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A MASSIVE EARTHQUAKE ROCKS PAKISTAN MEASURING 8.1 ON THE RICHTER SCALE

HITS REGION WITH EPICENTER IN AFGHANISTAN — 60KM FROM CHITRAL 

26th October 2015

8.1 EARTHQUAKE ROCKS PAKISTAN
EARTHQUAKE ROCKS PAKISTAN



EARTHQUAKE IN PAKISTAN AND AFGHANISTAN

EARTHQUAKE IN PAKISTAN AND AFGHANISTAN

MASSIVE EARTHQUAKE IN PAKISTAN

MASSIVE EARTHQUAKE IN PAKISTAN

MASSIVE 8.1 EARTHQUAKE IN PAKISTAN

MASSIVE 8.1 EARTHQUAKE IN PAKISTAN




Army chief orders relief measures

EARTHQUAKE IN PAKISTAN



Epicenter

According to the US GeologicalSurvey, an earthquake with magnitude  7.5 occurred at 2.09pm (PST) on Oct 26, 2015. It said the quake was 212.5 km deep and centred 82 km southeast of Feyzabad in a remote area of Afghanistan in the HinduKush mountain range.
8.1 EARTHQUAKE ROCKS PAKISTAN
EARTHQUAKE ROCKS PAKISTAN
The Pakistan Metrological Department said the magnitude of the quake was 8.1.
US Geological Survey has issued a detailed report and some of the excerpts are as follows
“On the north-western side of the Tibetan Plateau, beneath the Pamir-Hindu Kush Mountains of northern Afghanistan, earthquakes occur at depths as great as 200 km as a result of remnant lithospheric subduction. The curved arc of deep earthquakes found in the Hindu Kush Pamir region indicates the presence of a lithospheric body at depth, thought to be remnants of a subducting slab. Cross-sections through the Hindu Kush region suggest a near vertical northerly-dipping subducting slab, whereas cross-sections through the nearby Pamir region to the east indicate a much shallower dipping, southerly subducting slab. Some models suggest the presence of two subduction zones; with the Indian plate being subducted beneath the Hindu Kush region and the Eurasian plate being subducted beneath the Pamir region. However, other models suggest that just one of the two plates is being subducted and that the slab has become contorted and overturned in places.
Shallow crustal earthquakes also occur in this region near the Main Pamir Thrust and other active Quaternary faults. The Main Pamir Thrust, north of the Pamir Mountains, is an active shortening structure. The northern portion of the Main Pamir Thrust produces many shallow earthquakes, whereas its western and eastern borders display a combination of thrust and strike-slip mechanisms. On the 18 February 1911, the M7.4 Sarez earthquake ruptured in the Central Pamir Mountains, killing numerous people and triggering a landside, which blocked the Murghab River.”

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