Landslide inventory of northwestern Anatolia, Turkey

• Published in: Engineering geology 2005-02, Vol.77 (1), p.99-114
• Main Authors: Duman, Tamer Y., Çan, Tolga, Emre, Ömer, Keçer, Mustafa, Doğan, Ahmet, Ateş, Şerafettin, Durmaz, Serap
• Format: Article
• Language: English
• Subjects: Applied sciences; Buildings. Public works; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Exact sciences and technology; Geotechnics; Landslide; Landslide inventory mapping; Natural hazards: prediction, damages, etc; Soil mechanics. Rocks mechanics; Turkey; Zonguldak
• ISSN: 0013-7952; 1872-6917
• DOI: 10.1016/j.enggeo.2004.08.005

Turkey is heavily exposed to natural hazards such as earthquakes, landslides and floods. The total loss caused by landslides in terms of affected buildings, in a period of 35 years between 1959 and 1994, constitutes 27% of the entire loss from all natural hazards and is second after earthquakes. There are no other available data on either direct or indirect losses due to landslides on a national scale. The General Directorate of Mineral Research and Exploration (MTA) started the ‘Turkish Landslide Inventory Mapping Project’ in 1997 to improve understanding of regional and national landslide processes. The purpose of the project is to establish landslide inventory maps at medium (1:25,000), regional (1:100,000) and national (1:500,000) scales. Existing landslides are mapped on 1:25,000 scale topographic base maps by interpretation of aerial photographs and field investigations. The base maps are then digitized and stored in a geographic information system (GIS) database by the Geological Research Department of MTA. Hence, regional- and national-scale landslide maps will be available as well, as the work progresses. Landslides are classified as fall, topple, slide and flow and are broadly characterized as active or inactive. The landslides are also classified according to their relative depths, as shallow (depth5 m). The present paper will attempt to describe the project standards and its application to the area of 1:500,000 scale Zonguldak quadrangle. The study area extends to 39,081 km 2, and 7.1% of the area was found to be affected by landslides. A total 10,007 landslides (392 shallow-seated, 8020 deep-seated active and 1595 deep-seated inactive) were mapped in the area covering 2768 km 2. Cretaceous flysch, Paleocene–Eocene flysch and Paleocene–Middle Miocene volcanics are the most landslide-prone units and constitute 27.8%, 29.9% and 7.2% of the all landslides, respectively.