Saudi Arabia political map. Saudi Arabia map

ARABIAN PENINSULA

Arabian Peninsula

on Yu.-Z. Asia. From the II millennium BC. e. Peninsula inhabited by Arabs; his Arab, the name of Jezira al-Arab - "peninsula of the Arabs" (less often they use Bylyad al-Arab - "Country of the Arabs") . The area inhabited by the Arabs is Arabia, but Russian traditional Arabia, which is due to the borrowing of this name from Greek; from him and the Arabian Peninsula.

Geographical names of the world: Toponymic Dictionary. - M: AST. Pospelov E.M. 2001 .

ARABIAN PENINSULA

to the southwest Asia, the largest in the world. It is washed by the Red Sea, the Gulf of Aden and the Arabian Sea, the Gulf of Oman and the Persian Gulf. The shores are slightly dissected, plains and plateaus prevail, passing to the coasts into the marginal mountains. Off the coast of the Persian Gulf - the largest oil fields. The climate is tropical, dry, subtropical in the north. In summer, temperatures up to 55 °С are observed. Precipitation on the plains is 50-100 mm, in the mountains up to 500 mm per year. The channels of temporary streams - wadis are characteristic. Rocky and sandy deserts, in the mountains - areas of sparse forests and savannas.

Brief geographical dictionary. EdwART. 2008 .

Arabian Peninsula

(Arabian Peninsula), the largest in the world (area 2730 thousand km²) in the SW. Asia, washed by the Red and Arabian Seas, the Persian Gulf. Indian Ocean. Sev. the boundary is drawn along 30° north latitude. The peninsulas are stretched along the meridian for 2 thousand km and in latitude for 2.8 thousand km. It is inhabited almost exclusively by Arabs, hence the name of the peninsula. B.ch. takes Saudi Arabia , and Kuwait , Yemen , United Arab Emirates , Qatar And Oman . Jordan and Iraq are partly located on the peninsula. The peninsula is formed by the Arabian Platform, one of the fragments of the ancient supercontinent Gondwana. Southwest and southeast. edges occupy mountain ranges with max. 3760 m high. Plateaus and plains gently descend from them to the NE. Along the shores of the Red Sea there is a narrow strip of Tihama lowlands. The coastline is slightly indented, there are few convenient bays. The peninsula is located almost entirely in the zone of tropical deserts, preim. sandy and rocky. Wed-mon. the temperature of July is almost everywhere approx. 30°C or higher (max. 54°C). January temperatures are from 7 to 24 ° С. Precipitation in the plains is 100 mm/year, and in the mountains 500 mm/year. There are no permanent rivers, there are numerous dry channels - wadis. In deserts, vegetation is sparse or absent. In the mountains, there are savannas and sparse forests in places. On SW. the peninsula is the Arabian artesian basin. Islam, one of the world's leading religions, was born on A. p. It is professed by the vast majority of the inhabitants of the peninsula. Here in the cities Mecca And Medina , are the main shrines of Islam. On the coast and in the waters of the Persian Gulf. concentrated b.h. world oil reserves. Extensive sandy beaches, beautiful Coral reefs near the coast, monuments of the Middle Ages. architecture, east exotic and contemporary service make the peninsula attractive for tourists.

Dictionary of modern geographical names. - Yekaterinburg: U-Factoria. Under the general editorship of Acad. V. M. Kotlyakova. 2006 .

