Vulsini, also known as Volsini volcano, Vulsini Volcanic District, Vulsini Volcanic Complex and the Vulsinian District, is a circular region of intrusive igneous rock in Lazio, Italy, about 87 km (54 mi) to the north northwest of Rome, containing a cluster of calderas known to have been active in recent geologic and historical times. Potentially they still are active. The Vulsinian region is one of dozens of intrusive circular regions, most smaller than the Vulsinian, arranged in a band from Campania through Lazio, called the Roman Comagmatic Province. A comagmatic province is a geologic area of the same type and age igneous rock deriving from the same crustal magma. The Roman region is post-collisional; that is, the intrusions were not a result of the lateral stresses that created Italy a
Attributes | Values |
---|
rdf:type
| |
rdfs:label
| - Vulsini (cs)
- Apparato Vulsinio (it)
- Vulsini (fr)
- Vulsini (en)
- Вульсини (ru)
|
rdfs:comment
| - Vulsini je rozlehlý vulkanický komplex rozkládající se na 2 200 km2 v severní části regionu Lazio v Itálii. Je složený z více struskových kuželů a kalder, z nichž 16 metrů široká kaldera Bolsena v současnosti vytváří Bolsenské jezero. (cs)
- Vulsini, also known as Volsini volcano, Vulsini Volcanic District, Vulsini Volcanic Complex and the Vulsinian District, is a circular region of intrusive igneous rock in Lazio, Italy, about 87 km (54 mi) to the north northwest of Rome, containing a cluster of calderas known to have been active in recent geologic and historical times. Potentially they still are active. The Vulsinian region is one of dozens of intrusive circular regions, most smaller than the Vulsinian, arranged in a band from Campania through Lazio, called the Roman Comagmatic Province. A comagmatic province is a geologic area of the same type and age igneous rock deriving from the same crustal magma. The Roman region is post-collisional; that is, the intrusions were not a result of the lateral stresses that created Italy a (en)
- Vulsini, aussi appelé volcan Volsini, district volcanique du Vulsini, ensemble volcanique Vulsini ou encore district Vulsinien (en italien Apparato Vulsinio) est une zone volcanique d'Italie située dans la province de Viterbe de la région du Latium. Elle est composée de trois caldeiras, Bolsena, Latera et Vepe, ainsi que de 17 cônes de tuf. La caldeira de Bolsena est partiellement remplie par le lac du même nom. (fr)
- L'apparato Vulsinio, situato nella zona compresa tra i fiumi Paglia, Tevere e Fiora, fin quasi al Mar Tirreno, è formato da tre complessi vulcanici di epoche diverse: Bolsena, Montefiascone e Latera, che furono i protagonisti dei più estesi e devastanti fenomeni di vulcanismo che sconquassarono la regione circa 600.000 anni fa. La lunga vita dell'apparato è testimoniata dalla varietà di prodotti eruttati e dai fenomeni di vulcanismo secondario che dal Pliocene arrivano fino ad oggi con manifestazioni idrotermali e solfatariche. (it)
- Вульсини (итал. Vulsini) — кальдера, расположенная в регионе Лацио в 87 км к северо-западу от Рима, Италия. Кальдера состоит из туфовых конусов, кратеров, некоторые из которых заполнены водой, подобно озеру Больсена. Данный вулканический комплекс занимает площадь 2200 км². Сформировался в период 300 000 — 160 000 лет назад в результате взрывного извержения и обильного выхода лав на поверхность. Около 5 вулканических объектов вблизи кратера Латера имели плинианский тип извержения в конце плейстоцена. Последняя вулканическая активность происходила в местности Питильяно образованием пемз и туфов, которое было связано с вулканической деятельностью кальдеры Вепе, образованной 166 тыс. лет назад. Вулканическая деятельность характеризовалось возникновением шлаковых конусов и обильным выделением л (ru)
|
foaf:name
| |
name
| |
geo:lat
| |
geo:long
| |
foaf:depiction
| |
dcterms:subject
| |
Wikipage page ID
| |
Wikipage revision ID
| |
Link from a Wikipage to another Wikipage
| |
sameAs
| |
volcanic arc/belt
| |
dbp:wikiPageUsesTemplate
| |
thumbnail
| |
elevation m
| |
location
| |
photo
| |
photo caption
| - Lake Bolsena. The two tuff islands are visible in the distance. (en)
|
type
| |
georss:point
| |
has abstract
| - Vulsini je rozlehlý vulkanický komplex rozkládající se na 2 200 km2 v severní části regionu Lazio v Itálii. Je složený z více struskových kuželů a kalder, z nichž 16 metrů široká kaldera Bolsena v současnosti vytváří Bolsenské jezero. (cs)
- Vulsini, aussi appelé volcan Volsini, district volcanique du Vulsini, ensemble volcanique Vulsini ou encore district Vulsinien (en italien Apparato Vulsinio) est une zone volcanique d'Italie située dans la province de Viterbe de la région du Latium. Elle est composée de trois caldeiras, Bolsena, Latera et Vepe, ainsi que de 17 cônes de tuf. La caldeira de Bolsena est partiellement remplie par le lac du même nom. Les caldeiras se sont formées il y a 300 000, 166 000 et 160 000 ans respectivement pour la caldeira de Bolsena, de Vepe et de Latera. Sa seule et unique éruption des temps historiques enregistrée s'est produite en 104 av. J.-C. mais ses caractéristiques sont inconnues. (fr)
- Vulsini, also known as Volsini volcano, Vulsini Volcanic District, Vulsini Volcanic Complex and the Vulsinian District, is a circular region of intrusive igneous rock in Lazio, Italy, about 87 km (54 mi) to the north northwest of Rome, containing a cluster of calderas known to have been active in recent geologic and historical times. Potentially they still are active. The Vulsinian region is one of dozens of intrusive circular regions, most smaller than the Vulsinian, arranged in a band from Campania through Lazio, called the Roman Comagmatic Province. A comagmatic province is a geologic area of the same type and age igneous rock deriving from the same crustal magma. The Roman region is post-collisional; that is, the intrusions were not a result of the lateral stresses that created Italy and raised the Apennines, but were subsequent to Italy's creation. The Volsinian is the northernmost region. At relatively low altitude, the Vulsini calderas cover about 2,280 km2 (880 sq mi) and contain four Pleistocene-age depressions known as Bolsena, Latera, Vepe and Montefascione calderas. The latest activity occurred in 104 BC. The largest, the Bolsena caldera, which is roughly 16 km (9.9 mi) across, is filled with the waters of Lake Bolsena, which derive mainly from deep aquifers. Immediately to the northwest are the combined Latera and Vepe calderas, about 8 km (5.0 mi) by 11 km (6.8 mi). Vepe, to the north of Lake Mezzano (a very small crater lake west of Lake Bolsena) is what is known as a nested caldera; it arose in the previously existing Latera Caldera. Italian routes SS74 and SS312 follow the rim from Valentano through Latera westward, turning off before Mezzano on the other side. In addition the small Montefiascone caldera, also nested, lies between Montefiascone on its eastern rim and the lake. Two islands in the lake, Bisentina and Martana, were formed from airfall tuffs in Pompeii-like eruptions. Dozens of other tuff cones dot the region, mainly on the eastern side of the complex. (en)
|