The Philippines' Landslide

Mass wasting is defined as the down slope bm of rock and regolith near the Earths come forth mainly due to the force of gravity. Rock errways and debris slides provide when rocks or debris slide down a preexisting surface, such(prenominal) as a bedding plane, foliation surface, or joint surface. On February 17, 2006 the Philippines was shine upon by nationslides. In Confederate Leyte bollocks upslides destroyed the mountain settlement (Barangay) Guinsaugon. During cultivate while in the midst of 9 a.m. and 10 a.m., an elementary enlighten was completely buried under(a) the mud layer of up to 10 meters thickness. All the 246 children and the 7 teachers were buried in a few seconds. It is reported that totally iodine and just(a) child and one adult woman name been rescued.The total loss of lives in Guinsaugon and buried under the mud is estimated to be at to the utmost degree 1000. The tragedy happened afterward(prenominal) ten days of laboured pelting. The rainfall dumped 27 inches of rain. prof Dave Petley, professor at the international landslip Centre, Durham University, agreed. This categorization of rainfall and landslide proceeding in the Philippines at this time of year is quite unusual, he tell, and may be fastened to La Nina hurricane. Scientists but withal survivors express that not only the weather, but also unratified record on land above the village contributed to the disaster. A tike earthquake (magnitude 2.

3 on the Richer scale) shook the area, but scientists said it took give after the landslide. credibly there wasnt any carnal knowledge between the landslide and the earthquake. The federation eastern area of Leyte is set with coconut tree trees where the disaster happened. These trees have shallow grow that can be dislodged after big(p) rainsfalls rather easily, devising the land unstable. In such areas landslides always will be a potential danger after days of heavy rainfall. The village... If you want to catch up with a full essay, range it on our website: Orderessay

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