Moldavian Plateau

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Moldavian Plateau
Topography

Bukovinian Subcarpathians
Moldavian Subcarpathians


Suceava Plateau
Dniester Hills
Moldavian Plain
Bârlad Plateau
Central Moldavian Plateau


Bălți Steppe
Bugeac Steppe

Hydrography

Danube

Suceava
)
Prut
Dniester (Răut)
Black Sea

Climate

Romania
Moldova

Flora & Fauna

Flora of Romania
Flora of Moldova

List of mammals in Romania

List of mammals in Moldova

Protected areas in Romania

Protected areas in Moldova

The Moldavian Plateau (Romanian: Podișul Moldovei) is a geographic area of the historical region of Moldavia, spanning nowadays the east and northeast of Romania, most of Moldova (except the south), and most of the Chernivtsi Oblast of Ukraine (where it is known as the Pokuttyan-Bessarabian Upland[1]).

Limits

The old Principality of Moldavia comprised the entire Moldavian Plateau and some neighbouring geomorphological units such as the Carpathian Mountains

The Moldavian Plateau is bounded (in clockwise order), as follows.

The Moldavian Plateau comprises over two-thirds of the territory of the medieval

Principality of Moldavia, with the Eastern Carpathian Mountains and the Bugeac Plain representing the remaining part. This fact is the origin of the name of the plateau. This geographic area (including Eastern Carpathians and the Bugeac) is also called (especially by historians) the Carpathian-Dniester-Pontic region, or the Carpathian-Dniester region, since it is bounded by the Carpathians to the west, by the river Dniester to the north and east, and by the Black Sea (Pontus Euxinus) and the Danube
to the south-east and south.

Genesis

The Moldavian Plateau was formed at the end of the

badlands, which produce landslides or other natural hazards.[2]

The slope of the terrain follows the direction of the rivers: from northwest to southeast. Along them, the altitude decreases from 700 m (2,300 ft) to under 200 m (660 ft). The strata are disposed in North-South and northwest-southeast aligned layers, producing asymmetric valleys and ridges. Among the latter are the steep edge of the Bârlad Plateau (Romanian: Podișului Bârladului), known as the Iași Ridge (Romanian: Coasta Iașilor), the edge of the Central Moldavian Plateau (Romanian: Podișul Moldovei Centrale), known as the Cornești Hills, and the edge of the Dniester Hills, known as the Dniester Ridge.

The relief in the valleys of the rivers and creeks is quite conspicuous, so that the valleys have large

Răut Passage separates the main part of the Moldavian Plateau from the Dniester Hills

Composition

The Moldavian Plateau comprises several distinct regions:

  • The Bukovinian Subcarpathians in the northwest.
  • The Moldavian Subcarpathians in the west and southwest, has altitudes of up to 1,000 m (3,300 ft), but also includes depressions.
  • The Suceava Plateau (Romanian: Podișul Sucevei), situated in the northwest, has altitudes that exceed 700 m (2,300 ft) and long ridges.
  • The
    Dniester River
    and has elevations of approximately 300 m (980 ft).
  • The Moldavian Plain (Romanian: Câmpia Moldovei), in the center-north has elevations of approximately 200 m (660 ft):
    • The Jijia Plain, west of the river Prut.
    • The Middle Prut Valley, east of the river Prut, creeks tributary to the Prut, 2,930 square kilometres (1,131 sq mi).
    • The Bălți Steppe, east of the river Prut, creeks tributary to the Dniester, 1,920 square kilometres (741 sq mi).
  • The Bârlad Plateau (Romanian: Podișul Bârladului), situated in the south-center occasionally has heights over 500 m (1,600 ft), but is generally sloped from north at 400 m (1,300 ft) to the south at 200 m (660 ft).
  • The Central Moldavian Plateau (Romanian: Podișul Moldovei Centrale), situated in the center and southeast, has elevations that in the north-south direction decrease in altitude from 400 m (1,300 ft) to under 200 m (660 ft).
  • The
    Bugeac Plain, the last continuation of the Pontic–Caspian steppe
    .

Climate

The climate of this plateau is transitional

. Overall, the altitude affects the climate, with annual mean temperatures in the Suceava Plateau ranging between 6 °C (43 °F) and 8 °C (46 °F) and precipitation of 500 millimetres (19.7 in) to 800 millimetres (31.5 in) per year and, with annual mean temperatures of 8 °C (46 °F) to 10 °C (50 °F) and precipitation of 400 millimetres (15.7 in) to 500 millimetres (19.7 in) in the Moldavian Plain or Bârlad Plateau.

The main influence on the climate is Dry Continental with frequent cold north winds in winter. In the Suceava Plateau and the Dniester Hills, there is an influence of Scandinavo-Baltic climate with the circulation of masses of polar air in the winter.

Waters

Streams on the plateau flow into the Siret, Prut, or Dneister rivers. The Prut has the Jijia as its principal tributary. The Siret traverses and—with the exception of the Subcarpathians—limits the Moldavian Plateau

The lack of precipitation has required water management in the Jijia Plain and in the Bălți steppe which serves as a reservoir and for

Lake Stânca-Costești, Lake Dubăsari [ro
]), in the Siret Passage.

Natural resources

The Moldavian Plateau holds

kaolin (china clay), extracted and used to produce porcelain
.

Hemp is cultivated in the Suceava plateau, cereals and wine grapes (Vitis vinifera) in the Jijia Plain, Bălți steppe, Bârlad Plateau and Central Moldavian Plateau. In the Siret Passage they cultivate potatoes and sugar beets.

Fauna

Characteristic of the plateau are mammals such as goats, wild

owls, and fish include perch and the carp-like barbel
.

References

External links