The Atlantic Ocean is a vin. Atlantic Ocean: characteristics behind the plan Kursi geography. Why are leaks established

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The Atlantic Ocean gives way to the Pacific Ocean, and its area becomes approximately 91.56 million km². In other oceans, there is a strong porosity of the coastline, which establishes the abundance of the sea and inflows, especially near the pivnichny part. In addition, the total area of the basins of the rivers, which flow into the whole ocean or the south margin of the sea, is much larger, lower by the river, which flows into the other ocean. Another view of the Atlantic Ocean is a small number of islands and a foldable bottom relief, like winds under the water ridges and bottoms, making impersonal okremikh ugolovins.

Pivnichna part of the Atlantic Ocean

Cordoni and coastline. The Atlantic Ocean is divided into pivnіchnu and pivdennu parts, between them it is smart to draw beyond the equator. From the oceanographic point of the dawn, however, up to the main part of the ocean, one can see the equatorial leak, which expands by 5-8 ° m.l. Pivnіchny cordon sings to be held behind the Pivnіchny Polar stake. The cities of this cordon are marked by underwater ridges.

At Pivnichniy pivkul, the Atlantic Ocean can be heavily damaged by the coastline. It is clearly visible that the narrow part of the Pivnichna part of the river crosses the Pivnichniy Ilodovity Ocean with narrow channels. At the Pivnichny descent of the Devisov Protoka with a width of 360 km (at the latitude of the Pivnichny Polar Kol) behind the Baffin Sea, which can be seen up to Pivnichny ice-cold ocean. In the central part, between Greenland and Iceland, there is the Danish duct, the width of which is 287 km from the navigable area. Nareshti, at the pivnіchny descent, between Iceland and Norway, the Norwegian sea is spread out with a width of bl. 1220 km. At the exit of the Atlantic Ocean there are two water areas that go deep into the land. The greater pіvnіchna їх are initiated by the Pіvnіchnіm sea, yak to cross at the Baltic Sea with the Bothnian and Finnish inflows. On pіvden є system vnutr_shnyokontinentalnyh morіv - Seredzemny and Chorny - zagalnoy dozhina bl. 4000 km. At Gibraltar protoci, which connects the ocean from the Mediterranean Sea, there is one under one two parallel flow. The lower position is occupied by the flow, which is direct from the Mediterranean Sea to the Atlantic Ocean, the shards of the Mediterranean waters due to the more intensive evaporation from the surface are characterized by greater salinity, and also, by greater thickness.

Near the tropical zone, at the natural entrance of the Pivnichnaya Atlantic, the Caribbean Sea and the Mexican Influx, which crosses the ocean with the Florida Channel, are roamed. The coast of Pivnichnoy America is cut by small streams (Pamliko, Barnegat, Chesapeake, Delaware and the Long Island channel); on the pivnіchny entrance there are the streams of the Funda St. Lawrence, the Belle Isle channel, the Hudson channel and the Hudson creek.

The largest islands are in the middle of the peninsula part of the ocean; the British Isles, Iceland, Newfoundland, Cuba, Haiti (Hispaniola) and Puerto Rico. On the outskirts of the Atlantic Ocean there are a few groups of small islands - Azores, Canaries, Green Misu. Similar groups to the western part of the ocean. As a butt, you can show the islands of Bahamas, Florida Keys and Mali Antilles. The archipelagos of the Great and Lesser Antilles islands form an island arc, which is a part of the Caribbean Sea. Near the Pacific Ocean, arcs similar to islands are adjacent to areas of deformation of the earth's crust. Uzdovzh swollen sides of the arc are ripped deep water zholobi.

The basin of the Atlantic Ocean is developed by a shelf, the width of which varies. The shelf breaks deep gorges - tz. underwater canyons. Їхнє pojennya dosi vikkaє superechki. According to one theory, the canyons were pierced by small rivers, if the river was lower than the ocean. Another theory shows the molding of the diyalnistyu of turbid flows. It was allowed to let go, that muddy flows were the main agent, that deposited water on the days of the ocean and that the stench cut through the underwater canyons.

The bottom of the peninsular part of the Atlantic Ocean has a folded overturned relief, shelters along the bottom of the underwater ridges, hillocks, hollows and gorges. Most of the ocean floor, from a depth of approximately 60 m and up to a few kilometers, is covered with thin mulish deposits of dark blue or black-green color. Visibly a small area is occupied by skelnі vihodi and dilyanki of gravel-pebble and pishchanykh vіdkladen, as well as deep-water red clay.

