The middle mountains of the oceans. The Pacific Ocean? Zagalny characteristic that describes the Pacific Ocean

The most and the one who found the most of the oceans. Yogo area become 178.6 million km2. Win can easily accommodate all continents at once, and this one is called Great. The name “Quiet” is tied to F.'s im'yam, who had traveled around the world for a rise in price and had flown across the Pacific Ocean for friendly minds.

The whole ocean is really great: it occupies 1/3 of the surface of the entire planet and is 1/2 of the area. The ocean is oval-shaped, especially wide in the area.

The people who inhabit the Pacific shores and islands have been swimming on the ocean for a long time, have conquered its wealth. Evidence about the ocean bully accumulated as a result of swimming F.Magellan, J. ... Special for vivchennya was opened at the end of the day The Pacific... per the rest of the rock otrimanі new danі about yogo nature, it is designated glibina, vivchayutsya flows, bottom relief, ocean.

The part of the ocean from the shores of the Tuamotu islands to the shores is an area of ​​calm and style. For the rest of the day, Magellan and his companions called the Pacific Ocean. On the west side of the Tuamotu islands, the picture quickly changes. Spookyna the weather is here buvak ridko, call the dim burhlivi vіtri, It is not easy to go to. It’s so called new squalls, especially fierce ones in the chest. Less parts, more strong tropical cyclones. The stench comes on the cob in autumn, at the winter part of the stench passes into the warm winter.

The tropical waters of the Pacific Ocean are clean, clear-cut and average salinity. Їх dark blue color hostile to sposterіgachіv. Ale inodі vodi here fill up greens of colіr. Tse is tied with a branch of the marine life. In the equatorial part, the ocean is friendly Wash the weather... The temperature over the sea trims close to 25 ° С and it does not change much. There is a breath of peace of mind. An hour will be booming and calm. The sky is clear, the nights are even darker. Especially stylish in the zone of the islands of Polynesia. In the belt of calm, some of them are strong, a little more short-hour rage, especially at midday. Hurricanes are superbly rare here.

Warm water and ocean will take robots corals, which are without any problems. The southern coast of Australia stretches along the Great Reef. The most expensive "ridge" of organisms.

A part of the ocean is located under the influx of monstrosity and rapist whims. There are hot hurricanes here. Especially the fierce stench in the wine pavkul mіzh 5 and 30 °. Typhoons are partly from linden trees to gussets, in crescent trees to a month. The stench is born in the regions of the Carolynian and the Marian Islands і because of the "nabigi" on the shores, і. So, it’s hot and rainy on the tropical part of the ocean, the islands of Fiji, Novi Gebridi, Nova, it’s not for nothing that one of the most unhealthy days on earth is vaulted.

Pivnіchnі regions and the ocean are similar to pіvnіchnі, tіlki yak bi in the mirror image: a circle of water wrapping, albeit in the pіvdennіy part against, then in pіvnіchny - on vartovy; bad weather at sunset, when typhoons go to the bottom of the ocean bottom - the time of the greatest depths to the outskirts. Globokovnye traps reach for the viglyadi of the high zholobіv in the western and central parts of the ocean. Great welcome to share the ocean bed on the street. On the descent of the ocean, Skhidno-Tikhookeanske was raised, as a part of the system of mid-ocean ridges.

During the Danish hour, the Pacific Ocean plays an important role in the life of the region. Half of the Ribbon's catch is brought to the aquatorium, which is a part of the storage of small molluscs, crabs, shrimps, and krill. On the seafloor, the doers of the lands grow molluscs, growing water growth and vikoristovuyut in the family. On the shelf, carry out the development of metal rods, while on the shores of the Kalifornia island, add naphtha. Deyaki krainy describe sea ​​water and vikoristovuyt її. It is important to pass through the Pacific Ocean sea ​​routes, The length of the cich trails is even greater. Dobre rozvinenne shipfaring, the leading rank of the uzdovzh of the Uzbek continents.

Gospodarska dіyalnіst people called to obrudneniya waters of the ocean and to wininchuvannya deyakіvіvіv tvarin. So, in the XVIII century there were blames of sea cows, one of the participants in the expedition of V. In the Danish hour, there was a promise of intercourse. Great concern for the ocean is the obstruction of the waters, the entrances of the industry.

Roztashuvannya: encirclement of local Uzbeks, local Uzbeks of Pivnichnoi and Of America, At parties, at parties.
Area: 178.7 million km2
Average Glybin: 4282 m.

nai great glybin: 11022 m ( Marianska depression).

Bottom relief: Skhidno-Tikhookeanske pіdnyattya, Pіvnіchno-Vostochna, Pіvnіchno-Zakhіdna, Tsentralna, Skhіdna, Pіvdenna and іnshі ugoviny, glibokovodnі zholobi: Aleutska, Kurilo-, Marchіnskiy, Fіlіppіnі

bags: a large number of single-line and large-scale microorganisms; riba (pollock, oseledets, salmon, triska, sea bass, biluga, chum salmon, pink salmon, sockeye salmon, chaviga and bagato іnshikh); seals, seals; crabs, shrimps, oysters, squid, octopuses.

: 30-36.5 ‰.

current: warm -, Pivnichno-Tikhookeanske, Alaskinskoe, Pivdenno-Pasatne, Skhidno-Australiska; cold - Californian, Kurilsk, Peruvian, stretching out Western windows.

Dodatkova information: The Pacific Ocean is the largest in the world; having flipped Fernand Magellan for the first time in 1519, I called the ocean "Quiet", so for all three months of travel, Magellan's ships did not go into one storm; The Pacific Ocean has been taken for a period of time in the winter and winter regions, between which pass along the line of the adequate.

Storinka 2 z 13

The Pacific Ocean? Zagalny characteristic that describes the Pacific Ocean.

The Pacific Ocean? The characteristics of the Pacific Ocean are enigmatic. Table.

Named the ocean	Pacific Ocean
Area of ​​the Pacific Ocean:
By the seas	178.684 million km
without sea	165.2 million km
Average depth of the Pacific Ocean:
By the seas
without sea
best glybin	10 994 m (Marianska depression)
Travel to the Pacific Ocean:
By the seas	710.36 million km3
without sea	707.6 million km3
Average temperature
salinity
Width from entering the highway - from Panami to shidny uzberezhzh Mindanao Island
dovzhina from weekends to weekends, from the Bering Channel to Antarctica
number of islands
Creatures (number of species)	more than 100,000
Incl. vid_v rib
Incl. species of molluscs
species of algae

The Pacific Ocean? Description of the Pacific Ocean.

Pacific Ocean - the largest great ocean our planet, Scho borrow a third. On the th part of the fall, 49.5% of the surface area of ​​the Svitovoy Ocean falls and 53% of the water. The width of the ocean from the approach to the skid becomes 17,200 km, the width of the ocean from the start to the highway is 15,450 km. The area of ​​the Pacific Ocean is larger than the entire land area of ​​the Earth by 30 million square kilometers.

Pacific Ocean - the largest glib ocean our planet... The middle ground depth is 3984 meters, and the nibil'sha is 10 994 km (Marianska depression abo "Bezodnya Challenger").

Pacific Ocean - the largest warm ocean our planet. It is a great part of the ocean to lie in warm latitudes, so the average temperature of the waters (19.37 ° C) is two degrees above the temperature of the other oceans (with the blame of Pivnichny Lodovity).

