London Basin (original) (raw)
The London Basin is an elongated, roughly triangular sedimentary basin approximately 250 kilometres (160 mi) long which underlies London and a large area of south east England, south eastern East Anglia and the adjacent North Sea. The basin formed as a result of compressional tectonics related to the Alpine orogeny during the Palaeogene period and was mainly active between 40 and 60 million years ago.
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| dbo:abstract | The London Basin is an elongated, roughly triangular sedimentary basin approximately 250 kilometres (160 mi) long which underlies London and a large area of south east England, south eastern East Anglia and the adjacent North Sea. The basin formed as a result of compressional tectonics related to the Alpine orogeny during the Palaeogene period and was mainly active between 40 and 60 million years ago. (en) Le bassin de Londres est un bassin allongé, grossièrement triangulaire d'environ 250 km de long sur lequel se trouve Londres et une grande partie du Sud-Est de l'Angleterre et du Sud-Est de l'Est-Anglie ainsi que la mer du Nord environnante. Le bassin s'est formé à la suite d'une extension tectonique liée à l'orogenèse alpine durant le Paléogène et fut particulièrement actif il y a 60 à 40 millions d'années. Ce bassin fait partie intégrante du bassin sédimentaire intracratonique Anglo-Parisien à subsidence faible (sédimentation assez peu épaisse, aux dépôts de faible tranche d’eau dans des mers peu profondes et des lacs) contrôlé essentiellement par des processus eustatiques, constitué d'un socle hercynien sur lequel repose en discordance angulaire une couverture de 3 à 5 000 m. (fr) ロンドン盆地（英: London Basin）は、イギリス・ロンドンの周辺に発達する、ほぼ三角形の堆積盆地。テムズ川のほぼ下流域に当たる。盆地はほとんどが市街地で、人口が密集。アルプス造山運動期に、圧縮テクトニクスによって形成された。盆地の北西にチルターン丘陵、南にがある。 (ja) Il bacino di Londra è un bacino strutturale allungato, di forma vagamente triangolare, lungo circa 250 chilometri (160 mi), sottostante alla regione di Londra, a una vasta area dell'Inghilterra sudorientale, alla parte sudorientale dell'Anglia orientale e adiacente al Mare del Nord. Il bacino si è formato come risultato di una compressione tettonica correlata all'orogenesi alpina durante il Paleogene, attiva tra 40 e 60 milioni di anni fa. (it) Basen Londyński, ang. London Basin – nizina w Anglii (Wielka Brytania), w dolnym biegu Tamizy. Stanowi główny region rolniczy Wielkiej Brytanii. (pl) London Basin är en sänka i Storbritannien. Den ligger i riksdelen England, i den södra delen av landet, 26 km väster om huvudstaden London. Kustklimat råder i trakten. Årsmedeltemperaturen i trakten är 11 °C. Den varmaste månaden är juni, då medeltemperaturen är 20 °C, och den kallaste är januari, med 2 °C. (sv) Ло́ндонский бассе́йн (Ло́ндонская ни́зменность; англ. London Basin) — низменная равнина на юго-востоке Великобритании, в нижнем течении Темзы. Лондонский бассейн представляет собой синклинальное понижение, сложенное палеогеновыми и неогеновыми глинами, песками и гравием. Высота достигает 100 м. Имеются небольшие массивы дубовых и буковых лесов, на песках — сосновые боры и верещатники на бурых лесных почвах. В основе — культурные ландшафты (поля, огороды, парки). На территории Лондонского бассейна расположен город Лондон. (ru) 倫敦盆地（London Basin）是以英國倫敦為中心的一個狹長、三角形的沉積盆地，除去大倫敦外，它還包括了東安格利亞東南部和英格蘭東南英格蘭的部分地區，最東端緊鄰北海。它形成于4000至6000万年前古近紀的阿尔卑斯造山运动時期。倫敦盆地主要由泰晤士河灌溉，但其面積並不完全重疊。 位于盆地中的大倫敦都會區有近1000万居民。 (zh) |
