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

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10• amino into <strong>the</strong> causes <strong>of</strong> <strong>the</strong>se changes, and chemistry revealsto us <strong>the</strong> laws by which <strong>the</strong>y are governed. It has been saidby Bisch<strong>of</strong>_4. <strong>the</strong> celebrated chemical geolo_st, that our earth_as far as we know it_ is a'grcat chemical laboratory, in whichsinc_ <strong>the</strong> period <strong>of</strong> its creation uninterrupted chemical processeshave been in operation, and will continue so long as itdescribes its course around <strong>the</strong> sun. The soil, <strong>the</strong> atmosphere,animals, and plants, arc constantly undergoing changes ; andeach performs its part in <strong>the</strong> great and uninterrupted circle <strong>of</strong>transmutations.:Rocks arc composed <strong>of</strong> one or more distinct substancescalled simple minerals, such as quartz (silica), feldspar: mica_hornblende, carbonate <strong>of</strong> lime, tale, oxide <strong>of</strong> iron, &c. Thesesimple minerals are composed <strong>of</strong> elementary substances 2such"as oxygen, hydrogen_ carbon, silioium_ aluminum: potassium,sodium, calcium_ &c., which uniting toge<strong>the</strong>r in twos form binarycompounds ; and it is in this latter state that <strong>the</strong>y occurin minerals.• The most common binary compounds are silica, composed<strong>of</strong> oxygen and silicium; alumina_ <strong>of</strong> oxygen and aluminum;llme, <strong>of</strong> oxygen and calcium ; potash_ <strong>of</strong> oxygen and potassium,&c.Reeks are sometimes classified according to <strong>the</strong> prcdomi-* _ nancc <strong>of</strong> some one <strong>of</strong> <strong>the</strong> above bilmry coinpounds---as a siliciouSor arenaceous rock: one in which quartz predominates;an argilIasoous rock, one in which alumina or clay predomi-0nares; a calcareous rock, one <strong>of</strong> which lime is <strong>the</strong> principalconstituent; and a carbonaccous rock, one in which carbonprevails.Almost all <strong>the</strong> changes that take'place in <strong>the</strong> rocks andmaterials, organic or inorganic, which constitute <strong>the</strong> crust o_<strong>the</strong> oarth_ or grow upon its surface, have <strong>the</strong>ir origin in <strong>the</strong>transformations <strong>of</strong> <strong>the</strong> simple elementary bodies. Having aknowledge <strong>of</strong> <strong>the</strong> laws by which <strong>the</strong>se transformations aregoverned, we are able to apply <strong>the</strong>m to <strong>the</strong> various usefulpurposes <strong>of</strong> life.* BiBeh<strong>of</strong>'BGeologic--_IntroduetloD.NEW JERSEY GEOLOGICAL SURVEY

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