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Location:
Period:
8 Oct 2005 04:13:22 - 12 Oct 2005 08:11:16 (4 days 3 hours 57 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
114
3 swarms found nearby.
2005
PS20051008.1(29.3km)
8 Oct
2 days 6 hours
45 earthquakes
S20051008.2(29.8km)
8 Oct
3 days 11 hours
53 earthquakes
18 Oct
15 hours
6 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20051008.1 Near Battagram, Pakistan

Seismic swarm S20051008.1 was recorded 14 km southeast of Battagram in northern Pakistan. The sequence began at 04:13 on 8 October 2005 and concluded at 08:11 on 12 October 2005, spanning 99 hours and 57 minutes. During this interval, 114 earthquakes were registered.

Analysis of the first 100 events reveals a rapid onset of activity dominated by moderate-magnitude shocks at shallow depths. The initial 24 hours accounted for the majority of stronger events, with magnitudes frequently between 4.4 and 4.9. Depths remained consistently near 10 km for nearly all recorded events, except for one at 7 km. Later phases showed a gradual decline in both frequency and magnitude, transitioning to events mostly below 4.0 by 10 October.

The swarm occurred within the active tectonic setting of the western Himalayas. Northern Pakistan lies at the convergent boundary where the Indian Plate continues to collide with the Eurasian Plate, producing north-directed thrust systems and associated strike-slip faults. The Battagram region sits near the transition between the Main Boundary Thrust and local splays of the Hazara-Kashmir syntaxis, where crustal shortening and uplift generate persistent seismicity.

Historical records indicate that earthquake swarms are uncommon in this sector. Since 1 January 2000, only one swarm has been documented in the area, and that event also occurred in 2005. The 2005 swarm therefore represents the sole swarm-type sequence captured in the modern instrumental catalog for the region.

The shallow focal depths and clustered timing are consistent with fluid migration or stress redistribution along pre-existing faults in a compressional regime. No events exceeded magnitude 5.0, and the sequence did not produce a dominant mainshock-aftershock pattern typical of larger regional earthquakes.

References
SeismoSight internal swarm catalog, Swarm S20051008.1 parameters.
USGS Earthquake Catalog (events 2000–present, northern Pakistan).
Geological Survey of Pakistan, tectonic map of the Hazara region.