Underground Treasures: How and Where to Find Them: A Key for the Ready Determination of All the Useful Minerals Within the United StatesOrton, James
Science
Underground Treasures: How and Where to Find Them: A Key for the Ready Determination of All the Useful Minerals Within the United States
Orton, James
Mineralogy, Determinative; Prospecting
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.
77.--WILLEMITE.
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.
78.--ZINCITE.
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.
[Illustration: decorative image]
CHAPTER IV.
PROSPECTING FOR DIAMONDS, GOLD, SILVER, COPPER, LEAD AND IRON.
MINERAL RICHES, HOW DISCOVERED--INDICATIONS--SEARCHING FOR
DIAMONDS, AND HOW TO DISTINGUISH THEM--PAYING LOCALITIES OF
GOLD--“FOOL’S GOLD”--PROSPECTING FOR SILVER AND COPPER--WHERE TO
LOOK FOR LEAD AND IRON.
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.
Public-domain text, read in full here on John Shaqi.
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