Telephone and telegraph cables were laid on the shelf in the northern part of the Atlantic Ocean for the connection between Northern America and Northern Europe. Immediately up to the region of the peninsula-Atlantic shelf, there are areas of commercial fishing, which lie to the most productive in the world.

At the central part of the Atlantic Ocean, to pass, may repeat the outline of the coastlines, the majestic underwater girsky lansyug with a dozhina bl. 16 thousand km, under the name of the Mid-Atlantic Ridge. Tsei ridge divides the ocean into two approximately equal parts. Most of the peaks of this underwater ridge do not reach the surface of the ocean and are located at a depth of at least 1.5 km. Okremí naivishchi peaks rise above the river of the ocean and make up the islands - the Azores near the Pivnіchnіy Atlantic and Tristan da Cunha - near Pvdenny. On the pіvnі ridge oginaє uzberezhzhya Africa and continue further pіvnіch to the Indian Ocean. The rift zone stretches along the axis of the Mid-Atlantic Ridge.

The surface currents near the peninsular part of the Atlantic Ocean are collapsing behind the arrow of the year. The main elements of this great system are directed to the heat flow of the Gulf Stream, as well as Pivnichno-Atlantichna, Kanarska and Pivnichna Pasatna (Equatorial) currents. The Gulf Stream goes through the Florida Channel and the island of Cuba near the peninsula straight ahead from the US coast and approximately at 40° Mon. sh. idhilyaetsya on pivnіchny skhid, changing the name on Pivnichno-Atlantic flow. This current flows on two rivers, one of them follows on the shores of Norway and farther to the Pivnichniy Liodovitiy Ocean. The very weather and climate of Norway and all of Europe are significantly warmer, the lower one can be found at latitudes, which is indicative of the area that stretches from Nova Scotia to the rainy Greenland. The other hand turns to the sun and away to the sun on the shores of Africa, satisfying the cold Canary current. This current is collapsing into the midst of the West Indies and flowing into the Pivnichnaya Pastatnaya current, as if it were direct to the West Indies, and into the Gulf Stream. There is an area of stagnant waters, rich in algae and a view under the name of the Sargas Sea, on the pіvnіch pіvnіch vіd Pіvnіchnoi Pasatnaya techії. From spring to night, the cold Labrador Current, which seeps from the Baffin Stream and the Labrador Sea, and cold shores of New England, will pass from the spring to the Atlantic coast of North America.

Part of the Atlantic Ocean

Deyakі fahіvtsі bring to the Atlantic Ocean on pіvdnі the entire water expanse to the Antarctic ice sheet; others take for the frontier cordon of the Atlantic I will show the line that you get Miss Horn in New America with Miss Good Hope in Africa. The coastline near the main part of the Atlantic Ocean is significantly less damaged, the lower one is near the main part, here there are also daily inland seas, which inflow to the ocean could penetrate at the corners of the continents of Africa and Pivdenny America. The only great flood on the African coast of Guinea. On the shores of Pivdenny America, there are great inflows and innumerable. The most important edge of the mainland - Fire Land - can be pierced by the coastline, denuded by numerous ancient islands.

There are no great islands near the main part of the Atlantic Ocean, there are only isolated islands, such as Fernando de Noronha, Voznesinnya, São Paulo, St. Deer, the Tristan da Cunha archipelago, and on the extreme pіvdnі - Bouve, Pivdenna Georgia , Pivdenny Sandwich, Pvdenny Orkney, Falkland Islands.

The Crimea of the Mid-Atlantic Ridge, near the Pivdenny Atlantic, there are two main underwater mountain lancers. The Whale Ridge stretches across the pivdenno-western edge of Angola to about. Tristan da Cunha, de vin comes from the Mid-Atlantic. The ridge of Rio de Janeiro stretches from the islands of Tristan da Cunha to the city of Rio de Janeiro and a group of water high places.

