Coal Sentence Examples
Coal is found in the ground, too.
The city has immense coal piers.
Near the city are valuable coal mines, and there is one within the city limits.
Among later additions were gunmounting stores, boiler shop, boat sheds, canteen, coal stores, &c., together with a double dock 750 ft.
In my time too; the war brought some money in and coal was getting dug so's there was jobs.
The borough is finely situated in the Wyoming Valley among the rich anthracite coalfields of eastern Pennsylvania, and its inhabitants are chiefly engaged in the coal industry; in 1906 and 1907 (when it shipped 24,081,4 9 1 tons) Luzerne county shipped more anthracite coal than any other county in Pennsylvania.
It is the largest peanut market in the world, is in a great truck-gardening region, and makes large shipments of cotton (822,930 bales in 1905), oysters, coal, fertilizers, lumber, grain, fruits, wine, vegetables, fish and live stock.
Charcoal, coke or anthracite coal are the fuels generally used in slow combustion heating stoves.
Iron ore is found in the state in the coal hills (especially Laurel Hills and Beaver Lick Mountain), but the deposits have not been worked on a large scale.
Railway development in West Virginia has been due largely to the exploitation of the coal and lumber resources of the state.
AdvertisementIt is the carrier of a heavy tonnage of coal to Pittsburg, Pennsylvania.
The Flemish coal-basin, employing over 100,000 hands, produces 60% of the coal mined in France.
The Alleghany Plateau consists of nearly horizontal beds of limestone, sandstone and shales, including important seams of coal; inclines slightly toward the north-west, and is intricately dissected by extensively branching streams into a maze of narrow canyons and steep-sided hills.
Butter is the principal export, and petroleum, coal and iron the imports.
Large quantities of coal and tea are exported.
AdvertisementThe imports consist principally of coal, salt, grain and flour, groceries, textiles, wood, and mineral oils.
Coal.The principal mines of France are coal and iron mines.
After the year 1884 Labour troubles became very frequent, the New South Wales coal miners in particular being at war with the colliery owners during the greater part of the six years intervening between then and what is called the Great Strike.
Iron, coal and slate are the chief products, and copper and cobalt may be added.
Minerals remained for the most part unworked, though the profitable coal fields and oil wells in Ferghana were used when disturbances in Trans-Caspia cut Turkestan off from the Baku oil, on which it relies entirely for its industrial life.
AdvertisementEurope generally, the principal coal seams occur in the Upper Carboniferous, while the Lower Carboniferous is mainly composed of marine deposits, with, however, the first bed of coal near its summit.
The only important industries are connected with cotton and coal.
Bright, glance or pitch coal is another brilliant variety, brittle, and breaking into regular fragments of a black colour and pitchy lustre.
Black coal forms one of the principal resources of New South Wales; and in the other states the deposits of this valuable mineral are being rapidly developed.
Coal of a very fair description was discovered in the basin of the Irwin river, in Western Australia, as far back as the year 1846.
AdvertisementThe most important discovery of coal in the state, so far, is that made in the bed of the Collie river, near Bunbury, to the south of Perth.
The coal has been treated and found to be of good quality, and there are grounds for supposing that there are 250,000,000 tons in the field.
The coal mines of New South Wales give employment to 14,000 persons, and the annual production is over 6,600,000 tons.
Black coal has been discovered in Victoria, and about 250,000 tons are now being raised.
The quantity of coal extracted annually in Australia had in 1906 reached 7,497,000 tons.
It is a species of cannel coal, somewhat similar to the Boghead mineral of Scotland, but yielding a much larger percentage of volatile hydro-carbon than the Scottish mineral.
Excluding coal lines and other lines not open to general traffic, the length of railways in private hands is only 382 m.
It was hard indeed for a carter drawing coal to a gasworks to recognize the necessity which compelled a reduction in his wages because wool had fallen 20 7 0.
It has large coal mines, which form the south-western portion of the extensive Upper Silesian coal fields, the largest Austrian deposit.
Impure coal has also been recorded.
Belleville is in a rich agricultural region, and in the vicinity there are valuable coal mines, the first of which was sunk in 1852; from this dates the industrial development of the city.
The commerce of the lake consists principally of coal, wood pulp and building material, besides general merchandise.
Petroleum and coal have been worked, and there is a rich yield of chalk, while a good quality of bricks is made from the xxii.
Machines used for lifting only are not called cranes, but winches, lifts or hoists, while the term elevator or conveyor is commonly given to appliances which continuously, not in separate loads, move materials like grain or coal in a vertical, horizontal or diagonal direction.
A transporter of this kind, when fitted with a grab, is a very efficient machine for taking coal from barges and depositing it in a coal store.
Vessels go to Porman to land coke and coal, and to load iron ore and lead.
Timber is largely imported from the United States, Sweden and Russia; coal from Great Britain; dried codfish from Norway and Newfoundland.
Pipeclay and china clay, from Kingsteighton, are shipped for the Staffordshire potteries, while coal and general goods are imported.
This is mixed with small coal, and when redistilled gives an enriched dust, and by repeating the process and distilling from cast iron retorts the metal is obtained.
If the available water-power of Italy, already very considerable, be harnessed, converted into electric power (which is already being done in some districts), and further increased by reafforestation, the effect upon the industries of Italy will be incalculable, and the importation of coal will be very materially diminished.
A quantity of it is really brushwood, used for the manufacture of charcoal and for fuel, coal being little used except for manufacturing purposes.
This led to deficiencies in the supply of coal to the manufacturing centres, and to some diversion elsewhere of shipping.
The most important imports are minerals, including coal and metals (both in pig and wrought); silks, raw, spun and woven; stone, potters earths, earthenware and glass; corn, flour and farinaceous products; cotton, raw, spun and woven; and live stock.
In 1894 the excess of imports over exports fell to 2,720,000, but by 1898 it had grown to 8,391,000, in consequence chiefly of the increased importation of coal, raw cotton and cotton thread, pig and cast iron, old iron, grease and oil-seeds for use in Italian industries.
Lincoln is situated in a productive grain region, and has valuable coal mines.
Near Tokat copper pyrites, with iron and manganese, kaolin and coal are found; but most of the copper worked here comes from the mines of Keban Maden and Arghana Maden, on the upper Euphrates and Tigris.
Thus various parts of criminals, such as the thigh bone of a hanged man, moss grown on a human skull, &c., were used, and even the celebrated Dr Culpeper in the 17th century recommended " the ashes of the head of a coal black cat as a specific for such as have a skin growing over their sight."
The Eastern railway has works at Romilly, and there are iron works at Clairvaux and wire-drawing works at Plaines; but owing to the absence of coal and iron mines, metal working is of small importance.
The exports of Aube consist of timber, cereals, agricultural products, hosiery, wine, dressed pork, &c.; its imports include wool and raw cotton, coal and machinery, especially looms. The department is served by the Eastern railway, of which the main line to Belfort crosses it.
Columbus is near the Ohio coal and iron-fields, and has an extensive trade in coal, but its largest industrial interests are in manufactures, among which the more important are foundry and machine-shop products (1905 value, $6,259,579); boots and shoes (1905 value, $5,425,087, being more than one-sixtieth of the total product value of the boot and shoe industry in the United States, and being an increase from $359,000 in 1890); patent medicines and compounds (1905 value, $3,214,096); carriages and wagons (1905 value, $2,197,960); malt liquors (1905 value, $2,133,955); iron and steel; regalia and society emblems; steam-railway cars, construction and repairing; and oleo-margarine.
Coal deposits exist in the immediate vicinity of the town.
There are salt works and important coal deposits in its vicinity, the latter at Naricual and Capiricual, 12 m.
The coasting trade consists chiefly of imports of coal and provisions, the exports being principally timber for shipbuilding and flint for the Staffordshire potteries.
Frostburg is in the midst of the coal region of the state, and is itself almost completely undermined; it has planing mills and manufactures large quantities of fire-brick.
Iron, zinc and lead are found in the vicinity, and some coal is mined.
Bethune lies in the midst of the richest coal mines in France.
The other minerals found are silver, lead, copper, magnesium and lignite coal.
Sublimed sulphur also results from the spontaneous combustion of coal seams containing pyrites.
It is also produced during the putrefaction of organic substances containing sulphur and is found among the products obtained in the destructive distillation of coal.
The principal manufactures are firearms, ironmongery, earthenware, woollen cloth, beer, stoneware, zinc goods, colours and salt; in the neighbourhood are iron and coal mines.
The products of the province are tea (the best quality of which is grown at Gan-hwa and the greatest quantity at Ping-kiang), hemp, cotton, rice, paper, tobacco, tea-oil and coal.
This area is divided into nearly two equal parts - one, the Lei river coal-fields, yielding anthracite, and the other the Siang river coal-fields, yielding bituminous coal.
Small vessels may coal at Naos, an island in the Gulf of Panama, which is owned by the United States.