The Pacific Ocean- the most densely populated territory of the Earth, here in 50 powers live close to half of the population of our planet.

Pacific Ocean from the lower waters of the planet - here you see close to 60% of the catch of ribe.

Pacific ocean maє sami large reserves in carbohydrates the whole Svitovoy Oceans - there are close to 40% of all potential reserves of naphtha and gas.

Pacific ocean maє naybagatshu flora and fauna- there is a bag of 50% of all living organisms in the Svitovoy ocean.

The Pacific Ocean is the most "wild" ocean on the planet- there is more than 80% of the tsunami "populist". The reason for this is the large number of sub-water volcanoes.

The Pacific Ocean is a majestic transport- here pass the road.

View of the Pacific Ocean. Why Ocean "Pacific"?

Why Pacific Ocean Names "Quiet"? Adzhe tsemiy gryznyh from the oceans of the Earth: 80% of the tsunamis originate here, the ocean ryasnіє underwater volcanoes, celebrated by catastrophic hurricanes and storms. Just beyond the irony valley, Fernand Magellan, the first European glimpse of the Pacific Ocean, has gone one hour of his three thousandth sailing without ever having spent in a storm. The ocean will be quiet and laggy, for which I have given the name “Quiet”.

Before the speech, Magellan did not become the first European, like having smacked the Pacific Ocean. First Buv іspanets Vasco Nunєs de Balboa, which is a prelude to the Novy Svit. win by dragging american continentі viyshov on uzberezhzhі yak vіn thinking in the sea. Unbeknownst to him, before him is the greatest ocean of the Earth and giving this name the Pivdenne Sea.

Between and Climate of the Pacific Ocean. The Pacific Ocean?

On land:

Western cordon of the Pacific Ocean: at the lower Uzbeks of Australia and Eurasia.

Skhidny cordon of the Pacific Ocean: at the backs of the Uzbeks of the Holy Wine of America.

Pivnichna boundary of the Pacific Ocean: as soon as I grow up, I will become stranded by land - Russian Chukotka and American Alaska.

Pivdenna boundary of the Pacific Ocean: bilya of the pivnichny Uzbek coast of Antarctica.

Between the Pacific Ocean. Map.

With the big oceans:

Cordon of the Pacific Ocean with the Pivnichny Lydovitim Ocean: The border is held in the Bering Protoss from Mis Dezhnyov to Prince of Uelsk.

Cordon of the Pacific Ocean Atlantic Ocean: The border is drawn from Misu Horn along the meridian 68 ° 04 '(67?) W. For example, in the New York region from Eastern America to the Antarctic Peninsula through the Drake Channel, from Osti Island to Misu Shternek.

Cordon of the Pacific Ocean Indian Ocean:

- for the first day from Australia- along a skidny cordon of the Bassov channel to the island of Tasmania, further along the meridian 146 ° 55 'skidnoy dovgoti. d. to Antarctica;

- for a private visit from Australia- between the Andaman Sea and Malakkskoy, dal birch trees the island of Sumatra, the western prototype, the ancient birch of the Java island, the ancient cordon of the seas of the Bali and the Savu, the ancient cordon of the Arafur sea, the ancient western coast of the New Guinea and the western cordon.

Climat of the Pacific Ocean. Zagalny characteristic that describes the Pacific Ocean.

Climate of the Pacific Ocean in parts.

The part of the Pacific Ocean is very cold, as the water soaked in to go to the shores of Antarctica. Here in the winter period the water is covered with ice.

Climat of a private part of the Pacific Ocean kudi m'yakshe. At the same time, the fact that the Pacific Ocean is practically not in contact with the cold Pivnichny Lydovitim ocean, but is surrounded by land.

A part of the Pacific Ocean is warmer than the other part.

At tropical latitudes, the ocean will generate tense hurricanes - typhoons.

There are two zones of typhoon generation:

• on the way out of the Philippines - the typhoon collapses on the winter and winter through Taiwan, Japan and reach as far as the Bering channel.
• bilya shores of Central America.

A number of fallen fallen off unevenly over the surface of the planet's greatest ocean.

Flora, fauna and economically significant Pacific Ocean. The Pacific Ocean?

Flora and fauna of the Pacific Ocean is highly versatile. There is a bag of nearly half of the living organisms of the entire Svitovoy ocean. The price is explained by the majestic dimensions of the planet's greatest ocean and development natural minds.

Most types of sack in tropical and equatorial latitudes, in winter and in the middle latitudes ah types of development are common, but then there is a greater number of individuals of the skin species. For example, in the cold waters of the Bering Sea there are close to 50 species of seaweed, and in the warm waters of the Malaysian Archipelago there are close to 800 species. Alle the mass of algae of the Bering Sea on the other side is larger than the mass of algae in the Malaysian Archipelago.

The Glybin of the Pacific Ocean may not be amused by life. The creatures who live here, may be indifferent to Budova, a lot of them fluoresce, vipromineuchi light as a result chemical reactions... Dane is attached to serve for viewing huts and receiving video clips.

The Pacific Ocean is alive:

• over 850 species of algae;
• more than 100 yew. species of creatures (there are 3800 species of ribs from them);
• more than 6 yew. species of molluscs;
• close to 200 species of food, sluggish on a glybin of more than 7 yew. km.;
• 20 kinds of creatures that can be sluggish on a glybin of more than 10 yew. Km.

The economic value of the Pacific Ocean is a reference and description of the Pacific Ocean.

The Uzbek coast of the Pacific Ocean, the first island and the sea, has been developed uneventfully in the region. most apologetic industrial centersє Uzbeks of the USA, Japan and Pivdennoy Korea. The economy of Australia and New Zealand is also rich in what is tied to the development of the world's largest ocean.

Great significance in the life of the people of the Pacific Ocean yak dobuvannya їzhі... On the yogi part of the fit, up to 60% of the light catch of the ribe falls. Especially the promiscuous ribalism is rooted in tropical and inland latitudes.

Across the Pacific Ocean I love the important sea and good communities between the countries of the Pacific basin and transit routes between the countries of the Atlantic and Indian oceans.

Great economic significance of the Pacific Ocean and in the plan cinnamon copaline vid... There are up to 40% of the potential reserves of oil and gas in the Svitovoy Ocean. In a given hour, carbohydrates are delivered to the shelves of China, Indonesia, Japan, Malaysia, the other States of America (Alaska), Ecuador (Guayaquil inflow), Australia (Basov channel) and New Zealand.

Pacific Ocean Vicon and Velmi specific role in happy holiday: Here in the private part of the ocean There is a "tsvintar" that went out of the way of space ships.

Relief of the bottom, seas and islands of the Pacific Ocean. The Pacific Ocean?

Relief of the bottom of the Pacific Ocean - description and characteristic of the Pacific Ocean.

The bottom of the planet most oceanic... There is a Pacific plate near the ocean. To her adjoin plates: Nazca, Cocos, Juana de Fuca, Fіlіppіnska, on pіvdnі - Antarctic plate, and at pіvnіchі - Pіvnіchno-American. Such a large number of lithospheric plates produce a strong tectonic activity in the region.

