The Ancient Volcanoes of Great Britain, Volume 1 (of 2)Geikie, Archibald
History
The Ancient Volcanoes of Great Britain, Volume 1 (of 2)
Geikie, Archibald
Volcanoes -- Great Britain
These spherulitic quartz-porphyries of St. David's occur as bosses,
dykes (elvans) or veins, cutting through all horizons of the volcanic
group, and in one case apparently, if not actually, reaching the quartz
conglomerate. One of the best exposures of this intrusive character may
be seen in the cliff below Nun's Chapel, where the elvan runs along the
face of the cliff through the uppermost zone of the volcanic group,
cutting the strata somewhat irregularly. Apparently in connection with
this dyke, a network of intrusions of decomposed quartz-porphyry may be
observed in the shales along the face of the cliff immediately below
Nun's Chapel. On the whole, the intruded material has forced its way
along the bedding-planes of the shales, but has also broken across
them, sending out finger-like branches.
3. _Diabase Dykes and Sills._--The latest rocks of the St. David's
district are dykes and intrusive sheets of diabase, which traverse
all the other formations. The dykes are specially abundant in the
granite. One or two may be detected in almost every artificial opening
which has been made in that rock; while on the coast-section they are
here and there profusely abundant. They are likewise frequent in the
quartz-porphyries, and occur also in the volcanic group as well as in
the sandstones and shales above the conglomerate, but become fewer in
number as they recede from the granite centre.[92]
[Footnote 92: The occurrence of these dykes is paralleled by that of
the similar intrusions in the quartz-felsite of Llyn Padarn to be
afterwards described.]
In external characters, the rock composing these dykes and sheets may
be described as usually a dull dirty-green or yellowish-brown mass, to
which the old name of "wacke" might appropriately be given. It exhibits
the texture and mode of weathering of the more distinctly crystalline
members of the basalt family. It is occasionally amygdaloidal or
cellular, the kernels or cavities being arranged parallel with the
sides of the dyke. Here and there a rudely prismatic structure extends
between the walls.
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