William Henry Fitton

William Henry Fitton

Summary

Portrait of William Henry Fitton William Henry Fitton Transactions of the Geological Society (1811)

The city of Dublin is placed in a flat limestone country, at the distance of about five miles to the northward of a range of mountains, which form the verge of a mountainous district, extending from thence for more than thirty miles to the southward. Through this tract there passes in a south-western direction from the shore on the south side of Dublin bay, a broad body of granite, bounded on its eastern and western sides by incumbent rocks of great variety
Source: Wikisource

Portrait of William Henry Fitton William Henry Fitton Transactions of the Geological Society (1811)

On the shore at the base of Killiney-hill, the granite is traversed by numerous veins, many of which themselves consist of granite; and in some instances, two granite veins, differing from each other and from the mass, in fineness of grain and in proportion of their ingredients, are seen to intersect; one vein often deranging the continuity of the other's direction. The substance of these veins is perfectly continuous with that of the mass through which they run, and the surface of the fracture passes through both without interruption.
Source: Wikisource

Portrait of William Henry Fitton William Henry Fitton Transactions of the Geological Society (1811)

It is remarkable, that a compound much resembling that which I have described, occurs also in the County of Donegal, from whence specimens now in the cabinet of the Dublin Society, and that of Dublin College (No. 30.) , were obtained. The garnet and vesuvian in these specimens, are scarcely to be distinguished from those of Kilranelagh; and, as at that place, are accompanied by quartz, often of a similar greenish colour; with the addition however of bluish grey granular limestone, and a fibrous substance, not improbably tremolite, mixed with carbonate of lime.
Source: Wikisource

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