1870.] WHITAKEK SOFTH DOESET AND DEVON CHALK. 93 



4. — On the Chalk of the Southern Part of Dorset and Devon*. 

 !By William WniTAKERjEsq., B.A. (Lond.),F.G.S., of the Geological 

 Survey of England. 



As my rambles through. Dorset and Devon (in 1867-68) vrere made 

 from east to west, the same course wUl be followed in transcribing 

 my notes, a course that will alSo have the advantage of starting 

 from the point nearest to the Isle of Wight, the Chalk of which 

 has been described in a paper of which this may be taken as a con- 

 tinuation f. 



At the northern side of Swanage Bay, where the rocks are almost 

 vertical, the Upper Greensand, consisting of green -grey sand with 

 layers of nodular stones, is capped by evenly bedded Chalk Marl, 

 made up of alternations of lighter-coloured thicker and harder beds, 

 with darker thinner and softer, and forming a sort of ridge-and- 

 furrow foreshore, as in the Isle of Wight. The Chalk Marl has a 

 thick grey bed at top, and seems to be about 60 feet thick. It is 

 succeeded by hard bedded Chalk without flints, which again is soon 

 succeeded by a thin layer of the Chalk-rock, hard, with the usual ir- 

 regular-shaped green-coated nodular lumps (chiefly at the top) and 

 iron-pyrites. Above this is Chalk that weathers to a rough surface, 

 and higher up contains flints. Further east, at the highest part of 

 the cliff, the Chalk is less rough, and not so full of flints as in the 

 Isle of Wight. 



I was not able to get at the section between Ballard Hole and the 

 Foreland ; but enough has been already written on that part J. I 

 may remark, however, that two of the isolated pinnacles of Chalk 

 still have a little turf on the top, and so show the former continua- 

 tion of the land-surface, with its smooth sloping contour, due to sub- 

 aerial denudation, and greatly differing from the abrupt cliff against 

 which the sea washes. The cliff does not cut through the highest 

 part of the escarpment, but seems here to be along the flank of an old 

 pass or gap. 



In Studland Bay the junction of the Reading Beds and the Chalk 

 is piped ; but this is hardly- enough to prove unconformity between 

 the two formations. 



At the gap in the escarpment between Ballard and Nine-Barrow 

 Downs the almost vertical bedding is marked in part by distinct 

 even and parallel lines in the turf, caused by difference of growth 

 on harder and softer beds. 



A small pit on the flank of the escarpment about a mile and a 

 half eastward of Corfe Castle shows a northerly dip of about 60° in 

 the following beds : — 



* The district referred to is represented in Sheets, 16, 17, & 22 of the Map 

 of the Geological Survey of England. 



t Quart. Journ. Greol. Soc. vol. xxi. p. 400. 



J Rev. W. D. Conybeare, ' Outlines of the Geology of England and Wales,' 

 p. 110 (1822) ; Rev. W. B. Clarke, Mag. Nat. Hist. vol. x. pp. 414, 461 (1837) ; 

 Dr. J. Mitchell, ihid., p. 687 ; T. Webster in Englefield's ' History of the Isle of 

 Wight. ' 



