What is the name of the sea between England and France. Tunnel between England and France. Geographical position of the English Channel
It is called Dover. The Eurotunnel passes under its bottom. This is the famous English Channel, which is a surprisingly curious piece of land. And it is interesting not only for its landscapes, but also for its origin. What is the name of the narrowest part of the English Channel? Its location and features will be discussed in this article.
Geographical position of the English Channel
The strait connects the Atlantic Ocean with the North Sea. Its length is 578 kilometers, the width in the western part is 250 km, in the eastern part - 130 km. The smallest depth is 23.5 meters.
It is important to note that a unique tunnel has been built between the cities of Calais and Dover (as the narrowest part of the English Channel is called, we will learn a little lower).
More than 52 km (38 km of the route is located directly under the strait) is its length.
The main ports are Le Havre, Portsmouth, Cherbourg and Southampton. There are also islands, the largest of which are located off the coast of Great Britain (Isle of Wight) and off the coast of France (Channel Islands).
The history of the formation of the island of Great Britain
In ancient Rome, this strait was called Oceanus Britannicus, which translates as "British Ocean". As time went on, it got smaller and smaller. In it had the name - "British Sea", and today the sailors call this place simply "the sleeve" (The Sleeve).
Theoretically, on the site of the English Channel in ancient times there were low-lying lands (something like the Netherlands). Then the level of the sea surface began to rise and fill the vast valleys with ocean waters. This place became the bottom of the current strait that separated Great Britain from the mainland.
Before we find out which is the narrowest part of the English Channel, let's consider another theory of the origin of this strait.
A new version
More than 20 years ago, another, one might say, catastrophic theory of the development of events appeared. Most geographers perceive it as a bit far-fetched.
In the journal Nature, a scientific article by London-based scientists from Imperial College was published, which stated that the strait separating Great Britain and France was formed as a result of other natural processes. They believe that the cause of the birth of the English Channel was the catastrophic outflow of water from a huge lake, which was formed as a result of the confluence of the Rhine and Thames in the Ice Age.
Sanjeev Gupta, the head of these studies, said that more than 420 thousand years ago, Britain and France were connected by the Veld-Artois anticline. This is a chalk ridge, the height of which reached 180 meters precisely in the area of the strait under consideration, and lowlands lay in the western part of it. Water from the Rhine, Thames and other rivers flowed here through the North Sea.
And when the glaciers blocked the river water began to accumulate in a closed space, subsequently forming a huge lake, which was fed by rivers and the melting of the glacier.
What is the name of the narrowest part of the English Channel, its location
This site is located between the mother part of Europe and the island of Great Britain.
This is a magnificent place with beautiful landscapes, where on a clear sunny day you can see the buildings located on the other side of the strait, and at night you can see bright luminous lights.
The narrowest part of the English Channel is called the Pas de Calais or the Strait of Dover. Its width is only 32 km. It is located just between the French city of Calais and the English port of Dover. A passenger boat crosses the Pas de Calais in 1.5-2 hours. In this place, under water, the Eurotunnel was built.
Description
There is an expression in geology - a megaflood. They denote events that have occurred over the past 500 years in the territory that is now a water barrier between the islands of Britain and the continent. It's about about the same La Manche.
Translated from French, the English Channel means "sleeve". In the UK it is called the "English Channel". Its length is about 560 km, and its maximum width is 240 km. Approximately 34 km wide is the narrowest part of the English Channel.
Curious facts about the strait in general
- During the First World War, the Heards Deep depression, located at the bottom of the English Channel, was used by the British to bury chemical weapons. And after World War II (1941-1945), German weapons were flooded here. From 1946 to 1973, radioactive isotopes were buried here.
- The very first swimmer in human history to swim across the English Channel was Matthew Webb. This swim in 1875 lasted almost 22 hours (15 minutes less).
- Eurostar trains travel through the Eurotunnel at a speed of 160 kilometers per hour.
- On one of the islands of the strait called Sark, feudalism remained until 2008. The island was ruled until this very moment by the last island in Europe with this kind of management.
- A giant eel lives in the English Channel, the weight of which exceeds 100 kilograms, and the length reaches 3 meters.
- the only Railway operates on the island of Alderney (Channel Islands), built in 1847. Its length is 3 km. It works only in the summer and only on weekends and holidays.
