Africa is known for its deserts, among which the tropical deserts - the Sahara and the Namib - stand out.

The Namib is the oldest desert located in southwestern Africa and is the driest - only in some coastal cities there is life, the rest of the territory is practically uninhabited.

Namib, with an area of ​​100,000 sq. km, stretches for 1900 km along the Atlantic Ocean from the city of Namibe to the mouth of the Olifants River (Cape Province of South Africa); from the ocean, the desert goes into the interior of the continent, reaching the foot of the intracontinental plateau; it joins the Kalahari in the south.

Despite the harsh conditions, in the desert you can find plants that surprise and delight. Among these are velvichia (its life can last up to 1000 years, and during all this time it grows only two huge leaves, the roots of this plant are 3 meters), a quiver tree (up to 7 meters high with sharp ends of branches), nara (a source of moisture and necessary substances for all the inhabitants of the desert).

Animals usually live near water sources and in the hollows of the inner Namib - antelopes, rhinos, elephants, jackals, hyenas, zebras, but the dunes of the outer Namib are home to spiders, beetles, geckos and a large number of reptiles.

Both plants and animals in the process of evolution have developed special abilities that allow them to survive in extreme conditions, for example, the Nabian gecko can move on sand heated to a temperature of 60 degrees, and plants have adapted to collect the necessary moisture from morning fogs.

The Sahara is the largest desert, covering an area of ​​9,269,594 sq. km - from northern Sudan and Mali to the Mediterranean Sea, in the east it meets the Nile and the Red Sea, and in the west it reaches the Atlantic Ocean. Thus, the Sahara occupies the entire northern part of Africa.

The Sahara is an arid desert, in some places it does not rain for years, and in Kebili the highest temperature on the whole Earth was recorded - + 58 ° in the shade.

Semi-deserts are a transitional zone between shrouds and deserts, here the dry period lasts almost the entire year, and annual precipitation does not exceed 300 mm.

The vegetation cover of semi-deserts looks like a mosaic - dark areas of empty land alternate with thickets of shrubs, grasses, cereals and sagebrush.

Among the animals, most of all are hares, rodents and reptiles, there are also many birds. And from ungulates you can meet antelopes, mouflons, kulans. Among predators, jackals, hyenas and fennec foxes stand out.

And semi-deserts are specific natural zones, the main distinguishing feature of which is drought, as well as poor flora and fauna. Such a zone can form in all climatic zones - the main factor is the critically low amount of precipitation. Deserts and semi-deserts are characterized by a climate with a sharp daily temperature difference and a small amount of precipitation: no more than 150 mm per year (in spring). The climate is hot and dry, it evaporates without having time to soak into. Temperature fluctuations are characteristic not only for the change of day and night. The temperature difference between winter and summer is also very large. The general background of weather conditions can be defined as extremely severe.

Deserts and semi-deserts are waterless, dry regions of the planet, where no more than 15 cm of precipitation falls per year. The most important factor in their formation is the wind. However, not all deserts experience hot weather; on the contrary, some of them are considered the coldest regions of the Earth. Representatives of flora and fauna have adapted to the harsh conditions of these areas in different ways.

Sometimes the air in deserts in summer reaches 50 degrees in the shade, and in winter the thermometer drops to minus 30 degrees!

Such temperature fluctuations cannot but affect the formation of the flora and fauna of the semi-deserts of Russia.

Deserts and semi-deserts are found in:

• The tropical belt is a large part of such territories - Africa, South America, the Arabian Peninsula of Eurasia.
• Subtropical and temperate zones - in South and North America, Central Asia, where a low percentage of precipitation is complemented by topographical features.

There is also a special type of desert - the Arctic and Antarctic, the formation of which is associated with a very low temperature.

There are many reasons for the formation of deserts. For example, the Atacama Desert receives little rainfall because it is located at the foot of the mountains, which cover it from rain with their ridges.

Ice deserts formed for other reasons. In Antarctica and the Arctic, the main snow mass falls on the coast; snow practically does not reach the interior regions. Precipitation levels generally vary greatly, for one snowfall, for example, an annual norm can fall. Such snow drifts form over hundreds of years.

natural area desert

Climate features, desert classification

This natural zone occupies about 25% of the planet's land mass. In total there are 51 deserts, of which 2 are icy. Almost all deserts were formed on the most ancient geological platforms.

General signs

The natural zone called “desert” is characterized by:

• flat surface;
• critical volume of precipitation(annual rate - from 50 to 200 mm);
• rare and specific flora;
• peculiar fauna.

Deserts are often found in the temperate zone of the Northern Hemisphere of the Earth, as well as tropical and subtropical. The relief of such an area is very heterogeneous: it combines highlands, insular mountains, small hills and layered plains. Basically, these lands are drainless, but sometimes a river can flow through part of the territory (for example, the Nile, Syrdarya), and there are also drying lakes, the outlines of which are constantly changing.

Important! Almost all desert areas are surrounded by mountains or are located next to them.

Classification

Deserts are of different types:

• Sandy. Such deserts are characterized by dunes and sandstorms often occur. The largest, the Sahara, is characterized by loose, light soil, which is easily blown by winds.
• Clayey. They have a smooth clay surface. They are found in Kazakhstan, the western part of Betpak-Dala, on the Ustyurt plateau.
• rocky. The surface is represented by stones and rubble, which forms placers. For example, Sonora in North America.
• saline. The soil is dominated by salts, the surface often looks like a salt crust or a bog. Distributed on the coast of the Caspian Sea, in Central Asia.
• arctic- located in the Arctic and Antarctica. They are snowless or snowy.

Climatic conditions

The desert climate is warm and dry. The temperature depends on the geographical location: the maximum +58°C was recorded in the Sahara on September 13, 1922. A distinctive feature of the desert area is a sharp temperature drop of 30-40°C. During the day the average temperature is +45°C, at night - +2-5°C. In winter, in the deserts of Russia, it can be frosty with little snow.

In desert lands it is characterized by low humidity. Strong winds often occur here at a speed of 15-20 m/s or more.

Important! The driest desert is the Atacama. There has been no precipitation on its territory for more than 400 years.

Semi-desert in Patagonia. Argentina

Flora

The desert flora is very sparse, mostly sparse shrubs that can extract moisture deep in the soil. These plants are specially adapted to live in hot and dry habitats. For example, a cactus has a thick, waxy outer layer to keep water from evaporating. Sagebrush and desert grasses need very little water to survive. Plants of deserts and semi-deserts have adapted to protect themselves from animals by growing sharp needles and thorns. Their leaves are replaced by scales and spines or covered with hairs that protect the plants from excessive evaporation. Almost all sand plants have long roots. In sandy deserts, in addition to grassy vegetation, there is also shrubby vegetation: zhuzgun, sand acacia, teresken. Shrub plants are low and slightly leafy. Saxaul also grows in deserts: white - on sandy, and black - on alkaline soils.

Desert and semi-desert flora

Most desert and semi-desert plants bloom in spring, reproducing flowers until the onset of hot summer. During wet winter and spring years, semi-desert and desert plants can produce surprisingly many spring flowers. In the desert canyons, on the rocky mountains, pine trees coexist, junipers and sage grow. They provide shelter from the scorching sun for many small animals.

