Poetry in translation from Safarova Zarnigor

Young Central Asian teen girl with long dark hair, brown eyes, a white collared shirt and black sweater, with smoky dark styling surrounding the image. She's holding a book and the initials S.Z.Z. are in the lower right corner in white text on a blue tab.

I translated and analyzed Faynberg’s poem from Russian to English.

Сирень

Давай любовь свою оплачем.

Давай свидание назначим,

Не мучаясь и не грустя.

Сегодня. Десять лет спустя.

Давай сирени наломаем.

Любила ты? И я любил.

Апрель цветёт, как ненормальный.

Апрель заборы проломил.

Сирень горька и безутешна.

Сорви мне счастье наугад.

Мы изменились? Мы всё те же,

Как десять лет тому назад.В глазах твоих все те же кроны.

В моих — всё тот же синий дым.

Стекло с вином губами тронув,

Ты говоришь: «Горим?»

— «Горим!»

Куда? О чём? За что горим мы?

Ах, за начала всех начал!

За польский вальс неповторимый.

Он только нам с тобой звучал.

— Горим?

—Горим! За наши годы.

Кольцо на дно со звоном брось.

За то, что дым сирени горек.

За всё, что в жизни не сбылось.Любовь, куда? Не оглянулась.

О, это вечное «увы».

Горим же за чужую юность!

Они целуются, как мы.Горим за всё! За наши беды.

За эту музыку и боль.

За этот мир, от яблонь белый

И от сирени голубой.

Lilac

Let’s lament our love,

Let’s set up a date

Without torment or sorrow,

Today. Ten years later.

Let’s break lilac branches.

You loved, and I loved.

April blooms like it’s abnormal,

April breaks through the fences.

Lilacs are bitter and hopeless.

Tear out happiness for me at random.

Have we changed? We’re still the same

As ten years ago. In your eyes, it’s still the same foliage.

In my eyes, the same blue smoke.

Touching the glass with wine-soaked lips,

You say: “Are we burning?”

— “We’re burning!”

Where to? What about? What are we burning for?

Ah, for all the beginnings there are!

For the unique Polish waltz,

That only sounded for us.

— Burning?

— Burning! For our years.

Throw the ring to the bottom with a clang.

For the bitter smoke of lilacs.

For everything that hasn’t come true in life.

Love, where to? Without a glance,

Oh, this eternal “alas.”

We’re burning for someone else’s youth!

They are kissing, like we did.

Burning for everything! For all our sorrows.

For this music and pain.

For this world, white from apple trees

And blue from the lilacs.

The poem “Lilacs” delves into the complex theme of love, reminiscence, and the passage of time. It begins with an invitation to lament lost love and to set up a date ten years later without torment or sorrow, acknowledging the enduring nature of the emotive moment.

The author then employs vivid imagery by suggesting to break lilac branches, a symbolic act tied to the past relationship. The poem invokes the spirit of April, alluding to its abnormality, and depicts it shattering through the constraints, almost rebellious in its blooming.

The bitter and hopeless nature of the lilacs reflects the disillusionment and unfulfilled emotions tied to that past connection, calling for the unpredictable tearing out of happiness. The narrator questions if they’ve changed over the years, only to conclude that they remain the same as a decade ago, hinting at the persistence of their emotions.

The dialogue within the poem adds depth, as a conversation ensues about burning and the reasons behind it. The questioning of the purpose of their burning and the acknowledgment of past memories creates a reflective and introspective atmosphere, offering a sense of poignancy and longing.

The poem concludes with a broader reflection on burning for someone else’s youth, symbolizing feelings of lost opportunity and nostalgia. It captures a sense of yearning, loss, and a longing for the unfulfilled aspects of life.

In summary, the poem “Lilacs” conveys a deep sense of melancholy and introspection, blending vivid imagery with symbolic meaning to encapsulate the complexities of love, loss, and the passage of time. It evokes a poignant narrative that draws the reader into a contemplation of the enduring impact of love, memory, and the emotive threads that linger on throughout life’s journey.

✓Safarova Zarnigor Zokhid’s daughter student of Uzbekistan  state world languages university

Young aspiring researcher

Author of several scientific articles on gender in linguistics

Scientific works, poems, reviews, thesis and articles have been published at national and international newspapers, conferences and journals.

