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Ch. 2: Maine Pegmatites: Local Descriptions

Ch. 2: Maine Pegmatites: Local Descriptions Page of 170 Ch. 3: Economically important Pegmatite Minerals Text size:minus plus Restore normal size   Mail page  Print this page
FELDSPAR.                                                      127
quarrying districts to Trenton, the principal feldspar milling center, ace given below:
Freight rates per hundredweight on feldspar for carloads having a minimum weight of 40,000
pounds, May, 1909.
Bath, Me., to Trenton, N.J.................................... $0.15
Cathance, Me., to Trenton, N.J.................................17
Auburn, Me., to Trenton, N.J...................................16
The requirements of the potter's trade demand that in general the percentage of free quartz associated with the feldspar used shall not exceed 20 per cent in the ground product, and certain potters demand a spar which is nearly pure, containing probably less than 5 per cent of free quartz. In order to be profitably worked, in most feldspar mines between one-fourth and one-half of the total material excavated should contain less than 20 per cent of free quartz. Freshness of the feldspar is not essential.
A factor of the utmost importance in the mining of pottery spar is the quantity of iron-bearing minerals (black mica, hornblende, gar­net, or black tourmaline) which is present and the manner in which these minerals are associated with the feldspar. The requirements of the pottery trade demand that the spar be nearly free from these minerals, which if present produce, upon firing, brown discolorations in white wares. In order that a deposit may be profitably worked, these minerals, if present in any appreciable quantity, must be so segregated in certain portions of the deposit that they can be sepa­rated from the spar without much more hand sorting and cobbing than is necessary in the separation of the highly feldspathic material from that which is highly quartzose or rich in muscovite. A number of pegmatite deposits of coarse grain are rendered worthless for pot­tery purposes by the abundance of one or more of these iron-bearing minerals. The presence here and there of minute flakes of white mica (muscovite) is characteristic even of the highest grades of com­mercial feldspar, and chemically this mineral is not injurious. It is, however, exceedingly difficult to pulverize the thin, flexible mica plates to a fineness equal to that attained by the feldspar, and it is therefore necessary in mining to separate carefully as much of the muscovite as possible from the spar.
Operation on a large scale with the aid of modern machinery reduces the mining cost. Favorable topographic position—a situa­tion, for instance, that will permit the material to be excavated from a hillside opening instead of being hoisted from a pit—also reduces the cost.
MILLING.
The methods used for grinding feldspar for pottery, enamel ware, etc., are similar in a general way in all of the Eastern States and are very simple. The soda spar quarried in southeastern Pennsyl-
Ch. 2: Maine Pegmatites: Local Descriptions Page of 170 Ch. 3: Economically important Pegmatite Minerals
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