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In the Footsteps of St. Finbarre (Part 117) - At the Gates of Fortress Inniscarra E-mail
Written by Kieran McCarthy   
Thursday, 22 May 2008
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In the Footsteps of St. Finbarre (Part 117) - At the Gates of Fortress Inniscarra
Page 2

The demand for electricity continued to rise as the rural electrification project progressed and as more electricity was needed the suitability of the river Lee for a hydro scheme was investigated. The ideal river for a dam is a fast-flowing one with a steep fall like those in Scandinavia or Switzerland. Those types of rivers do not exist in Ireland. For the Lee hydroelectric scheme, a suitable location for a dam was considered. A narrow valley or gorge in a river was sought to build a dam. The right rock structure for foundations is vital. At Inniscarra the old red sandstone cutting supplied that perfectly. A few miles upstream a narrow cutting at Carrigadrohid was another suitable site.

With any civil engineering work, large or small, the physical geography of the place is important. The catchment area of the river Lee provided the impetus and water power for the Lee scheme. It had a good year- round water supply. The Lee above Inniscarra has a catchment area of 790 sq. km (305 sq. m) and an average rainfall of 1500 mm (59.6 ins). The catchment area comprises all the land drained by it and its tributaries. This portion of the Lee catchment area covers approximately 440 square miles (1150 square kilometres). The catchment area, which is more or less rectangular in shape and approximately 30 miles (48 km) long and 14 miles (22.4 km) wide, can be divided up into two well-defined stretches. The first is the highland section from Gougane Barra to near Macroom, the second is the cultivated valley from there to Carrigrohane. The Toon, Sullane, Foherish, Laney, Glaise, Dripsey, Shournagh and the Martin, which are the bulk of the tributaries, drain into the river from the north. While there are many small streams coming from the south, the main tributary here is the Bride. The major drainage from the north is due to the presence of the Derrysaggart and Boggeragh Mountains.

The third requirement is a head of water to power the station. That is determined by the gradient of the river. The river Lee potentially has sufficient gradient but only by backing up the river into large reservoirs. The 45 ft (14 m) fall at Carrigadrohid and the 100 ft (30 m) fall at Inniscarra give an adequate head of water. Minimum disruption of the local community was also deemed important. As much of the Lee valley is steep-sided and confined, it was considered that the loss of land and human habitation would be minimal. Otherwise the cost of disruption would have proved too much. The Lee more or less qualified on all four counts and the decision was made that the river Lee should become Ireland’s fourth major hydroelectric scheme.

To be continued…

Adapted from Kieran McCarthy & Seamus O’Donoghue, forthcoming, Generations, Memories of the Lee Hydroelectric Scheme, County Cork, Lilliput Press, Dublin, An ESB funded publication.


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