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
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In our eReader you can find the full English version of the book. Read The Geology of Cowal Including the Part of Argyllshire Between the Clyde And Lo Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book The Geology of Cowal Including the Part of Argyllshire Between the Clyde And Lo
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To quickly assess the difficulty of the text, read a short excerpt:
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.
What to read after The Geology of Cowal Including the Part of Argyllshire Between the Clyde And Lo?
You can find similar books in the "Read Also" column, or choose other free books by W William Gunn to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
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.
What to read after The Geology of Cowal Including the Part of Argyllshire Between the Clyde And Lo?
You can find similar books in the "Read Also" column, or choose other free books by W William Gunn to read onlineMoreLess
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