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- W2103803312 abstract "This district has already been the subject of papers published in the Quarterly Journal of the Society. The authors of these agree in accepting the coarse conglomerate exposed (for instance) on the upper part of the hill pierced by the eastern tunnel of the railway near Bangor, as the base of the Cambrian; but there is still some diversity of opinion as to the relations and extent of the subjacent series. The views on the latter point will be found respectively expressed in papers by myself and Professor Hughes in vol. xxxv.; and since the publication of the latter I have four times revisited the district, leaving, I believe, but few exposures of the rock unexamined (except such as may occur unknown to me in private grounds). As I adhere to my original opinion as to the sequence of the beds, I now ask leave to state as briefly as possible the additional evidence which I have succeeded in gathering. At the same time I am glad to take this opportunity of frankly admitting that in the part of his paper which treated of the relations of the conglomerate and the granitoid rock at Twt Hill I was wrong, and Prof. Hughes was substantially right. Repeated examination of the district and of specimens under the microscope has convinced me that, notwithstanding the apparent passage of the one into the other, the conglomerate is much later in date than the granitoid series. Whether it be of the same date as the" @default.
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- W2103803312 date "1883-02-01" @default.
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- W2103803312 title "On the Rocks between the Quartz-felsite and the Cambrian Series in the Neighbourhood of Bangor" @default.
- W2103803312 doi "https://doi.org/10.1144/gsl.jgs.1883.039.01-04.30" @default.
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