The main systems of currents in the middle part of the Atlantic Ocean are collapsing against the arrow of the year. Pivdenna Pasatna flow is directed to the exit. У виступу східного узбережжя Бразилії воно поділяється на дві гілки: північна несе води вздовж північного берега Південної Америки до Карибського басейну, а південна, тепла Бразильська течія, рухається на південь уздовж берегів Бразилії і приєднується до течії Західних Вітрів, або Антарктичної, яка прямує , а sweat on pіvnіchny skhіd. Part of the cold flow is water-reinforced and carries its waters to the African coastline, quenching the cold Bengel flow; the rest is allowed to come to Pivdenny Pasatnaya flow. The heat of the Guinean current is collapsing on the shores of Pivnichno-Zakhidnoy Africa into the Guinean inflow.

At first glance, the ocean of light is a gigantic static reservoir of salty water, a single ruh in which one sees the wind. However, this is far from the case - the skin ocean has dozens of great and small currents, which cover a significant part of its area. No blame and the Atlantic Ocean.

Classification of marine currents of the Atlantic

From long ago, the Atlantic is famous for its sea currents, seafarers vikoristovuyut richly build like a wide sea "road". Sea currents of the Atlantic Ocean There are two great circles of circulation, which may be isolated from each other. One of them is spreading near the pivnіchnіy part of the ocean, and the other one near the pvdenny part. At the same time, near the pivdenny "cruise", the water collapses against the year's arrow, and in the peninsular part of the Atlantic - on the contrary, behind the year's arrow. Directly similar to the revolution of delusions by the law of Corioles.

These circulation “colas” are not strictly insulated - on their outer edges, turbulent vortices are established at the sight of flows that are water-creaming. At the pіvnіchnіy pіvkulі, we mostly see Grenlandskoe, which is step by step to pass from Labradorskoe. Near Pivdenniy Pivnich, near Pivdenny Pasatny, there is a Gviansk current, which directs to Pivnich and flows there from Pivnichny Pasatny.

mustache sea currents of the atlantic ocean podіlyayutsya on warm and cold. Ale, such a pіdrozdіl є we will instantly lull. In taxonomy, the main role is played by the temperature of water dovkil. For example, mentally overbig the North Cape can have an average temperature of 6-8 about W, but it gets warmer, the temperature of the Barents Sea, where it goes, becomes less than 2-4 degrees. In a similar rank, the Canarian current is considered cold, although the temperature is rich, lower near the North Cape.

Crimea is below the temperature, the sea currents of the Atlantic Ocean are:

Gradient - vyklikanimi temperature difference and water thickness other parts seas.
Windy (drift) - the stench is blamed for the winds, mostly for the ocean in this area.
The tides, which blame the force of the gravity of the moon, that sun.

Cause blame for sea currents

The main reasons for the vindication of marine currents in the Atlantic Ocean are:

The strength of Corioles, which is blamed as the result of the inertia of a rare medium. The mass of the water that fills the ocean, simply does not catch up with the planet, which turns around on its own axis.
Temperature difference and water capacity. Qi factors appear to be critical for the vindication of clay flows.
Diya winds on the ocean surface.

All factors are not isolated, but poured onto the ocean near the complex, leading to the end of water circulation. The big currents are dangling around the depths of the expanse, which do not exceed a few hundreds of meters. Then, the width of the stench can reach a few hundred, or even a thousand kilometers. For example, the subantarctic current of the Western winds can be up to 2,000 km wide in an hour, moving 270 million cubic meters of water per second, which 2,000 times cross the Amazon.

Main marine currents of the Atlantic Ocean

Near the Atlantic, there are dozens (or even hundreds) of constantly wild sea currents. There is simply no ability to overcome them. Let's go to the most important ones. Before main sea currents of the Atlantic Ocean be seen:

