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List Of Fossiliferous Stratigraphic Units In Hungary
This is a list of fossiliferous stratigraphic units in Hungary. List of fossiliferous stratigraphic units in Hungary See also * Lists of fossiliferous stratigraphic units in Europe ** List of fossiliferous stratigraphic units in Slovakia ** List of fossiliferous stratigraphic units in Ukraine ** List of fossiliferous stratigraphic units in Romania ** List of fossiliferous stratigraphic units in Serbia ** List of fossiliferous stratigraphic units in Croatia ** List of fossiliferous stratigraphic units in Slovenia ** List of fossiliferous stratigraphic units in Austria References * {{DEFAULTSORT:Fossiliferous stratigraphic units in Hungary Geologic formations of Hungary, Fossiliferous stratigraphic units of Europe, Hungary Paleontology in Hungary, Hungary geography-related lists ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edelény Formation
Edelény is a town in Borsod-Abaúj-Zemplén county, Northern Hungary. It lies in the valley of Bódva River, north of the county seat, Miskolc. The historic L'Huillier-Coburg Palace is located there. History The area has been inhabited since ancient times (Paleolithic stone tools were found here). Edelény was first mentioned in 1299, but the village of Borsod, which was annexed to the town in the 20th century, was already mentioned in 1108 (Borsod ''comitatus'' belonged to the castle of Borsod in the Middle Ages). The residents of Edelény worked in agriculture in mediaeval times. During the Turkish occupation of Hungary, the town was deserted several times. In the 19th century, industry became more important in the area. In 1838, a sugar factory was built, and a Lignite, brown coal mine was opened. The Jewish population (1910: 8.3%; 1941: 7.9%) was deported and murdered in early June 1944. Two nearby villages were annexed to Edelény: Borsod in 1950, and Finke in 1963. Edel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tard Clay Formation
Tard is a village in Borsod-Abaúj-Zemplén county, Hungary Hungary ( hu, Magyarország ) is a landlocked country in Central Europe. Spanning of the Carpathian Basin, it is bordered by Slovakia to the north, Ukraine to the northeast, Romania to the east and southeast, Serbia to the south, Croatia a .... References External links Street map Populated places in Borsod-Abaúj-Zemplén County {{Borsod-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Polány Marl
Polány (german: Polern) is a village in Somogy county, Hungary Hungary ( hu, Magyarország ) is a landlocked country in Central Europe. Spanning of the Carpathian Basin, it is bordered by Slovakia to the north, Ukraine to the northeast, Romania to the east and southeast, Serbia to the south, Croatia a .... External links Street map (Hungarian) References Populated places in Somogy County {{Somogy-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Csolnok Marl
Csolnok (german: Tscholnok or ) is a village in Komárom-Esztergom County, Hungary Hungary ( hu, Magyarország ) is a landlocked country in Central Europe. Spanning of the Carpathian Basin, it is bordered by Slovakia to the north, Ukraine to the northeast, Romania to the east and southeast, Serbia to the south, Croatia a .... External links Street map (Hungarian) Populated places in Komárom-Esztergom County Hungarian German communities {{Komarom-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lutetian
The Lutetian is, in the geologic timescale, a stage or age in the Eocene. It spans the time between . The Lutetian is preceded by the Ypresian and is followed by the Bartonian. Together with the Bartonian it is sometimes referred to as the Middle Eocene Subepoch. Stratigraphic definition The Lutetian was named after Lutetia, the Latin name for the city of Paris. The Lutetian Stage was introduced in scientific literature by French geologist Albert de Lapparent in 1883 and revised by A. Blondeau in 1981. The base of the Lutetian Stage is at the first appearance of the nanofossil ''Blackites inflatus'', according to an official reference profile (GSSP) established in 2011. Of two candidates located in Spain, the Gorrondatxe section was chosen.See thwebsite of Eustoquio Molinafor these candidates. The top of the Lutetian (the base of the Bartonian) is at the first appearance of calcareous nanoplankton species ''Reticulofenestra reticulata''. The Lutetian overlaps with the Geisel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dorog Coal Formation