✓She has published three books internationally and her books are available for sale on Amazon and several other sites

Essay from Diyora Bakhodirovna

EFFICIENT EDUCATIONAL PROCESS AND TECHNOLOGIZATION OF EDUCATION

Karakalpak State University Kubeysinova Nilufar Makhmutovna

Abstract: In the article, the brief essence of pedagogical technology, innovation, innovative technologies, interactive methods in technological education is revealed. Ways to achieve the effectiveness of the educational process through technologization of education are highlighted.

The development and implementation of educational technologies as a scientific problem envisages conducting special scientific and pedagogical research. It should be noted that educational technology as a research object of pedagogy is not only a method of teaching specific subjects, but also requires a new approach to teaching social sciences. In this regard, it is worth noting that technology is is a process that leads to a quality change in the subject as a result of the effect shown by the subject on the object. Technology always provides for the execution of purposeful actions directed at the object in a certain sequence, using the necessary means and conditions.

Pedagogical technology (PT) is a social phenomenon that, as a result of the teacher’s systematic influence on students with the help of teaching tools, intensively forms predetermined social qualities in them, necessary for society. Since pedagogical technology is a social necessity, it first appeared in the USA in the 70s of the 20th century, and later it was widely used in the educational process in other developed countries. After gaining independence, scientists of Uzbekistan began to establish economic, social, political and scientific-educational relations with foreign countries.As a result, advanced and effective technologies began to enter our country. Along with this, the concept of progressive pedagogical technology in the world has also entered. V.P. Bespalko, one of the first among the CIS countries, described the need to introduce pedagogical technology into the educational process: “PT is a project of the process of forming a student’s personality, which can guarantee pedagogical success without depending on the teacher’s skills.” V. M. Monakhov, one of the Russian scientists, gives a brief definition that “PT is a system of orderly actions that lead to pre-planned results and must be performed”, and draws attention to its main features. According to his definition, “PT-technologies the educational process, increases its reproducibility and the stability of the pedagogical process, and frees it from the subjective characteristics of the executor of this process.” According to M. V. Klarin, PT is the design of the educational process based on predetermined target indicators with a technological approach to the educational process.According to Uzbek pedagogic scientists Nurali Saidakhmedov and Abdurakhmon Ochilov, PT is the process of intensive formation of predetermined personality qualities in them as a result of the teacher’s use of teaching tools to influence certain conditions on students. Pedagog scientist B.L. Farberman defines pedagogical technology as follows: PT is a new approach to the educational process, and social engineering in pedagogy is an expression of consciousness. It is a social phenomenon related to making the pedagogical process a standard based on technical capabilities and human technical thinking and creating its optimal project. In order to compare these definitions with the definitions given far abroad, we will quote the definition given by the Japanese pedagogue scientist T. Sakomoto: PT is the introduction of a systematic and complex way of thinking into pedagogy, in other words, a certain pedagogical process according to the definition of UNESCO, one of the authoritative agencies of the United Nations Organization, “PT is the design and implementation of the entire educational process, building technical and human resources in an interdependent manner in imparting and acquiring knowledge is to use the method of systematic approach”.If we analyze the mentioned definitions from a scientific and philosophical point of view, although the definitions given by foreign scientists and the definitions given by scientists of the CIS countries are close to each other, there are also significant differences. In particular, in the definitions of Sakomoto and UNESCO, special emphasis is placed on the principle of a collective approach. While the systematic approach is mentioned in the definitions given by the scientists of the CIS to PT, it can be seen that it was completely forgotten when the project of the educational process was being drawn up, and the laws and regulations of the principle of the systematic approach were not followed.

 Indeed, for a person who knows well the principle of a systematic approach to objective existence, as Sakomoto says, the concept that “PT is bringing the educational process to a certain system” is enough. Through this concept, it is possible to understand all other features of PT, that is, it is goal-oriented, it consists of several interrelated parts, and others. Because all these properties, according to the theory of systems, are integral qualities of things and phenomena called systems.The new concept of acquiring knowledge in the current educational system requires the use of various methods of modern pedagogical technology. The educational process is a system. Its constituent elements are the educational goal, the expected result, the teacher, the student, the content of education, the method of education, the form of education, educational tools, control and assessment. When designing the educational process, the above elements should be selected correctly. The introduction of pedagogical technologies in the educational process leads to the activity of the teacher as an organizer or consultant. This requires the qualities of independence, creativity and willpower from the student and the teacher.

