adsby.ru → Land of the Light

Naiglibshi sea traps

The main irregularities of the bed of ocean depressions are confirmed by negative and positive mega-forms in order. Negative mega-forms are evoked by abisal regions, and positive ones - by the girskiy relєf of the oceanskoe city-forming regions. Tsi forms represent two main types of development of ocean measles and lithosphere. Some stinks are introduced with platform and orogenic regimes in the minds of ocean measles. In the historical-genetic aspect, the analogy is unrealistic, even if the mega-form is given, it may be quite spiilar.

negative megaforms

abіsalnі pіvnini represent slightly sloping surfaces, roztasovani on to reach the vitrimanic views: from 3.5 to 5 km.

Based on the geomorphological position of the abysal plains and the stink of the ocean bed, add to a) periocean i b) revitalize.

Perioceanic Rivnini from continental passages at sea levels of 3.5-4 km. Їх the surface is heaped up to the central regions of the ocean, it is almost 5 km away from the middle of the mountain behind the abyssal skyla with the abyssal valleys on the mountain slopes.

revitalize the plain represent a variety of peri-oceanic rivnines, seen from them with outlines. In the vigorous smogs, all the ocean's great mountains (middle ridges, etc.), as well as the abysmal areas of the land. In the perioceanic regions, there is a stench in the stink of continental traffic.

abіsalnі ugovini є a typical mega-shape of the relief of the bed to the ocean, roztashovuchis on the depths of 4.5-6 km. Tilki in the depressions of the Ice Ocean, the bottoms of the valleys lie on a sea level of 3-4 km. The bottom of the large valleys (especially gliboks) is the relief of humpbacked valleys. Let it be admitted that they are volcanic volcanoes, being shield volcanoes and laccoli, which have settled in the minds of a thin (5-7 km pulling) ocean measles. The geomorphological position of the abysmal valleys in the boundaries of the depressions of the oceans is zoomed in by the development of ridges-ridges.

positive megaforms

Take time to smooth down the bottom of the oceans in the growth of its nature and scale. At least the value of the middle of them may middle ridges- areas of oceanic riftogenic mining.

middle ridges oceans represent a global system of elevations up to 60 yew. km and up to 2 yew wide. km, scho rises above the bottom of the summit abysal valleys up to 4-5, more than 6 km. In the structural form - the pristine shape of the basalt ball of ocean measles and the upper mantle of a special gnarled type, which, perhaps, as a result of the penetration of the speech of the upper mantle into the basalt ball.

At the beginning of the mid-mountain ridges, morphologically, one can see grabbed and crypt. They took the canopy, and the stars were easy to fold, so that the great fragmentation of the crypts was created. Shil and the crypt was accelerated by the peaks of the volcanic mountains and the depressions of the Prirozlomnoye were broken free. Naybilsh contrasting forms are often characterized by the central part of the star with the head rift valley - a glide depression, surrounded by breaks. The axes of the zones and the middle ridges are called “rift zones”. Ridges and rift valleys are represented, incl. and ultrabasic rocks, head rank, pink peridotites. The valley was steep and flat-bottomed, and the board was everywhere accelerated by volcanic clouds. The breakdown of the middle ridges can also be accelerated by breaks.

The middle ridges are characterized by the appearance of a in droves... Hiking in vimag of a local vivchennya. The vast expanses are heavy to the continental outskirts and the pericontinental submarine mountains.

Geological and geophysical characteristics of the middle ridges indicate the day-to-day development from the summaries of the abysmal and ugovyny. middle ridges The Pacific characterized by increased seismicity and manifestation of volcanism. For cich regions, the so-called zebra-like magnetic field of the line magnetic anomalies of the zebra sign is called. Along the middle ridges and outward to the ocean bed, there will be an acceleration in the number of growth.

microcontinent represent in the oceans of the day, folded by the crust of the continental type, even underwater. From the continents, the stench comes from the great abisal plains with the bark of the ocean type. Find out about the genesis of micro-continents: behind some of the manifestations, whole fragments have covered continents, behind the others - under-developed continents, now they are on the cob of their formation. Vyhodyachi zyavlennya about zagalny significant zonurnye depressions of the oceans, persistently poached є more imovirny.

underwater plateau represent the visochin with the oceanic type of measles, one for the child with increased strain. In the structural type of cerebral and vaulted-briar, it is accelerated by breaks. Rozlomi often turns in the relief of the plateaus near the viglyadi of the sub-water canyons. Summer days of the plateau (with depths of 2-3 km) and the islands are often set as great coral-volcanic mountains (for example, Bermuds'ki Islands). Geomorphologically, the area is timed to the emergence and surface, so I will drain the water-borne waters, so that the regions of the ocean bed are generally moving.

