Under the cold, our fingers shrink like lips before the astringency
while we are biting into fresh quinces.
We push our palms into the deep openings of the coats
– everyone in their warm pocket fireplaces,
earlobes and nose tips are witnessing the sharpness of the wind,
saying; Hurry home,
so we don’t stand here,
it’s always cooler by the water!
Don’t come back to hug me,
I’ll see you another day.
Now, hurry and get up there,
it’s cold by the water!
Azemina Krehić was born on October 14, 1992 in Metković, Republic of Croatia. Winner of several international awards for poetry, including: Award of university professors in Trieste, 2019.,„Mak Dizdar“ award, 2020. Award of the Publishing Foundation of the Federation of Bosnia and Herzegovina, 2021. „Fra Martin Nedić“ Award, 2022. She is represented in several international anthologies of poetry.
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)
J.J. Campbell (1976 – ?) is trapped in suburbia, plotting his escape. He’s been widely published over the years, most recently at Horror Sleaze Trash, The Beatnik Cowboy, The Asylum Floor, Misfit Magazine and Disturb the Universe Magazine. You can find him most days on his mildly entertaining blog, evil delights. (https://evildelights.blogspot.com)
The Space Maker
1
"Moon Walker"
Never dreamed
I would find myself
here
after so many years of life
on tender Mother Earth
rubberized boots
walking
and breathing through a mini globe
marvelling at the skin of the moon
a pitted and quiet
barren buffer against a cast
of stones and new discoveries
almost soundless
but eerie
as the distant horizon
takes on a reddest hue
bringing me to a stop
red smoke creeping toward me
settling over the mouths of craters
what could be burning
and where is it coming from?
I quicken my slow plodding
and come to the edge of a gaping crater
slow smoke reddish into a dull pink
coming out of a cave on the far wall
I consider climbing down
but something whooshes out of the cave
and flies over me
I duck
looking up as it passes
a Nazi insignia on the bottom
of an old flying saucer
war seems to be everywhere
I turn and face the sphere of earth
out there in dark space
so near I feel
I could touch it
seemingly nothing ever changes
so I wake up and wonder why
there's someone's blood in my bed.
2
Spinning
Sweet earth of blue
what have we done to you
I stand on your sister moon
squinting through space
over to your sphere
my slow spinning
mother earth
turning into a lonely
immense skull
but the great change is coming
earth reborn
with God's people.
3
Soon
All the land of all the people
all the years settled and dying
so many believing
sky, sea, and sacred places
and prayers and rapture
of saints to heavenly clouds
the Word
directing
footfall and stars
The Space Maker.
An ant
In the garden so small, yet bold,
An ant navigates, steadfast and old.
Tiny feet upon the earth they roam,
Seeking crumbs and treasures to bring home.
With strength not seen by a simple glance,
They carry burdens, they advance.
A colony working as one,
Their tasks in harmony, never undone.
Their homes underground, a bustling maze,
Where life's intricate dance always plays.
In unison, they toil and strive,
Their unity makes them truly thrive.
Oh, to be like the ant, small but strong,
To persevere when the journey seems long.
A testament to diligence and might,
The ant embodies a resilient light.
Don Bormon is a student of grade 9 in Harimohan Government High School, Chapainawabganj, Bangladesh.
Welcome, readers, to mid-January’s issue of Synchronized Chaos Magazine!
We recognize various observances this month: American civil rights leader Martin Luther King’s birthday, Holocaust Memorial Day, Clean Energy Month and World Braille Day and strive to make our publication as inclusive and welcoming as possible.
We are also hosting a free public literary reading in conjunction with the Association of Writing Programs conference next month in Kansas City, MO. This will be at 6pm on the evening of February 7th at Prospero’s Books. All are welcome to come and hear the readers!
Now for this month’s issue: Holding Up Our Corners of the Sky.
Don Bormon and Mahbub both encourage us to move forward into the New Year with optimism.
