Underground Treasures

 
Inscribed

TO

ROSSITER W. RAYMOND, PH. D.,

UNITED STATES

Commissioner of Mining Statistics;

EDITOR OF THE

ENGINEERING AND MINING JOURNAL;

AUTHOR OF

“The Mines of the West,” etc.

This little work was not written for mineralogists, but expressly for the landholder, the farmer, the mechanic, the miner, the laborer, even the most unscientific. It is designed to enable such to discover for themselves, minerals and ores of use in the arts, and thus develop the resources and ascertain the value of any particular farm or region. It may save the owner from ruinous bargains, and may reveal a mine of mineral wealth, more sure and more profitable than any bank.

A   K E Y
FOR THE READY DETERMINATION OF ALL
THE USEFUL MINERALS WITHIN THE
UNITED STATES.

MINERALS head the list of the sources of our nation’s wealth. Gold, iron, coal and marble have not only contributed largely to the enterprise and opulence of America, but at this very moment they exert a commanding influence in political circles. No one can prophesy the greatness of the commercial power which is sure to rise on their foundations.

No other country can boast of such vast and valuable mineral deposits. Yet our country is not half developed. Treasures lie undiscovered in our mountains and under our farms,—gems of “purest ray serene” and still more precious metals. Some will be accidentally brought to light; but the majority are so disguised that their real nature is not seen. How unpromising are the best ores of iron, zinc and silver and the rarest gems! Then, again, there is “mimicry” in the mineral kingdom; worthless stones are often good imitations of the valuable, and fortunes have been sunk in mining pyrites for gold, mica for silver and slate for coal. But if we wait for mineralogists to develop our mineral resources, we must wait a millenium, our country is so vast and scientific laborers so few. Fortunately, however, nature has stamped upon each mineral some peculiar feature or assemblage of characters which enable any one with average common sense to distinguish those which are of value in the arts.

The object of this work is to point out those distinctions so clearly and in popular language that those who do not claim to be scientific may determine specimens for themselves; in other words, to furnish a key for the ready determination of all the useful minerals within the United States.[1]

Two hundred and forty-four mineral species have been found within the bounds of the Union. Of these only one-third are of any use to the practical man. These eighty have certain general characters in common, but always some specific differences. The object is to divide them into groups, as the botanist divides the plants, and then to separate the individuals by some properties or features peculiar to each. Only those minerals are mentioned which are useful: any specimen, therefore, which does not fit any of the descriptions given, may be considered of no special value. By the term “color,” is meant the color of a fresh fracture, for the exposed surface often misrepresents the true aspect. Exact color is not meant, but “red” stands for reddish, “yellow” for yellowish, “white” for a light gray up to the perfectly transparent. “Magnetic” means that the specimen disturbs the needle of a compass, or that a magnet will take up fine particles. A mineral is “opaque” if the light will not pass through either the edges or a thin fragment. A “translucent” mineral is either clear as crystal or only allows light to pass dimly through a thin portion. “Effervescence” is the bubbling produced by the escape of a gas, as in soda-water. “Gravity” is the weight compared with that of an equal bulk of water. In the majority of cases the specimen can be determined without it; but there may be several doubtful cases which can be settled only by obtaining the gravity. This is done by first weighing a fragment of the mineral in a small apothecary or jeweler’s balance, reckoning it in grains. Then by a thread suspend it below one of the scales in a tumbler of water, taking care that the specimen is covered with water and does not touch the sides. Subtract the weight in grains as it hangs in the water from the first weight, and divide the first weight by the difference: the result is the gravity. Five per cent. should be allowed for impurities. Where exactness is not required, the gravity of a specimen may be judged by comparing it with well-known substances. Thus,

If the gravity of a mineral is 1.5, a cubic inch of it will weigh about ¾ ounce; if 2., 1 oz.; if 2.5, 1¼ oz.; if 3., 1½ oz.; if 4., 2 oz.; if 5, 2½ oz., etc.

There is no section of our country that may not reward a diligent search for precious or useful minerals. The rocks, however, between the Alleghanies and the Atlantic and between the Rocky Mountains and the Pacific furnish the greater variety and abundance. Here are found the best ores. Gold and silver seem to abound more on the western than eastern sides of both mountain-chains. A trap-region, like the shore of Lake Superior and the Connecticut River Valley, is likely to be a good locality for copper and iron. The Mississippi Valley, or the region of Bituminous Coal, furnishes chiefly iron and lead; gold, silver and copper are seldom found. In general, where the layers of rock lie level and contain fossil shells, it is a locality good only for soft coal, (New York excepted), iron ore, gypsum and salt. The regions of granite, slate, limestone, marble, etc., offer the greatest inducement to search for useful minerals.

FIRST see whether it will scratch common window-glass. If it will make the least mark, it belongs to division A; if not, it is to be found in group B. Next notice whether the light will shine through it: if it does not pass through even the edges or a thin splinter, it is opaque; if any light is allowed to pass, it is translucent. With a knife see if it is harder or softer than pure white marble; then, noting its color, compare it with the descriptions of minerals referred to by the numbers. If it agree with none, it may be considered of no use in the arts. To make doubly sure, get the gravity as described on page 12.

Examples: Suppose we have an unknown mineral in hand. We first try to scratch glass with it and find it impossible. It therefore belongs to section B. Next we find it is opaque and yellow, and evidently heavier and harder than marble. It must be one of two: 44 attracts the compass-needle, and this will not; it is consequently 26 or Copper Pyrites, if it agree with the description. If not, it is something of no great value.

You have found what you think is a diamond, Does the specimen scratch glass? Yes, easily, and is brittle. Can you see through it? You say it is clear as glass. Look now under section A, “translucent” series, number 6 (for it is colorless), and decide which of the four it is. The first one (27), is diamond; but do not let your wishes make it agree. Turning to the description, you read that it can not be scratched with a file or worn down on a grindstone. This decides against it. Besides, the gravity (2.5) is too little. With the next (57) it agrees perfectly, and you need not go further. Should the specimen, however, agree very well with rock crystal, only that its gravity (3.5) is too great, then it is topaz.

☞ All minerals that scratch glass are brittle, and all (save 32 and 46) are infusible or melt with great difficulty.

☞ The following minerals will burn, evaporate or melt without a flux in an ordinary fire: Nos. 2, 4, 5, 7, 10, 13, 14, 16, 18, 19, 21, 23, 24, 26, 29, 33, 35, 37, 44, 53, 55, 62, 63, 70, 71, 75. All but the following are heavier than marble: 2, 4, 6, 7, 10, 14, 16, 34, 36, 40, 47, 48, 56, 60, 61, 69, 71. Nos. 2, 50 and 58 alone dissolve in water.

☞ In determining color, be sure you have a fresh surface, for the outside is often deceptive. By “blow-pipe” is meant the tapering tube used by watch-makers.

WILL SCRATCH GLASS.

WILL NOT SCRATCH GLASS.

THIS stone is a mixture of several kinds of quartz, mainly the white, red, brown and black, disposed in layers or clouds. The layers are zigzag, circular or in straight bands (onyx). Occurs in irregular rounded masses; not very translucent; not altered by heat or acids; cannot be cut with a knife nor split into plates; takes a high polish; lustre glassy; gravity 2.5.

Value.—Used for jewelry and ornamental work, mortars, vases, knife-handles, burnishers, etc. The colors are deepened by boiling in oil and then in sulphuric acid.

Localities.—Found in granite and trap regions, generally by the shores of rivers, lakes and the sea; as, north-west shore of Lake Superior; Missouri, Columbia, Colorado and Connecticut Rivers; Crescent City, Cal.; Hancock County, Ga.; near Tampa Bay, Fla.; Fulton, Penn.; Yellowstone Lake, Wy.[3]

Occurs in mealy or solid crusts, often fibrous; dissolves in water; tastes sweetish-astringent; melts and froths up when heated.

Value.—Extensively used in dyeing and calico-printing, candle-making, dressing skins, clarifying liquors and in pharmacy.

Localities.—Found incrusting and impregnating dark slaty rocks, with yellow streaks. Cape Sable, Md.; Cleveland County, N. C.; coal slates on Ohio River, and in caves in Sevier, De Kalb, Coffee and Franklin Counties, Tenn.; also Esmeralda and Storey Counties, Nev.

Same as Rock Crystal, but colored purple or bluish violet. Generally in clustered crystals.

Value.—When clear and finely colored, it is a favorite gem.

Localities.—Usually found with agate. Keweenaw Point, Pic Bay and Gargontwa on Lake Superior; Bristol, R. I.; Surry, N. H.; East Bradford, Aston, Chester, Thornbury, Edgemont, Sadsbury, Birmingham, Middletown and Providence, Penn.; Greensboro, N. C.

Occurs massive; compact; high lustre; brittle; breaks with a curved surface; will not scratch marble; burns, but not readily, with a pale blue flame and little smoke; will not form coke by roasting; gravity 1.4 to 1.8.

Value.—Used for fuel and sometimes cut into inkstands, etc.

Localities.—Found in beds between slates and sandstones, and east of the Alleghany range only, as Eastern Pennsylvania; Portsmouth, R. I.; Mansfield, Mass.; North Carolina. No workable beds will be found in New York.

The rocks in anthracite regions are tilted, bent and broken, never level to any great extent. Impressions of leaves are good indications.

Occurs fibrous or granular; color lead gray, often tarnished; shining lustre, brittle; but thin pieces can be cut off with a knife; melts in a candle, at a high heat passing off in vapor; gravity 4.5.

Value.—The source of the antimony of commerce, containing seventy per cent.

Localities.—Found associated with Silver, Spathic Iron, Blende, Baryta and Quartz. Carmel, Me.; Lyme, N. H.; Soldier’s Delight, Md.; Aurora, Nev.; San Amedio Cañon and Tulare County, Cal.

Occurs finely fibrous, flax-like; flexible, not elastic; silky lustre, sometimes greenish; gravity 3.

Value.—Used for lining safes and steam-packing, and for making incombustible cloth, lamp-wicks, etc.

Localities.—Found in granite-regions east of the Alleghanies; often with Serpentine. Brighton, Dedham, Newbury, Pelham and Sheffield, Mass.; Milford, West Farms, Winchester and Wilton, Conn.; Chester, Mt. Holly and Cavendish, Vt.; Patterson, Phillipstown, Monroe and Staten Island, N. Y.; Brunswick, N. J.; East Nottingham, Goshen and Aston, Penn.; Bare Hills and Cooptown, Md.; Barnet’s Mills, Va.

Occurs massive; brittle; breaking with high lustre like hardened tar, and with curved surface; melts and burns readily with flame and smoke; gravity 1.2, sometimes floats on water.

Value.—Used for cements and varnishes.

Localities.—Found generally near the surface. Near the coast of Santa Barbara, Cal.; West Virginia, twenty miles south of Parkersburg.

Occurs in crystals and masses with glassy lustre, or earthy and dull; brittle; crackles and blackens, and finally fuses by heat; dissolves with effervescence in nitric acid; gravity 3.5.

Value.—A valuable ore of copper, containing sixty per cent.

Localities.—Found chiefly in lead and copper mines. Perkiomen lead mine, Cornwall, Phoenixville and Nicholson’s Gap, Pa; near New Brunswick, N. J.; near Mineral Point, Wis.; Polk County, Tenn.; Calaveras and Mariposa Counties, Cal.; near Virginia City, Mont.

Occurs in crystals, plates and masses; powder white; brittle; crackles when strongly heated; not dissolved in acids; easily distinguished by its weight; gravity 4.5, or twice as heavy as Gypsum.

Value.—Used extensively as white paint and in pottery.

Localities.—Found in mining districts, often with lead, copper and iron ores, and in limestone. Piermont, N. H.; Hatfield, Southampton and Leverett, Mass.; Cheshire and Berlin, Conn.; Pillar Point, Rossie, Carlisle, Scoharie, De Kalb, Gouverneur, N. Y.; Fauquier and Buckingham Counties, Va.; Union, Gaston and Orange Counties, N. C.; near Paris, and in Anderson, Fayette, Mercer and Owen Counties, Ky.; on Brown’s Creek and Haysboro, Tenn.; Bainbridge, O.; Scales Mound, Ill.; Prince Vein, Lake Superior; Mine-a-Barton, Mo.; near Fort Wallace, N. M.; Ingo County, Cal.

Occurs in masses, beds or seams; softer and duller than Anthracite; often a bright pitchy lustre; brittle, showing a slaty or jointed structure rather than curved surface; powder black; burns readily with yellow flame; by roasting forms coke; gravity 1.5 or less.

Value.—Used for fuel and the production of gas, coke, carbolic acid and aniline.

Localities.—Found west of Harrisburg, Pa., in rocks (slates and sandstones) less disturbed than in the Anthracite region. Western Pennsylvania; South-east Ohio; West Virginia; Eastern Kentucky and Tennessee to Tuscaloosa; North-west Kentucky; Illinois; Iowa; Missouri; Kansas; Arkansas; Northern Texas; Central Michigan; Owyhee County, Idaho; Deer Lodge and Gallatin Counties and sixty miles north-east of Bannock, Mont.

Occurs in crystals and masses; waxy lustre, but not always very apparent; usual color, rosin-yellow to dark brown; brittle; the powder, which is whitish to reddish-brown, dissolves in muriatic acid giving off the odor of rotten eggs; by roasting gives off sulphur-fumes; infusible alone, but on charcoal at a high heat gives off white fumes; gravity 4.

