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Copyright Information: All images are in the public domain and available for free. If you use this image, credit NOAA/NGDC, M. Mehrain, Dames and Moore. |
Typical major damage to buildings with many unreinforced shear walls. Note "X-cracking". Unreinforced hollow or solid brick masonry infill, extensively used in Iranian buildings, performed poorly during this earthquake. In Rasht, sixty kilometers from the epicenter, the buildings incurred widespread damage due to such unreinforced masonry sheer walls. However, two thick solid unreinforced masonry walls were placed at the opposite ends of some mid-rise buildings in Rasht. These walls acted as shear-resisting elements and appeared to have improved the overall performance of the buildings. Image Credit: M. Mehrain. Dames and Moore June 20, 1990 Northern Iran earthquake A magnitude 7.7 earthquake occurred in the Gilan Province between the towns of Rudbar and Manjil in northern Iran on Thursday, June 21, 1990 (June 20 at 21:00 GMT). The event, the largest ever to be recorded in that part of the Caspian Sea region, may have been composed of two or more closely-spaced earthquakes occurring in rapid succession. These quakes, exceptionally close to the surface for this region, were also unusually destructive. Event Data:
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