The surface level of the Hálslón Reservoir is now 625 metres above sea level. The reservoir surface level has increased by over 2 metres in the last 7 days and is expected to reach the ‘spillover’ level by this coming weekend; three weeks later than last year.
When the water level reaches the spillover level it creates the waterfall Hverfandi at the western end of the Kárahnjúka Dam, rushing down to the gorge rim and then surging downward 90-100 metres into the Hafrahvammagljúfur Gorge. The waterfall is powerful and can become more water rich than Dettifoss.
The cold spring experienced this year, especially in the north and east of the country, resulted in the delay of spring floods. The flow rate in the south of the country has been below average this summer: Þórisvatn is 5 metres below its top level and the Blanda Reservoir is 2.5 metres below its top level. Landsvirkjun does not expect these reservoirs to reach their top level this autumn. This situation has not affected Landsvirkjun’s energy supply this winter and will be further assessed when the drawdown of reservoirs is executed this autumn.
The flow rate to Landsvirkjun’s reservoirs is reliant upon changing weather conditions and it is therefore natural for the reservoirs not to reach their top level every year.
Hálslón Spillover 2007-2012 |
Year Date |
2012 7th of August |
2011 13th of September |
2010 28th of July |
2009 9th of September |
2008 16th of August |
2007 18th of October |