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Temenica | |
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The upper course of the Temenica, at Sobrače | |
Location | |
Country | Slovenia |
Physical characteristics | |
Mouth | |
• location | Krka |
• coordinates | 45°47′39″N15°07′27″E / 45.7942°N 15.1241°E Coordinates: 45°47′39″N15°07′27″E / 45.7942°N 15.1241°E |
Length | 27 km (17 mi) [1] |
Basin size | 103 km2 (40 sq mi) [1] |
Basin features | |
Progression | Krka→ Sava→ Danube→ Black Sea |
The Temenica is a river in Slovenia. It is one of the most typical influent streams of Slovenia's karst terrain. [2]
The name Temenica comes from the archaic common noun *temenica 'spring' (cf. Polish dialect ciemienica 'spring', Czech temenec 'spring'). [3]
The river goes under the surface twice. It originates in the southern part of the Sava Hills. It sinks for the first time near Dolenje Ponikve in several sinkholes. [4] It emerges again in the Mirna Peč Valley at Zijalo Spring. It runs above ground until a sinkhole near Goriška Vas, where it sinks for the second and last time. The third and last spring of the Temenica is located at Luknja pri Prečni. It flows through the Zalog Karst Field and it joins with the Krka River as its largest tributary. [5]
The Temenica's surface length is 27 kilometres (17 mi), [1] and its subterranean length is 1.75 kilometres (1.09 mi) measured in a straight line. [6]
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground.
Novo Mesto is the city on a bend of the Krka River in the City Municipality of Novo Mesto in southeastern Slovenia, close to the border with Croatia. The town is traditionally considered the economic and cultural centre of the historical Lower Carniola region.
Lower Carniola is a traditional region in Slovenia, the southeastern part of the historical Carniola region.
Dolenjske Toplice is a settlement near Novo Mesto in southeastern Slovenia and is the seat of the Municipality of Dolenjske Toplice. The area is part of the traditional region of Lower Carniola. The municipality is now included in the Southeast Slovenia Statistical Region. The town lies on the Sušica River, which joins the Krka 2 km north of town. It is a spa town known for its thermal baths established in 1658 by the Counts of Auersperg.
Mirna Peč is a rural settlement in southeast Slovenia. It is the seat of the Municipality of Mirna Peč.
Trebnje is a town in southeastern Slovenia.
The Krka is a river in southeastern Slovenia, a right tributary of the Sava. With a length of 94.6 km (58.8 mi), it is the second-longest river flowing in its entirety in Slovenia, following the Savinja.
Košarkarski klub Krka, commonly referred to as KK Krka or simply Krka, is a professional basketball team based in Novo Mesto, Slovenia. The team competes in the Premier A Slovenian Basketball League and the ABA League. The team's home arena is Leon Štukelj Hall. The club is a founding member and shareholder of the Adriatic Basketball Association.
The Reka, also the Inner Carniola Reka, is a river that starts as Big Creek in Croatia, on the southern side of Mount Snežnik, and flows through western Slovenia, where it is also initially known as Big Creek. The river is 54 kilometres (34 mi) long, of which 51 km in Slovenia. At the village of Škocjan it disappears underground through Škocjan Caves, flowing 38 km (24 mi) underneath the Slovenian Karst. The river continues as part of the Timavo in Italy, however, tracer studies have shown that it also feeds springs elsewhere on the Adriatic Coast between Trieste and Monfalcone. It has the pluvial regime.
The Radulja is a river of Slovenia. The river is 33 km (21 mi) in length. It is a left tributary of the Krka River.
Otočec is a settlement on the left bank of the Krka River in the Municipality of Novo Mesto in southeastern Slovenia. The area is part of the traditional region of Lower Carniola and is now included in the Southeast Slovenia Statistical Region.
Čatež ob Savi is a village on the right bank of the Sava River at its confluence with the Krka River in the Municipality of Brežice in eastern Slovenia. The area was traditionally part of Lower Carniola. It is now included with the rest of the municipality in the Lower Sava Statistical Region.
Breg pri Temenici is a settlement on the right bank of the Temenica River in the Municipality of Ivančna Gorica in central Slovenia. The railway line from Ljubljana to Novo Mesto runs just south of the settlement. The area is part of the historical region of Lower Carniola. The municipality is now included in the Central Slovenia Statistical Region.
The Eastern Lower Carniolan subdialect is a Slovene subdialect in the Lower Carniolan dialect group. It is spoken south of the Lower Sava Valley dialect in the watersheds of the Mirna and Temenica rivers, east of a line running from west of Trebnje and west of Novo Mesto to the lower Krka Valley. The dialect includes the settlements of Kostanjevica na Krki, Krmelj, Mirna, Mokronog, Novo Mesto, Raka, Šentjernej, Šentrupert, Škocjan and Trebnje.
Cink is a remote abandoned settlement in the Municipality of Dolenjske Toplice in southern Slovenia. The area is part of the traditional region of Lower Carniola and is now included in the Southeast Slovenia Statistical Region. Its territory is now part of the village of Podstenice.
The Municipality of Mirna Peč is a municipality in southeast Slovenia, located in the traditional region of Lower Carniola. The seat of the municipality, which was established in 1998, is Mirna Peč. With an estimated population of 2,800, the municipality is included in the Southeast Slovenia Statistical Region.
The Trnovo Forest Plateau is a karst plateau that constitutes the extreme northwest end of the Dinaric Alps. The Trnovo Forest Plateau has a karst character, without surface watercourses and broken up by closed valleys, outcroppings, hills, caves, shafts, and smaller karst features: solution pans, rills, karrens, and other features. Significant karst features include ice caves. The vegetation inversion at Big Paradana Ice Cave in the eastern part of the plateau, measuring 385 meters (1,263 ft) by 1,550 meters (5,090 ft), is a locus classicus and in the past ice was harvested from it and exported via Gorizia and Trieste to Egypt.
The Račna Karst Field is a karst field in the northern edge of the Lower Carniolan karst area, south of Grosuplje, Slovenia. It has rich natural and cultural value. Because of its ecological significance, it is anticipated that a nature park will be established there and that it will be included in the Natura 2000 program.
Dry Carniola is a small area in the northwest part of Lower Carniola.
The Rute Plateau is a karst limestone plateau in Lower Carniola, Slovenia with an area of about 9 square kilometers (3.5 sq mi).
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