In the Valdai plateau there are only a few beds of mediocre coal.
In the Moscow basin, which was a broad gulf of the Carboniferous sea, coal appears as isolated inconstant seams amidst littoral deposits, the formation of which was favoured by frequent minor subsidences of the seacoast.
The coal is here confined to the lower division of the system; the Upper Carboniferous (corresponding with the English Coal-Measures) is exclusively marine, consisting chiefly of Fusulina limestone.
Germany, and containing brown coal and amber, has been met with only in Poland, Courland and Lithuania.
The imports of foreign metals in the rough and of coal are steadily increasing, while the exports, never otherwise than insignificant, show no advance.
The minerals chiefly produced in the Urals are iron, coal, gold, platinum, copper, salt and precious stones.
The output of coal in the Urals is, altogether, less than 3% of the total for all the empire and 4% of the output of European Russia (exclusive of Poland) alone.
Coal takes, however, an altogether secondary place as a fuel in Russia; wood is much more extensively used, not only for domestic, but also for industrial purposes.
Machinery, coal, iron, woollens, ships, lead and copper are the commodities supplied by the United Kingdom.
Railways had their origin in the tramways (q.v.) or wagon-ways which at least as early as the middle of the 16th century were used in the mineral districts of England round Newcastle for the conveyance of coal from the pits to the river Tyne for shipment.
It may be supposed that originally the public roads, when worn by the cartage of the coal, were repaired by laying planks of timber at the bottom of the ruts, and that then the planks were laid on the surface of special roads or ways' formed between the collieries and the river.
A locomotive depot further includes stores of the various materials required in working the engines, coal stages at which they are loaded with coal, and an ample supply of water.
At a small roadside station, where the traffic is of a purely local character, there will be some sidings to which horses and carts have access for handling bulk goods like coal, gravel,.
With this assumption, 0.06 is the fraction of the heat energy of the coal which is utilized in the engine cylinders as mechanical work; that is to say, of the 15,000 B.Th.U.
Let E represent the pounds of coal burnt per hour in the fire-box of a locomotive, and let c be the calorific value in B.Th.U.
This maximum rate depends upon the kind of coal used, whether small, friable, bituminous or hard, upon the thickness of the fire, and upon the correct design and setting of the blast-pipe.
The maximum rate of combustion may be as much as so lb of coal per square foot of grate per hour, and in exceptional cases even a greater rate than this has been maintained.
A few experimental results are set forth in Table XX., from which it will be seen that with a relatively low rate of combustion, a rate which denotes very light service, namely lb of coal per square foot of grate per hour, the efficiency of the boiler is %, which is as good a result as can be obtained with the best class of stationary boiler or marine boiler even when using economizers.
This high mean pressure cannot be maintained for long, because as the speed increases the demand for steam per unit of time increases, so that cut-off must take place earlier and earlier in the stroke, the limiting steady speed being attained when the rate at which steam is supplied to the cylinders is adjusted by the cut-off to be equal to the maximum rate at which the boiler can produce steam, which depends upon the maximum rate at which coal can be burnt per square foot of grate.
If C is the number of pounds of coal burnt per square foot of grate per hour, the calorific value of which is c B.Th.U.
Holden developed the use of liquid fuel on the Great Eastern railway to a point beyond the experimental stage, and used it instead of coal with the engines running the heavy express traffic of the line, its continued use depending merely upon the relative market price of coal and oil.
For years the standard freight cars have held 60,000 lb and now many carry 80,000 lb or 100,000 lb; a few coal cars have even been built to contain 200,000 lb.
Coal trains, excluding the engine, weigh up to Boo or 900 tons, and travel at from 18 to 22 m.
The dark bituminous layers of clay slate, which occur intercalated among the quartzites, have led, here as elsewhere, to the hope of coming upon a seam of coal, but it is contrary to experience that coal of any value should be found in rocks of that age.
Peat is largely used as fuel, coal being obtained only at a cost of £3 a ton.
Its chief industry is the mining of anthracite coal; the principal establishments are railway repair shops, which in 1905 gave employment to 48.9% of all wage-earners engaged in manufacturing.
Its growth was accelerated by the establishment here, in 1863, of the shops of the railway from Pittston to Hawley built in 1849-1850 by the Pennsylvania Coal Company.
It has an increasing trade in iron, timber, coal and agricultural products, a trade which is fostered by a harbour opened in 1897; and also large factories for making aniline dyes and soda.
Large quantities of cranberries are raised in the township. Plymouth is a port of entry, but its foreign commerce is unimportant; it has a considerable coasting trade, especially in coal and lumber.
Parkersburg is the see of a Protestant Episcopal bishop. Oil, coal, natural gas and fire-clay abound in the neighbouring region, and the city is engaged in the refining of oil and the manufacture of pottery, brick and tile, glass, lumber, furniture, flour, steel, and foundry and machine-shop products.
It would take 20 tons of coal a day burned on each square foot of the sun's surface to supply the daily radiation.
Even if the sun were made of one mass of fuel as efficient as coal, that mass must be entirely expended in a few thousand years if the present rate of radiation was to be sustained.
The principal mining product is mercury, extracted at Idria, while iron and copper ore, zinc and coal are also found.
The principal imports are grain and agricultural produce, timber and coal, and the exports cement and fish.
Michoacan is essentially a mining region, producing gold, silver, lead and cinnabar, and having rich deposits of copper, coal, petroleum and sulphur.
It is marked by grey clays and sands, lignitic fossiliferous clays, beds of lignite or brown coal, sometimes 8 ft.
The lack of mineral resources, especially of coal and iron, of a good harbour (until the improvement of Gulfport), and of an adequate supply of labour has discouraged most kinds of manufacturing.
The state has two small areas in which bituminous coal occurs; one in the basin of the Dan and one in the basin of the Deep. Very little coal was produced in the state until the Civil War, when, in 1862 and again in 1863, 30,000 short tons were obtained for the relief of the Confederate government, an amount which up to 1905, when the yield was only 1557 short tons (falling off from 7000 short tons in 1904), had not since been equalled; in 1906, in 1907 and in 1908 no coal was mined in the state.
They consist chiefly of sandstone and conglomerate, but include workable seams of coal.
Its chief industry is the mining of anthracite coal at several collieries in the vicinity; and at Fountain Springs, 1 m.
Ashland has an excellent harbour, has large iron-ore and coal docks, and is the principal port for the shipment of iron ore from the rich Gogebec Range, the annual ore shipment approximating 3,500,000 tons, valued at $12,000,000, and it has also an extensive export trade in lumber.
In the vicinity are large deposits of coal, of glass-sand, and of clay suitable for brick and tile.
The mouth of the Fox was early visited by French explorers, and Father Hennepin is said to have discovered here in 1680 the first deposit of coal found in America.
The land around Beauly is fertile and the town drives a brisk trade in coal, timber, lime, grain and fish.
The exports consist chiefly of woollen yarn, woollens, cotton goods, cotton yarn, machinery, &c. and coal.
The country has a great wealth of minerals, silver having been found, and copper, lead, iron, coal and rock-salt being wrought with profit.
Steam coal of good quality is reported to exist about 30 m.
About 50,000 tons of coal of very poor quality are, however, extracted annually, and the same quantity of salt in the Armenian highlands and in Kuban.
The Coal Measures repose upon the Millstone Grit; the largest area of these rocks lies on the east, where they are conterminous with the coalfields of Yorkshire and Nottingham.
East of Bolsover, the Coal Measures are covered uncomformably by the Permian breccias and magnesian limestone.
The Coal Measures repose upon the Millstone Grit; the largest area of these rocks lieson the east, where they are conterminous with the coalfields of Yorkshire and Nottingham.
East of Bolsover, the Coal Measures are covered unconformably by the Permian breccias and magnesian limestone.
The principal mineral is coal.
Ironstone is not extensively wrought, but, on account of the abundant supply of coal, large quantities are imported for smelting purposes.
Iron has also been produced in Derbyshire from an early date, and coal mines were worked at Norton and Alfreton in the beginning of the 14th century.
Its industries include the manufacture of tiles, pasteboard wares and gardening implements, while there are coal mines in the vicinity.
Soon after her marriage miners had been brought from Lorraine to dig for gold at Crawford Moor, and she now carried on successful mining enterprises for coal and lead, which enabled her to meet the expenses of her government.
In the Carboniferous strata (Coal measures) remains of Hexapods become numerous and quite indisputable.
Barium chloride is present in some natural waters, and when this is the case the interaction of sulphates results in a deposition of barytes, as has occurred in the pipes and water-boxes of the Newcastle-on-Tyne coal mines.
Wheat, coal, cotton, petroleum, wood, lime and cement are brought into Venice for shipment to the Levant or for distribution over Italy and Europe.
The mineral wealth of Ohio consists largely of bituminous coal and petroleum, but the state also ranks high in the production of natural gas, sandstone, limestone, grindstone, lime and gypsum.