At the bottom of the Pacific Ocean, on the edges of the Pacific Plate, there is a so-called "Vognians kіlce" of the planet... There are earthquakes, volcanoes, tsunamis are constantly coming up.

"Vognanogo kiltsya" of the planet.

The bottom of the Pacific Ocean is literally in the sea lonely mountains volcanic hike. At present, nearly 10,000 have been racked up.

Moreover, it is foldable here system of sub-water mountain ridges Who found a number of retractings on the pivdeno and descend to the ocean - tse Skhidno-Tikhookeanske pidnyattya, then go to pivdni in the Pivdenno-Tikhookeansky ridge. The whole sub-water ridge extends the Pacific Ocean into two asymmetric parts - a great backward, de-overwhelming warm currents, and a small turn, de-panu cold Peruvian leak.

Independent islands and archipelagos We settled down as a result of volcanic activity, united in the vicinity of a part of the world - Oceania.

The largest depressions in the Pacific Oceanє: Chileyska, Peruanska, Pivnichno-Zakhidna, Pivdenna, Skhidna, Tsentralna.

The Pacific Ocean and the coastline. The Pacific Ocean?

As far as all the seas of the Pacific Ocean are concerned, they are growing on the winter and the backs of the world - the coast of Asia, Australia, and the Malaysian Archipelago. On the descent of the ocean, there are no great islands, not protruding much into the land, an inflow - the coastline is smooth. Vinyatok - Kaliforniy inflow - semi-enclosed sea of ​​the Pacific Ocean. Bilya shores of Antarctica roztashovane on one side of the sea to the ocean - the Ross Sea.

Islands of the Pacific Ocean.

We looked at the statistics of the Pacific Ocean, gave an opinion on the nutrition: What Pacific Ocean? Read on: Water the Pacific Ocean: water in the ocean, temperature in the ocean, salinity in the ocean, ice and color in the water in the Pacific Ocean.

the most water in the world, the area of ​​which is estimated at 178.62 million km 2, but the number of square kilometers is larger earthly land and more than twice the area of ​​the Atlantic Ocean. The width of the Pacific Ocean from Panami to the Uzbek coast of Mindanao becomes 17,200 km, and the length from winter to week, from the Bering Channel to Antarctica, 15,450 km. Vін prostagєat vіd remote shores Pivnіchno and Pіvdennaya America to the middle Uzbeks of Asia and Australia. In winter, the Pacific Ocean may become more landlocked, joining the Pivnichny Ice Ocean by the Bering Channel (the minimum width is 86 km). On the first day, it should reach the shores of Antarctica, and on the descent between the Atlantic Ocean, it should be carried out at 67 ° W. meridianu misu Horn; at the entrance of the boundary between the Eastern part of the Pacific Ocean and the Indian Ocean, it will be carried out along the 147 ° of the Great Departure, from the general positions of the Pivdenno-Skhidny Mystery on the Pivdennaya Tasmania.

Atlas of Oceans: Vol. 1. Pacific Ocean... L., 1974
Geography of the Holy Ocean: Pacific Ocean... L., 1981

Know the "PACIFIC OCEAN" on

Pacific Ocean- the most expensive, and far from the most Pacific ocean on Earth, which washes the shores of five continents of our planet.

Pacific Ocean

On our planet, the Pacific Ocean is the largest. Together with the seas Pacific Ocean area warehouse more than 178 million km 2. earthly surface there are more than half of them, covering the shores of five continents, around Africa.

The width of the Pacific Ocean becomes more than 17,000 km, and the distance to Antarctica is close to 15,450 km from the beginning of the Bering Channel to Antarctica.

The Pacific Ocean with the Pivnichny Lodovitim is surrounded by the Bering Channel, and the Pacific Ocean Magellanic Channel, the Panama Canal, the Drake Channel.

Water temperature in the Pacific Ocean start in the private part warm leaks Kurosio, Alaskan, Pivnichno-Pacific and cold Californian and Kuril, in the northern part warm Pivdenno-Pasatnoy, Shidno-Australian and cold - Peruvian plinth The water on the surface of the Pacific Ocean reaches up to +29 0 С, and closer to the pivnochі up to -1 0.

Seas in the Pacific Ocean, which wash the shores of our land, become a group of Far-Eastern seas (Beringov, Okhotsk and Yaponske). The stench of the most glibokovodnі, from the territory of Russia. І before speech, axis.

The Pacific Ocean on the map of the light and the map of the current

Pacific Ocean - current map

Meshkans of the Pacific Ocean

The Pacific Ocean has a magnificent number of bags. Half of all biomas and living organisms of the Holy Ocean are thrilled with their little house.

Yak and in all the oceans of our planet, the main mass of bags of plankton, algae and corals, store sharks, whales, jellyfish and, of course, turtles, which in the Pacific are more than a hundred species.

Over the last ten years, the activity of the people is much more significant for the flora and fauna of the Pacific Ocean, but do not marvel at them, but the prodovzhu has become interested in the most important comorie of the planet and a leader for the Bagatio lands and peoples.

Chomu Pacific Ocean was named Pacific

At 1513 r Vasco de Balboa moved from winter to winter the Panama Isthmus and called the ocean "Great". After 7 years, the rise of Magellan prowled the path (up to 3 months) Vognyana land - the Philippines Islands. For an hour the ocean will be more expensive, it will be quiet, like a mandrill, the sounds of the enemy, calling it Quiet.

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Before the speech, turn on the video before going to bed, the sounds of the ocean, the noise of the surf and the splash of hvil, it is simply unrealistic to help you fall asleep і baciti vіdminni from below)))))))

Quiet travel to the regions, winter and winter, and even earlier, it was three times - winter, central and new. The paths served as a cordon. The Pacific Ocean I will leave the volcanoes. There are a lot of them to be found in a sleepy camp, a little more formal. Oh so and they called it "The Fire of the Fire". On the descent of the girski ridge, go to the very shore. Sounds and gurkit from the power of volcanoes and vyverzhen also harmoniously blend into the “quiet” of these areas of the ocean.

Islands in the Pacific

In the Pacific Ocean there are islands of its own accord, which do not have any kind of relationship to the adjacent continents, continental islands, etc. Їх nachuyut up to 25,000. There is a lot of changing all the іnshі in three oceans.

Tsikavi near the islands of the volcanic trekking. Smells spread across the entire area of ​​the ocean. There is a great number of lines on them, purely good and clean water is presented as unforgettable paradise for people. The very same deyaki islands were called so - Raysky islands

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bagato islands in the Pacific otochenі coral reefs. Here they knew sob ribs, molluscs, ssavts. Bagato islets are found in a tropical climate, de vipados are richly fallen, and in their own right there is a boisterous development of growth. Often the stench perevoryuyutsya in the fair jungle.

A little bit of island views.

1. Koralovi - stink "grow" h. Call the tse boom like this - a fiery volcano that drifts over the water and zgasa. Coral reefs will feel yogo, reaching the bottom. The volcano gradually subsided or ruined under the inundation of waters, and the corals overflowed. This type of island is a favorite place for tourists.
2. volcanic islands... Rukh measles і streams of lava, іnіmayut yo over the surface of the waters і mount a mountain in the center. The roaming earth allows the growth of the line to grow quickly. They are populated by different creatures, and polipi set up the reefs around the whole island, streaming burhlivy onslaught of hwil. Tsі islands go to the water every now and then. The process can be found in millennia of rock, alley to find a call, then to grow on the birch of the lagoon.
3. Pidnyatiy atol. For an hour, earthlings in the coral reefs rise above the water up to a meter. Smells set up a peaceful plateau, there are a lot of beaches on them. It often stinks as a hotspot.