Value.—An ore of zinc (containing sixty-six per cent.) and a source of white vitriol. Often worked for its Silver and Gold.

Localities.—Found with lead and other ores. Lubec and Bingham, Me.; Eaton, Warren and Shelburne, N. H.; Sterling, Southampton and Hatfield, Mass.; Brookfield, Berlin, Roxbury and Monroe, Conn.; near Wurtzboro’, Cooper’s Falls, Mineral Point, Fowler, Ancram, Clinton and Spraker’s Basin, N. Y.; Wheatley and Perkiomen lead-mines, Schuylkill, Shannonville and Friedensville, Pa.; Austin’s lead-mine, Va.; Haysboro’, Brown’s Creek and Polk Counties, Tenn.; Prince Vein, Mich.; Dubuque, Ia.; Warsaw, Rosiclare and Galena, Ill.; Shullsburg, Wis.; Stillwater, Minn.

Occurs in masses or beds, looking much like hard brown earth; loose or porous and earthy, rather than compact and nodular; powder yellowish-brown; when strongly heated becomes black and magnetic; gravity nearly 4. An earthy yellow variety is called Yellow Ochre.

Value.—An important ore, yielding thirty-five per cent.

Localities.—Found in low, marshy grounds; widely distributed. Lebanon, N. H.; Berkshire and Plymouth Counties, Mass.; Columbia, St. Lawrence, Franklin and Jefferson Counties, N. Y.; New Limerick, Katahdin, Newfield, Shapleigh, Argyle, Clinton, Williamsburg and Lebanon, Me.; Darien and Martin Counties, Ind.; Monmouth County, N. J.; Somerset and Worcester Counties, Md.; Michigan, Ohio, Illinois, Wisconsin, etc.

Occurs in crystals and masses; metallic lustre; tarnishes yellow, gray and finally black; easily cut or broken; when heated gives off fumes of sulphur and antimony, affording a button of silver; dissolved in nitric acid, it silvers copper placed in it; gravity 6.

Value.—A rich ore of silver, containing over sixty per cent.

Localities.—Found in veins with other silver ores, in Nevada and Idaho.

Occurs like Bituminous Coal, but usually brownish-black with less lustre, and often showing a woody or slaty structure; powder always brown; contains fossil plants; gravity between 1.2 and 1.5.

Value.—Inferior to No. 10. Makes no coke. Can be used in the manufacture of alum.

Localities.—Found in thin veins or elliptical masses, never in extensive layers like Pennsylvania coal. Near Richmond, Va.; Deep River, N. C.; Michigan, Missouri, Texas; Evanston, Utah; Coal Creek and Bellmonte, Col.; Boreman, Dearborn River and Greenhorn Gulch, Mont.

Occurs in crystals and masses; glossy lustre; harder than marble; brittle; heated it swells up, becomes opaque and emits a green light; dissolves, when powdered, in hot sulphuric acid without effervescence; gravity 3.4.

Value.—An ore of zinc yielding from forty to sixty per cent.

Localities.—Found in limestone rock with other ores. Friedensville, Perkiomen, Phœnixville, Lancaster and Selin’s Grove, Pa.; Austin’s Mines in Wythe County, Va.; Claiborne County, Tenn.; Jefferson County, Mo.

Occurs in compact masses; dull lustre; brittle, breaking with a curved surface; burns readily but does not melt; does not soil the fingers; gravity about 1.2.

Value.—Used for fuel and for making gas, oil and ornaments.

Localities.—Found in the Mississippi Valley; Kentucky; Lick, Ohio; Illinois; Moniteau County, Mo.; Kenawha County, Va.; Beaver County, Pa.

Occurs in masses or pebbles; at first grayish, but by exposure to the sun becomes uniform flesh, red or brown, never striped,—although Carnelian may form one of the bands of an Agate; brittle, breaking with a curved surface; very hard; takes a fine polish; glassy or resinous lustre; gravity 2.6.

Value.—Used for jewelry. When of two layers, white and red, (properly called sardonyx,) it is used for cameos.

Localities.—Same as Agate.

Occurs crystallized, fibrous and massive; color white, often faint bluish; glassy lustre; very brittle; under the blow-pipe crackles and melts, tinging the flame red; does not dissolve in acids; gravity 4.

Value.—The source of nitrate of strontia, used in fire-works.

Localities.—Found in limestone, gypsum and sandstone. Rossie, Schoharie, Chaumont Bay, Depauville and Stark, N. Y.; Frankstown, Pa.; Strontian and Put-in-Bay Islands, Lake Erie; near Nashville, Tenn.; Fort Dodge, Iowa.

Occurs in crystals, in powder or masses; glassy lustre; brittle; dissolves in nitric acid with effervescence; heated strongly on charcoal crackles and fuses, giving a globule of lead; gravity 6.4.

Value.—A rich ore of lead yielding seventy-five per cent.

Localities.—Found in lead mines. Southampton, Mass.; Perkiomen, Phœnixville, Charlestown and Schuylkill, Pa.; Wythe County, Va.; Washington Mine, N. C.; Valle’s Diggings, Mine-la-Motte and Mine-a-Burton, Mo.; Davies and Rock Counties, Ill.; Blue Mounds, Wis.; Ingo County, Cal.

Occurs in compact masses; powder dark brown; small pieces sometimes attracted by the magnet; brittle, breaking with uneven surface; with borax melts into a green globule; not acted upon by acids; little lustre; gravity 4.4.

Value.—Used in making the chrome pigments.

Localities.—Found in Serpentine. Bare Hills, Cooptown and north part of Cecil County, Md.; Nottingham, W. Goshen, Williston, Fulton, Mineral Hill, Texas and Unionville, Pa.; Jay, New Fane, Westfield and Troy, Vt.; Chester and Blanford, Mass.; Loudon County, Va.; Yancy County, N. C.; North Almaden, New Idria and Coloma, Cal.

Occurs in granular or earthy masses; resembles iron-rust, but is a yellowish-red; powder scarlet; easily cut with a knife; thrown on red-hot iron, evaporates, giving off odor of sulphur; rubbed on copper, “silvers” it; gravity 9, or about as heavy as Copper.

Value.—The source of mercury (containing eighty-four per cent.) and vermilion.

Localities.—Found in slate and limestone rocks. Centreville, Coulterville, New Idria and New Almaden, and Lake and San Luis Obispo Counties, California; Idaho.

Occurs crystallized and massive; does not scratch glass easily; metallic lustre; tarnish, copper-red; powder, blackish-gray; brittle; heated on charcoal gives off sulphur fumes; heated with borax gives a blue glass; gravity 5.

Value.—An ore of cobalt, yielding twenty per cent.

Localities.—Usually found in slate or granite rocks with Copper Pyrites. Mineral Hill, Md.; Mine-la-Motte, Mo.

Occurs in irregular masses; metallic lustre; can be cut with a knife; malleable; ductile; fusible; gravity 8.8.

Value.—A source of copper and silver.

Localities.—Most abundant in the trap and “freestone” regions. New Brunswick, Somerville, Schuyler’s and Flemington, N. J.; Whately, Mass.; Cornwall and Shannonville, Pa.; Polk County, Tenn.; Keweenaw Point, Lake Superior; Calaveras, Amador and Santa Barbara Counties, Cal.; on Gila River, Ariz.

Occurs crystallized and massive; color, blackish lead-gray, often tarnished blue or green; nearly as hard as marble; brittle; a splinter will melt in a candle, giving off the odor of sulphur; dissolved in nitric acid, it will coat a knife-blade with copper; metallic lustre; gravity 5.5.

Value.—An ore of copper, yielding seventy-five per cent.

Localities.—Found at copper-mines. Simsbury, Bristol and Cheshire, Conn.; Schuyler’s Mines, N. J.; Orange County, Va.; near Newmarket, Md.; Lake Superior copper-region; La Paz, Arizona; Washoe, Humboldt, Nye and Churchill Counties, Nev.

Occurs in masses; metallic lustre; color pale copper-red; tarnishes gray to black; powder pale brownish-black; brittle; on charcoal melts giving the odor of garlic; becomes green in nitric acid; gravity 7.5.

Value.—An ore of nickel (containing forty-four per cent.) and arsenic.

Localities.—Found in granite regions. Chatham, Conn.

Occurs in crystals and masses; color brass-yellow; tarnishes green; metallic lustre when freshly broken; can be cut with a knife; brittle; powder greenish black; on charcoal melts giving off sulphur fumes; dissolves in nitric acid, making a green liquid; gravity 4.2.

Value.—If of a fine yellow hue, it is a valuable copper ore (yielding from twelve to forty per cent.) and source of blue vitriol.

Localities.—Found in mountainous or granite regions with other ores. Lubec and Dexter, Me.; Franconia, Unity, Warren, Eaton, Lyme, Haverhill and Shelburne, N. H.; Corinth, Waterbury and Strafford, Vt.; Southampton, Turner’s Falls, Hatfield and Sterling, Mass.; Bristol and Middletown, Conn.; Ancram, Rossie, Wurtzboro’ and Ellenville, N. Y.; Phœnixville and Pottstown, Pa.; Bare Hills, Catoctin Mountains, near Newmarket and Finksbury, Md.; Phœnix and Walton Mines, Va.; Greensboro, Charlotte and Phœnix Mines, N. C.; Hiwassee Mines, Tenn; Cherokee, Rabun and Habersham Counties, Ga.; Presque Island, Lake Superior; Mineral Point, Wis.; Union, Keystone, Empire and other mines, Calaveras County, La Victoire and Haskell claims in Mariposa County, Amador and Plumas Counties, Cal.; near Virginia City, Mont.

PROSPECTING DIAMOND DRILL.

Occurs in crystals and irregular angular masses; cannot be scratched by any other mineral or the file; brilliant lustre; feels cold to the touch; when rubbed on the sleeve exhibits electricity for hours; retains the breath but a short time; often tinged yellow, red, or green; gravity 3.5.

Value.—Used for jewelry, lenses and for cutting glass.

Localities.—Found in gold-regions, in river-washings of sand and pebbles; usually with coarse gold, but deeper down. Rutherford, Cabarras, Franklin and Lincoln Counties, N. C.; Hall County, Ga.; Manchester, Va.; Cherokee Ravine, N. San Juan, French Canal, Forrest Hill, Placerville and Fiddletown, Cal.

Occurs in granular masses, sometimes with bluish crystals; looks like fine grained iron ore; breaks with uneven surface; scratches quartz easily; very tough; brittle; gravity 4.

Value.—Used extensively as a cutting and polishing material.

Localities.—Found generally in limestone or granite with Magnetic Iron Ore. Chester, Mass.; Newlin and Unionville, Penn.; Macon and Guilford Counties, N. C.

Occurs in square crystals and in masses; glassy lustre; powder white; brittle; crackles when heated and then shines in the dark; does not effervesce with acids; is not scratched by marble; gravity 3.

Value.—Used as flux in glass and iron works.

Localities.—Found in limestone, granite, slate, etc., often at lead-mines. Blue Hill Bay, Me.; Westmoreland, N. H.; Putney, Vt.; Southampton, Mass.; Trumbull, Plymouth, Middletown and Willimantic, Conn.; Muscolonge Lake, Rossie and Johnsburg, N. Y.; near Franklin, N. J.; near Woodstock and Shepardstown, Va.; Smith County, Tenn.; Mercer County, Ky.; Gallatin County, along the Ohio, Ill. Castle Dome District, Ariz.

Occurs crystallized and in masses; generally made of coarse grains; brittle; powder dark reddish-brown; heated with soda turns bluish-green; dissolves in muriatic acid; gravity 5.

Value.—An ore of zinc.

Localities.—Found in limestone with Garnet and Zincite. Hamburg and Stirling Hill, N. J.

Occurs in crystals and masses; brilliant lustre; brittle; easily broken; powder, when finely rubbed is black; can be cut with a knife; heated it gives off sulphur and melts; dissolves in nitric acid leaving a white powder at the bottom; gravity 7.5—or a little heavier than cast-iron.

Value.—The main source of lead (yielding eighty per cent), and also smelted for the silver it contains. Used also in glazing stone-ware.

Localities.—Generally found in limestone with Iron Pyrites, zinc-ore, etc. That found in slate is richest in silver. Abounds in Missouri, Illinois, Iowa, Wisconsin and Arkansas; Rossie, Wurtzboro, Ancram, Macomb and Ellenville, N. Y.; Lubec, Blue Hill Bay, Bingham and Parsonsville, Me.; Eaton, Shelburne, Haverill, Warren and Bath, N. H.; Thetford, Vt.; Southampton, Leverett and Sterling, Mass.; Middletown and Roxbury, Conn.; Phœnixville, Charlestown, Schuylkill, Pequea Valley and Shannonville, Pa.; Austin’s and Walton’s Mines, Va.; Cabarras County, N. C.; Brown’s Creek and Haysboro, Tenn.; Chocolate River, Mich.; Ingo County, Cal.; on Walker’s River and Steamboat Springs, Nev.; Castle Dome and Eureka, Ariz.; Clear Creek County, Col.; Virginia City and Red Bluff Lode, Mont.; Cache Valley, Utah.

Occurs in crystals with four-sided faces; often nearly round; deep red, which grows darker by heat; rarely yellow; also in brown masses; melts at a high heat; brittle; not scratched by a knife; glassy lustre; gravity 4.