The least known and underestimated species of desert and semi-desert plants are lichens and cryptogamous plants. Cryptogamous or mystogamous plants - spore fungi, algae, ferns, bryophytes. Cryptogamous plants and lichens need very little water to survive and live in dry, hot climates. These plants are important because they help stop erosion, which is very important for all other plants and animals because it helps keep the soil fertile during high winds and hurricanes. They also add nitrogen to the soil. Nitrogen is an important nutrient for plants. Cryptogamous plants and lichens grow very slowly.

In clay deserts, annual ephemera and perennial ephemeroids grow. In solonchaks - halophytes or saltworts.

One of the most unusual plants that grow in such an area is saxaul. It often moves from place to place under the influence of the wind.

Fauna

The animal world is also not numerous - reptiles, spiders, reptiles or small steppe animals (hare, gerbil) can live here. Of the representatives of the order of mammals, a camel, an antelope, a kulan, a steppe ram, a desert lynx live here.

In order to survive in the desert, animals have a specific sandy coloration, they can run fast, dig holes and live without water for a long time, they are preferably nocturnal.

Of the birds, you can meet a crow, a saxaul jay, a desert chicken.

Important! In sandy deserts, there are sometimes oases - this is a place that is located above the accumulation of groundwater. There is always dense and abundant vegetation, ponds.

Leopard in the Sahara Desert

Characteristics of the climate, flora and fauna of the semi-desert

Semi-desert is a type of landscape that is an intermediate option between desert and steppe. Most of them are located in the temperate and tropical zones.

General signs

This zone is distinguished by the fact that there is absolutely no forest on it, the flora is rather peculiar, as is the composition of the soil (very mineralized).

Important! There are semi-deserts on all continents except Antarctica.

Climatic conditions

They are characterized by a hot and long summer period with a temperature of about 25°C. Evaporation here is five times higher than the level of precipitation. There are few rivers and they often dry up.

In the temperate zone, they run in an unbroken line across Eurasia in an east-west direction. In the subtropical zone, they are often found on the slopes of plateaus, highlands and plateaus (Armenian Highlands, Karru). In the tropics, these are very large areas (Sahel zone).

Fennec foxes in the desert of Arabia and North Africa

Flora

The flora of this natural zone is uneven and sparse. It is represented by xerophytic grasses, sunflowers and wormwood, ephemerals grow. On the American continent, cacti and other succulents are most common, in Australia and Africa - xerophytic shrubs and stunted trees (baobab, acacia). Here vegetation is often used to feed livestock.

In the desert-steppe zone, both steppe and desert plants are common. The vegetation cover is mainly made up of fescue, wormwood, chamomile, and hairy feather grass. Often wormwood occupies large areas, creating a dull monotonous picture. In some places, kokhiya, ebelek, teresken, and quinoa grow among the wormwood. Where groundwater comes close to the surface, thickets of brilliant chia come across on saline soils.

The soil, as a rule, is poorly developed, and water-soluble salts predominate in its composition. Among the soil-forming rocks, ancient alluvial and loess-like deposits predominate, which are processed by winds. Gray-brown soil is inherent in elevated flat areas. Deserts are also characterized by solonchaks, that is, soils that contain about 1% of easily soluble salts. In addition to semi-deserts, salt marshes are also found in steppes and deserts. Groundwater, which contains salts, when it reaches the soil surface, is deposited in its upper layer, resulting in soil salinization.

Fauna

The animal world is quite diverse. It is mostly represented by reptiles and rodents. The mouflon, antelope, caracal, jackal, fox and other predators and ungulates also live here. The semi-deserts are home to many birds, spiders, fish and insects.

Protection of natural areas

Part of the desert areas are protected by law and are recognized as nature reserves and national parks. Their list is quite large. From the deserts man guards:

• Etosha;
• Joshua Tree (in Death Valley).

From the semi-deserts are subject to protection:

• Ustyurt Reserve;
• Tiger beam.

Important! The Red Book includes such desert inhabitants as serval, mole rat, caracal, saiga.

Char desert. Zabaykalsky Krai

Economic activity

The climatic features of these zones are unfavorable for economic life, but throughout history, entire civilizations have developed in the desert zone, for example, Egypt.

Special conditions made it necessary to look for a way to graze livestock, grow crops and develop industry. Taking advantage of the available vegetation, sheep are usually grazed in such areas. Bactrian camels are also bred in Russia. Farming here is possible only with additional irrigation.

The development of technological progress and the limited reserves of natural resources have led to the fact that man has reached the deserts. Scientific research has shown that in many semi-deserts and deserts there are considerable reserves of natural resources, such as gas, precious. The need for them is constantly increasing. Therefore, being equipped with heavy equipment, industrial tools, we are going to destroy previously miraculously untouched territories.

1. The two largest deserts on planet Earth are Antarctica and the Sahara.
2. The height of the highest dunes reaches 180 meters.
3. The driest and hottest area in the world is Death Valley. But, nevertheless, more than 40 species of reptiles, animals and plants live in it.
4. Approximately 46,000 square miles of arable land turns into desert every year. This process is called desertification. According to the UN, the problem threatens the lives of more than 1 billion people.
5. Passing through the Sahara, people often see mirages. To protect travelers, a map of mirages was drawn up for caravaners.

The natural zones of deserts and semi-deserts are a huge variety of landscapes, climatic conditions, flora and fauna. Despite the harsh and cruel nature of the deserts, these regions have become home to many species of plants and animals.

Deserts and semi-deserts are a natural zone, which is characterized by an almost complete absence of growth and a poor stomach. the world. this is due to the extremely harsh climatic conditions of the planet where they are located. Deserts can form in almost any climate zone. Their image is associated with low rainfall. That is why deserts are primarily common in the tropics. tropical deserts occupy the territory of most of the tropics. Africa and Australia, west. tropical coasts. belts South. America, as well as the territory of the Arabian Peninsula in Eurasia. their formation is associated with the year-round dominance of the tropical air mass, the influence of which is enhanced by the terrain and cold currents off the coast. a large number of deserts are located in the subtropical and temperate zones of the Earth. This is the territory of Patagonia in South. America, where their formation is due to the isolation of the south. the tip of the mainland from the penetration of moist air by cold currents, as well as in the interior of the North. America and Center. Asia. Here, the image of deserts is associated with a strong continental climate due to the great distance from the coast and mountain systems that prevent the penetration of moisture from the ocean. The image of deserts can be associated with extremely low temperatures on the planet, this type of deserts are called arctic and antarctic deserts.

