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Englisch

run in the root xwindow

Telugu

రూట్ ఎక్స్ విండో లొ నడుపు

Letzte Aktualisierung: 2011-10-23
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Englisch

run in the specified xwindow

Telugu

నిర్దెశించిన ఎక్స్ విండో లొ నడుపు

Letzte Aktualisierung: 2011-10-23
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Englisch

do not run in the background.

Telugu

బ్యాక్‌గ్రౌండు నందు నడుపవద్దు.

Letzte Aktualisierung: 2011-10-23
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Englisch

are you still in the ground opposite team bowlers fear when delivary to bowl

Telugu

బౌలింగ్ చేయడానికి డెలివరీ అయినప్పుడు జట్టు బౌలర్లు భయపడుతున్నారు

Letzte Aktualisierung: 2019-12-24
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Referenz: Anonym

Englisch

kthreadd manages kernel threads. the children processes run in the kernel, controlling hard disk access, etc.

Telugu

name column tooltip. first item is the name

Letzte Aktualisierung: 2011-10-23
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Englisch

my house is a two storied building in the heart of the city. i feel lucky enough to have a house & all other facilities. the house is newly built by my father. before the first floor was constructed we used to live on the ground floor. we have a drawing room, a guest room, two bed rooms & two bathrooms attached with a puja room. my house is beautifully decorated by my mother. the rooms are full of sunlight which is really enjoyable in winters. we also have two balconies attached with the two bedrooms. the favourite part in my house is the small garden we have. my father has also made a swing for me. every evening i play with my friends & enjoy the sunset. we stay on the first floor. my grandparents stay in the ground floor. my grandma’s room is also my favourite place in the house. their room is filled with pictures of my childhood which i really enjoy to see.

Telugu

పిల్లల కోసం హిందీలో మేరా ఘర్ పై వ్యాసం

Letzte Aktualisierung: 2021-11-08
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Warnung: Enthält unsichtbare HTML-Formatierung

Englisch

a rabbit is a small mammal with long ears which can be seen in the fields which are close to the jungle. rabbits are found in different parts of the world. they live in burrows which are made inside the ground. during daytime they come on the ground to graze the grass and jump from one end to another. they are always alert from their predators while grazing in the field. when a predator chases a rabbit, it starts running in zig zag pattern in order to make their predator tired.

Telugu

కుందేలు పొడవాటి చెవులు కలిగిన చిన్న క్షీరదం, ఇది అడవికి దగ్గరగా ఉన్న పొలాల్లో కనిపిస్తుంది. ప్రపంచంలోని వివిధ ప్రాంతాల్లో కుందేళ్లు కనిపిస్తాయి. వారు భూమి లోపల చేసిన బొరియలలో నివసిస్తున్నారు. పగటిపూట వారు గడ్డి మేయడానికి మరియు ఒక చివర నుండి మరొక చివరకి దూకడానికి నేలపైకి వస్తారు. పొలంలో మేస్తున్నప్పుడు అవి తమ వేటాడే జంతువుల నుండి ఎల్లప్పుడూ అప్రమత్తంగా ఉంటాయి. ఒక ప్రెడేటర్ కుందేలును వెంబడించినప్పుడు, అది తమ ప్రెడేటర్‌ను అలసిపోయేలా చేయడానికి జిగ్ జాగ్ నమూనాలో పరుగెత్తడం ప్రారంభిస్తుంది.

Letzte Aktualisierung: 2022-05-05
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Englisch

a borehole is a narrow shaft bored in the ground, either vertically or horizontally. a borehole may be constructed for many different purposes, including the extraction of water, other liquids (such as petroleum) or gases (such as natural gas), as part of a geotechnical investigation, environmental site assessment, mineral exploration, temperature measurement, as a pilot hole for installing piers or underground utilities, for geothermal installations, or for underground storage of unwanted substances, e.g. in carbon capture and storage. contents

Telugu

బురెల్ న వ్యాసం

Letzte Aktualisierung: 2017-08-07
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Englisch