Value.—The clear deep red and yellow varieties are used for jewelry; the massive brown is ground for “emery.”

Localities.—Found in slate and granite rocks. Bethel, Parsonsfield, Phippsburg, Windham, Brunswick and Ranford, Me.; Hanover, Franconia, Haverhill, Warren, Unity, Lisbon and Grafton, N. H.; New Fane, Cabot and Cavendish, Vt.; Carlisle, Boxborough, Brookfield, Brimfield, Newbury, Bedford, Chesterfield and Barre, Mass.; Reading, Monroe, Haddam and Middletown, Conn.; Rogers’ Rock, Crown Point, Willsboro, Middletown, Amity, and near Yonkers, N. Y.; Franklin, N. J.; Pennsbury, Warwick, Aston, Knauertown, Chester, Leiperville and Mineral Hill, Pa.; Dickson’s Quarry, Del.; Hope Valley, Cal.; near Virginia City, on Yellowstone and Madison Rivers, Mont.

Occurs in scales, grains and nuggets, or disseminated through cellular quartz; metallic lustre; without tarnish; can be cut and hammered into thin plates; not dissolved by nitric acid; gravity 19, when pure and of a rich gold yellow color. The pale or brass yellow specimens are much lighter, the gravity being as low as 13. A grayish yellow gold, occurring in small, flat grains has a gravity of about 16.

Localities.—Found in veins of quartz running through greenish or grayish slates, the quartz at the surface being generally full of cavities and rusted, and the slates below the surface often containing little cubic crystals of Iron Pyrites: also in the valleys traversed by mountain-streams and in the river sands and gravel below. Iron and Copper Pyrites, Galena and Blende frequently contain gold. Masses of quartz and pyrites from the gold-regions, which make no show of gold, sometimes pay well; the value of such specimens can be

WASHING AURIFEROUS SANDS.

determined only by an assayer. Eastern range of Appalachians, as Habersham, Rabun, Clark, Hall, Lumpkin and Lincoln Counties, Ga.; Abbeville, Chesterfield, Union, Lancaster and Pickens Counties, S. C.; Montgomery, Cabarras, Mechlenburg, Burke and Lincoln Counties, N. C.; Spotsylvania, Buckingham, Fauquier, Stafford, Culpepper, Orange, Goochland and Louisa Counties, Va.; Dedham, Mass.; Bridgewater, Vt.; Canaan and Lisbon, N. H.; on Sandy River and Madrid, Me. Numberless points along the higher Rocky Mountains and western slope of Sierra Nevada, as near Santa Fe, Cerillos and Avo, New Mex.; San Francisco, Wauba and Yuma District, Ariz; between Long’s Peak and Pike’s Peak, Col.; Comstock Lode, Nev.; Owyhee, Boise and Flint Districts and Poorman Lode, Idaho; Emigrant and Alder Gulches, Red Bluff and near Jefferson River, Mont.; Josephine District, Powder, Burnt, and John Day Rivers, western slope of Cascade Mountains, and southern coast, Oregon; Tulare, Fresno, Mariposa, Tuolumne, Calaveras, El Dorado, Placer, Nevada, Yuba, Sierra, Butte, Plumas, Shasta, Siskiyou Amador and Del Norte Counties, Cal. Rare in the coal-regions and Mississippi Valley.

Occurs in foliated, scaly and granular masses; can be cut into thin slices, which are flexible, but not elastic; impressible by the nail; feels greasy; leaves a shining trace on paper; metallic lustre; not altered by heat or acids; gravity 2.

Value.—Used for pencils, polishing, glazing, for making steel, crucibles, overcoming friction, etc.

Localities.—Found in granite, slate and limestone rocks. Sturbridge, North Brookfield, Brimfield, Hinsdale and Worthington, Mass.; Cornwall and Ashford, Conn.; Brandon, Vt.; Woodstock, Me.; Goshen, Hillsboro and Keene, N. H.; Ticonderoga, Fishkill, Roger’s Rock, Johnsburg, Fort Ann, Amity, Rossie and Alexandria, N. Y.; Franklin and Lockwood, N. J.; Southampton and Buck’s County, Penn.; on the Gunpowder, Md.; Albemarle County, Va.; Wake, N. C.; Tiger River and Spartanburgh, S. C.; Sonora, Cal. (The soft black slate, often mistaken for Graphite, leaves a coaly trace on paper not a shining streak.)

Occurs in crystallized or granular masses; metallic lustre; color between steel-gray and iron-black; brittle; the powder dissolved in nitric acid makes a brownish green solution; melts at a red heat; gravity 5.

Value.—An ore of copper, (containing thirty-three per cent.) and silver, of which Nevada specimens have sixteen per cent.

Localities.—Found with gold, silver and lead. Kellogg Mines, Ark.; Mariposa and Shasta Counties, Cal.; Sheba and De Soto Mines, and near Austin, Nev.; Heintzelman and Santa Rita Mines, Arizona.

Occurs in plates, fibres coarse and fine, and massive; pearly or glistening; powder white, which if heated and mixed with water, turns hard; does not dissolve in sulphuric acid; may be scratched by the nail; gravity 2.3.

Value.—Used for stucco, manure, glazing, statuary, manufacture of glass, etc. A variety, called Satin Spar, worked into necklace beads and other ornaments, is finely fibrous and compact, taking a polish (though easily scratched,) and then resembles pearl or opal.

Localities.—Found with marl or clay, limestone and salt. Camillus, Manlius, Stark and Lockport, N. Y.; on the St. Mary’s and Patuxent, Md.; Washington County and Lynchburg, Va.; Charleston, S. C.; Poland, Ottawa and Canfield, O.; Davidson and Summer Counties, Tenn.; Grand Rapids and Sagenaw Bay, Mich.; Des Moines River, Iowa; Walker Lake and Six Mile Cañon, Nev.; Fort Dodge.

Occurs in crystals, wax-like masses, or in crusts; when scratched shows a shining streak; becomes brown on exposure; quite soft, easily cut; a small piece placed on zinc and moistened, swells up, turns black and shows metallic silver on being pressed with a knife; dissolves in hartshorn; gravity 5.5.

Value.—An ore of silver, yielding seventy per cent.

Localities.-Found in slate with other silver ores. Lake Superior Mining Region; Austin and Comstock Lode, Nev.; Willow Springs and San Francisco districts, Eldorado Cañon, Ariz.; Poorman Mine, Idaho.

Occurs in masses and square crystals; splendent lustre; color, bronze-yellow; brittle; strikes fire with steel; heated it gives off sulphur fumes; powder brownish; gravity 5.

Value.—Affords sulphur, copperas and alum. When found outside of the coal region, it often contains gold and silver.

Localities.—Found in all kinds of rocks. Bingham, Corinna, Farmington, Waterville, Brooksville, Peru and Jewett’s Island, Me.; Shelburne, Unity and Warren, N. H.; Baltimore, Hartford and Shoreham, Vt.; Heath, Hubbardston and Hawley, Mass.; Roxbury, Monroe, Orange, Milford, Middletown, Stafford, Colchester, Ashford, Tolland and Union, Conn.; Rossie, Malone, Phillips, Johnsburgh, Canton, Chester, Warwick and Franklin, Putnam and Orange Counties, N. Y.; Chester, Knauertown, Cornwall and Pottstown, Pa.; Greensboro’, N. C.; Mercer County, Ky.; Bainbridge, O.; Galena at Marsden’s Diggings, Ill.; on Sugar Creek, Ind.; mines of Colorado and California.

Occurs in masses, either in veins or as rounded stones; dull lustre, yet takes a high polish; breaks with a curved surface; not attacked by acids; is scratched by Rock Crystal; gravity 2.5.

Value.—Used for mosaics and other ornaments when compact, fine-grained and bright color.

Localities.—Found everywhere. Sugar Loaf Mountain and Machiasport, Me.; Saugus, Mass.; Castleton and Colchester, Vt.; Bloomingrove, N. Y.; Murphy’s, Col.; Red Bluff, Mont.

Occurs in beds; it is a fine, white clay, plastic when wet; when dry is scaly or compact; can be crumbled in the fingers and feels gritty; adheres to the tongue; does not dissolve in acids.

Value.—Used for the finest porcelain and for adulterating candy.

Localities.—Found generally with iron-ore and fire-clay. Common on the eastern slope of the Alleghanies; Branford, Vt.; Beekman, Athol, Johnsburgh and McIntyre, N. Y.; Perth Amboy, N. J.; Reading, Tamaqua and New Garden, Penn.; Mt. Savage, Md.; Richmond, Va.; Newcastle and Wilmington, Del.; Edgefield, S. C.; near Augusta, Ga.; Jacksonville, Ala.

Occurs in beds or masses, consisting of minute flattened grains; little lustre; generally soils the fingers; breathed upon has a clayey odor; color, brownish-red, powder more red; dissolves in strong muriatic acid with some effervescence; brittle; gravity 4.

Value.—An ore of iron yielding thirty-three per cent. Generally mixed with other ores at the furnace.

Localities.—Found in sandstone. Wayne, Madison, Oneida and Herkimer Counties, N. Y.; Marietta O.

Occurs in masses, with smooth rounded surfaces and fibrous structure; sometimes as hollow nodules, which are velvety-black inside; its powder when rubbed is yellowish-brown; when strongly heated turns black; scratches glass feebly; brittle; dissolves in hot aqua-regia; gravity 4.

Value.—A common ore of pig-iron, containing sixty per cent.; used also for polishing buttons, etc.

Localities.—Found in heavy beds with mica-slate, quartz, limestone, etc. Salisbury and Kent, Conn.; Amenia, Fishkill, Dover and Beekman, N. Y.; Richmond and Lenox, Mass.; Pittsfield, Putney, Bennington and Ripton, Vt.; Hamburgh, N. J.; Pikeland and White Marsh, Penn.; Marquette, Mich.; Makoquata River, Iowa; Iron Mountains, Stow and Green Counties, Mo.; Centerville, Ala.; near Raleigh and Smithfield, N. C.; on Coal Creek, Col.; and in coal areas generally.

Occurs in granular masses, coarse or fine; attracted by the magnet, or affecting the compass-needle; powder black; brittle; dissolves in muriatic acid; gravity 5.

Value.—An important ore, yielding sixty-five per cent.

Localities.—Found in granite, slate and limestone rocks. Warren, Essex, Clinton, Saratoga, Herkimer, Orange and Putnam Counties, N. Y.; Raymond and Marshall’s Island, Me.; Franconia, Jackson, Winchester, Lisbon, Swanzey and Unity, N. H.; Bridgewater, Chittenden, Marlboro, Rochester, Troy and Bethel, Vt.; Cambealon, R. I; Hawley and Bernardston, Mass.; Haddam, Conn.; Goshen, Webb’s Mine, Cornwall and White Marsh, Penn.; Hamburg, N. J.; Scott’s Mills and Deer Creek, Md.; Mitchell and Madison Counties, N. C.; Spartanburg, S. C.; Laclede and Crawford Counties, Mo.; Sierra County, (Gold Valley,) Plumas, Tulare, Mariposa, Placer and El Dorado Counties, Cal.

Occurs massive; brittle; deep orange-yellow; powder grayish-black; metallic lustre; tarnishes easily; slightly attracts the compass-needle; melts at a high heat, giving off sulphur-fumes; gravity 4.5.

Value.—Affords sulphur, copperas and nickel.

Localities.—Found in granite regions, often with copper and iron ores. Stafford, Corinth and Shrewsbury, Vt.; Trumbull and Monroe, Conn.; Port Henry, Diana and Orange County, N. Y.; Hurdstown, N. J.; Gap Mine, Lancaster County, Pa.; Ducktown Mines, Tenn.

Occurs in incrustations with smooth surface and fibrous; powder paler green than the mineral; brittle; by heat crackles and turns black; effervesces in acids; takes a fine polish, showing bands or rings; gravity 4.

Value.—Used for jewelry and inlaid work.

Localities.—Found in copper and lead mines. Cheshire, Conn.; Brunswick and Schuyler’s Mines, N. J.; Morgantown, Cornwall, near Nicholson’s Gap, Perkiomen and Phœnixville Lead Mines, Pa.; Petapsco Mines, Md.; Davidson County N. C.; Polk County, Tenn.; Left Hand River and Mineral Point, Wis.; Falls of St. Croix, Minn.; Jefferson County and Mine la Motte, Mo.; Calaveras County, Cal.; Big Williams’ Fork, Ariz.; Wild Cat Cañon and near Virginia City, Mont.

Occurs in masses; glassy lustre; color flesh or rose-red; becomes black on exposure; tough; melted with borax gives a violet-blue color; gravity 3.5.

Value.—Used in glazing stone-ware.

Localities.—Found in granite regions, often with iron-ore. Blue Hill Bay, Me.; Cummington, Warwick and Plainfield, Mass.; Irasburg and Coventry, Vt.; Winchester, and Hinsdale, N. H.; Cumberland, R. I.; Franklin and Hamburg, N. J.

Occurs coarse and fine granular; frequently veined or mottled; brittle; can be cut with a knife; takes a polish; effervesces with acids; reduced to quicklime by heat; a gray variety contains stems and joints of worm-like fossils; gravity 2.5.

