47
edits
Changes
Jump to navigation
Jump to search
created, to support Pensacola beach/storm topics
[[Image:GulfofMexico3D.png|thumb|right|300px|Gulf of Mexico in 3D perspective.]]
The '''Gulf of Mexico''' is the ninth largest [[body of water]] in the world. It is an ocean basin largely surrounded by the [[North America]]n continent and the island of [[Cuba]]. It is bounded on the northeast, north and northwest by the [[Gulf Coast of the United States]], on the southwest and south by [[Mexico]], and on the southeast by [[Cuba]]. The shape of its basin is roughly circular and approximately 810 [[nautical mile]]s (1,500 km) wide and filled with of sedimentary rocks and debris. It connects with the [[Atlantic Ocean]] through the [[Florida Straits]] between the U.S. and Cuba, and with the [[Caribbean Sea]] (with which it forms the [[mediterranean sea (oceanography)|American Mediterranean Sea]]) via the [[Yucatan Channel]] between Mexico and Cuba. [[Tides|Tidal ranges]] are extremely small due to the narrow connection with the ocean.
The gulf basin is approximately 615,000 [[square mile|mi²]] (1.6 million km²). Almost half of the basin is shallow intertidal waters. At its deepest it is 14,383 ft (4,384 m) at the [[Sigsbee Deep]], an irregular trough more than 300 [[nautical mile]]s (550 km) long.
It was probably formed approximately 300 million years ago as a result of the seafloor sinking.<ref name="epa">{{cite web
|url=http://www.epa.gov/gmpo/about/facts.html
|title=General Facts about the Gulf of Mexico
|publisher=
|accessdate=2006-12-27
}}</ref> There is evidence that the [[Chicxulub Crater]] was formed when a large [[meteorite]] hit the earth 65 million years ago which may have impacted the [[extinction of the dinosaurs]].<ref>{{cite web | url=http://web.ukonline.co.uk/a.buckley/dino.htm | title=Dinosaur Extinction Page | first=A. | last=Buckley | year=1997}}</ref>
==Principal features==
[[Image:Wide natural beach near Sabine Pass.jpg|thumb|left|300px|Gulf beach near Sabine Pass.]]
The Gulf of Mexico's eastern, north, and northwestern shores lie along the US states of [[Florida]], [[Alabama]], [[Mississippi]], [[Louisiana]], and [[Texas]]. This coastline spans 1,630 miles, receiving water from thirty-three major rivers that drain 31 states.<ref>{{cite web
|url=http://www.epa.gov/water/waterplan/documents/05guidance.htm#gulf
|title= National Water Program Guidance: FY 2005
|publisher=epa.gov
|accessdate=2007-01-21
}}</ref> The Gulf's southwestern and southern shores lie along the [[Mexican]] states of [[Tamaulipas]], [[Veracruz]], [[Tabasco]], [[Campeche]], [[Yucatán]], and the northernmost tip of [[Quintana Roo]]. On the southeast it is bordered by [[Cuba]]. It supports major American, Mexican and Cuban fishing industries. The outer margins of the wide continental shelves of Yucatán and Florida receive cooler, [[nutrient]]-enriched waters from the deep by a process known as [[upwelling]], which stimulates plankton growth in the [[euphotic zone]]. This attracts fish, shrimp, and squid. <ref>{{cite web | url=http://www.tsha.utexas.edu/handbook/online/articles/GG/rrg7.html | title=GULF OF MEXICO | work=Handbook of Texas Online | publisher=Texas State Historical Association}}</ref>. River drainage and atmospheric fallout from industrial coastal cities also provide nutrients to the coastal zone.
The [[Gulf Stream]], a warm Atlantic Ocean current and one of the strongest [[ocean current]]s known, originates in the gulf, as a continuation of the [[Caribbean Current]]-Yucatán Current-[[Loop Current]] system. Other circulation features include the anticyclonic [[gyre]]s which are shed by the [[Loop Current]] and travel westward where they eventually dissipate, and a permanent cyclonic [[gyre]] in the [[Bay of Campeche]]. The [[Bay of Campeche]] in Mexico constitutes a major arm of the Gulf of Mexico. Additionally, the gulf's shoreline is fringed by numerous bays and smaller inlets. A number of rivers empty into the gulf, most notably the [[Mississippi River]] in the northern gulf, and the [[Grijalva]] and [[Usumacinta]] Rivers in the southern gulf. The land that forms the gulf's coast, including many long, narrow barrier islands, is almost uniformly low-lying and is characterized by marshes and swamps as well as stretches of sandy beach.
