THE 
EED SANDSTONES, CONGLOMERATES, AND 
MAELS OF DEVONSHIRE. 
In the last paper which I had the pleasure of reading to the 
Members of this Institution, I gave some account of the principal 
phenomena exhibited by the Red Rocks in the cliff section, exten- 
ding from Torbay to the Straight Point* east of Exmouth. On 
this occasion, I purpose taldng up the history of the formation 
where it was then dropped, and following the coast-line from the 
Straight Point to Cbarton Bay, near the south-eastern verge of 
Devonshire, where the Triassic beds disappear beneath the White 
Lias. 
That the section to be investigated is of very considerable 
extent, will be seen from the following distances and bearings : — 
From Straight Point to Otterton Head 3 miles N. G0« E. t 
BY W. PENGELLY, F .E. S., F . G . S . 
DISTANCES. 
BKARINGS. 
Otterton Head to High Peake Cliff . 3 
High Peake Cliff to Beer Head 8 
Beer Head to White Cliff near Seaton 1 
White Cliff to Charton Bay 4 
N. 80"=* E. 
N. 80° E. 
N. 38' E. 
E. nearly. 
* Misprinted " Flat Point " in my second paper. — Trans. Plym. Inst., 
1862-3, p. 15, &c. 
t The distances and directions are measured on the Ordnance map. 
