THE LAND
Romania is noted for
its harmonious relief; it is roughly divided into thirds : the plains, the
hills and plateau and the mountains.
In a more or less central
position lie the Carpathians with their peaks of between 1,800 and 2,500 m., which
once protected the Dacians; there the Romanians' ancestors made their home.
The Carpathians are a
continuation of the Alps. They are the most sinuous chain of mountains in the
whole of Europe, with several extinct volcanoes. Metamorphic, volcanic and
sedimentary rocks with the most weird and fantastic shapes are a source of
attraction to both the expert and the ordinary visitor.
The peaks above 2,500 m. are
rare : Moldoveanu, Bucegi, Fagarash, Paring and Retezat. Traces of the glacial
period contribute in particular to the beauty of the mountain scenery.
Depressions, passes and
defiles cut passages through the mountain range. Some of the most famous
include the Iron Gates, the Turnu Roshu Gorge, and the long narrow corridor of
the Bicaz Gorges.
The Sub‑Carpathians ‑ this is
a chain of hills and depressions with similar characteristics to the
Carpathians, except that they are completely covered in forests and the soil is
particularly rich in minerais coai, salt and especially oil. These are high
hills, reaching 700‑800 m. and more.
PRINCIPAL MOUNTAIN PEAKS
|
|
|
|
Name |
Massif (County) |
Height in m. |
|
Moldoveanu |
Fagarash (Argesh) |
2543 |
|
Negoiul |
Fagarash (Argesh, Brashov,
Sibiu) |
2535 |
|
Paringul-Maro |
Paring (Gorj, Hunedoara) |
2518 |
|
Poleaga |
Retezat (Hunedoara) |
2509 |
|
Omul |
Bucegi (Prahova, Brashov,
Dimbovitra) |
2507 |
|
Coshtlia |
Bucegi (Prahova,
Dimbovitza) |
2495 |
|
Iezerul |
lazer (Argesh) |
2462 |
|
Papusho |
lezer (Argesh) |
2397 |
|
Pietrosul |
Rodna (Maramuresh) |
2305 |
|
Gugu |
Godeanul (Carash-Severin,
Hunedoara) |
2210 |
|
Suru |
Fagarash (Sibiu, Vilcea) |
2282 |
|
Inaul |
Rodna (Bistritza-Nasavd,
Suceava, Maramuresh) |
2280 |
|
Cindrelu |
Cindrelu (Sibiu) |
2245 |
|
La Om |
Piatra Craiului (Brashov,
Argesh) |
2239 |
|
Godeanul |
Godeanul (Carash-Severin,
Hunecloars, Gorj) |
2229 |
|
Tsarcu |
Tzarcu (Carash-Severin) |
2186 |
|
Virful lei Patru |
Shureanu (Hunedoara) |
2130 |
|
Pietrosul |
Caliman (Suceava, Muresh) |
2102 |
|
Shureanu |
Shareanu (Hunedoara) |
2061 |
|
Ciucash |
Ciucash (Brashov, Prahova) |
1956 |
|
Ceahlau (Tosca) |
Ceahlau (Neamtz) |
1904 |
|
Giumalau |
Rarau (Svceava) |
1857 |
|
Ocolash Mare |
Ceahlau (Neamtz) |
7857 |
|
Curcuboto |
Biharia (Bihor, Alba) |
1844 |
|
Vladeasa |
Biharia (Cluj) |
1836 |
|
Harghita |
Harghita (Harghita) |
1801 |
|
Pietrosul Domei |
Bistritza (Suceava) |
1794 |
|
Haghimashul-Mare |
Haghimash (Harghita) |
1793 |
|
Lacautzi |
Vrancei (Buzau, Covasna,
Vrancea) |
1777 |
|
GrIndushul |
Tarcau (Bateu) |
1662 |
|
Rarau |
Rarau (Suceava) |
1653 |
The Plateau ‑ a more regular
landscape, also rich in minerals : oil, salt and methane gas; mineral waters;
crops, orchards and forests.
The Transylvanian Plateau is situated
within the Carpathian mountains, and on the outside of the range, and
encircling them, are the somewhat lower subCarpathians. (500‑700 m.). Gentler
hills border the subCarpathians and lead down into the plains and the rivers.
The Plains ‑ the Romanian
Plain (Wallachia) and the Western Plain lie at a height of between 40‑100 m.,
with deep valleys cut by the Danube and its tributarias.
The fast flowing rivers of
the plain ‑ the Olt, Muresh, Somesh Siret, Argesh, Dimbovitza, Bistritza etc. ‑
rise in the Carpathians and eventually join the Danube, towards the sea.