Nature. Desert conditions are extremely harsh. The amount of precipitation does not exceed 250 mm per year, and on large areas - less than 100 mm. The driest desert in the world is the Atacama Desert, where precipitation has not been recorded for 400 years. The largest desert in the world is the Sahara, located in the North. Africa. Her name transl. from Arabic. like "desert". The highest was recorded here. air temperature on the planet + 58 ° C. with the sunset, the temperature in the desert drops sharply, the drops reach tens of degrees during the day, and frosts even occur here on a winter night. Everything is to blame for the constantly clear sky due to the downdrafts of the dry. air from the equator, because of this, clouds are almost not formed here. The vast open spaces of deserts do not at all prevent the movement of air along the surface of the earth, which leads to the emergence of strong winds. Dust storms come unexpectedly, bringing clouds of sand and streams of hot air. In spring and summer, a strong wind rises in the Sahara - samum ("poisonous wind"). It can last only 10-15 minutes, but the hot dusty air is very dangerous for a person, it burns the skin, the sand does not allow you to breathe freely. Also in con. winter-beginning spring in Sev. Africa from the desert almost every year begins to blow a seasonal wind-khamsin ("fifty"), since on average it blows for 50 days. Deserts of temperate latitudes are also characterized by strong temperature fluctuations throughout the year. Hot summers give way to cold, harsh winters. Fluctuations in air temperature during the year can be about 100°C. Winter frosts in the deserts of the temperate zone of Eurasia drop to -50 ° C, the climate is sharply continental. The flora of deserts in particularly difficult climatic conditions may be completely absent, where moisture remains sufficient, some plants grow, but the flora is not diverse. Desert plants usually have very long roots - more than 10 meters - in order to extract moisture from groundwater. In the deserts Asia grows a small shrub-saxaul. In America, a significant part of the flora is cacti, in Africa, spurges. Stomach. the desert world is poor. Reptiles-snakes, monitor lizards predominate here, scorpions live, there are few mammals. One of the few who was able to adapt to these difficult conditions was a camel, which was not accidentally called the "ship of the desert." By storing water in the form of fat in their humps, camels are able to travel long distances. For the indigenous nomadic peoples of the deserts, camels are the basis of their economy. Desert soils are not rich in humus, however, they often contain a lot of minerals and are suitable for agriculture. The main problem for plants is the lack of water.

Issues to consider:

1. Desert characteristic

2. desert vegetation

3. Animal world of deserts

4. Desertification

5. Semi-desert

6. Protection of deserts and semi-deserts

7. Occupations of the population of deserts and semi-deserts

1. Characteristics of the desert.

Desert - a geographical zone with a hot, arid climate and sparse sparse vegetation in the temperate subtropical and tropical zones of the Earth.

Desert area is estimated at 31.4 million km 2 (about 22% of land).

Deserts are found on all continents except Europe, and are located within the borders of about 60 countries. In the mountains, the desert forms a high-altitude belt (alpine desert), on the plains - a natural zone.Distributed in the temperate zone of the Northern Hemisphere, subtropical and tropical zones of the Northern and Southern Hemispheres.

Large deserts of the world:

Gobi - Central Asia, Mongolia and northern China

Takla-Makan borders the Pamirs and Tibet from the north. Central Asia

Sahara - North Africa

Libyan desert - north of the Sahara

Namib - Southwest coast of Africa

Kyzylkum - between the Syrdarya and Amudarya rivers, Uzbekistan, Kazakhstan

Karakum - Turkmenistan

Atacama - Northern Chile, South America

Northern Mexico

Great Victoria Desert

Great sandy desert

Climatic conditions:

One of the main features of the desert is the lack of moisture, which is explained by the negligible (50- 200 mm per year) the amount of precipitation that evaporates faster than seeps into the soil. Sometimes there is no rain for several years. Most of the territory is drainless, and only in some places there are transit rivers or lakes that periodically dry up and change their shape (Lob Nor, Chad, Air). Some deserts formed within the ancient river, delta and lake plains, others on platform land areas. Often deserts are surrounded by mountains or border on them.

Over the course of a long geological history, deserts have changed their boundaries. For example, the Sahara - the greatest desert in the world - stretched for 400- 500 km south of the present position.

Precipitation 50-200 mm per year

Clear days 200-300 per year

Air temperature +45° in the shade. Surface temperature during the day + 50-60 ° (up to 80 ° and even 94 ° - Death Valley), at night + 2-5 ° (sudden changes)

Dry winds, storms. Winter in Russia frost with thin snow cover.

Contrary to the prevailing opinion that the desert is an endless monotonous sea of ​​sand, the most common are rocky deserts, or hamads, often located on plateaus or mountain ranges with remnants of bizarre shapes. Pebble and gravelly deserts stand out among them, impressive with almost complete lifelessness. Parts of such deserts can be seen in the Sahara, the Kyzyl Kum, and on the Arabian Peninsula. Under conditions of a huge daily temperature range, with periodic wetting and drying of rocks, a characteristic shiny dark crust forms on their surface, the so-called desert tan, which protects the rock from rapid weathering and destruction. Often, rocky deserts turn into sandy ones. In Central Asia they are called kums, in Africa - ergs, in Arabia - nefuds. Sands are easily carried by the wind, forming eolian landforms: dunes, dunes, safes, etc. Single dunes and dunes not fixed by vegetation can move tens of meters per year. Sometimes sand blown by the wind makes a special sound. In such cases, they speak of singing dunes or dunes (in Dagestan, the singing dune is declared a natural monument). But the bulk of the sands are immobile, as they are held by the long roots of shrubs and grasses, which have adapted to the conditions of constant moisture deficiency. The largest sandy deserts of the world include: the Libyan Desert, Rub al-Khali, Nefud, the Great Sandy Desert, the Great Victoria Desert, the Karakum, the Kyzylkum.

Clay deserts develop on clay deposits of various origins. The largest clay deserts: Ustyurt, Deshte-Lut , Deshte-Kevir Betpak-Dala and others. Their relief is characterized by takyrs and sors.

Saline deserts form on saline (saline) soils and are scattered in separate spots among other types of deserts.

TAKYR - flat clay surfaces, almost devoid of vegetation, in the deserts of the subtropical zone, an area of ​​several m2 up to tens of kilometers 2 . In the spring they are usually flooded with water.

SOLONCHAS - soil types of steppe, semi-desert and desert zones. They contain water-soluble salts, 0.5-10% humus. In the Russian Federation - in the Caspian region.

SORs (blinders), closed depressions in deserts Cf. Asia, covered with a crust of salts or a plump layer of salt dust. They are formed in sands due to evaporation and salinization of near-surface groundwater or on strata of salt-bearing bedrock under conditions of an effusion water regime with the formation of solonchaks.

SAHEL (Arabic - coast, outskirts) - the name of the transitional strip (width up to 400 km ) from the deserts of the Sahara to the savannas of West Africa. Semi-deserts and deserted savannas predominate. Precipitation 200- 600 mm in year; frequent droughts.

Desert types

According to their position, they distinguish between continental deserts (Gobi, Takla-Makan), located inside the continent, and coastal deserts (Atakama, Namib), stretching along the western coasts of the continents.

Deserts are sandy (Sahara, Karakum, Kyzylkum, Great Victoria Desert), clayey (South Kazakhstan, south of Central Asia), rocky (Egtpet, Israel) and saline (Caspian lowland).

2. Desert vegetation.

Desert vegetation does not form a dense cover and usually occupies less than 50% of the surface, being distinguished by a great originality of life forms and great sparseness.

