Environmental Engineering Reference
In-Depth Information
5
A variety of large-scale denudation chronologies and associated large-scale schemes for
slope evolution have been proposed over the years. These reflected slope evolution in
particular climate regimes and crude estimated rates of denudation. Modern research
focuses on more detailed slope models and a materials science approach. Denudation
rates, calculated from sediment yields and laboratory experiments, show that surface
lowering rates are ultimately attuned to tectonic cycles and rates of plate motion.
FURTHER READING
Ahnert, F. (1998)
Introduction to Geomorphology
, London: Arnold. A comprehensive review of
the scope of geomorphology, commencing with general concepts, processes and controls and
leading to the principal geomorphic systems. The text is easy to read, up-to-date with modern
interpretations in a Quaternary environmental context, and is complemented by a good
geographical range of suitable illustrations.
Duff, P. M. D., ed. (1993)
Holmes's 'Principles of Physical Geology'
, fourth edition, London:
Chapman & Hall. This volume of nearly 800 pages is a major reference text for any student of
the physical environment. Although it ranges over the entire geological environment, a large
portion deals generally and then specifically with the processes which denude and sculpture
Earth's surface. Well written and concise, the text is supported by copious illustrations.
Goudie, A. S. (1995)
The Changing Earth: rates of geomorphological processes
, Oxford:
Blackwell. This is an essential companion to standard texts on denudation and geomorphic
processes. It provides concise definitions and brief explanations of geomorphic processes before
addressing its main interest in the rates at which they operate and denude the continents.
Acknowledging that the data are incomplete and often experimental, the topic is nevertheless
comprehensive in its selection of case studies and illustrations.
Selby, M. J. (1993)
Hillslope Materials and Processes
, Oxford and New York: Oxford University
Press. This remains an outstanding text which commences with a review of rock and soil
properties and strength. It proceeds via weathering to geomorphic processes, focusing on slopes,
slope failure and mass wasting before concluding with hill slope models and denudation rates.
The topic is exceptionally well illustrated, with case studies, line drawings and photographs.