We learned the name of the narrowest part of the English Channel, found out the history of the strait itself and realized that this place is one of the most interesting corners of the planet Earth.
The relief of the bottom of the English Channel
The bottom of the English Channel (English Channel) has a steep slope to depths of 25-50 m. To the southwest of Great Britain, this slope is composed of Paleozoic rocks and is cut by terraces, which are submerged platforms leveled by waves, bounded by ledges above and below. The foot of the most significant ledge is located at a depth of 45 m. Below the coastal zone is the bottom of the English Channel. usually flat, gradually decreasing to a maximum depth, which increases from B by 3 from 35 to 110 m. The monotony of the flat bottom is broken by three structures:
1) shoals and islands occurring at 3 from 2° W. and consisting of volcanic and metamorphic rocks 2) alluvial sediments - sandbars in the easternmost part of the English Channel and sand bars in the western 3) depressions; the largest is Hurd (from 49° 55" N, 2° 00" W to 49° 20" N, 4° 00" W). Virgins (49° 2" N, 4° 40" W) and Ouessant (48° 30" N, 5° 15" W).
The depressions have a number common features: they are all narrow troughs with parallel slopes, with the northern slope usually steeper. They are located in areas of development of Mesozoic rocks. Their origin is unknown. The origin of minor depressions near Great Britain is explained by the erosion of loose rocks by tidal currents.
Geology and history of the development of the English Channel
The western part of the English Channel is framed by Paleozoic rocks, the eastern part by Mesozoic and Cenozoic. The bottom of the English Channel is almost entirely composed of Cretaceous and younger rocks. Outcrops of Jurassic rocks in the western part are very few. The eastern part is crossed by the Vsldian anticline and its extension to Boulogne. The continuation of the northern flank of the anticline through the Pas de Calais (Strait of Dover) was proven by detailed geological surveys that were carried out to tunnel under the bottom of the strait. The rest of the bottom of the English Channel is mainly synclinal with the preservation of Upper Cretaceous and Tertiary rocks.
The geological succession of the sediment layers is incomplete: there are unconformities at the base of the Devonian red sandstone, at the base of the sediment layers of the Upper Cretaceous, Paleogene, Pliocene and modern sediments. Tertiary rocks were found on the continental slope in the area to the southwest of the English Channel at depths from 900 to 2500 m. It is assumed that in this place there should be their exposure. It is assumed that in the western part of the English Channel there was a depression in which sediments accumulated during the Triassic. But apart from this assumption, there is no data indicating the existence of the English Channel before the Tertiary period. Apparently, it was formed as a result of folding and subsidence of the earth's crust, possibly in the post-Eocene era, accompanied by erosion of Tertiary rocks and, to a lesser extent, older rocks.
Bottom sediments of the English Channel
In many places in the English Channel, bedrock can be raised by a shock tube, since the thickness of the layer of bottom surface sediments does not exceed a few centimeters. The absence of constant accumulation is the result of the activity of tidal currents, the speed of which throughout the entire English Channel reaches 1.5 knots, and in some places during spring tides and 3 knots. The sediments that are found in the English Channel are divided into two types. The first type is pebbles, material too coarse to be moved by existing currents, the second type is coarse sediment that is carried by tidal currents. The pebble is characteristic of the area adjacent to the coast of France, between the island of Ouessant (Ushant) and Cape Ag, but it has also been found in many other places.Pebbles are often well rounded and, apparently, under the action of waves since the Pleistocene, they are in their present position. The second type of sediments, apparently, is represented by fine-grained sand, which was formed as a result of the destruction of the Upper Cretaceous rocks.
In addition, the sand contains fragments of Paleozoic rocks brought from land. Quartz sand occurs in the area south of the Devonian and Cornish coasts, and may have been formed as a result of the destruction of underwater exposures of the "new red sandstone". In other places, sandy sediments consist of crushed shells and bryozoans. Silt is found only in a few small areas near the coast.
Every year, about 600 m3 of sand enters the North Sea through the Pas de Calais. It is believed that the sand moves further by 3, to the edge of the continental shelf. Sand ridges are not found to the E of the line passing along 3 ° W. d.; to the west of this line they exist and move in a westerly direction. There are no sand banks in the English Channel, with the exception of its easternmost part.
Hydrological regime of the English Channel
The climate of the English Channel area is moderate windy, cloudy, rainy. In winter, the entire water column moves towards B, while in summer, apparently, there is a movement of surface water from the coast and deep water to the coast.
