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Municipality Of Mirna Peč
The Municipality of Mirna Peč (; sl, Občina 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. Geography The municipality lies at the junction of the Dinaric Alps, the Pannonian Basin, and the Alps, making shallow carbonate bedrocks, in particular limestone, the prevailing substratum. The predominantly hilly landscape with frequent karst features consists of three valleys: the Igmanca Valley, the Temenica Valley, and the Globodol Polje. The Igmanca Valley The Igmanca Valley northeast of Mirna Peč is bounded by Šentjurij Peak ( sl, Šentjurijski vrh) to the south, Snakaš Hill to the west, and Mount Poljane ( sl, Poljanska gora, with the highest peak at 477 m) and Plešivica Hill to the northeast. Although white or gray Jurassic limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Municipalities Of Slovenia
Slovenia is divided into 212 municipalities ( Slovene: ''občine'', singular'' občina''), of which 12 have urban (metropolitan) status. Municipalities are further divided into local communities and districts. Slovene is an official language of all the municipalities. Hungarian is a second official language of three municipalities in Prekmurje: Dobrovnik/Dobronak, Hodoš/Hodos, and Lendava/Lendva. Italian is a second official language of four municipalities (of which one has urban status) in the Slovene Littoral The Slovene Littoral ( sl, Primorska, ; it, Litorale; german: Küstenland) is one of the five traditional regions of Slovenia. Its name recalls the former Austrian Littoral (''Avstrijsko Primorje''), the Habsburg possessions on the upper Adria ...: Ankaran/Ancarano, Izola/Isola, Koper/Capodistria, and Piran/Pirano. In the EU statistics, the municipalities of Slovenia are classified as "local administrative unit 2" (LAU 2), below 58 administrative units ('), which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolenja Vas Pri Mirni Peči
Dolenja Vas pri Mirni Peči () is a small village in the Municipality of Mirna Peč in southeastern Slovenia. The area is part of the historical region of Lower Carniola and is now included in the Southeast Slovenia Statistical Region The Southeast Slovenia Statistical Region ( sl, Jugovzhodna Slovenija statistična regija) is a statistical region in southeast Slovenia. It is the largest statistical region. The development of this region is largely the result of industry (the au .... Name The name of the settlement was changed from ''Dolenja vas'' to ''Dolenja vas pri Mirni Peči'' in 1953.''Spremembe naselij 1948–95''. 1996. Database. Ljubljana: Geografski inštitut ZRC SAZU, DZS. Notable people Notable people that were born or lived in Dolenja Vas pri Mirni Peči include: * Alojzij Progar (1857–1918), sculptor References External linksDolenja Vas pri Mirni Peči on Geopedia Populated places in the Municipality of Mirna Peč {{MirnaPec-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Čemše
Čemše () is a small settlement in the Municipality of Mirna Peč in southeastern Slovenia. The main regional road from Ljubljana to Novo Mesto runs along the western edge of the settlement. The area is part of the historical region of Lower Carniola. The municipality is now included in the Southeast Slovenia Statistical Region The Southeast Slovenia Statistical Region ( sl, Jugovzhodna Slovenija statistična regija) is a statistical region in southeast Slovenia. It is the largest statistical region. The development of this region is largely the result of industry (the au .... References External linksČemše on Geopedia Populated places in the Municipality of Mirna Peč {{MirnaPec-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Biška Vas
Biška Vas () is a village in the Municipality of Mirna Peč in southeastern Slovenia. It lies on the Temenica River north of Mirna Peč. The area is part of the traditional region of Lower Carniola. The municipality is now included in the Southeast Slovenia Statistical Region The Southeast Slovenia Statistical Region ( sl, Jugovzhodna Slovenija statistična regija) is a statistical region in southeast Slovenia. It is the largest statistical region. The development of this region is largely the result of industry (the au .... Name Biška Vas was attested in historical sources as ''Visezdorf'' in 1343, ''Vilessendorf'' in 1351, ''Swysitschdorff'' in 1420, and ''Wissestorff'' in 1433, among other spellings. References External linksBiška Vas on Geopedia Populated places in the Municipality of Mirna Peč {{MirnaPec-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natura 2000
Natura 2000 is a network of nature protection areas in the territory of the European Union. It is made up of Special Areas of Conservation and Special Protection Areas designated under the Habitats Directive and the Birds Directive, respectively. The network includes both terrestrial and Marine Protected Areas. History In May 1992, the governments of the European Communities adopted legislation designed to protect the most seriously threatened habitats and species across Europe. The Habitats Directive complements the Birds Directive adopted earlier in 1979 and together they make up the Natura 2000 network of protected areas. The Birds Directive requires the establishment of Special Protection Areas for birds. The Habitats Directive similarly requires Sites of Community Importance which upon the agreement of the European Commission become Special Areas of Conservation to be designated for species other than birds, and for habitat types (e.g. particular types of forest, grassland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rendzina