PRINCIPAL RIVERS
|
|
|
Name |
Total km |
|
Danube |
2 857 |
|
Prut |
950 |
|
Muresh |
741 |
|
Olt |
670 |
|
Siret |
676 |
|
lalomitze |
400 |
|
Somesh |
407 |
|
Jiu |
331 |
|
Argesh |
327 |
|
Buzau |
308 |
|
Bistritze |
290 |
|
Jijia |
287 |
|
Tirnave |
258 |
|
Birlad |
253 |
|
Dimbovitzo |
i37 |
|
Timish |
339 |
|
Moldova |
216 |
|
Vades |
215 |
|
CrIshul-Alb |
216 |
|
Tirnava•Mica |
183 |
|
Praheva |
176 |
|
Oltetz |
175 |
|
Suceava |
170 |
|
Arlesh |
167 |
|
Bege |
234 |
|
Trotush |
158 |
|
Somoshul-Mic |
153 |
|
NeaJlov |
150 |
|
|
PRINCIPAL LAKES
|
|
|
Name |
Genetic type (County) |
Lake |
|
Razelm |
sea lagoon (Tulcaa) |
394 |
|
Sinos |
sea lagoon (Constantza) |
166 |
|
Zmeica |
sea lagoon (Constantza) |
52 |
|
Izvorul Muntelul |
|
|
|
Bicaz |
artificial lake (Neamtz) |
33 |
|
Oltina |
viver lagoon (Constantza) |
30 |
|
Rastu |
water meadow lake (Doij) |
25 |
|
Bratesh |
water meadow Iake
(fisheries) (Galatz) |
24 |
|
Babadag |
viver and sea lagoon
(Tulcea) |
23 |
|
Mostishtaa |
viver lagoon
(Ilfov-lalomitza) |
23 |
|
Siutghiol |
sea lagoon (Constantza) |
21 |
|
Dranov |
water meadow lake (Tuleea) |
20 |
|
Tashaul |
viver and sea lagoon
(Constante) |
18 |
|
Gorgova |
water meadow lake -
delta-typs (Tulcea) |
13 |
|
Roshu |
water meadow lake -
deles-type (Tules) |
13 |
|
Techirghiol |
viver and sea lagoon
(Constante) |
11 |
|
Jirlav |
viver lagoon (Braila) |
11 |
|
Vldraru |
artifical lake (Argesh) |
8,27 |
|
Amara-Faurei |
viver lagoon (Buzau) |
7,80 |
|
Snagov |
viver lagoon (Ilfov) |
5,70 |
|
Sulitsa |
water meadow lake
(Botoshani) |
4,00 |
|
Cincish-Telluc |
artificial lake (Hunsdoara) |
2,61 |
|
Balei |
artificial lake (Bacau) |
2,40 |
|
Caldarushani |
viver lagoon (Ilfov) |
2,21 |
On the left bank of the
Danube lies the "Valley" an area composed of alluvial deposits.
Between the two branches of the
Danube, lie the lalomitza Marsh and the Braila Marsh. The latter has been
largely reclaimed and exploited agriculturally.
The connecting bridge between
the Danube and the Black Sea is the Dobrogea Plateau. It ranges from the
fertile Danube plains and the Delta to the remains of the Palaeozoic mountain
chain.
The Danube Delta ‑ the lowest
lying plain in Romania and still in the process of being formed. (See The
Danube Delta chapter) .
Romania has a temperate,
continental climate that is, generally hot summers and cold winters, sometimes
dry with snowfalls. Spring is quite short, while Autumn is often a prolonged
summer.
On the whole, this is a
fairly balanced climate, with damp sea air coming from the east, dry,
continental air from the west and mild Mediterranean air from the south.
Certain variations can be
explained by individual physical features ‑ mountains, valleys, depressions
etc.
The highest mean annual
temperatures are in the south ‑ Dobrogea, the Romanian Plain, the Banat Plain ‑
the lowest in the mountain areas particularly the Carpathian Peaks.
January temperatures vary
between ‑2°C and ‑10°C. In July, they are on an average 22‑25°C, cooler,
however, in the mountains ‑ about 8°C in the Retezat, Fagarash and Bucegi
Mountains.
Air masses are, on the whole,
irregular; west winds prevail in Transylvania; north and north‑east in Moldova;
north‑east and south‑east in the Bargan and the Dobrogea.
Rainfall is lowest on the
Black Sea coast : under 400 mm. annually, and highest in the mountains :
1000-1400 mm. The season of heaviest rainfall is spring.
Romania has an especially
varied flora and fauna ‑ the result of the relief and climate. The mountains,
the home of the chamois and the bearded vulture, are covered with conifers,
beeches and oak trees; orchards, vineyards, wheat, maize and sunflowers are to
be found in the hills and the plains.
The flora includes local
variations, known as "endemic elements" ‑ for example, the
Hierarchism type of the Composted family ‑ which are found only in Romania.
These are rare and of especial scientific interest and value.
Similarly, the fauna includes
species characteristics of the natural environments. One of the rarer species
to be found in the forests of Romania is the Carpathian Stag. Hares and
bustards are found in the steppe and pheasants in special reserves.
Romania's wildlife is
protected by laws and regulations, in particular the rarer species and many
natural reservations have been established.