Camelia Slave – University of Agronomic Sciences and Veterinary Medicine of Bucharest, 59 Mărăști Blvd, Bucharest, Romania




3rd International Scientific Conference on Recent Advances in Information Technology, Tourism, Economics, Management and Agriculture – ITEMA 2019 – Bratislava, Slovakia, October 24, 2019, CONFERENCE PROCEEDINGS published by the Association of Economists and Managers of the Balkans, Belgrade; Printed by: SKRIPTA International, Belgrade, ISBN 978-86-80194-23-3, ISSN 2683-5991, DOI:




The Danube Delta is recognition as natural international capital in Romania. In 1991 it was
designated as Ramsar site and World Natural Heritage Site for a surface of 50% of its area. Also, in 1992
it is recognized as a Biosphere Reserve. The Danube Delta is a large protected area at international
level, but at national level certain areas of the Danube Delta are only natural reserves. The Danube
Delta is recognized as a Natural Biosphere Reserve by Government Decision 248/1994. In 1994, a GEF
(Global Environment Facility) project was set and Park Administration implements the management
plan. The Danube Delta has so far been the only protected area with its own administration. At national
level, will be provided support for the establishment and strengthening of the necessary institutional
framework, for the adoption of the laws on protected areas and strengthening legislative framework.
Also, for preparation human resource which is a public participation component of popularization the
idea of nature conservation and protected areas. The purpose of this article consisted of choosing Danube
Delta area where the possible floods occur due to different weather phenomenon. To do this using
ArcMap 10.5 programs were conducted a simulation map of flooding in the area under study.



Convention, Danube Delta, Habitat, Protected Area, Maps.


[1] Bukari S.M., Ahmad M. A., Wai T.L., Kaamin M., Alimin N., (2015) Spatial Analysis in
determination of flood prone areas using geographic information system and analytical
hierarchy process at process at Sungai Sembrongs catchment, – Soft Soil Engineering International
[2] Coteţ P., (1973) Geomorfologia României, Editura Tehnică, Bucureşti,
[3] Gâştescu P., Ştiucă R., (2008) Delta Dunări – Rezervație a biosferei, Editura Dobrogea
[4] Giosan L., Donnelly J.P., Constantinescu S., Filip F., Ovejanu I., Vespremeanu-Stroe A.,
Vespremeanu E., Duller G.A.T. (2006). Young Danube delta documents stable Black Sea
level since the middle Holocene: morphodynamic, paleogeographic, and archaeological
implications. Geology, 34(9): 757-760,
[5] Ionesi L., (1994) Geologia unităţilor de platformă şi a orogenului Nord-Dobrogean, Editura
Tehnică, Bucureşti,
[6] Mutihac V., (1990) Structura geologică a teritoriului României, Editura Tehnică, Bucureşti,
[7] Romanescu G., (1995) Delta Dunării – privire geografică, Editura Glasul Bucovinei, Iaşi,
[8] Rusu I., Niță L., (2004), Pedologie – Solurile României, Editura Eurobit, Timișoara,
[10] CIAT, site accessed in Sept, 2019



Association of Economists and Managers of the Balkans – UdEkoM Balkan
179 Ustanicka St, 11000 Belgrade, Republic of Serbia