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بحث , تقرير إنجليزي جاهز / DESERTS للصف العاشر

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هذا تقرير الأنجليزي
DESERTS


Deserts are mainly found around the tropic of Cancer and tropic of Capricorn in Northern and Southern Hemispheres respectively. The common definition of desert is a region that receives less than 25cm of rain a year on average.

When people think of deserts, the following image comes to their minds : hot and arid land, vast expanses of sand, soil of reddish brown color, a sky of brilliant blue, no or very few plants, cacti, spiny leaves and camel is the only animal that they can think of.

The truth is not like that. It is not very common to find sand in a desert, but small rocks, pebbles and loose gravel on the surface layer instead. Only 15% of the world’ s desert surface is pure sand. (Parts of the Sahara and Arabia desert)

Desert occupies about one fifth to one third of the earth’ s surface. The rainfall pattern is not a seasonal one. Instead, rain usually falls in the form of sudden, violent thunderstorms. There may be several storms in a year or none for several years. The " average rainfall each year" is not calculated based on one year’ s rainfall, but on the total rainfall in a long period of time.

" How about the polar regions with sheets of floating ice?" You may ask. Large amount of water is locked up in the icecap. The average rainfall in the cold deserts located in polar regions is within 25cm.

The rate of evaporation ( known as " Moisture Index" ) can be used to classify deserts as there are extremely high temperatures, low humidities and very little cloud cover.

How extreme are the temperatures ? The daytime air temperature can reach 58oC (136oF) in the Sahara. Soil temperature may reach 80oC (176oF). For half a year, the average temperature of the Mongolian desert is below the freezing point. In Antarctica, the winter mean temperature is -30oC (41oF).

First of all lets talk about the weather in deserts .We all know that rain rarely falls in desert and when it comes, it comes in the form of thunderstorm.

In sandy desert, the rain usually drains away promptly and only change the landscapecomparatively slightly. In contrast, the torrential downpour in rocky deserts drains into wadis (rocky watercourses that is dry except after heavy rain). This deepen the dry valleys. Heavy downpour can build up into flash flood, carrying sand, gravel and then large rocks and boulders. Thus, at the end of most wadis, there is an enormous bank of sand and stone( known as "alluvial fan" ). The surplus sediment from the flash flood forms muddy lakes of different size and duration
Between wadis, there are flat plateaux in different extent called mesas. The mesas are isolated by the continuously widened wadi. The isolated mesas then become flat-topped, step-sided island in the desert, know as a buttle.

These lakes are particular seen in Australian desert. They lasts long enough to breed creatures like shrimps, frogs and wildfowl. Some of the lakes formed have high salt ************************************************** *************, which is thought to be derived from salt in the atmosphere, brought from oceanic spray.

Shallow, low-bottom-gradient lakes can be moved by wind stress over many square kilometers. When they dry up, an area of clay, silt, or sand encrusted with salt is found, known as playa.

Action of wind
Wind dehydrates soils and living things. Sand and dust particles are moved by desert winds. Desert winds also remove organic debris that makes the soil fertile. Since plants are scarce in deserts, wind erosion occurs more easily. Take Prairie States of North America as an example, a productive area was reduced in the 1930s to desert by desert wind (devastating tornado winds from desert), over-cropping and over-cultivating. The fine dust can be carried to kilometers away and thousands of meters up. Large amount of the fine duct rest in more temperate or moister regions and from the basis of loess (a fertile soil).

Impact of changes in temperature
Heat and cold produces the least observable effect in sandy desert. In contrast, their impact is much greater in rocky deserts.

In cold desert, rainfall is frozen at night in winter. When water goes into the tiny cervices and expands, the rocks are forced to split up.

In hot deserts, the fragmenting force of temperature is slower. Rock surfaces reach 70oC or 80oC at midday and cool down to freezing point at midnight. Expansion under the sun and contraction at night weaken the surface layers and cause flaking.

Secondly , lets talk about the different inhabitats that live in such places and how they adapt themselves in order to survive in such harsh weathers .

Desert plants have developed various ways to get as much water as possible and to reduce water loss.

Some plants have long roots to get water deep in the soil, or branched roots to get water over a wide area. With thick waxy layer on the stems and leaves, water can be retained and the tissues are protected from strong sunshine. Some plants have pin-like leaves to reduce water loss. Barrel Cactus

Many desert plants are succulents and they store water in their swollen stems or leaves.

Some desert plants are the " drought evaders" . They exist as seeds before the rain comes, and grow when it rains. They flower quickly to produce seeds and then die. There are " drought resisters" — perennial plants that possess the abilities of storing water, locating underground water or minimizing the use of water by various measures.