Dorog (german: Drostdorf) is a small town in Komárom-Esztergom County, Hungary. It lies north-west from the center of Budapest. Etymology The name comes from Slavic ''drugъ'' (drug) - a partner, comrade, "brother". History The valley between the Pilis and Gerecse mountains has been inhabited since the Neolithic. A Roman military road westwards from Aquincum passed by the present-day town of Dorog, where Roman dwellings with floor heating have been found, along with conduits, graves and milestones. When Hungary's kings resided at Esztergom in the 11th and 12th centuries, Dorog was where the cooks of the castle lodged. Roads from all directions met here in the Middle Ages, and the Chapter of Esztergom had the right to levy custom duties. The name, which appears in the form ''Durug'', ''Drug'' and ''Durugd'', is first mentioned in an extant document in 1181. The medieval settlement, destroyed in the Ottoman invasion, remained uninhabited from 1542 until 1649. German ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bartonian
The Bartonian is, in the ICS's geologic time scale, a stage or age in the middle Eocene Epoch or Series. The Bartonian Age spans the time between . It is preceded by the Lutetian and is followed by the Priabonian Age. Stratigraphic definition The Bartonian Stage was introduced by Swiss stratigrapher Karl Mayer-Eymar in 1857. The name derives from the coastal village Barton-on-Sea (part of New Milton) in southern England. The Barton Group, a lithostratigraphic unit from the south English Hampshire Basin, is of Bartonian age. The distinction between group and stage was made in the second part of the 20th century, when stratigraphers saw the need to distinguish between litho- and chronostratigraphy. The base of the Bartonian is at the first appearance of the calcareous nanoplankton species ''Reticulofenestra reticulata''. In 2009, an official reference profile (GSSP) for the base of the Bartonian had not yet been established. The top of the Bartonian Stage (the base of the Pria ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Priabonian
The Priabonian is, in the ICS's geologic timescale, the latest age or the upper stage of the Eocene Epoch or Series. It spans the time between . The Priabonian is preceded by the Bartonian and is followed by the Rupelian, the lowest stage of the Oligocene. Stratigraphic definition The Priabonian Stage was introduced in scientific literature by Ernest Munier-Chalmas and Albert de Lapparent in 1893. The stage is named after the small hamlet of Priabona in the community of Monte di Malo, in the Veneto region of northern Italy. The base of the Priabonian Stage is at the first appearance of calcareous nannoplankton species ''Chiasmolithus oamaruensis'' (which forms the base of nanoplankton biozone NP18). An official GSSP was ratified in 2020, and was placed in the Alano di Piave section in Alano di Piave, Belluno, Italy. The top of the Priabonian Stage (the base of the Rupelian Stage and Oligocene Series) is at the extinction of foram genus ''Hantkenina''. Sometimes local rock ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buda Marl
Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part of the cliffs of Dover, and the Channel Tunnel follows these marl layers between France and the United Kingdom. Marl is also a common sediment in post-glacial lakes, such as the marl ponds of the northeastern United States. Marl has been used as a soil conditioner and neutralizing agent for acid soil and in the manufacture of cement. Description Marl or marlstone is a carbonate-rich mud or mudstone which contains variable amounts of clays and silt. The term was originally loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions. These typically contain 35–65% clay and 65–35% carbonate. The ter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Törökbálint Formation
Törökbálint is a town in Pest county, Hungary. Törökbálint received town status on 1 July 2007. The city also has a German name, ''Großturwall'', which originates from the times of the Swabian immigration after the Ottoman times of Hungary. Geographic position Törökbálint is c. westwards from Budapest, between Diósd and Budakeszi, which were also Swabian settlements. Törökbálint can be directly approached from the motorways M0, M1 and M7. History Early history Until the 1st century, the Avaric peoples were the inhabitants of Hungary, which the Romans chased away. Both nations left their footprint over the entirety of Hungary, and in Törökbálint as well, though the region was uninhabited until the 6th century, well after the Roman invasion. Germanic tribes arrived around this time. After the Magyar settlement in the 9th century, the main leader of the Hungarians, Árpád, gave the lands around the present Törökbálint to prince Kond, whose son, Cs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