The coal fields, comprising a total area of 10,000 sq.
Coal was discovered here as early as 1770, and the mining of it was begun not later than 1828, but no accurate account of the output was kept until 1872, in which year it was 5,315,294 short tons; this was increased to 18,988,150 short tons in 1900, and to 26,270,639 short tons in 1908 - in 1907 it was 32,142,419 short tons.
There are 29 counties in which coal is produced, but 81.4% of it in 1908 came from Belmont, Athens, Jefferson, Guernsey, Perry, Hocking, Tuscarawas and Jackson counties.
Of far greater volume than the foreign commerce is the domestic trade in coal, iron, lumber, &c., largely by way of the Great Lakes.
The mineral wealth of Carinthia is great, and consists in lead, iron, zinc and coal.
Fibres and vegetable grasses, wool, hides and skins, cotton, sugar, iron and steel and their manufactures, chemicals, coal, and leather and its manufactures are the leading imports; provisions, leather and its manufactures, cotton and its manufactures, breadstuffs, iron and steel and.
Geologically, spiders date from the Carboniferous Period, Arthrolycosa and others from the coal beds of Europe and North America being closely allied to the existing genus Liphistius.
For a long time these shells or hulls, as they are called, were burned at oil mills for fuel, 22 tons being held equal to a cord of wood, and 43 tons to a ton of coal.
The surrounding country abounds in coal, iron ore, oil, clay, stone and timber, for which the city is a distributing centre.
The earlier supporters of the organic theory held that it was a product of the natural distillation of coal or carbonaceous matter; but though in a few instances volcanic intrusions appear to have converted coal or allied substances into oil, it seems that terrestrial vegetation does not generally give rise to petroleum.
Similarly there is a difference of opinion as to the conditions under which the organisms have been mineralized, some holding that the process has taken place at a high temperature and under great pressure; but the lack of practical evidence in nature in support of these views has led many to conclude that petroleum, like coal, has been formed at moderate temperatures, and under pressures varying with the depth of the containing rocks.
The land is poor in minerals, including coal; water-power also is deficient, so that the introduction of European industries is attended with difficulties even apart from the insecurity of affairs, which forbids such experiments as the improvement of agriculture by means of European capital.
Coal is found in the province of Hualgayoc at the southern extremity of the department, which is also one of the rich silver-mining districts of Peru.
Brazil's chief industrial importance is due to its situation in the heart of the "Brazil block" coal (so named because it naturally breaks into almost perfect rectangular blocks) and clay and shale region; among its manufactures are mining machinery and tools, boilers, paving and enamelled building bricks, hollow bricks, tiles, conduits, sewer-pipe and pottery.
Among the principal varieties are those which contain carbolic acid and other ingredients of coal tar, salicylic acid, petroleum, borax, camphor, iodine, mercurial salts, sulphur and tannin.
Imports are principally coal, iron and timber.
The finest agricultural land in the United States is near the lake, and there is an immense trade in all grains, fruits, livestock and lumber, and in products such as flour, pork, hides, leather goods, furniture, &c. Rich lead and copper mines abound, as also salt, iron and coal.
There are coal mines about 25 m.
It is in the Vermilion coal region, and clay for brick and tile is abundant in its vicinity.
The mineral wealth of Moravia, consisting chiefly of coal and iron, is very considerable.
The principal imports are coal, grain, manufactured articles and articles of luxury.
Coal is also found in large quantities near Kelung and sulphur springs exist in the north of the island.
The society grew in strength during the Civil War, when the increased demand for coal caused an influx of miners, many of them lawless characters, into the coal-fields, and in1862-1863it opposed enlistments in the Federal Army and roughly treated some of the enlisting officers.
After the war its activity was shown by an increasing number of assassinations, burnings and other outrages, until by 1875 it completely dominated the mining classes and forced a general strike in the coal regions.
Gowen (1836-1889), president of the Philadelphia and Reading Coal and Iron Company, sent James McParlan, an Irish Catholic and a Pinkerton detective (who some thirty years later attracted attention in the investigation of the assassination of Governor Steunenberg of Idaho), to the mining region in 1873; he joined the order, lived among the "Molly Maguires" for more than two years, and even became secretary of the Shenandoah division, one of the most notoriously criminal lodges of the order.
Imports include coal,timber, tar and hemp. Steam sawing, metal-founding, fish-salting, shipbuilding and repairing, and the manufacture of ship's-biscuits and fishing-nets are among the industries.
Timber makes up 59% of the imports, and coal and ships each about 30% of the exports.
Imports are coal, textiles, salt, grain and flour.
The chief imports are cotton piece goods, cotton twist, salt, sugar, provisions, railway materials, raw cotton, metals, coal, tobacco, spices and kerosene oil.
Minerals, in which Oberhessen is much richer than the two other provinces, include iron, manganese, salt and some coal.
The chief article of export is coal from the neighbouring collieries, the other leading exports being ale, whisky, glass and manufactured goods.
Eure-et-Loir exports the products of its soil and live-stock; its imports include coal, wine and wearing apparel.
Springfield is a trading and shipping centre for a prosperous agricultural region, and ships large quantities of bituminous coal from the immediate vicinity.
While washing out the sands of the North Saskatchewan for gold is still somewhat resorted to, the only real mining in Alberta is that for coal.
Vast beds of coal are found extending for hundreds of miles, a short distance below the surface of the plains.
The coal belongs to the Cretaceous beds, and while not so heavy as that of the Coal Measures is of excellent quality.
In the valley of the Bow river, alongside the Canadian Pacific railway, valuable beds of anthracite coal are worked, and the coal is carried by railway as far east as Winnipeg.
The usual coal deposits of Alberta are of bituminous or semi-bituminous coal.
Coal, oil, natural gas, clay and iron are found in the vicinity, and among the city's manufactures are iron, steel, glass, furniture and pottery.
The principal imports are manufactured cotton goods and other textiles, machinery, timber and coal.
On the south bank of the river is the township and urban district of Cowpen (pop. 17,879), with collieries and glass works; coal is shipped from this point by river.
In the Tertiary region are found small quantities of iron ore and an indifferent brown coal.
They serve the trade of Lake Pontchartrain and the Florida parishes, the lumber, coal, fish, oyster and truck trade of New Orleans, and to some extent are the highway of a miscellaneous coasting trade.
Much of the bituminous deposits is on the dividing line between asphalt and coal.
The state owes to this ruler the opening up of new railways across the great desert, which was formerly passable only by camels, and the tapping of the valuable coal deposits that occur in the territory.
Mehner patented heating the oxides of silicon, boron or magnesium with coal or coke in an electric furnace, and then passing in nitrogen, which forms, with the metal liberated by the action of the carbon, a readily decomposable nitride.
Bosnia is rich in minerals, including coal, iron, copper, chrome, manganese, cinnabar, zinc and mercury, besides marble and much excellent building stone.
After 1881 the Mining Company of Bosnia began to develop the coal and iron fields; and from 1886 its operations were continued by the government.
According to these statistics the most important articles of export are coal and turf, fruit, minerals, soda, iron and steel, and cattle.
The empire is rich in minerals, including gold, silver, lead, copper, iron, coal, mercury, borax, emery, zinc; and only capital is needed for successful exploitation.
Stock-raising, tobacco-growing, and coal and iron-mining are the industries of the district.
Cleveland's rapid growth both as a commercial and as a manufacturing city is due largely to its situation between the iron regions of Lake Superior and the coal and oil regions of Pennsylvania and Ohio.
Cleveland is the largest ore market in the world, and its huge ore docks are among its most interesting features; the annual receipts and shipments of coal and iron ore are enormous.
The discovery of iron ore in the Lake Superior region made Cleveland the natural meeting-point of the iron ore and the coal from the Ohio, Pennsylvania and West Virginia mines; and it is from this that the city's great commercial importance dates.
Of the Coal Measures above these, if they occur, we know nothing at present.
There is also coal on Kuhn Island.
Beds of this age, consisting of sandstones and coal, are found on the northern coast of Disco Island and the southern side of the Noursoak Peninsula, the beds in the former locality, " the Kome strata " of Nordenskiold, being the oldest.
Both these series contain numerous plant remains, evergreen oaks, magnolias, aralias, &c., and seams of lignite (coal), which is burnt; but in neither occur the marine beds of the United States.
It is limited to Disco Island, and perhaps to a small part of the Noursoak Peninsula, and the neighbouring country, and consists of numerous thin beds of sandstone, shale and coal - the sideritic shale containing immense quantities of leaves, stems, fruit, &c., as well as some insects, and the coal pieces of retinite.
A few other minerals may be noticed, and some have been worked to a small extent - graphite is abundant, particularly near Upernivik; cryolite is found almost exclusively at Ivigtut; copper has been observed at several places, but only in nodules and laminae of limited extent; and coal of poor quality is found in the districts about Disco Bay and Umanak Fjord.
