193 
ANGLESEY AND CAERNARVONSHIRE. 
‘sytney if "SHOOT OSOJSITOS WOOL “O 
‘purs UAMOTY “TT ‘SOLLOS OSOJSTYOG ‘OM SYSITOS ZINN’) “G 
OW SOYVIS YOU ‘OL “‘SyOOL are eee "p 
& : ‘go]BIS PUL SOUT jae °6 “BOUL YM ‘YOOd plopluvas porno[oo-qysiyT “Eg 
HISUA MSS OMS WRT CRGTAUCYG) “spoq ka3ep pue Sacioere ze) ‘uvijeu(T, “yoou ystyuid pue ystucord pouters-louly “G 
‘OJVAIULO]SUOD ULLIQULUD [Teseg “J, ‘yoOd PIOPULAS yarep ‘pourvis-oorey *T 
‘NVIUANVO 
ee 
g 
Se es ea 
aE 
! 
! 
| 
ee TOILIG *SOTORJULTT 
so0ig-Ay, 
‘NVIUGNVO 
= Se SN  —————— — 
L 8 OS 
RIT LI fi I MS fa 
{ LeUgtt SZ Wf (ey 
i S 
! | “ANNA 
‘Sopory-WATT ‘udsiq-A4-uey, 
Jo pue yj10 NN 
(‘o[IUL [ 0} seTOUT g o[BOS [e}Uoz1L0F{ ) 
‘hosopbuy ‘uoung hnaywmaz sooug-hz, 09 ‘bojovfunpy hq ‘uhug-h-wn,7, wWoutf WOYLI0I—'T, “STi 
but here large fragments of undoubted Dimetian rocks occur as 
well-rolled pebbles, and every variety found in the underlying 
zed in the pebbles or fragments in the con- 
T have had several of these pebbles cut, and also some 
€ recogni 
Ps 
Er, 
rocks may b 
Q.J.G.8. No. 15 
glomerate. 