Arabian Peninsula

in southwest Asia, juts out into the Indian Ocean, the seas and bays of which are washed (Gulf of Aqaba, Red Sea, Gulf of Aden, Arabian Sea, Gulf of Oman, Persian Gulf). Most of the peninsula is occupied by Saudi Arabia. Yemen and Oman are located to the southeast. coast, and Kuwait, United United Arab Emirates and Qatar in the north. Partially on the peninsula are Jordan and Iraq. Sev. the boundary is drawn along the line 30 ° N. sh., connecting sowing. extremities of the gulfs of Aqaba and Persian. Sometimes this border is drawn according to the state. Saudi Arabia's borders with Jordan and Iraq. Pl. 2730 thousand km² (the largest peninsula of the Earth). They are stretched along the meridian for 2 thousand km and in latitude for 2.8 thousand km. The coastline is slightly indented, good bays few. Formed northeast. part of the ancient Afro-Arabian platform. Volcanic eruptions and outpourings of basalts that once occurred formed extensive covers. In the northeast direction, the foundation of the platform is gradually submerged under the Meso-Cenozoic deposits. In the same direction, mountains and plateaus are replaced by plains, which are gently inclined towards Mesopotamian lowland. and the Persian Gulf. Max. high 3760 m, plateaus and plateaus in cf. 1800–2300 m, plains less than 1000 m, near the Persian Gulf less than 200 m. parts of the peninsula inclined layers of sandstones, limestones and clays form a series of cuesta heights. 300–400 m and a length of more than 1200 km. There are karst landforms on limestones. Between the mountains and the coast of the Red Sea is a narrow strip of the Tihama lowland. On S.-V. peninsula near the coast in the waters of the Persian Gulf concentrated a significant part of the world's oil and natural gas reserves. The climate is tropical, with trade winds; in the north, subtropical with winter precipitation. Average monthly air temperature to the center. parts of the peninsula in July 33.4 °C (max. 55 °C), in January 14 °C. Precipitation in the plains is from 100 to 300 mm per year, in the mountains 500, in some places up to 900 mm per year. Almost the entire peninsula is occupied by sandy and rocky (hamad) deserts (Great Nefud, Rub al-Khali, etc.). There are few permanent rivers, numerous dry channels - wadis. There are oases around wells and water sources. Vegetation is sparse or absent. In the mountains, there are savannas and sparse forests in places. There are many coral islands and shoals off the coast in the Red Sea.

Geography. Modern illustrated encyclopedia. - M.: Rosman. Under the editorship of prof. A. P. Gorkina. 2006 .

See what the "ARABIAN PENINSULA" is in other dictionaries:

Coordinates: Coordinates ... Wikipedia

On southwest Asia, the largest on Earth (over 2.7 million km²). It is washed in the west by the Red Sea, in the south by the Aden Hall. and Arabian m., in the east the Omani and Persian Gulfs. Indian ca. Plains and plateaus prevail, in the west, south and east ... ... Big Encyclopedic Dictionary

Arabia (from other Hebrew. Arab desert), the largest peninsula of Asia, in the southwest of the mainland. It is washed in the west by the Red Sea, in the south by the Gulf of Aden and the Arabian Sea, in the east by the Gulf of Oman and the Persian Gulf. northern border A. p. is usually carried out ... ... Great Soviet Encyclopedia

In the southwest of Asia, the largest on Earth (over 2.7 million km2). It is washed in the West by the Red Sea, in the south by the Gulf of Aden and the Arabian Sea, in the East by the Gulf of Oman and the Persian Gulf of the Indian Ocean. Plains and plateaus predominate, on ... ... encyclopedic Dictionary

Arabian Peninsula- in South-West Asia. From the II millennium BC. e. n ov is inhabited by Arabs; his Arab, the name Jezira el Arab pov Arabs (less commonly used Bylyad el Arab country of the Arabs). The area inhabited by Arabs, Arabia, but Russian. traditional Arabia, which is due to ... ... Toponymic Dictionary

In Croatia, the peninsula is a piece of land that is adjacent to the mainland or island on one side, and surrounded by water on all other sides ... Wikipedia

PENINSULA, a piece of land that extends far into the sea, lake or river and is surrounded on three sides by water. Largest peninsulas Arabian, Hindustan, Indochina... Modern Encyclopedia

Peninsula- PENINSULA, a piece of land that extends far into the sea, lake or river and is surrounded on three sides by water. The largest peninsulas are Arabian, Hindustan, Indochina. … Illustrated Encyclopedic Dictionary

Saudi Arabia- (Saudi Arabia) History of Saudi Arabia, political structure Saudi Arabia Sights of Saudi Arabia, economy of Saudi Arabia, culture of Saudi Arabia, Riyadh, Jeddah, Mecca, Medina Contents Contents Section 1.… … Encyclopedia of the investor

The Arabian Peninsula is a peninsula of Asia. One of the most large peninsulas our planet - Arabian, which is located on the border between Africa and Asia. Endless desert plateaus and low mountains cover most of the peninsula. Contrary to expectations, Arabian landscapes do not look boring and monotonous. These Amazing places are extremely rich in unique natural attractions and hide many unsolved mysteries.

One of the most impressive natural beauties of the peninsula is the Shammar Mountains, formed by pink granite rocks.