A small island in the Pacific Ocean

Still in the last century, in 50 rocks in the Pacific Ocean, a bulo was marked for purchase. The price of plastic virobi, as it is not in the snake, is laid out quickly. The obstruction of the plastic was lost to the wine-walker. At the edges of Indonesia, you can go to the rivers, so you can go to the ocean. Here plin smittya wear in singing misce... Win accumulate and make the majestic masu. One of these smithy spikes of colossal growths in the state of Texas. Tse sprazhnіsіnka smіttєzvalische

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Smitty Islands in the Pacific Ocean sail near the Hawaiian Islands, Alaska and California.

Plastic comes in to create the wrong school of flora and fauna of our planet. Bagato ptahіv and ribi to wrap up the shmats of plastic, take it for the good and go.

Smittava beaches in the Pacific Ocean shvidko zrost. Fakhіvtsі seem to be wagha smittya syagaє ponad 3,500,000 tons. There is one of the most magnificent creatures on the planet. Vona constantly get lost in one place through flood leaks. Smuga is dragging towards the state of California from the Hawaiian Islands.

Glybin of the Pacific Ocean

Glybin of the Pacific Ocean lie down from the miscy. In the middle of the year, the reach is close to 4000 m, ale є y glibshі mission. By value, it is possible to vvazat the ridges і pіdnyattya, depressions і zholobi. Not far from Pivdennoi America, two days of Chilean and Galapagos are being repaired. Yak butt can be made under the water of the plateau, over which there are Solomon Islands.

Close to the coast there can be bugs and traps. The stench is set in order with the volcanic mountains. Naybilsh see them Galatea, Challenger, Emden, Ramapo.

At the bottom of the ocean, there were high water mountains. Vvazayut, scho tse large volcanoes, such as rozmiti hvilami.

Trench in the Pacific

Pivdennish from the Marian Islands to be Marianska depression... tse the best depth in the Pacific Ocean... Warehouse more than 11 kilometers. Vona has a V-shaped shape. The length of the roads is 1500 km, the bottom reaches the vuzke from 1 to 5 km. A vice in a depression is 1000 times more than atmospheric, and there will be a blaze of life.

Tsunami in the Pacific

Unimportant in its name, up to 80% of tsunamis originate in the Pacific Ocean. The stench comes from earthquakes, volcanoes, zsuvi. And in the Pacific Ocean region there is a lot of seismic activity, and the greatest number of tsunamis is happening here. Before an hour for an earthquake, one part of the bottom sinks, but it sinks. The great obsyag lead vishtovkhut up on the mountain, so pretend to be visoka hvila.

Before the hour of the volcano, a bowl-shaped form takes shape. Water, zapovnyuchi її, approve the dovgy hvili. At the top of the high mountains, as you go on the surface, the tsunamis come all the way. Tsunami maє kilka hvil. Persha is not a great ruinous force і to introduce people to Oman. Vona yak bi gotuє shore to another, more strong hvili. Repeated hvilya can go through a few years.

Pacific Ocean і Druga Svitova Vіyna

Rocky has a different light Pacific Ocean becoming a spravozhnіsіnky theater of boyovyh dіy. Vіyna was over him in the twilight. There were hidden Japanese and American and sometimes Russian escadrilas. In the first place, the Allied Forces against Japan were held.

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I will not describe the message here, the article is still not about those. I will just describe the main battles and victories of the war in the Pacific Ocean.

• Pearl Harbor
• Singapore Defense
• Battle of the Ryukyu Islands

campaigns:

• in the Solomon Islands
• birmanska

operations:

• Malaysian
• Філіпінська (1941-1945)
• Gollandsko-Ost-Indska
• Gilbert-

I think that you want to know more, for all the phrases you know all the information. And we turn to those of our beautiful ocean. Naskіlki wіn beautiful, you can change yourself, marveling at the photo.

Pacific Ocean - photo

So, marvel at the photo, you will change one more time, it’s not for nothing Pacific Ocean can be found in the most mysterious and unknown ocean in the world.

I bash everyone to go for a ride in the Quiet, and try water for it))))))
Now you can turn around.

The area of ​​the Pacific Ocean with the seas is 178.7 million km earthly coo... The shape of the ocean is izometric, slightly twisted from the initial approach to the opening skid. The length of the first weekend is close to 16,000 km, from the approach to the highway up to 20,000 km. Nearly 710.4 million km 3 of water will be available for the new one, and 53% of the waters of the Svitovoy Ocean will be replaced. 78.9% of the total fall area is on the sea level from 3000 to 6000 m. The average depth to the ocean is 3976 m, the maximum is 11 022 m.

At the entrance to the ocean, pass along Uzbek Asia, Malax Protots, ancient and ancient outskirts of the Malaysian Archipelago, New Guinea, Torres Street, Uzbek Australia, Bass Channel, Tasman Islands until Antarctica, at the descent - along the Drake channel from Cape Shternek on the Antarctic Peninsula to Cape Horn in the archipelase of Vognyana land, the Uzbek coast of the Ancient and Eastern America, on the winter - from the Bering channel.

Shape the coastal line to reach the folds on the western periphery of the ocean and easily on the sidelines. At entry, the transition zone between the ocean bed and the continents is represented by a foldable complex of border and multi-sea seas, sharp arcs and glide-water zholobiv. Here, the most important thing on the Earth is spared horizontally and vertically, the dismemberment of earthly measles. At the gathering of the Uzbek Pivne and Pivdennaya America, poorly porous, on the day outskirts of the seaі large purchase of islands, glide-water zholobi roztashivayutsya without the middle from the mainland.

Features geographical position and the great expanses of the Pacific Ocean will welcome the change in the cold weather of the waters of the Pivnichniy Ice Ocean, or will allow the inflow of Antarctica, in conjunction with the cym of the pivnichna part of the ocean, it is warm, and now it is warm. A large part of the ocean has been roasted in the equatorial tropical latitudes, which is why it is the best from all the oceans. The position of the ocean in these latitudes encompasses the versatility of one's natural minds and resources, as well as the vision itself in the boundaries of all physical and geographical belts, with the blame of the Arctic.

The Pacific Ocean has no children for genesis, area and configuration of islands. For їх кількістю i home area(Close to 3.6 million km) in the first place in the middle of the ocean. Volcanic islands are developed across the entire aquatic ocean (Aleutsk, Kuril, Ryukyu, Hawaiian, Chatham, Easter, Galapagos, etc.) most islands Malay Archipelago, New Zealand ta in.). Biogenny islands are mainly located in equatorial-tropical latitudes (Karolinsky, Marshalls, Gilbert, Fiji, Tuamotu and in.). The islands and the central and western parts of the ocean are united by by name Oceania.

Geological Budova and bottom relief. On the outskirts of the continents occupy 18.2 million km 2 or close to 10.2% of the area of ​​the Pacific Ocean, including 5.4% on the shelf, 3.0% on the mainland and 1.8% on the mainland. Naybilsh is widely represented in the marginal seas of the western industrial sector, the Malaysian archipelago, the wine and the western Uzbek coast of Australia.