Coal was brought down from the hills on the backs of mules, and iron carried in two-ton wagons.
The commercial greatness of Cardiff is due to the vast coal and iron deposits of the country drained by the Taff and Rhymney, between whose outlets the town is situated.
The Rhymney railway to Cardiff was completed in 1858 and the trade of the port so vastly increased that the shipment of coal and coke went up from 4562 tons in 1839 to 1,796,000 tons in 1860.
There is ample equipment of fixed and movable staiths and cranes of various sizes up to 70 tons, the Lewis-Hunter patent cranes being largely used for shipping coal owing to their minimizing the breakage of coal and securing its even distribution.
The total exports of the Cardiff docks in 1906 amounted to 8,767,502 tons, of which 8, 433, 629 tons were coal, coke and patent fuel, 151,912 were iron and steel and their manufactures, and 181,076 tons of general merchandise.
Taking "the port of Cardiff" in its technical sense as including Barry and Penarth, it is the first port in the kingdom for shipping cleared to foreign countries and British possessions, second in the kingdom for its timber imports, and first in the world for shipment of coal.
The mineral wealth of the department is considerable, including coal as well as manganese and bituminous schist; plaster, building stone and hydraulic lime are also produced.
Building materials, brandy and coal are among the imports.
The whole district is rich in coal, the mining of which is extensively carried on.
Callias And Hipponicus The exports from Callao are guano, sugar, cotton, wool, hides, silver, copper, gold and forest products, and the imports include timber and other building materials, cotton and other textiles, general merchandise for personal, household and industrial uses, railway material, coal, kerosene, wheat, flour and other food stuffs.
Coal and limestone are found near the city.
Its principal imports are coffee (of which it is the greatest continental market), tea, sugar, spices, rice, wine (especially from Bordeaux), lard (from Chicago), cereals, sago, dried fruits, herrings, wax (from Morocco and Mozambique), tobacco, hemp, cotton (which of late years shows a large increase), wool, skins, leather, oils, dyewoods, indigo, nitrates, phosphates and coal.
Of the total importations of all kinds of coal to Hamburg, that of British coal, particularly from Northumberland and Durham, occupies the first place, and despite some falling off in late years, owing to the competition made by Westphalian coal, amounts to more than half the total import.
Gold is found in the sands of all its upper tributaries, and coal and petroleum are amongst the chief mineral products which have been brought into economic prominence.
The export trade in corn and import trade in coal is considerable.
This is a wooded chain of mountains, with many branches, rich in brown coal and culminating in the Göblberg (2950 ft.).
Coal occurs in many Jurassic fresh-water;basins, namely, on the outskirts of the Altai, in south Yeniseisk, about Irkutsk, in the Nerchinsk district, at many places in the Maritime province, and on the island of Sakhalin.
Granite and wood-pulp are exported, and coal and grain imported.
Mining is only of slight importance, small quantities of coal and iron-ore being extracted in the Alpine foothill region; graphite is found near Miihldorf.
The surrounding country has good farming land and large coal mines.
The native carbonate or cerussite (q.v.) occasionally occurs in the pure form, but more frequently in a state of intimate intermixture with clay ("lead earth," Bleierde), limestone, iron oxides, &c. (as in the ores of Nevada and Colorado), and some times also with coal ("black lead ore").
As a preliminary to the melting process, the "browse" left in the preceding operation (half-fused and imperfectly reduced ore) is introduced with some peat and coal, and heated with the help of the blast.
It puts through 9-12 tons of ore in twenty-four hours, reducing the percentage of sulphur to 2-4%, and requires four to six men and about 2 tons of coal.
A furnace is served by three men, working in eight-hour shifts, and requires about 2 tons of coal, which corresponds to about 110 gallons reduced oil, air being used as atomizer.
The principal imports are coal, timber and slates, and the principal export stone of the Transition limestone or Devonshire marble.
The principal exports are Portland stone, bricks and tiles and provisions, and the imports are coal, timber, garden and dairy produce and wine.
Fossil scorpions of the modern type are found in the Coal Measures.
A fact of special interest in regard to them is that the genus Poliochera, from the Coal Measures, appears to be a member of the same group. The name Cryptostemma, given to the first-known genus of the order, described by Guerin-Meneville, refers to the supposed concealment of the eyes by the movable cephalic sclerite.
Brown coal has been discovered in Courland, while peat is already a valuable fuel.
Imports include coal, grain, flour and wine.
Besides wool, leading imports are jute, cotton, flax, timber, petroleum, coal, pitch, wine, cereals, oil-seeds and oil-cake, nitrate of soda and other chemical products, and metals.
The principal exports are sugar, coal, cereals, wool, forage, cement, chalk, phosphates, iron and steel, tools and metal-goods, thread and vegetables.
Anthracite coal is found in the neighbourhood.
There are coal-mines at and near Eregli (anc. Heracleia) which yield steam coal nearly as good in quality as the English, but they are badly worked.
In southern Brazil, on the other hand, in Rio Grande do Sul, Parana, &c., the beds of this period are of terrestrial origin, containing coal seams and remains of plants.
Modern industrial development in some of the states has greatly increased the importation of machinery, electric supplies, materials for construction, coal, &c. Kerosene oil also figures among the principal imports, and beef cattle are imported for consumption by some cities.
Bituminous coal of an inferior quality is mined to a limited extent in Rio Grande do Sul, and another mine has been opened in Santa Catharina.
These coal deposits extend from Rio Grande do Sul north into the state of Sao Paulo.
C. White, of the U.S. Geological Survey, who found strata of fairly good coal at depths of 100 to 200 ft.
The town is, industrially, remarkable for its paper mills and mines of coal and other minerals.
Fine white freestone abounds in the immediate vicinity (as at Craigleith, from the vast quarry of which, now passing into disuse, the stone for much of the New Town was obtained) and furnishes excellent building material; while the hard trap rock, with which the stratified sandstones of the Coal formation have been extensively broken up and overlaid, supplies good materials for paving and road-making.
There is a harbour on the Elbe here, and a brisk trade is carried on in coal, grain and timber.
There is trade in agricultural produce, wine, metals, &c. The canal from the Rhone to the Rhine passes under the citadel by way of a tunnel, and the port of Besancon has considerable trade in coal, sand, &c.
The chief exports are fish, cereals, bacon; imports, petroleum and coal.
These harbours on the eastern side of Sydney are mainly frequented by cargo boats trading in coal, corn, frozen meat, wool, hides and various ores.
Standing in the centre of a great coal-bearing basin, Sydney is naturally the seat of numerous manufactures, to the prosperity of which the abundance and cheapness of coal has been highly conducive.
The Ecca shales contain some of the best coals of South Africa, but the seams contain much unmarketable coal.
This consists of sandstones and shales with thin seams of coal.
The existence of coal in the north-east districts on or near the surface of the ground was reported as early as 1839, but it was not until 1880 that steps were taken to examine the coalfields.
In 1889 the extension of the railway from Ladysmith through the coal area first made coalmining profitable.
In 1896 the total output of coal was 216,106 tons (valued at £108,053 at the pit's mouth), in 1908 it had increased to 1,669,774 tons (valued at the pit's mouth at £737,169).
There is a considerable trade in bunker and export coal at Durban, the coal bunkered having increased from 118,740 tons in 1900 to 710,777 in 1908.
In the last-named year 446,915 tons of coal were exported.
The chief exports, not all products of the province, are coal, wool, mohair, hides and skins, wattle bark, tea, sugar, fruits and jams. The import trade is of a most varied character, and a large proportion of the goods brought into the country are in transit to the Transvaal and Orange Free State, Natal affording, next to Delagoa Bay, the shortest route to the Rand.
The governor was strongly opposed to this step, as he was anxious to protect the coal supply, and also feared the moral effect of a withdrawal.
Coal is known to exist to the southeast of Kobdo, in the Tannu-ola, and in the basin of the Yenisei, but its age is unknown (fresh-water Jurassic ?).
Its chief mineral products are coal, nitre, sulphur, alum, soda, saltpetre, gypsum, porcelain-earth, pipe-clay, asphalt, petroleum, marble and ores of gold, silver, mercury, copper, iron, lead, zinc, antimony, cobalt and arsenic. The principal mining regions are Zsepes-Giimor in Upper Hungary, the Kremnitz-Schemnitz district, the Nagybanya district, the Transylvanian deposits and the Banat.
Coal is extensively mined in the region of Budapest-Oravicza, Nagybanya, Zalatna, at Brennberg near Sopron, at Salgo-Tarjan, Pecs, in the counties of Krasso-Szoreny, and of Esztergom, and in the valley of the river Zsil.
The production of coal and iron trebled during the period 1880-1900, amounting in 1900 to 6,600,000 tons, and 463,000 tons respectively.
Besides its manufactures of leather, silk, velvet and ribbons, Gandia has a thriving export trade in fruit, and imports coal, guano, timber and flour.