Oceanic crypts... Call us to establish a system of visochin, which are lined with coral-volcanic spores.

little visochini, More importantly coral-volcanic and volcanic, widespread in the oceans in the areas of development of the Mesozoic and Cenozoic volcanism. Among them, there are coral-volcanic mountains of linear and arc-like forms, which lead to great morphological growths. Among them there are giant volcanoes with typical oceanic-basalt-volcanism, as well as the upper waterways and volcanic islands (for example, Hawaii). Lonely sub-water mountains are often soaked by ring reefs - atols... The ancient coral-volcanic structures, in the process of bridging, set up the sub-water surface from the flattened surface at a depth of 1-2.5 km. Such flat-topped volcanic mountains are called guyots... The stench is widely widened on the Marcus-Necker ramparts in the Pacific Ocean and is indicative of its value.

In Danish hour, in the depressions of all oceans, regional enlargements of megaforms have been established, as well as a small form of growth. Їх widened growth in the skin ocean.

... Relief of the bed of the Pivnichny Ice-cold Ocean (Slo). Arctic middle ridge

More than 30 years ago, on physical and geographical maps, the bed was depicted as a flat, one-movable bottom. Until the present hour, a number of sub-water ridges and mountains have been established, which lead the Arctic basin to the decile of the ulovin.

Near the Pole Arctic basin of Peretinaє Lomonosov ridge, Scho to be repaired in the American sector by a close land Elsmirі primikє to the Siberian shelf in the region Novosibirsk Islands... From the shelf of Elsmir Island to Alpha plateau, scho go into the Mendelva ridge... Near the Siberian sector of the ocean, there is a ridge leading to the shelf of the Skhidno-Siberian Sea. Between the ridges of the flat-bottomed slopes of Makarov and Tollya with a maximum depth of ~ 4 km. Between the Mendeleva Ridge and the Alaska Shelf, it grows in the middle of the Great Ulogovina - Beaufort, її maximum glybin 4680 m. Near the shelf of Alaska - a sprinkle of small mountains, incl. Beaufort ridge the bottom of the valley is 909 m. The part of the bottom of the valley is flat.

The European-Siberian sector of the ocean grows Gakkel ridge... The axial part of the ridge is heavily divided into relief: a number of short ridges are extended by glide rift valleys, en-echelon yak mali bridging the axes of the ridge. Glibina valley up to 5 km or more. At the tsіy part of the ocean zooseredzhenі epіcentri zemtrusіv. The Gakkel Ridge runs through Svalbard for five days and goes there to the middle ridge of the Atlantic Ocean.

Lomonosov і Gakkel ridge is located Amundsen's ulogovina(The North Pole is located in the boundaries of the central street, the depth at the pole is 4316 m). Another ulogovin, I will name it to lie on the side of the Gakkel ridge the city of Nansen... Glibina її 5449 m -. The topography of the bottom of both sites is flat.

... Relief of the Atlantic Ocean bed.

It's easy to add your good robot to the knowledge base. Vicorize the form

Students, postgraduates, young people, who are victorious to develop the knowledge base in their own lives and robots, will be your best friend.

Posted on http://www.allbest.ru/

ocean depressions

Naybіlshі depressions, occupied by oceans, depressions outskirts of the sea, Which is developing in oceanic minds, middling depressions, which are formed between submarine ridges and peaks, and glibokovodnі zholobi... The stench is smoothly interconnecting one with one and the sumptuous oceanic children, not too quickly to think of the Budov and not to be turned in a clean viglyad. Typical representatives of the depressions of the outskirts of the seas є the depressions of the Okhotsk, Japanese, Skhidny, and the Pivdenno-Chinese seas, which constitute a garland of the walled outskirts of Eurasia. A lot of waterways and depressions are represented in the Pacific Ocean. Tse Guatemalska, Panamska, Peruvanska and Chiliyska ogovina, Bellinshausen ulogovina There are 4 types of oceanic depressions. 1. Glibokovodnі zholobi, roztasvanі along the periphery of the oceans, the most widespread in the Pacific Ocean, surrounded - in the Indian, locally - in Atlantic Oceanі to the Middle Earth Sea; start parallel to the bordering sharp arcs and young coastal girskiy sporums; may have a sharply asymmetric transverse profile. On the side of the ocean, before them, there is a glibokovna ryvnina, from the opposite side there is an island ridge or a high mountain ridge. The perevischennya of the peaks of the gir above the bottom of the zholobiv can reach record earthly values - 17 km. Takі zholobi types for thalassokraton uzberezh. 2. Zapininy outskirts seas, oblyamovuyut the Pacific Ocean, may be asymmetric Budova. On the vidminu from the 1st type, there is an island arc from the side of the ocean, and from the prototypical one there is a glide-water ravine. Formed in quasi-kraton districts. 3. Transverse, or seemingly, zholobi cross the ocean ridges, plateaus and structures of the continents. May be transversely, diagonally, or similarly to the plan of Budov, symmetrically prompted and straightforward. 4. Parallel industrial depressions rose parallel to the troughs of the 1st and 2nd types, as well as sharp arcs or ridges. The industrial depression is rosted between the inner volcanic and lasting non-volcanic sharp arcs.