Gulfstream. Tse, perhaps, one of the most grandiose and widely flowing currents of the Atlantic Ocean. Yogo width becomes 100-150 km, and the depth is 1 km. The hot water flow that moves with it becomes close to 75 million m3, which is dozens of times more than all the rivers of the planet. Take your cob from the Mexican butt, which is seen in the name: gulf stream - “stretching the flow”. Gave them the freedom to save the United States, step by step stepping into the fold.
Pivnichno-Atlantichny. On the first day, the Newfoundland Pivostrov - Gulf Stream splits into two new streams: the Pivnichno-Atlantic Current and the Canary. Pivnіchno-Atlantichne, scho transfer heat water, prodzhuє way Gulf Stream on skhіd, and reach pіvnіchno-zahіdny uzberezhzha Evropi, zumovlyuyuchi there m'yakiy climate. Near the Faroe region, you can see the Greenlandic spring current, and the region looks like Norway at the North Cape flow and reaches the Barents Sea. Zavdyaki youmu mi maєmo on the birch of the Pivnіchnogo icy ocean the port of Murmansk, which does not freeze.
Kanarske. Є pіvdennoy, right gіlkoy Pivnіchno-Atlantichnoy sea current. Passers-by of the western coast of the Iberian Pivostrov and Morocco, they reach the Canary Islands, wasting their strength. Prote z tsikh mist take the cob transatlantic Pivnichna pastatna flow.
Pivnichne pastatne. One of those who found the main sea currents of the Atlantic Ocean. Take your cob to protect the coast of Morocco and attack the American continent near the Caribbean Islands. Here it pours into the Caribbean Sea, smoothly turning into small currents, which as a result, people of the Gulf Stream. In such a rank, the great pivnіchnoatlantichne kolo is blinking.

Pivdenny near circulation takes the cob of the bіl pіvdenno-zahіdnyh shores of Africa like a cold Benguela current (called the coastal town in Angola). Far away, warming up, the water flow is moving like a passat, which is hazy from the continent on the way, flocking to the Pivdenny pastat current. Bіlya pіvnіchno-zahіdnogo edge of Brazil it is subdivided into two sleeves: pіvnіch vіdhilyаєtsya Gvіanska, and on pіvden - brazilskoe techії. Remains at the reach of the high Antarctic latitudes, angry from the plywood of the Western winds. The chilled mass of the water is transported to the skhіd, to the coast of Pivdenny Africa, sea currents in the atlantic ocean.

Vikoristannya sea currents of the Atlantic Ocean

Seafarers have long vikoristovuvali sea currents of the Atlantic to optimize the transfer. Most widely vіdomy butt, tse dearer than Christopher Columbus, who descended into Spain by the Canary Stream to the establishment of the "transatlantic" - Pivnichnoi pastatnoi techії. The big-small one made it safely and delivered Yogo to the islands of the West Indies.

Not losing the relevance of the sea currents of the Atlantic Ocean and today. If you failed to create a transatlantic crossing, then it’s not like “finding a bicycle”, but simply speeding along the sea path, we’ll beaten a century of it. Tobto, it is necessary to go down to the Canary Islands or the islands of the Green Misu (Cape Verde), and break with a fair wind and flow straight to the New World. I think the world will be similar to metal in a wide and wide river, obviously, with amendments to the far from river character of the open ocean. It’s not for nothing that a sailor seems to be a darn: be it an object, let in the water near the Canary Islands, wag in the Caribbean for a couple of months.

Turn back at Europe by the best way, through the Gulf Stream. Some sailors have the same order: "The way from the Canary Islands to Europe lies through America." This means that it is easier to turn around from the Canary Islands through the Caribbean Sea under the glass, to go “against the wool”, in spite of the overwhelmed winds and the Canary current, without respecting the great length of the route. Obviously, for motorized ships, the old sea board is no longer relevant, especially since there is a sufficient supply of canine on board.

Farther, having reached the Caribbean Sea, along the Florida Current we reach the Gulf Stream, and rise through the grandiose sea "river" to approximately 40 o. After that, it is turned on the way and in a song hour, following the Pivnichno-Atlantic stream, it reaches the western edge of Europe. Columbus himself turned his own hour on this route on his voyage to the West Indies.

When vikoristannі Gulf Stream dosvіdchenі yachtsmen do not recommend climbing higher than 40 degrees. At greater high latitudes, warm waters of the Gulf Stream are observed with the Labrador Pivnichnaya current with the usual climatic features: rapt winds, partial fogs and storms. It is not for nothing that the United States saves that region of Newfoundland for a long time, having taken the name "rotten cut of the Atlantic". AT winter hour don’t forget about the possibility of the Labrador flow being blamed for the first iceberg day – who else remembers the blockbuster of the 20th century “Titanic”?

A part of the Holy Ocean, bordered by Europe and Africa at once and Pivnіchnoy and Pivdenny America at sunset. The name resembles the name of the titan Atlas (Atlanta) in Greek mythology.

