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t_FIRST ANNUALREPORTOFTHE, GEOLOGIC
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SUPERINTENDENT'SREPORT.To his ]_'xe
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falls and courses, all depend, to a
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7accomplish this most successfully,
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9its proper basis. Had it not been
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11It is in consequence of such tran
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i3year 7a further appropriation of
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715currenoc of minerals ; and the e
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L17• , : P •The instrument rese
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oI,19along the Delaware River, and
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to the Delaware River/a little belo
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"23capital, as well as to thecounty
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25EXPENSES OF THE S1JRVEY.IJ'pon or
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'27Trigonometrical and Topographica
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crossing the county m a northeaster
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32"1st. The'Oneida or' Shawangunk "
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84',WAYWAYANDAMINH.This mine is sit
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36:e_'als; .in others it occurs in
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38though it requires much'more heat
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'40• "Them are other kinds of ore
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4_the foot of a sandstone ridge. It
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- Page 90: 46] Syenite.2. Magnetic iron_ from.
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- Page 104: its action upon soilS, but it very
- Page 108: 54Ri_,er is chiefly of a loamy, cal
- Page 112: i ,i"i,REPORT•OF PROFESSOR GEORGE
- Page 116: 58running into the Atlantic. With t
- Page 120: 6Obeen able to ascertain the areas
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- Page 128: 64. -Colt's NeCk, and indeed entire
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- Page 142: o7Okl/owledge, been found in Salem
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- Page 154: 76cellent effects. The dry-bank mar
- Page 158: A large number has been collected,
- Page 162: 8Ominatious having been made, besid
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- Page 170: 84On "examination and comparison of
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- Page 178: 88eept in containing much less phos
- Page 182: W90oxidation which iron pyrites_ in
- Page 186: NEW JERSEY GEOLOGICAL SURVEY
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94observed by Prof. Rogers), which
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REPORTOF EGBERT L. VIELR, TOPOGRAPH
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" l97the greatest care and accuracy
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prinelpal points were established b