Sayani Mukherjee describes cultivating herself as if she were a garden. Chimezie Ihekuna urges young Nigerian students to apply the lessons of their education to their lives, values, careers, and future leadership.
Makhfiratkhon Abduratkhmonova illustrates one young Uzbek woman’s pathway to success and recognition as a writer and intellectual. Davronova Lobar advises parents on how to raise confident children, while Saida Ismoilova speaks to having the courage to pursue our dreams.
Farkhodova Nodira extols the good exercise, glory, and discipline involved in playing sports. Dildora Toshtemirova reminds her fellow Uzbek nationals of the many vocational training opportunities in the country while Shabnam Shukhratova outlines the advantages of study-abroad programs for enriching students’ lives.
Taylor Dibbert also reflects on travel, in his piece where the speaker’s life begins to make more sense when he has a change of scene and visits Sri Lanka. Meanwhile, Daniel De Culla provides an earthier travelogue, about local customs on a trip to Morocco.
Image c/o Petr Kratochvil
Maja Milojkovic’s poem compares working artists to fish in an aquarium, constantly observed while trying to accomplish something meaningful. Graciela Noemi Villaverde touches on the more personal side of her poetic practice in a piece where she “meets” with her poetry.
Sitorakhon Buriyeva reminds us that life is short so we should make moral choices and make the most of our time.
J.K. Durick’s poetry explores our human limitations, what we can and cannot accomplish or change in life. J.J. Campbell dredges up the frailty of midlife: loneliness, physical weakness, awareness of one’s mortality. Niginabonu Amirova ponders human destiny and how we must all die, while Maftuna Sulaymonova highlights the cycle of life with a poem where a daughter cares for her aging mother.
Priscilla Bettis also looks at mortality, with gentle haikus about grief and the burial of a loved one. Mesfakus Salahin reminds us that we are all mortal and will all arrive equally empty-handed in the grave. Sabina Abdulazizova’s poetic speaker speculates on how she’d like to be remembered.
A.G. Davis’ poetry evokes death imagery alongside that of outer space and the mythical underworld. Christina Chin and Uchechukwu Onyedikam’s collaborative haikus also reference death and the underworld, alongside space aliens.
Faleeha Hassan’s lush, imaginative poem illuminates the death of creative imagination that is writers’ block. Noah Berlatsky evokes the impermanence of memory and how past relationships fade into the background.
Jerry Langdon illustrates the storm of heartbreak, when his speaker is no longer able to pull into the safe harbor of his past partner. Mavluda Rusiyeva also describes the intense pain of a broken romantic relationship. Gulsanam Abdullayeva speaks to lost love and heartbreak, while Mohichehra Rustamova quests for interpersonal and emotional peace while grieving having caused someone pain.
Maid Corbic’s poetry extols giving love, but recognizes that his love has limits because of his humanness. Cheryl Snell’s work also probes the limits of love, as she relates coldness and neglect within family relationships.
In contrast, John Culp talks of persevering in love, not shutting the door on each other, even in intense moments. Shukratova Shabnam offers a lament and a tribute to a mother’s hard work and sacrifice while Dildora Toshtemirova probes the complexities of a mother and daughter’s relationship.
Kristy Raines writes of a gentle companionship while Sayani Mukherjee evokes a moment where she meets with God, envisioning perfect communion and realization of her best self. In Charos Makhamova’s piece, spiritual and human love commingle, while Elmaya Jabbarova narrates a vivid dream of a spiritual union with a loved one from whom she draws inspiration. Abdusodiqova Fotima urges people to come to God with their pain, as He is a perfect listener.
David A. Douglas’ formal poem shows a bystander, powerless to prevent the train wreck he’s watching, but infused with courage from his faith to endure being a bystander and bear witness to the scene.
Favour Raymond also bears witness, to domestic violence and its impact on children. Daniel De Culla critiques and diminishes the power of today’s warmaking leaders by locating them within the historical context of other warlords whose empires have come and gone. Mykyta Ryzhykh describes the violence of modern warfare, yet illustrates how life as a whole perseveres and outlasts the individuals who are killed. Evie Petropoulou urges world leaders to pursue peace and justice and for all people to remember our interdependence.