Innovation (English innovation) means innovation. Innovative technologies are the introduction of innovations and changes to the pedagogical process, the activities of teachers and students, and reasonable interactive methods are used in its implementation. Interactive – (“Inter” is mutual, “act” – to act) is to act mutually. This

the uniqueness of the methods is the joint activity of the teacher and the student. The process of pedagogical cooperation occurs:

1. The student will not be indifferent during the lesson, he will go to independent thinking, creativity and research.

2. Continuity of the student’s interest in science during the educational process is ensured.3. The student approaches the problem independently.

        4. Continuity of the cooperative activity of the teacher and the student is ensured.

Pedagogical technology in the educational process is a coherent process in a clear sequence, it is a pedagogical process aimed at providing a goal-oriented, carefully planned and guaranteed result based on the needs of the student (teacher).

A teacher fulfills the social task of the society, prepares mature specialists. For this reason, the teacher must meet socio-political, pedagogical and personal requirements. Also, he believes in the name of independence, has comprehensively developed scientific thinking, has professional knowledge, is a deep expert in his field, master of pedagogical skills, has acquired pedagogical, psychological and methodological knowledge and skills, and has the ability to exert pedagogical influence. should have the ability to choose the most appropriate methods and tools. The process of pedagogical formation of a special subject teacher begins with the process of education at a higher educational institution. In the educational plans and programs of higher education institutions, the role of general technical sciences is important in teaching the secrets of this profession to the teachers of future labor education and providing scientific knowledge. General technical sciences serve to ensure technological readiness of labor education teachers. No matter how skilled a teacher of labor education may be, if he does not master technical and technological sciences well, he will not succeed in his work. Because the professional activity of a teacher of labor education is closely related to his technological training. That is why technical and technological sciences are of great practical importance in the system of training teachers of special subjects.

Conclusion: An effective solution to the problem of personnel training is, first of all, a professional who has deep knowledge of the fundamentals of psychology, pedagogy, economy, ecology, culture, law and other similar disciplines, who can meet today’s requirements, and who has comprehensive knowledge. It is related to teacher training.

References:

1. Law of the Republic of Uzbekistan “On Education”.

        2. Ismilova Z.K. Pedagogy. Textbook. – T.: Molya-iktisod, 2008.

        3. Ishmukhamedov R. and others. Innovative technologies in education. – T.: “Talent” fund of the President of the Republic of Uzbekistan.

4. Tolipov O’.Q., Usmanboyeva M. Practical foundations of pedagogical technology. – Tashkent, 2006.

Story from Brian Barbeito

Two dogs with brown fur and large pointed ears with a fallen log and autumn leaves in the background.
nature writing and the heart of the forest worlds

if there are twelve to twenty one forests, some loosely connected, some not connected at all, then the woodlands can in a way be seen or broadly interpreted as a being, as a living thing. and where then is the heart, the centre of it all? it is not what a surveyor or trail walker might at first think, which might be where a large pond waits at the bottom of a hill. and it might not either be the large northern tract that houses a marsh and indeed seems like something more extraordinary than the rest. or up by long wide fields that live at the purlieu of a connected woodlands,- it’s reeds and strange old tree branches watching all seasons and all things w/in each season. it is rather, at the end of the long walking trail that travels through autumnal leaves yellow and orange, and wild sumac preternaturally red. there are hundreds if not thousands of evergreens different in size, providing shade to the fairytale-like acres below. this is where the heart of the region’s forests is, and it is quiet and confident, healthy and untroubled by the outside world.

Essay from Ali Akramov

Effect of floods on geological processes in mountains

 National University of Uzbekistan

 Faculty of Hydrometeorology

 1st year student Akramova Shiringul

 Furqatjon’s daughter.

 e-mail: akramovali32@gmail.com

 Phone: +998995524473

 Abstract: Floods have a great influence on the geological processes in the mountains. As a result of the movement of the floods, complex processes such as decay, washing, erosion occur in the mountains. This causes the geological composition of the mountains to change.

Key words: floods, geological processes, terrain, meteorological phenomena, hydrological conditions, ponds, physiography.

Key words: floods, geological processes, terrain, meteorological phenomena, hydrological conditions, ponds, physiography.

