Strong quake in Manipur, India – Also felt in Bangladesh – May 25, 2020

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A strong earthquake has hit the north-eastern parts of India on Monday evening. According to the Indian Seismology Department the quake reached magnitude (ML) 5.5. It occurred in a depth of about 27 km near the city of Imphal. The United States Geological Survey (USGS) registered magnitude (mb) 5.1 and a depth of 60 km. Moderate to strong shaking was felt across Manipur and neighbouring states. A minor intensity was perceived in parts of Bangladesh, including the capital Dhaka.
Earthquake-Report expects minor damage in areas near the epicenter, basing on our experience. This includes cracked plaster, brick-walls and fallen furniture. Severe structural damage is unlikely.

Based on the present earthquake parameters (Magnitude, Depth, Population, etc) and our experience with earthquake damage impact, earthquake-report.com does expect at least some slight damage like cracks in walls, fallen tiles, etc.

Most important Earthquake Data:

Magnitude : 5.1

Local Time (conversion only below land) : Unknown

GMT/UTC Time : 2020-05-25 14:42:18

Depth (Hypocenter) : 61 km

Depth and Magnitude updates in the list below.


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0 AND x.m0 AND x2.m 1.0) AND (date_time >= 1590364800 AND date_time Refresh this list
SRC Location UTC Date/time M D INFO
USGS Kakching, India May 25 14:42 5.1 56 MAP
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MAP
GEOFON Myanmar-india Border Region May 25 14:42 5.1 61 MAP
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MAP
  • Narayanganj, Bangladesh – My location is: 23.637366, 90.508976
    Narayanganj, Bangladesh, Asia
  • Manipur – No damages
  • Zeliangrong Village – Very weak shaking
  • Kajidahar part-iii – Very strong shaking
  • EMSC Manipur, India Region May 25 14:42 5.1 60 MAP
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    MAP

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    City/Village where you felt the earthquake *
    Street or suburb (area) where you felt the earthquake
    Latitude (area) where you felt the earthquake
    Longitude (area) where you felt the earthquake
    Time that you felt the earthquake (local time)
    Shaking Strength *
    MMI II (Very weak shaking) ?

    People :
    Felt by persons at rest, on upper floors or favorably placed.
    MMI III (Weak shaking) ?

    People :
    Felt indoors; hanging objects may swing, vibration similar to passing of light trucks, duration may be estimated, may not be recognized as an earthquake.
    MMI IV (Light shaking) ?

    People :
    Generally noticed indoors but not outside. Light sleepers may be awakened. Vibration may be likened to the passing of heavy traffic, or to the jolt of a heavy object falling or striking the building.
    Fittings :
    Doors and windows rattle. Glassware and crockery rattle. Liquids in open vessels may be slightly disturbed. Standing motorcars may rock.
    Structures :
    Walls and frames of buildings, and partitions and suspended ceilings in commercial buildings, may be heard to creak.
    MMI V (Moderate shaking) ?

    People :
    Generally felt outside, and by almost everyone indoors. Most sleepers awakened. A few people alarmed.
    Fittings :
    Small unstable objects are displaced or upset. Some glassware and crockery may be broken. Hanging pictures knock against the wall. Open doors may swing. Cupboard doors secured by magnetic catches may open. Pendulum clocks stop, start, or change rate.
    Structures :
    Some large display windows cracked. A few earthenware toilet fixtures cracked.
    MMI VI (Strong shaking) ?

    People
    Felt by all. People and animals alarmed. Many run outside. Difficulty experienced in walking steadily.
    Fittings :
    Objects fall from shelves. Pictures fall from walls. Some furniture moved on smooth floors, some unsecured free-standing fireplaces moved. Glassware and crockery broken. Very unstable furniture overturned. Small church and school bells ring. Appliances move on bench or table tops. Filing cabinets or “easy glide” drawers may open (or shut).
    Structures :
    Slight damage to buildings with low standard. Some stucco or cement plaster falls. Large display windows broken. Damage to a few weak domestic chimneys, some may fall.
    Environment :
    Trees and bushes shake, or are heard to rustle. Loose material may be dislodged from sloping ground, e.g. existing slides, talus slopes, shingle slides.
    MMI VII (Very strong shaking) ?

