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
My own examination so far confirms the conclusions arrived at by
these observers. Like my predecessors in the Geological Survey,
however, I have been unable to detect anywhere in Caernarvonshire
or Merionethshire a base to the Cambrian system, and I am compelled
to agree with them in regarding as Cambrian (partly even as Lower
Silurian) all the rocks from Bangor to Llanllyfni, which have more
recently been classed as pre-Cambrian. But though thus supporting their
general stratigraphy, I am bound to acknowledge that they failed to
recognize the existence of a great volcanic series below the Arenig
horizon. The existence of this series, noticed by Sedgwick, was first
definitely stated by Professor Hughes,[84] and his statements have been
confirmed and extended by subsequent observers, notably by Professor
Bonney and Mr. Blake. The Cambrian period is thus proved to have been
perhaps even more continuously volcanic than the Lower Silurian period
was in Wales.
[Footnote 84: _Proc. Camb. Phil. Soc._ vol. iii. (1877), p. 89. The
Cambrian volcanic areas of North Wales are represented in Map II.]
The following table shows the subdivisions of the Cambrian system now
recognized in Britain:--
+----------------------+----------------------+-------------------------+
| Wales. | | |
| (Ranging up to | Western England. | N.W. Scotland. |
| 12,000 feet | (About 3000 feet.) | (About 2000 feet.) |
| or more.) | | |
+----------------------+----------------------+-------------------------+
|Upper or _Olenus_ Zones. | |
| Tremadoc Slates | Shineton Shales | Limestones, about 1500 |
| Lingula Flags | (_Dictyograptus_ | feet thick, divisible |
| (_Lingulella_, | or _Dictyonema_, | into seven groups |
| _Olenus_, etc.). | _Olenus_, etc.). | (_Archæocyathus_, |
| | | _Maclurea_, _Ophileta_,|
|Middle or _Paradoxides_ Zones. | _Murchisonia_, |
| Menevian group | Conglomerates and | _Orthoceras_, |
| (_Paradoxides_). | limestones (Comley),| and vast quantities of |
| | (Comley), with | annelid castings). |
| | _Paradoxides_, etc. | |
| | | |
|Lower or _Olenellus_ Zones. | |
| Harlech and | Thin quartzite | Shales ("fucoid beds"), |
| Llanberis | passing up into | with _Olenellus_, |
| group with | green flags, grits, | _Salterella_, etc. |
| basement volcanic | shales | Quartzites with annelid |
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