Key words: flooding, geological processes, relief, meteorological phenomena,
Hydrological conditions, water, physiography.


 Floods are caused by various geophysical mechanisms in a wide range and of great power. Objectives are considered on geological time and space scales, but the main criteria of climatic, topographical and geological factors of the channel predictably influence and limit the size and extent of local floods in floodplains. Many of these effects are specific and not topographical or climatic, with damage, for example, local correlation of specific types of floods. But some are less specific measures, including geological control over the time, location, connection and magnitude of natural dam failures. In this paper, we describe the main factors that affect the magnitude or insignificance of floods and how these factors vary temporally and spatially over geologic time and spatial scales. 

Or risks are addressed. Even experienced hydrologists and geologists each consider floods to be of scientific interest beyond modern experience, such as the Pleistocene Missoula floods. Such large floods are unique. 1. Due to its uniqueness and role in shaping the landscape, it played an interesting and dramatic role in phrasing 2. Flashes for inquiry and debate, but they are not and usually considered. Normal geophysical component 3. Certificate behavior. 

But really, floods of any size and source can be considered a geological process on the same level as any other Earth system, so tectonics and the atmosphere have attributes, causes, effects, and even correlations. Causes processes such as circulation. Practitioners of paleoflood hydrology, who study floods of various scales and in different geologic periods and environments [Kochel et al. Baker, 1982], well-placed rates and the evaluation, description, and even quantification of these correlations. Indeed, many of the articles in this volume present examples of floods that occur under certain conditions as a result of these geological, physiographic, and climatic interactions. The purpose of this paper is to provide a general context for individual paleoflood studies on landscapes. 

Systematic characterization of the spatial and temporal distribution of large floods and flood-causing mechanisms can thus provide a framework for the ecological status of floods and floods in Earth’s history. These results are consistent with the vapor and physical limits for surface flooding determined from total snow. A closer look at flood-generating processes From an empirical perspective, the magnitude, duration, and extent of river floods vary greatly depending on the source mechanism, global location, geology, and physiography, but despite this variation, how large a flood is.

There are real physical limits to what can be. Meteorological floods are caused by various types of storms that deliver a volume of water up to 1011 m3 for several days or weeks, as well as from seasonally stable climatic conditions that deliver more than 1012 m3 for several weeks or months, and the highest leads to flow. As much as 105 m³/s in large, continental-scale basins. The main limits for meteorological flooding depend, first of all, on the level and volume of precipitation, as well as on the efficiency of distribution of precipitation concentrates to channel networks. 

Global and US flood records show that primarily for basins affected by individual storms, the largest flows occur in areas where atmospheric moisture or storm tracks are intercepted by local topographic relief.For larger basins, the largest fluxes result from seasonally stable climate patterns and, on a global basis, tend to be in tropical regions with more moisture. The contribution of high-relief topography to meteorological flooding is particularly noteworthy because of its dual effects of (1) raising atmospheric moisture, thereby increasing local precipitation, and (2) facilitating more rapid concentration of runoff into channels. 

Floods from dam failures and terrestrial fresh water sources such as lakes and glaciers have similar total volumes to meteorological floods, up to 1013 m3, but larger 2-107 m³/s with waste. During the Pleistocene Ice Age, glaciers and changing hydrologic conditions disrupted drainage systems, causing the largest well-documented dam floods to breach ice dams and basin divides of the Great Lakes. From the Global perspective, the magnitude, duration, and extent of river floods vary greatly depending on the source mechanism, global location, geology, and physiography, but despite this variation, there are real physical limits to how large a flood can be. 

Meteorological floods are caused by various types of storms that deliver a volume of water up to 1011 m3 for several days or weeks, as well as from seasonally stable climatic conditions that deliver more than 1012 m3 for several weeks or months, and the highest leads to flow. As much as 105 m³/s in large, continental-scale basins. The main limits for meteorological flooding depend, first of all, on the level and volume of precipitation, as well as on the efficiency of distribution of precipitation concentrates to channel networks.

Global and US Water Regulations indicate that the largest runoff for a basin affected by individual storms in the first instance is when atmospheric moisture or storm tracks are intercepted by topography. For the larger basins, the largest fluxes result from seasonal climate conditions and occur in the tropics, where there is more moisture on a global basis. The contribution of relief topography to meteorological flooding is particularly high because of its two-fold effect of (1) raising atmospheric moisture, thereby increasing precipitation, and (2) concentrating flow movement into channels.  