In the rays of the setting sun, pink mountains with individual bright red inclusions of ore look fantastically beautiful. According to local legend, these red spots are the blood of the biblical fratricide Cain, forever baked on stones as a reminder to posterity of a terrible crime.

Video - STG. Arabia: camels, pipes, RMT

No less interesting is the Al-Hijaz mountain range, which stretches along the coast of the Red Sea. The slopes of the mountains covered with black frozen lava amaze with their gloomy, mystical beauty. The peculiar mysterious atmosphere of these places is enhanced by the mournful, harp-like sounds emitted by the singing dunes that adjoin the northern part of Al-Hijaz.

An eerie and at the same time fascinating impression is made by the Red Desert, so named for the unusual color of the sand - red, almost crimson. From a distance, this mysterious desert resembles a sea of blood. Its entire surface is dotted with furrows and funnels, in which small oases and springs are often hidden.

A trip to the Arabian Peninsula will not only allow you to admire the wonderful landscapes, but also make a trip through the desert on camels, get acquainted with the lifestyle of the Bedouins, and participate in a jeep safari on the dunes.

The beauty of the Arabian nature and extreme entertainment attract many tourists from all over the world to the Arabian deserts. Even more popular are the coastal regions of the peninsula, washed by the waters of the Arabian and Red Seas, the Persian, Aden and Oman Gulfs, and attracting many lovers to these parts. beach holiday. There are a huge number of resorts on the coast, both expensive and elite, and accessible to tourists with not very high income.

Saudi Arabia Panoramic Walk

Almost all states located on the Arabian Peninsula (United Arab Emirates, Yemen, Saudi Arabia, Bahrain, Oman, Kuwait, Qatar) pay considerable attention to the development of tourism. The most developed tourist infrastructure in the UAE. In popular resort centers of this country: Dubai, Abu Dhabi, Sharjah, Fujairah you can spend a fantastic vacation enjoying natural resources and great service.

For the most sophisticated and demanding tourists, a holiday in Abu Dhabi, which is rightfully considered one of the most luxurious cities in the world, is perfect. Those who like to combine beach holidays with exciting excursions it is better to choose Dubai, known for its distinctive architecture. Quiet and cozy Fujairah will appeal to those who want to take a break from the hustle and bustle of big cities.

IN last years More and more tourists prefer to rest in Qatar. natural conditions, the entertainment offered and the level of service at the resorts of this country practically do not differ from those in the UAE, but the prices are significantly lower.

Significant prospects for the development of tourism are also opening up for Oman, which surprises guests with a unique combination of exotic, ancient history and ultramodern. The country is replete with entertainment for every taste: exotic shopping, during which you can profitably purchase jewelry and carvings; magnificent ancient mosques, castles and fortresses - excellent examples of traditional Arab architecture; amazing natural attractions (for example, stalactite cave El-Khuta with a unique underground ecosystem); wonderful beaches, luxury hotels and affordable campsites and much more.

Arabian Peninsula on the map

Saudi Arabia attracts the attention of tourists, first of all, as a unique treasure trove of historical and cultural property. In the western part of the country, also known as Hijaz, one of the main shrines of the Muslim world is located - the ancient cities of Mecca and Medina, visited annually by thousands of pilgrims.

Adherents active rest also will not be disappointed with a trip to Saudi Arabia. Horse and camel tours, diving and deep sea hunting, yachting and boat trips on traditional Arab ships "Khuri" and "Sambuk" - all these types of entertainment will offer the attention of tourists best resorts countries.

A visit to any of the countries of the Arabian Peninsula will give a lot of vivid impressions and allow you to at least get a little closer to unraveling the mysteries of the mysterious exotic East.

The Arabian Peninsula in outline is not quite the right trapezoid, the long side of which extends from the northwest to the southeast. In the northeast, the peninsula is washed by the Gulf of Oman and the Persian Gulf, in the north it borders the Syrian Desert, in the southwest it is washed by the Red Sea, and in the south by the Gulf of Aden and the Arabian Sea. The total area of the peninsula is about 2.6 million square meters. km.

Geological structure and relief

In the geomorphology of the Arabian Peninsula, two characteristic features are noted: firstly, all mountain ranges are located on the outskirts of the peninsula and, secondly, more than 90% of the flow is directed towards the Persian Gulf or the Rub al-Khali depression.