jsome of the important merits and the demerits of joint family system in india are as follows: in india, the joint family system has continued down the ages for various reasons. as we all know, a particular social institution continues to exist so long as it has a purpose to serve. it always responds to the social requirements of the times. it stagnates and finally withers away only when there is no proper leadership to direct it. family image courtesy : jrobertsphotography.com.au/files/2713628/uploaded/20001.jpg in the indian context, the system continued due to a host of factors. first, our country was under foreign domination for several centuries. secondly, the leadership, perhaps unimaginatively, believed in continuity for its own sake, rather than in change. thirdly, there was a sort of indifferent passivity on the part of the leaders. it could, of course, be also due to the exhaustion of the will to act. be it as it may, let us now discuss the merits and the demerits of the system. merits of the joint family: (1) simple division of labour: joint family system enjoys all the advantages of a simple division of labour. here the work is distributed among the members on the basis of age and sex keeping individual ability in view. in an agricultural economy much manpower is needed for sowing, ploughing, harvesting and also protecting crops from heat and wind. the male members are engaged in such work as furrowing, sowing and irrigation. children, old persons and women watch the crops in the field particularly during the harvesting period. in this way, the co-operation of all members helps to save money that would have otherwise been paid to outside labourers. moreover, every member of the family is ensured of at least some food, clothing and shelter, which are very essential for a healthy and developed economy. (2) avoids fragmentation of land: so far as the joint family is concerned, the property is held in common. as such it does away with the evils of subdivision and fragmentation of land and promotes scientific farming. it enjoys all the advantages of large scale production. (3) money saving device: a joint family is advantageous from the economic standpoint. since things are consumed in a large quantity, they can be procured at a cheap rate. again so far as accommodation is concerned, the joint family saves money that would have otherwise been paid for establishing separate households. besides, the family saves considerable amount of money by not employing outside labour. (4) insurance against odds: favouring the joint family system pandit jawaharlal nehru has remarked that it is an insurance against difficult times. it provides social security to its members, especially to the old, the children, the insane, the widows, the physically handicapped and the helpless. further, the joint family plays an important role in providing much assistance and help at such time as pregnancy, sickness etc. life of an individual in the joint family is properly looked after right from the cradle to the grave. (5) place of recreation: the joint family is an ideal place for recreation. it is instrumental in creating a stimulating atmosphere through the cumulative effect of the lisping talk of the children, the expression of sisterly, brotherly and motherly love, the reproach of the elders and the fun and frolic of the other family members. in this way the joint family naturally acts as a veritable source of recreation with immunity from monotony and boredom. (6) satisfaction of basic needs: food, clothing and shelter are the basic needs of man. the joint family system caters to these basic needs of its members. (7) provides leisure: so far as joint family system is concerned, work is shared by all the members on the basis of age, sex and experience. hence they avail ample leisure. (8) social control: the joint family acts as an agency of social control. the social control .exercised by the joint family is informal in nature. under the constant vigilance of the elders, the undesirable and antisocial propensities of the youngsters are properly checked and thus they are not allowed to go astray. all members scrupulously observe family rules and regulations and respect the elders. (9) cradle of social virtues: the joint family fosters good qualities among its members. they are taught discipline, patience, co-operation, obedience, generosity, selfless service etc. which are virtues of a social life and a real possession of every individual. dr. r. k. mukherjee rightly observes, “the joint family system, based on the virtue of affection, produced that peculiar socio­economic outlook in indian economic organisation which contrasts so favorably with the aggressive individualism of the west.” (10) provides psychological security: the joint family provides psychological security to its members. by attaching supreme importance to collective interests it arrests the growth of excessive individualism and promotes social solidarity. (11) co-operation and economy: the joint family fosters co-operation and economy achieved by few other institutions. cultural unity and associational feeling are markedly visible among the members. (12) socialism in wealth: joint family instills the socialistic spirit among the members. according to jathar and berry, everyone in a joint family earns according to his capabilities but obtains according to his need. in this way, in a joint family the socialistic ideal “from each according to his ability, to each according to his needs” is realized. (13) continuity of culture: in a joint family, the younger members are immensely benefitted by the experiences of elders. the elders also guide the young members in developing joint family sentiment and broad social outlook. all these are potent factors in the continuance of cultural traditions. this institution of joint family though of ancient origin has not only survived for its manifold virtues but has stimulated the social life. it has ensured the continuity of rich traditional value and culture. demerits of the joint family: in the present context, the joint family system, for the most part, has lost its effectiveness. some of its merits have turned out to be dysfunctional in certain respects. the demerits of the joint family system are as follows: 1. hindrance in the development of personality: one of the ugliest features of the joint family system is that it stands in the way of the development of the personalities of its members. it so happens that the oldest member very often assumes rulership. he, in virtue of his age, tends to look upon all others as mere children. he behaves with them accordingly. as a result, the other members, though they are full-blown individuals, fail to develop their personalities in a natural way. they get dwarfed emotionally and intellectually. furthermore, the youngsters in the joint family do not get enough scope to develop qualities like adventure, initiative, self- determination, industriousness etc. 2. strife: one word of opposition or of self-assertion with dignity from the daughters-in-law is enough to set the house on fire literally. they are abused and even beaten by their husbands who are provoked to do so by their mothers. mutual hatred and jealousy among the daughters-in-law leads to enmity among the brothers themselves. there is round-the clock infighting over the doings of children. adults are compelled to spend their precious time in the setting of petty quarrels. the house gets divided against itself. 3. source of litigation: the joint family system encourages litigation. normally disputes occur at the time of the partition of movable or immovable property. often they assume serious proportions and ordinarily these are not settled without the intervention of the court of law. moreover, the disputes involve colossal wastage of time, energy, money and more importantly loss of mental equilibrium. 4. loss of privacy: privacy is practically absent in a joint family set-up. the newlywed couple hardly avail an opportunity to develop intimacy between them. this lack of privacy naturally leads to frustration and psychological disturbances. again over crowdedness also has its baneful effects on the development of children. 5. the deplorable condition of women: this is one of the major causes for the disintegration of joint family system. in the joint family, the daughters-in-law do not get any opportunity whatsoever to unfold their potentialities, talents etc. they are expected to serve the whole family like slaves. more often than not, they cannot afford to look after their own children for fear of censure etc. they can hardly meet their husbands during day time. the position is no better at night. the husbands return home and either fall asleep or merely gratify sexual impulse with them without any emotional overtones to the act. mothers-in-law do untold injustice to daughters-in-law. the other relatives make things even worse for the poor brides. this often leads to the very tragic phenomenon of commission of suicide. the husband-wife, mother-child relations become purely artificial without a touch of spontaneity about them. 6. lethargy and indolence: due to collective responsibility most members tend to be lethargic. the reason is simple. they get all the facilities, whether or not they work hard. the wives of the hard-working members instigate them not to exert themselves unnecessarily. the net result of all this is that while a few members do honest labour, the majority profit at their expense and do nothing but eat, sleep and bring forth offspring. 7. uncontrolled procreation: since the responsibility of bringing up children is purely collective, individual parents do not feel the necessity of limiting the size of their families. family planning does not confer any additional advantages on the practitioner in a joint set-up. nor does the member who earns more get any additional benefit there from. this has a highly depressing effect on such members and simultaneously, promotes irresponsibility among others. the upshot of it all is that they procreate children rather irresponsibly adding to the collective burden. 8. child marriage: incidence of child marriage is quite high in case of the joint family. factors like perception of marriage as a burden on the part of ‘karta’ and the eagerness of the elderly people to see the marriage of their grandsons and granddaughters lead to child marriage. child marriage not only affects the physical and mental health of the children but also contributes to the rapid growth of population. 9. limits social mobility: the joint family system hinders the process of social mobility. factors like intimate familial ties and sentimental attachment of the members to the family limit social mobility. 10. miserable economic condition: due to prevalence of many formidable factors such as the daily strife, the deplorable plight of women, absolute rule of elders, lack of responsibility on youngsters and blind procreation, the economic condition of the joint family becomes very dismal and miserable. everyone in a joint family knows that whatsoever he spends will be managed by the family. he will, therefore, not try to save but will, on the other hand, spend to the maximum. this is certainly an unhealthy practice pursued by some in a joint family set-up. again, being joint responsibility common property is neglected and particularly nobody pays any care and attention to the landed property. produce considerably comes down. there is no initiative and this result in lowering of standard. 11. hinders social change: the joint family system believes in conservative practices, status quo, customs and traditions. as such, the process of social change is arrested to a remarkable extent. to sum up, the defects of the joint family far outweigh the advantages which accrue from it and have negative them. consequently, the joint family is fast becoming disorganised. it is impossible to save the joint family system from disorganization, though its advantages can, with effort, be reinstituted in novel form in the nuclear families.

