One of the most interesting sections in Scotland faces Antrim. Here, on
the Ayrshire coast, between Girvan and Ballantrae, a complex of several
kinds of igneous rock and a region, not a little disturbed, of
"greywackes" and other sedimentary deposits present the geologist with
problems more than sufficiently perplexing. At these Lyell took the
opportunity of glancing, but a day's trip afforded no opportunity for
any serious attempt to read the riddle. That had to be left to a later
generation, and so it remained for over forty years. Something is now
known about the igneous rocks, though here work still remains to be
done; and the sedimentary deposits have been brought into order by the
labours of Professor Lapworth. They exhibit, according to his
description,[106] an ascending succession from the Llandeilo to the
Llandovery group, and appear to be more modern than some, if not all, of
the above-named igneous rocks. After their brief halt in this district
the Lyells went on to Forfarshire, and spent the rest of the autumn at
Kinnordy.
The winter was a busy time; he was writing steadily at his "Travels in
North America," and working up some of the more distinctly scientific
notes into formal papers for the Geological and other societies. Thus
occupied, more than a year slipped away, diversified only by a summer
visit to Scotland, attending the meeting of the British Association at
York, and a journey to the Haswell Colliery, Durham, together with
Faraday, as commissioners to examine into the cause of a recent
disastrous explosion, and see whether such accidents could be prevented.
Work at the "Travels in North America" took up all Lyell's spare time
during the winter, and the book was published in the earlier part of
1845.
Public-domain text, read in full here on John Shaqi.
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