Salinity reaches its maximum, and the temperature becomes minimum at the end of winter (35.3 ppm, 9-10°C in the western part and 6-6.5°C in the east). In summer, salinity drops by
0.1-0.5 ppm, the temperature of the surface layer reaches 15-17°C. Significant interannual fluctuations are observed. East of the meridian 2° W. due to strong tidal mixing along the vertical, the water remains homohaline and homothermal throughout the year, while to the west a significant thermocline forms and the temperature in the bottom layer does not exceed 10-11 ° C. Summer storms destroy this thermocline. Due to technical difficulties, the important area of the Channel Islands has been little explored.
In the Alderney Strait, the speed of the spring tidal current reaches 9.7 knots. It carries to the eastern part of the English Channel a large number of water that becomes rich in nutrients in the mixed waters of the Channel Islands. The waters of the Atlantic enter the North Sea through the English Channel and the Pas de Calais, although this direction of flow can be reversed due to winds blowing from the North Sea. In autumn, winter and spring, water comes mainly from 3 or NW, but in summer water comes from the SW, from the area where the temperature jump layer is located.
English Channel. Between England and FranceThe English Channel is one of the most famous maritime shipping routes in the world. Cliffs drop sheer into its waters on the French coast, in Normandy.
The English Channel is called by the French and the whole world. The English - with the patriotism of the islanders and perseverance, worthy of respect. - they call this strait the English Channel.
Looking at history, one might think that the strait itself “plays” for England, because it saved her many times from continental invaders. However, the English Channel is equally harsh to everyone: its waters have become the grave of millions of people and ships. However, at the end of the XX century. he still managed to be tamed, the breakthrough of the tunnel is one of the longest in the world.
WATER BARRIER
The English Channel is a French name. The British call this strait the British or (in direct translation) the English Channel. The latter has an older origin:
The ancient Romans called the body of water separating Britain from the continent Mare Britannicum, or the British Sea. 
In the II century. BC e. the ancient Greek scientist Herodotus called this water isthmus "Oceanus Britannicus". An interesting situation has developed around the name "English Channel". The French version has been known since the 17th century. and means sleeve. The Spaniards called the strait El Canal de la Mancha, the Portuguese called Canal da Mancha, the Italians La Manica, the Germans Ermelkanal.
The desire of each of the peoples to remake the name in their own way betrayed a persistent desire to claim ownership of these small, but significant waters. Control of the strait provided colossal advantages. Firstly, it was the closest route to England, and secondly, the shortest route to the Baltic Sea. Despite the wayward nature of the English Channel - frequent fogs, gale-force winds, high tides and treacherous currents - political and commercial importance outweighed all natural barriers.
According to the most rough estimates, the remains of several million people and tens of thousands of ships lie at the bottom of the strait: from Roman galleys to diesel submarines. Such is the price of the centuries-old battle for the strait.
None of this would have happened if the British Isles had remained part of continental Europe 10,000 years ago, during the last glaciation (Pleistocene). But the land in these places lay 120 m below sea level, and as the glaciers melted, water filled the lowlands, forming what we now call the English Channel.
In times of peace, the strait served noble purpose: was a kind of water bridge, through which there was a cultural exchange between the Celts and the peoples of inner Europe, contributing to the formation of new languages and nationalities. This is indicated by the obvious similarity of many dialects and customs common on both sides of the strait.
However, in difficult times for the population of Britain, the strait became a natural barrier to the conquerors, although not for everyone. The ancient Romans managed to successfully cross the strait and conquer Britain in the 1st century BC. n. e., Normans in 1066, William III of Orange in 1688
Beginning with Elizabeth I (1533-1603), the policy of the English kings in the area of the strait was to prevent an invasion of England from the continent. To do this, the British ensured that none of the major European powers controlled important ports on the other side of the strait. The formation of the British Empire would have been impossible if the British had not established the most severe control over the English Channel in their time.
The rise of England as "Queen of the Seas" began after 1588, when the Spanish "Invincible Armada" perished along its coast, partly in the English Channel, where it was covered by one of the fierce English Channel storms. On the occasion of the victory, Queen Elizabeth III ordered the minting of a medal with the Latin inscription Adflavit Deus et dissipati sunt ("God blew - and they scattered").