Telugu

ఉమ్మడి కుటుంబం వ్యాసం

Letzte Aktualisierung: 2015-08-25
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Referenz: Anonym

Englisch

nature, in the broadest sense, is the natural, physical, or material world or universe. "nature" can refer to the phenomena of the physical world, and also to life in general. the study of nature is a large part of science. although humans are part of nature, human activity is often understood as a separate category from other natural phenomena. the word nature is derived from the latin word natura, or "essential qualities, innate disposition", and in ancient times, literally meant "birth".[1] natura is a latin translation of the greek word physis (φύσις), which originally related to the intrinsic characteristics that plants, animals, and other features of the world develop of their own accord.[2][3] the concept of nature as a whole, the physical universe, is one of several expansions of the original notion; it began with certain core applications of the word φύσις by pre-socratic philosophers, and has steadily gained currency ever since. this usage continued during the advent of modern scientific method in the last several centuries.[4][5] within the various uses of the word today, "nature" often refers to geology and wildlife. nature can refer to the general realm of living plants and animals, and in some cases to the processes associated with inanimate objects – the way that particular types of things exist and change of their own accord, such as the weather and geology of the earth. it is often taken to mean the "natural environment" or wilderness–wild animals, rocks, forest, and in general those things that have not been substantially altered by human intervention, or which persist despite human intervention. for example, manufactured objects and human interaction generally are not considered part of nature, unless qualified as, for example, "human nature" or "the whole of nature". this more traditional concept of natural things which can still be found today implies a distinction between the natural and the artificial, with the artificial being understood as that which has been brought into being by a human consciousness or a human mind. depending on the particular context, the term "natural" might also be distinguished from the unnatural or the supernatural. contents 1 earth 1.1 geology 1.1.1 geological evolution 1.2 historical perspective 2 atmosphere, climate, and weather 3 water on earth 3.1 oceans 3.2 lakes 3.2.1 ponds 3.3 rivers 3.4 streams 4 ecosystems 4.1 wilderness 5 life 5.1 evolution 5.2 microbes 5.3 plants and animals 6 human interrelationship 6.1 aesthetics and beauty 6.2 value of nature 7 matter and energy 8 beyond earth 9 see also 10 notes and references 11 external links earth main articles: earth and earth science view of the earth, taken in 1972 by the apollo 17 astronaut crew. this image is the only photograph of its kind to date, showing a fully sunlit hemisphere of the earth. earth (or, "the earth") is the only planet known to support life, and its natural features are the subject of many fields of scientific research. within the solar system, it is third closest to the sun; it is the largest terrestrial planet and the fifth largest overall. its most prominent climatic features are its two large polar regions, two relatively narrow temperate zones, and a wide equatorial tropical to subtropical region.[6] precipitation varies widely with location, from several metres of water per year to less than a millimetre. 71 percent of the earth's surface is covered by salt-water oceans. the remainder consists of continents and islands, with most of the inhabited land in the northern hemisphere. earth has evolved through geological and biological processes that have left traces of the original conditions. the outer surface is divided into several gradually migrating tectonic plates. the interior remains active, with a thick layer of plastic mantle and an iron-filled core that generates a magnetic field. this iron core is composed of a solid inner phase, and a fluid outer phase. it is the rotation of the outer, fluid iron core that generates an electrical current through dynamo action, which in turn generates a strong magnetic field. the atmospheric conditions have been significantly altered from the original conditions by the presence of life-forms,[7] which create an ecological balance that stabilizes the surface conditions. despite the wide regional variations in climate by latitude and other geographic factors, the long-term average global climate is quite stable during interglacial periods,[8] and variations of a degree or two of average global temperature have historically had major effects on the ecological balance, and on the actual geography of the earth.[9][10] geology main article: geology three types of geological plate tectonic boundaries. geology is the science and study of the solid and liquid matter that constitutes the earth. the field of geology encompasses the study of the composition, structure, physical properties, dynamics, and history of earth materials, and the processes by which they are formed, moved, and changed. the field is a major academic discipline, and is also important for mineral and hydrocarbon extraction, knowledge about and mitigation of natural hazards, some geotechnical engineering fields, and understanding past climates and environments. geological evolution the geology of an area evolves through time as rock units are deposited and inserted and deformational processes change their shapes and locations. rock units are first emplaced either by deposition onto the surface or intrude into the overlying rock. deposition can occur when sediments settle onto the surface of the earth and later lithify into sedimentary rock, or when as volcanic material such as volcanic ash or lava flows, blanket the surface. igneous intrusions such as batholiths, laccoliths, dikes, and sills, push upwards into the overlying rock, and crystallize as they intrude. after the initial sequence of rocks has been deposited, the rock units can be deformed and/or metamorphosed. deformation typically occurs as a result of horizontal shortening, horizontal extension, or side-to-side (strike-slip) motion. these structural regimes broadly relate to convergent boundaries, divergent boundaries, and transform boundaries, respectively, between tectonic plates. historical perspective main articles: history of the earth and evolution plankton inhabit oceans, seas and lakes, and have existed in various forms for at least 2 billion years.