glibokovodnі zholobi

In the outskirts of the oceans, special forms of the bottom relief - glibokovodnі zholobi have emerged. Quite often the university traps with steep, tough grapples, which can stretch for hundreds or thousands of kilometers. The depth of such depressions is very large. Glybokovodnі zholobi may be as close as possible to the bottom. Itself to be found in them great glibini oceans Call the jolly rosters from the oceanic side of the sharp arcs, repeating the vigin, or the bridle of the continent. Glibokovodnі zholobi - tse crossed the zone between the mainland and the ocean.

Osvita zholobіv is tied with the fall of the lithosphere plates. The oceanic plate goes down and goes down to the continental. At the end of the oceanic plates, Zanuryuyuchis in the mantle, make a joke. Areas of glibokovnykh zholobіv are located in zones of manifest volcanism and high seismicity. Tse will explain to you, how do you fix the fools to the brink lithospheric plates.

On the thought of large, glibokovodnі zholobi vvazayutsya marginal valleys and there is also an intensive accumulation of fallen off zruynovannyh gіrsky rocks.

The greatest on Earth - Mariansky Zholob. Yogo glibina reach 11022 m. Vin boulevards in the 50th rock expedition on the radiansky pre-glorious ship "Vityaz". Doslіdzhennya cієї Expedition Mali is even more important for vivchennya zholobіv.

Globokovodnі zholobi Earth

The name of the fool	Glibina, m
Mariansky Zholob
Tonga (Oceania)
phіlіppіnsky zholob
Kermadek (Oceania)
Izu-Ogasawara
Kuril-Kamchatka Zholob
Zholob Puerto Rico		Atlantic
japanese jolob
Pivdenno-Sandvichev Zholob		Atlantic
Chilean zholob
Aleutska Zholob
Zondsky Zholob		Indian
Central American grotto
Peruvian Zholob

The ocean bed is laid out on the deepest

Interes to vivchennya dna open to the ocean Especially since it has been established, it has been established that there is a widening of the springs of earthlings growing between continents and oceans. Say, an earthquake was put on Pamir. From the day of the day in the earth's crust, the springs were beaten, so quiet, as they appear at the water, as they throw a stone in it. Vladivostok is especially sensitive, put it through a sprinkle of hilin to write down on the line a little bit more. Ale the axis of the earthquake was placed in the Hawaiian Islands. The ride from Vladivostok to the Hawaiian Islands is about the same as before to Pamiru, and if you are less likely to try it, it is much faster. Who's on the right?

Seemingly, the broadening of the spring hvil is more, more important and more important than the middle, in such a stench it expands. Does it mean that the bottom of the ocean is piled up by other rocks, below the mainland? Ale tsei visnovok needs to be changed.

The earth's crust has two main types of crystalline rocks. One of them is an admittedly light breed with an average pet carriage of 2.7, which can serve as a butt. Інshiy - large breed, rich in oxides of gold and magnesium (pitoma vaga - close to 3.1); before them basalt, gabro and іn are introduced.

In the whole majestic expanse of the central and peripheral parts of the Pacific Ocean, neither on the islands, nor on the days there are no light breeds. Maybe bootie, there їkh zagalі dumb? It would be necessary to know how I will be able to take advantage of the food price. In this way, the appearance of force has come to light.

Do you know if a kilogram weight does not mean a kilogram? Accurate springy wagons show the visibility (however, it rolls around in milligrams) in the її ї vases on the equators and the big poles, on the rivers and in the mountains. On the right, in the one that was attracted to the center of the Earth, it is stronger than the stench of our neighbor. Ale w earthly kulu the spike will flatten. To that, the poles are 20 kilometers closer to the center of the Earth, lower eqvator, and the force of heavy there is greater. How to climb with weight to the top high mountains Then it will appear, but there is less power there. In the first place, we are away from the center of the Earth, but in a different way, burn out from more light generations, so volodiyut is due to weak attractions.

