Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-15T02:02:19.508Z Has data issue: false hasContentIssue false

The Upper Carboniferous Rocks of the Stainmore Coalfield

Published online by Cambridge University Press:  01 May 2009

T. D. Ford
Affiliation:
Geology Department, University College, Leicester.

Abstract

The sequence of Upper Carboniferous rocks in the outlier at the western end of Stainmore Pass is described. The Upper Yoredale Series is shown to be separated by an unconformity from the overlying “Millstone Grit” series. The Coal Measures are about 800 feet thick and appear to be unconformable on the “Millstone Grit”. Hitherto unrecorded non-marine faunas and floras indicate horizons near the base and at the top of the Modiolaris zone. The sequence of Upper Carboniferous rocks at Stainmore is briefly compared with those of surrounding coalfields.

Type
Articles
Copyright
Copyright © Cambridge University Press 1955

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

Carruthers, R. G., 1938. Alston Moor to Botany and Tan Hill. Proc. Yorks. Geol. Soc., xxiii, 236253.Google Scholar
Chubb, J., and Hudson, R. G. S., 1925. An unconformity in N.W. Yorkshire, Proc. Yorks. Geol. Soc., xx, 257291.CrossRefGoogle Scholar
Dix, E., 1934. The Sequence of Floras in the Upper Carboniferous. Trans. Roy. Soc. Edinb., lvii, 789838.CrossRefGoogle Scholar
Eastwood, T., 1953. British Regional Geology: Northern England, 3rd Edn.Google Scholar
Ford, T. D., 1954. The Upper Carboniferous Rocks of the Ingleton Coalfield. Quart. Journ. Geol. Soc., cx, 231266.CrossRefGoogle Scholar
Goodchild, J. G., 1890. Former Extent of Coal Measures in N.W. England. Trans. Westmorland Nat. Hist. Assn., No. 7.Google Scholar
Hudson, R. G. S., 1941. The Mirk Fell Beds of Tan Hill. Proc. Yorks. Geol. Soc., xxiv, 259289.Google Scholar
Trotter, F., 1952. Sedimentation Facies in the Namurian of N.W. England. Liverpool & Manchester Geol. Journ., i, 77112.Google Scholar
Trotter, F., 1954. The Cumberland Coalfield, in The Coalfields of Great Britain by A. E. Trueman, 314324.Google Scholar
Trueman, A. E., and Weir, J., 19461955. British Carboniferous Non-Marine Lamellibranchs. Palaeont Soc., London.Google Scholar
Turner, J. S., 1935. The Structural Geology of Stainmore. Proc. Geol. Assoc., xlvi, 121151.CrossRefGoogle Scholar