[11] an animation showing the movement of the continents from the separation of pangaea until the present day. earth is estimated to have formed 4.54 billion years ago from the solar nebula, along with the sun and other planets.[12] the moon formed roughly 20 million years later. initially molten, the outer layer of the earth cooled, resulting in the solid crust. outgassing and volcanic activity produced the primordial atmosphere. condensing water vapor, most or all of which came from ice delivered by comets, produced the oceans and other water sources.[13] the highly energetic chemistry is believed to have produced a self-replicating molecule around 4 billion years ago.[14] continents formed, then broke up and reformed as the surface of earth reshaped over hundreds of millions of years, occasionally combining to make a supercontinent. roughly 750 million years ago, the earliest known supercontinent rodinia, began to break apart. the continents later recombined to form pannotia which broke apart about 540 million years ago, then finally pangaea, which broke apart about 180 million years ago.[15] during the neoproterozoic era covered much of the earth in glaciers and ice sheets. this hypothesis has been termed the "snowball earth", and it is of particular interest as it precedes the cambrian explosion in which multicellular life forms began to proliferate about 530–540 million years ago.[16] since the cambrian explosion there have been five distinctly identifiable mass extinctions.[17] the last mass extinction occurred some 66 million years ago, when a meteorite collision probably triggered the extinction of the non-avian dinosaurs and other large reptiles, but spared small animals such as mammals. over the past 66 million years, mammalian life diversified.[18] several million years ago, a species of small african ape gained the ability to stand upright.[11] the subsequent advent of human life, and the development of agriculture and further civilization allowed humans to affect the earth more rapidly than any previous life form, affecting both the nature and quantity of other organisms as well as global climate. by comparison, the great oxygenation event, produced by the proliferation of algae during the siderian period, required about 300 million years to culminate. the present era is classified as part of a mass extinction event, the holocene extinction event, the fastest ever to have occurred.[19][20] some, such as e. o. wilson of harvard university, predict that human destruction of the biosphere could cause the extinction of one-half of all species in the next 100 years.[21] the extent of the current extinction event is still being researched, debated and calculated by biologists.[22] atmosphere, climate, and weather lightning blue light is scattered more than other wavelengths by the gases in the atmosphere, giving the earth a blue halo when seen from space a tornado in central oklahoma main articles: atmosphere of earth, climate and weather the earth's atmosphere is a key factor in sustaining the ecosystem. the thin layer of gases that envelops the earth is held in place by gravity. air is mostly nitrogen, oxygen, water vapor, with much smaller amounts of carbon dioxide, argon, etc. the atmospheric pressure declines steadily with altitude. the ozone layer plays an important role in depleting the amount of ultraviolet (uv) radiation that reaches the surface. as dna is readily damaged by uv light, this serves to protect life at the surface. the atmosphere also retains heat during the night, thereby reducing the daily temperature extremes. terrestrial weather occurs almost exclusively in the lower part of the atmosphere, and serves as a convective system for redistributing heat. ocean currents are another important factor in determining climate, particularly the major underwater thermohaline circulation which distributes heat energy from the equatorial oceans to the polar regions. these currents help to moderate the differences in temperature between winter and summer in the temperate zones. also, without the redistributions of heat energy by the ocean currents and atmosphere, the tropics would be much hotter, and the polar regions much colder. weather can have both beneficial and harmful effects. extremes in weather, such as tornadoes or hurricanes and cyclones, can expend large amounts of energy along their paths, and produce devastation. surface vegetation has evolved a dependence on the seasonal variation of the weather, and sudden changes lasting only a few years can have a dramatic effect, both on the vegetation and on the animals which depend on its growth for their food. climate is a measure of the long-term trends in the weather. various factors are known to influence the climate, including ocean currents, surface albedo, greenhouse gases, variations in the solar luminosity, and changes to the earth's orbit. based on historical records, the earth is known to have undergone drastic climate changes in the past, including ice ages. the climate of a region depends on a number of factors, especially latitude. a latitudinal band of the surface with similar climatic attributes forms a climate region. there are a number of such regions, ranging from the tropical climate at the equator to the polar climate in the northern and southern extremes. weather is also influenced by the seasons, which result from the earth's axis being tilted relative to its orbital plane. thus, at any given time during the summer or winter, one part of the earth is more directly exposed to the rays of the sun. this exposure alternates as the earth revolves in its orbit. at any given time, regardless of season, the northern and southern hemispheres experience opposite seasons. weather is a chaotic system that is readily modified by small changes to the environment, so accurate weather forecasting is limited to only a few days.[citation needed] overall, two things are happening worldwide: (1) temperature is increasing on the average; and (2) regional climates have been undergoing noticeable changes.[23] water on earth the iguazu falls on the border between brazil and argentina main article: water water is a chemical substance that is composed of hydrogen and oxygen and is vital for all known forms of life.[24] in typical usage, water refers only to its liquid form or state, but the substance also has a solid state, ice, and a gaseous state, water vapor or steam. water covers 71% of the earth's surface.[25] on earth, it is found mostly in oceans and other large water bodies, with 1.6% of water below ground in aquifers and 0.001% in the air as vapor, clouds, and precipitation.