France tried twice more to conquer England: during the Seven Years' War (1756-63) and during the Napoleonic Wars (1800-15). Both times the "guests from the continent" gathered a huge fleet, but never invaded the island. A significant role was played here by all the same famous English Channel winds and storms, which, to spite the French, began on the most favorable day for the invasion.
Whatever name the strait bears and whoever it belongs to, it applies equally to sailors on both sides. Hurricane winds, heavy rain, giant waves, high tides and thick fog are common in quiet places. Before the opening of the Eurotunnel, bad weather created big problems for ferries. 
NEW HORIZONS
20th century showed that the importance of the English Channel as a defensive line did not decrease at all even with the development of aviation and rocket science. But with the end of the era of world wars, the English Channel again became a link between England and Europe.
Fisher, First Lord of the British Admiralty, declared shortly before the outbreak of the First World War: "Five keys keep the world shut: Singapore, Cape Town, Alexandria, Gibraltar and Dover." The importance of the English Channel port of Dover remained decisive for the defense of the strait. 
On July 25, 1909, Frenchman Louis Blériot crossed the English Channel for the first time in his monoplane, starting at Calais and landing at Dover. The British were made clear that the English Channel was no longer an insurmountable barrier to enemy troops. In addition, Germany began to hastily build submarines, which was an even greater threat to England. The British had to fight on land in order to get close to the German submarine bases, but only in 1918, when the war was drawing to a close, the threat of an invasion of England from under the water was finally eliminated during the famous Zeebrugee Raid and the complete naval blockade of Germany .
During World War II, the theater of operations at sea moved to the Atlantic, as the shallow waters and narrow inlets of the English Channel were too dangerous for large-capacity ships. Having abandoned a direct invasion (Operation Sea Lion), the German troops concentrated on submarine warfare, laying minefields and rocket-and-artillery attacks on England across the strait.
In May 1940, the British Expeditionary Force, which fought on the side of France, retreated through Dunkirk along with the remnants of the French army under the onslaught of the advancing German army. It was the most ambitious rescue operation in the history of wars: in just a few days, 338 thousand soldiers were evacuated during Operation Dainemo
During 1940-1945, the Germans built the most powerful fortifications on the continental side of the strait, called the Atlantic Wall. Many have survived to this day, becoming tourist attractions. German troops managed to occupy several islands in the strait, but did not advance further. The Atlantic Wall fell in 1944, during the opening of the Second Front and the implementation of Operation Overlord to land Allied troops in Normandy. 
After the end of the war and with the beginning of the unification of Europe, the issue of transport links between the British Isles and the continent became acute. Ferry crossings were morally and technologically outdated and could not cope with the transportation of goods, cars and railway cars. About 3.5 million people lived on the banks of the English Channel, in dire need of a modern crossing.
The idea of building a tunnel under the English Channel has a long history. Back in 1802, the French engineer Albert Mathieu-Favier proposed a project for a tunnel for traveling in carriages by the light of oil lamps. There were other projects, and even construction began: twice in 1876 and 1922, but both times the construction was frozen for political reasons. 
Tunnel in the English Channel, "Channel"
New project was launched in 1973 The underground crossing was opened in 1994 and was named the Eurotunnel. This is a double-track railway with a length of about 51 km (39 km under the English Channel). Thanks to the tunnel, it is now possible to get from Paris to London in 2 hours and 15 minutes; in the tunnel itself, the trains are 20-35 min.
Channel Tunnel photography
1. The Channel Tunnel is the world's longest underwater tunnel that runs under the English Channel and connects England with France. 
2. The length of the tunnel is 50 kilometers, 38 of them are laid under the seabed. The tunnel under the strait was opened in 1994 as part of a modern transport system. 
3. Over the past 200 years, many ways have been proposed to overcome the English Channel. The tunnel project was proposed in 1802, and after 90 years the development of the project began.
4. Even Napoleon III suggested crossing the strait. So Queen Victoria, in agreement with Napoleon III, approved a new French tunnel plan in 1860, and construction began, however, the tunnel did not advance further than 2 km. 
5. Now there are three tunnels: two railway and one service, the distance between each is 30 meters. On the English coast, work began in December 1987, and on the French coast a little later. Both sides spent a month laying each kilometer. The tunneling took three years. 
