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pro vyhledávání: '"Gallois, R.W."'
Autor:
Gallois, R.W., Goldring, R.
Publikováno v:
In Proceedings of the Geologists¿ Association 2007 118(3):265-275
Autor:
Gallois, R.W.
The type sections of the Kimmeridge Clay Formation and the upper part of the Kimmeridgian Stage are cliff and foreshore exposures close to the village of Kimmeridge, Dorset. The succession is made up of rhythmic alternations of mudstone, organicrich
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Autor:
Gallois, R.W.
Multidisciplinary studies carried out in advance of site investigations of the areas at Lyme Regis, Dorset most threatened by a combination of landslides and marine erosion included sidescan-sonar, bathymetric and seismic-reflection surveys in the ad
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Autor:
Gallois, R.W.
Like many small coastal towns in the UK, Sidmouth in Devon was founded on the valley sides adjacent to a river outfall that provided a natural harbour. Subsequent expansion of the town in the late 18th and early 19th centuries, when living by or visi
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Autor:
Gallois, R.W.
The Axmouth to Lyme Regis Undercliffs National Nature Reserve in east Devon includes the most famous mass-movement feature in Britain, the Bindon Landslide of Christmas Day 1839. Tens of millions of tonnes of rock, older landslide debris and beach de
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Autor:
Gallois, R.W.
The unglaciated part of southern England was subject to periglacial climates that lasted for more than 20 ka on at least eight occasions during the last 750 ka. There are large outcrops of Jurassic mudstones in south-west England, principally the Lia
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Autor:
Gallois, R.W.
A proposed gas-storage site at the former Upper Osprey Ministry of Defence site on the north east coast of the Isle of Portland is underlain by landslide debris and man-made deposits that wholly conceal an outcrop of Kimmeridge Clay Formation. Histor
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Autor:
Gallois, R.W., Etches, S.M.
Species of the ammonite Gravesia (Salfeld, 1913) have a widespread distribution in Europe over a relatively narrow stratigraphical range in the late Kimmeridgian and early Tithonian stages. The genus is a warm-water form that reaches its maximum stra
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Autor:
Gallois, R.W.
The Black Ven-Spittles landslide is an old, probably Pleistocene, complex of interacting coastal landslides that are in the process of being reactivated as a result of a combination of man-made works and marine erosion. The upper part of the complex
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