Localities.—Brandon, Rutland, Dorset, Shoreham, Pittsford, Middlebury, Fairhaven, Cavendish, Lowell, Troy and Sudbury, Vt.; West Stockbridge, Egremont, Great Barrington, Lanesboro, New Ashford, Sheffield, New Marlboro, Adams, Cheshire and Stoneham, Mass.; Clinton, Essex, Dutchess, Onondaga, Putnam, St. Lawrence, Warren and Westchester, Counties, N. Y.; Smithfield, R. I.; New Haven, Milford, Conn.; near Philadelphia, N. J.; Texas and Hagerstown, Md.; Lancaster County, Pa.; Jefferson and Genevieve Counties, Mo.; Knox and Sevier Counties, Tenn.; Joliet, Ill.; Cherokee and Macon Counties, N. C.; Marquette, Mich.; near Deep River and on the Michigamig and Menominee Rivers, Wis.

Occurs in masses, which can be split into very thin, elastic leaves; pearly lustre; at a high heat becomes opaque; gravity 3.

Value.—Used for doors of stoves, etc.

Localities.—Found in granite regions. Buckfield, Freeport and Oxford, Me.; Acworth, Grafton and Alstead, N. H.; Chesterfield, Barre, Mendon, South Royalston, Brimfield, Goshen and Russell, Mass.; Monroe, Haddam and Middletown, Conn.; Warwick, Edenville, Edwards, Monroe and Greenfield, N. Y.; Pennsbury, Thornbury, Unionville, Middletown and Chestnut Hill, Pa.; Jones’ Falls, Md.

Resembles Specular Iron Ore, but consists of thin shining scales or leaves; powder dark red; a thin flake is translucent, showing red light; feels somewhat slippery.

Value.—Used as an ore of iron and for polishing.

Localities.—Hawley, Mass.; Piermont, N. H.; Ticonderoga, N. Y.; Warwick, Penn.; Loudon County, Va.

Occurs in thin crusts, delicate needles, or disseminated through the loose earth in caves; glossy lustre; brittle; cool, saline taste; crackles and burns brightly on live coals; a little harder than Gypsum.

Value.—Used in the manufacture of gunpowder, fulminating powders, nitric acid, etc.

Localities.—Marion County, Ky.; White County, Tenn.; near Rosiclare, Ill.; Silver Peak, Nev.

Occurs in masses and little columns, often with small rounded surfaces; one ore is soft enough to be impressed by the nail, and soils; the other will scratch glass faintly; heated with borax, makes a violet glass; dissolves in hot muriatic acid, giving forth a yellowish-green gas; gravity 4 to 5.

Value.—Used for bleaching and for obtaining oxygen.

Localities.—Found in granite regions, often with iron-ore. Brandon, Bennington, Monkton, Irasburg and Chittenden, Vt.; Hillsdale, Westmoreland and Westchester, N. H.; Plainfield, West Stockbridge and Conway, Mass.; Salisbury and Kent, Conn.; Montgomery County, Md.; Lake Superior Mining Region; Dubuque, Iowa; Deep Diggings, Mo.; Red Island, Cal.; Martinsburg, N. Y.

Occurs in grains or lumps; metallic, silvery lustre; can be hammered out; heavier and harder than silver; not dissolved in nitric acid; gravity 17.

Value.—Nearly equal to Gold. Used for making chemical and philosophical apparatus, for coating copper, brass, etc.

Localities.—Found in river-gravel with Gold. Rutherford County, N. C.; Klamath region, Cape Blanco, on Salmon River, South Fork of Trinity, Butte, Honcut, Cañon and Wood’s Creeks, and on Middle Fork of American River, Cal.; at Gold Flat, Nev.

Occurs in crystals and masses; cochineal-red; powder brownish-red; nearly opaque; brittle; dissolves in nitric acid; heated on charcoal yields a globule of copper; gravity 6.

Value.—Affords copper, (sixty per cent.,) and blue vitriol.

Localities.—Found in trap regions with other copper ores. Schuyler’s, Somerville, New Brunswick and Flemington Mines, N. J.; Cornwall, Pa.; Ladenton, N. Y.; Lake Superior Region. Not abundant.

54—Red Hematite.

Occurs in compact masses, with rounded surfaces or kidney-shaped; fibrous structure; color brownish-red to iron-black; but powder invariably red; when black, the lustre is somewhat metallic, otherwise dull; brittle; scratches glass with difficulty; dissolves slowly in strong muriatic acid; gravity 4.5 to 5.

Value.—An ore of iron, yielding from thirty-six to fifty per cent. In powder, used as pigment and for polishing metals.

Localities.—Found usually in beds with granite or limestone. Aroostook County and Hodgdon, Me.; Antwerp, Ticonderoga, Crown Point and Gouverneur, N. Y.; Vernon, N. J.; West Whiteland, Pa.; Chatham and Orange Counties, N. C.; Marquette, Mich; Shasta County, Cal. This mineral graduates into a soft, earthy variety, called red ochre, and into a compact, slaty variety, called red chalk, which has a clayey odor when breathed on.

Occurs in crystals and masses; metallic lustre; brittle; powder cochineal-red; easily cut; at a high heat yields a silver globule; the powder heated with potash turns black; gravity 6.

Value.—An ore of silver yielding sixty per cent.

Localities.—Found at gold and silver mines. Washoe and Austin, Nev.; Poorman Lode, Idaho.

Occurs in masses; wax-like; a trifle harder than marble; when fresh can be scratched by the nail; soapy feel; takes a polish; cleavable; gravity 2.8.

Value.—Used as a marble and worked into inkstands, etc.

Localities.—Found with steatite, serpentine, limestone, etc. Antwerp, Canton, Fowler, De Kalb, Edwards, Russell and Gouverneur, N. Y.

Occurs in crystals and masses; transparent; glassy lustre; colorless; tough; brittle; not acted upon by acids or heat; electric by friction; gravity 2.5.

Value.—Cut for ornaments, lenses, etc.

Localities.—Common in sandstone, limestone and iron ore. Paris, Me.; Benton and Bartlett, N. H.; Sharon and Woodstock, Vt.; Pelham and Chesterfield, Mass.; Ellenville, Little Falls, Watervliet, Fairfield, Middleville, Fowler, Antwerp, Rossie, Lake George and Palatine, N. Y.; Minnesota Mine, Lake Superior; Ouachita Spring, Ark.

Occurs in irregular beds or masses; brittle; saline taste; crackles in the fire.

Localities.—Found with gypsum, clay and sandstone. Washington County, Va.; Petit Anse, La.; Silver Peak, Nev.; Salmon River Mountains, Oregon.

Occurs in crystals generally; metallic lustre; powder pale brown; brittle; unchanged by heat or acids; if powdered and fused with potash, then dissolved in muriatic acid, the solution boiled with tinfoil assumes a beautiful violet color; gravity 4.

Value.—Used for coloring porcelain and artificial teeth.

Localities.—Found in granite and, limestone rocks. Warren, Me.; Merrimack, and Warren, N. H.; Bristol, Putney and Waterbury, Vt.; Windsor, Shelburne, Barre, Conway and Leyden, Mass.; Monroe, Conn.; Warwick, Edenville, Amity and Kingsbridge, N. Y.; Sudsbury, West Bradford, Parksburg, Concord and Newlin, Pa.; Newton, N. J.; Crowder’s and Clubb Mountains, N. C.; Habersham and Lincoln Counties, Ga.; Magnet Cave, Ark.

Occurs in masses; feeble, resinous lustre; color oily green; powder whitish; often yellowish gray on the outside; can be cut easily; takes a fine polish; becomes reddish by heat; gravity 2.5—same as Marble.

Value.—Worked into mantels, jambs, table-tops, and many other ornaments.

Localities.—Found as a rock in large masses. Deer Isle, Me.; Baltimore, Cavendish, Jay and Troy, Vt.; Newbury, Blanford, Middlefield and Westfield, Mass.; Newport, R. I.; near New Haven and Milford, Conn.; Port Henry, Antwerp, Syracuse, Warwick, Phillipstown, Canton, Gouverneur, Johnsburg, Davenport’s Neck, New Rochelle and Rye, N. Y.; Frankford, Hoboken and Montville, N. J.; Texas, Pa.; Cooptown, Md.; Patterson, N. C.; Calaveras County, Cal.; Alder Gulch, Mont. Marble veined with serpentine is called verd-antique.

Occurs in incrustations and masses; color bluish-green; not fibrous; surface smooth; easily cut; does not effervesce in acid; blackens by heat; gravity 2.

Value.—An ore of copper, yielding thirty per cent.

Localities.—Found with other copper ores. Somerville and Schuyler’s, N. J.; Morgantown and Cornwall, Pa.; Wolcottville, Conn.; Big Williams’ Fork, Ariz.

Occurs in masses, or strings and threads penetrating rocks and native copper and galena; metallic lustre; tarnishes grayish black; can be cut in slices and hammered out; dissolved in muriatic acid, it turns black on exposure; gravity 10.

Localities.—Chiefly found with copper near trap-rocks, and in fine grained galena and dark brown blende. Gold contains from one to fifteen per cent. Bridgewater, N. J.; Davidson and Stanley Counties, N. C.; Lake Superior Region; Poorman’s Lode, Idaho; Comstock Lode and Montezuma Ledge, Nev.; Alpine County and Maris Vein, Cal.; Clear Creek County, Col.

Occurs in small lumps, plates and threads; color dark gray; cuts like lead; melts in a candle giving off sulphur fumes; gravity 7.

Value.—The most important ore of silver, containing eighty-seven per cent.

Localities.—May be found almost everywhere, except in the coal regions; associated with other ores, quartz, limestone, baryta, etc. Most abundant where mineral veins cross one another. Comstock Lode, Gold Hill, Reese River, Cortez District and Silver-Sprout Vein, Nev.; Clear Creek County, Nev.

Occurs in crystals and masses; metallic lustre; color tin-white to steel-gray; powder dark gray; brittle; gives off garlic odor in a candle; melted with borax makes a deep blue glass; gravity 6.5 to 7.

Value.—An ore of cobalt and arsenic, containing eighteen to seventy per cent.

Localities.—Found in veins in granite regions with other ores, Mine la Motte, Mo.; Chatham, Conn.

Occurs in masses, often rounded, covered with minute crystals, or honeycombed; color white, dirty yellow or stone color; glassy lustre; brittle; effervesces in nitric acid; barely scratches glass; barely translucent; gravity 4.4.

Value.—Yields fifty per cent. of zinc.

Localities.—Found generally in limestone with galena and blende. Friedenville, Lancaster and Perkiomen, Pa.; Linden and Mineral Points, Wis.; Lawrence, County, Ark.; Ewing’s Diggings, Minn.

Occurs in crystals or plates somewhat curving; also (in coal regions) in nodules with concentric layers like an onion; brittle; color varies from white to yellowish-brown or dark-brown; strongly heated it blackens and will then attract the compass needle; the powder effervesces in nitric acid; melted with borax makes a green or yellow glass; gravity 3.8.

Value.—Yields thirty per cent. of iron, well adapted for steel.

Localities.—Found in granite and coal-formations, often with other ores. Plymouth, Vt.; Sterling, Mass.; Roxbury, Conn.; Antwerp, Herman and Rossie, N. Y.; Fentress and Harlem Mines, N. C.; Coal Regions of Western Pa., Virginia, Eastern Ohio, etc.

Occurs crystallized and in large masses, high metallic lustre; color steel-gray or iron-black; brittle; opaque except when very thin; the powder when very fine and rubbed on white paper shows red; the powder dissolves slowly in muriatic acid; by a strong heat yields a black mass which attracts the needle; gravity 5.

Value.—Yields from fifty to seventy per cent. of iron.

Localities.—Found in granite regions. Marquette, Mich.; Pilot Knob and Iron Mountains, Mo.; St. Lawrence County, N. Y.; Bartlett, Lisbon and Franconia, N. H.; Chittenden and Weathersfield, Vt.; Sauk County, Wis.

Occurs in pyramidal crystals; glassy lustre; powder white; scratches rock-crystal; by heat becomes black; gravity 3.5.

Value.—A gem; clear specimens weighing over four carats, are valued at half the price of the diamond.

Localities.—Found in granular limestone and clay. Amity and Gouverneur, N. Y.; Franklin and Byram, N. J.; Bolton and Boxborough, Mass.

Occurs in masses, consisting of minute pearly scales or grains; can be marked by the nail; hardens by heat; soapy feel; gravity 2.5.

Value.—Used for fire-stones, tubes, in manufacture of porcelain, etc.

Localities.—Found in beds with limestone, serpentine and slate. Orr’s Island, Me.; Francestown, Keene, Orford and Pelham, N. H.; Athens, Cavendish, Marlboro, Moreton, New Fane, Bradboro, Troy, Waterville, Westfield, Weathersfield and Windham, Vt.; Middlefield, Lenox and Westfield, Mass.; Manayunk and Chestnut Hill, Pa.; Albemarle and Loudon Counties, Va.; Staten Island and St. Lawrence County, N. Y.; Bare Hills, Md.

Occurs in crystals and in fibrous or granular masses; glassy lustre; brittle; thin pieces melt before a blow-pipe tinging the flame red; effervesces with acids; gravity 3.6.

Value.—A source of nitrate of strontia used in fire-works.

Localities.—Found in limestone. Schoharie, Muscalonge Lake, Chaumont Bay and Theresa, N. Y.

Occurs in crystals, masses and crusts; brittle; can be easily cut; burns with a blue flame and sulphur odor; gravity 2.