[26][27] oceans hold 97% of surface water, glaciers and polar ice caps 2.4%, and other land surface water such as rivers, lakes and ponds 0.6%. additionally, a minute amount of the earth's water is contained within biological bodies and manufactured products. oceans a view of the atlantic ocean from leblon, rio de janeiro. view of the earth where all five oceans visible earth's oceans arctic pacific atlantic indian southern world ocean v t e main article: ocean an ocean is a major body of saline water, and a principal component of the hydrosphere. approximately 71% of the earth's surface (an area of some 361 million square kilometers) is covered by ocean, a continuous body of water that is customarily divided into several principal oceans and smaller seas. more than half of this area is over 3,000 meters (9,800 feet) deep. average oceanic salinity is around 35 parts per thousand (ppt) (3.5%), and nearly all seawater has a salinity in the range of 30 to 38 ppt. though generally recognized as several 'separate' oceans, these waters comprise one global, interconnected body of salt water often referred to as the world ocean or global ocean.[28][29] this concept of a global ocean as a continuous body of water with relatively free interchange among its parts is of fundamental importance to oceanography.[30] the major oceanic divisions are defined in part by the continents, various archipelagos, and other criteria: these divisions are (in descending order of size) the pacific ocean, the atlantic ocean, the indian ocean, the southern ocean and the arctic ocean. smaller regions of the oceans are called seas, gulfs, bays and other names. there are also salt lakes, which are smaller bodies of landlocked saltwater that are not interconnected with the world ocean. two notable examples of salt lakes are the aral sea and the great salt lake. lakes lake mapourika, new zealand main article: lake a lake (from latin lacus) is a terrain feature (or physical feature), a body of liquid on the surface of a world that is localized to the bottom of basin (another type of landform or terrain feature; that is, it is not global) and moves slowly if it moves at all. on earth, a body of water is considered a lake when it is inland, not part of the ocean, is larger and deeper than a pond, and is fed by a river.[31][32] the only world other than earth known to harbor lakes is titan, saturn's largest moon, which has lakes of ethane, most likely mixed with methane. it is not known if titan's lakes are fed by rivers, though titan's surface is carved by numerous river beds. natural lakes on earth are generally found in mountainous areas, rift zones, and areas with ongoing or recent glaciation. other lakes are found in endorheic basins or along the courses of mature rivers. in some parts of the world, there are many lakes because of chaotic drainage patterns left over from the last ice age. all lakes are temporary over geologic time scales, as they will slowly fill in with sediments or spill out of the basin containing them. ponds the westborough reservoir (mill pond) in westborough, massachusetts. main article: pond a pond is a body of standing water, either natural or man-made, that is usually smaller than a lake. a wide variety of man-made bodies of water are classified as ponds, including water gardens designed for aesthetic ornamentation, fish ponds designed for commercial fish breeding, and solar ponds designed to store thermal energy. ponds and lakes are distinguished from streams via current speed. while currents in streams are easily observed, ponds and lakes possess thermally driven microcurrents and moderate wind driven currents. these features distinguish a pond from many other aquatic terrain features, such as stream pools and tide pools. rivers the nile river in cairo, egypt's capital city main article: river a river is a natural watercourse,[33] usually freshwater, flowing toward an ocean, a lake, a sea or another river. in a few cases, a river simply flows into the ground or dries up completely before reaching another body of water. small rivers may also be called by several other names, including stream, creek, brook, rivulet, and rill; there is no general rule that defines what can be called a river. many names for small rivers are specific to geographic location; one example is burn in scotland and north-east england. sometimes a river is said to be larger than a creek,[34] but this is not always the case, due to vagueness in the language.[35] a river is part of the hydrological cycle. water within a river is generally collected from precipitation through surface runoff, groundwater recharge, springs, and the release of stored water in natural ice and snowpacks (i.e., from glaciers). streams a rocky stream in hawaii main article: stream a stream is a flowing body of water with a current, confined within a bed and stream banks. in the united states a stream is classified as a watercourse less than 60 feet (18 metres) wide. streams are important as conduits in the water cycle, instruments in groundwater recharge, and they serve as corridors for fish and wildlife migration. the biological habitat in the immediate vicinity of a stream is called a riparian zone. given the status of the ongoing holocene extinction, streams play an important corridor role in connecting fragmented habitats and thus in conserving biodiversity. the study of streams and waterways in general involves many branches of inter-disciplinary natural science and engineering, including hydrology, fluvial geomorphology, aquatic ecology, fish biology, riparian ecology and others. ecosystems loch lomond in scotland forms a relatively isolated ecosystem. the fish community of this lake has remained unchanged over a very long period of time.[36] lush green aravalli mountain range in the desert country-rajasthan, india. a wonder how such greenery can exist in hot rajasthan, a place well known for its thar desert an aerial view of a human ecosystem. pictured is the city of chicago main articles: ecology and ecosystem ecosystems are composed of a variety of abiotic and biotic components that function in an interrelated way.[37] the structure and composition is determined by various environmental factors that are interrelated. variations of these factors will initiate dynamic modifications to the ecosystem. some of the more important components are: soil, atmosphere, radiation from the sun, water, and living organisms. central to the ecosystem concept is the idea that living organisms interact with every other element in their local environme

