critical state” for centuries. Your model suggests that the 7.96 kPa Radial Stress was the decisive force that “unzipped” these ancient buried structures.
  • Caribbean: The shaking from the Charleston quake was so powerful that it was felt clearly in Cuba, which fell within our Tidal Stress Belt (TSB).