Localities.—Found in limestone and gypsum, and around geysers and sulphur springs. Springport, N. Y.; on the Potomac, twenty-five miles above Washington; Put-in-Bay Island, Lake Erie; Clear Lake, Cal.; Santa Barbara County, Col.; Humboldt County, Nev.

Occurs in crystals, grains and masses; high lustre; powder gray or brownish; brittle; will strike fire with steel; unaltered by heat or acids; gravity 7,—being nearly as heavy as lead-ore.

Value.—The only ore of tin, containing seventy-nine per cent. No gold-mine ever paid such profits as the tin mines of Cornwall.

Localities.—Jackson, N. H.; Temescal, Cal.; Boonville, Idaho; near Fredericktown, Mo.

Occurs in crystals; glassy lustre; brittle; scratches rock-crystal; not acted upon by ordinary heat or acids; gravity 3.5.

Value.—A gem; the most esteemed are the rose-red and white.

Localities.—Found in granite. Trumbull, Willimantic and Middletown, Conn.; Crowder’s Mountain, N. C.; Thomas’s Mountains, Utah.

Occurs in crystals, usually in long, slender three-sided prisms which break easily, glassy lustre; brittle; becomes milk-white by heat; scratches rock-crystal and garnet; gravity 3.

Value.—Used for jewelry.

Localities.—Found in granite rocks. Paris, Albany and Hebron, Me.; Chesterfield and Goshen, Mass.; Newlin and Marple, Pa.

Occurs in crystals and masses; metallic lustre; quickly tarnishes; color between copper-red and light-brown; powder pale grayish-black; dissolves in nitric acid; at a high heat melts to a copper globule; heated on charcoal gives off fumes of sulphur; gravity 5.

Value.—An important ore of copper yielding sixty per cent.

Localities.—Found in granite, freestone, etc., with other ores. Bristol and Cheshire, Conn.; Mahoopeny, Pa.; Copper Mines of N. J.

Occurs in masses; earthy and loose; can be broken by the fingers, and soils; no lustre; melted with borax makes a violet glass; feels very light.

Value.—Used in bleaching and for making smalt.

Localities.—Found in low places, generally in the vicinity of slate or iron ore beds. Warren, Vt.; Blue Hill, Hodgdon and Thomaston, Me.; Columbia and Duchess Counties, Austerlitz, Canaan Centre and Martinsburg, N. Y.; East Bradford and White Marsh, Pa.; Mine la Motte, Mo.

Occurs in crystals and masses; feeble lustre; brittle; can hardly be cut with a knife; sometimes scratches glass; makes a jelly in muriatic acid; gravity 4.

Value.—Contains seventy per cent. of zinc.

Localities.—Found in limestone with zincite. Franklin and Sterling, N. J.

Occurs in foliated masses or grains, powder orange-yellow; brittle; dissolves in acids without effervescence; gravity 5.5.

Value.—Yields seventy-five per cent. of zinc.

Localities.—Found in limestone with Franklinite, Garnet, etc. Sterling Hill and Mine Hill, N. J.

THE mineral riches of a country are frequently discovered by attentively observing the fragments brought down by the action of water from the hills into the valleys; and on tracing these to their several sources, the veins from which they were originally detached, are in many instances found. Water also acts in another way a very important part in the discovery of mineral veins, as by closely examining the faces of the different gullies and ravines, which intersect a country, a ready means is afforded of ascertaining whether its strata are traversed by metalliferous deposits; and, therefore, in exploring with a view to its mineral productions, no opportunity should be lost of observing the various sections thus naturally laid bare.

When fragments of an ore are found on a hill-side, it is very evident that the vein must lie higher up. If the vein is horizontal and the fragments are found on the top of the hill, there is no probability of finding much if any of the vein, for generally it has been washed away. Ore-veins, however, are almost always nearly vertical; so that boring is of little use, as it might pass by the richest vein, or, striking it lengthwise, give a too favorable result.

As heavy minerals do not drift far, metals are always found near their source.

Horizontal beds can be worked at the least cost.

Pockets and nodules, or any detached masses of minerals, are soon exhausted. Veins, lodes and beds are most valuable.

Boring a three-inch hole, which costs about $1 a foot, is a good method of testing a mineral vein or bed which lies more or less horizontally. A shaft may be sunk in sandstone for from $6 to $3 per cubic yard; in slate and gravel, at from $2 to $1.

The existence of mineral springs, and the rapid melting of the snow in any locality, are no indications of ores.

Searching for Diamonds.—Few things are so unpromising and unattractive as gems in their native state. Hence their slow discovery. There is little doubt that diamonds exist in many places as yet unknown, or where their presence is unsuspected. It is very difficult for the unpracticed eye to distinguish them from crystals of quartz or topaz. The color constitutes the main difficulty in detecting their presence. They are of various shades of yellowish brown, green, blue and rose-red, and thus closely resemble the common gravel by which they are surrounded. Often they are not unlike a lump of gum arabic, neither brilliant nor transparent. The finest, however, are colorless, and appear like rock-crystals.

In Brazil, where great numbers of diamonds, chiefly of small size, have been discovered, the method of searching for them is to wash the sand of certain rivers in a manner precisely similar to that employed in the gold fields, namely, by prospecting pans. A shovelful of earth is thrown into the pan, which is then immersed in water, and gently moved about. As the washing goes on, the pebbles, dirt and sand are removed, and the pan then contains about a pint of thin mud. Great caution is now observed, and ultimately there remains only a small quantity of sand. The diamonds and particles of gold, if present, sink to the bottom, being heavier, and are selected and removed by the practiced fingers of the operator. But how shall the gems be detected by one who has had no experience, and who in a jeweler’s shop could not separate them from quartz or French paste? The difficulty can only be overcome by testing such stones as may be suspected to be precious. Let these be tried by the very sure operation of attempting to cut with their sharp corners glass, crystal or quartz. When too minute to be held between the finger and thumb, the specimens may be pressed into the end of a stick of hard wood and run along the surface of window glass. A diamond will make its mark, and cause, too, a ready fracture in the line over which it has traveled. It will also easily scratch rock-crystal, as no other crystal will.

But a more certain and peculiar characteristic of the diamond lies in the form of its crystals. The ruby and topaz will scratch quartz, but no mineral which will scratch quartz has the curved edges of the diamond. In small crystals this peculiarity can be seen only by means of a magnifying glass; but it is invariably present. Interrupted, convex or rounded angles, are sure indications of genuineness. Quartz crystal is surrounded by six faces; the diamond by four. The diamond breaks with difficulty; and hence a test sometimes used is to place the specimen between two hard bodies, as a couple of coins, and force them together with the hands. Such a pressure will crush a particle of quartz, but the diamond will only indent the metal.

The value of the diamond is estimated by the carat, which is equal to about four grains, and the value increases rapidly with its weight. If a small, rough diamond weigh four grains, its value is about $10; if eight grains, $40; if sixteen grains, $640. A cut diamond of one carat is worth from $50 to $100.

The imperfections of the diamond, and, in fact, of all cut gems, are made visible by putting them into oil of cassia, when the slightest flaw will be seen.

A diamond weighing ten carats is “princely;” but not one in ten thousand weighs so much.

If a rough diamond resemble a drop of clear spring water, in the middle of which you perceive a strong light; or if it has a rough coat, so that you can hardly see through it, but white, and as if made rough by art, yet clear of flaws or veins; or, if the coat be smooth and bright, with a tincture of green in it,—it is a good stone. If it has a milky cast, or a yellowish-green coat, beware of it. Rough diamonds with a greenish crust are the most limpid when cut.

Diamonds are found in loose pebbly earth, along with gold, a little way below the surface, towards the lower outlet of broad valleys, rather than upon the ridges of the adjoining hills.

Searching for Gold.—The paying localities of gold deposits are the slopes of the Rocky and Alleghany Mountains. Gold need not be looked for in the anthracite and bituminous coal-fields nor in limestone rock. It is seldom found in the beds of rivers. The thing itself is the surest indication of its existence. If soil or sand is “washed” as described in Chapter V., and the particles of gold are not heavy enough to remain at the bottom but float away, the bed will not pay.

Along streams rather high up among the mountains, and in the gravelly drift covering the slopes of the valley below, are the best prospects. Where the stream meets an obstacle in its path or makes a bend or has deep holes, there we may look for “pockets” of gold. Black or red sands are usually richest. Gold-bearing rock is a slate or granite abounding in rusty looking quartz veins, the latter containing iron pyrites or cavities. Almost all iron pyrites and silver ores, may be worked for gold. When the quartz veins are thin and numerous rather than massive, and lie near the surface, they are considered most profitable. Few veins can be worked with profit very far down. As traces of gold may be found almost everywhere, no one should indulge in speculation before calculating the percentage and the cost of extraction. Gold-hunting, after all, is a lottery with more blanks than prizes.

The substances most frequently mistaken for gold are iron pyrites, copper pyrites and mica. The precious metal is easily distinguished from these by its malleability (flattening under the hammer) and its great weight, sinking rapidly in water.

Searching for Silver.—This metal is usually found with lead ore and native copper. Slates and sandstones intersected by igneous rocks as trap and porphyry, are good localities. Pure silver is often found in or near iron ores and the dark brown zinc blende. The Colorado silver lodes are porous at the surface and colored more or less red or green. Any rock suspected of containing silver should be powdered and dissolved in nitric acid. Pour off the liquid and add to it a solution of salt. If a white powder falls to the bottom which upon exposure turns black, there is silver in it. Silver mines increase in value as in depth, whereas gold diminishes as we descend.

Searching for Copper.—The copper ores, after exposure, or after being dipped in vinegar, are almost invariably green on the surface. They are most abundant near trap dykes. The pyrites is generally found in lead mines, and in granite and clay-slate. Copper very rarely occurs in the new formations, as along the Atlantic and Gulf borders, and in the Mississippi Valley south of Cairo.

Searching for Lead.—Lead is seldom discovered in the surface soil. It is also in vain to look for it in the coal region and along the coast. It must be sought in steep hills, in limestone and slate rocks. A surface cut by frequent ravines or covered by vegetation in lines, indicates mineral crevices. The galena from the slate is said to contain more silver than that from the limestone. The purest specimens of galena are poorest in silver; the small veins are richest in the more precious metal. A lead vein is thickest in limestone, thinner in sandstone and thinnest in slate.

Searching for Iron.—Any heavy mineral of a black, brown, red or yellow color may be suspected to be iron. To prove it, dissolve some in oil of vitriol and pour in an infusion of nut-gall or oak-bark; if it turns black, iron is present. If a ton of rich magnetic ore costs more than $4 at the furnace, good hematite more than $3, and poor ores more than $1.50 or $2, they are too expensive to pay, unless iron is unusually high. Deep mining for iron is not profitable. Generally speaking, a bed of good iron ore, a foot thick, will repay the cost of stripping it of soil, etc., twelve feet thick. Red and yellow earths, called ochres, contain iron. Magnetic ore is easily found by a compass.

ONE of the first questions asked after the discovery of a metallic ore, is—“will it pay?” We propose to state in plain words a method of determining the character and value of the principal ores, so that any intelligent man, however unscientific, may answer his own question. The chemical analysis or exact assaying of ores is too complicated, and must be left to professional assayers.

“Will it pay?” is an important query; for many ores of even precious metals, are not “paying.” Whether an ore is profitable depends not so much upon the relative value of the metal as upon the ease of separating it from the rock or “gangue” as it is called. Thus the minimum percentage of metal, below which the working of the ore ceases to be profitable is—

That is, an ore of iron which contains less than 25 per cent. of metal will not pay for working; for the reduction of iron in comparison with copper ore is very difficult. Gold is very easily extracted, and hence some quartz rocks which do not apparently contain a particle of gold, pay well, a bushel of rock often yielding half an ounce.

Iron occurs in large masses or beds; but the other metals are scattered in fragments through sand or soil, or exist in veins running through rocks.

Washing for Gold and Platinum.—This operation, called “panning,” is the oldest and simplest method of extracting the precious metals. At the present time, it furnishes to Russia nearly all the gold produced in that empire. It is based on the principle that substances of different weights may be separated by means of water,—the heaviest going to the bottom first. To examine the bank or bed of a river, suspected to contain gold, fill a milk-pan with the sands and carry it to a tub or pool of quiet water. Dip it under, stirring the mass with one hand or a stick. Then pour off the muddy water, fill with fresh water stirring again, and again pour off the light sand, clay, etc. Scales of gold will sink fast; mica flakes will take their time. Repeat this process till all the fine particles are washed off; then allow just enough water to enter the pan as will cover the sand. By shaking the pan and gradually lowering the side by which it is held, the light sand will flow off, leaving in the corner a heap of coarse sand. Put in a small quantity of water and turn the pan around so as to create a gentle current, when the precious metal, if there be any, can be easily detected,—the gold by its bright lustre, the platinum by its lead color, and both by their malleability. Particles of gold are of uniform color and are either flat or rounded; while other yellow grains are angular. Holding the pan in the sunshine, secure any glittering glassy crystals, and test them for diamonds or rock-crystals. A magnet will remove any particles of magnetic iron-ore.

Assay of Gold Ore.—Gold may be found in quartz rock, in iron and copper pyrites, and in silver ores.