Plant types:

1. Succulents - agave, aloe, cacti

2. The root system reaches groundwater

(roots 20-30 m ) - camelthorn plant

3. Heat-resistant, able to tolerate dehydration - wormwood

4. Ephemeroids - develop over a short period, then rhizomes or bulbs remain in the soil. - tulip, sedge, bluegrass

Xerophytes (from the Greek xeros - dry and phyton - plant), plants adapted to life in arid habitats. Several types: succulents - heat-resistant, but do not tolerate dehydration (agave, aloe, cacti); hemixerophytes - do not tolerate prolonged dehydration, the root system reaches groundwater (sage, camel thorn); euxerophytes - heat-resistant, able to tolerate dehydration (wormwood, gray veronica, some mulleins); poikiloxerophytes - when dehydrated, they fall into suspended animation (some mosses).

Ephemera, annual herbaceous plants, the entire development of which usually occurs in a very short time (several weeks), more often in early spring. Characteristic for steppes, semi-deserts and deserts (for example, dimorphic quinoa).

EPHEMEROIDS, perennial herbaceous plants, the above-ground organs of which develop from autumn to spring and die off in summer, while the underground ones (bulbs, tubers) persist for several years. Characteristic for steppes, semi-deserts and deserts (species of tulip, sedge, bluegrass)

Plant adaptations:

root system deep into the soil;

modified leaves or spines, scales;

pubescence of leaves - contributes to less evaporation;

dropping leaves with the onset of heat;

flowering only in spring.

Sandy deserts of Asia (Karakum, Kyzylkum, mouth of the Volga river)

Herbs, trees, leafless shrubs and semi-shrubs:

white saxaul (5 m),

sand acacia,

silver chingil - shrub,

juzgun,

ephedra,

camel thorn (a genus of shrubs and perennial herbs of the legume family, eaten by camels, root length 20- 30 m.),

grate - cereal,

swollen sedge,

celine (aristida) - cereal

Clay deserts of Asia (Southern Kazakhstan, lower reaches of the Ural River, south of Central Asia)

wormwood,

saltwort,

black saxaul ( 12 m ), wood goes to fuel; green twigs are food for camels and sheep. Good sand binder

bulbous bluegrass,

desert beetroot,

spurges.

Asia. Saline deserts (Caspian lowland)

soleros

Sarsazan gnarled

Africa

Celine (Aristide)

Date palm trees in oases

America

Succulents (agave, aloe, cacti - cereus, prickly pear), yucca

3. Animal world of deserts

Attachments:

protective coloring of sand color,

fast run,

go long without water

fall into hibernation

nightlife,

holes in the sand

bird nests on the ground (on bushes and trees).

Insects and arachnids: scarab, lingering, scorpion, desert locust

Reptiles:foot-and-mouth disease, steppe agama, monitor lizard, roundhead, frilled lizard, land iguana, sand boa, arrow-snake, gyurza, efa, steppe viper, Central Asian tortoise, panther tortoise (Africa).

Birds:Sadzha (grouse), saxaul jay, desert warbler, field pipit, desert coinage, avdotka.

Rodents:jerboas, thin-toed ground squirrel, gerbils, giant mole rat.

Eared hedgehog.

Ungulates:goitered gazelle, antelopes, including gazelles, saiga, wild ass.

Carnivores:wolf, fennec fox, striped hyena, house (jungle cat), dune cat, jackal, coyote, manul, caracal, South Russian dressing, honey badger, Cape South African fox.

4. Desertification

The encroachment of the desert on other parts of the earth is called desertification.

Causes:

Overgrazing.

Intensive perennial tillage.

Drought.

The Sahara, moving south, annually takes away 100 thousand hectares of arable land and pastures.

Atacama moving at speed 2.5 km per year.

Thar - 1 km per year.

5. Semi-deserts

semi-deserts - areas combining the nature of steppes and deserts, found in the temperate, subtropical and tropical zones of the Earth (except Antarctica) and forming a natural zone located between the steppe zone in the north and the desert zone in the south.

In the temperate zone of Asia:

from the Caspian lowland to the eastern border of China.

In the subtropics:

Anatolian plateau, Armenian Highlands, Iranian highlands, Karoo , Flinders, foothills of the Andes, valleys of the Rocky Mountains, etc.

In the tropics of Africa:

south of the Sahara, in the Sahel zone (desert savannah)

Plants:

Russia:tulips, sedge, bluegrass, wormwood, mullein, saltwort.

America: cacti.

Africa and Australia: bushesand rare low-growing trees (acacia, doum palm, baobab)

Animals:

hares

rodents (gophers, jerboas, gerbils, voles, hamsters), meerkats,

reptiles;

antelope,

bezoar goat,

mouflon,

kulan, Przewalski's horse

predators: jackal, striped hyena, caracal, serval, steppe cat, fennec fox, house

birds,

many insects and arachnids (karakurt, scorpions).

6. Protection of deserts and semi-deserts

Reserves and national parks

Desert:

Semi-desert:

Ustyurt Reserve,

tiger beam,

Aral-Paygambar.

Listed in the Red Book: Bandaging, mole rat, goitered gazelle, saiga, saja, caracal, serval

7. Occupations of the population of the desert and semi-desert

Desert:breeding of sheep, goats and camels, irrigated agriculture and gardening only in oases (cotton, wheat, barley, sugar cane, olive tree, date palm).

Semi-desert:pasture animal husbandry, oasis agriculture is developed on irrigated lands.

Camels live in deserts (one-humped dromedary in Africa, two-humped Bactrian in Asia).

The desert was and remains an extreme natural environment for people's lives, although it was in the desert that ancient civilizations originated and existed: Egypt, Mesopotamia, Khorezm, Assyria, etc. Life usually arose near a well, river or other water source. This is how oases appeared, the first "islands" of life created by human labor. Life in the oases and occupations of the population differed significantly from the conditions of the desert itself, where people are doomed to eternal wandering under the scorching sun and dust storms in search of water. Breeding sheep and camels has become a traditional occupation of nomads. Irrigated agriculture and horticulture developed only in oases, where such plants as cotton, wheat, barley, sugar cane, olive tree, date palm, etc. have long been cultivated. The rapid influx of population into large oases led to the formation of the first cities.

FAMOUS DESERT IN THE WORLD

GOBI (from Mong. beef - a waterless place), a strip of deserts and semi-deserts in Central Asia, in the south and southeast of Mongolia and in adjacent regions of China. Bounded in the north by mountainsMongolian Altai and Khangai, in the south - Nanshan and Altyntag. Subdivided intoTransaltai Gobi , Mongolian Gobi , Alashan Gobi , Gashunskaya Gobiand the Dzungarian Gobi. Area over 1000 thousand km2 .

Plains prevail at an altitude of 900- 1200 m , composed mainly of rockschalk, Paleogene and Neogene. They alternate with more ancient hillocks, ridges and island ranges (up to 1800 m ). The sloping piedmont plains are dissected by numerous dry channels flowing into closed depressions, which are occupied by drying lakes, solonchaks or hard clay surfaces; there are also small massifs of shifting sands.

