• Landform
  • Surface landform

polje

poljes, karst poljes, interior valley

1.

In 1895, Cvijic defined a polje as a large karst depression, with a wide, flat and nearly horizontal floor, completely enclosed between steep slopes.

White and Culver, 2012 po Cvijić, 1895

2.

The word polje signifies a field or a large plain, and it is still widely used in Slav languages without particular reference to karstic terrain (Sweeting 1972, Roglič 1974), although poljes in the karst of Slovenia are usually called dolina or dol (Gams 1994).

Ford and Williams, 2007 po Sweeting, 1972 in Roglić, 1974

3.

Poljes are an important component of karst, where, aside from the bottoms of major dolines, they are one of the rare formations that can support large-scale agriculture.

Gilli, 2015

4.

polje - a large closed depression draining underground, with a flat floor across which there may be an intermittent or perennial stream and which may be liable to flood and become a lake. the floor makes a sharp break with parts of surrounding slopes.

Gillieson, 1996

5.

Karst poljes are natural retainers of discharge surpluses and important regulators of water conditions in rivers in the lower parts of river basins.

Knez, Petrič and Slabe, 2011

6.

Karst poljes are the largest flat-floored enclosed depressions in karst.

Mihevc, Prelovšek in Zupan Hajna, 2010

7.

polje : In areas of karst topography, a very large closed depression, in some places several kilometers long and wide, having a flat floor either of bare limestone or covered by alluvium, and surrounded by generally steep walls of limestone. Synonym : interior valley.

Monroe, 1970

8.

Karst poljes are large karst depressions with flat bottoms, which are the result of solutional processes and karst water drainage.

White and Culver, 2012

9.

Poljes are the largest closed depressions observed in the karst terrains.

White and Culver, 2012

FORM and surrounded by generally steep walls of limestone
closed
depressions with flat bottoms
largest flat-floored enclosed depressions
LOCATION in areas of karst topography
in rivers in the lower parts of river basins
in karst
SIZE in some places several kilometers long and wide
large
CONTAINS having a flat floor either of bare limestone or covered by alluvium
CAUSE natural
result of solutional processes and karst water drainage
FUNCTION important regulators of water conditions
retainers of discharge surpluses
draining underground
they are one of the rare formations that can support large-scale agriculture
COMPOSITION karstic terrain
RESULT which may be liable to flood and become a lake