To ascertain if any gold is present in quartz, reduce the rock to powder and sift it. A certain quantity, say half a peck, is then washed as above described, till a manageable quantity of sand is left. If there is any show of gold, dry the mass and put it in a bowl or glass dish, and add an ounce of quicksilver, stirring the mixture well with a wooden rod. The quicksilver, which will unite with every particle of gold which may be there, is then poured off into a soft leather (chamois) bag. This is squeezed to remove superfluous quicksilver, and a pasty amalgam is left, which is put into an iron vessel and heated red hot. The yellow powder remaining is mixed with saltpetre and melted, when a button of pure gold will be found in the crucible. Quartz ores should yield $6 to the ton in order to pay.

To test pyrites for gold, reduce a given quantity to powder and wash as before; then roast the residue at a red heat. Upon cooling, add quicksilver and treat as just described. Pyrites should yield $1 of gold to the bushel of ore to be profitable.

Native silver often contains gold. To separate them, carefully flatten the alloy with a smooth hammer on an anvil, and then boil it in strong nitric acid in a glass flask for about ten minutes. Carefully pour off the acid into a vial, and wash the powder in the flask (which is fine gold) with water and dry. To the liquid in the vial add a solution of common salt. The white powder which falls should be removed, washed with water, and fused with powdered chalk or iron filings; a button of pure silver is the result.

Any substance supposed to be or to contain gold may be tested by dissolving it powdered in aqua regia and then pouring in a solution of copperas; if there is gold, the reddish-brown precipitate, by rubbing, assumes a bright metallic lustre.

To tell whether a globule of silver has any gold in it, put it on a white porcelain dish and moisten it with a drop of nitric acid: if it is pure silver, it will dissolve and retain its white color; if mixed with gold, it will soon turn gray or black.

To test the purity of gold, rub some of it off on a hard black flint slate, and apply to the mark a drop of aqua fortis. If the gold is pure, the yellow streak remains unchanged, but if alloyed it partly disappears; if it is only an imitation of gold, it vanishes altogether.

A ready method of finding the amount of gold in a quartz rock with considerable accuracy, is by taking the specific gravity of the rock (well cleaned) as given on page 13. If the gravity is not over 2.7, it contains little or no gold. If it is 3, it very likely is gold-bearing, although pyrites may be present. But if it is over 5, it is undoubtedly auriferous, and if 12, it is very rich in gold.

It is generally considered that the sand of any river is worth working for the gold it contains, provided it will yield twenty-four grains to the hundred weight.

Assay of Silver Ore.—Pure silver is easily recognized. But lead and copper ores often contain a large percentage of the precious metal.

To detect silver in lead ore, dissolve the powdered ore in strong nitric acid; pour off the liquid and insert a piece of pure copper. If silver is present, it will go to the bottom. Or, add to the liquid a solution of common salt, and it will instantly become cloudy or white. If lead ore yields three ounces of silver to a ton, it may be worked for the silver as well as the lead. In Colorado, the average value of silver-bearing galena is $100 per ton.

To test the copper ores for silver, dissolve them in nitric acid; then add a few drops of muriatic acid, and if silver is present, a white curdy precipitate will fall to the bottom. Native copper, when polished, often shows white spots of silver.

To estimate the proportion of silver in lead ore, reduce a known quantity of the clear ore to powder, mix with a little dry soda and a few nails, and heat in a round-bottomed iron pot or crucible. The lead which is obtained should then be put in a cup having ashes at the bottom, and strongly heated in an open furnace. A globule of silver will be left, if any is present, and being weighed, the percentage can be found.

Rich silver ores may be reduced by mixing them with ten parts of common salt, and exposing the mass for hours in an open furnace, stirring it frequently. When cold reduce to powder and mix with an equal quantity of quicksilver and enough water to make a paste, and agitate the mixture for two days, when the amalgam will fall to the bottom. The amalgam is then squeezed in a leather bag and washed.

Silver glance will yield its metal by heating it before a blow-pipe.

Assay of Copper Ore.—When the ore is native copper and rock, as at Lake Superior, it should be pounded and the earthy matter washed away. Then mix with a little potash or soda and bring to a high heat in a crucible.

Other copper ores may be tested by dissolving them powdered in dilute aqua regia. The presence of silver will be shown by a white powder on the bottom. Then add considerable ammonia. If there is any copper a blue liquor will be produced. Strain this through tissue paper, and evaporate to dryness. Dissolve the residue in muriatic acid, and by putting in a piece of iron or zinc, the copper will fall down. Or, add to this solution pure potash; dry and weigh the powder thrown down; every 5 parts of it contains 4 parts of copper.

Gray copper and red copper ores may be assayed by heating with charcoal, (both powdered,) in a furnace. Malachite and azurite should be smelted with borax; Copper pyrites and silicate of copper with soda or powdered marble.

A ton of copper ore which contains ten per cent. of metal, pays $25 at the furnace. The ore of copper when roasted, turns black; and when thrown into nitric acid makes a sky-blue solution. A clean knife-blade put into this solution will be coated with copper.

Assay of Iron Ore.—Take a known quantity of the ore in fine powder and mix thoroughly with dry borax (or with one part of fluor spar, one of charcoal and four of salt,) and expose it for an hour in a covered crucible lined with charcoal to a white heat in a wind-furnace for an hour. A button of iron will be found at the bottom, which determines the percentage.

Assay of Zinc Ore.—If the weighed ore is roasted with powdered charcoal, white flowers of zinc will be formed on a piece of cold iron held over it. After thorough roasting, the residue should be weighed; the loss is the oxide of zinc, and every 100 parts of this contain 81 of metal.

All the ores of zinc will dissolve in either nitric or hot sulphuric acid.

Assay of Tin Ore.—Tin-stone will yield up its metal if mixed with charcoal, borax and soda, and heated on the hearth of a furnace or before a blow-pipe.

The presence of tin may be tested by dissolving the metal thus roasted out, in aqua regia and adding a decoction of Brazil-wood: if the metal was tin, the liquid will be colored a beautiful crimson.

Assay of Lead Ore.—Both galena and cerussite are rich ores, and when abundant pay well. They are easily reduced by heat, the former being usually mixed with charcoal and iron filings. If a western backwoodsman wants shot or bullets, he kindles a fire in a hollow tree or an old stump, puts some galena on the charred wood, and melts it down. After cooling, he finds the metal at the bottom. The smelting of a ton of lead costs about $6. The average price per ton of galena is $30. When galena is dissolved in warm nitric acid, a clean plate of zinc placed in it will be coated with brilliant blades of lead; if the galena contains silver, a plate of copper will be served in the same way. A solution of chromate of potash poured into a solution of lead ore in nitric acid will throw down a yellow powder.

To Test the Purity of Graphite.—Its value depends upon the amount of its carbon. Pulverize and then dry at a heat of about 350 degrees, twenty grains of it; then place it in a tube of hard glass four or five inches long, half an inch wide and closed at one end. Add twenty times as much well dried oxide of lead and well mix. Weigh the tube and contents, and afterwards heat before a blow-pipe till the contents are completely fused and no longer evolve gases. Ten minutes will suffice for this. Allow the tube to cool and weigh it. The loss in weight is carbonic acid. For every twenty-eight parts of loss there must have been twelve of carbon.

ANY spring which contains a large amount of foreign matter, as gas, salts and earthy ingredients, is called mineral water. The special prominence of any ingredient gives it its particular name. Many iron springs contain salt, salt springs contain iron, and both may contain gas; the name is derived from the most prominent ingredient.

Our country is rich in mineral springs; there is not a State without one. But in general they are most numerous in hilly or mountainous regions, especially where the rocks are much deranged in position, or “faulted,” as the miners say. As for example, in Eastern New York and in the valley between the Blue Ridge and the Alleghany from Harper’s Ferry to the Natural Bridge. The Pacific States, also, are as remarkable for the number and variety of their mineral springs as for their metallic ores.

Carbonated or Gas Springs.—Springs of this class have a peculiar sparkling character and are continually sending up bubbles of gas. When the quantity of gas is small, it may be detected by adding a little lime water which will give it a milky appearance and deposit a white sediment; or, dip in a piece of blue litmus paper (which can be had of most druggists), and if there is any carbonic acid gas in the water, it will be reddened; or, pour in a little vinegar, stir well, and then add a little finely powdered sugar, when the gas, if it is there, will rise in small bubbles.

The most celebrated carbonated springs are the following: Saratoga and Ballston, N. Y.; Clarendon, Vt.; Sweet Springs in Shover’s Valley, Pa.; Bladon and Bailey Springs, Ala.; “Boiling Springs” near Pike’s Peak, Col.; Beer Springs near Bear River, Or. These springs contain salt, soda, magnesia, lime and iron, and are sometimes classed as saline, soda or chalybeate springs.

Chalybeate or Iron Springs.—The presence of iron in a spring may be ascertained by pouring into it an infusion of nut-galls, of logwood or of tan-bark, which will change it immediately to a black or dark color. If the water contains much iron, it may be recognized by its inky taste and by a yellowish powder on the border of the spring or at the bottom of a tumbler when allowed to stand awhile.

If waters have a cool but earthy taste, they contain lime; if bitter, they have magnesia. The “soda springs,” so called, are often only saline, carbonated or magnesia waters.

The most famous iron springs are at Saratoga, Sandlake and Catskill, N. Y.; West Bethel, Fryeburg, Eberne and Bethel, Me.; Schooley’s Mountain in Washington, N. J.; Bedford, Pittsburg, Frankfort and York, Pa.; Brandywine Springs, Del.; Red Sweet Springs in Monroe County, Rawley’s Spring in Rockingham County, and Huguenot Springs in Powhattan County, Va.; in Bath County, Ky.; Yellow Springs, O.; twenty miles east of Knoxville, Tenn.; Madison County, Geo.; Raymond and Lynchburg, Miss.; near Ogden City, Utah; near Mt. Shasta, Col.

Sulphur Springs.—These are easily recognized by their unpleasant odor, resembling that of rotten eggs. The water blackens silver and a solution of sugar of lead.

Sulphur springs are very numerous. The best known are at Saratoga, Sharon, Clifton, Avon, Manlius, Chittenango, Dryden and Richfield, N. Y.; Highgate and Newburg, Vt.; Togus, Bethel and West Newfield, Me.; Shover’s Valley, Carlisle and Doubling Gap, Pa.; Winchester and Warrenton, Va.; Greenbrier and Monroe Counties, W. Va.; Bath County, Ky.; White’s Creek near Nashville and in Granger County, Tenn.; Spartanburg, S. C.; Butts County, Geo.; Tallahatta, Ala.; Tampa, Fla.; near Bitter Creek and Great Salt Lake, Utah; along the Yellowstone River, Mont.; Jackson, Cal.

Acid or Alum Springs.—These waters have a more or less sour taste and redden blue litmus-paper.

They are found at Byron and Oak Orchard, N. Y.; Blossburg, Pa.; Bath, Richmond and Rockbridge, Va.

Magnesian or Epsom Springs.—These have a bitter taste. To test any water for magnesia, add to a glass of it a solution of phosphate of soda and some hartshorn; if magnesia is present, the liquid first becomes turbid, and finally minute crystals fall to the bottom.

There are Epsom springs at Harrodsburg and Perryville, Ky.; Westport, O.; Raymond, Miss.; Orange County, Ind.; Scott County, W. Va.

Saline or Salt Springs.—These contain a large percentage of common salt, and are recognized by their taste. They generally contain many ingredients, (generally seven or eight,) but the salt predominates. A well should contain at least ten per cent. of salt to pay for working. The Syracuse spring yields a bushel of salt to every thirty-three gallons; while the Great Salt Lake contains 22 per cent. Among the most important salt wells are those at Syracuse, Salina and Liverpool, N. Y.; Lubec, Me.; Shannondale, Va.; Bath County, Ky.; Athens County, O.; Hartford, Ind.; Saginaw, Mich.; Oneida, Idaho.

Thermal or Warm Springs.—Any spring is so called, the temperature of which throughout the year is above that of the soil around it. They generally occur near the line of junction between the granite or igneous rocks and the stratified rock (slate or limestone) resting upon its flanks. The temperature of such waters in the United States ranges from 73 to 200 degrees, the latter being reached by the Geysers of Montana. Many iron and sulphur springs are also thermal.

The most noted warm springs are at Lebanon, N. Y.; in Bath, Berkley, Monroe and Scott Counties, Va.; Buncombe Counties, N. C.; French Brood River, Tenn.; Meriwether County, Geo.; Washitaw, Ark.; Salt Lake Valley, Utah; near Pyramid Lake, Nev.; along the Malheur and Fall Rivers, Or.; Lincoln Valley, Idaho; on Gardiner’s River, in Madison County, and especially in the Yellowstone Basin, Mont.

Artesian Wells.—To sink a flowing well with any reasonable prospect of success, it is essential that the spot selected should be lower than land in the vicinity, although those higher elevations may be several miles away. The layers of the rocks, also, should dip towards the spot rather than away from it. The best indication, but not a certain one, is a great basin-shaped valley, to the centre of which the rocks dip on one or more sides. Sandy, lime and slate rocks are more propitious than granite.

