link.springer.com

Weathering

Weathering may be defined as the disintegration or decomposition of rocks in situ. In contrast with metamorphic processes, weathering takes place within the range of temperatures found at and near the earth's surface. A rock undergoing weathering is not static; on the contrary, in certain weathering processes some minerals and elements are lost, others gained, and yet others redeposited at another level at the same site. There is considerable movement of material beneath the ground surface. But the main mass of the rock remains in situ and is not transported.

Many weathering processes are known in outline and in theory, but in many instances what actually takes place in nature is obscure. It is in any case rather unreal to define and explain most weathering processes in isolation, for several processes commonly combine to cause rock weathering, of which two general types are recognized. Physical (or mechanical) weathering involves rock disintegration, without any alteration of the...

References

  • Blackwelder, E., 1933, The insolation hypothesis of rock weathering, Am. J. Sci., 26, 97–113.

    Article  Google Scholar 

  • Chapman, R. W., Greenfield, M. A., 1949, Spheroidal weathering of igneous rocks, Am. J. Sci., 247, 407–429.

    Article  Google Scholar 

  • Goldich, S. S., 1938, A study of rock weathering, J. Geol., 46, 17–58.

    Article  Google Scholar 

  • Griggs, D. T., 1936, The factor of fatigue in rock exfoliation, J. Geol., 44, 783–796.

    Google Scholar 

  • Keller, W. D., 1955, Principles of Chemical Weathering, Columbia, Mo., Lucas Bros., 88pp.

    Google Scholar 

  • Linton, D. L., 1955, The problem of tors, Geograph. J., 121, 470–487.

    Google Scholar 

  • Merrill, G. P., 1921, Rocks, Rock-weathering and Soils, New York, London, Macmillan Co., 411pp.

    Google Scholar 

  • Ollier, C. D., 1963, Insolation weathering: examples from central Australia, Am. J. Sci., 261, 376–381.

    Article  Google Scholar 

  • Reiche, P., 1950, A Survey of Weathering Processes and Products, Revised ed., University of New Mexico Press, 95pp.

    Google Scholar 

  • Rougerie, G., 1959, Lateritisation et pédogénés inter-tropicales, L'inf. Géogr., 199–205.

    Google Scholar 

  • Trendall, A. F., 1962, The formation of ‘apparent peneplains’ by a process of combined lateritisation and surface wash, Zeit. Geomorphol., 6, (N.S.), 183–197.

    Google Scholar 

  • Wilhelmy, H., 1958, Der Klimamorphologie der Massengesteine, Braunschweig, G. Westerman, 238pp.

    Google Scholar 

  • Williams, J. E., 1949, Chemical weathering at low temperatures, Geograph. Rev., 39, 129–135.

    Article  Google Scholar 

Cross-references

Download references