Floods from external dams and terrestrial freshwater sources such as lakes and glaciers have total volumes similar to meteorological floods, up to 1013 m3, but less than 2-107 m³/s. L is greater. With. The Pleistocene glacial reglaciations disrupted fluctuating hydrologic resource systems, leading to the failure of ice dams and basin divides of the Great Lakes, the largest well-documented dam floods. From the Global perspective, the magnitude of river floods, a very global place, varies with water volume and power source mechanism, geology, and physiography, but depending on the difference, there are real physical limits to how large flood transport can be. Meteor floods are caused by seasonal climatic conditions of several days or weeks up to 1011 3, while the control of the water volume is different, leads to big. As much as 105 m³/s in large, continental-scale basins.

The main limits for meteorological flooding depend, first of all, on the level and volume of precipitation, as well as on the efficiency of distribution of precipitation concentrates to channel networks. Global and US flood records show that primarily for basins affected by individual storms, the largest flows occur in areas where atmospheric moisture or storm tracks are intercepted by local topographic relief. 

For larger basins, the largest fluxes result from seasonally stable climate patterns and, on a global basis, tend to be in tropical regions with more moisture. The contribution of high-relief topography to meteorological flooding is particularly noteworthy because of its dual effects of (1) raising atmospheric moisture, thereby increasing local precipitation, and (2) facilitating more rapid concentration of runoff into channels. 

Floods from dam failures and terrestrial fresh water sources such as lakes and glaciers have similar total volumes to meteorological floods, up to 1013 m3, but larger 2-107 m³/s with waste. During the Pleistocene Ice Age, glaciers and changing hydrologic conditions disrupted drainage systems, causing the largest well-documented dam floods to breach ice dams and basin divides of the Great Lakes. 

From the Global perspective, the magnitude, duration, and extent of river floods vary greatly depending on the source mechanism, global location, geology, and physiography, but despite this variation, there are real physical limits to how large a flood can be. Meteorological floods are caused by various types of storms that deliver a volume of water up to 1011 m3 for several days or weeks, as well as from seasonally stable climatic conditions that deliver more than 1012 m3 for several weeks or months, and the highest leads to flow. As much as 105 m³/s in large, continental-scale basins. The main limits for meteorological flooding depend, first of all, on the level and volume of precipitation, as well as on the efficiency of distribution of precipitation concentrates to channel networks. 

Global and US flood records show that primarily for basins affected by individual storms, the largest flows occur in areas where atmospheric moisture or storm tracks are intercepted by local topographic relief. For larger basins, the largest fluxes result from seasonally stable climate patterns and, on a global basis, tend to be in tropical regions with more moisture. The contribution of high-relief topography to meteorological flooding is particularly noteworthy because of its dual effects of (1) raising atmospheric moisture, thereby increasing local precipitation, and (2) facilitating more rapid concentration of runoff into channels. 

Floods from dam failures and terrestrial fresh water sources such as lakes and glaciers have similar total volumes to meteorological floods, up to 1013 m3, but larger 2-107 m³/s with waste. During the Pleistocene Ice Age, glaciers and changing hydrologic conditions disrupted drainage systems, causing the largest well-documented dam floods to breach ice dams and basin divides of the Great Lakes.

From the Global perspective, the magnitude, duration, and extent of river floods vary greatly depending on the source mechanism, global location, geology, and physiography, but despite this variation, there are real physical limits to how large a flood can be. Meteorological floods are caused by various types of storms that deliver a volume of water up to 1011 m3 for several days or weeks, as well as from seasonally stable climatic conditions that deliver more than 1012 m3 for several weeks or months, and the highest leads to flow. As much as 105 m³/s in large, continental-scale basins. The main limits for meteorological flooding depend, first of all, on the level and volume of precipitation, as well as on the efficiency of distribution of precipitation concentrates to channel networks.


REFERENCES

 1.E. Costa, U.S. Geological Survey, 10615 Sf Cherry Blossom

Dr., Portland OR, 97216.

