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

Faial Channel : ウィキペディア英語版
Faial-Pico Channel

The Faial-Pico Channel ((ポルトガル語:Canal Faial-Pico)) is an long channel that separates the islands of Faial and Pico in the central group of the archipelago of the Azores. The strait is divided into various depressions, calderas and micro-systems, referred to as ''Baixas''.
==Geography==

The Baixa do Norte is located from ''Ponta da Espalamaca'', at a depth of approximately , to a depth reaching below sea level.〔 The leading edge of the ''Baixa do Norte'' reef includes a series of large rocky outcrops, of less than in size. Considered a minor reef, the ''Baixa do Norte'' has been used by some fishers, who extended their catches from the ''Baixa da Barca''.〔 The ''Baixa'' is characterized by peaks at the depth, with large blocks of rock and a fishery of considerable dimension. In comparison, the southern margins is characterized by peaks to about consisting of peaks and valleys.〔
The southern or Baixa do Sul is a meridianal reef situated southeast of the port of Horta.〔 It is located approximately below sea level. The entire channel is distinguished by geological structures, including two sub-aquatic caldeiras, between diametre.〔
Until about below sea level, the area is dominated by extensive uninterrupted boulders, with a terrain that is rugged and divided by metres. Some of these cassums are broken by abrasive calderas, formed from large boulders grinding into the reef floor. These ''covas de gigante'' (''giant holes''), some deep and diameters that permit movement.

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「Faial-Pico Channel」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.