UY riiE a(u:ncy of watf.k. 127 
},f remains of land animals can 
“ave been preserved. 
carcases of such ani- 
into 1 r ^ livers in their seasons of flood, 
.»ay at'fi T"”'*’ “‘"“■'S'' i‘ 
remain, ■ "^i j*?'’?' ®‘™"Se to 6nd terrestrial 
ofX I’ 'l l “ ^"“<*<1 at the bottom 
till ?K ‘““"'■"y ™“a>>es on recollec- 
on that the materials of stratifted rolls me 
derived m great part from the Detritus of more 
»i 
■l«y re, Mi,. i.,e„sd life ,L "hh sand 
'>"ildi.e.ofa„cis„rFOT, “““P' Pdm Ue.., .,.j 
4" Vl X°f r, -j! r 
r «pcdcr:ridt:i 
fora r«. P« vtTtrZSlI, r’ ““ 
tlrifted up from the shore bv tl 
*«rface in nianv parts u ! ^ ^ The 
all the irregular forms of cSedtnow ^and 
covered with undulations like tb^ ’ T'^ P''®®ents a surface 
-ater upon sand on Tsea shore p" "h 
tl‘e loose sand and solid limestone’ andT"^ 
^ow growing i„ the island. ^ 
fond b, of :: d a .rdTJS 
of Bude, and Perran 7^ i , ® the vil- 
t'^ice destroyed, and buL u H 
^traordinary tempests at d T ’ 
Geol. Soc of On ’ ‘^'*t'‘''t'“tervalsoftime. See Trans 
•lameson’s Tr i ® Geological Manual, 3rd edit, p 84 md 
Not. G of C..io,-. Thror, of Eoiih, su,"" 