Telugu

nature, in the broadest sense, is the natural, physical, or material world or universe. "nature" can refer to the phenomena of the physical world, and also to life in general. the study of nature is a large part of science. although humans are part of nature, human activity is often understood as a separate category from other natural phenomena. the word nature is derived from the latin word natura, or "essential qualities, innate disposition", and in ancient times, literally meant "birth".[1] natura is a latin translation of the greek word physis (φύσις), which originally related to the intrinsic characteristics that plants, animals, and other features of the world develop of their own accord.[2][3] the concept of nature as a whole, the physical universe, is one of several expansions of the original notion; it began with certain core applications of the word φύσις by pre-socratic philosophers, and has steadily gained currency ever since. this usage continued during the advent of modern scientific method in the last several centuries.[4][5] within the various uses of the word today, "nature" often refers to geology and wildlife. nature can refer to the general realm of living plants and animals, and in some cases to the processes associated with inanimate objects – the way that particular types of things exist and change of their own accord, such as the weather and geology of the earth. it is often taken to mean the "natural environment" or wilderness–wild animals, rocks, forest, and in general those things that have not been substantially altered by human intervention, or which persist despite human intervention. for example, manufactured objects and human interaction generally are not considered part of nature, unless qualified as, for example, "human nature" or "the whole of nature". this more traditional concept of natural things which can still be found today implies a distinction between the natural and the artificial, with the artificial being understood as that which has been brought into being by a human consciousness or a human mind. depending on the particular context, the term "natural" might also be distinguished from the unnatural or the supernatural. contents 1 earth 1.1 geology 1.1.1 geological evolution 1.2 historical perspective 2 atmosphere, climate, and weather 3 water on earth 3.1 oceans 3.2 lakes 3.2.1 ponds 3.3 rivers 3.4 streams 4 ecosystems 4.1 wilderness 5 life 5.1 evolution 5.2 microbes 5.3 plants and animals 6 human interrelationship 6.1 aesthetics and beauty 6.2 value of nature 7 matter and energy 8 beyond earth 9 see also 10 notes and references 11 external links earth main articles: earth and earth science view of the earth, taken in 1972 by the apollo 17 astronaut crew. this image is the only photograph of its kind to date, showing a fully sunlit hemisphere of the earth. earth (or, "the earth") is the only planet known to support life, and its natural features are the subject of many fields of scientific research. within the solar system, it is third closest to the sun; it is the largest terrestrial planet and the fifth largest overall. its most prominent climatic features are its two large polar regions, two relatively narrow temperate zones, and a wide equatorial tropical to subtropical region.[6] precipitation varies widely with location, from several metres of water per year to less than a millimetre. 71 percent of the earth's surface is covered by salt-water oceans. the remainder consists of continents and islands, with most of the inhabited land in the northern hemisphere. earth has evolved through geological and biological processes that have left traces of the original conditions. the outer surface is divided into several gradually migrating tectonic plates. the interior remains active, with a thick layer of plastic mantle and an iron-filled core that generates a magnetic field. this iron core is composed of a solid inner phase, and a fluid outer phase. it is the rotation of the outer, fluid iron core that generates an electrical current through dynamo action, which in turn generates a strong magnetic field. the atmospheric conditions have been significantly altered from the original conditions by the presence of life-forms,[7] which create an ecological balance that stabilizes the surface conditions. despite the wide regional variations in climate by latitude and other geographic factors, the long-term average global climate is quite stable during interglacial periods,[8] and variations of a degree or two of average global temperature have historically had major effects on the ecological balance, and on the actual geography of the earth.[9][10] geology main article: geology three types of geological plate tectonic boundaries. geology is the science and study of the solid and liquid matter that constitutes the earth. the field of geology encompasses the study of the composition, structure, physical properties, dynamics, and history of earth materials, and the processes by which they are formed, moved, and changed. the field is a major academic discipline, and is also important for mineral and hydrocarbon extraction, knowledge about and mitigation of natural hazards, some geotechnical engineering fields, and understanding past climates and environments. geological evolution the geology of an area evolves through time as rock units are deposited and inserted and deformational processes change their shapes and locations. rock units are first emplaced either by deposition onto the surface or intrude into the overlying rock. deposition can occur when sediments settle onto the surface of the earth and later lithify into sedimentary rock, or when as volcanic material such as volcanic ash or lava flows, blanket the surface. igneous intrusions such as batholiths, laccoliths, dikes, and sills, push upwards into the overlying rock, and crystallize as they intrude. after the initial sequence of rocks has been deposited, the rock units can be deformed and/or metamorphosed. deformation typically occurs as a result of horizontal shortening, horizontal extension, or side-to-side (strike-slip) motion. these structural regimes broadly relate to convergent boundaries, divergent boundaries, and transform boundaries, respectively, between tectonic plates. historical perspective main articles: history of the earth and evolution plankton inhabit oceans, seas and lakes, and have existed in various forms for at least 2 billion years.[11] an animation showing the movement of the continents from the separation of pangaea until the present day. earth is estimated to have formed 4.54 billion years ago from the solar nebula, along with the sun and other planets.[12] the moon formed roughly 20 million years later. initially molten, the outer layer of the earth cooled, resulting in the solid crust. outgassing and volcanic activity produced the primordial atmosphere. condensing water vapor, most or all of which came from ice delivered by comets, produced the oceans and other water sources.[13] the highly energetic chemistry is believed to have produced a self-replicating molecule around 4 billion years ago.