The western part of the peninsula is composed mainly of outcropping igneous and metamorphic rocks, while in the east these rocks are covered with very thick strata of sedimentary deposits ranging in age from Early Paleozoic to modern. Therefore, in western regions such minerals can be found, the origin of which is associated with magmatic processes, and the presence of oil-bearing or coal-bearing areas is unlikely. Nevertheless, certain oil-bearing horizons can be found in the section of the Red Sea coast.

The lowland bordering the Red Sea is called Tihama; sometimes distinguish between Hijaz, Asir and Yemeni Tihama. From the rear side of Tihama, at various distances from the coast, from north to south, bare blocky mountains stretch in an almost continuous chain. In the range of Jabal al-Shafa, in the northern Hijaz, the high peak is Jebel el-Loz, reaching 2536 m, and the peaks surrounding it have heights from 1800 to 2100 m. The peak of Jebel Dhaka, lying to the east of the city of Mecca, has a height of 2504 m, and towards the south the heights are increasing. The maximum height is reached by Mount Jebel Maet (3,701 m), located to the west of Sana'a, the capital of Yemen. Thanks to high mountains, and also due to the fact that these mountains lie in the path of the monsoons blowing from the Indian Ocean, Yemen receives more precipitation than any other part of the Arabian Peninsula, which is why it is the most densely populated.

The watershed formed by the mountains of Hijaz, Asir and Yemen is 80-120 km from the coast; steep streams cut through the western slopes of the mountains deep gorges, and on the gentler eastern slopes, the consequent rivers 2 formed much more extensive system runoff. The core of the western ranges is composed of granites and metamorphic rocks, and most of these mountains, continuing into southern Yemen, are covered with volcanic rocks.

The mountains that border the southeastern tip of the Arabian Peninsula stretch from Aden to eastern Dhofar. In the western Hadhramaut, adjacent to the Gulf of Aden, their average height ranges from 1800 to 2400 m. One peak north of the city of Mukalla reaches a height of 3337 m. Towards the east, the heights decrease, and in Dhofar the mountains do not exceed 900 m. The exception is the peak north of Murbat, whose height is 2652 meters.

The mountains of Hadhramaut and Dhofar are composed mainly of sedimentary deposits, gently sloping northward towards the Rub al-Khali depression, but the southern slopes of the mountains are uneven and steep. Researchers believe that tectonically, these mountains are a large monoclinal block, slightly inclined to the north, towards the depression. Rub al-Khali, and abruptly ends in the south as a result of a fault, which is closely related to the graben that forms the depression of the Gulf of Aden.

Between the eastern extension of the Dhofar mountains and the southern spurs of the Oman ranges there is a low-lying plain about 240 km long, the average height of which is about 150 m above sea level.

The mountains of Oman are sharply dissected, their maximum height ranges from 2100 to 3000 m. The mountains have steep eastern and western slopes and are a ridge raised as a result of folding. In their morphology and geological structure, they are similar to the ranges of Iran, but have nothing in common with the mountains of the southwestern and southeastern parts Arabian Peninsula.

Description of the crossing through the Arabian Peninsula from the Red Sea to the Persian Gulf

Tihamah and Hijaz mountains. To the east of the narrow coastal lowlands of the Tihama, bordering the Red Sea, the heavily dissected and uneven mountains of the Hijaz rise sharply. The western ranges, composed mainly of igneous and metamorphic rocks, are very resistant to erosion, which explains their real height. Their initial uplift was due to movements that occurred intermittently over a long geological time along the western fault zone. The western slopes of the Hijaz mountains represent a giant fault wall, and the opposite slopes were formed as a result of a slight inclination of a block torn off by a rupture in eastbound. In the northeastern foothill belt, the Paleozoic sandstones, gently dipping to the east, lie on the Precambrian basement, and south of Tebuk, the early Paleozoic sandstones are covered by extensive basaltic lava flows, here called "harra". The eastern slopes of the Hijaz mountains gradually merge with the central plateau.

Central plateau of the Arabian Peninsula

To the east of the mountainous region described above, there is a vast desert central plateau, the width of which is approximately 500 km. Most of The plateau is composed of Precambrian igneous and metamorphic rocks. In its western part, there are several large lava covers of a relatively young age. Between Medina and the southwestern edge of the Great Nefud desert, the basement is underlain by almost undisturbed massive sandstones dating back to the Cambrian-Ordovician. The great explorer Douty gives a wonderful description of this and other parts of northern Najd.