To act for the roses only to the Quiet; yogo area to become approximately 91.56 million km2. In other oceans, there is a strong porosity of the coastline, which establishes the abundance of the sea and inflows, especially near the pivnichny part. In addition, the total area of the basins of the rivers, which flow into the whole ocean or the south margin of the sea, is much larger, lower by the river, which flows into the other ocean. Another one vіdmіnіstyu Atlantic ocean The number of islands is perceptibly small and the folding relief of the bottom, like springs under the water ridges and uplifts the impersonal okremikh ugolovin.

Powers protecting the Atlantic Ocean-49 lands:

Angola, Antigua and Barbuda, Argentina, Bahamas, Barbados, Benin, Brazil, Great Britain, Venezuela, Gabon, Haiti, Guyana, Gambia, Ghana, Guinea, Guinea-Bissau, Grenada, Democratic Republic of the Congo, Dominica, Dominica, Spain, Cape -Verde, Cameroon, Canada, Ivory Coast, Cuba, Liberia, Mauritania, Morocco, Namibia, Nigeria, Norway, Portugal, Republic of the Congo, Sao Tome and Principe, Senegal, Saint Kitts and Nevis, Saint Lucia, Suriname , USA, Sierra Leone, Togo, Trinidad and Tobago, Uruguay, France, Equatorial Guinea, PAR.

PIVNICHNA PART OF THE ATLANTIC OCEAN

Podіlyaєtsya on pіvnіchnu and pіvdennu parts, between the two yakimi mentally carried out beyond the equator. From the oceanographic point of the dawn, however, up to the main part of the ocean, one can see the equatorial leak, which expands by 5-8 ° m.l. Pivnіchny cordon sings to be held behind the Pivnіchny Polar stake. The cities of this cordon are marked by underwater ridges.

Cordoni and coastline

At Pivnіchnіy pіvkulі May be heavily damaged by the coastline. Yogo vuzka pіvnіchna chastina z'єdnuєtsya z Pіvnіchniy Ilodovity ocean troma narrow channels. On the Pivnіchny descent of the Devіsov Prokat with a width of 360 km from the Baffin Sea, which can be seen to the Pivnіchny Icy Ocean. In the central part, between Greenland and Iceland, there is the Danish duct, the width of which is 287 km from the navigable area. Nareshti, at the pivnіchny descent, between Iceland and Norway, the Norwegian sea is spread out with a width of bl. 1220 km. At the exit Atlantic ocean there are two water areas that go deep into the land. The greater pіvnіchna їх are initiated by the Pіvnіchnіm sea, yak to cross at the Baltic Sea with the Bothnian and Finnish inflows. On the first day, there is a system of inland continental seas - the Middle Earth and the Chorny - a deep valley bl. 4000 km.

PERELIKI

Surface leaks near the pivnichny part Atlantic ocean crumble for the year's arrow. The main elements of this great system are directed to the heat flow of the Gulf Stream, as well as Pivnichno-Atlantichna, Canary and Pivnichna Pasatna (Equatorial) flows. The Gulf Stream goes through the Florida Channel and the Island of Cuba near the Pivnichniy straight ahead to save the USA and approximately 40° latitude. idhilyaetsya on pivnіchny skhid, changing the name on Pivnichno-Atlantic current. This current flows on two rivers, one of them follows on the shores of Norway and farther to the Pivnichniy Liodovitiy Ocean. The other hand turns to the sun and away to the sun on the shores of Africa, satisfying the cold Canary current. This current is collapsing into the midst of the West Indies and flowing into the Pivnichnaya Pastatnaya current, as if it were direct to the West Indies, and into the Gulf Stream. There is an area of stagnant waters, rich in algae and a view under the name of the Sargas Sea, on the pіvnіch pіvnіch vіd Pіvnіchnoi Pasatnaya techії. From spring to night, the cold Labrador current passes, which seeps from the Baffin Stream and the Labrador Sea and the cold coast of New England.

ISLANDS of the Atlantic Ocean

The largest islands are in the middle of the peninsula part of the ocean; the British Isles, Iceland, Newfoundland, Cuba, Haiti (Hispaniola) and Puerto Rico. On the outskirts Atlantic ocean There is a small group of small islands - Azores, Canaries, Green Misu. Similar groups to the western part of the ocean. As a butt, you can show the islands of Bahamas, Florida Keys and Mali Antilles. The archipelagos of the Great and Lesser Antilles islands form an island arc, which is a part of the Caribbean Sea. Near the Pacific Ocean, arcs similar to islands are adjacent to areas of deformation of the earth's crust. Uzdovzh swollen sides of the arc are ripped deep water zholobi.