Volcanoes of Ocean Depressions

Ocean depressions occupy 71% of the Earth's surface. They have grown tens of thousands of sub-water volcanic mountains and hundreds of volcanic islands. They are characterized by the development of the so-called "oceanic" basalts, which grow from continental ones. Tse abo oceanic tolerance, or pools of sodium basalt. In oceanic basalt toleitites, there is a high level of growth and a low amount of calories. Magma їх melt on chap. close 40 km, and luzhny basalts - on a head. 40 - 70 km.

At the zealous evolution of oceanic volcanism, it was brought up in the slightest hour by the change of thickened basalts by the luzhnyi. Toleitic basalt widened in the sub-oceanic islands and sub-water volcanoes, In the middle oceanic ranges. Basalt puddles fix the peaks of oceanic islands and sub-water volcanoes. Most volc. in oceanic depressions it is confined to the rozlomny zones.

good luck happy news about the shifting of the lithospheric plates, vvazhaєtsya, scho in the mid-ocean ridge. the breakdown of the lithosphere into the link with the rise of the glacial melts. Basalt lavas create a new lithosphere and crust of the ocean floor. Vona step by step zsuvaєtsya in the direction of the middle ridge. to the periphery of oceanic depressions. There, the plates of the oceanic lithosphere are pushed up to the edge of the arc, or to the active edge of the continents. In such a rank, є interconnection between volcanic processes, which occurs during the recovery of basaltic magma in the mid-oceanic Rifts and andesite magma in the underthrust zones. These processes are especially developed in the Pacific Ocean.

Marianska depression zberigak secrets to klimatu

oceanic depression glide-water trough

Oceanic traps play a major role in the form of a climate. Before such a visit came a visit to the analysis of the data, taken from the glide-water bathyscaphe, until it reached the Marian depression - the most accessible place on the planet. The descent of the robotic bathyscaphe was built in the end of 2010. This is the first stage of the message, which is called on by the role of the Holy Ocean in the cycle of carbon, the most intensive biochemical process on the planet.

The Marian depression, also seen as a Bezodnya Challenger, is the best place in the ocean. Vona roztasovana in the Pacific Ocean, pulling the Marian Islands for 1500 kilometers, steep (seven-nine degrees) grabbed and flat bottom with a width of one-five kilometers. More than once a glide-water device has reached the bottom. June 23, 1960 US Navy Lieutenant Don Walsh and Swiss Elder Jacques Pikar dropped to an estimate of 10,915 meters on the Trinst bathyscaphe.

I will look at the great difficulties, tied up with the previous tsikh glybin (the grip of 1100 atmospheres, the darkness and the temperature, close to zero, and also foldable for the revitalization of the bathyscaphe's history), with the help of the word of additional technical In the last decade, the international team of preliminaries from the Copenhagen University was informed about the success of such a bathyscaphe and published the first results of the expedition.

Then we came to visnivka, where the ocean depressions were going to melt the double oxide in the carbon (CO2 is the most common form in the carbon in the biosphere), moreover, it was more active, but it didn’t play a role earlier, and it didn’t play the shape. "We wanted to make a difference, some organic material to be deposited on the days and to come up with a lot of material in bacteria, or to fall, or to fold." organic speech, Yake, there is an intensive processing of bacteria. There are more bacteria, less on depths there are six thousand meters on high-water ravines (high-water ocean ravines), which were previously used by the head utilizers of the organics ", - said Glad VVS.

Moreover, the building is disproportionately large due to the area of the surface, occupied by depressions. "If I want to take the trap to occupy only two close to the two to the surface of the ocean, I think that the role of the circle in the coal is still great, in that sense, the stench, imovirno, I am fueled by the functions of the pastry, the same to accumulate more organic matter, lower in other parts of the ocean ", - said Glad.

Ocean depressions are going on like dioxide in coal is similar before, like on the surface of the planet a fox. Such pastes can be used in a straight line, global warming, І perceptions of the ecosystem of the planet in pіvnovazі. "Chim more in the coal will flood the Svitovy ocean, more sour in the atmosphere", - said Glad.

In this past, the Max Planck Institute of Marine Microbiology in Bremen, the Japanese Agency for Marine Geology and Technology (JAMSTEC) and Copenhagen University will take part. The robotic bathyscaphe reached the bottom of the trap in three years after the start. For the accumulation of the accumulated in the coal for the first time, the folds and stashed folds are attached. Schob vitrimati vise up to 11-kilometer water stop, all sensors bullet from titanium alloys. On the offensive stage of the day, it’s time to stand up, skillet in the coal accumulate in the depressions in the broken parts of the ocean floor.