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| rdfs:comment | The London Basin is an elongated, roughly triangular sedimentary basin approximately 250 kilometres (160 mi) long which underlies London and a large area of south east England, south eastern East Anglia and the adjacent North Sea. The basin formed as a result of compressional tectonics related to the Alpine orogeny during the Palaeogene period and was mainly active between 40 and 60 million years ago. (en) Le bassin de Londres est un bassin allongé, grossièrement triangulaire d'environ 250 km de long sur lequel se trouve Londres et une grande partie du Sud-Est de l'Angleterre et du Sud-Est de l'Est-Anglie ainsi que la mer du Nord environnante. Le bassin s'est formé à la suite d'une extension tectonique liée à l'orogenèse alpine durant le Paléogène et fut particulièrement actif il y a 60 à 40 millions d'années. Ce bassin fait partie intégrante du bassin sédimentaire intracratonique Anglo-Parisien à subsidence faible (sédimentation assez peu épaisse, aux dépôts de faible tranche d’eau dans des mers peu profondes et des lacs) contrôlé essentiellement par des processus eustatiques, constitué d'un socle hercynien sur lequel repose en discordance angulaire une couverture de 3 à 5 000 m. (fr) ロンドン盆地（英: London Basin）は、イギリス・ロンドンの周辺に発達する、ほぼ三角形の堆積盆地。テムズ川のほぼ下流域に当たる。盆地はほとんどが市街地で、人口が密集。アルプス造山運動期に、圧縮テクトニクスによって形成された。盆地の北西にチルターン丘陵、南にがある。 (ja) Il bacino di Londra è un bacino strutturale allungato, di forma vagamente triangolare, lungo circa 250 chilometri (160 mi), sottostante alla regione di Londra, a una vasta area dell'Inghilterra sudorientale, alla parte sudorientale dell'Anglia orientale e adiacente al Mare del Nord. Il bacino si è formato come risultato di una compressione tettonica correlata all'orogenesi alpina durante il Paleogene, attiva tra 40 e 60 milioni di anni fa. (it) Basen Londyński, ang. London Basin – nizina w Anglii (Wielka Brytania), w dolnym biegu Tamizy. Stanowi główny region rolniczy Wielkiej Brytanii. (pl) London Basin är en sänka i Storbritannien. Den ligger i riksdelen England, i den södra delen av landet, 26 km väster om huvudstaden London. Kustklimat råder i trakten. Årsmedeltemperaturen i trakten är 11 °C. Den varmaste månaden är juni, då medeltemperaturen är 20 °C, och den kallaste är januari, med 2 °C. (sv) Ло́ндонский бассе́йн (Ло́ндонская ни́зменность; англ. London Basin) — низменная равнина на юго-востоке Великобритании, в нижнем течении Темзы. Лондонский бассейн представляет собой синклинальное понижение, сложенное палеогеновыми и неогеновыми глинами, песками и гравием. Высота достигает 100 м. Имеются небольшие массивы дубовых и буковых лесов, на песках — сосновые боры и верещатники на бурых лесных почвах. В основе — культурные ландшафты (поля, огороды, парки). На территории Лондонского бассейна расположен город Лондон. (ru) 倫敦盆地（London Basin）是以英國倫敦為中心的一個狹長、三角形的沉積盆地，除去大倫敦外，它還包括了東安格利亞東南部和英格蘭東南英格蘭的部分地區，最東端緊鄰北海。它形成于4000至6000万年前古近紀的阿尔卑斯造山运动時期。倫敦盆地主要由泰晤士河灌溉，但其面積並不完全重疊。 位于盆地中的大倫敦都會區有近1000万居民。 (zh) |
| rdfs:label | Bacino di Londra (it) Bassin de Londres (fr) London Basin (en) ロンドン盆地 (ja) Basen Londyński (pl) Лондонский бассейн (ru) London Basin (sv) 倫敦盆地 (zh) |
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