34 PROCEEDINGS COTTESWOLD CLUB 1904 
one, we shall have the complete sequence of deposits from 
the Upper Keuper to Lower Lias. This conclusion is 
followed out in the Table showing a “ Generalized Section 
of the Maximum Development of the Rhetic Series in 
Worcestershire,” and their relationship to the sub- and 
super-jacent stages (see page 44). 
From near Primsland End, 11% miles south-west of 
Droitwich Road Station, to a little south of Broughton 
House—a distance of three miles—the (Upper Keuper) 
red marls are faulted against the Lower Lias. A pond 
about 100 yards south of Upper Goosehill Farm shows 
red marls; whilst along the ridge a little to the south 
again are traces of Lower Lias limestone with Ostrea 
fassica. Broughton Green is situated on high ground, 
the escarpment being very marked to the west. In the 
east bank of the road-cutting opposite Broughton House, 
the “ Tea-green Marls” are exposed with bands of harder 
marl; whilst about 350 yards to the north-west, the base- 
ment-bed of the Rhetic (a sandstone) is seen resting 
upon similar marls in a pond-section. Along the escarp- 
ment the “ Tea-green Marls” are frequently exposed ; for 
example, 100 yards north-west of the pond-section referred 
to, and in an old pit—now utilized as a wood-yard—and 
roadsides a quarter of a mile south-east of Mere Hall. In 
the sides of the pond a little to the south-east of “ Little 
Lodge,” the Rhztic sandstone (17) is again visible, resting 
upon the “Tea-green Marls.” A valley then in.errupts 
the continuity of the escarpment. On the north side the 
‘“Tea-green Marls” are frequently in evidence, and there 
are numerous pieces of sandstone containing obscure casts 
of lamellibranchs, and covered with annelid-tracks and 
other markings. In the field south of, and in the cutting 
on the main-road from Droitwich, where it climbs the 
escarpment, the creamy-white marlstones of the “ Tea- 
green Marls” much resemble at a distance pieces of 