G. E. Grant, USDA Forest Service, Pacific Northwest Research

Station, 3200 Jefferson Way, Corvallis. OR 97331

lE. O’Connor, U.S. Geological Survey, 10615 SE Cherry

1990 Blossom Dr., Portland OR, 97216. (oconnor(usgsgov)

Essay from Mahbuba Juraboyeva

Young Central Asian woman with long slightly curly hair, black eyes, and a white blouse with black dots. She's got a green background behind her.

What should be the speech of a lawyer?

        It is known that every professional talk a lot about the important aspects, problems and solutions of his field, people can attract attention. Effective speech and eloquence are also very important in the field of law. Speech is a person’s life; therefore, it is impressive and correct in written and oral speech must be able to speak beautifully. So, mastering speech culture and language standards, is his ability to use the means of expression in different situations. Public speaking, first of all, deep knowledge and experience of the same topic from us demand the moral right to speak in front of others is enough. That is why, we should not be afraid of public speaking. After all, the main thing is not that you speak beautifully, but that you have an idea worth saying is what you can deliver to your audience. Lawyers are always human has to communicate a lot with. It is different during the communication period there may be situations. In similar situations, the lawyer himself. He should be able to manage and convince people through his speech. For example, the court to the rights of another client while the lawyer defends his client not to use offensive words, to make people sitting in the courtroom to his speech.

He should be able to attract, most importantly, he should be able to prove that his client is right should be able to find evidence. If he cannot find such evidence, the lawyer is in court he may not be able to protect his client, he may end up in a disadvantageous situation. Or rather, if a strong opinion is expressed, but it is not delivered correctly, it is the citizen’s fault to prove his innocence or, if he is guilty, to impose a just punishment against him also causes difficulties. If the law is the main tool of the lawyer, the effective expression of it is the word. That’s why the lawyer’s voice he must have an impressive power, only then he can convince everyone to his opinion convinces. In my opinion, every lawyer has his own way of speaking it is required to show that he is a cultured person. Employees in the legal field the symbol of the state. Accordingly, when citizens turn to them, they are obliged to answer, realizing their responsibilities. Lawyers during his career in different audiences, in front of people of various levels it is necessary for them to master the skill of making a successful speech. Of this and for him, first of all, knowing what to deliver to the audience is his main thing able to express ideas clearly and succinctly, having a confident tone, sincere being able to attract the audience to his speech is one of the most important aspects.

             The great American writer Mark Twain says the following in one of his works cited the idea: “To prepare a bright urgent speech, usually it will take me more than three weeks.” So, public speaking at first glance, it seems easy to be able to speak, but the unique knowledge is huge as responsibility demands. Even great orators avoid public speaking they form their speech first. In conclusion, lawyers in speech, first of all, having the ability to convince others is important. Because this is one of the sensitive issues in their work.

                                              Juraboyeva Mahbuba Asqarbek                               Student of Tashkent State Law University   

Essay from Aziza Umurzakova

Young Central Asian teen girl with long dark hair, brown eyes, a white tee shirt, and a watch on her wrist.
Aziza Umurzakova
The role of preschool education, family and society in child education

Abstract:  Through this article, you will learn about the role of pre-school education, family and society in child education. 
Keywords:  Child education, family education, community impact, small state, educational departments.

In 1779, Johann Friedrich Oberlin and Louise Scheppler founded the first institution in Strasbourg for the care and education of preschool children whose parents were away during the day. [5] Around the same time, in 1780, that similar infant institutions were established in Bavaria , in 1802 Pauline zur Lippe founded a preschool in Detmold.
Pre-school, also known as a kindergarten, primary school or play school, is an educational institution that offers children early childhood education before they begin compulsory primary school education. It can be public or private and may be subsidized by public funds.

When talking about the education system, which is of decisive importance in our lives, we have to repeat the wise words of our grandfather Abdulla Avloni: education is a matter of life and death for us," said the President.  

No matter what field we choose, we cannot achieve any changes or a prosperous life without educating modern mature personnel. 

The preparation of such personnel, the healthy gene pool of the nation, begins first of all with the preschool education system. When you compare a child who attended kindergarten with a child who did not attend kindergarten, it is not difficult to notice that there is a huge difference in their thinking level. That is why we raised the issue of revision of the preschool education system to the level of state policy and started great work in this regard. If we do not carry out this work thoroughly, it will be difficult for us to achieve a quality change in the entire education system, to ensure the continuity of education, - Shavkat Mirziyoyev said.

