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

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posed <strong>of</strong> one or more <strong>of</strong> <strong>the</strong> following simple minerals :--feldspar_quartz, hornblende, and mica.. They occur in veins_dikes_ great irregular masses traversed by joints and divisionalplanes, constituting mountains_ ridges, &c.AquEous Rocg_s.--The aqueous rocks arb those whichhave been formed by <strong>the</strong> agency <strong>of</strong> water, from <strong>the</strong> disintegratedparticles <strong>of</strong> o<strong>the</strong>r rocks transported by currents, and depositedas sedimcnt, in <strong>the</strong> form <strong>of</strong> strata, beds, layers, laminm_&c. They very <strong>of</strong>ten contain organic remains <strong>of</strong> plants andanimals.META_IOI1PHIC RocKs.--The metamorphic rocks are thosewhich have been formed by aqueous agencies, and subsequentlyso much altered in <strong>the</strong>ir texture by <strong>the</strong> action <strong>of</strong> heat_as to resemble igneous rocks. They contain no visible organicremains.The above is a very general classification <strong>of</strong> roeks_ derivedfrom <strong>the</strong>ir origin. The)- are subdivided into groupscalled systems_ according to <strong>the</strong>ir relative age. It is to be regrettedthat much confusion prevails in regard to <strong>the</strong>ir nomen-.elature.Every country, and almost every geologist, has a particularsystem <strong>of</strong> names, derived ei<strong>the</strong>r from characteristic fossils,localities, or some lithulogical peculiarity <strong>of</strong> <strong>the</strong> rocks. Thosemost generally used and understood in this country_ are thnnomenclature <strong>of</strong> <strong>the</strong> English geologists, and that proposed by<strong>the</strong> geologists <strong>of</strong> <strong>the</strong> New York survey. Thd former is chieflyderived from localities in Great Britain, <strong>the</strong> latter from locali*ties in N'ewYork where particular groups <strong>of</strong> rocks arc welldeveloped. As this was <strong>the</strong> first attempt at a complete classification<strong>of</strong> <strong>the</strong> rocks <strong>of</strong> this country_ it has been generallyadopted in different States <strong>of</strong> <strong>the</strong> Union, and undoubtedly willremain as a standard <strong>of</strong> comparison. Geologieal investigationarranges and classifies <strong>the</strong> roeks_ represents <strong>the</strong>ir extent, thickness,and order <strong>of</strong> arrangement_ by means <strong>of</strong> sections, pr<strong>of</strong>iles,&c. ; points out and describes <strong>the</strong> valuable mineral deposits <strong>of</strong>each formation, and <strong>the</strong> manner in which <strong>the</strong>y may be workedand applied to various economical purpose_ But in order toiLLNEW JERSEY GEOLOGICAL SURVEY

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