The height of the Central Plateau ranges from 1050 to 1350 m above sea level, however, the height of individual depressions drops to 900 m, and individual ridges of elevations rise to 1800 m. time periodically drying up). These rivers formed strongly extensive network. A characteristic feature of the landscape are low, irregularly shaped hills separated by wide wadis (dry channels) filled with alluvial deposits. The area is desert-like, except for the rare thorny bushes and tough grasses that grow in isolated depressions.

Kuestovy district

Between the Central Plateau and Dakhna there is an area about 320 km wide, with a monoclinal slope to the east. A distinctive feature of the relief here is the presence of six to eight well-defined ridges stretching from north to south and representing typical cuestas with steep steep western and gentle eastern slopes. Particularly prominent are the Tuvaik Ridge, composed of Upper Jurassic limestones with a length of about 800 km, and the Aruma Cuesta Ridge, composed of Upper Cretaceous limestones and having the same extent. Both ridges clearly reflect the general nature of the relief and geological structure this area. The height of the Tuvaik range is approximately 840 m above sea level and 240 m above the level of the surrounding plains and lower ridges located to the west. The Arum Range, which rises 540 meters above sea level, stands out less, since it rises only 120 meters above the plain adjoining it from the west. The remaining cuesta, located almost parallel to the two main ones, are not so high and long. Nevertheless, some of them, against the background of the adjacent monotonous plains, seem very impressive. flat areas adjacent to western slopes many, though not all, cuestas are "nefuds" (nufuds, or nafuds), that is, vast expanses covered with dunes, sandy ridges, and sandy mounds.

The prevailing northwesterly winds in this area have a westerly component, as a result of which the Nefud sands slowly move to the east; but here the sands run up against a natural barrier formed by the above-described cuestas and individual table heights and remnants. Therefore, the sands slowly but continuously move southward parallel to the general strike of neighboring cuestas.

The cuesta ridges and flat spaces of the kuesta region were formed as a result of differential weathering of dense limestones, less dense sandstones and pliable clayey rocks, which are constituent parts sedimentary strata with a general slight slope. These rocks, listed in order of their predominance in the section, are well exposed here, but to the east, towards the Persian Gulf, they are covered by younger deposits, lithologically similar and also widely developed. Such sedimentary strata are favorable for the formation of oil and coal in them, but are not promising for metals.

Dahna (Little Nefud Desert), directly adjacent to the Arum and Tuvaik ridges, is one of the most distinctive regions of the eastern part of Saudi Arabia. It stretches from the desert of Great Nefud to the desert of Rub al-Khali for about 1300 km, its width varies from 25 to 80 km, and the average height is about 450 meters above sea level.

The Pedsh of the northern part of Dahna are mostly fixed. There is a vegetation cover consisting of small shrubs and grass. Dunes and sand mounds, which are usually characteristic of shifting sands, are rare here. Nevertheless, in the western part of Dahna, south of the Maakala-Riyadh road, there are dunes, and towards the south their number is increasing. According to available information, mobile dune sands are predominantly developed on the southern margin of Dakhna. The sands of Dahna are medium to fine grained, and their color, due to the presence of hematite, approaches orange-red, especially in the morning and at dusk.

in winter and in early spring Dahna is a good pasture for livestock. The Bedouins living here produce the name "Dahna" from the word "dihi", that is, "fat", apparently in connection with the excellent quality of the local pastures. True, most likely Dahna means "red" - a name that could come from the characteristic reddish color of the sands. Water is scarce in the Dahna region, and the Bedouins who herd their camels there have to make do with little water for weeks; They feed mainly on dates and camel milk.

Summan Plateau

The Summan Plateau, 80 to 240 km wide, is located east of Dakhna. From the surface, the plateau is composed of both pebble deposits and bedrock. Near Dakhna, it is mostly flat rocky terrain, but further to the east the plateau is indented by watercourses, which cause the relief to be dissected. The Kuesta ridge of Khufuf-Sarar, bordering the plateau from the east, forms a very uneven upland and consists of separate hills-outliers and extensive table heights, deeply protruding into the coastal lowlands. The height of the Summan Plateau near this ridge is approximately 240 m, and the height of its western margin, adjacent to Dakhna, is about 400 m, due to which a slope to the east is formed from 1/2 to 3/4 meters per 1 km. The surface of the plateau is generally monotonous and deserted. However, after rare but heavy rains, a rather dense grassy cover and flowers appear here.

