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・ Gulf of Argostoli
・ Gulf of Asinara
・ Gulf of Bahrain
・ Gulf of Batabanó
・ Gulf of Bomba
・ Gulf of Boni
・ Gulf of Boothia
・ Gulf of Bothnia
・ Gulf of Burgas
・ Gulf of California
・ Gulf of California moisture surge
・ Gulf of California Rift Zone
・ Gulf of California xeric scrub
・ Gulf of Carpentaria
・ Gulf of Catania
Gulf of Cazones
・ Gulf of Chania
・ Gulf of Chiriquí
・ Gulf of Corcovado
・ Gulf of Corinth
・ Gulf of Corinth basin
・ Gulf of Corryvreckan
・ Gulf of Cádiz
・ Gulf of Darién
・ Gulf of Euboea
・ Gulf of evaluation
・ Gulf of execution
・ Gulf of Fethiye
・ Gulf of Finland
・ Gulf of Finland Naval Command


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Gulf of Cazones : ウィキペディア英語版
Gulf of Cazones

Gulf of Cazones ((スペイン語:Golfo de Cazones)) is a large gulf in southern Cuba. It is located at the south by the provinces of Matanzas and Cienfuegos, between the northeast edge of the Jardinillos Bank on the south, and Piedras and other cays and reefs on the north. It is considered dangerous for sailing vessels to cross because of calms and cross currents.
==Geography==
Two miles east-northeast of the south point of Diego Perez Cay is the beginning of the northeast section of the Jardinillos (or Jardines) bank which continues to the southeast of East Rock. East Rock is situated approximately a cable from the northeast end of East Guano Cay, to which it is connected by a reef. This northern edge of the bank rises like a wall with one or two sandy patches on it above water. With Pedras Cays and the reefs on the north, it forms the Gulf of Cazones. A submerged platform, between 3 and 4 fathoms (5.5 to 7.3 metres) deep, exists between the Bay of Pigs, the Gulf of Cazones, the Gulf of Batabano, and the Isle of Pines. It is also inferred that the Gulf of Cazones may have been created due to a geological fault.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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