The mineral products include silver, lead, coal, copper, and iron.
A thriving export trade is carried on in agricultural produce, condensed milk is manufactured, and slate is extensively quarried in the neighbourhood, while some coal is exported from the neighbouring fields.
Mieres is the chief town of a mountainous, fertile and well-wooded region in which coal, iron, and copper are extensively mined and sulphur and cinnabar are obtained in smaller quantities.
Seams of coal lie near the base, some of them exceeding 20 ft.
The minerals chiefly mined besides gold are diamonds and coal, but the country possesses also silver, iron, copper, lead, cobalt, sulphur, saltpetre and many other mineral deposits.
There are extensive beds of good coal, including thick seams of steam coal near the Rand and other goldfields.
Coal appears to have been first discovered in the neighbourhood of Bronkhorst Spruit between the Wilge and Olifants rivers, where it was so near the surface that farmers dug it up for their own use.
In 1887 coal was found at Boksburg in the East Rand, and a mine was at once started.
The principal collieries are those at Boksburg and at Brakpan, also on the East Rand, with a coal area of 2400 acres; at Vereeniging and Klerksdorp, near the Vaal; at Watervaal, 12 m.
Like that of Natal the Transvaal coal burns with a clear flame and leaves little ash.
Next in value came wool (£226,000), horses and mules (£110,000), skins, hides and horns (£106,000), tobacco (£89,000), tin, coal, copper and lead.
The department imports coal, lime, stone, salt, raw sulphur, skins and timber and exports agricultural and mineral products, bricks and tiles, and other manufactured goods.
In this process the purified ore is mixed with about one-fifth of its weight of a noncaking coal or anthracite smalls, the mixture being moistened to prevent it from being blown off by the draught, and is then fused on the sole of a reverberatory furnace for five or six hours.
The shipping trade is considerable, chiefly in coal, timber and agricultural produce.
There is a steady export of coal, and the harbour is provided with a wet dock and patent slip. In smuggling days the "Canty carles" of Dysart were professed "free traders."
The city's chief interest is in the tobacco industry; it has also considerable trade in other agricultural products and in coal; and its manufactures include carriages and wagons, bricks, lime, flour and dressed lumber.
The imports include manufactured articles of all kinds, hardware and building materials, earthenware and glassware, furniture, drugs and medicines, wines, foodstuffs, coal, petroleum and many other things.
The principal minerals are gold, copper, iron, sulphur, coal, asphalt and petroleum.
The principal coal deposits developed are at Naricual, near Barcelona, and a railway has been constructed to bring the output to the port of Guanta.
There has been some development in the manufacture of agricultural machinery and implements, vehicles, pianos and furniture, and some older industries, such as tanning leather and the manufacture of saddles and harness, the milling of wheat and Indian corn, distilling, soap-making, &c. At Guanta there is a factory for the manufacture of patent fuel from Naricual coal and asphalt.
The chief imports are coal, timber and iron, and the exports grain and other agricultural products and salt.
From 1783 to 1825 agricultural produce was exported and coal imported.
Pittston is in the midst of the richest anthracite coal region of the state, and fire-clay also abounds in the vicinity.
The mineral wealth is great, including copper, tin, lead, zinc, iron and especially coal.
Bituminous coal and natural gas are found in the vicinity, and the borough ships coal and lumber, and has various important manufactures.
The mineral resources include silver, gold, copper, lead, tin, iron and coal, and mining is the chief industry.
Bath also manufactures lumber, iron and brass goods, and has a considerable trade in ice, coal, lumber and iron and steel.
They sometimes cause a serious dislocation of railway and other traffic. Their principal cause is the smoke from the general domestic use of coal.
Among these are the Corn Exchange in Mark Lane, where the privilege of a fair was originally granted by Edward I.; the Wool Exchange, Coleman Street; the Coal Exchange, Lower Thames Street; the Shipping Exchange, Billiter Street; and the auction mart for landed property in Tokenhouse Yard.
Anthracite is mined in the St Lucia Bay district, and bituminous coal is found in the Nqutu and Kyudeni hills.
Meantime the coal mines near St Lucia Bay were opened up and connected with Durban by railway.
The term 1 is not limited to underground operations, but includes also surface excavations, as in placer mining and open-air workings of coal and ore deposits by methods similar to quarrying, and boring operations for oil, natural gas or brine.
Special methods of mining are dealt with in the separate articles on Coal, Gold, and other minerals and metals.
Fragments of coal, or soil stained black with coal, will be found near the outcrop tif coal beds.
The bed of fire-clay under a coal seam, being impervious to water, frequently determines the horizon of numerous springs issuing from the hillsides.
As the coal and the associated rocks usually contain pyrites, these springs are often chalybeate.
In the case of the cheaper and more abundant minerals, such as coal and iron ore, and of large deposits of low-grade ores, the extent and character of the deposit can generally be determined by surface examinations at comparatively small expense.
In the case of coal, salt, iron ore, pyrite and other homogeneous minerals, boring may give all the information required.
In coal mines, entries and headings, bords and walls serve similar purposes.
Examples of other mining methods will be found under Coal.
In the United States cars in the coal and iron mines hold from 2 to 4 tons.
To mine ore or coal at minimum cost it is necessary to work the mine plant at nearly or quite its full capacity and to avoid interruption and delays.
In coal mining the market demand varies in different seasons, and surface storage is sometimes necessary to permit regular work at the mines.
In coal-mines we have to deal with " fire-damp " or marsh gas, and with inflammable coal dust, which form explosive mixtures with air and frequently lead to disastrous explosions resulting in great loss of life.
In dry and dusty mines the danger may be greatly lessened by sprinkling the working places and passages, and the removal of the accumulated dust and fine coal.
Mine fires may originate from ordinary causes, but in addition they may result from the explosion of fire-damp or from the accidental lighting of jets of fire-damp issuing from the coal.
In some mining districts the coal is liable to spontaneous combustion.
A fire underground speedily becomes formidable, not only in coal but also in metal mines, on account of the large quantity of timber used to support the excavations.
These laws are enforced by mine inspectors of the timber produces falls of ground, making necessary the excavawho are empowered to call upon the courts and other government tion and removal at times of hundreds of tons of heated rock and burning coal, in order to reach the fire.
It is necessary, however, to keep the mine sealed until the burning timbers, or coal, and the red-hot rocks have become cool, or the fire will again break out.
When large areas are undermined, as in submarine coal mining, it is best to have several hundred feet of protecting rock.
In some mines dust seems to have but little effect on the health of the miners; indeed it is even claimed by some that coal dust decreases the mortality from phthisis.
He had organized in 1826 a society to develop the coal and iron of the Aveyron, and the name of Decazeville was given in 1829 to the principal centre of the industry.
Coal, fireclay and blue and red brick clay are dug in the neighbourhood; and there are also market gardens.
Coal is found in the Tertiary deposits in the valley of the Irrawaddy and in Tenasserim.
In its three chief mineral products, earthoil, coal and gold, Burma offers a fair field for enterprise and nothing more.
Coal is found in the Thayetmyo, Upper Chindwin and Shwebo districts, and in the Shan States; it also occurs in Mergui, but the deposits which have been so far discovered have been either of inferior quality or too far from their market to be worked to advantage.
In some English works coal is still employed for direct heating with various forms of mechanical stokers.
These small furnaces are frequently arranged for direct coal firing, but regenerative gasfired furnaces are also employed.
In England directly-heated coal furnaces are still in common use, which in many cases are stoked by mechanical feeders.
A certain proportion of soda ash (carbonate of soda) is also used in some works in sheet-glass mixtures, while " decolorizers " (substances intended to remove or reduce the colour of the glass) are also sometimes added, those most generally used being manganese dioxide and arsenic. Another essential ingredient of all glass mixtures containing sulphate of soda is some form of carbon, which is added either as coke, charcoal or anthracite coal; the carbon so introduced aids the reducing substances contained in the atmosphere of the furnace in bringing about the reduction of the sulphate of soda to a condition in which it combines more readily with the silicic acid of the sand.
Before the glass is introduced, the annealing kiln is heated to dull red by means of coal fires in grates which are provided at the ends or sides of the kiln for that purpose.
In 1615 all patents for glass-making were revoked and a new patent issued for making glass with coal as fuel, in the names of Mansel, Zouch, Thelwall, Kellaway and Percival.
To the last is credited the first introduction of covered crucibles to protect the molten glass from the products of burning coal.
Burning the coal on a voyage has the reverse effect on a steamer.
The discovery of coal in the neighbourhood stimulated and altered its industries.
Fareham has a considerable trade in corn, timber and coal; the creek being accessible to vessels of 300 tons.
It is the centre for a farming region, in which there are deposits of coal, iron, lead and shale, and there are various manufactures in the city.
Tamaqua is in a rich anthracite coal district, and coal-mining is its chief industry..
