Map sheet search for E009

Map sheet search for E009

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1 Rothbury (B&Sup) [Folded Map]

Format Folded Map ISBN 9780751835809
Scale 1:50 000 Sheet(s) Covered E009
Version B&Sup Year Published 2009


2 Rothbury (B&Sup) [Flat Map]

Format Flat Map ISBN 9780751835793
Scale 1:50 000 Sheet(s) Covered E009
Version B&Sup Year Published 2009


3 Rothbury (S) [Flat Map]

This is a 1966 reprint of 1934 map [Flat Map]

Format Flat Map ISBN 9780751836677
Scale 1:50 000 Sheet(s) Covered E009
Version S&D Year Published 1934


4 Rothbury (S) [Folded Map]

This is a 1966 reprint of 1934 map [Folded Map]

Format Folded Map ISBN 9780751836660
Scale 1:63 360 Sheet(s) Covered E009
Version S&D Year Published 1934


5 Rothbury district - Sheet Explanation for sheet E009 [Booklet]

Sheet Explanations provide a brief description and interpretation of the geology of the relevant BGS 1:50 000 scale map sheet area. More detailed geological information for the same area is available via the Sheet Descriptions. Sheet Explanations are printed A5 booklets and are available either singly, or as a pack together with the relevant 1:50 000 scale map, where this map is available. Carboniferous rocks, deposited between about 350 and 310 million years ago, underlie the entire district. Most of the area is covered by a varying thickness of superficial deposits, and only in the northwest does the form of the ground bear any clear relation to the underlying bedrock structure. The Carboniferous succession, nearly 3000 m thick, was deposited in the Northumberland–Solway Basin. The Carboniferous sedimentary rocks represent the gradual infilling of the fault-controlled trough. Deposition in lagoonal coastal-flat environments in the early Carboniferous was followed by fluvial deposition and by the deposition of rhythmic units of limestone, mudstone, sandstone and coal on low-lying deltaic swamps with repeated shallow marine incursions. Extensional movements during early Permian times led to the emplacement of the Whin Dolerite Sill-swarm and of associated dykes of the Northern England Tholeiitic Dyke-swarm. A few basaltic dykes were intruded during the early Palaeogene. Superficial deposits of Quaternary age were deposited during the last, Devensian, glaciation. Postglacial and recent deposits include, alluvium, river terrace deposits and peat inland, with blown sand, tidal river, salt-marsh and marine deposits on the coast. [Booklet]

Author Lawrence, DJD et al Collation 210 x 145 mm; 36 pages
Format Booklet ISBN 9780852726938
Sheet(s) Covered E009 Year Published 2011


6 Rothbury district map pack - Sheet Explanation for sheet E009 plus 1:50 000 (B&Sup) map [Booklet and Map Pack]

This pack contains a Sheet Explanation for the district and the complementary 1:50 000 scale Bedrock Geology and Superficial Deposits map (folded). Sheet Explanations provide a brief description and interpretation of the geology of the relevant map sheet area. The A5 Sheet Explanation booklet and the map are supplied in a transparent wallet. While it is possible to buy the map and Sheet Explanation separately, buying them together as map pack saves you £3. Carboniferous rocks, deposited between about 350 and 310 million years ago, underlie the entire district. Most of the area is covered by a varying thickness of superficial deposits, and only in the northwest does the form of the ground bear any clear relation to the underlying bedrock structure. The Carboniferous succession, nearly 3000 m thick, was deposited in the Northumberland–Solway Basin. The Carboniferous sedimentary rocks represent the gradual infilling of the fault-controlled trough. Deposition in lagoonal coastal-flat environments in the early Carboniferous was followed by fluvial deposition and by the deposition of rhythmic units of limestone, mudstone, sandstone and coal on low-lying deltaic swamps with repeated shallow marine incursions. Extensional movements during early Permian times led to the emplacement of the Whin Dolerite Sill-swarm and of associated dykes of the Northern England Tholeiitic Dyke-swarm. A few basaltic dykes were intruded during the early Palaeogene. Superficial deposits of Quaternary age were deposited during the last, Devensian, glaciation. Postglacial and recent deposits include, alluvium, river terrace deposits and peat inland, with blown sand, tidal river, salt-marsh and marine deposits on the coast. [Booklet and Map Pack]

Author Lawrence, DJD Format Booklet and Map Pack
ISBN 9786000008277 Sheet(s) Covered E009
Year Published 2011  



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