From the northeast, the northern part of the Summan plateau is adjoined by "dibdiba" - pebble plains, stretching for 340 km from northwest to southeast and having a width of over 160 km. The word "dibdiba" is believed to come from an Arabic root and refers to the sound that occurs when the hooves of camels hit pebbles and stones. Dibdiba is a slightly undulating plain with fairly extensive flat areas. Vegetation here is sparse and occurs mainly only in depressions, where water accumulates during periods of rain. The surface of this plain is very suitable for fast driving, and medium-sized aircraft can land here almost everywhere.

coast of the persian gulf

This area includes the band west coast Persian Gulf, stretching from Kuwait in the north to the Qatar Peninsula in the south. The large oil fields discovered here in recent years make this area one of the most significant centers of oil production in the Middle East. In the coastal strip, located in the zone of gentle folding between the monocline of the Arabian block and the intensively dislocated structures of the mountains of Iran and Oman, seven oil fields have already been discovered by now, and other oil-promising uplifts are in line for detailed geological research and exploratory drilling. Other vast flat areas, completely covered with sands and pebbles, deserve the attention of researchers, where drilling work has so far been carried out on a limited scale.

Most of the coastal region is composed of modern sands and Miocene sediments. In Dahran and in the northern part of the Abqaik uplift from under the cover of Miocene rocks to the surface on large areas Eocene limestones come out. Outcrops of Eocene limestones, although not so significant, are also found in other places of the coastal region. Here, these rocks usually occur at a depth not exceeding 150 meters. With the exception of the Dammam dome, buried uplifts are very poorly recognized on the surface. However, geophysical surveys and structural drilling have shown that the entire coastal region is more or less folded and that the Cretaceous layers are much more strongly folded than the exposed or shallow Eocene layers. Nevertheless, the dip angles here, as a rule, do not exceed 7° even at depth. How far to the west this belt of folding development is unknown.

Although the eastern coastal zone of Saudi Arabia is generally a desolate and monotonous area, there are artesian wells that supply water to date palm oases, of which the most significant are Hofuf and El Qatif. The presence of artesian waters in coastal zone due mainly to the general gentle slope of the layers to the east between the east-central part of Saudi Arabia and the Persian Gulf. Rainwater, penetrating into the rocks in the higher regions of inner Arabia, gradually seeps into the depths and then flows through porous layers enclosed between impermeable layers to the east. If the aquifer is opened with a borehole or a well, the water will rise to the surface, forming an artesian well, a common occurrence in the Persian Gulf.

The area south of Kuwait and approximately as far as Jubail (27° N) is predominantly low, undulating sandy ridges, sometimes covered with rather dense vegetation, consisting of small groups of shrubs and stiff creeping grass. The Arabs call this area "dikaka". The sands, fixed by the root system of grasses and shrubs, are mostly immobile here. Sand hills and small sand ridges, formed by the wind and fixed by vegetation, are a significant obstacle to driving, but you can make a good road here by smoothing out bumps with a road roller or scraper.

The western part of the southern outskirts of the "dikaka" region abuts against the steep uplift of Kidam-Sarar facing the east. However, further to the north, this uplift breaks up into a series of isolated mesas and remnants. West of Kuwait and Neutral Zone coastal region passes into pebble plains (dibdiba).

At Jubail begin sand dunes, and towards the south, the dune belt widens, merging with the well-known dune terrain of Jafur, which passes into the desert of Rub al-Khali. The height of the dunes in this area ranges from 20 to 45 m, and the width exceeds 350 m.

On the coast of the Gulf of Salva, the steep uplift of Okair-Salva rises, facing east, but, turning at Okair to the west, it disappears under the sands of Jafur. The sands of Jafur now cover flat pebbly plains which reappear further west between these sands and another precipitous uplift, 370 km long and facing a steep slope to the east. This uplift runs in an almost straight line, starting about 50 km north of Khufuf and ending 65 km south of Jabrin.

The general direction of the coastline between the base of the Qatar Peninsula and Kuwait is quite straight, however, due to the lowlands covered with coastal salt marshes, sandbars and shallows coastline appears to be finely incised. From the coast inland, the height of the terrain increases with each kilometer by about one meter.