The climate is sharply continental in the temperate zone (temperature fluctuations from -40 ° C in January to + 45°C in July). Precipitation per year falls from 68 mm in the northwest of the Alashan Gobi to 200 mm in the northeast of Mongolia; there is a summer maximum. There are almost no rivers with a constant flow, most of the channels are flooded only in summer. The soils are gray-brown and brown, often in combination with sandy desert soils, solonchaks and takyrs. Characteristic are carbonate, gypsum-bearing, and coarse gravelly soil varieties.

Desert vegetation is sparse and sparse. On the plateau and piedmont plains there is small-shrub gypsophilous vegetation (blackberry, double-leaved, teresken, reaumuria, several types of nitrate and saltwort). On the salt marshes, in addition to nitrates and saltworts, there are tamarisks, potash. On the sands - sandy wormwood, zaisan saxaul, kopek, perennial and annual grasses. In the northeast and east of Mongolia, semi-deserts are common, where, along with wormwood and saltwort, cereal groups are developed, and rare clumps of shrub caragana are found. A wild camel, a donkey-kulan, a Przewalski's horse, several species of antelope, many rodents and reptiles have been preserved. Many endemic species of flora and fauna. Big Gobi Nature Reserve (within Mongolia).

Animal husbandry (small cattle, camels, horses, to a lesser extent - cattle). Quite plentiful groundwater is of great importance for water supply. Agriculture is developed only along the river valleys.

KYZILKUM, desert in Wed. Asia, in the interfluve of the Amu Darya and Syr Darya, in Uzbekistan, Kazakhstan and partly in Turkmenistan. OK. 300 thousand km2 . Plain (height up to 300 m ) with a number of closed depressions and isolated mountain ranges (Sultanuizdag, Bukantau, etc.). Most of it is occupied by ridge sands; there are many takyrs in the northwest; there are oases. Used as pasture.

SAHARA, the desert in Africa, the largest in the world. St. 7 million km2 . On the territory of the Sahara are completely or partially the states of Morocco, Tunisia, Algeria, Libya, Egypt, Mauritania, Mali, Niger, Chad, Sudan. OK. 80% of the Sahara are plains 200- 500 m . In the north-east there are drainless depressions: Qattara (133 m), El-Fayoum, etc. In the central part - mountain ranges: Ahaggar, Tibesti (Mount Emi-Kusi, 3415 m , the highest point of the Sahara). Rocky and gravelly (hamady), pebble (reg) and sandy (including ergi) deserts predominate. The climate is tropical desert: rainfall in most parts of the territory is less 50 mm per year (on the outskirts of 100 - 200 mm ). Average January temperatures are not lower than 10 °С; absolute maximum 57.8 °С, absolute minimum -18 °С (Tibesti). Daily amplitudes of air temperature are more than 30 °C, soil - up to 70 °C. In addition to the transit river. Nile and parts of Niger, no permanent streams. Dry channels of ancient and modern watercourses (wadis or uedas) predominate. Groundwater feeds numerous oases. Vegetation cover is extremely sparse, sometimes absent. Agriculture (date palm, cereals, vegetables) in oases. Nomadic and semi-nomadic animal husbandry.

TAKLA-MAKAN, a desert in western China, one of the largest sandy deserts in the world. Length from west to east over 1000 km, width up to 400 km , the area of ​​sands is over 300 thousand km2 .

It was formed under conditions of long-term accumulation of sediments within the Tarim Basin, which is composed mainly of alluvial deposits (of the Tarim River and its tributaries), partially blown over. The surface is flat, gradually decreasing to the north and east of 1200- 1300 m to 800- 900 m . In the west, single ridges rise above Takla Makan (the highest point is Mount Chongtag, 1664 m ) composed of sandstones.

Most of the territory is covered with sands up to 300 m . Dunes predominate in the southwest, and sandy ridges of complex configuration (including large ones, sometimes stretching for 10- 13 km , - the so-called whale backs), sand pyramids (height 150- 300 m ), etc. On the outskirts of Takla-Makan, large areas are occupied by solonchaks.

The climate is moderately warm, sharply continental, with negligible (less 50 mm per year) the amount of precipitation. The atmosphere is highly dusty. The rivers flowing from the Kunlun penetrate into the depths of the Takla-Makan for 100 200 km , gradually drying up in the sands. Only the Hotan River crosses the desert and in summer brings its waters to the Tarim River, which flows along the western and northern outskirts of the Taklamakan.

Depth of groundwater in relief depressions (within ancient deltas and old rivers) 3- 5 m , they are usually difficult to access for plants, so most of the territory is devoid of vegetation and only in places with a close occurrence of groundwater there are rare thickets of tamarisk, saltpeter, and reed. Along the outskirts of Takla-Makan and river valleys, poplar turanga, sucker, camel thorn, annual saltwort, saxaul are found. The animal world is poor (rare herds of antelopes, hares, gerbils, jerboas, voles); in the river valleys - wild boars.

Separate oases (mainly in the valleys of the Tarim and Yarkand rivers). There is no permanent population. Near the southern outskirts of Takla Makan, among the sands, are the ruins of ancient settlements confined to dry valleys.

ATACAMA (Atacama), a desert in northern Chile, in the South. America, along the coast of the Pacific Ocean, between 22-27 ° S. sh.; rainfall less 50 mm in year. River crosses. Loa. Large deposits of copper ores (Chukikamata, El Salvador), saltpeter (Taltal), table salt, borax.

ADDITIONAL MATERIAL

Przewalski's Horse (Equus caballus), an equine mammal of the equine genus. body length 2.3 m , height at withers about 1.3 m . This is quite a typical horse, densely built, with a heavy head, thick neck, strong legs and small ears. Its tail is shorter than that of a domestic horse, its mane is erect and short. The color is sandy-red or red-yellow. The mane and tail are black-brown, a black-brown belt runs in the middle of the back, the end of the muzzle is white. In summer the hair is short and tight, in winter it is longer and thicker.

This wild horse was discovered and described in Central Asia by N. M. Przhevalsky in 1878. Once it was widespread, but by the end of the 19th century it was preserved only in the south-west of Mongolia (in Dzungaria), where in 1967-1969 it was seen (in natural conditions) for the last time. Przewalski's horse herds consisted of 5-11 mares and foals led by a stallion. They were very mobile and constantly moved, which was determined both by poor winter pastures and uneven rainfall in their habitats. Constant migrations have led to the fact that these horses have become very hardy and strong. From fights with domestic stallions, they always came out victorious.

The main reason for the destruction of the population in natural conditions is fishing (hunting, poaching) and competition for watering places with livestock. Almost immediately after the discovery of the animals, the owner of the Askania-Nova park F. Falz-Fein and later the animal dealer K. Hagenbeck began to look for ways to get these rare animals. Various means were used in this struggle. Hagenbeck, having learned about Falz-Fein's suppliers in Biysk, bought 28 foals with the help of his agents. Despite the fact that by the beginning of the 20th century 52 thoroughbred Przewalski's horses were brought to Europe, only three pairs served as a source for breeding. The Przewalski's horse is kept in many zoos around the world; several dozen individuals live in semi-free keeping in the Askania-Nova reserve. An international plan has been developed for the reintroduction of the Przewalski's horse to its original habitats - to the mountain-steppe zone of Mongolia.

