Búrfell II Power Station

2018Hydropower

Búrfell II Power Station was commissioned on 2 July 2018 and is located 300 metres underground in Sámsstaðaklif.

Located underground

Búrfell Power Station II contributes up to 300 GWh of renewable electricity annually by improving the utilisation of water resources in the Búrfell hydropower system.

The station is located underground in Sámsstaðaklif and is equipped with a 100 MW Francis turbine. A 370 m headrace canal connects the station to the intake reservoir Bjarnalón, while a 2,200 m tailrace canal returns water to the Fossá river, approximately 1 km downstream from the original Búrfell Power Station.

Water travels from the headrace canal through a 110 m pressure shaft to the turbine before being discharged through the tailrace canal.

Key numbers

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Photos from Búrfell II Power station

The Þjórsá and Tungnaá Area

The Þjórsá and Tungnaá area is home to seven of Landsvirkjun’s hydropower stations: Búðarháls, Búrfell, Búrfell II, Hrauneyjafoss, Sigalda, Sultartangi and Vatnsfell. The area also includes Vaðalda Wind Farm, Iceland’s first wind power plant, as well as Hafið, a wind energy test site with two experimental turbines.

At the heart of the system is Þórisvatn, Iceland’s largest natural lake and the region’s main reservoir. Water collected in the Kvíslaveita diversion system and Hágöngulón flows through Þórisvatn before being used by power stations farther downstream.

The Þórisvatn reservoir system was developed between 1970 and 1972 as part of the expansion of hydropower generation in the area. Its reservoirs, dams, canals and control structures make it possible to store water, regulate flows and optimise energy production throughout the year.

Construction of the Kvíslaveita diversion system began in 1980 and was completed in 1997. The system collects water from tributaries and the upper reaches of the Þjórsá River and diverts it to Þórisvatn.

Hágöngulón was developed between 1997 and 1999 and covers an area of 37 km². It increases the utilisation of water resources in the Kaldakvísl catchment by storing water during the summer months.

Together, Þórisvatn, Kvíslaveita, Hágöngulón and a number of smaller reservoirs form the backbone of the hydropower system in the Þjórsá and Tungnaá area.