VOL. XV. (1) RHETIC ROCKS 25 
Crowle a thick deposit of sandstone containing one or 
more species of the genus Schzzodus (in the form of 
casts) is exposed in the side of the road opposite the 
turning for the Church from the Worcester road; and 
again in the sides of the pond at Crowle Green. 
a.—The Crowle Section. 
The best section of the Lower Rhetic in Worcester- 
shire—of which, however, there is no mention, except 
that it was visited by a party of the Dudley and Midland 
Geological Society on May 29, 1877 ‘—is situated at the 
junction of the road from the house known as “ Frisland” 
and that from Oddingley. It is easily accessible: not like 
that section seen in the railway-cutting at Dunhampstead, 
which is necessarily difficult of access. The beds in the 
THE CROWLE SECTION. 
(“Tea-Green Marls.") 
Upper Keuper. - 
“Tea-Green Marls" 
Maris. 
pee, 
Scale : 
ae Horizontal. 
«, Diets it 20 Feet. 
9 F Vertical. 
8 Feets 
> Fic, 1 
Crowle section are affected by a fault (fig. 1) having 
a downthrow of about 14 feet. The ‘“Tea-green Marls,” 
which are well exposed, comprise creamy white marls, 
1 Proceedings, Vol. iii., p, 106; but see also Geol. Mag., Dec. 4, Vol. x., 1903, p. 80. 