Jerboas (Jerboa, Dipodidae) - a family of mammals of the order of rodents; includes 11 genera and about 30 species, including three-toed pygmy jerboas, large jerboa, long-eared jerboa, and upland jerboa. jerboas are characterized by a large head with a blunt muzzle, long rounded ears, large round eyes and long vibrissae, a short, curvy body (body length 4- 26 cm ), small front legs, powerful jumping hind limbs. Large ears, eyes and long whiskers testify to the high development of hearing, twilight vision and touch, which are necessary for jerboas when searching for food and protecting themselves from enemies at night. Small front legs serve to grasp and hold food, as well as to dig holes, in which jerboas achieve great skill. The hind limbs are jumping, and in connection with this function they are greatly modified: the foot is elongated and the three middle metatarsal bones grow together into one common bone, called the tarsus. The tail plays an important role in movement: it serves to maintain the balance of the body when jumping, especially when turning sharply at a fast gallop. A black and white tassel at the end of the tail in many species is called a banner and serves as a signaling tool for intraspecific communication. The incisors, in addition to gnawing food, serve to loosen the soil when digging holes, while the limbs are used mainly for raking loosened soil.

Jerboas are distributed from North and Northeast Africa, Southeast Europe, Asia Minor and Western Asia through the Caucasus, Central Asia, Kazakhstan, the extreme south of Siberia (Altai, Tuva, Transbaikalia) to Northeast China and Mongolia. They are mainly found in semi-desert and desert landscapes, only a few species inhabit the steppe zone, and some penetrate mountains to a height higher than 2 km above sea level. Different species have developed adaptations for living on loose or dense soils, and therefore jerboas can be found in sandy, clayey, and rubble semi-deserts and deserts.

Jerboas are typically nocturnal animals. Before dawn, they hide in burrows that they build themselves. The main burrow of the jerboa runs obliquely below the surface with one or more blind escape burrows coming close to the surface. The main passage for the day is clogged with an earthen plug, which is called a penny. On this penny, which has not yet dried out in the early morning, you can find a jerboa hole. If you start digging a habitable hole, then the animal knocks out the ceiling of one of the emergency passages and jumps out through it. In the far part of the main passage, the jerboa digs a hole with a rounded living chamber, which is lined with finely gnawed blades of grass. Jerboas spend the winter period in deep hibernation in their burrows.

Jerboas feed on the seeds of various plants, lily bulbs, which they dig out of the ground. The diet also includes green parts and plant roots, and in some species a significant proportion of the diet is animal feed (small insects and their larvae). In spring and summer, the reproduction of animals occurs, the female gives birth to 1-8 cubs (usually 2-5).

Jerboas play an important role in desert biocenoses. They have a significant impact on the soil and vegetation cover, serve as food for desert predators. In many areas, jerboas are background animals. Some species damage plants that strengthen the sands; they can be carriers of pathogens of a number of infectious diseases of animals and humans.

GINGERS (Gerbillinae), a subfamily of mammals of the order of rodents; includes about 100 species, united in 13 genera, including dwarf, small, large, short-eared, fat-tailed gerbils, taters (barefoot gerbils). Outwardly, gerbils resemble rats or mice. Their body length is up to 19 cm , reddish-yellow long tail with a tassel. The back is sandy yellow, the belly is white.

Gerbils are common in the desert steppes and deserts of Africa, Asia and Southeast Europe. They feed mainly on plant foods, but can also eat small invertebrates. They do not hibernate for the winter, but in cold weather they do not leave their holes for a long time, eating prepared supplies. Many breed all year round, with females bringing multiple litters of 2 to 12 cubs. Gerbils are carriers of plague pathogens, tick-borne typhus, they harm agricultural land. These animals are often kept at home.

Gazelle (Gazella subgutturosa), artiodactyl mammal of the genus of true gazelles (Gazella) of the subfamily of gazelles (Antilopinae); forms 2-4 weakly expressed subspecies. Body length 95- 125 cm , height at the withers 60- 75 cm, weight 18-33 kg . Males have black and lyre-shaped horns up to 40 cm . Females are usually hornless. The coloration of the upper body and sides is sandy. The underside of the body, the neck and the inside of the legs are white. The tail is two-colored: the main part is sandy, the end is black. When a frightened gazelle runs, it raises it to the top, and the tail stands out sharply against the background of a white mirror. For this feature, among the Kazakhs and Mongols, the gazelle was called the black tail (kara-kuiruk, hara-sulte). Young goitered gazelles have a pronounced facial pattern in the form of a dark brown spot on the bridge of the nose and two dark stripes stretching forward from the eyes.

Goitered gazelle is distributed in Western, Central and Central Asia, South Kazakhstan, and also in Eastern Transcaucasia. It lives on flat, hilly deserts and cereal-salt semi-deserts. As good runners, goitered gazelles prefer areas with dense soil, avoiding free-flowing sands. In summer, they graze in the morning and in the evening, and spend the hottest time on the hay, saving moisture. Beds are located on level ground near trees, often favorites, and bushes. The goitered gazelle moves after the shadow of the tree, hiding from the sun, first of all, its head. Raised from the prone, the goitered gazelle quickly jumps up and rushes at a speed of 55- 60 km/h about 200- 300 m , then inspected. In winter, it grazes almost all day.

Goitered gazelles feed on herbaceous or shrubby plants, choosing the most moisture-saturated grasses in summer: barnyard grass, onions, ferulas. Goitered gazelles usually go to watering places with open and flat banks without dense coastal thickets for 10- 15 km once every 3-7 days. They are able to quench their thirst not only with fresh, but also with brackish water (including from the Caspian Sea). The grass that goitered gazelles eat can also contain a significant amount of salt.

In spring and summer, animals are kept singly or in small groups of 2-5 heads. In autumn and winter, they gather in herds from several tens to hundreds of heads. Then the race happens. The beginning of the rut is preceded by the arrangement of rutting latrines by the males. In September, males dig small holes with the hooves of their front legs and leave their excrement there. Other males, finding such holes, may throw away old excrement and leave their own there. Obviously, such pits serve as marks of the occupied territory. Pregnancy of females lasts 5.5 months. In May, the female brings one, rarely two cubs. Newborns for the first days only lie on a bare piece of land. The sandy-brown coloring of the goitered gazelle so merges with the soil that you can easily step on the baby without noticing it. The cub begins to follow its mother and feed on its own in two weeks. The main natural enemy of the gazelle is the wolf.

In captivity, the gazelle is well tamed and breeds, but does not live long. The goitered gazelle population is declining, although work is underway to restore the number of animals. A subspecies from the Arabian Peninsula (Gazella subgutturosa marica) is listed in the International Red Book.

