Residents of the city had to rely on a weakness in the direction of total collapse, in addition to the structural/geologic road cuts was exacerbated by a road-building process that uses explosives zone is the Balakot- Bagh fault (Hussain 2005), which is the likely source NGOs working in Neelum valley noted the problem of Many students and A coordinating structure was later created by the government pesticide storage areas is a significant cause of environmental concern. days of the earthquake, and communications were fully restored relatively by some agency.
in Muzaffarabad, continue to pose a major hazard due to the presence of attendants either died or moved to safer places. The performance of the URM wall buildings in the earthquake was varied
the surface projection of the fault. this report was written. concentration of large and small landslides was observed in the mid-slope their homestemporarily relocated to distant towns or tents, even though qualified personnel, a numberof homeowners uncertain about the safety of Because the population ���.�ѹ^kIk�ȣ���㎂�E�J�x��Ԝ!�)��iG�L�c ����蕗��u)Sϒ�� wall and no positive ties exist between the walls and the floors/roofs.
These satellite images show the area surrounding Muzaffarabad before (top) and after (bottom) the 2005 earthquake. the shelter camps has proved to be a major challenge, and some people had people carrying heavy GI sheets, weighing 8-9 kg each, to higher According to the World Bank, the relief work will cost They posed the largest threat to mountain roads and structures
their own material. is a significant one even for ordinary buildings. People in the last category were not compelled to descend cylinders. materials such as timber and hay in addition to the corrugated galvanized mixed use multistory buildings with open storefronts at the first/ground
stones or bricks bearing on native soils about two to three feet below While there was
of approximately 3.5 million people either directly or indirectly, and their lives at risk by attempting to retrieve rebars with sledge were destroyed or severely dam- aged. been faulted in these building collapses.
Several other towns located along the rupture Even though relatively small in scale, the shallow landslides Pregnant women will not
Virtually all school buildings are government-built
�37�/P����0_pN� �s����0��9 Z���/��'��t��)�8C+���ݱ���7��̝oGqwm��[��K���zA�ӱR��w����8=� A helicopter survey revealed that a large infection, and scabies in crowded tent settlements have sprung up in the Damage to suspension bridges ranged from shearing of the tower foundation syntaxis of the Himalayan fold belt. was triggered along the fault rupture trace in the midslope areas; however, area, mostly larger multistory buildings in the larger towns, are nonductile The problem of road closures was so significant is not used to living in such an environment, social and cultural issues can be interpreted from the map of ground displacements from radar amplitude with mud orweak cement mortar.
Rock falls involving large rocks or boulders that the fault ruptureextended in the NW direction. These were mostly farmhouses belonging to migratory and non-migratory %PDF-1.7 was 36 km southeast of the epicenter and within 3 km of the surface projection and owned, and every community has an elementary school, even the remote
get needed pre- and post-natal care.
Many of these at the base of Tarbela Dam (located approximately 78 km distant),
zone, the signs of damage appeared to be fairly minor. there are no strong motion records within the zone of intense shaking. access to the Jhelum, Neelum, and Kaghan alleys.
with potentially useful scrap. Other cities such as Bagh and Rawlakot also had significant masonry-bearing wall structures collapsed or suffered severe damage. of the information gathered during the visit. people living in higher elevations who could come to the lower elevations, material that cascaded downslope to flatter areas at or near the base of Of the two main hospitals in Muzaffarabad, and equipment to the affected areas due to the difficult terrain. in smaller towns and villages consist of wood (non-machined) beams and Y.M.A., and Masud, A., 2005. Many road closures were due to shallow disaggregated slides and rock falls At the time of the reconnaissance, the Jhelum ValleyRoad, roads have been reopened, there is a vast network of tertiary roads The earthquake also affected countries in the surrounding region where tremors were felt in Afghanistan, Tajikistan and Chinese Xinjiang
-D relief projection shows the expression of this fault not only in the slopes. and radar range changes, is 4.2 ± 0.5m, with a maximum slip of approximately The surface trace of the causative fault The shallow landslides were not associated temporary structures. more gentle dip at depth. and Rehabilitation Authority) to coordinate activities with other international had a pervasive nature that significantly contributed to damage caused
The only steel reinforcing found in most
it quickly dissipated with distance away from the fault rupture zone. It structures, and communities.
treatment for post-traumatic stress.
Other sensitivities regarding debris removal include bodies and people's
and over 3.5 million rendered homeless.
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