    People
    General alarm. Difficulty experienced in standing. Noticed by motorcar drivers who may stop.
    Fittings :
    Large bells ring. Furniture moves on smooth floors, may move on carpeted floors. Substantial damage to fragile contents of buildings.
    Structures :
    Unreinforced stone and brick walls cracked. Low standard buildings cracked with some minor masonry falls. A few instances of damage to buildings of ordinary workmanship. Unbraced parapets, unbraced brick gables, and architectural ornaments fall. Roofing tiles, especially ridge tiles may be dislodged. Many unreinforced domestic chimneys damaged, often falling from roof-line. Water tanks Type I burst. A few instances of damage to brick veneers and plaster or cement-based linings. Unrestrained water cylinders (hot-water cylinders) may move and leak. Some common windows cracked. Suspended ceilings damaged.
    Environment :
    Water made turbid by stirred up mud. Small slides such as falls of sand and gravel banks, and small rock-falls from steep slopes and cuttings. Instances of settlement of unconsolidated or wet, or weak soils. Some fine cracks appear in sloping ground. A few instances of liquefaction (i.e. small water and sand ejections).
    MMI VIII (Severe shaking) ?

    People
    Alarm may approach panic. Steering of motorcars greatly affected.

    Structures :
    Low standard buildings heavily damaged, some collapse. ordinary workmanship buildings damaged, some with partial collapse. Reinforced masonry or concrete buildings damaged in some cases. A few instances of damage to buildings and bridges designed and built to resist earthquakes. Monuments and pre-1976 elevated tanks and factory stacks twisted or brought down. Some pre-1965 infill masonry panels damaged. A few post-1980 brick veneers damaged. Decayed timber piles of houses damaged. Houses not secured to foundations may move. Most unreinforced domestic chimneys damaged, some below roof-line, many brought down.

    Environment :
    Cracks appear on steep slopes and in wet ground. Small to moderate slides in roadside cuttings and unsupported excavations. Small water and sand ejections and localized lateral spreading adjacent to streams, canals, lakes, etc.

    MMI IX (Violent shaking) ?

    Structures
    Many low standard buildings destroyed. Ordinary workmanship buildings heavily damaged, some collapse. Reinforced masonry or concrete buildings damaged, some with partial collapse. Buildings and bridges designed and built to resist earthquakes damaged in some cases, some with flexible frames seriously damaged. Damage or permanent distortion to some buildings and bridges, designed and built to normal use standards. Houses not secured to foundations shifted off. Brick veneers fall and expose frames.

    Environment :
    Cracking of ground conspicuous. Landsliding general on steep slopes. Liquefaction effects intensified and more widespread, with large lateral spreading and flow sliding adjacent to streams, canals, lakes, etc.

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    Strong earthquake – Cook Strait, New Zealand – May 24, 2020

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    Have you felt the shaking? If Yes, tell us by using the I FELT IT form behind the earthquake or at the bottom of this page.

    This earthquake has been felt strongly in the lower North Island (Wellington, Wairarapa & Manawatu-Wanganui Regions) and the upper South Island (Marlborough, Nelson & Tasman Regions). Highest reported intensities are MM6 (minor damage possible to contents like crockery and glassware).

    Currently there are no reports of damage, but reports on RNZ of objects falling from shelves in Foxton near the epicentre of the quake (books thrown from bookshelves).

    This quake is associated with the subduction of the Pacific Plate beneath the North Island. Based on depth (37km according to GeoNet), it may be the result of thrust faulting in the overlying Australian Plate. Earthquakes of this size and depth in this area are not very common – the last such comparable quake struck in September 1991 (M5.6, 87km depth).

