Hydrographic Analysis of the Goodwin Sands and the Brake Bank Author(s): R. L. Cloet Source: The Geographical Journal, Vol. 120, No. 2 (Jun., 1954), pp. 203-215 Published by: The Royal Geographical Society (with the Institute of British Geographers) Stable URL: https://www.jstor.org/stable/1791536 Accessed: 10-10-2019 09:26 UTC REFERENCES Linked references are available on JSTOR for this article: https://www.jstor.org/stable/1791536?seq=1&cid=pdf-reference#references_tab_contents You may need to log in to JSTOR to access the linked references. JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact
[email protected]. Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at https://about.jstor.org/terms The Royal Geographical Society (with the Institute of British Geographers) is collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 185.71.73.245 on Thu, 10 Oct 2019 09:26:35 UTC All use subject to https://about.jstor.org/terms HYDROGRAPHIC ANALYSIS OF THE GOODWIN SANDS AND THE BRAKE BANK R. L. CLOET ofThere the Goodwinmust be Sands.few mariners Together whowith arethe ignorantBrake Bank, of thethe Sands existence form anda the dangers distinct submarine morphological unit, much less complex than the banks in Figure i the Thames Estuary, or the series of sandbanks off the Franco-Belgian shore- line.1 Because of this relative simplicity we are in a position to analyse the movements in which the two banks are subject (see Fig.