121 I Ml PERMIAN FORMATION. 



Soi'TIl SOAEIiE (a.) 



Ft. in. 



Alluvial (or Drift) Strata 21 



T ( Lower Lias Clay and Limestone, about 34 



ljlAS [Bhsetio Beds, about 45 



r New Bed Marl Keuper 614 



Trias : Lower Keuper Sandstone 252 



i \. u Red Sandstone (Middle and Lower Bunter) 564 



'Upper Permian Marls 88 6 



Upper Magneeian Limestone 40 6 



Middle Permian Marls 141 



i:\n .. I. i mi Limestone 26 



Marl slates. dark Oolitic Dolomites, and grey Dolomitic 

 Sandstones and Shales.containingaxini (?)and plant 



remains, with Breccia lit. thick at base 193 o 



n . (Coal Measures, (? Upper,) indurated Red Marls, with 



UBBOMUiROtb... | Q0dul( I Of In, list.. Q6 10 



i To be continued. ) 



2,030 



THE FLORA OF WARWICKSHIRE. 



AN ACCOUNT OF THE FLOWERING PLANTS AND FERNS 

 OF THE COUNTY OF WARWICK. 



HY JAMES K. RAGNALL. 



(Continued from page 104.) 



PAPAVERACEvE . 

 PAPAVER. 

 P. somniferum, Linn. White Poppy. 



Occurs as a casual on waste heaps and in cornfields ; iu cornfields, 

 My ton, //. B. ; waste heaps in Wheyporridge Lane, Solihull ; 

 a mere waif from cultivation.] 



P. Rhoeas, Linn. Field Poppy. 



Colonist : In cornfields, &c. Common. June, July. 



Occurs all through the county. 



Var. h. strigosum, Bcenn. 



I d cornfields. Bare. 

 II. BAyton and Milverton, II. /.'., Exchange Club Report, 1877, page 13. 



P. dubium, Linn. Long Smooth-headed Poppy. 



Colonist : On hanks, waysides, and in cornfields, &o. Common. 



June to August. 

 Var, a. Lamottei, Bor. 

 Abundant all through the county. 

 Var. b. Lecoqii, Lamot. 

 Cornfields, &c, in Lias and marly soils. Rare. 



tabulating of the rocks in the above section differs in several respects 



that adopted i>\ Profe boi Bull in Ins paper on the South Searlo boring, 



before the institute of Civil Engineers in L877. (See Proo. Inst, civil 



I eers, Vol, \li\.. part Lii.) I may say thai I have reeonstrurted this section, 



nation of the Cores, and a col n pari son of same with 



rock specimens of the formations to which 1 assign them, So far as the 



cerned, l vouch for the correctness of my section. Mr. 



ne, iii the new edition of the "Survey Memoir of the Geology of the 



1 ),)" seems to he ve ignored my paper on the 



South Soarle Bed lQ.J.G.8., vol. \\\v.. D. 812.) and fallen into the same error 



ij and Hull did, vi-.. of taking the Marl Slates of the 

 Soarle section to belong to the Carboniferous formation Hence tho uecessit\ 

 of this foot-note. 



