. Manual of the geology of Ireland. ian south, at Rooneys Rocks, in a thin bed of redshale, close to an intruded mass of quartz rock, Oldhamiaantiqua is to be found. A few portions of the same fossilwere found in a green, arenaceous shale at Cahore Point,also tracks and burrows ; while in red shale, at the bathing-place to the north of Cahore House, are markings of Old-hapiia radiata. pTo the SW., on the coast south-east of Bannow, fossilsare very numerous ; (pidkamia antiqua and discreta (?)being abundant in some beds)\while O. radiata also these were found burrows o
. Manual of the geology of Ireland. ian south, at Rooneys Rocks, in a thin bed of redshale, close to an intruded mass of quartz rock, Oldhamiaantiqua is to be found. A few portions of the same fossilwere found in a green, arenaceous shale at Cahore Point,also tracks and burrows ; while in red shale, at the bathing-place to the north of Cahore House, are markings of Old-hapiia radiata. pTo the SW., on the coast south-east of Bannow, fossilsare very numerous ; (pidkamia antiqua and discreta (?)being abundant in some beds)\while O. radiata also these were found burrows of Arenicolites, two orthree other kind of tracks, and markings that look verylike Graptolites. /Here the Cambrian and Cambro-Silurianrocks are very much entangled together (Figs. 3^ and ^b\iwhile in both there are intrusions of quartz-rockj£ someof these being evidently contemporaneous with the deposi-tion of the Cambrian rocks, while others are newer thanthe Cambro-Silurians. It is remarkable that while the i8 Geology of Ireland,. Catnbiian. 19
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