Very often, when people think of mammals in desert, they usually think of camels only. In fact, almost all of the mammalian orders have their representatives in the deserts.

To avoid the heat, some small mammals live in shelters underground, where the temperature fluctuations are not as much as those on the surface. Most important of all, the maximum temperature in burrows is much lower than that on the surface. They usually come out at night to search for food and store the food in burrows.
The Kangaroo Rat

Large mammals, like gazelles, onyx, asses and camels, find their shelters in the shade of a rock or tree. As the excessive heat may kill them, some of them lose heat by evaporation, which can only increase the staying power by 2-3oC. Of course, water must be available for sweating. They get water from waterholes and by eating plants and preys. The Mountain Lion

The small mammals have greater surface area to weight ratio. They gain and lose heat quickly and thus face greater problems in maintaining an acceptable body temperature range. Any animal living in desert has to have a gut that is able to excrete almost dry faecal material and a kidney that draws minimum water from blood. There are "summer hibernates" that minimize their ****bolic rates in summer to avoid water lost through respiration.

Some mammals, like hares, have large ears densely populated with blood vessels to remove heat.
Desert Carnivores obtain water from their preys. The dog and cat families lack sweat glands. They remove heat by panting which in turn lose much water so they are found mostly at the desert margins near a permanent water source.

With feathers, birds can keep out of external cold, heat loss and as well as external heat gained, for feathers can trap a layer of insulating air. The feathers are under muscular control and can be held erect. When there is a breeze, the upright feathers direct the air movement down to cool the skin.

Birds cannot sweat. They pant or flutter to remove heat.

Some flesh-eating birds don’ t need to drink as they can get enough moisture from their preys. The seed-eating birds need to drink daily and thus they are restricted in a number of places
where they can nest. Roadrunner
Birds find shelters underground, in the shade of rocks or bushes. Flying at high attitudes enables them to avoid heat. Birds can tolerate 3oC body temperature rise above normal level. No birds can survive at above 45oC.
Reptiles possess scaly skin to conserve moisture. They can control their body temperature by gaining or losing heat from surroundings. By using external heat, they do not need as much energy as the birds and mammals. Hence they need less food and breathe at a lower rate, which help them to conserve moisture.

Black-collared Lizard
The skins of the amphibians are soft and moist. This property allows the skin to respire and absorb oxygen from air and water. It seems unlikely that they can be found in deserts. Though, some frogs and toads manage to survive in the arid area. They must complete their life cycles before the wetlands evaporate after the rain, for their eggs have to develop in lakes or pools.

Most of the small animals like insects and arachnids (eg. Spiders, scorpions) have waterproof cuticles or shell mainly composed of a substance called chitin, which is hard, strong and impervious to many gases and liquids. It prevents them from drying up by the heat. The different stages of the invertebrates have various ways to prevent drying up. The egg is surrounded by a tough shell that is impervious to drought. It can last for months or even years, waiting for the rain to come. The larval stage often develops underground to avoid the heat. In the pupal stage, the cocoon or chrysalis protect the moth. The adult invertebrates, as protected by the chitinous exoskeleton, may live a long and productive life. It may lead a short life in the extreme, depending on the fat stored in its body. The short life is long enough for it to mate and lay eggs.
Tarantulas

Have you ever thought of the problems that face people who live in deserts ??Well there are quite a few .

If on the morning of a hot summer day, a healthy adult is placed in the middle of a desert without water for an hour, he will lose 0.9l of water by perspiring and he will be very thirsty. At the mid afternoon, he will lose about 5 to 8 kg of his weight. At night, if the daytime temperature is higher than 48.9oC, he may be dead. 3.8l of water a day is still not enough to save a man’s life from the heat for a week.

Loss of salt and clothing are also major problems .Through continuous sweating and intake of fresh water, the salt concentration in the body falls and causes severe cramping of muscles and headaches. Thus not only water , a source of salt is also essential.To avoid the heat, people in deserts have to dress up carefully :The long, flowing robes shield the skin from the sun and allow air to reach the body. The clothes are loose-fitting to prevent immediate sweat evaporation so that the body does not dehydrate so quickly in the very dry air. Headgear shields the head from the sun. Veils protect the face and keep the sand out of the mouth. The clothes also keep the people warm at night and in winter.

As for the homes ,some people live in permanent homes such as the mud houses of some Native Americans. The nomads carry with them portable homes as they move their livestock from place to place. All desert homes need to be well insulated from extreme heat and cold. Tents made of densely woven goat’s hair or thick-walled homes are suitable. Since rain is torrential, they need to be water proof.

