Detailed Presentation
The Danube Delta began to be formed in Quaternary, in the icy era consisting of two distinct periods:
the continental period - produced by the marine regression, when the shore was very much withdrawn and the arms of the Danube launched visible canyons in what it is now the continental platform
the gulf period - that followed a transgression. The hypothesis about the coast issued by Grigore Antipa and confirmed by P. Zencovici, admits the presence of a gulf, isolated by the marine currents through transversal narrow reefs and which finally formed the bank.
The Danube clogged this surface in the conditions of a reduced tide of about 70 cm. The continuous clogging shaped the present aspect of the delta. "The place where a new land is being created". When the Danube Delta is seen from Tulcea Hills, it looks like a green surface crossed by silver stripes.
The Danube Delta is a plain, which is continuously being formed, it has an average altitude of 50 cm and it is made up of:
positive relief (narrow reefs, islands, drift woods)
negative relief (the Danube arms, channels, brooks, swamps, marshes and lakes).
The land of the delta represents 13% of its surface and it is made up of:
river narrow reefs that accompany the Danube arms and are oriented towards West-East with an altitude of 0.5-5 m.
marine narrow reefs oriented towards North-South; Letea is remarkable for its altitude of 124 m, the maximum altitude for the delta and also Caraorman, Dranov, Ivancea, Saraturile, etc.
continental narrow reefs that represent residuum from the land before the delta was formed: Chilia and Stipoc.
The quantity of alluvial deposits brought by the Danube every year, to which are added the residuum of the dead organisms, the eolian dust etc. will make the percent of land increase to the detriment of the negative relief.


birds of Danube Delta
The symbol of Danube Delta.
Tulcea
Beautiful landscapes