The first settlement here was made in 1799 and anthracite coal was discovered in 1817.
In the neighbourhood there are numerous large collieries, and coal is shipped from wharves on the riverside, vessels of 300 or 400 tons being able to reach the quays at high tide.
There is a large export trade in coal, I copper, iron and tin, mostly shipped from nieghbouring ports, while the principal imrorts are timber and general merchandise.
From this tunnel the coal is conveyed by rail for i 2 m.
With the latter system practically as much sugar is obtained from the canes as by diffusion, and the resulting megass furnishes, in a well-appointed factory, sufficient fuel for the crop. With diffusion, however, in addition to the strict scientific control necessary to secure the benefits of the process, fuel - that is, coal or wood - has to be provided for the working off of the crop, since the spent chips or slices from the diffusers are useless for this purpose; although it is true that in some plantations the spent chips have to a certain extent been utilized as fuel by mixing them with a portion of the molasses, which otherwise would have been sold or converted into rum.
In the best days of the so-called Jamaica Trains in Demerara, three-quarters of a ton of coal in addition to the megass was burned per ton of sugar made, and with this for many years planters were content, because they pointed to the fact that in the central factories, then working in Martinique and Guadeloupe, with charcoal filters and triple-effect evaporation, 750 kilos of coal in addition to the megass were consumed to make woo kilos of sugar.
Thus, supposing that moo lb of coal were required to work a single vacuum pan, evaporating, say, 6000 lb of water in a given time, then 500 lb of coal would be required for a double-effect apparatus to do the same work, 333 lb for a triple effect, 250 for a quadruple effect, and 200 lb for a quintuple effect.
In some places where coal costs 60s.
There is considerable agricultural trade, and iron founding is carried on; while in the neighbourhood some copper, lead, granite and slate are worked and exported in small vessels; coal, timber and general merchandise being imported.
Coal has been worked near Noumea, and kaolin is found in places.
The charge of the retorts consists of a mixture of 1100 lb of roasted calamine and 550 lb of dry powdered coal per furnace.
Zinc oxide, ZnO, is maufactured for paint by two processes - directly from the ore mixed with coal by volatilization on a grate, as in the Wetherill oxide process, and by oxidizing the vapour given off by a boiling bath of zinc metal.
Airdrie was a market town in 1695, but owes its prosperity to the great coal and iron beds in its vicinity.
It lies in a hilly district rich in coal and iron, while a hard basaltic intrusion known as Rowley rag is largely quarried.
The three isomeric cresols are found in the tar obtained in the destructive distillation of coal, beech-wood and pine.
Several large islands fill the upper bay near the eastern shore; some are used as coal deposits for the great steamship companies, and one (Flores) is used as an immigrants' depot.
The church of St John the Baptist, principally Perpendicular, - has in its tower three bells presented by Charles Both this town and the adjacent urban district of Radstock (pop. 3355) have a considerable trade in coal, which is mined in the vicinity.
Ottawa has an important trade in grain and live-stock; soft coal and natural gas are found in the vicinity; the manufactures include flour, windmills, wire-fences, furniture, bricks, brooms and foundry products.
Coal mining is an important industry, and the borough is supplied with natural gas.
The export of coal in that year was 74,000 tons, and copper ore 937 tons (vide supra, § Minerals).
The imports consist mainly of European manufactured goods (especially British cotton), machinery, flour, alcohol, sugar, timber, coal and petroleum.
Like the similar sandstone in Bolivia, it includes seams of coal and is frequently impregnated with cinnabar.
Within these limits are to be found most of the minerals known - gold, silver, quicksilver, copper, lead, zinc, iron, manganese, wolfram, bismuth, thorium, vanadium; mica, coal, &c. On or near the coast are coal, salt, sulphur, borax, nitrates and petroleum.
In,the vicinity of some of the deposits of argentiferous galena are large coal beds, but timber is scarce on the table-lands.
Coal has been found in extensive beds near Piura, Salaverry, Chimbote, Huarmey and Pisco on the coast, and at Goillarisquisga, Huarochiri and other places in the interior.
Timber, pig-iron and iron ore are the leading imports, and coal, produce and iron the chief exports.
When the substance operated upon is of uncertain composition, as, for example, coal, wood, coal-tar, &c., the term destructive distillation is employed.
The southern half of the province, that portion south of the Yangtsze Kiang, forms part of the Nan-shan, or hilly belt of the south-eastern provinces, and produces, besides cotton, coal and iron ore, large quantities of green tea.
The principal articles imported are cotton and cotton goods, coffee, coal, cereals, hides, fruit and tobacco; the principal articles exported are wool and woollen goods,.
The exports mainly consist of grain, cattle, fish, dairy produce and potatoes; the imports of coal and timber.
The principal exports are grain, eggs, cattle, linen cloth and flax, and the imports include timber, groceries and coal.
The province contains gold, silver, copper, iron, lead, coal and salt, but mining has never been developed to any extent.
Coal is also found and several salt mines are worked.
The port has a small trade in coal, live-stock and farm produce.
It chiefly consists of stratified volcanic tuffs rich in coal, lignite, fossilized plants and an invertebrate fauna.
The mineral wealth of Saxe-Coburg-Gotha is insignificant, small quantities of coal, lignite, ironstone and millstone being annually raised.
There is trade in coal, but 1 i.
The mineral wealth of Baden is not great; but iron, coal, zinc and lead of excellent quality are produced, and silver, copper, gold, cobalt, vitriol and sulphur are obtained in small quantities.
The dock is specially designed and equipped for dealing with the coal, timber, grain and wool trades.
Long jetties spring out on either side of the entrance, curving round about midway in order to run parallel to the river, thus forming a huge funnelshaped entrance; the eastern jetty forms a landing-stage for passenger traffic and the western is designed for the shipment of bunker and cargo coal.
Eight hydraulic hoists, of the most up-to-date pattern, are capable of shipping 5,600 tons of coal per hour.
Imports include cotton and silk goods, coal, iron and steel, petroleum, timber, raw wool, cotton yarn and cork.
Next in importance comes the mining of brown coal, which has also been carried on for a long time.
Cod-liver oil and salted fish are exported with some reindeer-skins, fox-skins and eiderdown; and coal and salt for curing are imported.
The convenience also with which the energy of waterfalls can be converted into electric energy has led to the introduction of chemical industries into countries and districts where, owing to the absence of coal, they were previously unknown.
The same inventor has patented the application of electrolysed chlorides to the purification of starch by the oxidation of less stable organic bodies, to the bleaching of oils, and to the purification of coal gas, spirit and other substances.
Coal is mined in the neighbourhood.
Coal is mined in the vicinity; the city has a large trade with the surrounding agricultural district (whose distinctive product is beans); the Michigan Central railway has car and machine shops here; and the city has many manufacturing establishments.
It dates from the completion of the railway to the coal mines of Naricual and Capiricual nearly 1 2 m.
It possesses excellent wharves, does a large import trade in coal, and has shipbuilding yards, breweries, distilleries, cloth aid paper factories, glass-works, copper-works, soap-works and rice mills.
Charleston is in the midst of a region rich in bituminous coal, the shipment of which by river and rail constitutes one of its principal industries.
It is near the great mineral deposits of Virginia, Tennessee, West Virginia, Kentucky and North Carolina; an important distributing point for iron, coal and coke; and has tanneries and lumber mills, iron furnaces, tobacco factories, furniture factories and packing houses.
The town has two interesting museums. Emden is the seat of an active trade in agricultural produce and live-stock, horses, timber, coal, tea and wine.
Bituminous coal, natural gas and oil abound in the vicinity; the river provides excellent water-power; the borough is a manufacturing centre of considerable importance, its products including iron and steel bridges, boilers, steam drills, carriages, saws, files, axes, shovels, wire netting, stoves, glass-ware, scales, chemicals, pottery, cork, decorative tile, bricks and typewriters.
Devoting himself to the economic side of geology in various parts of North America, he was enabled to bring out in 1861 A Practical Treatise on Coal, Petroleum and other Distilled Oils.
Coal and iron are wrought in the neighbourhood.
Lebanon has thick deposits of lignite coal, but of inferior quality owing to the presence of iron pyrites.
Coal has not been found, but peat may be exploited under favourable economic conditions.
The year 1890 was one of great depression following the exhaustion of the surface ore, but the provision of better machinery and cheaper coal led to a revival in 1891.
Large quantities of timber are imported from Canada and Norway; coal, iron, manufactured goods and agricultural produce are the chief exports.
It is on the Glasgow & South-Western railway, and has a harbour and dock from which coal and goods are the main exports.
Although the state is supposed to have several of the minerals found in this part of Mexico (silver, cinnabar, iron, lead, gold, petroleum and coal), its mining industries continue undeveloped and neglected.
Brown coal is obtained at the entrance of Shag valley, 40 m.