The [[continental shelf]] is quite wide at most points along the coast, most notably at the Florida and [[Yucatán Peninsula]]s. The shelf is exploited for its [[petroleum|oil]] by means of offshore drilling rigs, most of which are situated in the western gulf and in the [[Bay of Campeche]]. Another important commercial activity is fishing; major catches include red snapper, amberjack, tilefish, swordfish, and various grouper, as well as shrimp and crabs. Oysters are also harvested on a large scale from many of the bays and sounds. Other important industries along the coast include shipping, petrochemical processing and storage, military use, paper manufacture, and tourism.
[[Image:GulfMexTemps 2005Hurricanes.gif|thumb|300px|Graph showing the overall water temperature of the Gulf between Hurricanes [[Hurricane Katrina|Katrina]] and [[Hurricane Rita|Rita]]. Although Katrina cooled waters in its path by up to 4°C, they had rebounded by the time of Rita's appearance.]]
The gulf's warm water temperature can feed powerful Atlantic [[hurricane]]s causing extensive human death and other destruction as happened with [[Hurricane Katrina]] in 2005. In the Atlantic, a hurricane will draw up cool water from the depths and making it less likely that further hurricanes will follow in its wake (warm water being one of the preconditions necessary for their formation). However, the Gulf is shallower and its entire water column is warm. When a hurricane passes over, although the water temperature may drop it soon rebounds and becomes capable of supporting another tropical storm.<ref>{{cite web | url=http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=17038 | title=Warm Waters Provide Fuel for Potential Storms | publisher=[[NASA Earth Observatory]] | accessdate=2006-05-05}}</ref>
The Gulf is considered [[aseismic]]: however, mild tremors have been recorded throughout history (usually 5.0 or less on the [[Richter scale]]). A 6.0 tremor was recorded on [[September 10]], [[2006]], 250 miles off the coast of [[Florida]] which caused no damage, but could be felt throughout the [[Southeastern United States]]. No damage or injuries were reported.<ref>{{cite web
|url=http://www.wftv.com/news/9817047/detail.html
|title=Central Florida Feels Quake
|publisher=
|accessdate=2006-12-27
}}</ref>
Earthquakes such as this may be caused by interactions between sediment loading on the sea floor and adjustment by the crust.<ref>{{cite web
|url=http://www.clas.ufl.edu/users/russo/florida_eq.html
|title=Earthquakes in the Gulf of Mexico
|publisher=
|accessdate=2006-12-27
}}</ref>
==Pollution==
Because of the ever increasing amount of [[nitrogen]] and [[phosphate]]s dissolved in the waters of the Gulf of Mexico, pollution has more than doubled since 1950. Current estimates suggest that three times as much nitrogen is being carried into the Gulf today compared with levels 30 years ago or at any time in history in the water. Every summer there is now an area south of the Louisiana coastline, larger than the [[U.S. state]] of [[Massachusetts]] at over 7,000 mi² (18,000 km²) that is [[hypoxia (environmental)|hypoxic]]. These waters do not carry enough oxygen to sustain marine life. This annually enlarging [[dead zone (ecology)|dead zone]] is a major threat to the fishing industry and to public health.
[[Image:Fishing Fleet in Biloxi.jpg|thumb|3000px|right|Fishing boats in Biloxi]]Also, there are frequent "[[red tide]]" algae blooms<ref>{{cite web
|url=http://www.tulane.edu/~bfleury/envirobio/enviroweb/DeadZone.htm
|title=The Gulf of Mexico Dead Zone and Red Tides
|publisher=
|accessdate=2006-12-27
}}</ref> that kill fish and marine mammals and cause respiratory problems in humans and some domestic animals when the blooms reach close to shore. This has especially been plaguing the southwest Florida coast, from the [[Florida Keys]] to north of [[Pasco County, Florida]].
==See also==
*[[Charlotte Harbor (estuary)|Charlotee Harbor Estuary, Florida]]
*[[Coastal Ecosystems in Florida]]
==References==
<div class="references-small">
<references />
</div>
==External links==
*[http://www.observernews.net/artman/publish/article_001724.shtml 6.0 Earthquake reported on 9-10-2006]
*[http://www.gsajournals.org/gsaonline/?request=get-abstract&doi=10.1130%2F0091-7613(1982)10%3C103:SOTCGO%3E2.0.CO%3B2 GSA article on Gulf seismic activity from 1982]
*[http://www.epa.gov/water/yearofcleanwater/docs/Hypoxia_Factsheet.pdf EPA factsheet on hypoxia]
*[http://www.ncat.org/nutrients/hypoxia/hypoxia.html Gulf of Mexico hypoxia]
*[http://gulfsci.usgs.gov/ Gulf of Mexico Integrated Science]
==Gallery==
<center><gallery>
Image:Katrina-14628.jpg|[[Hurricane Katrina]] on Gulf Coast.
Image:gulf-mexico-watershed.gif|[[Mississippi river]] watershed.
Image:GulfOfMexicoBeach.jpg|Gulf of Mexico beach.
