. Acadian Geologie [microform]: Die geologische Struktur, organischen und mineralischen Ressourcen von Nova Scotia, New Brunswick und Prince Edward Island. Geologie; Paläontologie; Geologie; Geologie; Naturwissenschaft; Paléontologie; Géologie; Géologie. [Mens von Lügen, diese s von Dif-Ormationen k'ery fair das Erz, das hatte iramit der, auf dem p in diesem Beinvenen) f Kupfer, da bei al Struck, die wlcdge der Ordnungsmäßigkeit r Duncan hinreichend zu einem sehr ineer und jandoned. Eine Excel - Die) oniferous mplicated ic Felsen jn Der [ands lOAvs, ^s in bunten Ip bei hohen tauchen Ausbildung lumerous fcome Dis-gesehen-s

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. Acadian geology [microform] : the geological structure, organic remains and mineral resources of Nova Scotia, New Brunswick and Prince Edward Island. Geology; Paleontology; Geology; Geology; Geologie; Paléontologie; Géologie; Géologie. [mens of lies, this s of dif- ormation k'ery fair the ore, that had iramit of on which p at this veins of )f copper, since, by at struck al, which wlcdge of regularity r Duncan ufficiently at a very ineer, and jandoned. an excel- lOAvs the )oniferous mplicated ic rocks jn of the [ands, the ^s seen in -coloured Ip at high dipping Formation lumerous fcome dis- sisting of pact trap, distance appears angular 1 TUURO TO CAPE DOR. 103 1 t S fragnionts of lilack shale constituting a kind of breccia. The sand- stone underlying this bed of trap contains small nodules of sclcnite and narrow veins of reddish fibrous gypsum. No other volcanic rocks occur in the coast .section near these trap conglomerates. Westward of this place, the section is occupied for about three miles by soft red sandstones with greeni.sli bands, dipping generally to the .south-west: some of them are divisible into very thin layer.s, wliilst others arc compact and form beds sevci-al feet in thickness. Near ^foosc liivcr, the red sandstones meet black .slinles and hard gray sand.stoncs of the Carboniferous system, containing Cordaites, Ferns, and Lvpidodcndra* At this place the junction of the two groups of rocks was not, at the time of my visit, well expo.sed in the cliflf, and had the ajjpearance of a fault; but as seen in the horizontal section on the beach, the rod sandstone with a .south-we.st dip seems to overlie unconformably the carboni- ferous strata, dijijjing at a high angle to the E.N.E. On the west side of Moose Kiver the Carboniferous strata include three large masses of trap which have altered the grits and shales in contact with them, causing them to assume reddish colours. IJcyoiul the last of these masses of trap, the shales and grits, there dip- ping

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• bookcentury1800
• booksubjectgeology
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