130 ME. S. S. BUCKMAN ON THE BAJOCIAN [Feb. T9OI, 



Generalized Section of the North Cotteswolds. 



Tjy .. Thickness in 7- 7... 



tormation. c, , Localities. 



I. Upper Trigonia- 6 Above Snowshill ; Farmcott 



grit. Wood; near Campden 



Hill Farm ; Bourton 

 Clump. 



V. Notgrove Free- 25 Above Snowshill ; Farmcott 



stone. Wood ; near Campden 



Hill Farm ; Snowshill — 

 road to Broadway Tower. 

 VI. Gryphite-grit ... 3f Sudeley Hill. 



VII. T. Buckmani-grit. lo" Sudeley Hill. 



VIII. Lower Trigonia- 7 to 10 Sudeley Hill ; Stan way 



grit. Hill. 



IX. Upper Snowshill 15 to 20 Stan way Hill ; Seven Wells. 



Clay. Generally in neighbour- 



hood of Broadway Tower. 



IX a, Tilestone About 15 Bourton Clump; near 



Hyates Pits ; Guiting 

 Hill. 

 1X6. Lower Snows- 5 Bourton Clump; Guiting 



hill Clay. Hill. 



X. Harford Sands. 10, or perhaps Near Snowshill; Bourton 



more. Clump ; Upton Wold ; 



Sudeley Hill. 

 XI. Upper Freestone. 



IV. Detailed Sections in the Noeth Cotteswolds. 



The following sections give the evidence upon which the gene- 

 ralized section has been founded. The first section is nearest to 

 Cleeve HiU, and has necessarily most affinity therewith. It is as 

 follows : — 



Section I. — Farmcott Wood and Sudeley Hill. 

 (From Winchcombe 1| miles east, by the side of the main road to 



Stow.) 



A. Farmcott Wood. 



Ft. Ft. 



Upper Trigonia- I. 1. Shelly limestones with earthy 



grit. partings : numerous Trigonice 



(moulds) and the characteristic 



brachiopoda 6 



Notgrove Free- V. 1. Whitish, very oolitic stone, with 



stone. a planed and bored surface. 



Level-bedded 6f 



2. The same, but very noticeably 



false-bedded shown 8 



Add about 10 feet for the difference 

 in ground-level between this ex- 

 posure and the next. Probably 

 some feet more should be added 



for the dip 10^ 



25 