</gallery></center>
{{coor title dms|25|22|07|N|90|23|26|W|type:waterbody}}
[[Category:Gulf of Mexico| ]]
The '''Gulf of Mexico''' is the ninth largest [[body of water]] in the world. It is an ocean basin largely surrounded by the [[North America]]n continent and the island of [[Cuba]]. It is bounded on the northeast, north and northwest by the [[Gulf Coast of the United States]], on the southwest and south by [[Mexico]], and on the southeast by [[Cuba]]. The shape of its basin is roughly circular and approximately 810 [[nautical mile]]s (1,500 km) wide and filled with of sedimentary rocks and debris. It connects with the [[Atlantic Ocean]] through the [[Florida Straits]] between the U.S. and Cuba, and with the [[Caribbean Sea]] (with which it forms the [[mediterranean sea (oceanography)|American Mediterranean Sea]]) via the [[Yucatan Channel]] between Mexico and Cuba. [[Tides|Tidal ranges]] are extremely small due to the narrow connection with the ocean.
The gulf basin is approximately 615,000 [[square mile|mi²]] (1.6 million km²). Almost half of the basin is shallow intertidal waters. At its deepest it is 14,383 ft (4,384 m) at the [[Sigsbee Deep]], an irregular trough more than 300 [[nautical mile]]s (550 km) long.
It was probably formed approximately 300 million years ago as a result of the seafloor sinking.<ref name="epa">{{cite web
|url=http://www.epa.gov/gmpo/about/facts.html
|title=General Facts about the Gulf of Mexico
|publisher=
|accessdate=2006-12-27
}}</ref> There is evidence that the [[Chicxulub Crater]] was formed when a large [[meteorite]] hit the earth 65 million years ago which may have impacted the [[extinction of the dinosaurs]].<ref>{{cite web | url=http://web.ukonline.co.uk/a.buckley/dino.htm | title=Dinosaur Extinction Page | first=A. | last=Buckley | year=1997}}</ref>
==Principal features==
[[Image:Wide natural beach near Sabine Pass.jpg|thumb|left|300px|Gulf beach near Sabine Pass.]]
The Gulf of Mexico's eastern, north, and northwestern shores lie along the US states of [[Florida]], [[Alabama]], [[Mississippi]], [[Louisiana]], and [[Texas]]. This coastline spans 1,630 miles, receiving water from thirty-three major rivers that drain 31 states.<ref>{{cite web
|url=http://www.epa.gov/water/waterplan/documents/05guidance.htm#gulf
|title= National Water Program Guidance: FY 2005
|publisher=epa.gov
|accessdate=2007-01-21
}}</ref> The Gulf's southwestern and southern shores lie along the [[Mexican]] states of [[Tamaulipas]], [[Veracruz]], [[Tabasco]], [[Campeche]], [[Yucatán]], and the northernmost tip of [[Quintana Roo]]. On the southeast it is bordered by [[Cuba]]. It supports major American, Mexican and Cuban fishing industries. The outer margins of the wide continental shelves of Yucatán and Florida receive cooler, [[nutrient]]-enriched waters from the deep by a process known as [[upwelling]], which stimulates plankton growth in the [[euphotic zone]]. This attracts fish, shrimp, and squid. <ref>{{cite web | url=http://www.tsha.utexas.edu/handbook/online/articles/GG/rrg7.html | title=GULF OF MEXICO | work=Handbook of Texas Online | publisher=Texas State Historical Association}}</ref>. River drainage and atmospheric fallout from industrial coastal cities also provide nutrients to the coastal zone.
The [[Gulf Stream]], a warm Atlantic Ocean current and one of the strongest [[ocean current]]s known, originates in the gulf, as a continuation of the [[Caribbean Current]]-Yucatán Current-[[Loop Current]] system. Other circulation features include the anticyclonic [[gyre]]s which are shed by the [[Loop Current]] and travel westward where they eventually dissipate, and a permanent cyclonic [[gyre]] in the [[Bay of Campeche]]. The [[Bay of Campeche]] in Mexico constitutes a major arm of the Gulf of Mexico. Additionally, the gulf's shoreline is fringed by numerous bays and smaller inlets. A number of rivers empty into the gulf, most notably the [[Mississippi River]] in the northern gulf, and the [[Grijalva]] and [[Usumacinta]] Rivers in the southern gulf. The land that forms the gulf's coast, including many long, narrow barrier islands, is almost uniformly low-lying and is characterized by marshes and swamps as well as stretches of sandy beach.
The [[continental shelf]] is quite wide at most points along the coast, most notably at the Florida and [[Yucatán Peninsula]]s. The shelf is exploited for its [[petroleum|oil]] by means of offshore drilling rigs, most of which are situated in the western gulf and in the [[Bay of Campeche]]. Another important commercial activity is fishing; major catches include red snapper, amberjack, tilefish, swordfish, and various grouper, as well as shrimp and crabs. Oysters are also harvested on a large scale from many of the bays and sounds. Other important industries along the coast include shipping, petrochemical processing and storage, military use, paper manufacture, and tourism.
