LAKES IN RELATION TO GEOLOGICAL FEATURES 493 
Chuilinn^ a' (Conon basin). — Vol. II. Part I. p. 289. 
Clair (Ewe basin).— Vol II. Part I. p. 240. 
Claise Fearna, na. — Rock-basin in Lewisian Gneiss. 
Clickhimin.— Drift-dammed in hollow of Old Red Sandstone. 
Cliff. — Ponded by gravel at the margin of the present beach. 
Clings Water. — Rock-basin in altered Old Red Sandstone strata, partly 
drift-dammed. 
Clousta. — Resting partly on Old Red Sandstone and partly on drift. 
Clubbi Shuns. — Small rock-basin in granite of Roeness Hill^ Shetland. 
Clunie (Ness basin). — Valley rock-basin in schists and granite ; simple 
U-shaped basin with irregular sides strewn with moraines. 
Clunie (Tay basin). — Small shallow lake ponded by drift. 
CoiNNiCH^ NA. — Ponded by drift. 
Coir' an Fhearna. — ^Rock-basin along strike of crystalline schists in valley 
open at both ends^ which drained part of the ice from Central 
Sutherland (see Loch a' Bhealaich). 
Coire NAM Meann. — Rock-basin in Moine schists. 
CoLLASTER. — Partly on rock and partly in drift, 
Cornish. — Ponded by drift in hollow near the edge of the Loch Doon 
granite mass. 
CouLiN (Ewe basin).— Vol. II. Part I. p. 240. 
Craggie (Oykell). — Rock-basin in Moine schists. 
Craige^ na. — Small drift-dammed loch lying on crystalline schists. 
Crann.— Vol. II. Part I. p. 289. 
Craobhaig, na. — Rock-basin in Lewisian Gneiss. 
Creagach.— Vol. II. Part I. p. 329- 
Creige Leithe, na. — Rock-basin in Lewisian Gneiss separated by a bar 
of stones from Loch nan Garbh Chlachan. 
Cro Criosdaig. — Rock-basin in Lewisian Gneiss. 
Crocach.— Vol. II. Part I. p. 188. 
Crogavat. — Rock-basin in Lewisian Gneiss. 
Crombie Den. — Artificial reservoir in hollow cut out of boulder clay and 
Lower Old Red strata by stream. 
Crunachan. — Remnant of a loch in drift nearly silted up. 
CuAiCH^ NA. — Rock-basin in Moine schists. 
CuiL AiRiDH a' Flod. — Rock-basin in Lewisian Gneiss. 
CuiL NA SiTHE. — Ponded by drift. 
Cuinne^ NAN. — Hollow in drift resting on Moine schists. 
Cults. — Kettle-hole in fluvio-glacial deposits of 100-ft. raised beach. 
Daimh^ AN (Shin basin). — Vol. II. Part I. p. 307. 
Daimh (Tay basin). — Rock-basin in crystalline schists. 
Dalla's. — Kettle-hole in fluvio-glacial deposits. 
Damh (Torridon basin). — Rock-basin in valley open at both ends. The 
lower end of the lake lies in Lewisian Gneiss, which here forms a 
pre-Torridonian hill projecting through the basal members of the 
Torridon Sandstone^ and the remainder rests on that formation. 
