Hostname: page-component-848d4c4894-wg55d Total loading time: 0 Render date: 2024-06-09T14:49:48.941Z Has data issue: false hasContentIssue false
  • English
  • Français

Wave Action in Shore Platform Formation

Published online by Cambridge University Press:  01 May 2009

A. B. Edwards
Get access Rights & Permissions [Opens in a new window]

Abstract

Erosion of headlands along the southern coast of Victoria results chiefly from the attack of storm waves, and is concentrated above a defined level, marked by certain level shore platforms, whose surfaces are at about high tide level. These platforms are initiated and maintained by storm wave erosion. Their surfaces undergo planation and lowering, chiefly by the scouring action of waves of translation, but increasingly by water-layer weathering as the platforms age and widen.

Type
Articles
Information
Geological Magazine , Volume 88 , Issue 1 , February 1951 , pp. 41 - 49
Copyright
Copyright © Cambridge University Press 1951

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

1 Bartrum, J. A., 1935. Shore Platforms. Rept. Aust. and N.Z. Assoc. Adv. Sci., xxii, 135–143.Google Scholar
2 Edwards, A. B., 1941. Storm-Wave Platforms. Journ. Geomorph., iv, 223–236.Google Scholar
3 Edwards, A. B. 1942. The San Remo Peninsula. Proc. Roy. Soc. Vict., liv, 59–74.Google Scholar
4 Edwards, A. B. 1945. The Geology of Phillip Island. Proc. Roy. Soc. Vict., lvii, 1–16.Google Scholar
5 Hills, E. S., 1949. Shore Platforms. Geol. Mag., lxxxvi, 137–152.CrossRefGoogle Scholar
6 Jutson, J. T., 1949. The Shore Platforms of Lorne, Victoria. Proc. Roy. Soc. Vict., lxi, 43–59.Google Scholar
7 Wentworth, C. K., 1938. Marine Bench-Forming Processes: Water Level Weathering. Journ. Geomorph., i, 6–32.Google Scholar