Egypt Seismic Intelligence | 3D Global Earthquake Telemetry & Impact Model

Tectonic Plates

Wavefronts

Terrain Mesh

NRIAG Stations

Cities & Heatmap

Graticule

Rupture Telemetry PROPAGATING

Magnitude (Mw)

6.2 Mw

Focal Depth

45.0 km

Epicenter Coords

35.12°N, 26.85°E

Tectonic Source

Hellenic Arc

Mechanism: African Plate oceanic crust plunging beneath the Aegean microplate. Deep focal depth allows long-period waves to traverse the Mediterranean basin efficiently into Egypt.

HELWAN (HLW) // VERTICAL (Z) PRE-ARRIVAL

0.0s P-Arrival (--s) S-Arrival (--s) 300s

Egyptian Impact Matrix NRIAG NETWORK

LOCATION	DIST	P-ARR	S-ARR	INTENSITY

Why Cairo & Delta Feel Mediterranean Shocks: Thick soft alluvium clay and deep sedimentary basin in the Nile Valley act as a natural acoustic resonator, amplifying low-frequency seismic shear waves and trapping surface waves, which causes tall buildings in Cairo to sway noticeably even from 600-800 km away.

TIME SINCE RUPTURE: 00:00.0 s P-WAVE: 0 km | S-WAVE: 0 km STATE: EXPANDING

P-Wave (8.0 km/s)

S-Wave (4.5 km/s)

Surface (3.5 km/s)