Ocean traps are no better off to marvel at. In 2008, the International Expedition under the Certificate of the British University of Aberdeen showed up to seven thousand meters of waterless ribs, shrimps and other crayfish. Expedition of fahivts to the end of the ocean, near the Uzbek coast of Chile and Peru in the half-dwelled part of the Pacific Ocean, de glibina is 7500 meters. Todi winnicklo three meals: what you see is how you grunt, how to vitrify a colossal grip and how to multiply. Judging from usy, the persistent nourishment of the virishene - organics, like oceanic glibinas "wet", like cosmic black diri.

Heads of Budov and Oceanic Depressions

It is obvious that they were like a divine water and ocean rapids, and the vast expanses of ocean mountains were seen in our sight. Mi will beat it b there wondrous i unseen light, Unlike all those that will leave us on land.

Suchasnі pictures of the Holy Ocean, folded together, show a real picture of the underwater relfu.

The mainland islands are high above the ocean bed, lying 5-6 km lower. It is characteristic for large continents of the land to gently descend beyond the coastal line of seas and oceans and stretch there for a few dozen, and in baguettes (for example, in the Arctic) for a few hundreds of miles of rings.

The surface of the continental miles is even more gently healed into the ocean. All the time, it’s the same kind of village that is the same as it’s the land of the mainland. The stench was taken when the folding land-shelf was washed with small rivulets, as well as for the rakhunok vivitryuvannya, a little later, the ocean was flooded by the waters. The continents of ice - the majestic storehouses of water - greatly podtanil, and the waters of the ocean "went from the shores", flooding the coastal waters of the ancient land. On the continent, you can go back to the mainland near the typical pagorites of the ice-covered hikers, the surplus of river valleys, the ancient coastal ridges. In the small mountains of the Earth, the mountains of the continental miles are not the same. The stench lies in the deformation of the continental outskirts, viclikanikh tectonic rocks... Call the mainland mileena to quickly shave and change steeply falling down the mainland shil.

Lateral profile of the Indian Ocean, luscious continental crust (evil), oceanic crust and rift zone 1. Fluffy rocks of the sedimentary chokhl. 2. Consolidation of the breed of the siege chokhal. 3. Granite breed of mainland measles. 4. Basalt rocks of the ocean floor. 5-7. Glibinni breed of the upper mantle.

The height of the mainland grasses syagaє is 4-5 km; The stinks are even steeper and on the heels there are few people who see the high mountain ridges of the land. By the masses of the continents, they began to cross into the line of striking ledges. The surface of the grasses is foldable: the steps and ledges are divided into non-segmented sub-water canyons. Often there are three mountain ridges and land valleys. There are closed streets, as they open up from the open ocean under the water or the mountain ridges appear above the water. The tops of such ridges often form a garland of islands - sharp arcs, which are even more characteristic of the Pacific Ocean.

The width of the mainland grasses through the steep fall of the zazvychay is not large - close to 50-100 km, altogether, as it grasped fragmentation into a number of steps, the paths and sharp arcs, I will cross the zone wide (up to 1000 km). Bilea of continental grapples in the bagatech people are drawn to the glib and vuzky oceanic jolobies. This is where the ocean is most located, which is 10 km away.

In the central parts of the ocean, the glibini does not stretch 6.5 km. In the area of mainland grafts, earthquakes are seen. The land of the continent in the cich regions is going down or down, trembling, viginayutsya. Especially abundant earthlings are tied with sharp arcs and glide-water troughs, in which there are no volcanoes. Along the Uzbek coast of the Pacific Ocean, the volcanoes are famous for the Pacific "in the open fire."

Scheme of the post-development development of the break, abo the rift zone. 1. Basalt ball, abo oceanic crust... 2-3. Breed the upper mantle.

Sailing of the ocean bottom wicked gigant hvili - tsunamis, collapse on the shore. Throughout the continental grasping and beyond the deep ditches of oceanic frogs, the vastness of the oceanic bed is being repaired. The yogo surface is collapsible. It is either hunchbacked, sometimes in a big way, and it is ideally flat. Distributed by the systems of payments on the outskirts of the street. On the lodges of the ocean without water volcanic mountains that and non-livid pagorbi, mabut, also volcanic hiking. At the back of the ocean floor there are troughs - tectonic breaks.

