Technical Adventure Equipment For Climbing Mountaineering

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The high relief of unstable mountains makes Northern Pakistan very weak to intensive landslides when an earthquake strikes the area. Both the MKT and the MMT turn eastward within the Hazara-Kashmir syntaxial bend near the the main Boundary Thrust (MBT), the area of major tectonic plate collision. Most earthquakes in Pakistan happen within the north and western sections of the country along the boundary of the Indian tectonic plate with the Iranian and Afghan micro-plates. A lot of the earthquakes in Pakistan happen within the north and western areas, alongside the boundary of the Indian tectonic plate with the Iranian and Afghan micro-plates. Earthquakes along this explicit fault have been chargeable for considerable destruction prior to now. As indicated, numerous earthquakes happen along the Chaman Fault System. In the northern a part of Pakistan, the Hindu Kush mountains converge with the Karakoram Range, a part of the Himalayan mountain system. The Chaman Thrust Fault system extends along Pakistan's frontier with Afghanistan

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Heavy monsoon rains - notably in the event that they happen before or after an earthquake, might be the catalyst to additional devastating landslides. Secondly, although it does rain quite a lot in the course of the low season, more often than not the rains arrive within the afternoon. The National Disaster Management Committee, chaired by His Excellency Chief Executive Officer, Abdullah Abdullah, held a meeting this afternoon to assemble preliminary harm reports and start coordinating assessments and responses. This earthquake was by far the most destructive disaster in the region. Strong earthquake aftershocks may also trigger additional landslides of unstable mountain slopes and endanger villages in the area. The Ministry of Public Works and the Ministry of Defence have dispatched gear and crews to clear the landslides and restore access to the road network. The earthquake disrupted the cellular network leading to intermittent entry to the mobile network and hampered efforts to acquire info on the impact of the earthquake

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