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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Indian Peninsula
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India
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Srinagar India (3)
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Jammu and Kashmir
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Jammu (1)
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Kashmir (1)
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Srinagar India (3)
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fossils
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Invertebrata
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Brachiopoda (1)
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Mollusca
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Bivalvia (1)
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microfossils
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geologic age
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Cenozoic
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Quaternary
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Holocene (1)
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Mesozoic
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Triassic
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Lower Triassic
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Permian-Triassic boundary (1)
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Paleozoic
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Permian
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Upper Permian
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Permian-Triassic boundary (1)
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Primary terms
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Asia
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Indian Peninsula
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India
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Srinagar India (3)
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Jammu and Kashmir
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Jammu (1)
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Kashmir (1)
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Srinagar India (3)
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Cenozoic
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Quaternary
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Holocene (1)
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earthquakes (1)
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geophysical methods (1)
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ground water (1)
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Invertebrata
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Brachiopoda (1)
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Mollusca
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Bivalvia (1)
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Mesozoic
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Triassic
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Lower Triassic
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Permian-Triassic boundary (1)
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Paleozoic
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Permian
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Upper Permian
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Permian-Triassic boundary (1)
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sedimentary structures
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seismites (1)
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slope stability (1)
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sedimentary structures
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sedimentary structures
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seismites (1)
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Srinagar India
SHAKEN AND STIRRED: SEISMITES AND TSUNAMITES AT THE PERMIAN-TRIASSIC BOUNDARY, GURYUL RAVINE, KASHMIR, INDIA
Srinagar, the capital city of Kashmir, has been shaken numerous times by earthquakes in the past millennium, most recently by damaging earthquakes in 1885 (M 6.2, 30 km to the west) and 2005 (M 7.6, 200 km to the west) with estimated EMS (European Macroseismic Scale) intensity VI–VII. Earthquakes in Kashmir in earlier historical times are known only from fragmentary archival sources. We present and analyze unique, repeat photographs of the Pandrethan Temple near Srinagar, which we conclude can provide clues to the severity of nineteenth-century earthquakes. Photos taken in 1868 and 1885 and recently show that the temple, a 5.5-m-square masonry-block structure constructed ca. A.D. 920, was undamaged by these two earthquakes. We conclude that displaced blocks visible in the earliest extant photograph are the result of stronger shaking in the past, the most probable causal earthquake being in 1828. Considering the fragility of the structure, we conclude that anything greater than EMS intensity IX would have caused structural collapse. We thus conclude that Pandrethan has not experienced EMS intensity greater than VIII in the past 200 yr, and possibly not in the past millennium.