Oil Wells.—Where there are marks of disturbance and misplacement of the rocks, there the experienced sink wells. Rugged hills and sharply-defined valleys are, generally, signs of such dislocation. The line or “break” from which the rocks dip like the roof of a house is considered most favorable. There is no such thing as an “oil rock,” for the oil is found at different depths, and the fissure containing it is more or less vertical. In Pennsylvania, the greatest flowing wells have been found in the third sand rock. No limestone has afforded any large supply of oil. Coal in no large quantities is ever found upon or in the immediate vicinity of the oil territory. The “show of oil” increases in value as a sign, with the depth at which it is found. Especially is the finding of a large amount of imprisoned gas, though no oil may be present, regarded as a good indication that oil is near. In the bituminous coal region, a gas spring indicates the probable existence of oil in the rocks below. But generally, “surface shows” are seductive. The great oil belt runs south-westerly from Oil Creek, Pa., to Burning Springs, West Va. But Ohio, Kentucky, Tennessee, Georgia, Alabama, Missouri, Texas, Illinois, Indiana, Michigan and Southern California are also rich in petroleum.

“BRISTOL Stones,” “Irish Diamonds,” “Cape May Diamonds,” and “California Diamonds,” are skillfully-cut quartz crystals. They are easily detected by the file and by their lightness.

“Paris Brilliants” are more dangerous counterfeits, and are very often sold for genuine. The great establishment of Boarguiguon, in Paris, is the most famous manufactory of artificial gems in the world, employing about one hundred hands. The gems are such perfect imitations that they can be distinguished from real stones only by the closest scrutiny of those experienced in such matters. They fail chiefly in hardness; in brilliancy and gravity they nearly or quite equal the genuine.

Nature has made the most precious stones with the most common materials. The diamond is purified charcoal; while the matter of clay and white pebbles is the base of all other gems.

The chemist has imitated nature in the production of colored gems. The base of these imitations, called “pastes,” is “strass”—a white glass compound of 300 parts of pure sand, 96 of potash, 27 of borax, 514 of white lead, and one of arsenic. The mixture is put into a crucible and kept at a high heat for 24 hours. This is the philosopher’s stone which competes with Golconda. The uncolored glass is used in making mock diamonds and white topaz. Another paste which has very great brilliancy, and, unfortunately, the same gravity as the diamond, is made by melting 100 parts of pure sand, 150 of red lead, 30 of calcined potash, 10 of calcined borax and one of arsenic, keeping the mixture melted for two or three days and then cooling very slowly. Each ingredient is separately reduced to a fine powder.

False Ruby is made by fusing together of strass one ounce and six drams, glass of antimony 37 grains, and purple of cassius one grain; then add eight parts more of strass and fuse for thirty hours; cool and remelt pieces in a blow-pipe. Or, melt five ounces of strass and one dram of manganese.

False Topaz can be made from 1008 grains of strass, 43 grains of glass of antimony and one grain of purple of cassius.

False Sapphire.—Add to eight ounces of strass 52 grains of pure oxide of cobalt.

False Emerald.—To one pound of strass add one dram of verdigris and fifteen grains of crocus martis. Or, take 2304 grains of strass, 21 grains of green oxide of copper, and one grain of oxide of chrome. Or, take an ounce and a half of rock-crystal, six drams of dry soda, two drams of dry borax, two drams of red lead, one dram of nitre, twenty grains of red oxide of iron, and ten grains of green carbonate of copper.

False Carnelian.—Strass two pounds, glass of antimony one pound, rouge two ounces, manganese one dram.

False Amethysts and Opals are manufactured; but the fine opal defies imitation, and the amethyst is too common in nature to allow much margin for the “pastes.”

In distinguishing true and false gems, no one character should be depended upon. All genuine stones will bear rough handling; if the merchant says “hands off,” refuse to purchase. Any gem worth buying is worth testing.

First: try the hardness. The file will make no impression on the diamond and ruby, and will with difficulty scratch the other gems; while the “pastes” are easily marred. All the precious stones scratch window glass, although opal will not attack common bottle glass. All imitations easily yield to sand. The sapphire is the hardest of colored gems, and opal is the softest. The emerald will hardly scratch rock-crystal; its counterfeit not at all. Topaz will scratch ordinary ruby, but will not touch sapphire.

Secondly: as to weight. This is the most accurate method, but the stone must be taken from its setting. The mode of taking the gravity has already been given (page 13), and the amount of each is stated in Chapter II. Garnet is the heaviest of gems; weighed in water it loses only one-fourth of its weight; i. e., if a red garnet be suspended by a fine thread from a delicate balance and immersed in a glass of water under it, one-quarter of its ordinary weight in air must be added to the pan from which it is suspended to restore the equilibrium. In like manner, ruby and sapphire lose a little more. The diamond and white topaz lose two-sevenths of their weight. Rock-crystal, amethyst, carnelian and agate lose five-thirteenths; and opal about one-half, being the lightest of gems. The emerald loses more than one-third.

As “paste” can be made so as to have the same specific gravity as the genuine article, this test alone can not be relied upon; but very few of the imitations are so carefully made. The test is very convenient in distinguishing gems of like color from each other, as oriental ruby, spinel ruby and red tourmaline, and green tourmaline and emerald.

Thirdly: characteristics depending on light and electricity. It is not easy to look through a diamond of the first water, while imitations readily permit objects to be seen through them. A very delicate and perfect test of a diamond, distinguishing it from all colorless gems, as white topaz, white sapphire and white zircon, but not from “pastes,” is to look through it at a pin-hole in a card. This requires some dexterity, and the gem should be fixed to a steady object by a bit of wax at a proper distance. A true diamond will show but one hole, all the others will show two. As white topaz, when large, is a magnificent stone, it is often palmed off for a diamond of great value; but this test is invariably certain.

A true diamond retains its brilliancy under water.

When a colored stone is placed in the path of the solar spectrum (the row of seven colors into which sunlight is separated by a prism), its color will vary with the portion of the spectrum which falls upon it; and two stones of the same color, but of a different nature, will exhibit different effects. Thus, a paste placed beside a fine colored gem, betrays its worthlessness. A simpler method of testing stones is to look at them through a bit of glass, colored red, yellow, blue or green. Every stone will exhibit, under this test, properties peculiar to itself, and by which its

SEARCHING FOR DIAMONDS.

nature may be recognized. This is also a severe test for the purity of tint; for if pure and unmixed, the stone will appear completely black in every other light but its own color. Milky and turbid stones can not bear this test.

A first-class ruby has the color of the blood as it spirts from an artery. The deeper the hue of the emerald the more it is valued; it loses none of its brilliancy by artificial light. The pale rose topaz, the kind most esteemed, is artificially colored by heating it.

If topaz or tourmaline be gently heated, it becomes electric and will attract a thread or suspended pith-ball. No imitation will do this. All real gems when rubbed will attract the pith-ball, and retain the power a long time; the pastes also become electric, but soon lose their attraction. Rub a glass tube with a piece of flannel and bring it near a suspended pith-ball; the latter will be strongly attracted and then repelled. Immediately rub a genuine diamond and bring it near the ball, and it will be attracted. A paste diamond thus rubbed would repel it.

Finally: the breath remains much longer on the pastes than on real gems. The former also betray under a magnifying glass small air bubbles. Diamonds and other first-class stones are always cold to the touch.

False Pearls.—These are glass beads coated with a mixture of three ounces of scales of the blay or bleak fish, half an ounce of fine glue, one ounce of white wax and one ounce of pulverized alabaster. Powdered opal is sometimes used; also the powdered pearl of the oyster and other shells soaked in vinegar, and made up with gum tragacanth. Artificial pearls are usually brittle, and do not weigh more than two-thirds as much as the genuine.

False Corals.—These are made of resin and vermilion; or of marble powder made into a paste with varnish or soluble glass and a little isinglass, colored by Chinese vermilion, and then moulded. They are used for setting in cheap jewelry. The knife shows it to be too soft to be genuine.

Artificial Gold.—The following oroid or imitation gold is sometimes sold for the genuine article which it closely resembles. Pure copper, 100 parts by weight, is melted in a crucible, and then 6 parts of magnesia, 3.6 of sal-ammoniac, 1.8 of quicklime and 9. of tartar are added separately and gradually in the form of powder. The whole is then stirred for about half an hour, and 17 parts of zinc or tin in small grains are thrown in and thoroughly mixed. The crucible is now covered and the mixture kept melted for half an hour longer, when it is skimmed and poured out.

Any imitation of gold may be detected by its weight, which is not one-half of what it should be, and by its dissolving in nitric acid while pure gold is untouched.

IT was on the 19th day of January, 1848, that James W. Marshall, while engaged in digging a race for a saw-mill at Coloma, about thirty-five miles eastward from Sutter’s Fort, found some pieces of yellow metal, which he and the half-dozen men working with him at the mill supposed to be gold. He felt confident that he had made a discovery of great importance, but he knew nothing of either chemistry or gold-mining, so he could not prove the nature of the metal nor tell how to obtain it in paying quantities. Every morning he went down to the race to look for the bits of the metal; but the other men at the mill thought Marshall was very wild in his ideas, and they continued their labors in building the mill, and in sowing wheat and planting vegetables. The swift current of the mill-race washed away a considerable body of earthy matter, leaving the coarse particles of gold behind; so Marshall’s collection of specimens continued to accumulate, and his associates began to think there might be something in his gold mines after all. About the middle of February, a Mr. Bennet, one of the party employed at the mill, went to San Francisco for the purpose of learning whether this metal was precious, and there he was introduced to Isaac Humphrey, who had washed for gold in Georgia. The experienced miner saw at a glance that he had the true stuff before him, and, after a few inquiries, he was satisfied that the diggings must be rich. He made immediate preparation to go to the mill, and tried

THE SAW-MILL OF COLOMA.
THE PLACE WHERE GOLD WAS FIRST DISCOVERED IN CALIFORNIA.

to persuade some of his friends to go with him; but they thought it would be only a waste of time and money, so he went with Bennet for his sole companion.

He arrived at Coloma on the 7th of March, and found the work at the mill going on as if no gold existed in the neighborhood. The next day he took a pan and spade, and washed some of the dirt in the bottom of the mill-race in places where Marshall had found his specimens, and, in a few hours, Humphrey declared that these mines were far richer than any in Georgia. He now made a rocker and went to work washing gold industriously, and every day yielded to him an ounce or two of metal. The men at the mill made rockers for themselves, and all were soon busy in search of the yellow metal. Everything else was abandoned; the rumor of the discovery spread slowly. In the middle of March Pearson B. Reading, the owner of a large ranch at the head of the Sacramento valley, happened to visit Sutter’s Fort, and hearing of the mining at Coloma, he went thither to see it. He said that if similarity of formation could be taken as a proof, there must be gold-mines near his ranch; so, after observing the method of washing, he posted off, and in a few weeks he was at work on the bars of Clear Creek, nearly two hundred miles north-westward from Coloma. A few days after Reading had left, John Bidwell, now representative of the northern district of the State in the lower House of Congress, came to Coloma, and the result of his visit was that, in less than a month, he had a party of Indians from his ranch washing gold on the bars of Feather River, twenty-five miles north-westward from Coloma. Thus the mines were opened at far distant points.

The first printed notice of the discovery of gold, was given in the California newspaper published in San Francisco on the 15th of March. On the 29th of May the same paper, announcing that its publication would be suspended, says:—“The whole country, from San Francisco to Los Angelos, and from the sea-shore to the base of the Sierra Nevada, resound with the sordid cry of gold! gold! gold! while the field is left half planted, the house half built, and everything neglected but the manufacture of picks and shovels, and the means of transportation to the spot where one man obtained one hundred and twenty-eight dollars’ worth of the real stuff in one day’s washing; and the average for all concerned, is twenty dollars per diem.”

The first to commence quartz mining in California were Capt. Wm. Jackson and Mr. Eliason, both Virginians, and the first machine used was a Chilian mill.

The Reid Mine, in North Carolina, was the first gold mine discovered and worked in the United States, and the only one in North America from which, up to 1825, gold was sent to the Mint.

SEPARATED from California by the snowy chain of the Sierra, the State of Nevada has been celebrated, since 1860, for its silver mining. In November, 1859, the news of the discovery of silver mines near Lake Washoe was confirmed at San Francisco; and in June, 1860, the mines of Washoe, the central western portion of the State, had already sent such rich results to Europe, that the French Ministers of Finance and Commerce despatched a mining engineer to Nevada to make a close inspection of these wonderful mines. It seemed as if the world were about to be inundated with silver, as it had been by gold ten years previously; and what would those economists now say, who had only recently counselled that the value of gold coin should be lowered or that gold should be demonetized on account of the disturbed relation of these precious metals—the bases of the standard of payment throughout the world generally. Whilst the French engineer visited Nevada and prepared his report, the miners of Washoe continued working their veins of metal. At the present time, 1881, the mines on the eastern slope of the Sierra Nevada annually produce about $12,500,000 of silver, chiefly from the Comstock lode; the total yield of gold from the quartz mines of California is about $17,000,000 per annum. The Comstock lode, in the State of Nevada, may be ranked among the most productive metalliferous deposits ever encountered in the history of mining enterprise; its productive capacity, as now being developed, surpassing, if the mass of its ores do not in richness equal, those of the most famous mines of Mexico and Peru.