[14] continents formed, then broke up and reformed as the surface of earth reshaped over hundreds of millions of years, occasionally combining to make a supercontinent. roughly 750 million years ago, the earliest known supercontinent rodinia, began to break apart. the continents later recombined to form pannotia which broke apart about 540 million years ago, then finally pangaea, which broke apart about 180 million years ago.[15] during the neoproterozoic era covered much of the earth in glaciers and ice sheets. this hypothesis has been termed the "snowball earth", and it is of particular interest as it precedes the cambrian explosion in which multicellular life forms began to proliferate about 530–540 million years ago.[16] since the cambrian explosion there have been five distinctly identifiable mass extinctions.[17] the last mass extinction occurred some 66 million years ago, when a meteorite collision probably triggered the extinction of the non-avian dinosaurs and other large reptiles, but spared small animals such as mammals. over the past 66 million years, mammalian life diversified.[18] several million years ago, a species of small african ape gained the ability to stand upright.[11] the subsequent advent of human life, and the development of agriculture and further civilization allowed humans to affect the earth more rapidly than any previous life form, affecting both the nature and quantity of other organisms as well as global climate. by comparison, the great oxygenation event, produced by the proliferation of algae during the siderian period, required about 300 million years to culminate. the present era is classified as part of a mass extinction event, the holocene extinction event, the fastest ever to have occurred.[19][20] some, such as e. o. wilson of harvard university, predict that human destruction of the biosphere could cause the extinction of one-half of all species in the next 100 years.[21] the extent of the current extinction event is still being researched, debated and calculated by biologists.[22] atmosphere, climate, and weather lightning blue light is scattered more than other wavelengths by the gases in the atmosphere, giving the earth a blue halo when seen from space a tornado in central oklahoma main articles: atmosphere of earth, climate and weather the earth's atmosphere is a key factor in sustaining the ecosystem. the thin layer of gases that envelops the earth is held in place by gravity. air is mostly nitrogen, oxygen, water vapor, with much smaller amounts of carbon dioxide, argon, etc. the atmospheric pressure declines steadily with altitude. the ozone layer plays an important role in depleting the amount of ultraviolet (uv) radiation that reaches the surface. as dna is readily damaged by uv light, this serves to protect life at the surface. the atmosphere also retains heat during the night, thereby reducing the daily temperature extremes. terrestrial weather occurs almost exclusively in the lower part of the atmosphere, and serves as a convective system for redistributing heat. ocean currents are another important factor in determining climate, particularly the major underwater thermohaline circulation which distributes heat energy from the equatorial oceans to the polar regions. these currents help to moderate the differences in temperature between winter and summer in the temperate zones. also, without the redistributions of heat energy by the ocean currents and atmosphere, the tropics would be much hotter, and the polar regions much colder. weather can have both beneficial and harmful effects. extremes in weather, such as tornadoes or hurricanes and cyclones, can expend large amounts of energy along their paths, and produce devastation. surface vegetation has evolved a dependence on the seasonal variation of the weather, and sudden changes lasting only a few years can have a dramatic effect, both on the vegetation and on the animals which depend on its growth for their food. climate is a measure of the long-term trends in the weather. various factors are known to influence the climate, including ocean currents, surface albedo, greenhouse gases, variations in the solar luminosity, and changes to the earth's orbit. based on historical records, the earth is known to have undergone drastic climate changes in the past, including ice ages. the climate of a region depends on a number of factors, especially latitude. a latitudinal band of the surface with similar climatic attributes forms a climate region. there are a number of such regions, ranging from the tropical climate at the equator to the polar climate in the northern and southern extremes. weather is also influenced by the seasons, which result from the earth's axis being tilted relative to its orbital plane. thus, at any given time during the summer or winter, one part of the earth is more directly exposed to the rays of the sun. this exposure alternates as the earth revolves in its orbit. at any given time, regardless of season, the northern and southern hemispheres experience opposite seasons. weather is a chaotic system that is readily modified by small changes to the environment, so accurate weather forecasting is limited to only a few days.[citation needed] overall, two things are happening worldwide: (1) temperature is increasing on the average; and (2) regional climates have been undergoing noticeable changes.[23] water on earth the iguazu falls on the border between brazil and argentina main article: water water is a chemical substance that is composed of hydrogen and oxygen and is vital for all known forms of life.[24] in typical usage, water refers only to its liquid form or state, but the substance also has a solid state, ice, and a gaseous state, water vapor or steam. water covers 71% of the earth's surface.[25] on earth, it is found mostly in oceans and other large water bodies, with 1.6% of water below ground in aquifers and 0.001% in the air as vapor, clouds, and precipitation.[26][27] oceans hold 97% of surface water, glaciers and polar ice caps 2.4%, and other land surface water such as rivers, lakes and ponds 0.6%. additionally, a minute amount of the earth's water is contained within biological bodies and manufactured products. oceans a view of the atlantic ocean from leblon, rio de janeiro. view of the earth where all five oceans visible earth's oceans arctic pacific atlantic indian southern world ocean v t e main article: ocean an ocean is a major body of saline water, and a principal component of the hydrosphere. approximately 71% of the earth's surface (an area of some 361 million square kilometers) is covered by ocean, a continuous body of water that is customarily divided into several principal oceans and smaller seas. more than half of this area is over 3,000 meters (9,800 feet) deep. average oceanic salinity is around 35 parts per thousand (ppt) (3.5%), and nearly all seawater has a salinity in the range of 30 to 38 ppt. though generally recognized as several 'separate' oceans, these waters comprise one global, interconnected body of salt water often referred to as the world ocean or global ocean.