Peolpe living in the deserts are called nomads who can be classified into three main groups : hunter-gatherers, pastoralists and traders.

Hunter gatherers move as small, independent bands within the area in which they know where are the waterholes, important trees, patches of smaller food plants and potential food animals. They move daily, monthly or semi-annually.

Postoralists move from place to place depending on the needs of their domesticated stock like sheep, goats or camels. Their targets are places with prolonged and predictable grass supply. Some of them may also hunt while others may cultivate an area near where they settle and grow cereal crops. They may also trade when they get a chance.

Traders are mobile merchants with trains of pack animals like camels, asses, mules or yaks with them. They supply goods produced on one side of the desert to the town people.

To conclude , you can see that there are lots of information that most people don’t know about deserts . Most of us think there is only one type of deserts , hot deserts , and even a bigger number of people don’t know the variuos plants and animals that live in deserts and how they cope themselves to the weather conditions . This report is just a summary of the great wonders of deserts as there is lots more that scientists are trying to discover nowadays .

Resources:
Eyewitness Guides — Desert by Miranda Macquitty (A Dorling Kindersley Book)
Deserts, A Miracle of Life by Jim Flegg (Blandford Press)
Life Nature Library — The Desert (Time-Life Books Inc.)

مسروق خخ , أن شاء الله يعجبكم مشكورين على المرور مقدما

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التصنيفات
الصف الثاني عشر

English report about deserts of the world الصف الثاني عشر

بليييييييييييييييييييز اي حـــــــــــــــــد مسوي تقرير انجليزي ينزله حقي بليييييييييييييييييييييييز
يوم الاحد اخر يوم ولازم اسلم التقرير

بليييييييييييييييييييييييييييييييييز

اختكم
عازفة الصمت

لقراءة ردود و اجابات الأعضاء على هذا الموضوع اضغط هناسبحان الله و بحمده

التصنيفات
الصف الثاني عشر

تقرير عن Deserts -تعليم اماراتي

أبي تقرير عن Deserts

لقراءة ردود و اجابات الأعضاء على هذا الموضوع اضغط هناسبحان الله و بحمده

التصنيفات
الصف الثاني عشر

ابي تقرير عن … Deserts of the world … للصف الثاني عشر

السلام عليكم …
أخبـــاركم عساكم بخير …
فديتكم يالغاليين لا تردوني ..
يوم الخميس اخر يوم في تسليم التقرير ..
وبصرااحه تعبت وانا ادور ..
ف يااااليت لو تساعدوني …

ابي تقرير عن … Deserts of the world

يتظمن التقرير ..
مقدمه / Introduction
معنى الصحراء / Meaning of Desert
أنواع اصحـراء / Kinds of deserts
المواقع /
الطقس والمناخ / Weather & Climate
حيوانات / Animals
خــاتمه / Conclusion
مصادر ومراجع / source & References

وسلامتكم … بليز ساعدوني لو بكلمه

لقراءة ردود و اجابات الأعضاء على هذا الموضوع اضغط هناسبحان الله و بحمده

التصنيفات
الصف الثاني عشر

تقرير Deserts of the world للصف الثاني عشر


Deserts of the world

The Desert Biome
Deserts are places on earth that are characterized by little vegetation and rain. They are made up of sand or rocks and gravel. Deserts cover about one-fifth of all the land in the world. Most deserts lie along the Tropic of Cancer and Tropic of Capricorn, imaginary lines that lie north and south of the equator.

Deserts
The Middle East and North Africa make up the driest region of the earth. Nearly two thirds of the region is desert. A desert is land that receives an average of less than ten inches of rain per year. The Sahara of northern Africa is the largest desert in the world.

World’s Largest Deserts

Factmonster: Principal Deserts of the World

North American Deserts
North American Deserts

Sonora Desert

Sonoran Desert
The Sonoran Desert of Southern Arizona and Northwestern Mexico is well known for its beauty and many spectacular and grand cacti. The abundant cacti and other succulents simply defy the harsh climate with exuberant biodiversity.

Southwest Deserts
A traveler crossing overland from Los Angeles to Big Bend National Park in West Texas encounters three of North America’s four great deserts, each ecologically distinct and strikingly beautiful.

Great Basin Desert
The Great Basin Desert, the largest U. S. desert, covers an arid expanse of about 190,000 square miles and is bordered by the Sierra Nevada Range on the west and the Rocky Mountains on the east, the Columbia Plateau to the north and the Mojave and Sonoran deserts to the south.

