Mont Jinfo: diferència entre les revisions
Pàgina nova, amb el contingut: «{{Indret}} {{inacabat}} '''Jinfo Shan''' (''Golden Buddha Mountain'', Jinfoshan, Chin Shan, Jinfushan, Chin fu shan, chin fo shan, Chinese: 金佛山), the hi...». |
(Cap diferència)
|
Revisió del 16:59, 15 nov 2018
| ||||
| Tipus | Muntanya  | |||
|---|---|---|---|---|
| Part de | carst de la Xina meridional | |||
| Localització | ||||
| Entitat territorial administrativa | Nanchuan District (RP Xina) (en)  | |||
| ||||
| Serralada | Muntanyes Dalou | |||
| Dades i xifres | ||||
| Altitud | 2.238 m | |||
| Prominència | 2.238 m | |||
| Superfície | Patrimoni de la Humanitat: 6.744 ha zona tampó: 10.675 ha | |||
| Lloc component de Patrimoni de la Humanitat | ||||
| Tipus | Patrimoni natural | |||
| Data | 2014 (38a Sessió), Criteris PH: (vii), (viii) i (ix) | |||
| Identificador | 1248-004 | |||
| Candidat a Patrimoni de la Humanitat | ||||
| Data | 29 novembre 2001 | |||
| Identificador | 1624 | |||
 |
Aquest article o secció s'està elaborant i està inacabat. Un viquipedista hi està treballant i és possible que trobeu defectes de contingut o de forma. Comenteu abans els canvis majors per coordinar-los. Aquest avís és temporal: es pot treure o substituir per {{incomplet}} després d'uns dies d'inactivitat. |
Jinfo Shan (Golden Buddha Mountain, Jinfoshan, Chin Shan, Jinfushan, Chin fu shan, chin fo shan, Chinese: 金佛山), the highest peak of Dalou Mountains, located in the upper reach of the Yangtze River, is situated in Nanchuan District, the Municipality of Chongqing. Jinfo Shan és una muntanya aïllada amb cliffs up to 300 m surrounding its part superior relativament plana. Its major vegetation types include subtropical broadleaf forest, coniferous forests and subalpine meadow. Besides typical karst topography of gorges, stone forests and cave systems, Jinfo Shan és conegut per la seua excepcional diversitat de planes formada per 4768 seed plants.[1] També és un refugi per als animals en perill confinats a les karst regions com l'espècie Trachypithecus francoisi. Amb les its outstanding karst features i biodiversitat superba, Jinfo Shan ha sigut llistat com un possible Patrimoni Mundial des del 2001.[2]
Geografia
El Mont Jinfo és una syncline mountain. The platform and terrace are composed of Permian limestone in the upper part with about 2000m a.s.l. In the meanwhile, karst geomorphologies in large scale on the surface or underground are found. The shale and sandstone of Silurian lay in the middle of Jinfo from 1000m to 1500m asl.. The low part of Jinfo is supported by the limestone and dolomite of Cambrian and Ordovician. Plenty of small- and microforms of karst are formed in this area. There are many cliffs and gorges in Jinfo Mt., the north slope is steep and the south slope is slight. The geomorphology of the Jinfo can be divided into two types:
- Gorge in the low part of Jinfo Mt. whose elevation is about 800-1200m asl and relative height about 500m. It formed by water down cutting and eroding.
- Platform of Mid-mountain distributes the area above 1200m asl of Jinfo Mt., Bozhi Mt. and Qingba Mt.. The relative height is 500-1000m. The way of the mountain extension is identical to the tectonic line. The top of the Mts. is a relic erosional basis.[3]
Clima
It is in the subtropical humid monsoon zone with annual mean temperature of 8.2 °C and precipitation of 1,434.5 mm on the top of the mountain.[4]
Referències
- ↑ Yi, S.; Huang, Y.; Shen, M.; Xie, S; Liang, G. «Additions to the seed plants flora of Jinfo Mount. Nature Reserve in Chongqing.». Ecological Science, 26, 2007, pàg. 242–245.
- ↑ «Jinfushan Scenic Spot».
- ↑ Kuang, Mingsheng. «Karst Ecological System of Jinfo Mountain of Chongqing». [Consulta: 26 setembre 2011].
- ↑ Wu, Yuexia; Jiang, Yongjun; Yuan, Daoxian; Li, Linli «Modeling hydrological responses of karst spring to storm events: example of the Shuifang spring (Jinfo Mt., Chongqing, China)». Environ Geol, 55, 55, 2008, pàg. 1545–1553. DOI: 10.1007/s00254-007-1105-z.