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NJDEP - NJGS - First Annual Report of the Geological Survey of the ...

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84',WAYWAYANDAMINH.This mine is situated on <strong>the</strong> Wawayanda Mountain, half amile from <strong>the</strong> New York State line, and two and a half milesnor<strong>the</strong>ast <strong>of</strong> <strong>the</strong> Wawayanda :Lake. The prevailing char_/cter<strong>of</strong> <strong>the</strong> rock, in which <strong>the</strong> ore occursi is gneiss.. It is exceedinglyvariable in composition and texture. Mica enters butslightly into any <strong>of</strong> <strong>the</strong> rocks throughout <strong>the</strong> whole mountain,and in many places it is entirely absent When en,irely absent_hornblende_ or magnetic iron ore, in grains, takes itsplace, forming a syenitie gneiss. The rock in some places iscomposed only <strong>of</strong> feldspar and quartz_ <strong>the</strong> former being itsprincipal ingredient.• Four deposits <strong>of</strong> ore havt_been opened and _vorked. Theirprevailing course is nor<strong>the</strong>ast aud southwest_ and <strong>the</strong>ir dipfrom twenty to forty degrees to <strong>the</strong> sou<strong>the</strong>ast..Commencing at <strong>the</strong> sou<strong>the</strong>asterly deposit, and taking <strong>the</strong>min <strong>the</strong>ir numerical order, we find that <strong>the</strong> flint is not'worked •at <strong>the</strong> present time, and has not been for several years, because<strong>the</strong> Qre is more accessible and more abundant ia <strong>the</strong> o<strong>the</strong>rdeposits. On account <strong>of</strong> <strong>the</strong> water in <strong>the</strong> shaft, and <strong>the</strong> dilapidatedcondition <strong>of</strong> its timbering_ I was unable to make a per-.sonal examination_ but I was, however, informed by <strong>the</strong> miningcaptain, that it has been worked to <strong>the</strong> depth <strong>of</strong> one hundred',• and ten feet, and c_te hundred on <strong>the</strong> deposit ; and that, <strong>the</strong>ore is from twelve to fourteen feet in width, at <strong>the</strong> bottom <strong>of</strong>'<strong>the</strong> shah.• The Second deposit occurs fifty feet northwest, "<strong>of</strong> <strong>the</strong> first.It has been worked to <strong>the</strong> depth <strong>of</strong> eighty feet, and one hundredfeet on <strong>the</strong> deposit ; and at its pr_entin width.del_th is thirty feetThe third deposit is seventy-five feet from <strong>the</strong> second.Here <strong>the</strong> ore occurs in <strong>the</strong> form <strong>of</strong> a bed, or irregular deposit_varying from two to twelve fe_t, iu width. __t its presentdepth, one extremity <strong>of</strong> <strong>the</strong> workings shows <strong>the</strong> ore six feet inwidth_ and <strong>the</strong> o<strong>the</strong>r two feet.NEW JERSEY GEOLOGICAL SURVEY

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