An evaluation of climate, crustal movement and base level controls on the Middle-Late Pleistocene development of the River Severn, U.K.

@article{Maddy2002AnEO,
  title={An evaluation of climate, crustal movement and base level controls on the Middle-Late Pleistocene development of the River Severn, U.K.},
  author={D. Maddy},
  journal={Netherlands Journal of Geosciences - Geologie en Mijnbouw},
  year={2002},
  volume={81},
  pages={329 - 338}
}
  • D. Maddy
  • Published 1 December 2002
  • Geography, Geology, Environmental Science
  • Netherlands Journal of Geosciences - Geologie en Mijnbouw
Abstract The Pleistocene development of the lower Severn valley is recorded in the fluvial sediments of the Mathon and Severn Valley Formations and their relationship to the glacigenic Wolston (Oxygen Isotope Stage 12), Ridgacre (OIS 6) and Stockport (OIS 2) Formations. The most complete stratigraphical record is that of the Severn Valley Formation, which post-dates the Anglian Wolston Formation and comprises a flight of river terraces, the highest of which is c.50 m above the present river… 
The origin and dynamics of Wakkerstroom Vlei, Mpumalanga Province, South Africa.
The formation and common occurrence of riparian wetlands within the semi-arid Highveld interior of South Africa, a landscape setting undergoing extensive long-term fluvial incision, is an enigma and
Quaternary vertical crustal motion and drainage evolution in East Anglia and adjoining parts of southern England: chronology of the Ingham River terrace deposits
Prior to its disruption during the Anglian glaciation (MIS 12), the Ingham or Bytham River used to flow eastwards across central England and East Anglia into the southern North Sea. It thus had a
Plio‐Pleistocene fault reactivation within the Crag Basin, eastern UK: implications for structural controls of landscape development within an intraplate setting
This study examines the long‐term neotectonic evolution of the Crag Basin of eastern England during the Plio‐Pleistocene (c. 4.0–0.48 Ma) and the influence of neotectonics on coastal and drainage
Speleothem U-series constraints on scarp retreat rates and landscape evolution: an example from the Severn valley and Cotswold Hills gull-caves, UK
Modelling landscape evolution requires quantitative estimates of erosional processes. Dating erosional landscape features such as escarpments is usually difficult because of the lack of datable
...
...

References

SHOWING 1-10 OF 89 REFERENCES
The Somme valley terrace system (northern France); a model of river response to Quaternary climatic variations since 800,000 bp
Recent research on the Somme Valley terrace deposits, that began in 1987, has resulted in an integrated sequence of geological and geomorphological evidence for this area that is of particular
Thames River sediments of the British Early and Middle Pleistocene
Fluvial sequences of the Maas : a 10 Ma record of neotectonics and climatic change at various time-scales
Around 10 million years ago, the interplay of tectonics, climate and sea level changed markedly in the southern North Sea Basin. One of the results was the start of rapid progradation of the
Lithospheric flexure, uplift, and landscape evolution in south-central England
The high level river gravels in Oxfordshire (the Northern Drift Group), which range in age from Early Pleistocene to around 450 ka, contain pebbles that were derived from a source area to the north
...
...