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The Bahamas is expected to be highly affected by sea level rise because at least 80% of the total land is below 10 meters elevation. [19] [20] As a small island developing state, the Bahamas is vulnerable to escalating disease outbreaks, and climate change could affect the seasonality of outbreaks and transmission of disease. [21]
This channel and the Providence Channels are the two main branches of the Great Bahama Canyon, a submerged geological feature formed by erosion during periods of lower sea level. During their early history the Tongue of the Ocean and the Providence Channel were broad, relatively shallow basins flanked by growing carbonate banks. As the Blake ...
The Blake Basin, also called the Blake–Bahama Basin, is a deep area of the Atlantic Ocean which runs along the east coast of the United States.It starts at the northern part of the Bahamas and continues up toward New York.
The slopes around them however, such as the border of the Tongue of the Ocean in the Great Bahama Bank, are very steep. The Banks were dry land during past ice ages, when sea level was as much as 120 meters (390 feet) lower than at present; the land area of the Bahamas today thus represents only a small fraction of their prehistoric extent.
Geography Now (also stylized as Geography Now!) is an American educational YouTube channel and web series created and hosted by Paul Barbato. It profiles UN-recognized countries in the world in alphabetical order and covers additional topics related to physical and political geography. The channel was started in August 2014 and has gained over ...
Atlantic Ocean North Atlantic Ocean. Caribbean. West Indies. Lucayan Archipelago; Time zone: Eastern Standard Time , Eastern Daylight Time ; Extreme points of the Bahamas High: Mount Alvernia on Cat Island 63 m (207 ft) Low: North Atlantic Ocean 0 m; Land boundaries: none; Coastline: North Atlantic Ocean 3,542 km
The Bahamas as seen from space. The egress of the Great Bahama Canyon into the Atlantic Ocean is the dark blue channel at upper center.. The Great Bahama Canyon is a V-shaped [1] submarine canyon system in the Bahamas that cuts between the Abaco Islands to the north and Eleuthera island to the south.
Abyssal Zone: Beneath the thermocline is the deep ocean or abyssal zone, where temperatures remain relatively uniform, hovering just above freezing (0°-3°C). This cold, dense water originates from polar regions, where surface water cools, sinks, and spreads towards the equator along the ocean floor, forming the deep ocean circulation system.