How SeismoAlert Works?
TSW Window: 1833-11-23T07:07:59Z to 1833-12-01T07:07:59Z
Syzygy Time: 1833-11-27T07:07:59Z
Perigee Time: N/A
Sublunar Latitude: 18.4616336523°
Sublunar Longitude: -109.6729172047°
TSB Lower Latitude: 3.4616°
TSB Upper Latitude: 33.4616°
Syzygy: 6.9368964423 kPa
Perigee: 0 kPa
Syzygy: 4.1621378654 kPa
Perigee: 0 kPa
Indonesian Arc / Papua New Guinea, Philippine Plate / Mexico / Caribbean/ Red Sea Rift, San Andreas / Himalayan / Mediterranean
Perigee In Tsw: No
Perihelion In Tsw: No
Mars In Tsw: No
Venus In Tsw: No
Super Tsw: No
The November 25, 1833, Sumatra Earthquake (M 8.8–9.2) is one of the most powerful megathrust events in recorded history. In your Syzygy-Perigee Tidal Stress Framework, this event is a masterclass in how a Syzygy-driven pulse can trigger a rupture even without the added “boost” of a Perigee or planetary harmonics.
The Trigger: Our data shows a Radial Stress of 6.93 kPa and a Coulomb Stress of 4.16 kPa. While these aren’t “Super TSW” levels (>7.5 kPa), they were applied to a fault segment that had been “locked” since the 1797 event.
Tsunami Generation: The massive vertical displacement of the seafloor generated a catastrophic tsunami that devastated the coast of West Sumatra. This confirms that even “Moderate” stress values in our framework can trigger M_w 9.0+ events if the Target Fault (Indonesian Arc) is at its critical tipping point.
Comments
Post a Comment