Fifty-three percent (53%) of the total number of slides here occurred on 25% to 50% or 14° - 27° slope (Fig. Washington D.C.: National Press Academy. In these communities, the leaders also reported that persons whom they did not know even procured relief by using their names. This triangular shaped building occupied a prime corner site on Session Road and had reasonably regular stiffness except for two floors at the lower end. Bulletin NZ National Society for Earthquake Engineering. These were being operated and maintained by the National Power Corporation (NPC). The need for such measures has long been felt because of the high vulnerability of the Country to natural disaster. But to a certain extent, the propensity to ask assistance was determined by the impact the earthquake had on the physical assets of the households.

Bulletin of the New Zealand National Society for Earthquake Engineering: 9(1).Amin, E., R. Tabanlar, and F. delos Reyes, 1990, Earthquake Information Bulletin No. Earthquake-related effects ranged from fissuring of rice fields, landsliding that dammed rivers, and river-flooding of settlement areas.

The average is for the full 20 meters deep borehole. The following morning, his dogs howled and his pigs became restless. Those who have relatives in Baguio City can still recall the fear and the anxiety of not knowing what happened to their loved ones because of broken communication lines. Ceres . Afterwards, uncooked food was simply distributed to the individual households through a certain system. The interview schedule had to be edited twice to include a list of specific set of domestic and non domesticates which the subject is made to specifically respond to. (1991), there are two main segments the Philippine Fault - central section from Bondoc peninsula to Mindanao and the northern segment. July 1.9, 1.990.Rescue proceeds slowly. for seven consecutive days before the quake. Lasting images of the earthquake. The much publicized efficiency and managerial skills of NGOs have also been put to question by the miscarriage of some projects assigned to NGOs recently.A cursory review of the composition, leadership and actions of the NGOs that have been emerging lately reveals the growing influence of the elite and vested interest groups, belying the claim that NGOs embody or articulate popular/mass sentiment or will.


Generally, the graphs indicate an approximate value of less, than 10 MPa for depths not greater than 10 meters in the damaged areas, except in La UDi0n w where there are values way above the approximate value for certain depths. But verbal reports of the building motion in previous earthquakes suggested a marked torsional response. The communities who managed to have these resources were less dependent on external assistance. Rescue and recovery work especially in earthquake-caused disasters, likewise require special skills. The first observations start with a high frequency at seven days before the earthquake. Some of the relief goods from Cagayan were transported by land direct to Aritao.In Dagupan City, the immediate need was water. Contact with local consultants and government engineers has provided further insights into the effects of the earthquake and the key issues faced in the design and construction of seismic resistant buildings and infrastructure.There is much to be gained by sharing and discussing the effects of the July 16 Earthquake, and it is hoped that the following observations will assist in providing buildings and infrastructure of increasingly better seismic performance.The range of types of damage and its widespread geographic location is indicated by the following.Baguio suffered major losses to buildings, especially hotels.Dagupan lost a key bridge and many buildings subsided due to liquefaction of foundation soils.Major roads in the mountain regions were devastated by landslip which exposed slopes to subsequent rains.Roads on the plains were extensively damaged by liquefaction.Many bridges on national, provincial and barangay roads were damaged due to landslip and liquefaction.Hundreds of schools and hospitals over a wide area were damaged or destroyed due to ground shaking,liquefaction and ground subsidence.Several areas suffered damage directly attributable to fault movement, particularly to roads.Damage to natural environment was substantial. Because of its non repetitive nature, the event could easily pass unnoticed. Province and Pantabangan (PEP), Nueva Ecija (Figure 4).Being an international concern, the international geoscientific community sent several Maps to conduct aftershock monitoring and studies. Hence, we send out at least 20 in each team.


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