Some unusual ripple marks in carboniferous limestone near spittal, north Northumberland
By: Shiells, K.A.G
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Material type: 
ArticleDescription: 498-502pp ; Illustration.Subject(s): Carboniferous limestone - North Northumberland - Great Britain | Bedding plane irregularities | Dynamic geology | Ripple marks - Carboniferous limestone
In:
Geological magazine : Vol. 100 Iss. 1-6 Year. 1963Summary: Abstract
Ripple marks of unusual dimensions are recorded from the Sandbanks Limestone (Middle Limestone Group) at a foreshore locality 3 miles south of Spittal in North Northumberland. The structures are thought to have been formed in a partially cohesive calcareous mudas wave-oscillation ripples which have undergone penecontemporaneous modification.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode |
|---|---|---|---|---|---|---|
Article
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Library and Information Centre Periodical Section | Bound Journal Collection | Not for loan | 002548_70 | ||
Serials/Scientific Journal
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Library and Information Centre Periodical Section | Bound Journal Collection | 550 GEO (Browse shelf) | Available | 002548 |
Abstract
Ripple marks of unusual dimensions are recorded from the Sandbanks Limestone (Middle Limestone Group) at a foreshore locality 3 miles south of Spittal in North Northumberland. The structures are thought to have been formed in a partially cohesive calcareous mudas wave-oscillation ripples which have undergone penecontemporaneous modification.
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