Near the Bering Sea, nearly half of the bottom area falls on the shelf with small depths and virgin relief. It is characterized by the appearance of traces of flooded river valleys and recreational forms of ice relief of large marine abrasion-accumulative processes. The mainland was seized by a wide one with signs of a skid-and-earthen partition and great sub-water canyons. The continent is poorly rotated, at the sight of a one-man and high accumulative trail.

On the shelf of the Sea of ​​Okhotsk, the coastal milina is clearly visible, it is an abrasive-accumulative drainage basin surrounded by a depth of 100 m and an open shelf, which covers the entire central part of the sea with small depressions up to 1000-1500 m. streams. The mainland pidnizhzhya is a vuzka valley, set with wine products of kalamut streams and sunshine. The Japanese sea shelf has nasty twists and turns and I borrowed only the area in the Tatar prototype. The mainland seized the performances of the vuzkoy smog of a steeply healed bottom. Relief of the Shelf of the Shidno-Chinese and Zhovtoy Seas, made by forceful alumina wedges in the Yangtzi and Huangkhe rivers. Tilki in coastal smoothies widened food ridge, fixed by tidal currents. Near the Pivdenno-Chinese Sea and the seas of the Malay Archipelago, there is also a submarine suburb of the mainland. Near the budova shelf zones my role grate corals with equipment and special features of accumulation, carbonate and pyroclastic litter.

For the first time in Australia, there is a great shelf, which is characterized by widespread widening of carbonate litter and coral reefs. On the way out of Australia, you will find yourself in the lightest lagoon, facing the sea by the largest bar reef in the lighthouse. The Great Barrier Rift dividing the swamp of coral reefs and islands, shallow inflows and channels, stretching in the meridional straight line for 2500 km, with a width of about 2 km in the private part, and up to 150 km. On the descent of the reef, the straight line is shaved to the mainland. The peculiar morphostructure of the Paleozoic age є the New Zealand plateau, which is a shave of the mainland earth measles not tied to the mainland. Mayzhe from the sides of the plateau is bordered by wide, dissected sub-water canyons, by a continental slope step by step to pass into sub-water.

The relief of the underwater outskirts of Pivnichnaya America is characterized by significant fragmentation, the appearance of numerical depressions, flat-topped ponds, wide transverse valleys. Bilya shores of Alaska win a lot of ice cakes. Maximum fragmentation, with good turning tectonic divisions, the relief of the Californian Borderland is developed. The Vuzky shelf is surrounded by a ledge on depths of 1000-1500 m. The mainland has seized up with numerous sub-water canyons, the cones of the wine that can fix the plague of the mainland. Bilya shores of Central and Eastern America, the shelf is even narrower with a width of up to decile kilometers. Pivdennish 40 ° S NS. the wine grows wider, less fragmentation. The role of the mainland skyla is on the continental board of glibokovodnykh zholobiv. The continent is practically not rotated.

The continental outskirts of Antarctica grow into a shallow staging of the edge of the shelf (mostly up to a depth of 500 m), a dissected relief, wide expansions of ice and icebergs. The mainland covered wide, covered with sub-water canyons. The good deceit of the mainland is represented by a flat-out abductor by the plague.

Transitional areas The Pacific Ocean occupies 13.5% of the total area and according to the regular conditions of the gullies of the near seas, sharp arcs and glide-water zholobiv. Smells are found at the lower stages of development and development according to the set, configuration and development of these components. It is characterized by foldable earth measles and is referred to the geosynclinal type. Seismic and in the nearness of the Pacific set the earthquake and volcanic volcanism in the Pacific.

The Western-Pacific sector sees the onset of transition regions: Aleutian, Kuril-Kamchatska, Yaponska, Skhidno-Kitayska, Indonesian-Philippines, Boninsko-Marianska, Malevsky, Vytyazkuyatska (At the same part of the ocean, the young transition regions are roztasovani on the cordon with the bed of the ocean) ...

The Shidno-Pacific sector has two transition regions: Central American and Peruvian-Chileyska. Here the transitional zone is twisted only by glide-water troughs. On the outskirts of the sea and sharp arcs. The role of sharp arcs in the tsіі zіonі vіkonuyut young folds of the structure of Central and Pіvdennaya America.

Mid-ocean ridges occupy 11% of the area of ​​the Pacific Ocean and are represented by the Pivdenno-Pacific and Skhidno-Pacific uplifts. Along the way, there is a single structure, with a length of about 11,700 km, and a part of the planetary system and mid-ocean ridges. The stench is characterized by a vault-like Budova, significant width (up to 2000 km), the swamp of the axial rift valleys, intertwined with transverse transform rifts. The rift system of the axial zone and the mensh is twisted, lower in the Mid-Atlantic and other ridges of the type. Some of the most visible structures, such as the great density of earth measles under the crest, seismicity, volcanism, high values ​​of heat flow and a number of them, are manifested even more intensely. At pivnich from ekvodor Skhidno-Tikhookeanske pivnittya sounds. The rift zone of the ridge has become more steep. In the region of Kalifornia, the structure is drawn to the mainland. W o'clock to connect to the coverage of the Californian Borderland, the great active development of San Andreas, the depression of Sacramento and the Iosemite Valley, the glib structures of the Great Basin and the head rift of the Skelyastikh Gir. Mid-ocean views of the Pacific Ocean may be seen in the Chilean landscape and Galapagos rift zone. In addition, to the system of mid-oceanic ridges to lay, roztasovani on the first ocean descent of the Gorda, Juan de Fuca and Explorer ridges. The mid-ocean ridges are characterized by crust Riftogenic type, which grows more high, less oceanic.

Pacific bed borrowing 65.5% of the total area and may be more often located in the boundaries of the ocean lithosphere plates The upper part grows in the middle at the depth of 5500 m. The mid-oceanic rise extends to the ocean bed on two parts, with dimensions and features of the bottom relief. The skhidna part is occupied by the great ugolovinas and morphostructures knitted in the main from the Skhidno-Pacific podnyattyam. The western sector is characterized by a large foldable budget and versatility of forms of relєfu. Practically all morphological types of sub-water lifts of the ocean bed are developed here: ocean valleys, brilovy mountains, volcanic ridges, outskirts and ridges, around mountains (Guyot). The ridges and elevations of the Pacific Ocean rise one way through the same oceanic valleys. Heads from them є: Pivnichno-Zakhidna (6671 m), Pivnichno-Skhidna (7168 m), Fіlіppіnska (7759 m), Skhidno-Marianska (6440 m), Tsentralna (6478 m), Zakhidno-Karolіnska (5798 m) -Karolinskaya (6920 m), Melanesiyska (5340 m), Pivdenna (6600 m), Chiliyska (5021 m) and Bellinshausen (5290 m). For the relief of the bottom of the gorges, there are characteristic humpbacks, some of the planes (the Bellinshausen gorge) of the abisal pavnini, around the sub-water peaks, Guyot and the latitudinal rifts extending up to 4000-5000 km. Naybilsh great rosters timed to Pivnichno-Skhidnoy ugovina: Mendosino, Marie, Moloka, Clarion, Clipperton. Significant breakdowns in the central part of the ocean occur for each day from the following: Galapagos, Markizki, Easter, Challenger.

