Hostname: page-component-84b7d79bbc-2l2gl Total loading time: 0 Render date: 2024-07-28T10:02:16.977Z Has data issue: false hasContentIssue false
  • English
  • Français

Storm Waves and Shore-forms of South-Western Scotland

Published online by Cambridge University Press:  01 May 2009

S. Ting
S. Ting
Affiliation:
Glasgow University.
Get access Rights & Permissions [Opens in a new window]

Extract

The effect of waves on a shore depends largely on the angle of approach, for the energy of the advancing waves tends to erode the headlands and drift the products of erosion into the bays. Wave refraction applies to waves approaching the shore in any direction, but is only ideally developed in ordinary weather conditions or by approaching waves caused by distant storms. Locally developed storm waves usually approach the shore at an oblique angle to its general trend, owing to the failure of wave refraction and are the most effective where locally they meet the shore at right angles. Beach drifting will be in operation along the section of the shore which happens to be at an angle oblique to the direction of the approaching waves.

Type
Original Articles
Information
Geological Magazine , Volume 74 , Issue 3 , March 1937 , pp. 132 - 141
Copyright
Copyright © Cambridge University Press 1937

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

page 132 note 1 Johnson, D. W., Shore Processes and Shoreline Development, 1919, 74.Google Scholar

page 133 note 1 Shore Processes and Shoreline Development, p. 66.Google Scholar

page 133 note 2 Ting, S., “Beach Ridges of S.W. Jura.,” Scot. Geogr. Mag., 52, 1936, 182–7.Google Scholar

page 134 note 1 “The Geology of Jura, Knapdale, and N. Kintyre,” Mem. Geol. Sun. Scotland, 1911, 127.Google Scholar

page 135 note 1 Geikie, A., Text-book of Otology, 3rd ed., Macmillan, 1893.Google Scholar

page 135 note 2 “The Geology of the Orkneys,” Mem. Geol. Surv. Scotland, 1934, 10.Google Scholar

page 137 note 1 The term “outlet” is equivalent to the term “inlet”. The former term is used with reference to rivers draining into the sea through an opening in an off-shore form, while the latter is preferred in cases when the tidal currents or waves are considered.

page 139 note 1 Chambers, Gazetteer of Scotland, 1832, map.Google Scholar

page 139 note 2 Groome, Ordnance Gazetteer of Scotland, 1884, map.Google Scholar

page 139 note 3 Gulliver, F. P., “Shoreline Topography,” Proc. Acad. Art. and Sci., 34, 1898–9, pp. 208–209, 227, 232, figs. 21, 31.Google Scholar