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There are important coal-beds in India of Permian age. There are coal-beds of Liassic age in South Hungary and in Texas, and of Jurassic age in Virginia, as well as at Brora in Sutherlandshire; there are coals of Cretaceous age in Moravia, and valuable Miocene Tertiary coals in Hungary and the Austrian Alps. Again, older than the true carboniferous age, are the Silurian anthracites of Co.
"If you think that," she said, "why don't you come with us? A few others will be there, so we shall not be quite alone." I accepted the invitation with delight. I said good-by to London on the earliest day possible. In a train which was almost empty I traveled much at my ease from King's Cross Station to Brora. Not a tourist was to be seen anywhere.
Bean from these Yorkshire coal-bearing beds, point to the estuary or fluviatile origin of the deposit. At Brora, in Sutherlandshire, a coal formation, probably coeval with the above, or at least belonging to some of the lower divisions of the Oolitic period, has been mined extensively for a century or more.
Stonesfield Slate. Fossil Mammalia. Fuller's Earth. Inferior Oolite and Fossils. Northamptonshire Slates. Yorkshire Oolitic Coal-field. Brora Coal. Palaeontological Relations of the several Subdivisions of the Oolitic group.
The fact is, that I have seen in sandstone the empty mould of marine shells with some siliceous crystallization, so far as I remember, which corresponded perfectly with that idea. The place I saw this was in a fine white sandstone accompanying the coal, upon the sea side at Brora in Sutherland.
Another important area of production in eastern Virginia contains coal referable to the Jurassic age, and is similar in fossil contents to the Jurassic of Whitby and Brora. The main seam in eastern Virginia boasts a thickness of from 30 to 40 feet of good coal.
In part of Sutherlandshire, near Brora, common granite, composed of feldspar, quartz, and mica is in immediate contact with Oolitic strata, and has clearly been elevated to the surface at a period subsequent to the deposition of those strata. This breccia consists of fragments of shale, sandstone, and limestone, with fossils of the oolite, all united together by a calcareous cement.
But, Master, like a peaceful man avoiding contention, thou didst never answer this blustering Franck, but wentest quietly about thy quiet Lea, and left him his roaring Brora and windy Assynt. How could this noisy man know thee and know thee he did, having argued with thee in Stafford and not love Isaak Walton?
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