Lowlands covered with salt marshes, or "sebka", stretch almost along the entire Arabian coast Persian Gulf. They were formed as a result of the filling of small bays or other bodies of water with sand brought, apparently, from the desert, with the simultaneous evaporation of sea water. At relatively shallow depths, you can always find water in the sebks. As a result of evaporation, a certain amount of salt was deposited in them, and salt and sand form an inhomogeneous mixture, which dries up and gives a crust several centimeters thick. The surface of such solonchaks is usually located at a level to which moisture rises above the usual level of subsoil waters. Below this level, sand and dust remain damp and immobile, while above it they dry up and are blown away. The flat surface of such salt marshes is usually quite dense, and it is possible to lay good roads requiring little maintenance.

The Arabian Sea and numerous resorts located on its coast are especially popular with those who prefer first-class beaches, ancient sights and a wide range of modern entertainment. Due to the popularity of coastal areas, the Arabian Sea is easy to find on the map.

Arabian Sea on the world map

The Arabian Sea is one of the largest and deepest, and its temperature perfect for swimming at any time of the year.

Green, Persian, Eritrean - such names were given in ancient times to the Arabian Sea.

Where is it located and what ocean does it belong to?

The Arabian Sea is located in the northern hemisphere Asian parts of the world. In the east it is bounded by the Hindustan Peninsula, and in the west by the Arabian Peninsula. The water area includes several bays at once, the largest of which are:

Omani;
Cambay;
Kutch;
Aden gulf (connects to the Red Sea).

Read also about the delights of the Red Sea's underwater world.

Among the seas that make up the Indian Ocean, the Arabian and the seas are ahead of their neighbors, being the largest of them. They are connected by the Babel-Mandeb Strait, and what is especially remarkable, the Red Sea is located to the west.

Climatic features

Climate Arabian Sea – warm monsoon, and it is strongly influenced by weather peninsulas of Hindustan. average temperature sea water on the coast is from +22 to +28°C. Its performance does not fall below +20 degrees.

Such conditions are especially attractive for those who prefer the resorts of this water area - one of the most beloved by tourists.

Characteristics

It is not just that the Arabian Sea is considered one of the largest in the Indian Ocean, as well as occupying fifth place in size and depth in the world. Its area is 3.8 million square meters. km, and maximum width reaches 2400 km. The depth in some places is 5800 meters.

Relief of the Arabian Sea heterogeneous- according to the characteristics, it has a general slope from north to south. The shores are indented with bays and bays, some are high and rocky, while others are low-lying deltas. The Carlsberg Ridge divides the bottom into two large sections, forming two basins. The first of them is Arabian, the second is Somali.

To make the trip as comfortable as possible, choose the right suitcase. Read on for tips on selection.

Very rich and varied undersea world flora and fauna of the sea. Laminaria, brown and red algae live here. Among living organisms, about 100 commercial species of fish, shrimp, crabs and lobsters predominate. Also found in Arabian waters clownfish, angelfish, gobies, triggerfish, lionfish, sardinella.

In the Arabian Sea are found sharks- brindle, mako, reef, blackfin and blue. Off the coast of Hindustan, industrial fishing is especially developed. Tuna, marlin, mackerel and sardines are mined here.

coast map

Countries, islands and resorts washed by the Arabian Sea are one of the the most popular tourists from all over the world.

Resorts are in demand due to the warm climate and excellent conditions for recreation.

What continents and countries does it wash?

Since the Arabian Sea occupies the northwestern part of the Indian Ocean, its waters wash the coast of countries Asia and northeastern Africa. From the side of Hindustan, these include India (including Goa), Pakistan, Maldives and. The countries of the Omani Peninsula, washed by the sea, include Oman and Yemen, and on the African continent - the coast of Djibouti and Somalia.

Major resorts

Most Popular And major resorts Arabian Sea - India, its Goa, Maldives and Oman. All of them attract travelers with incredible exoticism, luxurious coast, developed infrastructure And great opportunities for a fabulous holiday.

One of the brightest places goa- a resort with everything necessary for tourists. Of all the Indian states, it is the most suitable for recreation, although it is only a narrow coastal strip. First of all, it attracts a variety of beaches and the opportunity to relax inexpensively.

It is customary to divide into Southern and Northern, and their main differences are in the level and quality of service. On north prefer to come those who like inexpensive, but rich vacation. There are a lot of budget places for overnight stays, affordable prices for services, but not always clean beaches. But it is never boring - noisy parties are constantly held on the coast of the Arabian Sea.

But even despite the noise and fun, vacationers have the opportunity to find a secluded beach and have a good time.