Bahora Boboyeva conveys the terror of a family facing political or ethnic persecution. Jeff Rasley describes a riot where activists leave ordinary passersby to bear the brunt of repercussions for their actions.
Brian Barbeito witnesses and laments people’s increasing post-pandemic harshness and pettiness. Arthur Chertowsky describes slowly losing his ability to read or listen to books as he ages, wondering if he is slowly dying away as he ages.
Fayzullo Usmonov narrates the struggles he faced while growing up in poverty and earning a hard-won university admission. Many other contributors discuss education, including Rejabova Dildora, who outlines modern teaching methods for primary education, Mashxura Maxammatova, who suggests innovative methods for teaching English to youngsters, Fatillaeva Nehrinoz, who discusses language instruction in higher education, Shamuratova Shoira, who highlights podcasts as a tool for language learning, Malika Isomiddinova, who covers new methods for teaching vocabulary, and Alisher Ergashev, who goes into information technology tools for teaching foreign languages.
Farrukh Amirov’s poetic speaker escapes real-world injustice through retreating into the historic poetry of his nation.
Dilnoza Xusanova remembers Erkin Vakhidov, a versatile legend of Uzbekistan’s literary heritage. Bahora Boboyeva discusses Bernard Shaw’s sophisticated analysis of social class, education, and personality formation in Pygmalion. Diyora Bakhodirovna outlines psychological theories of the concept and development of personality.
In his latest set of postwoman poems, Mark Young receives deliveries of various icons of history and culture. Lorette C. Lukajic offers up 13 different ways of looking at Edward Hopper’s painting Nighthawks, about the loneliness, or peaceful solitude, of being in a quiet cafe in the evening.
Duane Vorhees writes of history, the passage of personal and mythic time. Z.I. Mahmud’s essay analyzes how T.S. Eliot and Samuel Taylor Coleridge viewed the purposes of art and literature.
Mirzaliyeva Zarinakhan outlines the history of church reformer Jan Hus, while Daniel De Culla evokes the character of an old fashioned road cleaner. Rbs Nsj gives the background of the Village of the Saint shrine which faithful Uzbeks visit on pilgrimage. Farangiz Safarova discusses Korean greetings and social etiquette.
Arts video journalist and filmmaker Federico Wardal announces his upcoming interview with Italian journalist and music promoter Adriano Aragozzini.
Some more modernist writers play with language. Jim Meirose’s onomatopoetic tale appears to concern a spear-throwing game while Daniel Y. Harris encodes Proxy Godbot the Black Hat Hacker into verse that resembles software. J.D. Nelson contributes his signature word fragments for a piecemeal glimpse of the world.
Laylo Mamatova shares the history of the Central Asian spring holiday of Navruz, while Zuhra Ruzmetova waxes effusive about the beauty of Uzbekistan in the spring. Wazed Abdullah writes of the history embedded within a long-flowing river while Muntasir Mamun Kiron rejoices in the beauty of the land and culture of his native Bangladesh, Lilian Dipasupil Kunimasa anticipates the fun of summer in an upbeat piece and takes comfort in gentle winds, and Mahbub Alam reflects on a foggy, quiet morning.
Isabel Gomez de Diego’s photography explores how people experience built environments, on small and larger scales.
Steps
The auric field
Of my own nemesis
Own your tribe
Nurture the sockets of your heart
As if a newly polished
High school ground
That transports your
Little brittle garden
Into a big pool of
Melancholic ambrosia.
My other half as if it
Gently spoke my rawness
My wet treasured hydrangeas
Into a wooden coffin of
Tumultuous laughing stock
The soft peached rainbow
Bulking around the lawn
The little trinklet of a choir
My sudden bemused allegory
It's fair enough
Leaden steps
With my own nemesis