. The Quarterly journal of the Geological Society of London. e visible at the eastern corner 10 0 18. Limestone 12 0 17. Green and red ash 5to7 0 16. Sandstone, with vertical cylindrical bodies 2 6 15. Fine ash 2 0 14. Lenticular limestone-band 0 3to6 13. Coarse ash, with highly-calcareous bands in thelowerpart, numerous laige fragments of lime-stone and some of grit in the upper part 11 6 12. Coarse ash 3 (i 11. Brown ash, very much decomposed and 1 2 10. Limestone 0 4 9. Ash as above (11), the upper part containing numerous lamellibranchs (Edmondia) 22 0 8. Beddish crinoidal limest
. The Quarterly journal of the Geological Society of London. e visible at the eastern corner 10 0 18. Limestone 12 0 17. Green and red ash 5to7 0 16. Sandstone, with vertical cylindrical bodies 2 6 15. Fine ash 2 0 14. Lenticular limestone-band 0 3to6 13. Coarse ash, with highly-calcareous bands in thelowerpart, numerous laige fragments of lime-stone and some of grit in the upper part 11 6 12. Coarse ash 3 (i 11. Brown ash, very much decomposed and 1 2 10. Limestone 0 4 9. Ash as above (11), the upper part containing numerous lamellibranchs (Edmondia) 22 0 8. Beddish crinoidal limestone 1 I) 7. Ash, as above 2 0 6. Argillaceous limestone 1 0 5. Ash, as above 3 6 4. Compact, somewhat argillaceous limestone 0 0 3. Ash, as above 11 0 2. Limestone, in bands 3to6 inches thick, with part-ings of red shale and, at about a foot fromthe top, one of green ashy material; the upper-most band of limestone is very 7 O1. Massive limestone, with much chert, to the base of the section about 90 6 [ 142 ] g -3 <»& C) CO • I—I. [ 143 ] iOS 2Q O © MS J*9 So be
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Keywords: ., bookcentury1800, bookdecade1840, booksubjectgeology, bookyear1845
