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

Key Biscayne (island) : ウィキペディア英語版
Key Biscayne

Key Biscayne is an island located in Miami-Dade County, Florida, United States, between the Atlantic Ocean and Biscayne Bay. It is the southernmost of the barrier islands along the Atlantic coast of Florida, and lies south of Miami Beach and southeast of Miami. The key is connected to Miami via the Rickenbacker Causeway, originally built in 1947.
The northern portion of Key Biscayne is home to Crandon Park, a county park. The middle section of the island consists of the incorporated Village of Key Biscayne. The southern part of the island is now protected as Bill Baggs Cape Florida State Park, adjacent to Biscayne National Park, one of the two national parks in Miami-Dade County.
==Geography==

Key Biscayne, although named a "key", is not geologically part of the Florida Keys, but is a barrier island composed of sand eroded from the Appalachian Mountains, carried to the coast by rivers and then moved along the coast from the north by coastal currents. There is no hard bedrock near the surface of the island, only layers of weak "shelly sandstone" to depths of or more.〔Blank. p. 150.〕 The coastal transport of sand southward ends at Key Biscayne. In the 1850s Louis Agassiz noted that "()outh of Cape Florida no more silicacious sand is to be seen."〔Blank. p. 75.〕 (The beaches in the Florida Keys, by contrast, consist primarily of finely pulverized shells.)〔Blank. p. 36.〕 Geologists believe that the island emerged around 2000 BCE, soon after the sea level stopped rising, as the sand built up to form new barrier islands on the southern Florida coast.〔Blank. p. 3.〕
Key Biscayne is elongated in the north-south direction, tapering to a point at each end. It is approximately long and to wide. The northern end of the island is separated from another barrier island, Virginia Key, by Bear Cut. The southern end of the island is Cape Florida. The Cape Florida Channel separates the island from the Safety Valve, an expanse of shallow flats cut by tidal channels that extends southward about to the Ragged Keys, at the northern end of the Florida Keys. Only Soldier Key, approximately 200 yards (200 m) by 100 yards wide (100 m), lies between Key Biscayne and the Ragged Keys.〔Voss, Gilbert L. and Nancy A. (1955) "An Ecological Survey of Soldier Key, Biscayne Bay, Florida," ''Bulletin of Marine Science of the Gulf and Caribbean.'' 5(3):203-29. Found at () URL retrieved December 12, 2010〕 The Cape Florida Channel (ten to eleven feet (to three-and-a-half meters ) deep in 1849) and Bear Cut (four feet (little more than one meter ) deep in 1849) are the deepest natural channels into Biscayne Bay. They provided the only access for ocean-going vessels to Biscayne Bay until artificial channels were dredged starting early in the 20th century. In 1849 the island had a fine sandy beach on the east side, and mangroves and lagoons on the west side.〔Blank. pp. 26, 63-68.〕 The average elevation of the island is less than five feet (1.5 m) above sea level.〔Blank. p. 172.〕
Key Biscayne is located at (25.690329, -80.165118).

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「Key Biscayne」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.