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Hull, E. (1862) On Iso-diametric Lines, as means of representing the Distribution of Sedimentary Clay and Sandy Strata, as distinguished from Calcareous Strata, with special reference to the Carboniferous Rocks of Britain. Journal of the Geological Society, 18 (1) 127-146 doi:10.1144/gsl.jgs.1862.018.01-02.27

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Reference TypeJournal (article/letter/editorial)
TitleOn Iso-diametric Lines, as means of representing the Distribution of Sedimentary Clay and Sandy Strata, as distinguished from Calcareous Strata, with special reference to the Carboniferous Rocks of Britain
JournalJournal of the Geological Society
AuthorsHull, E.Author
Year1862 (February 1)Volume18
Issue1
PublisherGeological Society of London
DOIdoi:10.1144/gsl.jgs.1862.018.01-02.27
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Mindat Ref. ID310034Long-form Identifiermindat:1:5:310034:3
GUID0
Full ReferenceHull, E. (1862) On Iso-diametric Lines, as means of representing the Distribution of Sedimentary Clay and Sandy Strata, as distinguished from Calcareous Strata, with special reference to the Carboniferous Rocks of Britain. Journal of the Geological Society, 18 (1) 127-146 doi:10.1144/gsl.jgs.1862.018.01-02.27
Plain TextHull, E. (1862) On Iso-diametric Lines, as means of representing the Distribution of Sedimentary Clay and Sandy Strata, as distinguished from Calcareous Strata, with special reference to the Carboniferous Rocks of Britain. Journal of the Geological Society, 18 (1) 127-146 doi:10.1144/gsl.jgs.1862.018.01-02.27
In(1862, February) Journal of the Geological Society Vol. 18 (1) Geological Society of London

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Hull, E. (1868) III. On the Causes which seem to have Regulated the Relative Distribution of the Calcareous and Sedimentary Strata of Great Britain, with Special Reference to the Carboniferous Formation. Transactions of the Geological Society of Glasgow, 3 (1) 33-44 doi:10.1144/transglas.3.1.33
Huxley, T. H. (1862) On a Stalk-eyed Crustacean from the Carboniferous Strata near Paisley. Journal of the Geological Society, 18 (1) 420-422 doi:10.1144/gsl.jgs.1862.018.01-02.55
Hull, Edward (1861) On Isometric Lines, and the Relative Distribution of the Calcareous and Sedimentary Strata of the Carboniferous Rocks of Britain. The Geologist, 4 (10) 454-455 doi:10.1017/s1359465600004068
Hull, E. (1868) On the Thickness of the Carboniferous Rocks of the Pendle Range of Hills, Lancashire, as illustrating the Author's views regarding the "South-easterly Attenuation of the Carboniferous Sedimentary Strata of the North of England". Journal of the Geological Society, 24 (1) 319-323 doi:10.1144/gsl.jgs.1868.024.01-02.41
Harkness, R. (1862) On the Position of the Pteraspis Beds, and on the Sequence of the Strata of the Old Red Sandstone Series of South Perthshire. Journal of the Geological Society, 18 (1) 253-258 doi:10.1144/gsl.jgs.1862.018.01-02.38
Jamieson, T. F. (1862) On the Ice-worn Rocks of Scotland. Journal of the Geological Society, 18 (1) 164-184 doi:10.1144/gsl.jgs.1862.018.01-02.30
Everest, R. (1862) On the Lines of Deepest Water around the British Isles. Journal of the Geological Society, 18 (1) 37-42 doi:10.1144/gsl.jgs.1862.018.01-02.16
(1862) Donations to the Library of the Geological Society. Journal of the Geological Society, 18 (1) 43-477 doi:10.1144/gsl.jgs.1862.018.01-02.17
(1862) Part II. Miscellaneous. Journal of the Geological Society, 18 (1) doi:10.1144/gsl.jgs.1862.018.01-02.64
(1862) Errata et Corrigenda. Journal of the Geological Society, 18 (1) doi:10.1144/gsl.jgs.1862.018.01-02.01
(1862) Annual General Meeting, Feb. 21, 1862. Journal of the Geological Society, 18 (1) doi:10.1144/gsl.jgs.1862.018.01-02.02
 
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