Access the full text.
Sign up today, get DeepDyve free for 14 days.
References for this paper are not available at this time. We will be adding them shortly, thank you for your patience.
PART IV. THE TURKISH STRAITS CHAPTER I. GENERAL OBSERVATIONS ON THE STRAITS " Section I. Topography and Description of the Straits. Whereas the term "the Turkish Straits" legally includes also the Sea of Marmara, which divides the S,traits from the point of view of legal status; in the geographical sense it includes only the Dardanelles, i. e. the waterway between the Aegean Sea (Turkish: the White Sea) and the Sea of Marmara and the Bosphorus., the straits between the latter and the Black Sea(i). By origin the Turkish Straits belong to the so-called "Einbruch- . strassen"(2). The violent volcanic eruptions which led to that lowering of the bottom of the Mediterranean basin which caused the pressure of the western ocean to break through the isthmus . uniting Europe and Africa where the Straits of Gibraltar now are, cf. ante Part II, Section 43, are believed to have brought about a similar development at the eastern extremity of the Mediterranean, where first the Black S,ea penetrated the isthmus between that sea and the Sea of Marmara, and the latter then the isthmus between it and the Aegean Sea( 3 ) . (1) For the topography, navigation conditions etc. of
Nordisk Tidsskrift for International Ret – Brill
Published: Jan 1, 1943
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.