240 MR. GARDINER AND PROF. REYNOLDS ON || May 1902, 
it lies. The dip of these beds is somewhat variable and is, as a 
rule, a little west of south. They have yielded :— 
Chonetes striatella, Dalm. Spirifer elevatus, Dalm. 
Rhynchonella nucula, Sow. Pterinea sp. 
Spirifer crispus, His. | Crinoidal ossicles. 
B(9). This band of green ash occupies the little inlet immediately 
east of Carrigard. 
B(13) is a thick band of rhyolite, which forms almost the whole 
of the rocky peninsula north-west of Owen. The rock is generally 
of the compact pale-green type, but shows a considerable amount 
of variability, and is sometimes banded. Often it contains numerous 
xenoliths, causing it to resemble a tuff; and there are some un- 
doubted tuff-bands present in it. 
In the southern part of the exposure the rocks begin to show 
signs of crushing and disturbance. These are still more marked in 
B(14), and increase till the fault at the little inlet of Owen is 
reached. 
. 
(c) The Coast-Section from Coosmore to Coosglass. 
For the greater part of this long coast-section the succession 
is easy to make out, as the beds, though sometimes faulted, are not 
much disturbed. From Trabaneclogher to Ferriter’s Cove, the 
coast runs in the main with their strike. The following is the 
succession: at the top :— 
Thickness in feet. 
CL). Gritty laps andl ielaties: 50324scnctesse some ee ee about 550 seen 
| Here follows a gap without exposures, equivalent 
to a thickness of about 200 feet. | 
C(2) Green and yellow sandstones and slates, with ashy 
baride in the lower ipart- ovo y..cce ce eee about 420 seen 
C(3) Green ash, with large dark fragments .................. 8 
C (4) “Red sandstone with ash-bands ...3../....00..d:2.2e ee 340 
Cb). Intrusive preenstones 2.5.4: .aasvnaesiaade 2s dees nee eae 30 
C (6). Fairly coarse salt} io.: tisn522 dee ctens+aeet-e ac eee ee fh 
C(7) Rhyolite, with two ash- bands, >->,.ce te eee ae 248 
C(8) Ashes, weathering pale-grey or white.................-00 25 
C (9) Caleareous sandstone and flags, with thin ash-bands. 1390 
C (10) Coarse conglomerate, with a fine grit-band ............ 30 
C (11) Sandy and ashy beds and conglomerate ............... 70 
C (12) Blayolite: 2.55.0, 2 <ccsnss cate seaae te eae ~onedans Sie eee 25 
CUS). ABM. 05.0i0i ee cnd Soe eens tape sens Ae ee 31 
C (14) Sandy limestone, weathering veliow .............. ceo 40 
C (15) Red sandstone, with ashy and shaly layers ...:........ 180 
C (16) Brown and yellow sandstone, much crushedand veined 40? 
@(17):Green rhyolite and ash ....ca0ccgdaeees. ee eee eee 6 
Fault. 
C (8) Labradorite-porphtyrite. ...../7..0.0 32-8 scan ee oe 115 
Fault. 
C(19) Pimkeand green slates .:21.05:-)ia0ke Yeekey eee a eee 210 
C20) Conmplomerate: | i1. 625 .60-0d605055: Anglo peed oe ee 6 
Excluding the intrusives, this gives a thickness of 3624 feet seen. 