The Carpathian system is richer in metallic ores than any other mountain system of Europe, and contains large quantities of gold, silver, copper, iron, lead, coal, petroleum, salt, zinc, &c., besides a great variety of useful mineral.
It has a considerable trade in oil and coal and in the agricultural products of the surrounding region, and has various manufactures.
The town has a handsome church (Early English and Decorated), a grammar school, and some trade in coal, timber, malt and cheese.
A marine force was raised to stop smuggling; and the subtraction of coal during coaling operations was stopped by drastic legislation.
The main imports were coal, timber, metals, jute.
The town lies between the valleys of the Ehen and its tributary the Dub Beck, in a district rich in coal and iron ore.
The city is in one of the most productive coal regions of the state, has a large jobbing trade, and is an important centre for the insurance business.
Sulphuretted ores are smelted, either with or without a preliminary calcination, with metallic iron; calcined ores may be smelted with carbon (coal).
Calcination in reverberatory furnaces and a subsequent smelting in the same type of furnace with the addition of about 3% of coal, lime, soda and fluorspar, has been adopted for treating the Bolivian ores, which generally contain the sulphides of bismuth, copper, iron, antimony, lead and a little silver.
Grain and fruit are grown in large quantities, and much coal is mined in the vicinity of Kirksville.
It has various industries, including saw and planing mills, shipbuilding, glassworks and factories for wood-pulp, barrels and potato flour; and an active trade in exporting timber, ice, wood-pulp and granite, chiefly to Great Britain, and in importing from the same country coal and salt.
The development of manufacturing in Delaware has not been so extensive as its favourable situation relative to the other states, the facilities for water and railway transportation, and the proximity of the coal and iron fields of Pennsylvania, would seem to warrant.
In mining, a "gouge" is the layer of soft rock or earth sometimes found in each side of a vein of coal or ore, which the miner can scoop out with his pick, and thus attack the vein more easily from the side.
Coal and other minerals have been discovered.
Coal, textiles and iron and steel goods figure prominently amongst the imports, and emery, leather, lemons, sponges, flour, valonia and iron ore amongst the exports.
The chief exports are stone for road-making, butter, eggs and vegetables; the chief imports are coal, timber, superphosphates and wine from Algeria.
The vicinity abounds in coal, but is principally agricultural, and Clinton's chief interest is in trade with it.
In its most general sense the term " coal " includes all varieties of carbonaceous minerals used as fuel, but it is now usual in England to restrict it to the particular varieties of such minerals occurring in the older Carboniferous formations.
On the continent of Europe it is customary to consider coal as divisible into two great classes, depending upon differences of colour, namely, brown coal, corresponding to the term "lignite" used in England and France, and black or stone coal, which is equivalent to coal as understood in England.
Stone coal is also a local English term, but with a signification restricted to the substance known by mineralogists as anthracite.
In France and Belgium, however, a peculiar word, houille, is generally used to signify mineral coal.
Littre suggests that it may be related to the Gothic haurja, coal.
Anthracite is from the Greek a vepa, and the term lithanthrax, stone coal, still survives, with the same meaning, in the Italian litantrace.
It must be borne in mind that the signification now attached to the word coal is different from that which formerly obtained when wood was the only fuel in general use.
Coal then meant the carbonaceous residue obtained in the destructive distillation of wood, or what is known as charcoal, and the name collier was applied indifferently to both coal-miners and charcoal-burners.
The spelling " cole " was generally used up to the middle of the 17th century, when it was gradually superseded by the modern form, " coal."
Coal is an amorphous substance of variable composition, and therefore cannot be as strictly defined as a crystallized or definite mineral can.
Lignite and cannel are usually dull and earthy, and of an irregular fracture, the latter being much tougher than the black coal.
As a rule, the density increases with the amount of carbon, but in some instances a very high specific gravity is due to intermixed earthy matters, which are always denser than even the densest form of coal substance.
These peculiarities of structure may vary very considerably within small areas; and the position of the divisional planes or cleats with reference to the mass, and the proportion of small coal or slack to the larger fragments when the coal is broken up by cutting-tools, are points of great importance in the working of coal on a large scale.
Salt, in the form of brine, is sometimes present in coal.
Hydrocarbons, such as petroleum, bitumen, paraffin, &c., are also found occasionally in coal, but more generally in the associated sandstones and limestones of the Carboniferous formation.
Gases, consisting principally of light carburetted hydrogen or marsh gas, are of ten present in considerable quantity in coal, in a dissolved or occluded state, and the evolution of these upon exposure to the air, especially when a sudden diminution of atmospheric pressure takes place, constitutes one of the most formidable dangers that the coal miner has to encounter.
The classification of the different kinds of coal may be considered from various points of view, such as their chemical composition, their behaviour when subjected to heat aa s sifica= or when burnt, and their geological position and iron.
This class of c coal burns with a very small amount of flame, produc ing intense local heat and no smoke.
The term is, however, a convenient one, and one whose use is almost a necessity, from its having an almost universal currency among coal miners.
This excess is greatest in what is Gas known as cannel coal, the Lancashire kennel or candle coal, so named from the bright light it gives out when burning.
Cannel is more compact and duller than ordinary coal, and can be wrought in the lathe and polished.
In Nassau and Bavaria woody structure is very common, and it is [[Table I]].-Elementary Composition of Coal (the figures denote the amounts per cent).
When coal is heated to redness out of contact with the air, the more volatile constituents, water, hydrogen, oxygen, and nitrogen are in great part expelled, a portion of the carbon being also volatilized in the form of hydro carbons and carbonic oxide,-the greater part, however, remaining behind, together with all the mineral matter or ash, in the form of coke, or, as it is also called, " fixed carbon."
The former class undergo an incipient fusion or softening when heated, so that the fragments coalesce and yield a compact coke, while the latter (also called free-burning) preserve their form, producing a coke which is only serviceable when made from large pieces of coal, the smaller pieces being incoherent and of no value.
Lignite or brown coal includes all varieties which are intermediate in properties between wood and coals of the older.
A coal of this kind is generally to be Lignite distinguished by its brown colour, either in mass or in the blacker varieties in the streak.
By the term " ash " is understood the mineral matter remaining unconsumed after the complete combustion of the carbonaceous portion of a coal.
It may also be rendered visible if a smooth block of free-burning coal is allowed to burn away quickly in an open fire, when the ash remains in thin grey or yellow bands on the surface of the block.
The composition of the ash of true coal approximates to that of a fire-clay, allowance being made for lime, which may be present either as carbonate or sulphate, and for sulphuric acid.
An indication of the character of the ash of a coal is afforded by its colour, white ash coals being generally freer from sulphur than those containing iron pyrites, which yield a red ash.
In this coal, as well as in the lignite of Tasmania, known as white coal or Tasmanite, the sulphur occurs in organic combination, but is so firmly held that it can only be very partially expelled, even by exposure to a very high and continued heating out of contact with the air.
Under ordinary conditions, from s to 4 of the whole amount of sulphur in a coal is volatilized during combustion, the remaining 4 to being found in the ash.
It is generally largest in lignites, which may sometimes contain 30% or even more, while in the coals of the coal measures it does not usually exceed from 5 to io%.
By making very thin sections and employing high magnification (1000-1200 diameters), Renault has been enabled to detect numerous forms of bacilli in the woody parts preserved in coal, one of which, Micrococcus carbo, bears a strong resemblance to the living Cladothrix found in trees buried in peat bogs.
Clearer evidence of their occurrence has, however, been found in fragments of wood fossilized by silica or carbonate of lime which are sometimes met with in coal seams.
The subsequent change of peaty substance into coal is probably due to geological causes, i.e.
Such changes seem, however, to have been very rapidly accomplished, as pebbles of completely formed coal are commonly found in the sandstones and coarser sedimentary strata alternating with the coal seams in many coalfields.
The variation in the composition of coal seams in different parts of the same basin is a difficult matter to explain.
We might therefore expect to find coal wherever strata of estuarine origin are developed in great mass.
This is actually the case; the Carboniferous, Cretaceous and Jurassic systems (qq.v.) contain coal-bearing strata though in unequal degrees,- the first being known as the Coal Measures proper, while the others are of small economic value in Great Britain, though more productive in workable coals on the continent of Europe.
The Coal Measures which form part of the Palaeozoic or oldest of the three great geological divisions are mainly confined to the countries north of the equator.
The nature of the Coal Measures will be best understood by v1.19 considering in detail the areas within which they occur in Britain, together with the rocks with which they are most intimately associated.
In the southern coalfields it is usually known by the miners' name of " Farewell rock," from its marking the lower limit of possible coal working.
The Coal Measures, forming the third great member of the Carboniferous series, consist of alternations of shales and sandstones, with beds of coal and nodular ironstones, which together make up a thickness of many thousands of feet - from 12,000 to 14,000 ft.
The uppermost portion of the Coal Measures consists of red sandstone so closely resembling that of the Permian group, which are next in geological sequence, that it is often difficult to decide upon the true line of demarcation between the two formations.