[[Image:GulfMexTemps 2005Hurricanes.gif|thumb|300px|Graph showing the overall water temperature of the Gulf between Hurricanes [[Hurricane Katrina|Katrina]] and [[Hurricane Rita|Rita]]. Although Katrina cooled waters in its path by up to 4°C, they had rebounded by the time of Rita's appearance.]]
The gulf's warm water temperature can feed powerful Atlantic [[hurricane]]s causing extensive human death and other destruction as happened with [[Hurricane Katrina]] in 2005. In the Atlantic, a hurricane will draw up cool water from the depths and making it less likely that further hurricanes will follow in its wake (warm water being one of the preconditions necessary for their formation). However, the Gulf is shallower and its entire water column is warm. When a hurricane passes over, although the water temperature may drop it soon rebounds and becomes capable of supporting another tropical storm.<ref>{{cite web | url=http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=17038 | title=Warm Waters Provide Fuel for Potential Storms | publisher=[[NASA Earth Observatory]] | accessdate=2006-05-05}}</ref>
The Gulf is considered [[aseismic]]: however, mild tremors have been recorded throughout history (usually 5.0 or less on the [[Richter scale]]). A 6.0 tremor was recorded on [[September 10]], [[2006]], 250 miles off the coast of [[Florida]] which caused no damage, but could be felt throughout the [[Southeastern United States]]. No damage or injuries were reported.<ref>{{cite web
|url=http://www.wftv.com/news/9817047/detail.html
|title=Central Florida Feels Quake
|publisher=
|accessdate=2006-12-27
}}</ref>
Earthquakes such as this may be caused by interactions between sediment loading on the sea floor and adjustment by the crust.<ref>{{cite web
|url=http://www.clas.ufl.edu/users/russo/florida_eq.html
|title=Earthquakes in the Gulf of Mexico
|publisher=
|accessdate=2006-12-27
}}</ref>
==Pollution==
Because of the ever increasing amount of [[nitrogen]] and [[phosphate]]s dissolved in the waters of the Gulf of Mexico, pollution has more than doubled since 1950. Current estimates suggest that three times as much nitrogen is being carried into the Gulf today compared with levels 30 years ago or at any time in history in the water. Every summer there is now an area south of the Louisiana coastline, larger than the [[U.S. state]] of [[Massachusetts]] at over 7,000 mi² (18,000 km²) that is [[hypoxia (environmental)|hypoxic]]. These waters do not carry enough oxygen to sustain marine life. This annually enlarging [[dead zone (ecology)|dead zone]] is a major threat to the fishing industry and to public health.
[[Image:Fishing Fleet in Biloxi.jpg|thumb|3000px|right|Fishing boats in Biloxi]]Also, there are frequent "[[red tide]]" algae blooms<ref>{{cite web
|url=http://www.tulane.edu/~bfleury/envirobio/enviroweb/DeadZone.htm
|title=The Gulf of Mexico Dead Zone and Red Tides
|publisher=
|accessdate=2006-12-27
}}</ref> that kill fish and marine mammals and cause respiratory problems in humans and some domestic animals when the blooms reach close to shore. This has especially been plaguing the southwest Florida coast, from the [[Florida Keys]] to north of [[Pasco County, Florida]].
==See also==
*[[Charlotte Harbor (estuary)|Charlotee Harbor Estuary, Florida]]
*[[Coastal Ecosystems in Florida]]
==References==
<div class="references-small">
<references />
</div>
==External links==
*[http://www.observernews.net/artman/publish/article_001724.shtml 6.0 Earthquake reported on 9-10-2006]
*[http://www.gsajournals.org/gsaonline/?request=get-abstract&doi=10.1130%2F0091-7613(1982)10%3C103:SOTCGO%3E2.0.CO%3B2 GSA article on Gulf seismic activity from 1982]
*[http://www.epa.gov/water/yearofcleanwater/docs/Hypoxia_Factsheet.pdf EPA factsheet on hypoxia]
*[http://www.ncat.org/nutrients/hypoxia/hypoxia.html Gulf of Mexico hypoxia]
*[http://gulfsci.usgs.gov/ Gulf of Mexico Integrated Science]
==Gallery==
<center><gallery>
Image:Katrina-14628.jpg|[[Hurricane Katrina]] on Gulf Coast.
Image:gulf-mexico-watershed.gif|[[Mississippi river]] watershed.
Image:GulfOfMexicoBeach.jpg|Gulf of Mexico beach.
</gallery></center>
{{coor title dms|25|22|07|N|90|23|26|W|type:waterbody}}
[[Category:Gulf of Mexico| ]]
