The Geology of Cowal Including the Part of Argyllshire Between the Clyde And Lo
The Geology of Cowal Including the Part of Argyllshire Between the Clyde And Lo
W William Gunn
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A little south-west of this it ceases to be traceable. Near the " h " of " Leamhanin " the outcrop of green beds above the one we have been describing is hardly 50 yards wide, and is separated from the next overlying green bed by an interval of quartzose and phyllitic mica schist. The interval has been mapped to near the sides of the alluvium f mile east of Ballimore. The last clear section of it is in the burn J mile slightly north of east of Ballimore : here the width of green beds below the ...interval is less than in Leamhanin and less than that of the interval. The top of a greywacke schist horizon occurs on the south-west side of the Hell's Glen fault, between the first " a " and ' d " of " Monovechadan. " On the south-east side of Stob Liath, this line, together with the lampro- phyre sheets a little above it, is thrown by a series of north-west faults, all of which shift the south-west side towards the south-east, the same direction as the Hell's Glen fault. One-eighth of a mile south of the first "i" of " Drimsyniebeg " the fault in Gleann Canachadan breaks through the line.
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