The basins and uplifts of the Pacific Ocean bed have an oceanic crust. Mysce of a granite ball is a "other ball", which will be built up from gorged siege or volcanogenic rocks. The need for a siege ball to change from 1000 to 2000 m, at least every day. The urge of the "other ball" to go from hundreds to thousands of meters, in some districts it is also outside. The average tension of the basalt ball becomes close to 7000 m.

Donnie attachments and corisnі copalini The Pacific Ocean to reach the rіznomanіtnі. Terrigenous fallen trees occupy close to 10% of the Pacific Ocean floor area. The stench in the main time before the submarine outskirts of the continents, ale it grows in the outskirts of the seas, glide-water troughs and navigate on the edge of the bed to the ocean. Terrigenous iceberg attachments make the smog up to 1000 km wide for the shores of Antarctica. The most widening of carbonate foraminiferous debris (close to 38%), which occupy a significant area of ​​the bottom for a day as far as 60 ° S. NS. At the first stage, the branches are surrounded by the summit surfaces of the ridges and the second branches, and in the warehouses of the mules they carry the donny foraminifera. The pteropod is attached to the bottom of the bottom of the Coral Sea. Corals fall off less than 1% of the ocean area and grow on the shelves and continental cliffs in the equatorial-tropical belt. Turtles fall off on all shelves, except for the Antarctic. Biogenic creamy falloffs cover more than 10% of the bottom area and form three main zones: individual and new siliceous diatom mules in high latitudes and equatorial siliceous radials. In areas of constant and quarter volcanism, pyroclastic release is more likely to occur. Near the link with the depths of glibin, 4500-5000 m of the bottom area in the Pacific Ocean (close to 35%) is covered with glibokovodnogo red clay.

Practically everywhere on the Pacific Ocean bed widening of the zalizo-manganese concretions, which occupy an area of ​​close to 16 million km 2. The average instead of the concave becomes 7.3-7.8 kg / m 2, and in the vicinity of the ocean reaches 70 kg / m 2. Їх zagalny stocks are estimated at 17 yew. Bln. Tons. The United States and Japan are responsible for the pre-industrial production of gold-manganese concretes. From the last cinnamon copalins in the form of concretes, phosphorite and barite are seen. Industrial reserves of phosphorites are known from the Californian Uzbek coast, on the shelf of the Japanese islands, along the coast of Peru and Chile, New Zealand, on the sub-water uplifts in the open ocean and other regions. Potential reserves of the price are estimated at hundreds of milliard tons.

More importantly, the development of metal bearing minerals in the Pacific Ocean is important: rutile (titanium ore), zircon (zirconium ore), monocyte (torin ore) and others. Providne a place in this type of loan from Australia, the deduction of the uzberezhzhya rassipi is drawn by 1.5 yew. Km. Coastal-marine rosipi casiterite ( tin'yana ore) Roztashovuyutsya on the Pacific Uzbek coastal Asia and Australia. Titanium-magnetite and magnetite ( Zalizna ore) Rozsipy distributed in the areas of the Japanese Islands, the Malaysian Archipelago, the Kuril Ridge and the coast of Alaska. The genera of gold-bearing deposits emerged from the western Uzbek coast (Alaska, California) and the Old (Chile) America. Platinum Pisces are added to the coast of Alaska. Ore-forming hydrothermies have emerged in the Californian floodplains and other regions in the region of rift zones near the Galapagos Islands.

The non-difficult brown copalins go to mean the genus glauconite, pyrite, dolomite, awakening materials: gravel, sand, clay, vapnyak-turtle and in. In the bagatokh regions of the Pacific shelf zone, significant genera of oil and gas have been discovered. Near some areas of the shelf of the shores of Japan, Australia, New Zealand, and the Middle Ages, the layers of a cam'yan vugilla are covered.

climat In the Pacific Ocean sleepy radioactivity and circulation of the atmosphere.

Rice number of total sleepy radioactivity changes from 3000-3200 MJ / m 2 in subarctic and Antarctic latitudes up to 7500-8000 MJ / m 2 in equatorial-tropical. The value of the radioactive radioactive balance varies from 1500-2000 to 5000-5500 MJ / m 2. At the same time, the negative radiobalance is promoted for the first time from the line: the middle part of the Sea of ​​Japan - the northern edge of the island. Vancouver (up to -80 MJ / m2); in linden - on half a day from 50 ° S. NS. The maximum monthly value (up to 500 MJ / m 2), the balance is attainable in the regions of the tropics, in the present - in the winter season, in the linden - at the wine region.

Near latitudes pіvnіchnoі pіvkulі roztashovutsya Aleut minimum, more turns in the winter period. In the subpolar region of the Pivdennaya Pivkul, the Antarctic belt of a low vice is seen. At the subtropical latitudes of both pivkul over the ocean there are centers of two permanent baric maximums: Pivnichno-Pacific (Hawaiian) and Pivdenno-Pacific. Undovzh ekvatora roztashovutsya ekvatorialna depression. Baric centers can also be infused into the climate of the Pacific Ocean, as they are set over the adjacent continents: the seasonal Asian maximum (wintering), the werewolf Australian baric center (maximum charge and minimum in the last period).

Vidpovid to the rise of the main baric centers, the systems and vіtrіv are formed. Subtropical maxima and equatorial depression zoom in on the adoption of passages in tropical latitudes. The repetition rate of passages in the first season should be close to 80%, with a speed of 6-15 m / s (up to 20 m / s), at a speed of up to 60-70%, with a speed of 6-10 m / s. The weather is calm near the convergence zone. In the middle latitudes, the most characteristic western ones, especially in the new period, deceive the greatest strength and steel. At the high latitudes of the coast of Antarctica, there is a tendency to cross. Near the pivnichno-western part of the Pacific Ocean, monsoon circulations are swirling. Winter is winter and winter is winter, sometimes it is winter and winter is winter. Maximum flexibility during the winter tied to the passages of tropical cyclones. The regions of the region lie between 20 and 5 ° latitude in the dermal period, with a maximum repetition rate in autumn and autumn. Most of the tropical cyclones in the Pacific Ocean are promoted to the area of ​​the roasted sea, the Philippines Islands and 170 ° c. In the middle of the month, there are 27 typhoons, in the vicinity of rock there are up to 50, of which nearly half of them are hurricanely fast in the morning of 33 m / s.

Middle Twist temperature fierce in near equatorial latitudes become + 26 - + 28 ° С, for the shores of Antarctica, it drops to -10 ° С, and in the Bering prototype up to -20 ° С. ° С in the Bering archipelago and up to -25 ° С near Antarctica. maximum temperature In the morning (up to +36 - +38 ° С), they are more likely to be located in the area of ​​the wine trail to the turn of the Philippines Sea, as well as near the Californian and Mexican Uzbeks. Minimum values ​​are in Antarctica (up to -60 ° C). The highest temperature ranges are typical for the winter-western monsoon region of Asia - 20-25 ° С. In the equatorial latitudes, the amplitude does not change 2-4 ° С.