6. The tunnels are laid 45 meters below the seabed. 
7. Thanks to the tunnel, you can easily visit London from Paris in just 2 hours and 15 minutes, given that the trains are in the tunnel itself from 20 to 35 minutes. 
8. The diameter of the tunnels is 7.3 meters, the length of each tunnel is about 50 kilometers, of which 38 pass under the water. 
9. The tunnel under the Channel is a truly grandiose tunnel, it is also called the "Eurotunnel". 
10. Cars carry trains, cars simply enter special cars and leave at the other end. 
11. The tunnel was opened in 1994 on May 6, Elizabeth II and President Mitterrand. This is how we saw the Channel Tunnel and its photographs.
CURIOUS FACTS
Herds Deep - a depression at the bottom of the English Channel - was used by the British during the First World War to bury chemical weapons. After the Second World War, German weapons were flooded here. Similar operations continued until 1974. In the period 1946-73. the depression was used to flood radioactive waste.
Eurostar trains travel through the Eurotunnel at a speed of 160 km/h.
The Channel Islands, which are part of the two crown dependencies of Jersey and Guernsey, are under the jurisdiction of the British monarchy, but are not part of the UK and are not part of the EU, although they are part of the customs territory of the EU.
On about. Sark (Channel Islands) until 2008, the feudal system of government was preserved - the last in Europe. The island was governed by a council of elders.
The giant sea eel, or conger, living in the English Channel, reaches a length of 3 m and weighs more than 100 kg
On about. Alderney (Channel Islands) operates the only railway on the islands. Built in 1847, 3 km long, open only in summer, on weekends
and holidays.
British swimmer Matthew Webb was the first in the history of mankind to cross the English Channel in 1875 in 21 hours and 45 minutes. The slowest swim across the strait - 28 hours 44 minutes. (Jackie Cobell, UK, 2010).
The British Isles are separated from the rest of the continent by a narrow channel between the North Sea and the Atlantic Ocean. We have collected several interesting facts about this narrow isthmus.
The strait between France and the British Isles we know as the English Channel French name. And the British call it the English Channel - theEnglishChannel , thereby as if claiming their rights to it. Most other countries use names borrowed from French, such as "el Canal de la Mancha" in Spanish.
The narrowest point of the English Channel is the Strait of Dover or Pas de Calais: on the one hand, there is the city of Dover, on the other, the French coast of the Hauts-de-France region. The width of the strait in this part is only 37 km: the opposite side is perfectly visible in good weather.
The English Channel was formed relatively recently by geological standards: only 200 thousand years ago. In those days, there was a lake in the North Sea region, bounded by a glacier. The waters of the lake broke through the glacier and caused a huge flood, as a result of which the isthmus between modern Britain and France was washed away.
The English Channel had an important defensive function for Britain. Although the width of the strait is small, and it could be overcome even on ancient ships (the Romans, the Normans, and William of Orange sailed to the islands), the journey was rather difficult. Strong currents, tides, squally winds, thick fogs destroyed many ships.
Experienced swimmers can swim across the Pas de Calais. The first person to swim across the strait without a life jacket was Briton Matthew Webb, who took almost 22 hours. The time record was set by Australian swimmer Trent Grimsey in 2007 - only 7 hours. Surprisingly, in the entire history of the strait, fewer people swam across than Everest conquered: only about a thousand people. 
Due to currents and weather, the water temperature in the English Channel does not rise above 18 degrees even in summer, and usually stays around 15-16 degrees during the warm months. At the same time, the strait does not freeze in winter - even ice does not form near the coast. This is due to the warm current of the Gulf Stream.
Under the Pas de Calais, the Eurotunnel was built, which connects the UK and France - the cities of Dover and Calais. Its length is 51 kilometers, 39 of which lie under water. It is the third longest railway tunnel in the world. It was even included in the list of modern wonders of the world.
Now you know about the English Channel no less than the British. The main thing is not to forget to call it correctly in English - the English Channel, because it's easy to forget and say the French version, and the British are unlikely to like it.
The English Channel, which separates the coasts of France and Great Britain, has always played a very important role in history. Many nations sought to lay claim to this narrow strait, which was reflected in the difference in its names. The ancient Greeks called the water isthmus "Oceanus Britannicus", the Portuguese and Spaniards - the da Mancha channel, the Italians called it La Manica, and in the German lands the strait was called the Ermelkanal. But the modern name came from the French language, in translation from which the name of the strait means "sleeve". Although the inhabitants of the British Isles stubbornly continue to call it the English Channel.
