Hostname: page-component-78c5997874-xbtfd Total loading time: 0 Render date: 2024-11-02T23:14:38.169Z Has data issue: false hasContentIssue false

The Yorkshire Dogger

Published online by Cambridge University Press:  01 May 2009

Extract

In parts of Rosedale and Farndale the Serpula Beds are exactly as in Fryup and Danby; they consist of very fine-grained sandstones or silts, blue, grey, green, yellow, or brown in colour, according to the degree of oxidation, and always full of worm tubes. In many specimens it is clear that practically the whole of the material has been passed through the bodies of worms, leading to a very confused structure. The worm tubes may be several inches long: they are only occasionally vertical or straight, but usually arranged in an irregular manner. Fossils, usually broken and badly preserved, are sporadic, but deter-minable ammonites of the striatulum and dispansum zones have been recorded in different parts of the area (Macmillan, 1932, and this paper).

Type
Articles
Copyright
Copyright © Cambridge University Press 1949

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

Anderson, W., 1942. Jurassic Iron Ores, Cleveland District Wartime Pamphlet No. 23, Geol. Surv. of Great Britain.Google Scholar
Black, M., 1934. Sedimentation of the Aalenian Rocks of Yorkshire. Proc. Yorks. Geol. Sec., xxii, 265.CrossRefGoogle Scholar
Fairbridge, H. W., 1946. Submarine Slumping and the location of oil bodies. Bull. Am. Assoc. Petrol. Geol., 30, 34.Google Scholar
Fox-Strangways, C., and Barrow, G., 1915. The Geology of the Country between Whitby and Scarborough, 2nd Edition. Mem. Geol. Surv., 35 and 44.Google Scholar
Fox-Strangways, C., Reid, C, and Barrow, G., 1885. The Geology of Eskdale, Rosedale, etc. Mem. Geol. Surv., 96.Google Scholar
Hallimond, A. F., 1925. Iron Ores: Bedded Ores of England and Wales. Mem. Geol. Surv. Special Reports on Mineral Resources of Great Britain, xxix.Google Scholar
Hemingway, J. E., 1949. A Revised Terminology and Subdivision of the Middle Jurassic Rocks of Yorkshire. Geol. Mag., lxxxvi, 67.CrossRefGoogle Scholar
Lamplugh, G. W., Wedd, C. B., and Pringle, J., 1920. Iron Ores (contd.).- Bedded Ores of the Lias, Oolites, and Later Formations in England. Mem. Geol. Surv. Special Reports on the Mineral Resources of Great Britain, xii.Google Scholar
MacMillan, W. E. F., 1932. Notes on Dogger Horizons in North-East Yorkshire. Proc. Yorks. Geol. Soc., xxii, 122.CrossRefGoogle Scholar
Marley, J., 1870. Magnetic Ironstone of Rosedale Abbey. Trans. N.E. Inst. M. and M. Eng., xix, 193.Google Scholar
Pettijohn, F. J., 1949. Sedimentary Rocks, 77. New York.Google Scholar
Rastall, R. H., 1905. The Blea Wyke Beds and the Dogger in North-East Yorkshire. Quart. Journ. Geol. Soc., lxi, 441.CrossRefGoogle Scholar
Rastall, R. H., 1939. On Rutile in the Dogger. Geol. Mag., lxxvi, 109.CrossRefGoogle Scholar
Rastall, R. H., and Hemingway, J. E., 1939. Black Oolites in the Dogger of North-East Yorkshire, Geol. Mag., lxxvi, 225.CrossRefGoogle Scholar
Rastall, R. H., and Hemingway, J. E., 1940. The Yorkshire Dogger. I.—The Coastal Region. Geol. Mag., lxxvi, 177197 and 257275.CrossRefGoogle Scholar
Rastall, R. H., and Hemingway, J. E., 1941. The Yorkshire Dogger. II.—Lower Eskdale. Geol. Mag., lxxviii, 351.CrossRefGoogle Scholar
Rastall, R. H., and Hemingway, J. E., 1943. The Yorkshire Dogger. III.—Upper Eskdale. Geol. Mag., lxxx, 209230.CrossRefGoogle Scholar