When the temperature rises above the ocean, there is a significant inflow of the continents, ocean currents... In the boundaries of the equatorial-tropical belt Zakhidna chastina The Pacific Ocean, behind the vinyaty area adjacent to Asia, is warmer than the skidniy. In the middle latitudes of the winter season, navpaki, it is colder down the road. In the world of the new generation, such indications cannot be spared.

middle badness over the Pacific Ocean there are maximum values ​​in the latitudes of 7-9 points. In equatorial won, the trochi is lower and become 6-7 points. In the zone of subtropical baric highs, the temperature changes up to 3-5 points, and in the surrounding areas of the winter season - up to 1 point.

Most of the fall vipad in the equatorial-tropical zone of convergence of passages, intensive visceral traffic flows are developing. Here, the rychna sum has fallen over 3000 mm. In the middle latitudes, the number of fallen falls from 1000 mm at entry to 2000 at the descent of the ocean. There are fewer drops of water in the zone of the secondary periphery of subtropical baric highs, and then there are low wind flows and cold ocean currents. At the end of the Californian Pivostrov, the amount of fallen leaves does not change 300 mm, but for the coast of Peru and the winter Chile 100 and 30 mm. In the backwoods of the subtropical regions, the number of litter grows up to 1000-2000 mm. At high latitudes, both seasonings are due to low temperatures and low brewing, the number of fallen falls to 300 mm at weekends and 100 at weekends. In the inner-tropic zones of convergence and in the subtropical regions, in a high grip, they fall more and more evenly stretching out to the rock. In the region of the Aleutian Minimum, as well as in the subpolar and subpolar latitudes of the winter season, there is a recurrence of fall growth during the winter period. In the monsoon region, in the winter-western part of the Pacific Ocean, the maximum falloff occurs in summer.

fogs most often take place in the middle latitudes, especially above the aquatorium, which is prone to the Kuril and Aleutian Islands, de average number of days with fogs reach 40, with a maximum in lіtnіy period... In the middle latitudes of the winter season, most of the time does not last for 10-20 days.

Hydrological mode. Roztashuvannya surface leaks in the Pacific Ocean, it is mainly due to the peculiarities of the circulation of the atmosphere over the water and the summit continents. In the oceans, analogous atmospheric and genetic systems are formed by them. At pіvnіch from 40 ° mon. a subpolar cyclonic circulation is seen, which is stored from the Alaska, Aleutsky, Kamchatka, Kuril and Pivnichno-Pacific flows. On the first day of the cycle of leakage systems, a subtropical anticyclonal circulation begins to develop, and the Syrchan Pasatnym, Kurosio, Pivnichno-Pacific and Californian currents become established. At low latitudes Pivnichne passatna, Mezhpassatnoe (Equatorial prototype) and Pivdenna passatna current establish two high tropical cyclonic circuits. At the Pivdenniy Pivkul, a subtropical anticyclonal circulation is also promoted, which is stored in the Pivdenny Passat, Skhidno-Australian, Western and Peruvian currents. The current of Zakhidnykh vіtrіv vzaєmodі, with a weakly turning by the coastal Antarctic platen skid directly, confirming the subpolar cyclonic circulation. Anti-cyclonic and cyclonic circuits of leaks are not generally closed systems. The stench is intertwined with oneself and called for the help of other currents.

An important role in the circulation of the waters of the Pacific Ocean is to superimpose the Cromwell's compensatory flow, which collapses under the Pivdenny Pasatny plate at a depth of 50-100 m in sideways... The length of the current flow is close to 7000 km, the width is about 300 km and the width is about 1.8 to 3.3 km / year. The average rate of major surface leaks is 1-2 km / year, and the rate of Kurosio and Peruvian leaks is up to 3 km / year.

Near the Pacific Ocean vіtrovі hvili(Up to 34 m). Hvilyova's activity has been increased to speed up from 40-50 ° N. NS. і 40-60 ° S sh., de pid hour to the storm dovzhina hvil reachє 100-120 m, height 6-8 m, inodі up to 15-20 m, with a period of 10 s. The area with the most stormy activity in the development of Antarctica and New Zealand on the outskirts of the Macquarie Island, due to the middle height of the mountains is close to 3 m. ...

In a large part of the Pacific Ocean, there are many ways to prevent melt... In the middle of the ocean, you get the right water. Small districts in the equatorial region and in the winter (Kuril Islands, skid of Kamchatka) may add more water. The average tidal range is 1-2 m. At the bays of the Alaska inflow - 5-7 m, in the Cook bay - up to 12 m. The maximum inflow value is indicated in the Penzhinskaya Bay (Sea of ​​Okhotsk) - 13.2 m.

The Pacific Ocean is the warmest of the oceans. Middle Richna temperature yogo surface waters to become 19.1 ° C. The price is surrounded by the majestic dimensions of the ocean, the growth of a large part (close to 50%) in the equatorial tropical latitudes and the significant isolation from the Icelandic Ocean.

The rise in the temperature of the surface waters of the Pacific Ocean is mainly due to the heat exchange with the atmosphere and the circulation of waters, often damaging the sublatitudinal directions of the isotherms. Most high water temperatures are more prevalent in the equatorial-tropical latitudes - +25 - +29 ° С. Rock the western sector of the ocean is 3-7 ° C colder than the dark one. At the same time, the water temperature in the Bering prototype becomes +5 - +6 ° С. In the middle and polar latitudes, there are no significant changes in the temperature of the waters between the western and contiguous parts of the ocean. In the area of ​​floating ice in Antarctica, the water temperature rises slightly up to +2 - +3 ° С. NS.

salinity rose waters of the Pacific Ocean are, by the head rank, processes of moisture exchange on the surface and circulation of waters. The water balance in the ocean is characterized by a hundred permutations of the amount of atmospheric fallout and streamflow over the amount of vaporization. The salinity of the waters in all the depths of the lower, lower in the other oceans. The highest salinity of surface waters is reduced in subtropics up to 35.5 ‰ in Pivnichniy pivkuli and up to 36.5 ‰ in Pivdenny. In the near-equatorial zone, salinity decreases to 34.5 ‰ і mensh, at high latitudes - to 31-30 ‰ at winter and up to 33 at winter. Bridging shores on the descent of the ocean currents wine grows salty waters from the high latitudes in the lower latitudes, at the entrance - more salty waters from the lower ones in the high latitudes.

ice-making in the Pacific oceans are seen in the Antarctic regions, as well as in the Bering, Okhotsk, Japanese and Zhovtom seas, in Alaska, inlets of the Uzbek coast of Kamchatka and the island of Hokkaido. At the private part of the ocean, there are no ice floes. Boundary ice is 4-6 months, tovshchina - 1-1.5 m. The floating ice does not descend below 40 ° N. NS. at about. Hokkaido і 50 ° N NS. at the skid banks of the Alaska outflow. Wine ice from Pivnichniy icy ocean practical for the day. There are a few coastal icebergs (Malaspina) at the winter tributaries of Alaska, but there are not many icebergs. Call the ice in the private part of the ocean not a serious crossroads for ocean navigation. Near the part of the ocean, there is a great deal of ice that is constantly present, and all this is seen to extend far into the distance. The middle of the floating Antarctic ice The charge to pass in the area 61-64 ° S. NS. In the vicinity of the mountains with suvorian winters, ice will expand to 56-60 ° S. NS. The edge of the floating ice is close to 70 ° S. NS. Bagatorial packs of ice, typical for the Central Arctic, in Antarctica on the day. The onslaught of the continents of Antarctica icebergs give an ear to the number of icebergs, which are grapevine up to 48-48 ° S. NS. The main areas and establishment of icebergs are the Ross and Amundsen Seas. Average size of icebergs 2-3 x 1-1.5 km, maximum up to 400 x 100 km. The height of the above-water part varies from 10-15 m to 60-100 m.

insight in the Pacific and Antarctic latitudes, the ocean rises from 15 to 25 meters. In equatorial-tropical latitudes, the growth rate is up to 30-40 m at the descent and up to 40-50 m at the ocean setting.