Rendzina (or ''rendsina'') is a soil type recognized in various soil classification systems, including those of Britain and Germany as well as some obsolete systems. They are humus-rich shallow soils that are usually formed from carbonate- or occasionally sulfate-rich parent material. Rendzina soils are often found in karst and mountainous regions. The term ''rendzina'' originated via Russian from the Polish ''rędzina'', of unknown origin.https://www.merriam-webster.com/dictionary/rendzina Merriam-Webster In the World Reference Base for Soil Resources, rendzina soils would be classified as leptosols, chernozems, kastanozems, or phaeozems, depending on their specific characteristics. Development and distribution Rendzina soils typically develop from solid or unconsolidated rocky material that is carbonate- or sulphate-rich. Limestone is by far the most common, but others include dolomite, gypsum, marble, chalk and marlstone. Alongside physical weathering, which breaks down the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Terra Rossa (soil)
Terra rossa (Italian for "red soil") is a well-drained, reddish, clayey to silty soil with neutral pH conditions and is typical of the Mediterranean region. The reddish color of terra rossa is the result of the preferential formation of hematite over goethite. This soil type typically occurs as a discontinuous layer that ranges from a few centimeters to several meters in thickness that covers limestone and dolomite bedrock in karst regions. The high internal drainage and neutral pH conditions of terra rossa are a result of the karstic nature of the underlying limestone and dolomite.Torrent, J., 2005. ''Mediterranean soils.'' In: Hillel, D. (Ed.), ''Encyclopaedia of Soils in the Environment,'' vol. 2. Elsevier Academic Press, Oxford, pp. 418–427.Merino, E., Banerjee, A. and Dworkin, S., 2006. ''Dust, terra rossa, replacement, and karst: serendipitous geodynamics in the critical zone.'' ''Geochimica et Cosmochimica Acta,'' 70(18), p. A416.Vingiani, S., Di Iorio, E., Colombo, C. an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Polje
A polje, also karst polje or karst field, is a large flat plain found in karstic geological regions of the world, with areas usually . The name derives from the Slavic languages and literally means 'field', whereas in English ''polje'' specifically refers to a karst plain or karst field. In geology A polje, in geological terminology, is a large, flat-floored depression within karst limestone, whose long axis develops in parallel with major structural trends and can become several miles (tens of kilometers) long. Superficial deposits tend to accumulate along the floor. Drainage may be either by surface watercourses (as an ''open polje'') or by swallow holes (as a ''closed polje'') or ponors. Usually, the ponors cannot transmit entire flood flows, so many poljes become wet-season lakes. The structure of some poljes is related to the geological structure, but others are purely the result of lateral dissolution and planation. The development of poljes is fostered by any blockage i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Goriška Vas, Mirna Peč
Goriška Vas () is a small village in the Municipality of Mirna Peč in southeastern Slovenia. The municipality is included in the Southeast Slovenia Statistical Region. The area is part of the traditional region of Lower Carniola Lower Carniola ( sl, Dolenjska; german: Unterkrain) is a traditional region in Slovenia, the southeastern part of the historical Carniola region. Geography Lower Carniola is delineated by the Ljubljana Basin with the city of Ljubljana to the no .... References External linksGoriška Vas on Geopedia Populated places in the Municipality of Mirna Peč {{MirnaPec-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Estavelle
In karst geology, estavelle or inversac is a ground orifice which, depending on weather conditions and season, can serve either as a sink or as a source of fresh water. It is a type of ponor or sinkhole A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are locally also known as ''vrtače'' and shakeholes, and to openi .... References Karst Cave geology Dinaric karst formations Dinaric Alps {{geology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sinkhole
A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are locally also known as ''vrtače'' and shakeholes, and to openings where surface water enters into underground passages known as ''ponor'', swallow hole or swallet. A ''cenote'' is a type of sinkhole that exposes groundwater underneath. A ''sink'' or ''stream sink'' are more general terms for sites that drain surface water, possibly by infiltration into sediment or crumbled rock. Most sinkholes are caused by karst processes – the chemical dissolution of carbonate rocks, collapse or suffosion processes. Sinkholes are usually circular and vary in size from tens to hundreds of meters both in diameter and depth, and vary in form from soil-lined bowls to bedrock-edged chasms. Sinkholes may form gradually or suddenly, and are found worldwide. Formation Natural processes Sinkholes may capture surf ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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