These are not, however, always found together, the Coal Measures being often covered by strata belonging to the Trias or Upper New Red Sandstone series.
The areas containing productive coal measures are usually known as coalfields or basins, within which coal occurs in more or less regular beds, also called seams or veins, which can often be followed over a considerable length of country without change of character, although, like all stratified rocks, their continuity may be interrupted by faults or dislocations, also known as slips, hitches, heaves or troubles.
The thickness of coal seams varies in Great Britain from a mere film to 35 or 40 ft.; but in the south of France and in India masses of coal are known up to 200 ft.
In some instances the coal seams may be changed as a whole, as for instance in South Wales, where the coking coals of the eastern side of the basin pass through the state of dry steam coal in the centre, and become anthracite in the western side.
Coal has also been found in Kent, in the neighbourhood of Dover.
In Scotland coal is worked at various points (principally in the west) in the Clyde-Forth lowlands..
Coal has also been found in an extension northward from this field towards Antwerp, while westward the same field extends into north-eastern France.
Coal is widely distributed in Germany.
Coal is pretty widely distributed in Spain, and occurs in several districts in the Balkan peninsula.
The European region poorest in coal (proportionately to area) is Scandinavia, where there is only one field of economic value - a small one in the extreme south of Sweden.
Coal is worked to some extent in Sumatra, British North Borneo, and the Philippine Islands.
In Arkansas, Oklahoma and Texas, and along the line of the Rocky Mountains, extensive fields occur, producing lignite and bituminous coal.
Coal is known at several points in Alaska, and there are rich but little worked deposits in Mexico.
In South America coal is known in Venezuela, Colombia, Peru, northern Chile, Brazil (chiefly in the south), and Argentina (Parana, the extreme south of Patagonia, and Tierra del Fuego), but in no country are the workings extensive.
Africa is apparently the continent poorest in coal, though valuable workings have been developed at various points in British South Africa, e.g.
Australia possesses fields of great value, principally in the south-east (New South Wales and Victoria), and in New Zealand considerable quantities of coal and lignite are raised, chiefly in South Island.
The questions, what is the total amount of available coal in the coalfields of Great Britain and Ireland, and how long it may be expected to last, have frequently been discussed since the early part of the 19th century, and particular attention was directed to them after the publication of Stanley Jevons's book on The Coal Question in 1865.
Although in the years 1870-1903 the amount raised was 5,694,928,507 tons, this later estimate was higher by 10,707,382,769 tons than that of the previous commission, the excess being accounted for partly by the difference in the areas regarded as productive by the two commissions, and partly by new discoveries and more accurate knowledge of the coal seams. In addition it was estimated that in the proved coalfields at depths greater than 4000 ft.
In 1873 there could be seen, in the thick coal seams of Bengal, near Raniganj, a seam about 50 ft.
The operations by which the coal is reached and laid out for removal are known as " winning," the actual working or extraction of the coal being termed " getting."
When the field is won by the former method, the coal lying above the level is said to be "level-free."
The mode of winning by level is of less general application than that by shafts, as the capacity for production is less, owing to the smaller size of roadways by which the coal must be brought to the surface, levels of large section being expensive and difficult to keep open when the mine has been for some time at work.
A more cogent reason, however, is to be found in the fact that the principal coalfields are in flat countries, where the coal can only be reached by vertical sinking.
The actual coal measure strata, consisting mainly of shales and clays, are generally impervious to water, but when strata of a permeable character are sunk through, such as the magnesian limestone of the north of England, the Permian sandstones of the central counties, or the chalk and greensand in the north of France and Westphalia, special methods are required in order to pass the water-bearing beds, and to protect the shaft and workings from the influx of water subsequently.
The freezing machines were kept at work for 200 days, and 2191 tons of coal were consumed in supplying steam for the compressors and circulating pumps.
Poetsch in 1883, and originally applied to shafts passing through quicksands above brown coal seams, has been applied with advantage in opening new pits through the secondary and tertiary strata above the coal measures in the north of France and Belgium, some of the most successful examples being those at Lens, Anzin and Vicq, in the north of France basin.
The laying out of a colliery, after the coal has been won, by sinkings or levels, may be accomplished in various ways, according to the nature of the coal, its thickness and dip, and the extent of ground to be worked.
Where a large area cannot be commanded, it is best to sink to the lowest point of the field for the convenience of drawing the coal and water which become level-freein regard to the pit.
Where properties are much divided, it is always necessary to maintain a thick barrier of unwrought coal between the boundary of the mine and the neighbouring workings, especially if the latter are to the dip. If a prominent line of fault crosses the area it may usually be a convenient division of the fields into sections or districts.
The first process in laying out the workings consists in driving a gallery on the level along the course of the coal seam, which is known as a " dip head level," and a lower parallel one, in which the water collects, known as a " lodgment level."
The junction of the levels with the pit is known as the " pit eye "; it is usually of an enlarged section, and lined with masonry or brick-work, so as to afford room for handling the wagons or trams of coal brought from the working faces.
The removal of the coal after the roads have been driven may be effected in many different ways, according to the custom of the district.
A portion of this may be got by the process known as robbing the pillars, but the coal so obtained is liable to be very much crushed from the pressure of the superincumbent strata.
A coal seam with a soft pavement and a hard roof is the most subject to a " creep."
This accident generally arises from an improper size of pillars; some roofs, however, are so difficult to support that sits take place where the half of the coal is left in pillars.
In the Northumberland steam coal district, where it is carried out in the most perfect manner, the bords are 5 to 6 yds.
In the same figure is also shown the method of working whole coal and pillars at the same time, a barrier of two or three ranges of pillars or a rib of solid coal being left between the working in the solid and those in the pillars.
By this method the whole of the coal is got backwards, the main roads being kept in solid coal; the intermediate levels not being driven till they are wanted, a greater amount of support is given, and the pillars are less crushed than is usual in pillar working.
The second great principle of working is that known as longwall or long-work, in which the coal is taken away either in broad faces from roads about 40 or 50 yds.
The principal road extends from the shafts southward; and on both sides of it the coal has been removed from the light-shaded area by cutting it back perpendicularly towards the boundaries, along faces about 50 yds.
The roads for drawing the coal from the working faces to the shaft are kept open by walling through the waste or goaf produced by the fall of the unsupported roof.
Another method consists in driving towards the boundary, and taking the coal backward towards the shafts, or working homeward, allowing the waste to close up without roads having to be kept open through it.
This is of course preferable, but is only applicable where the owner of the mine can afford to expend the capital required to reach the limit of the field in excess of that necessary when the raising of coal proceeds pari passu with the extension of the main roads.
Against these advantages must be placed the difficulties attending the maintenance of roads through the goaves, and in some cases the large proportion of slack to round or large coal obtained.
Pillar working, in the whole coal, is generally reputed to give a more advantageous proportion of round coal to slack, the latter being more abundantly produced on the removal of the pillars, but as these form only a small portion of the whole seam, the general yield is more advantageous than in the former method.
The ventilation of pillar working is often attended with difficulty, and the coal is longer exposed to the influence of the air, a point of importance in some coals, which deteriorate in quality when exposed to a hot damp atmosphere.
Where the whole of the coal is removed at once there is less chance of surface damage, when the mines are deep, than with pillar workings.
The most typical example of this kind of working in England is afforded by the thick coal of South Staffordshire, which consists of a series of closely associated coal seams, varying from 8 to 12 or 13, divided FIG.
The main level or gate road is driven in the benches coal, or lower part of the seam, while a smaller drift for ventilation, called an air heading, is carried above it in one of the upper beds called the slipper coal.
The order in which the coal is cut is shown in the dotted and numbered squares in the figure.
The coal is first cut to the top of the slipper coal from below, after which the upper portion is either broken down by wedging or falls of itself.
About onehalf of the total coal (or less) is obtained in the first working; the roof is then allowed to fall, and when the gob is sufficiently consolidated, fresh roads are driven through it to obtain the ribs and pillars left behind by a second or even, in some cases, a third, _!?/i _ ?
The loss of coal by this method is very considerable, besides great risk to life and danger from fire.
A level is driven in a sandstone forming the floor, along the course of the coal, into which communications are made by cross cuts at intervals of 16 yds., which are driven across to the roof, dividing up the area to be worked into panels.
These are worked backwards, the coal being taken to a height of 20 ft., the opening being packed up with stone sent down from the surface.
In France and Germany the method of filling the space left by the removal of the coal with waste rock, quarried underground or sent down from the surface, which was originally used in connexion with the working of thick inclined seams by the method of horizontal slices, is now largely extended to long-wall workings on thin seams, and in Westphalia is made compulsory where workings extend below surface buildings, and safety pillars of unwrought coal are found to be insufficient.
In some anthracite collieries in America the small coal or culm and other waste are washed into the exhausted workings by water which gives a compact mass filling the excavation when the water has drained away.