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Geology of Yorkshire
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Details
In Yorkshire there is a very close relationship between the major topographical areas and the geological period in which they were formed. The Pennine chain of Hills in the west is of Carboniferous origin. The central vale is Permo-Triassic. The North York Moors in the north-east of the county are Jurassic in age while the Yorkshire Wolds to the south east are Cretaceous chalk uplands. The plain of Holderness and the Humberhead levels both owe their present form to the Quaternary ice ages. The strata become gradually younger from west to east. Much of Yorkshire presents heavily glaciated scenery as few places escaped the great ice sheets as they advanced during the last ice age.
Weitere Informationen
- Allgemeine Informationen
- GTIN 09786130293642
- Editor Frederic P. Miller, Agnes F. Vandome, John McBrewster
- Sprache Englisch
- Genre Geowissenschaften
- Anzahl Seiten 112
- Größe H220mm x B150mm x T7mm
- Jahr 2010
- EAN 9786130293642
- Format Fachbuch
- ISBN 978-613-0-29364-2
- Titel Geology of Yorkshire
- Untertitel Yorkshire, North York Moors, Yorkshire Wolds, Holderness, South Yorkshire Coalfield, Paleozoic, Lake District, Carboniferous, Dike (geology), Yorkshire Dales, Vale of Pickering, Humberhead Levels
- Gewicht 183g
- Herausgeber Alphascript Publishing
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