A few representative photos of the failed slope are given here showing various aspects of the disaster. The first one shows a Google Earth imagery before the disaster struck the village.
If you look closely at the failed material, there are no large debris which is an indication that it is a loess failure. Anthropogenic activities may be partly responsible for this failure. Though the Afghans
were stunned at this sight, the geological community was not. Shroder et al., 2011 has identified 34 locations of failed loess slopes in NE Afghanistan.
non-porous and on top of that are huge amounts of loess. Loess mostly consists of fine grained material, which is very porous and can be easily eroded. The excess rain and irrigation water makes it soaked and a minor tremor would cause a process called liquefaction where the entire material starts to flow like a
Was it preventable?
Yes, absolutely. We have techniques to stabilize such areas should they affect human settlements, but they are at the bottom of priority list for a developing country like Afghanistan. Fixing
markers on the unstable slope can indicate the villagers that the slope might be failing and they can move to safer locations.
This particular event had very little to do with climate change notoriously known as global warming! As mentioned earlier, irrigation, crop patterns, heavy rains, unstable slopes and undercutting by a stream all contributed to this disaster.
Unfortunately, this is not the end of the ordeal for the tragedy-struck Afghan village. Another potential threat is looming for Ab Barak. The landslide has blocked the drainage around the village and a lake has
started to form as can be seen in the attached photos. This lake can burst any time as there is no active monitoring currently going on. The Afghan government needs to step up to the plate and start paying more attention to protecting its citizens from environmental disasters.
Dr. Asim Yousafzai. No part of this document may be reproduced without permission from the author.