翻訳と辞書
Words near each other
・ "O" Is for Outlaw
・ "O"-Jung.Ban.Hap.
・ "Ode-to-Napoleon" hexachord
・ "Oh Yeah!" Live
・ "Our Contemporary" regional art exhibition (Leningrad, 1975)
・ "P" Is for Peril
・ "Pimpernel" Smith
・ "Polish death camp" controversy
・ "Pro knigi" ("About books")
・ "Prosopa" Greek Television Awards
・ "Pussy Cats" Starring the Walkmen
・ "Q" Is for Quarry
・ "R" Is for Ricochet
・ "R" The King (2016 film)
・ "Rags" Ragland
・ ! (album)
・ ! (disambiguation)
・ !!
・ !!!
・ !!! (album)
・ !!Destroy-Oh-Boy!!
・ !Action Pact!
・ !Arriba! La Pachanga
・ !Hero
・ !Hero (album)
・ !Kung language
・ !Oka Tokat
・ !PAUS3
・ !T.O.O.H.!
・ !Women Art Revolution


Dictionary Lists
翻訳と辞書 辞書検索 [ 開発暫定版 ]
スポンサード リンク

Ubinas Volcano : ウィキペディア英語版
Ubinas

Ubinas is an active stratovolcano in the Andes of southern Peru. Until 2006, this stratovolcano had not erupted for about 40 years.
==Description==
Ubinas is located in southern Peru. The upper slopes of the volcano, composed primarily of Pleistocene andesitic lava flows, steepen to nearly 45 degrees. The steep-walled, 1.4 km wide and 150 m deep summit caldera contains an ash cone with a 500-m-wide funnel-shaped vent that is 200 m deep. Debris-avalanche deposits from the collapse of the SE flank of Ubinas extend 10 km from the volcano.
The volcano is a composite cone built on a high plateau formed from Oligocene-Miocene (Neogene) ignimbrites and intrusive rocks. Ubinas comprises two edifices that divide two major periods of its eruptive behaviour. The first is the lower volcano under 600 m high called Ubinas 1 (eruptive period >376 ka), which collapsed and formed a debris-avalanche deposit as far as 12 km downstream Rio Ubinas. This collapse was followed by an eruption of non-welded ignimbrites, ponding to a thickness of 150 m over 5 km from the summit, and in turn was covered by a 100 m thick ash/pumice deposit. Ubinas 1 is overlain by a steeper cone more than 900 m high called Ubinas 2 (eruptive period <376 ka). Ubinas 2 formed the summit caldera, with walls up to 300 m high that consist of hydrothermally altered lava flows and floored by a 20 m thick pile of lapilli and ash-fall layer. This morphology was created by frequent eruptions in the Late Holocene from the younger inner crater. The inner crater is under 200 m high and shows pervasive hydrothermal alteration and abundant fractures. Countless explosive events have taken place inside the summit caldera during the last 9.7 ky, and it has been suggested by Thouret et al. that the caldera be considered gravitationally unstable.〔Thouret et al., 2005, Ubinas: the evolution of the historically most active volcano in southern Peru., Bull Volcanol, 67, p. 557-589〕

Image:Ubinas ash cloud - ISS.jpg|Ash cloud from Ubinas, viewed from the ISS, 14 August 2006
Image:Ubinas Volcano, Peru.jpg|True-colour satellite image of Ubinas


抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Ubinas」の詳細全文を読む



スポンサード リンク
翻訳と辞書 : 翻訳のためのインターネットリソース

Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.