[28][29] this concept of a global ocean as a continuous body of water with relatively free interchange among its parts is of fundamental importance to oceanography.[30] the major oceanic divisions are defined in part by the continents, various archipelagos, and other criteria: these divisions are (in descending order of size) the pacific ocean, the atlantic ocean, the indian ocean, the southern ocean and the arctic ocean. smaller regions of the oceans are called seas, gulfs, bays and other names. there are also salt lakes, which are smaller bodies of landlocked saltwater that are not interconnected with the world ocean. two notable examples of salt lakes are the aral sea and the great salt lake. lakes lake mapourika, new zealand main article: lake a lake (from latin lacus) is a terrain feature (or physical feature), a body of liquid on the surface of a world that is localized to the bottom of basin (another type of landform or terrain feature; that is, it is not global) and moves slowly if it moves at all. on earth, a body of water is considered a lake when it is inland, not part of the ocean, is larger and deeper than a pond, and is fed by a river.[31][32] the only world other than earth known to harbor lakes is titan, saturn's largest moon, which has lakes of ethane, most likely mixed with methane. it is not known if titan's lakes are fed by rivers, though titan's surface is carved by numerous river beds. natural lakes on earth are generally found in mountainous areas, rift zones, and areas with ongoing or recent glaciation. other lakes are found in endorheic basins or along the courses of mature rivers. in some parts of the world, there are many lakes because of chaotic drainage patterns left over from the last ice age. all lakes are temporary over geologic time scales, as they will slowly fill in with sediments or spill out of the basin containing them. ponds the westborough reservoir (mill pond) in westborough, massachusetts. main article: pond a pond is a body of standing water, either natural or man-made, that is usually smaller than a lake. a wide variety of man-made bodies of water are classified as ponds, including water gardens designed for aesthetic ornamentation, fish ponds designed for commercial fish breeding, and solar ponds designed to store thermal energy. ponds and lakes are distinguished from streams via current speed. while currents in streams are easily observed, ponds and lakes possess thermally driven microcurrents and moderate wind driven currents. these features distinguish a pond from many other aquatic terrain features, such as stream pools and tide pools. rivers the nile river in cairo, egypt's capital city main article: river a river is a natural watercourse,[33] usually freshwater, flowing toward an ocean, a lake, a sea or another river. in a few cases, a river simply flows into the ground or dries up completely before reaching another body of water. small rivers may also be called by several other names, including stream, creek, brook, rivulet, and rill; there is no general rule that defines what can be called a river. many names for small rivers are specific to geographic location; one example is burn in scotland and north-east england. sometimes a river is said to be larger than a creek,[34] but this is not always the case, due to vagueness in the language.[35] a river is part of the hydrological cycle. water within a river is generally collected from precipitation through surface runoff, groundwater recharge, springs, and the release of stored water in natural ice and snowpacks (i.e., from glaciers). streams a rocky stream in hawaii main article: stream a stream is a flowing body of water with a current, confined within a bed and stream banks. in the united states a stream is classified as a watercourse less than 60 feet (18 metres) wide. streams are important as conduits in the water cycle, instruments in groundwater recharge, and they serve as corridors for fish and wildlife migration. the biological habitat in the immediate vicinity of a stream is called a riparian zone. given the status of the ongoing holocene extinction, streams play an important corridor role in connecting fragmented habitats and thus in conserving biodiversity. the study of streams and waterways in general involves many branches of inter-disciplinary natural science and engineering, including hydrology, fluvial geomorphology, aquatic ecology, fish biology, riparian ecology and others. ecosystems loch lomond in scotland forms a relatively isolated ecosystem. the fish community of this lake has remained unchanged over a very long period of time.[36] lush green aravalli mountain range in the desert country-rajasthan, india. a wonder how such greenery can exist in hot rajasthan, a place well known for its thar desert an aerial view of a human ecosystem. pictured is the city of chicago main articles: ecology and ecosystem ecosystems are composed of a variety of abiotic and biotic components that function in an interrelated way.[37] the structure and composition is determined by various environmental factors that are interrelated. variations of these factors will initiate dynamic modifications to the ecosystem. some of the more important components are: soil, atmosphere, radiation from the sun, water, and living organisms. central to the ecosystem concept is the idea that living organisms interact with every other element in their local environme

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introduction i am a student of class ix i the kakatpur high school. there is a beautiful garden in front of my school. it is a famous garden in our area. shape and size the garden of our school is oblong in shape. it is three hundred feet long and two hundred feet broad. it is strongly fetched on all sides. fruit and flowers our school garden is full of tress and creepers. there are the plants of fruits, flowers and vegetables. there is a well at the middle of the garden. the garden is divided into four parts. in one there are flower plants only. these are the plants of marigold, jasmine, champak and rose. in another part there are fruit-plants. there are the plants of apple, guava, papaya, banana and cocoanut. in the third part there are the plants of vegetables, such as potato, brinjal, tomato, gourd, pumpkin, bitter-gourd, snake-gourd, bean and arum. in the fourth part there are spinach and other greens. in winter we grow cabbages and cauliflowers. we also grow onions and garlic’s. how we work in the garden the day scholars work in the garden during their gardening-periods. but the boarders work in the evening. we spade the ground and make the beds. we sow seeds and plants trees. in morning and evening we water the plants. we keep the garden neat and clean. we sell the products in the market and we pay the money to the school office. conclusion my school garden is very useful to me. here i get the knowledge of gardening. gardening gives us food and exercise. my school garden is very nice to look at. hence i like it most.

Telugu

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