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Updated: May 10, 2025


Coal is compressed and mineralized vegetal matter. Its varieties depend on the perfection to which the peculiar change called bituminization has been carried, and also, as shown in the table below, on the degree to which the volatile substances and water have escaped, and on the per cent of carbon remaining. Peat Lignite Bituminous Coal Anthracite Dismal Swamp Texas Penn. Penn.

Surrounded by the granite and other rocks of the Dartmoor hills in Devonshire, is a formation of clay, sand, and lignite, long known to geologists as the Bovey Coal formation, respecting the age of which, until the year 1861, opinions were very unsettled.

She patted them down in front of all four wheels. Her crisp hands looked like the paws of a three-year-old boy making a mud fort. Her nails hurt from the mud wedged beneath them. Her mud-caked shoes were heavy to lift. It was with exquisite self-approval that she sat on the running-board, scraped a car-load of lignite off her soles, climbed back into the car, punched the starter.

The reader must he reminded in particular that the above calculations take no account of the German production of lignite, which yielded in 1913 13,000,000 tons of rough lignite in addition to an amount converted into 21,000,000 tons of briquette. This amount of lignite, however, was required in Germany before the war in addition to the quantities of coal assumed above.

There are other freshwater formations with lignite, besides those on the Lake of Zurich, as those of Wetzikon near the Pfaffikon Lake, of Kaltbrunnen, of Buchberg, and that of Morschweil between St. Gall and Rorschach, but none probably older than the Durnten beds.

This great work, and those of Adolphe Brongniart, Unger, Goppert and others, show that this class of fossils is beginning to play the same important part in the classification of the tertiary strata containing lignite or brown coal as an older flora has long played in enabling us to understand the ancient coal or carboniferous formation.

Beds of lignite formation lie on the north side of Graham Island between Tow Hill and Chown Point, on the Yakoun and Mamin rivers of Massett Inlet, on Lignite Brook and Naden Harbor and on the west coast near the sea otter hunters' camp of Tledoo. Coal has also been found at the head of Skaloo Inlet.

In most lignites there is, as a rule, a comparatively large proportion of sulphur, and in such cases it is rendered useless as a domestic fuel. It has been used as a fuel in various processes of manufacture, and the lignite of the well-known Bovey Tracey beds has been utilised in this way at the neighbouring potteries.

Given, that on a coal or lignite field, or at a waterfall, 100 horse-power is developed by the combustion of fuel or by the fall of water driving a turbine, this power can be electrically transmitted to a mine or GROUP OF MINES, say 100 miles away, with only a loss of some 30 horse-power.

Wall, 'is identically the same with the substances produced immediately above or below seams of coal, which have taken fire, and burnt for a length of time. There is lignite and other coaly matter enough in the rocks to have burnt like coal, if it had once been ignited; and the cause of ignition may be, as Mr. Wall suggests, the decomposition of pyrites, of which also there is enough around.

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