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Šoštanj Fault
The Šoštanj Fault (; ) is a fault in Slovenia. It connects the Periadriatic Fault with the Lavanttal Fault and strikes NW-SE. Movements along the fault are dextral strike-slip and took place in the Pliocene. The fault is named after the town of Šoštanj Šoštanj (; ) is a town in northern Slovenia. It is the seat of the Municipality of Šoštanj. The area is part of the traditional region of Styria. The entire municipality is now included in the Savinja Statistical Region. History Šoštanj w .... References Geology of Slovenia Seismic faults of Europe {{Slovenia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slovenia
Slovenia, officially the Republic of Slovenia, is a country in Central Europe. It borders Italy to the west, Austria to the north, Hungary to the northeast, Croatia to the south and southeast, and a short (46.6 km) coastline within the Adriatic Sea to the southwest, which is part of the Mediterranean Sea. Slovenia is mostly mountainous and forested, covers , and has a population of approximately 2.1 million people. Slovene language, Slovene is the official language. Slovenia has a predominantly temperate continental climate, with the exception of the Slovene Littoral and the Julian Alps. Ljubljana, the capital and List of cities and towns in Slovenia, largest city of Slovenia, is geographically situated near the centre of the country. Other larger urban centers are Maribor, Ptuj, Kranj, Celje, and Koper. Slovenia's territory has been part of many different states: the Byzantine Empire, the Carolingian Empire, the Holy Roman Empire, the Kingdom of Hungary, the Republic of Venice ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Periadriatic Fault
The Periadriatic Seam (or fault) is a distinct geologic fault in Southern Europe, running ''S-shaped'' about from the Tyrrhenian Sea through the whole Southern Alps as far as Hungary. It forms the division between the Adriatic plate and the Eurasian plate. Tectonics and geology Within the Eastern Alps, the line marks the border between the Central Eastern Alps and the Southern Limestone Alps. In the Western Alps it forms the division between the southern Apulian foreland and the central crystalline zones of the Alps. Continental collision is still going on, with the Apulian and Eurasian plates still converging. The central zones of the Alps are rising too, causing vertical slip along the fault. The result is the set of major fault zones collectively named Periadriatic Seam. Movement along the Periadriatic Seam is the cause for the earthquake zone between Vienna and Friuli. The last destructive earthquake happened in Friuli in 1976. The uplift caused violent erosion of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lavanttal Fault
The Lavanttal Fault (or Pöls-Lavanttal Fault, Labot Fault; ) is a seismically active fault that stretches from Austria in the north to Slovenia in the south. The fault strikes NNW-SSE and shows dextral strike-slip movements. In the southern part, the Lavanttal Fault displaces the Periadriatic Fault or Balaton Fault. Movements along the fault led to the formation of the Fohnsdorf Basin and the Lavanttal Basin The Lavanttal ('Lavant Valley', , Gams, Ivan. 1992. "Labotska dolina." ''Enciklopedija Slovenije'', vol. 6. Ljubljana: Mladinska knjiga, pp. 87–87. or ; Southern Bavarian: ''Lovnthol'') lies in the Lavanttal Alps in southern Austria in the eas .... References Geology of Austria Geology of Slovenia Seismic faults of Europe {{seismology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pliocene
The Pliocene ( ; also Pleiocene) is the epoch (geology), epoch in the geologic time scale that extends from 5.33 to 2.58See the 2014 version of the ICS geologic time scale million years ago (Ma). It is the second and most recent epoch of the Neogene Period in the Cenozoic, Cenozoic Era. The Pliocene follows the Miocene Epoch and is followed by the Pleistocene Epoch. Prior to the 2009 revision of the geologic time scale, which placed the four most recent major glaciations entirely within the Pleistocene, the Pliocene also included the Gelasian Stage, which lasted from 2.59 to 1.81 Ma, and is now included in the Pleistocene. As with other older geologic periods, the Stratum, geological strata that define the start and end are well-identified but the exact dates of the start a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Šoštanj
Šoštanj (; ) is a town in northern Slovenia. It is the seat of the Municipality of Šoštanj. The area is part of the traditional region of Styria. The entire municipality is now included in the Savinja Statistical Region. History Šoštanj was first mentioned in written documents dating to around 1200 as ''Schönstein'' in relation to its castle. As a market town it was first mentioned in 1348. It was given town status in 1919 and until the 1960s was the center of the Šalek Valley (). In 1963 nearby Velenje Velenje (; ''Leksikon občin kraljestev in dežel zastopanih v državnem zboru,'' vol. 4: ''Štajersko''. 1904. Vienna: C. Kr. Dvorna in Državna Tiskarna, p. 272.) is the List of cities and towns in Slovenia, sixth-largest city of Slovenia, and t ... became the administrative center. Šoštanj again became a municipal center in the late 1990s. The town has a long leather-working history, with industrial-scale activity going back to 1788. The factory was owned by the Wo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of Slovenia
Slovenia is situated in Central Europe, touching the Alps and bordering the Adriatic Sea. The Alps—including the Julian Alps, the Kamnik–Savinja Alps and the Karawank chain, as well as the Pohorje massif—dominate northern Slovenia along its long border to Austria. Slovenia's Adriatic coastline stretches approximately from Italy to Croatia. The term ''karst'' originated in southwestern Slovenia's Karst Plateau (), a limestone region of underground rivers, gorges, and caves, between Ljubljana and the Mediterranean. On the Pannonian plain to the east and northeast, toward the Croatian and Hungarian borders, the landscape is essentially flat. However, the majority of Slovenian terrain is hilly or mountainous, with around 90% of the surface 200 meters or more above sea level. Location Slovenia's location is where southeastern and Central Europe meet, where the Eastern Alps border the Adriatic Sea between Austria and Croatia. The 15th meridian east almost corresponds to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