The Atlantic Ocean is one of the largest and deepest water basins, which yields beyond its size to the Pacific Ocean. Win a note of what you take from yourself fresh water from the great land of dry land and the western polar regions of the earth's backwaters at the sight of a wide channel.

short description

The area of the Atlantic Ocean will be 91.66 million square meters. km, of which 16% is occupied by the seas, inlets and channels. The wine is great, which occupies a large territory from the subarctic latitudes to the coast of Antarctica.

The average depth is 3736 meters, at that hour the maximum depth of the Atlantic Ocean is fixed at the Puerto Rico trench and it becomes 8742 meters.

Rice. 1. Atlantic Ocean.

Average indicators of salinity of ocean waters are not more than 35%.

The Atlantic Ocean has a low unique rice, which lets you breathe in other oceans:

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clearly pronounced dissection of the coastline, which forms the sea and inflows;
the temple of the open area of the pools of the river, which carry their own water into the ocean
a small number of islands and breeding islands;
folding relief of the bottom with a great number of underwater ridges, rises and ridges.

The Atlantic is famous for the most powerful current in the world - the Gulf Stream. Rukh yoga water is incredibly strong - 140 million cubic meters. m drive per second. It will be born out of saving the Bahamas, and then we will enter the Atlantic.

Features of the climate

On the surface of the Atlantic, the climate is reminiscent of a great diversity, mindful of the influx of advancing factors:

the meridional length is great;
circulation of the affected masses;
water exchange from Pivnichnym Ice-free ocean, the Mediterranean Sea and the Arctic seas.

In the world, in the distance, in the equatorial line, there is a change in the type of climate, cooling of the surface waters and, apparently, a change in the warehouse of the organic light of the ocean. The average water temperature in the equatorial belt becomes 26°C, dropping to 0°C in the polar regions.

Rice. 2. Tropics of the Atlantic Ocean.

In the boundless expanses of the Atlantic basin, all climatic zones are represented, which are on the planet. Skin from them may be low vіdminnosti:

In the equatorial zone of the ocean waters warm up to the maximum, and for a long time the temperature practically does not change. In addition, the zone of fogs and falls (approximately 3000 mm per river).
Tropical latitudes are characterized by strong falls and insignificant temperature fluctuations stretching through the earth.
For subtropics, it is typical to remember additional and seasonal fluctuations in temperature. Atmospheric fall fall, over importantly, vlіtku.

Tropical hurricanes are a frequent phenomenon in the subtropics - the force of atmospheric whirlwinds with a wind speed of hundreds of kilometers per year. Nalyutish hurricanes are panning at the basins of the Caribbean Sea.

In calmer latitudes, in warm weather, the temperature again does not exceed 10-15 C, and the charge drops to -10 C. Fall falls calmly and regularly (about 1000 mm). These latitudes are characterized by the most severe storms.
In the subpolar zones, the maximum river temperature reaches 30°C. In the winter the temperature can drop down to -40°С, and in the summer it can warm up to +1-5°С.

Flora and fauna

The great length of the ocean and the diversity of climatic zones zoomed in on the diversity of the baggers of the Atlantic. Yogo vodi became a familiar house for two hundred thousand sightings of creatures and roslin.

At pivnіchnyh latitudes panuє kelp, and at the dead - red algae are transported. Phytoplankton at all latitudes.

Live in the polar and pomirnih belts see different trisky, oseledets, flounder. These are represented by pinnipeds and cetaceans.

Only in the Atlantic Ocean are the only seas in the world, as there are no shores - the Sargas Sea. It is rotting in the middle of the water surface and is surrounded by sea currents. The entire area of the Sargas Sea is filled with stormy algae - sargas.

Tropics are characterized by windmills, sharks, ribeyes. From sea creatures turtles, dolphins, sperm whales are shooting. Rich and cephalopods: squids, octopuses.

Rice. 3. Flying ribs.

The list of water-bearing fauna is also striking: all kinds of corals, sponges, molluscs, crustaceans, and chrobaks linger in the oceanic depths.

What did we recognize?

When enrolled in the "Atlantic Ocean" for the program of geography of the 7th class, we were recognized as geographically expanding the Atlantic Ocean, especially its climate. So I got to know the flora and fauna of the Atlantic.