Education is a social phenomenon.  It is from the time when the personal society appeared there is.  In order for a person to be the most perfect breed on earth, he must first be educated necessary.  Abu Lays Samarkandi's work "Bostanul-arifin" on upbringing and education explaining the meaning: "O son, before you educate your children, A well-mannered, well-mannered, and educated person grows up in a well-educated family is enough," he said.  This idea has a special place in Ibn Sina's work.  "To whom Whatever Pandu advises, follow it yourself first," says Allama.  

East thinkers, pedagogic scientists, what is the education for raising a perfect person who justified its necessity, its essence and content. The educational process is organized between educators and students and is a goal-oriented collaborative process. The purpose of education is to form a comprehensive personality. The content of education is related to the set goals and tasks knowledge, skills, beliefs, personality qualities that should be acquired by students character, behavior system is understood.

Preschool Educational Institution, in turn, cooperates with parents those who started it.  This is the most effective cooperation with the family in raising a child one of the methods.  The content of work with parents is varied  and it is necessary to discuss some issues together.  

For example:  

• about the role of the family in raising children, the role of parents laws on preparing children for school;
 
• on the annual work plan of the pre-school education institution; 
• issues about the work of the parents' community are among them.

According to scientific sources, human personality is formed under the influence of three factors.The first of them is the influence of the external social environment in which a person is born and grows up. The second is social education that is systematically given to a person over a long period of time. Is the effect of upbringing, and finally, the third is genetic, which is given to a person through generation is the influence of factors.  Thus, in the psychic development of a person and personal The role of the external social environment and education is decisive in the formation of qualities is important.  This, in turn, is the role of the family and society in the upbringing of the child's personality also shows that the role is extremely large.

 In short, preschool education, family and society in child education also has an equal contribution.  Because the child is the first to receive education in the family further forms, strengthens and brief explanation in preschool education, learns the elements of education through advice or games.  And the upbringing he had certainly applies in society and mutual relations.  This is the basis of child education is considered.

References:
1. O.U. Hasanboyeva, M.X. Tojiyeva, Sh.K. Toshpolatova et al. Preschool education pedagogy. A textbook for pedagogical colleges. (Completed and revised 2nd edition). T .: «ILM ZIYO», 2011. - 184 p.
2. Kushmatova Maftuna Mahamadali qizi. Topic: Family relations and social psychological features of upbringing in child rearing. Graduation thesis. Andijon-2017
3. Islamova, M. Sh. "Fundamentals of Forming a Professional Worldview." Science and Education 2.Special Issue 1 (2021): 78-87.
4. Usarov, J. E., G. N. Sharipova, and Sh. S. Abdusamatova. "The role of student self-development competence in the effectiveness of education and its importance in practice." Science and Education 2.Special Issue 1 (2021): 276-285. 5. Usarov, J. E., L. G. Boboxodjaeva, and N. Yusupova. "The mixed form of education as a modern approach to the pedagogical education cluster." Science and Education 2.Special Issue 1 (2021): 286

Umurzakova Aziza was born 2004 in Uzbekistan.She is a student of Jizzakh State Pedagogical University. From a young age,she was interested in literature .About a lot of articles have been published in magazines of Europe, America, Germany , Great Britain and Uzbekistan magazines and conferences.

Poetry from Kholida Toirjonova

One Day

One day, I will leave this world behind
Leaving my existence to be forgotten by you
However I came, that's how I will go
You won't perceive the struggles I've endured.
When the day comes, my silence will break your heart,
You'll wish to hear a single word from me.

When the day comes, I'll become your pain,
You'll wish for me to return, but in vain.
When the day comes, my eyes that spoke of love,
Will be deprived of the light of affection.
No matter how many regrets you have for me,
Love will always conquer sorrow's affliction.
I have no desire to burn my dreams,
You wash away my hopes like clay and soil.

I am leaving, perhaps just like you did once,
Now you too are growing old and weary.
I'm leaving behind everything in my past,
Leaving, crossing over the world's surface.
Maybe one day you'll hear a whisper from me,
Letting go of the memories and set me free.

I ventured into darkness on a starry night,
The sky united with the silent earth.
My unspoken words were left behind,
I escaped from this deceitful world.
Don't mourn or cry for this stranger,
False mourners are unnecessary when I'm gone.

If one day I leave you all alone,
It is my eternal liberation from those who have passed.