Military geography: The influence of terrain in the outcome of the Gallipoli Campaign, 1915

Authors: Doyle, P. and Bennett, M.R.

Journal: Geographical Journal

Volume: 165

Issue: 1

Pages: 12-36

ISSN: 0016-7398

DOI: 10.2307/3060508

Abstract:

The Gallipoli Campaign of 1915 was one of the most strategically significant theatres during the Great War of 1914-1918. The land campaign followed the failure of the naval expedition which was intended to force the Dardanelles by sea power alone, silencing the Turkish forts on the narrows and forcing entry to the Sea of Marmara and ultimately to Constantinople (Istanbul). This paper examines the impact of terrain on the outcome of the land campaign. A land system analysis of the Gallipoli Peninsula was carried out, and five land systems, based on aspects of geology, geomorphology, hydrogeology and vegetation, were identified. The landings of 25 April 1915 were made at Cape Helles and Anzac Cove, with objectives to capture the high ground. The land system analysis demonstrates that these landing places were disadvantaged by terrain, with steep, deeply-incised slopes, narrow beaches and inadequate water supplies. A later landing at Suvla Bay in August 1915 had more terrain advantages, with wide landing beaches and locally available water supplies, but the tactical advantages of a lightly held terrain were not exploited. Overall, the Gallipoli Campaign failed primarily because of: inadequate planning and leadership by the Allied forces; poor communications; the efficiency of the Turkish armies in the siting of defensive positions according to terrain; the lack of detailed information with regard to terrain and geology available to the British and ANZAC troops; and a paucity of locally-derived groundwater supplies.

Source: Scopus

Preferred by: Matthew Bennett

Military Geography: the influence of terrain in the outcome of the Gallipoli Campaign, 1915

Authors: Doyle, P. and Bennett, M.R.

Journal: GEOGRAPHICAL JOURNAL

Volume: 165

Pages: 12-36

ISSN: 0016-7398

DOI: 10.2307/3060508

Source: Web of Science (Lite)