Close to the continental grappling on the surface of the bed of the ocean through tovschі accumulate there, the fall often grows old, so step by step to get angry with the lower part of the grasp. As the mainland shyly lay a deep-water trough, then the ocean stretches along the edge of the bed, as a rule, a wide marginal ridge. The tse of the statement tectonically is a free reaction of the ocean bed to the progynous zholoba.

In the middle of the ocean, the most significant mid-ocean ridge is located on the outskirts of the street. First they came to the Atlantic and Indian oceans, and then they came to see the stench come into one back-of-the-world planetary system and stretch from the Icelandic Ocean through the Atlantic and Indian into the Pacific. Tsya girska system, which operates all earthly food, reaching up to 60 yew. Km. Anything similar to mid-oceanic ridges on land Nemaє - aje all girski systems continents, as if the great stench would not boil, all the roses between the depressions of the oceans.

The mid-ocean ridges are large girders with a width of hundreds of kilometers and a height of about 2-3 km. The stench is stored from the decilky parallel mountain ridges. They grabbed them to descend to the ocean bed in wide steps.

Near the most central part of the bridle, the ridges of the ridge cut through the so-called rift gorges. For їх name the entire axis zone of the mid-oceanic ridges is called the rift. Rift gorges and rift zones in the geological relationship, superbly tsikavi. There is a wide range of seismic activity; skin day buvaє up to 100 earthlings. There is a strong flow of heat from the Earth, and volcanic activity is widespread. Near the walls of the rift gorge and on the ridges of the rift ridges lying down to the new rift ridges, the clay rocks of the Earth are exposed. Admittedly, the mid-ocean ridges have been established there, and the great mantle breeds have grown up in the mountains under the infusion of radioactive growth. Smells vychavlyuyuyut up the hill across the trenches of earthly measles, spreading to the side, - looking horizontally, the changing continents and the rise of mountain ridges in the rift zone.

On the ocean lodge there are vuzki, vyagnuty, with steep grapples and peaks of the plateau. The stench may sound like a clayey structure - the blocks of earthly measles have been lifted up the mountain, as they are not strong until earthlings. Before they are referred to: the Lomonosov ridge in Pivnichny Ice ocean, Nazca Ridge in the Quiet and T. D.

Є Another type of sub-water ridges is volcanic ridges. The stench was made with lancers of sub-water volcanoes, how to sit on the zagalny plinth and encircled with their grabbers. For example, the Hawaiian sub-water ridge in the Pacific Ocean. It is drawn to a few thousand kilometers from the central part of the ocean, as far as the Commander Islands. The peaks of the paved part of the ridge stand above the water near the view of the Hawaiian Islands.

On the ocean floor there is a scene and it is so called - wide massifs with strongly sloping grabs. Even more often, cone-like underwater mountains grow on the surface of the shafts. As a rule, there are no volcanoes; stench the stench of majestic coral sporides, as they appear over the surface of the ocean near the view of coral islands - the atols. Yaksho navіt a gassed volcano, sagging its earth crust, if it sinks, without interruption the growing corals begin to drift off the island. If the cold water rises in the water, or if the volcano descends, it will shine so quickly, but the stench is not "Vikradennya" behind it. In the vastness of the oceans (especially in the Pacific), there are free atols. Tse islands Tuamotu, Tubua, Karolinsky, Marshalls, Ellis, Gilberta, Fenix and without lonely atols. A large part of the cich islands is knitted with lancers, which means that the volcanoes begin to grow out of the water. The system of valleys extends the bed of the Pacific Ocean into a series of great valleys: Pivnichno-Zakhidna, Pivnichno-Skhidnu, Marianska, Central, Pivdenna, Bellinshausen, Chiliyska, Panamska.

Є Another miracle is the peculiarity of the Budova ocean bed - this is the name of the zone. It’s high and superbly connected to the smog of a foldably crushed bottom: either steep sloping ledges, or combs and zholobi, or simply folding the rails. The stench stretches for hundreds and thousands of kilometers. Zoni to talk about those who were pricked and shaved, or if they were smitten for sure one one; As a result, the Shvi were established in the earthly crust. The change could be made horizontally, in hundreds of kilometers, and in the vertical direction, for hundreds and two or three thousand meters. Infected vvazhayut, scho head cause The coverage of the zones of breakdowns served as an uneven distribution of earth measles towards the rift zones of the mid-oceanic ridges.

Posted on Allbest.ru

You can see the same "oceanic traps" in the following vocabularies:

Oceanic wastelands of the Holy Avalon and Burin ...

