Abstract
A large stream is a river and earth’s lifeblood. While flowing to the oceans, they drain about 68 % of the earth’s land surface; the remainder is either covered by ice or drains into closed basins. Areas draining to the sea are common in humid regions, whereas those draining to the interior closed basins occur in arid regions or in areas of active tectonic subsidence.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Hamblin WK, Christiansen CH (2008) Earth’s Dynamic Systems. Printice Hall, Upper Saddle River 767 p
Leopold LB, Wolman MG, Miller JP (1995) Fluvial Processes in Geomorphology. Dover Publications Inc., New York, USA (Reprinted)
Morisawa M (1985) Rivers. Longman Inc., New York 222 p
Robert A (2003) River processes: an introduction to fluvial dynamics. Hodder Arnold, London
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
Copyright information
© 2014 Springer India
About this chapter
Cite this chapter
Jain, S. (2014). Streams. In: Fundamentals of Physical Geology. Springer Geology. Springer, New Delhi. https://doi.org/10.1007/978-81-322-1539-4_8
Download citation
DOI: https://doi.org/10.1007/978-81-322-1539-4_8
Publisher Name: Springer, New Delhi
Print ISBN: 978-81-322-1538-7
Online ISBN: 978-81-322-1539-4
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)