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・ Big Belt Mountains
・ Big Belt National Forest
・ Big Ben
・ Big Ben (album)
・ Big Ben (comics)
・ Big Ben (disambiguation)
・ Big Ben (Heard Island)
・ Big Ben (horse)
・ Big Ben (locomotive)
・ Big Ben (solitaire)
・ Big Ben Aden
・ Big Ben Bolt
・ Big Ben Chor Praram 6
・ Big Ben Strikes Again
・ Big Bend
Big Bend (Florida)
・ Big Bend (Texas)
・ Big Bend Community College
・ Big Bend Country
・ Big Bend Cowboy Hall of Fame
・ Big Bend Dam
・ Big Bend gambusia
・ Big Bend Gold Rush
・ Big Bend Historical Area
・ Big Bend National Park
・ Big Bend of the Colorado State Recreation Area
・ Big Bend of the Columbia River
・ Big Bend Power Station
・ Big Bend Ranch State Park (Texas)
・ Big Bend Rancheria


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Big Bend (Florida) : ウィキペディア英語版
Big Bend (Florida)

The Big Bend region of Florida, U.S.A., is an informal region of the state with no official surveyed boundary. It generally includes the counties of the Florida Panhandle east of the Apalachicola River. The Big Bend Coast is the marshy coast without barrier islands that extends along the Gulf of Mexico coast of Florida from the Ocklockonee River to Anclote Key.
Private agencies that self-identify as serving the Big Bend region often include Franklin, Gadsden, Jefferson, Leon, Liberty, Madison, Taylor and Wakulla counties in their service areas.〔.〕〔(【引用サイトリンク】url=http://uwbb.org/counties/ )〕 The principal city in the region is Tallahassee.
The Big Bend Coast is the marshy coast extending about from the mouth of the Ocklockonee River around Apalachee Bay and down the west coast of peninsular Florida to Anclote Key. This stretch of coast includes the coasts of Wakulla, Jefferson, Taylor, Dixie, Levy, Citrus, Hernando and Pasco counties. The Big Bend Coast is a drowned karst region, covered with salt marsh. It includes freshwater springs, oyster reefs, and the delta of the Suwannee River. There are barrier islands west of the Oklockonee River and south starting with Anclote Key, but there are no barrier islands between those places. The Big Bend Coast has little or no sand or mud. The karst topography has produced an irregular, frequently exposed, bedrock surface. Due to the width of the adjacent continental shelf (over ), low gradient slope of the coast (1:5000), and shelter from the usual wind direction of storms, the Big Bend Coast is generally subject to low wave energy. The coast is subject to storm surges.〔.〕〔.〕
==See also==
Gulf Coastal Lowlands

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「Big Bend (Florida)」の詳細全文を読む



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