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Neblina massif : ウィキペディア英語版
Cerro de la Neblina

Cerro de la Neblina (lit. "Mountain of the Mist"〔Myers, C.W., E.E. Williams & R.W. McDiarmid (9 September 1993). (A new anoline lizard (''Phenacosaurus'') from the highland of Cerro de la Neblina, southern Venezuela ). ''American Museum Novitates'', no. 3070: 1–15.〕), also known as Serra da Neblina in Brazil〔 Cronemberger, F.M., P. Wallace, E. Bertold, R.R. de Oliveira & J. Bastos (2007). In: ''Anais do VIII Congresso de Ecologia do Brasil, 23 a 28 de Setembro de 2007, Caxambu - MG''. Sociedade de Ecologia do Brasil.〕 and Sierra de la Neblina in Venezuela,〔 is a sandstone massif located in the northern Amazon Basin. It is a tilted, heavily eroded plateau, with a deep canyon in its central portion (Cañón Grande), drained by the Baria River. The southeastern ridge of the massif forms part of the Brazil–Venezuela border, and it is where the massif reaches its highest elevation, the Pico da Neblina in Brazilian territory. At above sea level,〔() (13 September 2004). (Four Brazilian peaks have their altitude changed ). Instituto Brasileiro de Geografia e Estatística.〕 this is the highest mountain of the entire Guayana Shield.〔 The slightly shorter Pico 31 de Março / Pico Phelps lies a few hundred metres away on the border itself and is Brazil's second-highest mountain, and the highest mountain in Venezuela outside of the Andes. The massif's other named peaks include Pico Cardona, Pico Maguire, and Pico Zuloaga.〔〔 Brewer-Carías, C. (2012–2013). ''Río Verde'' 9: 73–88.〕 To the north of Cerro de la Neblina lie the smaller outcrops of Cerro Aracamuni and Cerro Avispa, both reaching approximately in elevation.〔Huber, O. (1995). Geographical and physical features. In: P.E. Berry, B.K. Holst & K. Yatskievych (eds.) ''Flora of the Venezuelan Guayana. Volume 1. Introduction.'' Missouri Botanical Garden Press, St. Louis. pp. 1–61.〕
The massif was first explored in 1954 by an American expedition led by Bassett Maguire that performed an aerial inspection and then climbed the massif's northwestern slopes.〔Maguire, B. (January 1955). Cerro de la Neblina, Amazonas, Venezuela: a newly discovered sandstone mountain. ''Geographical Review'' 45(1): 27–51. 〕〔Maguire, B. & J.J. Wurdack (October 1959). The position of Cerro de la Neblina, Venezuela. () In: Geographical record. ''Geographical Review'' 49(4): 563–588. 〕〔 Brewer-Carías, C. (2011–2012). (La Neblina: el tepuy más alto y remoto ). ''Río Verde'' 6: 61–74.〕 In January 1999, a group of carnivorous plant enthusiasts climbed Pico da Neblina following a 30 km hike up the previously unexplored northeastern ridge.〔Rivadavia, F. (December 1999). (Neblina expedition. ) ''Carnivorous Plant Newsletter'' 28(4): 122–124.〕
Cerro de la Neblina is sometimes referred to as the Neblina Massif,〔McPherson, S., A. Wistuba, A. Fleischmann & J. Nerz (2011). ''Sarraceniaceae of South America''. Redfern Natural History Productions, Poole.〕〔Carvalho, F.A., A. Salino & C.E. Zartman (July 2012). New country and regional records from the Brazilian side of Neblina Massif. ''American Fern Journal'' 102(3): 228–232. 〕 though this term may also encompass Cerro Aracamuni and Cerro Avispa (a grouping of mountains more precisely known as the Neblina–Aracamuni Massif).〔 The Neblina–Aracamuni Massif has a total summit area of roughly and an estimated slope area of , of which Cerro de la Neblina accounts for and , respectively.〔
==See also==

* Distribution of ''Heliamphora''
* Neblina uakari
* Pico da Neblina National Park

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