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Pennsylvania Geology Final Report Volume 1 1981

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222 GEOLOGICAL SURVEY OF PENNSYLVANIA.<br />

Banks in the hydromica belt south of York.<br />

Leaders Hill old opening, f m. W. of New Paradise ;<br />

slates dip 84°, S. 70° E. No ore showing.<br />

Hess hank., 5 m. S. of York, 2 m. W. of Logansville ;<br />

150' long, 15' deep ; 1868 ; ore too sandy; slates ashestiform.,<br />

vertical, strike N. 20° E.<br />

Falkenstine shaft, abandoned.<br />

Meyefs {B.) bank, 1200' N. W. of Gladfelter's railroad<br />

lean ore in vertical slate striking N. 30° E.<br />

station ;<br />

StambacK s sJtaft, \ in. W. of station in dark slates<br />

;<br />

holding crystals of micaceous and magnetic ore.<br />

Gladfeltef s bank, f m. W. of station, 10' deep in vertical<br />

slates, striking N. 34° E.<br />

Geisselman s bank, J m. W. of railroad between Gladfelter's<br />

and Seven Valley (Smysers) stations ; four small<br />

shafts sunk 1870, in hydromica slates impregnated with<br />

iron oxide.<br />

Thomas Iron Co.''s banks, J m. S. W. of Smyser's railroad<br />

station ; two banks and three shafts, ^ acre and f acre,<br />

engine house, drifts, etc.*<br />

Walters- bank, | m. N. of W. of Hanover Junction railroad<br />

station 1872 much hard limonite still visible in<br />

; ;<br />

bunches in ciay of decomposed coarse-grained slate ; f acre,<br />

40' deep.<br />

Croufs bank, I m. N. E. of Strickhauser' s station, Han.<br />

Br. RR., 800' along the road, 18' deep; hard, compact<br />

sometimes operated.<br />

sandy limonite ;<br />

KnotwelV s shaft on the York I. Co.'s hill; Aug. 1874,<br />

had reached hard ore (at 27') same as York Co.'s ore.<br />

mat., 10.94; sulphur, none; phosphorus, 0.69; alum., 1.92; lime, 0.17; mag-<br />

nesia, 0.56; manganese, 0.33 ; undetermined, 0.91.<br />

A finely laminated bluish limestone containing white crystalline limestone<br />

scattered through it in spots resembling in certain portions a calcareous<br />

conglomerate, in others simply mottled, appears in both banks, and in the<br />

run, dips 85°, N. 20° W. In a quarry near by it is so mixed with crystalline<br />

hydromica flakes as to mimic hj'^dromica schist, although containing 78 per<br />

cent of carb. lime and magnesia; thickness perhaps 400'. This is an im-<br />

portant observation. (C, p. 15. )<br />

* Statistics in C, p. 27. AnaU'sis : Iron, 51.7 ; no sulphur ; phos., 0.052 ; sil. ,<br />

6.0; alum., 16.4, etc.

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