Changes in drainage networks since 1820, Southern Tablelands, N.S.W.

作者: R. J. Eyles

DOI: 10.1080/00049187708702716

关键词:

摘要: Summary During the well‐documented period of exploration and initial settlement Southern Tablelands, many drainage lines contained chains ponds. Cultural influences, particularly ringbarking trees grazing sheep, cattle rabbits between 1840 1950, caused ponds to be destroyed by channel entrenchment. Changes since 1820 have followed sequence: chain ‘scour’ ponds, discontinuous gully, continuously incised channel, containing ‘fixed bar’ permanently flowing stream. Since improvements in farm management practices application soil conservation methods certain catchments further increased diversity fluvial forms. are illustrated evidence from early survey plans, aerial photographs fieldwork.

参考文章(6)
G. Pickup, Geomorphic effects of changes in river runoff, Cumberland Basin, N.S.W. Australian Geographer. ,vol. 13, pp. 188- 193 ,(1976) , 10.1080/00049187608702692
E. B. KRAUS, Recent Climatic Changes Nature. ,vol. 181, pp. 666- 668 ,(1958) , 10.1038/181666A0
R. J. Coventry, Abandoned shorelines and the late quaternary history of lake George, New South Wales Journal of the Geological Society of Australia. ,vol. 23, pp. 249- 273 ,(1976) , 10.1080/00167617608728939
K H Northcote, Atlas of Australian soils ,(1966)
L. J. Durham, Soil conservation in the Bredbo area J. Soil Conserv. N.S. W. ,vol. 17, pp. 57- 674 ,(1961)