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Birth of the Danube Delta
Travelling on the arms, canals and lakes at the mouths of the Danube,
tourists will undoubtedly wonder about their birth, about the genesis of
the entire ecosystem of the delta. Indeed this is a real realm of
passionate problems, wich required considerable efforts for the
scientists. We contend this, because passionate scientific debates were
held on the genesis of the delta, hypotheses were advanced, wich could
be confirmed or invalidated by obvious testimonies alone.
Geographic Location
→ the Buceag Highland
To the south-west → the Tulcea Hills
To the south-east → the Black Sea
Relief
The Delta is a wide-stretched surface, we could even say an even area
with an average altitude of only 0.31m. The low parts within the region
are in the beds of the arms and lakes on the:
Chilia arm (-36m)
Sulina arm (-18m)
Saint Gheorghe arm (-26m)
Then the lakes:
Belciug (-12m)
Rosu (-2,5m)
Gorgova (-2,5m)
Matita (-2m)
The highest altitudes are on the Chilia bank (6,5m), Letea bank (13m),
as well as in the area of the Caraorman dunes, in the region of the
Razelm lagoon complex, where the rocky islands of Bisericuta (4m) and
Popina (49m) are located.
Hidrography
The hydrographic network of the delta is of a particular interest from
the geographic, economic and tourist point of view. The hydrographic
network supplies the lakes with water, with mineral and organic
substances brought by the water, and secures travel to areas where it is
not possible to go on foot. This network includes: the Danube arms,
backwaters, and canals. As to the arms, they are four, of which only
three have mouths at sea: Chilia, Sulina and Saint Gheorghe. The Tulcea
arm is defined between the two “ceatals†(as the arms ramifications
are called there) Chilia and Saint Gheorghe. The Tulcea arm and the
Chilia arm initially were one of the two delta arms. Later on, the other
two arms separated: Sulina and Saint Gheorghe. In order to avoid certain
confusions, some researchers consider that only three arms should be
taken into account: Chilia, Sulina and Saint Gheorghe. The Sulina arm
has lost its initial natural character due to man’s
Intervention. At the beginning it was dredged just at its mouth soon
after 1858, and later on all along its course, that is between 1880 and
1903, when due to the lay out, its length was shortened from 83.8 km to
62.6 km. By the improvements made by building groins, lighthouses, and
laying slabs and beacons a.o., this water course has lost both its old
aspect and the name of arm, being put down on maps and papers as a
“canalâ€Â. The improvement and upkeep work at the Sulina canal was not
confined to the mentioned period alone it was continued, since it is a
waterway of international importance, being part of the Danube’s
maritime sector with a total length of 170 km.
The hydrographic network is quite complex and the reader will be able
to pursue it easily both on the map and on the sketches showing tourist
routes.
Flora and fauna
The vegetation of the delta grows in various suroundings: flowing
water (rivers) , standing water (lakes, swamps), land liable to
overflooding, banks, dunes, beaches. It is estimated that the Danube
Delta includes about 1,150 plant species.
Plancton – floatin microscopic plants – and zooplancton –
floatin microscopic animals – are quite abundant both in flowing and
standing waters. Plancton is used by fish for food. The speed of flowing
water does not allow the growth of large plants. Various algae species
populate this dynamic medium, their number reaching some millions in one
cubic metre.
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