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The Atlantic Ocean is respected by one of the largest and largest in terms of size, and the other by the size of space Pacific Ocean. This ocean has the most developments and developments, as if equal to other water areas. Its simplicity is like this: it is immediately framed by the shores of Pivnichnoy and Pivdenny America, and at the sunset of its borders it ends with Europe and Africa. On Pivdni vin to cross at Pivdenniy ocean. And from the pivnіchnogo side between Greenland. The ocean is winding down because there are few islands in the new arc, and the relief of its bottom is all folded and the structure can be folded. The line of the shore is broken.

Characteristics of the Atlantic Ocean

If you talk about the area of the ocean, it occupies 91.66 million square meters. km. It can be said that part of this territory is not the ocean itself, but the springs of the sea, inlets. The volume of the ocean is 329.66 million square meters. km, and the average depth is 3736 m. There, the deepest trench of Puerto Rico, is considered by the greatest depth to the ocean, which becomes 8742 m.

Atlantic Ocean from the pivnichnogo side

The cordon to the ocean from pіvnochi poddekudi is marked by ridges, spread under the water. At this pivkul, the Atlantic is framed by a broken line of the coast. Small її pіvnіchna part of z'єdnana z Pіvnіchniy Lodovitim ocean dekilkom with narrow channels. The Devil's Canal is roztashovana at the Pvnіchny descent and connects the ocean with the Baffin Sea, which is also considered to belong to the Pvnіchny Icy Ocean. Closer to the center, the Dansk channel is less wide, lower Devіsіv. Between Norway and Iceland, the Norwegian Sea is closer to the pivnіchny immediately.

At the first entrance of the Pivnichnaya current to the ocean, there is a Mexican influx, as it happens to be the Florida channel. And also the Caribbean Sea. Here you can see an impersonal inflow, such as Barnegat, Delaware, Hudson’s inflow and others. On the same side of the ocean you can see the biggest islands, which are famous for their popularity. Tse Puerto Rico, all-worldly sights of Cuba and Haiti, as well as the British Isles and Newfoundland. Closer on the slope you can see small groups of islands. Tse Canary Islands, Azores and Green Misu. Closer to the west - the Bahamas, the Mali Antilles.

Part of the Atlantic Ocean

Some of the geographers are aware that the pivdenny part, the whole stretch to the Antarctic. How to establish a cordon at Miss Horn and Miss Good Nadiya of two continents. The shore on the pivdni of the Atlantic Ocean is not so pierced as on the pivnoch, and there are no seas here. There is one great inflow of Africa - Guinea. The farthest point on pіvdnі - tse Fire Land, yak framed by small islands near the great kіlkost. So here it is not possible to build the great islands, but also the islands, like Fr. Ascension, St. Deer, Tristan da Cunha. On the extreme pіvdnі you can see Pvdenny islands, Bouvet, Falkland and others.

As far as the flow on the pivdni ocean, then all the systems are flowing against the year's arrow. Right off the bat of Brazil Pivdenna Pasatna currents are roaring. One mile is going to the pivnich, flowing through the white of the pivnichny coast of Pivdenny America, filling the Caribbean basin. And the friend is vvazhaetsya pіvdennoy, warm arc, the bіla bіla brazіlії і nezabara zadnuієє z'dnuєє z'dnuetsya tekієyu, potіm prаmuє є skhіd. Frequently it turns and transforms into the Benguela crossing, which is blown away by its cold waters.

Significant reminders of the Atlantic Ocean

The Belize Barrier Reef has a special underwater cave. Її was called Blakitnaya dira. It’s deep inside, and in the middle of the millings there are a number of ovens, like tunnels intermingling with each other. The depth of the cave reaches 120 m and is considered unique in its kind.

There are no people, I wouldn’t know about bermuda tricot. Adzhe vіn roztashovaniya in the Atlantic Oceanі and rozburhuє vyavu rich zabobonnyh mandrіvniki. Bermudi to talk about their riddle, but at the same time they sneer at uncertainty.

In the Atlantic itself, you can touch the unseen sea, as if there were no shores. And all that is out of place in the middle of the expanse of water, and its borders cannot be framed by dry land, show the border of the sea only. The only sea in the whole world, for example, such unique data is called the Sargasso Sea.

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