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The Hæmatite Deposits of Glamorganshire

Published online by Cambridge University Press:  17 March 2016

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Extract

During the last few years, the native iron-making resources of South Wales have received considerable assistance from the re-discovery and working of some very remarkable deposits of hæmatite in the county of Glamorganshire. I propose in the present article to describe two of the most important, perhaps, of those veins of ore, which are found in the districts of Llantrissant and Llanharry, near Cowbridge, and at Newton Nottage, near Bridgend;—the iron-ore in the latter locality being associated with a very large and curious deposit of manganese, chiefly psilomelane. Prefatory to this description, it may not be out of place to give a few remarks on the physical geology of the surrounding country, inasmuch as this district possesses ample materials to engage the attentive and careful examination of the geologist, particularly in relation to the origin of the mineral deposits in question. The exploitation of these hæmatite-mines will have the effect, commercially, of giving a great development and increased prosperity to the iron-manufacture in the district south of Cardiff; while, as a social result, their being worked will probably bring back to a population, at present agricultural, the mining and metallurgical occupations of the ancient fore-dwellers on the soil, and, what is most desirable, give constant occupation to a very large number of the working classes.

Type
Research Article
Copyright
Copyright © Cambridge University Press 1859

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References

page 245 note * This rock, mostly in a disintegrated state, often occupies hollows in the limestone, where it is considered to be in sitû, and it is questionable whether it does not belong to the Millstone-grit or its equivalent. In North Staffordshire, the hollows in the Carboniferous limestone are similarly filled at Oakamore, near Chesdle, and the argillo-siliceous sands are there largely quarried for use in the potteries, from their possessing highly refractory qualities for the manufacture of lining-tiles for the kilns.

page 246 note * Rolled shells of a species of Gryphæa are common in the drift.

page 251 note * Geologist, vol. i p. 270. 1858.

page 255 note * The section is purposely exaggerated to better show the details—the real thickness of the several beds is mentioned in the text.