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Dobličica
Dobličica Creek is a stream in White Carniola. It is part of a karst aquifer. Due to its geological and hydrological characteristics and urbanization of the area, it is considered sensitive and subject to pollution.
==Geography==
Dobličica Creek has its source in the eastern foothills of Mount Poljane ((スロベニア語:Poljanska gora)) at Lake Dobliče ((スロベニア語:Dobličko jezero)), which is across and up to deep. The bed of the lake is covered with large boulders, among which karst water flows from two depressions. A karst spring with a constant flow feeds the lake, with an outflow in a broad but shallow channel. The upper part of the creek bed is rocky mixed with sand, and the banks are loamy. Soon after the source, another spring adds its water to the flow from the lake. The channel is bordered by typical riverside vegetation and meanders through meadows before being joined by Potok Creek and emptying into the Lahinja River at Črnomelj. Dobličica Creek and the Lahinja River surround the old town center of Črnomelj on three sides.〔Melik, Anton. 1964. ''Rast naših mest v novi dobi''. Ljubljana: Slovenska Akademija Znanosti in Umetnosti, p. 89.〕〔Dular, Janez, & Sneža Tecco Hvala. 2007. ''Jugovzhodna Slovenija v starejsi Zelezni dobi / South Eastern Slovenia in the Early Iron Age''. Ljubljana: ZRC, p. 184.〕
A catchwater for the White Carniola water system was created near the lake in 1958.〔Savnik, Roman, ed. 1971. ''Krajevni leksikon Slovenije'', vol. 2. Ljubljana: Državna založba Slovenije, p. 31.〕
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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