Hostname: page-component-78c5997874-94fs2 Total loading time: 0 Render date: 2024-11-19T11:36:22.058Z Has data issue: false hasContentIssue false

The Middle Grits of Derbyshire

Published online by Cambridge University Press:  01 May 2009

Extract

The River Amber on its way from the Erewash Valley Coalfield to its junction with the Derwent near Ambergate crosses the upturned edges of the Millstone Grit Series. Near the point where the river enters the grit belt at Bullbridge a boring for water was put down in the grounds of the Amber Dye Works during the latter half of the year 1936. My thanks are due to the directors of Stevensons (Dyers), Limited, for giving me every facility for examining the core, and to Mr. S. G. Clift for assisting me in the examination and in collecting. My thanks are also due to Dr. C. J. Stubblefield for valuable criticisms and suggestions during the writing up of this note.

Type
Articles
Copyright
Copyright © Cambridge University Press 1946

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

(1) Bisat, W. S. 1928. The Carboniferous Goniatites of England and their Continental equivalents. Congr. de Strat. Carb. Heerlen, 1927, p. 117.Google Scholar
(2) Davies, W. 1941. On a boring in the Millstone Grit Series at Hallam Head, Sheffield. Proc. Yorks. Geol. Soc., xxiv, pt. iv, 242.Google Scholar
(3) Gibson, W., and others. 1908. The Geology of the Southern part of the Derbyshire and Nottinghamshire Coalfield. Mem. Geol. Surv.Google Scholar
(4) Gibson, W., and others 1913. The Geology of the Northern part of the Derbyshire Coalfield. Mem. Geol. Surv.Google Scholar
(5) Trueman, A. E., and Deans, T. 19321933. A new Lamellibranch Fauna from the Millstone Grit of Bingley, Yorkshire. Trans. Leeds Geol. Assoc., v, 1.Google Scholar
(6) Wray, D. A. 1929. The Carboniferous Succession in the Central Pennine Area. Proc. Yorks. Geol. Soc., xxi, 228.CrossRefGoogle Scholar
(7) Wray, D. A. and Trueman, A. E. 1931. The Non-marine Lamellibranchs of the Upper Carboniferous of Yorkshire and their Zonal sequence. Summary of Progr. Geol. Surv. for 1930, pt. iii, 70.Google Scholar
(8) Wright, W. B., and others. 1927. The Geology of the Rossendale Anticline. Mem. Geol. Surv.Google Scholar