. Handbuch der Geologie von Irland. ^ jfi^ Sh/^^^^^^^^^^^^ k^(in der gelben Sandstein, rAnodonta Jukesii, w&s gefunden/am unteren Glanmire Road, eine Meile und eine Hälfte osten ofCork und Gokane Punkt, westlich von Toe-Kopf, wo arealso der Pflanzen Adiantites Hibernicusand Sagenaria; die Stängel der Pflanzen, nur, sind Kopf und Castlehaven foundbetween Toe. In diesen localitiesthe gelbem Sandstein ist unter Karbon Schiefer, butin die gelben Sandstein, unter dem unteren LimestoneShale an Talg Brücke, an der Kreuzung von Cork und Waterford, wie Assemblage von Fossilien auftritt. Es scheinen, dass die Fa

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. Manual of the geology of Ireland. ^jfi^Sh /^^^^^^ k^ (in the Yellow Sandstone, rAnodonta Jukesii, w&s found /at the Lower Glanmire road, a mile and a half east ofCork, and at Gokane Point, west of Toe Head, where arealso associated with it the plants Adiantites Hibernicusand stems of Sagenaria; the plants, only, are foundbetween Toe Head and Castlehaven. In these localitiesthe Yellow Sandstone is under Carboniferous Slate ; butin the Yellow Sandstone, under the Lower LimestoneShale at Tallow Bridge, junction of Cork and Waterford, a like assemblage of fossils occurs. It might seem that the famous fossil localities at Kiltor-can, south-west of Thomastown, County Kilkenny, and in 62 Geology of Ireland. the promontory of Hook Head, County Wexford, shouldbe here mentioned ; these, however, are apparently in the Old Red Sandstone, or Lower Carboniferous Sandstonesand shales like those of the central plain, and the questionof their age will be discussed in the next chapter. Plate III.]. IV. H. Baily, del. Lower Carboniferous Fossils. 63 CHAPTER V. CARBONIFEROUS FORMATION. Lower Carboniferous. In the previous chapter are described the Carboniferousrocks peculiar to SW. Ireland ; they being most typicalin the county of Cork. In this and the succeeding chapteris given a brief history of the Carboniferous rocks of therest of the country, divided into Upper and Lower. (TheLower Carboniferous includes all the rocks from the base ofthe arenaceous rocks, generally called Old Red Sand-stone, to the uppermost bed of the Upper Limestone, while the Upper Carboniferous is represented by the CoalMeasures. The Old Red Sandstone is included in the Carboniferousformation, because in no place in Ireland has it a definedupper boundary, one group graduating into the other;and usually the lowest grey and blue beds of grits orshales of the Carboniferous formation are taken as itsuppermost limits. Furthermore, only in Munster and inthe hills between Lough Erne and Pomeroy, Counties ofFerman

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• bookcentury1800
• bookdecade1870
• bookpublishe
• booksubjectgeology