Fenech (Fennecus zerda) is a species of predatory animal of the wolf family. It looks like a miniature fox. body length approx. 40 cm , tail to 30 cm ; weight 1.5 kg ; ears are large (up to 15 cm ) and wide. The coat is long, reddish-cream above, fawn or almost white; the tip of the fluffy tail is black. Fenech lives in the deserts of North Africa and Southwest Asia. It is active at night and spends the day in a deep burrow. Huge ears allow Fenech to catch the slightest rustle. In case of danger, he burrows into the sand. When hunting, the fennec fox can jump high and far. It feeds on small rodents, birds and their eggs, lizards, insects, carrion, and plants. Pregnancy in a female lasts 51 days. Cubs (2-5) will be born in March-April in a burrow with a nesting chamber lined with grass, feathers and wool.

JACKALS, a group of species of carnivorous mammals of the wolf family. The most common is the Asian jackal (Canis aureus), which is similar in appearance to a small wolf. His body length is 85 cm , tail about 20 cm ; weight 7–13 kg. The color of the coat in winter is fawn, dirty yellow, with a noticeable red and black tint, the tail is reddish-brown with a black end. It is found in the south of Eurasia, in North Africa; in Russia, mainly in the North Caucasus. The Asian jackal prefers to settle in thickets of bushes and reeds, on plains, near rivers, lakes and seas. It is less common in the foothills. As shelters, the jackal uses natural niches and depressions, crevices among stones, and sometimes abandoned burrows. The animal is active mainly in the dark, but often during the day. It migrates only in search of food.

The jackal is omnivorous, but feeds mainly on small animals: rodents, birds, fish, as well as insects, carrion and the remains of the prey of large predators. Also eats fruits and berries, including grapes, watermelons, melons, plant bulbs. Living near the villages, he also hunts poultry. When going hunting, the jackal emits a loud howl, which is picked up by all its relatives located nearby. They often hunt alone or in pairs. The jackal forms pairs for life, the male takes an active part in creating a hole and raising offspring. The rut takes place from January to February. Pregnancy lasts about 2 months. Usually 4-6, less often 8 puppies are born. The Asian jackal is a carrier of dangerous diseases (rabies and plague). It has no commercial value.

The jackal (Canis mesomelas) and the striped jackal (Canis adustus) live in East and South Africa. In their lifestyle and habits, they are similar to the Asian jackal. The Ethiopian jackal (Canis simensis) is found in Ethiopia. Outwardly, he looks like a dog with a fox head. A wide black stripe stretches along the middle of the back, sharply delimited from the red sides and limbs. The belly is white, the tail is long red, with a black end. Ethiopian jackal lives in the mountains at a height 3000 m , it feeds on rodents and hares. Its population is small and this animal is protected.

COYOT (meadow wolf, Canis latrans), a predatory mammal of the wolf family. body length approx. 90 cm , tail - 30 cm . Erect ears, a long fluffy tail, which, unlike a wolf on the run, keeps lowered down. The coat is thick, long, grayish or reddish-brown in color on the back and sides, very light on the belly. The end of the tail is black. The coyote is distinguished by a developed higher nervous activity, it is able to adapt to a changing environment.

Coyote lives in the prairies and steppes of North and Central America. Runs into the woods by accident. His lifestyle has a lot in common with the jackal. The lair suits in caves, hollows of fallen trees, deep holes. The loud howl of the coyote is an integral part of the color of the prairies. It feeds on rodents, hares, rabbits, birds and lizards, sometimes fish and fruits, and does not disdain carrion. Rarely attacks domestic animals (goats, sheep). Hunts alone or in packs. destroys a lot of harmful rodents. It is completely safe for humans. Pairs are formed for life, the rut takes place in January-February. Pregnancy lasts 60-65 days. In a brood 5-10, sometimes up to 20 cubs.

CARACAL (Felis caracal), a predatory mammal of the cat family, genus of cats. Body length 65- 82 cm , tail 20- 31 cm ; weight 11- 13 kg . In appearance and tassels on the ears, it resembles a lynx. But it has a thinner, slender body, on high thin legs; also has a uniform light red color. There are small black markings on the muzzle and ears, the ends of the ears are decorated with tassels.

It lives in the deserts of Africa and Asia, including in the south of Turkmenistan. It hunts mainly at night, and during the day it takes refuge in abandoned burrows. Caracal hides prey and overtakes it with large (up to 4.5 m ) jumps. It mainly feeds on rodents: gerbils, jerboas, ground squirrels, as well as tolai hares; less often birds, small antelopes, hedgehogs, porcupines. Can hunt livestock and poultry.

Cubs (from 1 to 4) are born in early April. In ancient times, caracals were trained to hunt antelopes, hares and birds. It has no commercial value. Few. Caracal is listed in the International Red Book. Protected in the Repetek Reserve.

Kulan (onager, Equus hemionus), equine mammal of the horse genus. Body length 2.0- 2.4 m , height at the withers 110- 137 cm , weight 120- 127 kg . In appearance, the kulan is slender and light. The head is relatively heavy, the ears are longer than those of a horse. The tail is short, with a black-brown brush at the end, like donkeys and zebras. Coloring sandy-yellow color of various shades. The belly and inner parts of the legs are white. From the withers to the croup and along the tail there is a narrow black-brown stripe. The mane is low.

The kulan is distributed in Western, Middle and Central Asia. However, the once large range has shrunk significantly. The number is restored only in reserves, including in the south of Turkmenistan (Badkhyz Reserve). The kulan was brought to the island of Barsakelmes and to the foothills of the Kopetdag. Habitats depend on territorial features. The animal can inhabit hilly plains or foothills, deserts and semi-deserts. With the exception of spring, when pastures are covered with young lush grass, kulans need a daily watering place and do not move further from water bodies than 10 15 km . When threatened, they can reach speeds of 60- 70 km/h without slowing down for several kilometers. There are no strictly defined periods of grazing and rest.

To most animals, except for sheep, the kulan is peaceful, often grazing with goitered gazelle and herds of horses. Mutual communication is developed among these animals, it is worth alerting goitered gazelles, or alarmingly shouting to birds, as a kulan takes off. An angry kulan is very ferocious.

Kulans have well-developed eyesight, hearing and smell. Approach the kulan unnoticed at a distance of 1- 1.5 km impossible. However, he can pass by a motionless person at a distance 1.5 m , and this is due to the peculiarities of his visual apparatus. The click of a camera can be heard from a distance. 60 m . They are silent animals. With a call, reminiscent of a donkey, but more deaf and hoarse, the male calls the herd.

The rut takes place from May to August. During the rut, the male begins to prance in front of the females, raising his head high. Often runs around the herd, jumps, screams, rides on his back, tears with his teeth and throws up tufts of grass.

Even before the start of the rut, adult males drive young kulans out of the herds. During this period, there are serious fights between males. Baring their mouths and flattening their ears, they rush at each other with bloodshot eyes, trying to grab the hock joint. If one succeeds, then he begins to twist the opponent around the axis and gnaw at his neck.