Mojave Desert
The transition from the hot Sonoran Desert to the cooler and higher Great Basin is called the Mojave Desert. This arid region of southeastern California and portions of Nevada, Arizona and Utah, occupies more than 25,000 square miles.

The Chihuahuan Desert
Most of the Chihuahuan Desert — the largest desert in North America covering more than 200,000 square miles — lies south of the international border. In the U.S. it extends into parts of New Mexico, Texas and sections of southeastern Arizona. Its minimum elevation is above 1,000 feet, but the vast majority of this desert lies at elevations between 3,500 and 5,000 feet.

The Chihuahuan Desert Region
A desert region can be defined many ways. To a physical scientist such as a meteorologist, a desert can be defined as an area receiving an average annual rainfall of 10" or less.

Welcome to the Chihuahuan Desert
The Chihuahuan Desert is the easternmost and southernmost of the four North American deserts: the Great Basin Desert, the Sonoran Desert, the Mojave Desert, and the Chihuahuan Desert.

The Chihuahuan Desert
The Chihuahuan Desert is the easternmost, southernmost, and largest North American desert. Most of it is located in the states of Chihuahua and Coahuila in Mexico, but fingers of the Chihuahuan reach up into eastern Arizona, southern New Mexico, and Texas, and down to the states of Zacatecas, and San Luis Potosi in Mexico. This desert is quite large – about 175,000 square miles – making it bigger than the entire state of California.

White Sands Desert of New mexico
At the northern end of the Chihuahuan Desert lies a mountain ringed valley called the Tularosa Basin. Rising from the heart of this basin is one of the world’s great natural wonders – the glistening white sands of New Mexico.

Deathe Valley
Although Death Valley is in California, it’s right on the California-Nevada border, closer to Las Vegas than to Los Angeles. Apart from the unexpected snowcapped mountains of winter, it’s a lonely and arid place pockmarked with suspicious looking mounds and crackling salt flats, crisscrossed by crevassed earth and powdered with relentless sand dunes.

Death Valley National Park
Many first time visitors to Death Valley are surprised it is not covered with an endless sea of sand. Less than one percent of the desert is covered with dunes, yet the shadowed ripples and stark, graceful curves define "desert" in our imaginations.

OneWorld Magazine: Deserts of Our World
OneWorld Magazine would like you to experience the diversity and cultural richness of the world’s deserts, if only virtually. Over the next 4 weeks we will bring you a selection of articles, paintings, sculptures, poems and photographs of men and women who have been challenged by the uniqueness of a desert, defeated by its dimensions, rewarded by its remoteness. Our delivery is by no means comprehensive — for every grain of sand there is a desert word, a desert painting, a desert thought.

Asian Deserts
Gobi Desert

Middle Eastern/African Deserts
The Sahara Desert

Sahara Desert
Sahara Desert, is a great desert area, lying in Northern Africa, and the western portion of the broad belt of arid land ,extends from the Atlantic Ocean eastward past the Red Sea to Iraq.

Sahara Desert
Here’s a fact to challenge popular imagination: more people drown in the Sahara than die from exposure or thirst. It may not rain often and it may not rain long but, in the capricious ways of this vast inland plain, when it does rain, it rains with devastating ferocity.

Wadi Rum: Jordan
Catch a camel into the Wadi Rum desert and you’ll find yourself in ‘Heroic and Biblical Adventure’ country. You’d be forgiven for thinking that, at any moment, you’ll stumble across a bearded and besandalled Charlton Heston looking square-jawed and self-righteous. It was, after all, in this neck of the woods that seas got parted and the tribes of Israel did some serious wandering.

South American Deserts
Atacama Desert
The Atacama desert in Chile is as parched as a parson’s Sunday sermon. In fact, it’s the driest desert in the world. There are parts of it where rain has never been recorded and the precious little precipitation (1cm/0.3in per year) that does fall comes from fog.

Cold Deserts
Ultima Thule, Greenland
There’s nothing in the law books that says a desert has to be hot, sandy and unpleasant; it’s equally legitimate for a desert to be cold, icy and unpleasant. As long as it’s uncultivated and uninhabitable it makes the grade, desertwise, and Ultima Thule is a shoo-in.

Siberia, Russia
Think Siberia and think cold. Think hoarfrosted faces, howling wolves, frozen mountains, salt mines, human chain gangs and exile. Maxim Gorky once called it a ‘land of chains and ice’ and, until recently, the description still held good. Tsars and Party apparatchiks might have had opposing political ideologies but they were of one mind when it came to Siberia.

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