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

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87texposes a, mass'<strong>of</strong> ore nine feet i a width, associated to a considerableextent with grains <strong>of</strong> qua/'tz and ;feldsPar;but freefrom iron pyrites: Small specks <strong>of</strong> carbonate and sulphuret<strong>of</strong> copper, ire disscmif_ated through some :parts <strong>of</strong> it, but notin a sufficient qdantity to injure it'as a 'furnace. ore, for whichit will answer an excellent purpose. " • "Following <strong>the</strong> summit <strong>of</strong> <strong>the</strong> Wallkin Mountain towards .<strong>the</strong> sbuthwest, I observed many indications <strong>of</strong> large deposits<strong>of</strong> ol'e. Undoubtedly very extensive beds may be.opened inthis vicinity, which atno distant day-Will prove a source <strong>of</strong>• great pr<strong>of</strong>it to <strong>the</strong>ir proprietors.' 'SHERMANTSMINE.This mine is situated on Slack Brook, three quarters <strong>of</strong>'amile sou<strong>the</strong>ast <strong>of</strong> Sparta. Several deposits <strong>of</strong> ore are exposedon ei<strong>the</strong>r side <strong>of</strong> <strong>the</strong> brook, varyifig from three to ten feet inwidth. ' They are very irregular, having no well defined walls,and, in many places, it is difficult to ascertain <strong>the</strong>ir limits, bec_iuse<strong>the</strong> ore is disseminated to a considerable extent through<strong>the</strong> adjoining rocks.• " : ' _ ' HEMATITE. :[This ore <strong>of</strong> iron I when pure, has a,'meiallic appearance ; is<strong>of</strong> various shades <strong>of</strong> color, and is'composed <strong>of</strong> seventy metalliciron and thirty oxygen, in one hundred parts. 'I_ is easilyclistinguished from o<strong>the</strong>r ores <strong>of</strong> iron by its reddish streaJ_ andl_owder. 'In nature it rarely cecum in a pure state, hut gener-_.lly mingled with 'lime, silica, alumina, &c._ when its valuedcper_ds on <strong>the</strong> nature and proportion <strong>of</strong> <strong>the</strong> .foreign materialIt is generally found in beds or irregular deposits associatpdwith igneous and metamorphic rocks, .more frequently in <strong>the</strong>latter, or at <strong>the</strong> junction <strong>of</strong> <strong>the</strong> two. A great part <strong>of</strong> <strong>the</strong> ironmanufactured in different countries is "from this ore, and al-NEW JERSEY GEOLOGICAL SURVEY

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