The English Channel (together with the Pas de Calais) connects the North Sea and the Atlantic Ocean, has a relatively short length - 578 km, and its width ranges from 32 km to 250 km.
History of the English Channel
The English Channel has always been at the center of historical events, since control over it gave great advantages: it was the shortest way, both to the Baltic Sea and to the shores of Britain. Navigation along the strait was fraught with many difficulties - the weather here is very changeable, strong winds often blow, thick fogs descend. Combined with the complex nature of the currents and high tides, crossing this waterway has always been a challenge. But the commercial and political significance of the strait outweighed all obstacles.
Despite the insidiousness of the English Channel, many conquerors were able to overcome it. Even in the first century, the ancient Romans crossed the strait, in 1066 the Normans landed on the coast of Britain, and in the 17th century - William of Orange. But still, the water isthmus protected the British well: scientists believe that at the bottom of the strait there are skeletons of tens of thousands of ships from different times and peoples.
Since the mid-16th century, English monarchs have established tight control over the English Channel, using frequent storms and their rebuilt ships to protect against the encroachments of the Spanish and French fleets. The port of Dover played a special role in the defense of the strait.
However, with the advent of airplanes, the strait ceased to be a reliable barrier for enemy troops, and the creation of submarines further aggravated the situation. The British had to resort to a complete naval blockade of Germany in 1918 to ward off the threat of an invasion of the islands.
German troops returned to the English Channel at the beginning of World War II, despite the impossibility of using large ships there (the strait is too shallow for them). Realizing that a direct invasion was impossible, the Nazis set up many minefields and led fighting in the strait with the help of submarines, and also fired at the coast.
At the beginning of 1940, British troops were evacuated to the islands from the continent during Operation Dainemo, which went down in history as the largest military rescue operation. The Nazis created the strongest fortifications on the continental coast ("Atlantic Wall") and occupied several islands in the strait. These fortifications were recaptured from the Germans during the Allied landings in Normandy in 1944.
After the end of the war, the English Channel began to play a key role in the unification of Great Britain and continental Europe - a huge flow of goods was transported using ferries. There was a need for a new type of transport communication, and in 1973 a project was launched to build an underwater tunnel. Such projects existed before: in 1802, it was proposed by the French engineer A. Mathieu-Favier, and in 1876 and 1922, construction even began, which was stopped due to various political problems.
Construction was carried out from two sides - English and French, and the accuracy of passage in the tunnel was controlled by a laser positioning system. On May 6, 1994, the underground path was opened and named. Now the road from the continent to the island takes 2 hours and 15 minutes, and the train moves under water for about half an hour.
Strait today
Today, the strait still plays a huge role in the life of the peoples inhabiting its shores and islands, keeping their history and traditions.
On the banks of the English Channel, some historical sights have been preserved: the 13th century Cornet castle, forts, the ruins of the Atlantic Wall, Brittany lighthouses. The infamous Heards Deep at the bottom of the strait - in the First world war the British flooded it with chemical weapons.
On the island of Sark in the English Channel, until 2008, there was a feudal system of government, the only one in Europe when the island was ruled by elders.
The English Channel has always been of interest to athletes and researchers. In 1909, the French pilot Blériot flew over the strait for the first time and landed in Dover, and in 1912 his flight was repeated by the first woman, an American G. Quimby. In 1974, a researcher from Wales, B. Thomas, crossed the English Channel in an Indian bull boat, trying to prove the common origin of Welsh and Indian boats.
The conquest of the wayward strait took place not only on vehicles - about 900 people overcame it by swimming, struggling with high waves, currents and wind, being in water with a temperature of no higher than 18 degrees.
The championship in this overcoming belongs to the Briton M. Webb, who swam the English Channel in 21 hours and 45 minutes. in 1875. The record for time belongs to the Bulgarian P. Stoychev - he swam across the strait in 6 hours 57 minutes and 50 seconds in 2007.
In women, the record was set by the Czech athlete I. Glavachova in 2006, swimming across the strait in 7 hours 25 minutes and 15 seconds, and for the first time a woman ventured into such a swim in 1912 (American G. Ederle).
The famous strait continues to inspire new records and achievements of athletes and engineers, and it is likely that many more realized ideas and implemented projects will be associated with it.
English Channel - VIDEO
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