Environmental Catastrophe Continues in the Affected Areas


Waste dumped unhygienically outside a tented settlement

Flash-floods and Landslides

Landslides caused by the earthquake have temporarily obstructed river channels at many locations. However, between Hattian Bala and Chakaar, a massive landslide has completely blocked the course of the river across two valleys, creating two lakes. The height of the dike created by the slide is approximately 200m. The communities both upstream and downstream of this blockage are threatened by this situation, particularly if it rains and rains heavily. There is also a danger of further landslides in the event of heavy rains and snow. This is especially so during the period of January to March, known for its heavy precipitation. All precaution should be taken to avoid locating relief settlements on mountain slopes as well as sites directly under them. This is because the earth has already loosened due to the massive earthquake and its aftershocks. Ominously, snow and heavy rains would further reduce the gradient at which landslides can occur.


Landslide between Hattian Bala and Chakaar blocking the river

Degradation of Forests and Timber Trade

The need for shelter and fuel for hundreds of thousands of affected people have put the already depleted forests in the region under a great potential threat. But any further degradation of this precious natural resource would drastically reduce the livelihoods options of the local people, increasing their vulnerability. The situation also demands that any timber stocks in the affected areas should be used locally for reconstruction and other related needs. However, in anticipation of imposition of government controls or subsidies, stocked timber is rapidly being transported out of the earthquake affected areas for more profitable marketing elsewhere.

Siltation of Mangla Dam

The landslides caused by the earthquake deposited massive volumes of silt and sediments into the rivers flowing through the affected region. Aftershocks, some of them equivalent to fairly strong earthquakes in their own right, have further added to these seismo-sediments. Rivers Kunhar, Neelum and Jehlum - and their various tributaries – are the most affected by this phenomenon. They are carrying this load downstream to the Mangla reservoir, greatly increasing the risk of silting this already silted dam, and reducing the life and capacity of this reservoir. A project for increasing the capacity of the reservoir has been in the planning phase. In view of current hazards, the technical feasibility may need to be reviewed and revised.




Conventional reconstruction from timber
 


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