Swash and swash mark
作者： K. O. Emery , J. F. Gale
关键词: Geology 、 Outcrop 、 Geomorphology 、 Water table 、 Swash
摘要: The time interval between swashes was found to be longer for gentle marine beaches than steep ones owing differing effectiveness of the as wave filters. This relationship offers a possible means determining angle beach slope from aerial reconnaissance. Swashes that cross outcrop water table leave swash marks are farther apart on ones. Three factors control this spacing interference beach, width exposed per unit tide fall, and permeability beach.
harvard.edu
agu.org参考文章(6)
William H. Twenhofel, Treatise on Sedimentation. The Journal of Physical Chemistry. ,vol. 37, pp. 261- 262 ,(1933) , 10.1021/J150344A017
M. B. ROSALSKY, A STUDY OF MINOR BEACH FEATURES AT FIRE ISLAND, LONG ISLAND, NEW YORK Annals of the New York Academy of Sciences. ,vol. 12, pp. 9- 16 ,(1949) , 10.1111/J.2164-0947.1949.TB01859.X
O. F. Evans, Floating sand in the formation of swash marks Journal of Sedimentary Research. ,vol. 8, pp. 71- 71 ,(1938) , 10.2110/JSR.8.71
F. P. Shepard, D. L. Inman, Nearshore water circulation related to bottom topography and wave refraction Transactions, American Geophysical Union. ,vol. 31, pp. 196- 212 ,(1950) , 10.1029/TR031I002P00196
K. O. Emery, Transportation of marine beach sand by flotation Journal of Sedimentary Research. ,vol. 15, pp. 84- 87 ,(1945) , 10.2110/JSR.15.84
W. H. Wunk, Surf beats Transactions, American Geophysical Union. ,vol. 30, pp. 849- None ,(None) , 10.1029/TR030I006P00849