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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Kashmir earthquake 1885
Revisiting Two Damaging Indian Earthquakes of 1885: Kashmir and Bengal Available to Purchase
Damage due to 30 May 1885 Kashmir earthquake. a) Damaged Durbar Rooms, Sher... Available to Purchase
Isoseismal Map in MSK-64 scale of 30 May 1885 Kashmir earthquake. MBT- Main... Available to Purchase
(a) Pre‐1885 Kashmir earthquake picture of the southeast corner of the Sank... Available to Purchase
(a) Pre‐1885 Kashmir earthquake picture ( Cole, 1869 ) and (b) a recent pho... Available to Purchase
(a) Pre‐1885 Kashmir earthquake picture ( Cole, 1869 ) and (b) a present ph... Available to Purchase
(a) Pre‐1885 Kashmir earthquake photograph ( Cole, 1869 ) and (b) a present... Available to Purchase
(a) Pre‐1885 Kashmir earthquake photograph ( Cole, 1869 ) and (b) a present... Available to Purchase
(a) Pre‐1885 Kashmir earthquake photograph ( Cole, 1869 ) and (b) a present... Available to Purchase
The Ancient Temples of Kashmir Turned from Marvel to Ruin by Earthquakes? A Case Study of the Pattan Twin Temples (A.D. 883–902) Available to Purchase
Historical earthquakes in Srinagar, Kashmir: Clues from the Shiva Temple at Pandrethan Available to Purchase
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.