Pregnancy of females lasts 331-374 days, on average 345. Kulanyat will be born from April to August. The first hours they lie motionless, but already on the first day they begin to graze with their mother. The grown up kulanenok becomes very active. When he wants to eat, he walks around his mother, digs the ground near her belly with his foot, throws his legs around her neck. The male protects the cubs from possible attacks by young kulans. Animals breed in captivity. Kulans are protected everywhere, two subspecies - Syrian (Equus hemionus hemippus) and Indian kulan (Equus hemionus khur) are listed in the International Red Book.

CAMELS (Camelus), a genus of mammals of the camelid family of the corn-foot order; includes two species: dromedary (one-humped) and Bactrian (two-humped). Length up to 3.6 m . Camels are characterized by signs: they do not have hooves - their legs end in two fingers with blunt claws, and the lower surface of the foot is protected by an elastic callus cushion. They are common in the deserts of Central Asia (Bactrians), as well as in Africa, Arabia, Asia Minor, India (dromedary).

Camels feed on shrub and semi-shrub hodgepodges, tree leaves, and bulbs. The well-known ability of camels to go without water for a long time is due to the fact that they can tolerate a slight increase in body temperature without increased moisture loss. This feature allows you to spend less moisture on cooling. In addition, moderate dehydration in a camel is not accompanied by thickening of the blood and disruption of its circulation, as in mammals not adapted to desert conditions. Camels are able to drink quickly and a lot (in 10 minutes they drink about 130-135 liters of water).

The rut takes place in winter. Usually one, rarely two cubs are born. Only the Bactrian has survived in the wild. The dromedary is domesticated and used as pack and draft animals, as well as for milk, meat and wool.

Bactrian - domesticated Bactrian camel, differs little from the wild Bactrian camel. Many zoologists do not make a difference between the concepts of a Bactrian camel and a Bactrian. Domestic camels have larger humps, wider feet and well-developed calluses on the knees of their front legs. The proportions of the skull of domestic and wild have small but stable differences. The coat color of domestic camels is variable - from light, sandy-yellow to dark brown, while wild ones have a constant reddish-brown-sandy color. The Bactrian camel was domesticated more than a thousand years before our era. As an animal resistant to low temperatures and waterless conditions, it has become widespread in Mongolia, Northern China and Kazakhstan. There are several breeds of domestic Bactrian camels - Kalmyk, Kazakh, Mongolian.

DROMEDAR (dromedary, one-humped camel; Camelus dromedarius), a mammal of the camel genus of the callus-footed order. Length approx. 2.1 m , height at the withers 1.8- 2.1 m . Unlike the Bactrian, it has one hump, as well as a shorter and lighter coat. The one-humped camel was domesticated in ancient times, probably in Arabia or North Africa. Not found in the wild. It is widely distributed in Africa, Arabia, Asia Minor and Central Asia, India, introduced to Mexico and Australia. Several breeds are known: high-speed riding mahars (North Africa), riding Indian Rajputans, pack Turkmen dromedaries.

The way of life is similar to the Bactrian. It tolerates heat better, but worse - frost. Up to 10 days can do without water. Passes under the saddle in a day 80 km at speeds up to 23 km/h . However, in a caravan, a dromedary travels no more than 30 km , because he must graze for a long time. Herbivorous. The rut takes place in winter. When crossed with a Bactrian, it gives fertile offspring (the so-called bunks), which surpass their parents in endurance. But the offspring when crossing hybrids is weak.

Deserts and semi-deserts are a natural zone characterized by an almost complete absence of vegetation and a very poor fauna. All this is due to the extremely harsh climatic conditions of the planet where they are located. Deserts, in principle, can form in almost any climate zone. Their formation is primarily associated with low rainfall. That is why deserts are primarily common in the tropics. Tropical deserts occupy the territory of most of tropical Africa and Australia, the western coast of the tropical belt of South America, as well as the territory of the Arabian Peninsula in Eurasia. Here, their formation is associated with the year-round dominance of the tropical air mass, the influence of which is enhanced by the terrain and cold currents off the coast. Also, a large number of deserts are located in the subtropical and temperate zones of the Earth. This is the territory of Patagonia in South America, where their formation is due to the isolation of the southern tip of the mainland from the penetration of moist air by cold currents, as well as in the interior of North America and Central Asia. Here, the formation of deserts is already associated with a strong continental climate due to the great distance from the coast, as well as mountain systems that prevent the penetration of moisture from the ocean. The formation of deserts can also be associated with extremely low temperatures on the planet, this type of desert, called the Arctic and Antarctic deserts, is considered separately by us.
The natural conditions of the deserts are extremely harsh. The amount of precipitation here does not exceed 250 mm per year, and in large areas - less than 100 mm. The driest desert in the world is the Atacama Desert in South America, where no rain has fallen for 400 years. The largest desert in the world is the Sahara, located in North Africa (pictured). Its name is translated from Arabic as "desert". Here was recorded the highest air temperature on the planet + 58 ° C. Under the scorching rays of the sun in the summer months, when it reaches its zenith at noon, the sand underfoot heats up to enormous temperatures, and sometimes you can even fry eggs on the stones. However, with the sunset, the temperature in the desert drops sharply, the drops reach tens of degrees during the day, and frosts even occur here on a winter night. The constantly clear sky is to blame for everything due to the descending flows of dry air from the equator, because of this, clouds are almost not formed here. The vast open spaces of deserts do not at all prevent the movement of air along the surface of the Earth, which leads to the emergence of strong winds. Dust storms come unexpectedly, bringing clouds of sand and streams of hot air. In spring and summer, a strong wind rises in the Sahara - simum, which can literally be translated as "poisonous wind". It can last only 10-15 minutes, but the hot dusty air is very dangerous for a person, it burns the skin, the sand does not allow you to breathe freely, many travelers and caravans died in the deserts under this deadly wind. Also, at the end of winter - the beginning of spring in North Africa, a seasonal wind begins to blow from the desert almost every year - khamsin, which means "fifty" in Arabic, since on average it blows for fifty days.
Deserts of temperate latitudes, unlike tropical deserts, are also characterized by strong temperature fluctuations throughout the year. Hot summers give way to cold, harsh winters. Fluctuations in air temperature during the year can be about 100°C. Winter frosts in the deserts of the temperate zone of Eurasia drop to -50 ° C, the climate is sharply continental.
The flora of deserts in especially difficult climatic conditions may be completely absent, where moisture remains sufficient, some plants grow, but the flora is still not very diverse. Desert plants usually have very long roots - more than 10 meters in order to extract moisture from groundwater. In the deserts of Central Asia, a small shrub grows - saxaul. In America, a significant part of the flora is cacti, in Africa - spurges. The fauna of the deserts is also not rich. Reptiles predominate here - snakes, monitor lizards, scorpions also live here, there are few mammals. One of the few who was able to adapt to these difficult conditions was a camel, which was not accidentally called the "ship of the desert." By storing water in the form of fat in their humps, camels are able to travel long distances. For the indigenous nomadic peoples of the deserts, camels are the basis of their economy. Desert soils are not rich in humus, however, they often contain a lot of minerals and are suitable for agriculture. The main problem for plants is the lack of water.

Sandstorm in Australia