- (a. Submarine ridges, submarine ranges, oceanic ridges, oceanic ranges; n. Ozeanische Bergrucken; f. Dorsales oceaniques; I. Cordilleras oceanicas, sierras oceanicas, cadenas de montaсos oceanicas) linearly vyyagnyuyattya, ... ... geological encyclopedia

Decrease on the surface of the Earth, closed from each side or less from the side. It grows across tens and hundreds (more than a thousand) km. Hiking is tectonic. Tectonic V. regions and trivial sinking of the earth ... ... Velyka Radianska Encyclopedia

The term is old, I will call it oceanic glibokovodnі zholobi. * * * Glibokovaya depressions glibokovodniy depressions, old terms, I will call more oceanic glibokovodnі zholobi (div. Oceanic ... encyclopedic vocabulary

Girski construct one system at the bottom of the Svitovoy ocean to operate the whole earth's kulu. Zagalna dovzhina ponad 60 yew. Km, width up to 2 yew. Km, nominal height 3 4 yew. M, near the top float over the ocean near the viglyad ... ... encyclopedic vocabulary

happy encyclopedia

Girski construct one system at the bottom of the Svitovoy ocean to operate the whole earth's kulu. The courtyard of St. 60 yew. Km, width up to 2000 km, nominal height 3 4 yew. M, near the peaks rise above the ocean at the viglyad ... ...

- (a. Mid ocean ridges; n. Mittelozeanische Gebirgsrucken; f. Dorsales oceaniques mediannes; I. Cordilleras del medio oceano) underwater rise of ocean beds in zones of active spreading (divergence) of lithospheric plates ... geological encyclopedia

Mid-Ocean Ridge- the middle oceanic ridge, girski sporud, which set up one system at the bottom of the Svitovoy ocean, which operates the entire earthly soil. Zagalna dovzhina ponad 60 yew. Km, width up to 2000 km, nominal height up to 4 km, near the peaks rise over ... Іustrovaniy encyclopedic vocabulary

The term is old, I will call it oceanic water-water jolly ... Great Encyclopedic Dictionary

books

Everything about the Earth and the oceans. Infection our divovizna planet is standing in front of you yak on the valley! Report barvisty panoramas show how the earth's crust is pretending, why the islands are located, the mountains and oceanic depressions. ...

Misce, kudi nikoli did not penetrate sleepy light, misce, in which the ocean could hardly be reached without risk for life and for life, deluxe wondrous things, more similar to the planetary forms of life, described by all the writers of life, describing

For this purpose, the intelligence, which is a glimpse of the depressions in the oceans, is followed by a trocha of zupiniti on its designation. Geologists describe the oceanic gulls, as well as deeply depressions or tremors at the bottom. The depth of the oceanic trough should not be less than 5,000 meters.

Such traps are set up through the congestion of the slabs. In these regions, there are most often strong earthquakes and volcanoes. It is possible to say that the deep water troughs of the Holy Ocean are constantly changing: their form changes, the amount of food and glybin changes. Until now, unconcerned about the continuous development of technological progress, set the exact depth of the bagatokh depressions, let’s go without reaching. Like the same spoken vishche, be it zanurennya in the deep water trough of the Svitovoy ocean tied with a great rizik for life in vchenyh. The majestic grip on the glide-water apparatus, which is the strongest for the organism of the people, is not allowed to continue until it is too light, which can be easily imparted from the cosmos. Varto also means that instead of souring in deep-water depressions I don’t change 2, a maximum of 3%, and, all the same, there is a sense of life. Life is marvelous, you can say it is confident, і doesn’t look like you, you can walk on our majestic planet.

Marianska depression

Marianska depression, for how її is called inchenі Mariansky zholob, a sign, mabut, skin school. I will call my name vіn otrimav through those close to him the Marian Islands. For the very reason, I will not name the water trough of the Svitovoy Ocean in honor of the Challenger ship, which, to the word, and vidkriv її, which stood in 1857, was 8,200 meters long. Naturally, the trick is not accurate. Yak bi was not there, Mariansky zholob, more precisely yogo mіsce, I will call it "Bezodnya Challenger", є the greatest misnomer on Earth. "Bezodnya Challenger" is named not in honor of the first ship, but in honor of the ship Challenger II, the team behind the help of the ranger in 1951 set a depth of 10,899 meters deep.

