THE LAND

 

 

RELIEF

 

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) .

 

 

CLIMATE

 

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.


 

 

FLORA AND FAUNA

 

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.