The known limits of this lode cover a space of 22,546 feet in a nearly due north and south direction (magnetic). The variation of the needle in that locality is 16½ degrees east. Upon this extensive seat of metalliferous deposits, the mines are divided into three groups: the Virginia Group, seventeen mines, with claims of 13,549⅓ feet; Gold Hill Group, nine mines, of 6,397¼ feet; American Flat Group, three mines, of 2,600 feet. The three groups of twenty-nine mines thus occupy a total length on the lode of 22,546 feet. The Comstock lode was discovered in 1859, by a pit sunk for a water hole on the ground of the Ophir mine; milling the ore began in October of the same year, but the amount of bullion taken out in 1860 is estimated at but $100,000. Since then the Comstock has become the greatest gold and silver mine in the world. To the end of 1878 the yield was estimated at $291,162,205, as follows: From 1860 to 1870 inclusive, of gold and silver together, unclassified, $102,466,240; 1871 to 1878 inclusive, gold, $88,691,498, silver, $91,278,623; 1877 and 1878, gold and silver, unclassified, $1,725,844. Making allowance for the loss by slimes and tailings, the gross contents of the lode as worked up to 1878 are estimated at $363,961,205. About 6,500,000 tons of ore have been extracted in this time, which a good authority estimates of an average value to the company of $45 per ton of 2,000 pounds.[5]

ANNUAL PRODUCTION of GOLD and SILVER in the UNITED STATES from 1853 to 1880, inclusive.

[From the Reports of the Director of the Mint.]

The consumption of Gold and Silver in the Arts and Manufactures from 1874 to 1879, inclusive, in the United States, was estimated by the Director of the Mint, in 1879, as follows:

A, B, C, D, E, F, G, H, I, J, K, L, M, N, O, P, Q, R, S, T, U, V, W, Z

Acid or alum springs, 109
Agate, 20, 21
localities, 21
value, 20
Alleghenies, 14
Alum, 21
localities, 21, 22
springs, 109
value, 21
American Flat group, silver mines, 136
Amethyst, 22
false, how made, 117
localities, 22
value, 22
Anthracite, 22, 23
localities, 23
value, 23
Antimony ore, 23, 24
localities, 23
value, 23
Artesian Wells, 111, 112
Artificial gold, how made, 125
jewelry, how made and detected, 114-125
Asbestus, 24
localities, 24
value, 24
Asphaltum, 24, 25
localities, 25
value, 25
Assay of copper ore, 100-102
gold ore, 95-98
iron ore, 102
lead ore, 103, 104
ores, 92-104
silver ore, 99, 100
tin ore, 102, 103
zinc ore, 102
Atlantic coast, 14
Azurite, 25
localities, 25
smelting, 101
value, 25

Baryta, localities, 26
or heavy spar, 26
value, 26
Bidwell, John, 130-132
Bituminous coal, 27
localities, 27
region, 14
Blende, 27, 28
localities, 28
value, 28
Blowpipe, 17
Bog iron ore, 29
localities, 29
value, 29
Boring, 83
Brazil, diamonds in, 84
Bristol stones, 114
Brittle silver ore, 30
localities, 30
value, 30
Brown coal, 30
localities, 30
value, 30
Brown Hematite or Limonite, 56, 57

Calamine, 31
localities, 31
value, 31
California diamonds, 114
discovery of gold in, 127-133
Cannel coal, 31, 32
localities, 32
value, 32
Cape May diamonds, 114
Carbonated or gas spring, 106, 107
Carnelian, 32
false, how made, 117
localities, 32
value, 32
Celestine, 32, 33
localities, 33
value, 33
Cerussite, 33
and Galena, reduction of, 103
localities, 33
value, 33
Chalybeate or iron springs, 107, 108
Chromic iron, 34
localities, 34
value, 34
Cinabar, 34, 35
localities, 35
value, 35
Clear Creek, Cal., gold in, 132
Coal, anthracite, 22
bituminous, 27
brown, 30
cannel, 31, 32
Cobalt pyrites, 35
localities, 33
value, 35
Coloma, Cal., discovery of gold there, 127
Colorado silver lodes, 89
Colors, distinction of minerals by, 12
Comstock Lode, 135-137
gold and silver produced from, 136, 137
Connecticut river valley, 14
Copper, 36
glauce, 36
localities, 36
value, 36
gray copper ore, assaying, 101
localities, 36
nickel, 37
localities, 37
value, 37
ore, assay of, 100-102
gray, 51
red, 65
red, assaying, 101
variegated, 78
ores, test for silver, 99
testing, 100-102
silver in, 101
percentage of in ores, which will pay, 101
pyrites, 37, 38, 90
localities, 38
smelting, 101
value, 38
searching for, 90
seldom in new formations, 90
silicate of, 70
smelting, 101
value, 36
where found, 14, 90
Corals, false, how made, 124

Descriptive list of useful minerals, 20-80
Diamond, 41
estimation of the value of, 86
imperfections of, 86
localities, 41
value, 41
Diamonds, characteristics of, 85, 86
colors of, 83
finest, 84
in Brazil, 84
in their native state, 83
mode of discovering in Brazil, 84
prospecting for, 83-87
where found, 87
Directions for determining specimens by the key, 15-19
Discovery of silver in Nevada, 134-137

Effervescence in minerals, 12
Eliason, Mr., 133
Emerald, false, how made, 116
to test, 118
Emery, 41, 42
localities, 42
value, 42
Epsom springs, 109, 110

False amethyst, how made, 117
carnelian, how made, 117
corals, how made, 124
False emerald, how made, 116
opal, how made, 117
pearls, how made, 124
ruby, how made, 116
sapphire, how made, 116
topaz, how made, 116
Feather river, Cal., gold in, 132
Fluor spar, 42
localities, 42
value, 42
Franklinite, 43
localities, 43
value, 43

Galena, 43, 44
and Cerussite, reduction of, 103
localities, 44
purest specimens poorest in silver, 91
value, 43
Garnet, 44, 45
localities, 45
the heaviest of gems, 118
to test, 118
value, 45
Gas springs, 106, 107
Gems, to test by weighing in water, 118
true and false, how to distinguish, 117-124
Glass, minerals which will not scratch, 16, 19
minerals which will scratch, 15, 18
Gold, 46-50
and platinum, washing for, 94, 95
and silver consumed in the arts in the United States, 137, 138
and silver, production of the United States, 137, 138
and silver where they abound, 14
artificial, how made, 125
bearing rock, 88
bearing sands, 88
extraction of, 93
Hill group, silver mines, 136
how distinguished, 89
imitation, how to detect, 125
in California, discovery of, 127-133
in California, first announcement of discovery, 132
in quartz rock, to find the amount of, 98
localities, 46-50
mine first worked in the United States, 133
ore, assay of, 95-98
searching for, 87-89
substances mistaken for, 89
testing any substance supposed to contain, 97
to separate from silver, 97
to test the purity of, 98
where found, 87-89
Granite regions, 14
Graphite, 50, 51
localities, 50, 51
to test the purity of, 104
value, 50
Gravity, mode of determination of, 12
Gray copper ore, 51
localities, 51
value, 51
Gypsum, 14, 52
localities, 52
value, 52

Heavy spar or baryta, 26
Hematite, brown, 56, 57
Horizontal beds, 82
Horn silver, 53
localities, 53
value, 53
Humphrey, Isaac, 128

Indications for minerals, 81
Irish Diamond, 114
Iron, chromic, 34
how it occurs, 94
ore, 14
assay of, 102
bog, 29
brown hematite, 56, 57
lenticular, 56
magnetic, 57,  58
magnetic, found by the compass, 91
micaceous, 62
red hematite, 65, 66
specular, 73, 74
pyrites, 53, 54
localities, 54
value, 53, 54
searching for, 91
spathic, 73
springs, 107, 108
testing minerals for, 91

Jackson, Captain Wm., 133
Jasper, 54
localities, 55
value, 55
Jewelry, artificial, how made and detected, 114-125

Kaolin, 55, 56
localities, 55
value, 55

Lead ore, assay of, 103, 104
to detect silver in, 99
searching for, 90
veins, thickest, 91
where found, 90
Lenticular iron ore, 56
localities, 56
value, 56
Limestone regions, 14
Limonite or brown hematite, 56, 57
localities, 57
value, 57

Magnesian springs, 109, 110
Magnetic, 12
iron ore, 57, 58
found by the compass, 91
localities, 58
value, 58
pyrites, 58, 59
localities, 59
value, 59
Malachite, 59, 60, 101
localities, 59, 60
value, 59
Manganese, oxyd of, 63, 64
spar, 60
localities, 60
value, 60
Marble, 60, 61
localities, 61
regions, 14
Marshall, Jas. W., discovery of gold in California by, 127-131
Metals, found near their source, 82
how they occur, 94
Mica, 61, 62
localities, 62
value, 62
Micaceous iron ore, 62
localities, 62
value, 62
Mineral riches, how discovered, 81
springs, 105-112
location of, 105
no indications of ores, 83
what are they, 105
Minerals as a source of our nation’s wealth, 9
descriptive list of, 20-80
regions which offer best inducements to search for, 14
sections of the United States, richest in, 14
species in the United States, how many, 11
specific gravity of, 12, 13
useful in the United States, 11
which will not scratch glass, 16, 19
which will scratch glass 15, 18
Mississippi Valley, 14
Money in the rocks, 9

Nickel, copper, 37
Nitre, 63
localities, 63
value, 63
Nodules, 82

Ochres, 91
Oil wells, 112, 113
Opal, false, how made, 117
the softest of colored gems, 118
Opaque minerals, 12
Ore on a hillside, indications of, 82
veins generally vertical, 82
when it will pay, 92
Ores, assay of, 92-104
minimum percentages of metal in which will pay, 93
Oxyd of Manganese, 63, 64

Pacific coast, 14
Panning, 94, 95
Paris brilliants, 114
Pastes, composition of, 115
Pearls, false, how made, 124
Platinum, 64
localities, 64
value, 64
washing for, 94, 95
Pockets, 82
Precious stones, color and order of hardness, 126
Prospecting for diamonds, 83-87
Pyrites, iron, 53, 54
cobalt, 35
copper, 37, 38, 90
magnetic, 58, 59
testing for gold, 96
yield of gold by, 97

Quartz mining in California, commencement of, 133
ores, yield of, 96
rock, to find the amount of gold in, 98
testing for gold, 95, 96
Quicksilver, use of in assaying, 96

Reading, Pearson B., 131
Read mine, first gold mine worked in United States, 133
Red copper ore, 65
localities, 65
value, 65
hematite, 65, 66
localities, 66
value, 65
silver ore, 66
localities, 66
value,  66
Rennselaerite, 67
localities, 67
value, 67
River sand, worth working for gold, 98
Rock crystal, 67
localities, 67
value, 67
salt, 68
localities, 68
suspected of containing silver, treatment of, 89
Rocky mountains, 14
Ruby, characteristics of, 85
false, how made, 116
spinel, 74
to test, 118, 123
Russia, gold how obtained in, 94
Rutile, 68
localities, 68
value, 68

Saline or salt springs, 109, 110
Salt springs, 110
Sapphire, false, how made, 116
the hardest of colored gems, 118
to test, 118
Searching for copper, 90
diamonds, 83-87
gold, 87-89
iron, 91
lead, 90
silver, 89, 90
Serpentine, 69
localities, 69
value, 69
Shaft, cost of sinking, 83
Silicate of copper, 70
localities, 70
smelting, 101
value, 70
Silver, 70, 71
and gold, consumption in the arts in the United States, 137, 138
and gold, production of the United States, 137, 138
glance, 71
localities, 71
reducing, 100
value, 71
horn, 53
in copper ores, 101
in lead and copper ores, 99
in lead ore, to detect, 99
to estimate the proportion of, 99, 100
in Nevada, 134-137
localities, 70
native gold in, 97
ore, assay of, 99, 100
brittle, 30
red, 66
ores, rich reduction of, 100
pure easily recognized, 99
searching for, 80, 90
to test a globule of for gold, 97
to test copper ores for, 99
where found, 89
Slate regions, 14
Smaltine, 72
localities, 72
value, 72
Smithsonite, 72
localities, 72
value, 72
Spar manganese, 60
Spathic iron, 73
localities, 73
value, 73
Specific gravity, mode of determination of, 12, 13
Specular iron ore, 73, 74
localities, 74
value, 74
Spinel ruby, 74
localities, 74
value, 74
Steatite, 75
localities, 75
value, 75
Stones, precious, color and order of hardness, 126
Strass for making false jewels, 115
Strontianite, 75, 76
localities, 76
value, 76
Sulphur, 76
localities, 76
springs, 108, 109

Testing minerals, 15-19
Thermal springs, 110, 111
Tin ore, 76, 77
assay of, 102, 103
localities, 77
value, 76
presence of, testing for, 103
Topaz, 77
characteristics of, 85
false, how made, 116
localities,  77
to test, 118, 120, 123
value, 77
Tourmaline, 77
localities, 77
to test, 123
value, 77
Translucent minerals, 12
Trap regions, 14
True and false gems, how to distinguish, 117-124

United States, consumption of gold and silver in the arts, 137, 138
gold and silver statistics of, 137, 138
Useful minerals, descriptive list of, 20-80
in the United States  11

Valuable minerals disguised, 10
Variegated copper ore, 78
localities, 78
value, 78
Veins, lodes and beds most valuable, 82
Virginia group, silver mines, 136

Wad, 78, 79
localities, 79
value, 78
Warm springs, 110, 111
Washing for gold and platinum, 94, 95
Washoe lake, silver mines near, 134
Wells, artesian, 111, 112
Willemite, 79
localities, 79
value, 79

Zincite, 79, 80
localities, 80
value, 79
Zinc ore, assay of, 102