doslіdzhennya Marian trap were conducted with enviable regularity. To the cutaneous vcheny I want to set the exact amount of "No Challenger". On this year's day, three people left only in the special glide-water devices, Vitrimuyut the grip of the grip, descend into the very depths of the Svitovoy ocean. The most recent history took place in 1960. Preslidnik Jacques Pikar together with an important lieutenant of the Navy With the new States of America going down to the dayless. Wonderfully, even in the first place, all the fittings were fixed at 11,512 meters. Pikar buv vvrazhivanii tim, which is practically at the very bottom of the wine, having poured ribs all over the place, as in an unreasonable rank they vitrized the grip of a stoppage of water more than 11 kilometers. The legendary film director James Cameron sank to the bottom of the Marian depression recently, in the early spring of 2012. Winning material on a 3D camera and zooming in on taking samples of water and seeing live organisms, so that you linger in impenetrable weather. Soon, a documentary film will appear on the National Geographic channels, which is based on Kemeron's knowledge of ultra-hot knowledge technology victories. In fairness, it is true that it was unimportant for the last time, numerical probes, until the present moment, the depth of the Marian trap is accurate, but it has a V-shaped form and stretched over 1,500 kilometers, it’s a pity, not a pity.

javanska depression

Javanska depressions do not get involved deep depression v Indian Ocean Ale and enter in the so-called Tikhookeanske in the fire ring: її dovzhina become more than 4,000 km, and the most important place at 7,730 meters is located not far from the island of Bali. The width of the Javanese depression ranges from 10 to 50 (!) Kilometers. On її days, covered by canyons and upstairs, there are permanently active volcanoes, earthquakes are seen. The most promising and restless place in the Indian Ocean was built in the distant 1906 by the command of the ship from Nimechchin under the name "Planets".

Peruvian-Chilean Zholob

The Peruvian-Chilean zholob, which is called the Atakamskiy zholob, which he found in all the world. Yogo dozhina become 6,000 km. Besides, it is rightfully possible to carry it to the widest treks of the Holy Ocean, as one of the seven wonders is known to the world: its width is 90 kilometers. The most popular place of the Peruvian-Chilean zholob is located in the depression of Richards: for the rest of the data of its depth, it is practically 8070 meters. Yak and deeply trapped, Atakamskiy zholob is constantly seismically active. The number of earthquakes and the rise of volcanoes are often the reason for the occurrence in the whole region of giant hwil - tsunamis.

Aleutska Zholob

Looking at the glibokovodnі sea trails of the Svitovoy ocean, it is hard not to guess Aleut zholob, which stretched from Alaska to Kamchatka. Tsei zholob, in the context of Peruvian-Chilean, the call is not great: it’s a little more than 3,400 kilometers, and the axis best glybin, Registered with an echolot - mayzhe 7,700 meters. Tsikavo those who are not satisfied with the result of the creation of the American and Pacific plates. Undovzh zholobi slabs wiggled and made the cloud, all the good things, the Aleutian Islands.

Japanese depression

The Japanese depression stretches "all" for 1,000 kilometers at the entrance to the Pacific Ocean, and it is V-shaped and shaped not far from the islands of Hokkaido, Bonin and Honshu. At the given moment, the maximum amount of glybin was taken to increase the glybin at 8,412 meters... In 1989, the expedition went far into the distance to the specified level of 6 525 meters, the distance from the distance became not safe. In 2008, the Japanese socially with the English zoomed to reach 7,700 meters of water, and they took pictures of ribs and their living organisms. It’s a pity, you see ribs that linger on such slopes, it’s practically unwise, it’s hard to go to the surface, as it’s just going to break out in a vice. Japanese zholob to get involved in active seismic zone The very fact that the Japanese islands endure are often suffering from earthquakes and great tsunamis, as they pop up from the crust of plates.

Globokovodnі trischini Svitovoy oceans, as one of the 7 wonders of the underwater svіtu

Unimportant to those who have trapped in the Svitovoy Ocean until the end of the day, they have rightfully been brought up to one seven wonders of the water world... In a whole lot of nothing wondrous, even those who are crazy about people, should be important to explain from a scientific point of view. On the other hand, it is not clear to the full extent that the processes take place in the setting of large, wide and wide fractures. It’s too unfortunate, і explain, as on such depths, kudi nicoli did not penetrate the sleepy light, and the grip of water 1070 times the atmospheric, lifeless life. First they showed the rest of the life, the fauna there to reach the richness. A large number of organisms are able to cope on such depths as they follow the additional light signals, such as vipromyuyut їkh tila. Riddles of glibokovyh sea gorges of the Svitovoy ocean hvilyuyut people nіtrohi not less, nіzh riddles, as to put in front of us Vsesvіt. And what about some of the main miracles, not just underwater light, but the efforts of our planet?