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

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66htindrcd feet at Red Bank, and in <strong>the</strong> lffevisinks iit is equally ..thick. Whenever this sand has any degree <strong>of</strong> firmness it isfull <strong>of</strong> <strong>the</strong> impressions and casts <strong>of</strong> shells and ,o<strong>the</strong>r fossils.The lower part <strong>of</strong> this bed is a very friable sand i towards itsupper part a gi'cenish clay is found mixed with <strong>the</strong> sand, givingto it a good degree <strong>of</strong> firmness; <strong>the</strong> rock at Tinton Falls is anoxampte <strong>of</strong> this. The.uppar part <strong>of</strong> this bed, from four to sixfeet,'is a l_yer <strong>of</strong> greenish indurated clay, in some places hardenwagh to be called a rock. It slakes on exposure to <strong>the</strong>wea<strong>the</strong>r. No marl grains are found in it; but i_ is called.marl 'by rainy farmers, and is pr<strong>of</strong>itably used as such ....The _econd bed <strong>of</strong> marl is not so extensively developed in• this part <strong>of</strong> <strong>the</strong> country as <strong>the</strong> first elan; though it' is considerablythicker. Its several layers may be described as fol -_. lows :--1. A layer <strong>of</strong> marl containing but very f_w fossils; itslower part almost clean grains; clay is mixed With.<strong>the</strong> grainsin <strong>the</strong>'upper part, in many localities. The colo_.<strong>of</strong><strong>the</strong> grainsin this layer, and indeed in <strong>the</strong> whole bed, isl green with ashade-<strong>of</strong> yellow, unlike those in <strong>the</strong> first bed_ in which <strong>the</strong>color is green, with a shade <strong>of</strong> black or dark blue. I have notin any place in this part <strong>of</strong>'<strong>the</strong> county found <strong>the</strong> layer workedmore than fourteen.feet, though I believe it to be much thicker.In <strong>the</strong> pits <strong>of</strong> Mr. Imlay, on Crosswicks Greek, a short distancebelow lqew Egypt, it is nearly twenty-five feet.2. 2k layer <strong>of</strong> from ten to fourteen feet <strong>of</strong> marl, with nu- ".merous shells. A streak in'<strong>the</strong> uppcr part <strong>of</strong> tt_is, for two orthree feet, is almost solid with shells <strong>of</strong> <strong>the</strong> T erebratula hat.lani;'and ano<strong>the</strong>r layer near <strong>the</strong> bottom <strong>of</strong> it is cqually solidwith shells <strong>of</strong> <strong>the</strong> Gryphaea convexa. This layer graduallyloses its marl grains, at <strong>the</strong> upper part; and runs into3. 2k layer <strong>of</strong> broken shells with more or less sand.intermixed,and containing scarcely any marl grain_.. The color <strong>of</strong>this marl is yellow or g_ay. In <strong>the</strong> neighborhood <strong>of</strong>'Eatontownit is called yellow _narl.. No localities have been visitedin Eastern Monmouth where it has been penetrated more thanfourteen feet, but, near Salem it has been opened for more thantwenty feet.NEW JERSEY GEOLOGICAL SURVEY

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