Teluk Fundy: Perbedaan antara revisi
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{{Infobox body of water
| name = Teluk Fundy
| native_name =
| native_name_lang =
| other_name = The Bay of Fundy, Baie de Fundy
<!-- Images -->
| image = Image:Wpdms nasa topo bay of fundy - en.jpg
| alt =
| caption = Teluk Fundy
| image_bathymetry =
| alt_bathymetry =
| caption_bathymetry =
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| location = [[New Brunswick]], [[Nova Scotia]], [[Maine]]
| group =
| coordinates = {{Coord|45|00|N|65|45|W|scale:2000000|display=inline,title}}
| type = [[Estuari]]
| etymology = Kemungkinan besar dari Bahasa Prancis ''Fendu'', yang bermakna "membagi".
| part_of =
| inflow =
| outflow = [[Teluk Maine]]
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| date-built = <!-- {{Start date|YYYY|MM|DD}} For man-made and other recent bodies of water -->
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| date-flooded = <!-- {{Start date|YYYY|MM|DD}} For man-made and other recent bodies of water -->
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| max-depth = <!-- {{convert|VALUE|UNITS}} must be used -->
| volume = <!-- {{convert|VALUE|UNITS}} must be used -->
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| elevation = <!-- {{convert|VALUE|UNITS}} must be used -->
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| temperature_low = <!-- {{convert|VALUE|UNITS}} must be used -->
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| image_map =
| caption_map =
|pushpin_map=Nova Scotia
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| website =
| reference = {{Designation list
| embed = yes
| designation1 =
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}}}}
[[Berkas:Ddfrrs.jpg |jmpl|ka|250px|Teluk Fundy.]]
'''Teluk Fundy''' adalah [[teluk]] yang terletak di [[Pantai]] [[Timur]] [[Kanada]] yang membentang dari [[pantai]] [[utara]] [[Maine]] ke [[Kanada]] antara [[New Brunswick]] dan [[Nova Scotia]]. Teluk ini mempunyai luas sebesar 270 km².<ref>{{en}} Yeo, R.K, Risk, M.J., 1981, The sedimentology, stratigraphy, and preservation of intertidal deposits in the Minas Basin System, Bay of Fundy: Journal of Sedimentary Petrology, v. 51, p. 245-260.</ref> Selain itu, teluk ini mempunyai selisih [[air]] pasang surut 16,2 meter, yang paling tinggi di [[dunia]]. Sebanyak 100 juta kubik air [[laut]] mengalir masuk dan keluar ke dalam teluk ini setiap terjadi pasang surut dalam rentang waktu sekitar 6 jam.<ref>{{en}} Klein, G.D., 1963, Bay of Fundy intertidal zone sediments: Journal of Sedimentary Petrology, v. 33, p. 844-854.</ref>
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