A series of destructive earthquakes strikes northwestern Afghanistan: GFZ

10/10/2023 Worldwide Earthquakes Topic 3: Ruhelose Erde │GFZ Pressemitteilung PM_2023 Slider

First analyses of satellite and GEOFON data give insights into the processes around the Herat fault, a region that is considered to be seismically rather inactive.

Earthquake area northwest of Herat in northwest Afghanistan. InSAR satellite data are shown: Radar interferometry can be used to record deformations of the earth's surface. Particularly strong changes (ring patterns) are shown where the earthquake centres are (dots). (GFZ/Kakar)

Map of northwestern Afghanistan around the earthquake area northwest of Herat. Deformations of the Earth's surface are shown in bright colours: blue areas mark elevation by several ten cm, red areas mark lowering by several ten cm. Dots mark the earthquake centres. Smaller pic inside shows the faults in Afghanistan and the more active region in the eastern part of the country. — Earthquake area northwest of Herat in northwest Afghanistan. Calculated deformation of the region from measured satellite radar interferometry data: In blue – elevation by several ten cm (= lower distance to the satellite). In red – lowering by several ten cm (= growing distance to the satellite). Smaller pic inside shows the faults in Afghanistan and the more active region in the eastern part of the country. *(Graphic: Kakar, GFZ)*

Right: Set-up of GPS-Infrastructure in the eastern part of Afghanistan by GFZ scientists in 2014/15 as part of the GFZ’s Central Asian Global Change Observatory. Left: GFZ-scientists teach their Afghan colleagues how to operate the stations. — Setting-up GPS-Infrastructure in the eastern part of Afghanistan by GFZ scientists in 2014/15 as part of the GFZ’s Central Asian Global Change Observatory. Those instruments are used to detect Earth surface movements in the range of cm. The data of these stations were used for the publications on the subducted slab. GFZ-scientists teach their afghan colleagues how to operate the stations. *(Photos: Kakar, GFZ)*

First analyses of satellite and GEOFON data give insights into the processes around the Herat fault, a region that is considered to be seismically rather inactive.

Update: 16. October 2023)

A series of major earthquakes has shaken northwestern Afghanistan, a region where so far no large quakes have been detected. On Saturday, October 7, two destructive earthquakes occurred ~30 km NW of the Afghan town Herat with magnitudes of 6.2 and 6.3 (geofon.gfz-potsdam.de), at 11:11 am and 11:43 am local time in Afghanistan (6:41 and 7:13 UTC) and at a depth of only about 10 km. Earthquakes at such shallow depths can have particularly devastating effects.

Herat is the second largest city in the country after Kabul. Local agencies claim at least 2000 casualties (dpa, ZEIT), and thousands more injured people. According to the WHO at least 600 houses in thirteen Afghan villages were destroyed.

In the early morning of 11 October at 5:11 a.m. local time (0:41 UTC), the third strong quake within a few days occurred about 10 kilometres west of the previous epicentres, and a fourth on 15 October at 8:06 a.m. local time (3:36 UTC) north of Herat, both with a magnitude of 6.3 at a depth of about 10 kilometres.

First major earthquakes in this region for centuries

These were the first large earthquakes (M > 4,5) which have been detected in that region since official data are available at around 1900. In contrast to the east of the country which regularly experiences larger quakes – most recently last summer, the northwest is considered seismically largely inactive: There are no historical proofs of similarly devastating events in the region for centuries.

More aftershocks to be expected

In addition to the main shocks, the GEOFON monitoring service detected 20 aftershocks with M ≥ 4.3 so far (16.10., 17:40 UTC), 12 of them in the first two days after the first event. In addition, many smaller earthquakes could have been felt in the area. Seismic activity can be expected to remain elevated for at least several weeks.

Rupture in the Herat Fault System

Our preliminary analysis of seismic and satellite-geodetic data (radar satellite interferometry, InSAR) reveal that the earthquakes ruptured a 10-20 km-long western segment of the ~700 km-long Herat fault system that traverses the Hindu Kush Mountain range from West to East. And the region around the epicentre has risen by about 40 cm in an area of about 20 km x 30 km.

The Hindu Kush is part of the Alpine-Himalayan Mountain belt and located to the west of the Himalayan Mountain range. It has been built by the pressures exerted due to the Indian plate bulldozing northward into the Eurasian plate.

Analysis of the four main shocks suggests that these earthquakes are thrust events with approximately east-west strikes, which accommodate north-south shortening.

Need for further scientific studies on the region – though with only sparse observational opportunities available

The recent seismic activity underscores the critical need for a thorough scientific study in the region, given its rarity. The analysis of the earthquakes benefited from a seismic station in Kabul, which is part of the GFZ’s GEOFON network and part of GFZ’s Global Change Observatory Central Asia, the latter focusing on Earth-related hazards. However, our in-situ observations are sparse in this region due to the long-term political unrest in the region: there is a limited number of seismic station and no additional GNSS-satellite measurements at all at the western end of the Herat fault. This poses a significant challenge in accurately modelling these Afghan earthquakes and drawing reliable conclusions.

Background: seismically active and inactive regions in Afghanistan

The Herat fault is considered to be seismically inactive. Background seismicity focuses along the foothills of the Hindu Kush (USGS). Near Herat, in the western foothills of the Hindu Kush, only a few smaller M 4 earthquakes occur roughly every 10 years.

But crustal seismicity increases where the eastern Hindu Kush connects to the tectonically highly active Pamir mountains. Together with our GFZ seismologists we recently reported an ongoing break-off of the subducted slab (Kufner et al., 2021). In consequence, crossing the eastern Hindu Kush from South to North, westward crustal motion increases by ~10 mm/yr (Kufner et al., 2020), with crustal strain distributed across the whole orogen.

What drives the current quake in detail remains an open question so far

In general, the western part of the Hindu Kush is accumulating less seismic strain than the eastern part, because of the increasing distance to the active plate-boundary and the ongoing slab break-off.

However, this should not be taken as a fact to imply that large events could not occur along the Herat fault. This giant fault has a very distinct morphologic (topographic) expression and, in geologic times, must clearly have played an important role. The fact that the western segment of it was inactive for the last thousand years does not fully exclude the occurrence of future large earthquakes – as we could observe now (Ambraseys and Bilham, 2003).

Text by N. Kakar (Section 1.2), S. Metzger (Section 4.1), T. Schöne (Section 1.2), F. Tilmann (Section 2.4), J. Saul (Section 2.4), P. Büyükakpınar (Section 2.1).

Edited by Uta Deffke

Information sources:

GEOFON earthquake monitoring:

https://geofon.gfz-potsdam.de

Central Asian Fault data base:
esdynamics.geo.uni-tuebingen.de/faults
Mohadjer, S., Ehlers, T.A., Bendick, R., Stübner, K., Strube, T.: A Quaternary fault database for central Asia, Nat. Hazards Earth Syst. Sci., 16, 529-542, 2016. doi:10.5194/nhess-16-529-2016

Herat fault information:

Nicholas Ambraseys, Roger Bilham; Earthquakes in Afghanistan. Seismological Research Letters 2003; 74 (2): 107–123. doi: 10.1785/gssrl.74.2.107

GFZ publication on slab-break off:

Kufner, S.-K., Kakar, N., Bezada, M., Bloch, W., Metzger, S., Yuan, X., Mechie, J., Ratschbacher, L., Murodkulov, Sh., Deng, Z., Schurr, B. (2021), The Hindu Kush slab break-off as revealed by deep structure and crustal deformation, Nature Comm., 12, 1685. doi:10.1038/s41467-021-21760-w (open access)