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Lingza - Ministry of Power

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30<br />

Preliminary Feasibility Report<br />

<strong>Lingza</strong> HE Project (3 x 40 MW)<br />

This water conductor system shall be housed within the rock types <strong>of</strong> gneisses with<br />

occasional bands <strong>of</strong> augen gneisses. A thick band <strong>of</strong> quartzite was observed in vicinity <strong>of</strong><br />

place Be. This band appears to be 150-200m thick. Since the contact between the two is<br />

under a debris its nature could not be ascertained. The gneisses and quartzites are strong<br />

to very strong and are expected to <strong>of</strong>fer a good tunneling media. The rock types trend<br />

NE-SW dipping 40-65º towards NW (Plate-4.1). Sufficient superincumbent cover is<br />

available above the tunnel. Prima-facie no major drainage appears to have deeply incised<br />

the proposed tunnel alignment.<br />

4.3.3 <strong>Power</strong>house<br />

The powerhouse location was fixed keeping in view the FRL <strong>of</strong> Panan Scheme.<br />

Accordingly, it was proposed to keep the tail water above the FRL <strong>of</strong> Panan Scheme. A<br />

foot track runs above the proposed powerhouse location and the present appraisal is<br />

based on the observations made along this foot track. At the proposed powerhouse<br />

location the formation are exposed as steep rocky escarpments. A thick pile <strong>of</strong> slope wash<br />

material occupies the area along the foot track. An underground powerhouse has been<br />

contemplated since steep ridges bind the area. The underground powerhouse area shall be<br />

housed within gneisses, which occupy the area. These trend NE-SW dipping towards NW<br />

(Plate-1). Fair to good rock media is expected during powerhouse excavation. Sufficient<br />

superincumbent cover is available above the proposed powerhouse cavern. The<br />

orientation <strong>of</strong> powerhouse shall be suitably aligned with respect to principal<br />

discontinuity.<br />

4.4 SEISMICITY<br />

The site lies within Zone-IV <strong>of</strong> seismic zoning map <strong>of</strong> India IS 1893 (Part-I) 2002.<br />

Technical report on seismic history and seismicity <strong>of</strong> the teesta basin <strong>of</strong> sikkim covering<br />

proposed sites for hydroelectric schemes has been collected from IMD and enclosed as<br />

annexure 4.2. The report contains a list <strong>of</strong> earthquake events that have occurred within

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