Near the Pacific Ocean tepee water Top, bottom, top, bottom and bottom. The power of surface water masses is initiated by the processes of heat and moisture exchange on the surface of the ocean. It smells like a strain of 30-100 m, depending on the variability of temperatures, salinity, power and seasonal variation of authorities. The top of the head is in the minds pomirnoy zone formed as a result of autumn-winter cooling and water mixing, and in the sinks of a warm climate - a way of lowering more salty surface waters. The stench comes from the surface altered salinity and brilliance, at water temperatures in the paths and subtropics of 13-18 ° C, and in the middle latitudes 6-13 ° C. climatic minds The depth of the cordon with the industrial waters rises from 200 to 600 m. in addition to the muscular climatic minds and the peculiarities of the vertical circulation of waters. In the middle and high latitudes, the stink may have a temperature of 3-5 ° C and a salinity of 33.8-34.7 ‰. The lower boundary of the structural zone is located at depths from 900 to 1700 m. The water depth of the Pacific Ocean is established in the main as a result of the drainage of the cold waters of the Antarctic and the Bering Sea with further expansion along the basins. Їх the lower boundary pass at a depth of 2500-3000 m. The bottom water masses set up on the Antarctic shelf and step by step rise along the bottom, close all the waterways to the ocean. The stench is characterized by one-man salinity (34.6-34.7 ‰) and low temperature (1-2 ° C). Glybinny and bottom water masses become close to 75% of the total volume of the Pacific Ocean.

Superintendents for the majestic dimensions of the aquatic environment and the versatility of natural minds organic light The Pacific Ocean is found for a number of species, ecological spilot, foreign biomass and industrial biological resources. Phytoplankton of the Pacific Ocean is represented mainly by one-line algae (close to 1300 species), moreover, all the stench is more pronounced before the first and the atom. There is a large part of the growth in the coastal zones, in the shallow waters of the ocean and in the areas of upwelling. For the high and middle latitudes, both pivkul are characterized by a mass of development of burrow algae, especially the group of lamіnarіevih. In the equatorial-tropical widely widened fucus, great green (up to 200 m) and red water growth. Donna the growth of the Pacific Ocean is close to 4 yew. Types of algae and up to 30 species of quart (sea grasses).

Tvarinniy svit The Pacific Ocean behind a viewable warehouse is 3-4 times larger than in the other oceans. Here are all groups of creatures of organisms bagging in the Svitovoy Ocean. Especially rich for a number of species of fauna of the back regions of the Pacific Ocean in the equatorial-tropical regions. At the seas of the Malaysian archipelago there are 2 yews. The species of ribs, such as those in the seas on the middle of the ocean, are only close to 300. There are a few more species of ribs in these waters, less in the analogous seas of the other oceans. The coral fauna is widely developed in the regions of the Zond Islands and in the winter period of Australia. There are 6000 species of molluscs near the tropical waters of the bag. The fauna of deep-water parts is native to the ocean. On the slopes, there are 8.5 km of sacks of 45 species of creatures, of which approximately 70% are endemic. Here they re-ferment holoturia, lamellar gabernias, polykheti, ophiuria and other organisms, fixed up to life in the ultra-abyssal. The fauna of the Pacific Ocean is seen as an old-fashioned collection of systematic groups, endemism and hygantism of their representatives. The ancient ones are lingering here Morski Yizhakiі ribi (yordanіya, gіlbertіdіya і ін.), endemic ssavtsi - sea ​​cat, Sea beaver, sea lion, giant music, oysters, the largest two-stalked mollusk tridacna, wago up to 300 kg.

The Pacific Ocean is growing in high biological productivity. The growth of primary products and biomass is based on latitudinal geographic zoning, according to the provisions of the main oceanic water cycles and dynamic zones (convergence, divergence, upwelling). Areas of significant productivity are confined to subpolar, pommer and equatorial zones (250-500 mg C / m 2). In the middle of these zones, the maximum value of primary production and biomass is associated with upwelling zones. At tropical latitudes, the bioproductivity is lower (100 mg C / m2 or less). In the central regions of the subtropical gyres, the won is minimal and does not overtake 50 mg C / m 2.

The Pacific Ocean has three biogeographic regions: Pivnichno-Pacific, Tropic-Indo-Pacific and Antarctic. The Pivnichno-Pacific region is characterized by salmon and far-grown sardine; Tropic-Indo-Pacific - sharks, flying ribs, tuna; Antarctic - nototenevie.

Perche mіsce middle of promislovikh biological resources The Pacific Ocean is occupied by ribs (85% of the catch), others - molluscs, crayfish, golkoshkiri and іnshі nonribnі ob'єkti industry, including water growth (10%), in the third - marine savtsі (5%). In the Pacific Ocean, 45% of the ribs get in the light.

The main districts and industries are located in the ancient, ancient, modern, remote and ancient parts of the ocean. Central regions and interconnections of warm waters of the Kurosio and cold streams of the Kuril current, the zone of penetration of the warm Alaskan current in the high latitude, shelf areas at the setting of the ocean and zones of upwelling for the coast of the Spanish and especially America. Since the 70s, the catch of ribi has grown in the Antarctic regions. The main promises of the Pacific ribs: pollock, anchovy, oseledets, sardine, horse mackerel, mackerel, saury, salmon, tuna, triska, hake. flounder, halibut, sea bass. Also in the oceans there is a promiscuity of whales and spineless whales. Significant development, especially for an hour, was taken away by mariculture.

The Pacific Ocean is seen (according to D.V. Bogdanov, 1991) all physical and geographic belts with the blame of the arctic. There are some significant indications of the natural minds of the remote, remote and central regions of the ocean, in between the belts they see physical-geographic regions... When the regions are designated, the particularities of their geographic position, climatic minds, hydraulic regime, stages of development of natural processes and phenomena, etc. In the western part of the Pacific Ocean, in the capacity of physical and geographic regions, the outskirts of the sea are welcomed, and in the mainland - zones of intensive upwelling. Pivnichny subpolar belt: Bering Sea, Sea of ​​Okhotsk; pivnichny pomirny belt : The area of ​​the inflow of Alaska, the Japanese sea, the Zhovte sea; pіvnіchny sub tropical belt : Kaliforniy region, Kurosio, Skhidno-China sea; pivnichny tropical belt: Філіпінська district, Pivdenno-Chinese sea, Kalifornyysky inflow; equatorial belt : Panama region, Australian-Asian seas, New Guineas sea, Solomon sea; paved tropical belt: Peruvian region, Skhidny region, Koralovo sea from the subdistricts of the Great Bar'erniy reef; pivdenny subtropical belt: Tasman Sea; pivdenny pomirny belt: Chileysky district; pivdenny subpolar belt; new polar belt: Ross Sea.