    Edit (20:26 UTC, 08:26 NZST): Currently there have been 9 located aftershocks, with magnitudes 1.5-3.7. Aftershocks may reach M4.8-5.0, but due to the depth of the earthquake a M4.2-4.8 is more realistic for the largest aftershock. There is always the possibility a larger aftershock may occur, but this is very low, especially given the depth of this earthquake. John Ristau (Seismologist, GNS Science) has said on RNZ that there is no tsunami threat due to the relatively low magnitude & the depth of the earthquake. The aftershock sequence should not be too energetic due to the depth of this earthquake.

     

    Edit (20:38 UTC, 08:38 NZST): A moment tensor solution has been published by GeoNet – New Zealand’s geological hazards agency. This states that the earthquake was moment magnitude 5.6, with a focal depth of 44km, and was the result of oblique normal faulting. This confirms that the earthquake was associated with the subduction of the Pacific Plate beneath the North Island of New Zealand.

     

    Edit (20:51 UTC, 08:51 NZST): A local magnitude 3.9 aftershock struck at 08:47 NZST – this is the largest aftershock so far. Determining which GeoNet felt reports are for this aftershock or for the mainshock is still not possible yet, but I suspect this quake was probably only felt locally (Levin, Foxton, Foxton Beach).

    Most important Earthquake Data:

    Magnitude : 5.5

    Local Time (conversion only below land) : Unknown

    GMT/UTC Time : 2020-05-24 19:53:32

    Depth (Hypocenter) : 47 km

    Depth and Magnitude updates in the list below.


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    USGS Foxton, New Zealand May 24 22:44 4.2 35 MAP
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    City/Village where you felt the earthquake *
    Street or suburb (area) where you felt the earthquake
    Latitude (area) where you felt the earthquake
    Longitude (area) where you felt the earthquake
    Time that you felt the earthquake (local time)
    Shaking Strength *
    MMI II (Very weak shaking) ?

    People :
    Felt by persons at rest, on upper floors or favorably placed.
    MMI III (Weak shaking) ?

    People :
    Felt indoors; hanging objects may swing, vibration similar to passing of light trucks, duration may be estimated, may not be recognized as an earthquake.
    MMI IV (Light shaking) ?

    People :
    Generally noticed indoors but not outside. Light sleepers may be awakened. Vibration may be likened to the passing of heavy traffic, or to the jolt of a heavy object falling or striking the building.
    Fittings :
    Doors and windows rattle. Glassware and crockery rattle. Liquids in open vessels may be slightly disturbed. Standing motorcars may rock.
    Structures :
    Walls and frames of buildings, and partitions and suspended ceilings in commercial buildings, may be heard to creak.
    MMI V (Moderate shaking) ?

    People :
    Generally felt outside, and by almost everyone indoors. Most sleepers awakened. A few people alarmed.
    Fittings :
    Small unstable objects are displaced or upset. Some glassware and crockery may be broken. Hanging pictures knock against the wall. Open doors may swing. Cupboard doors secured by magnetic catches may open. Pendulum clocks stop, start, or change rate.
    Structures :
    Some large display windows cracked. A few earthenware toilet fixtures cracked.
    MMI VI (Strong shaking) ?

    People
    Felt by all. People and animals alarmed. Many run outside. Difficulty experienced in walking steadily.
    Fittings :
    Objects fall from shelves. Pictures fall from walls. Some furniture moved on smooth floors, some unsecured free-standing fireplaces moved. Glassware and crockery broken. Very unstable furniture overturned. Small church and school bells ring. Appliances move on bench or table tops. Filing cabinets or “easy glide” drawers may open (or shut).
    Structures :
    Slight damage to buildings with low standard. Some stucco or cement plaster falls. Large display windows broken. Damage to a few weak domestic chimneys, some may fall.
    Environment :
    Trees and bushes shake, or are heard to rustle. Loose material may be dislodged from sloping ground, e.g. existing slides, talus slopes, shingle slides.
    MMI VII (Very strong shaking) ?

    People
    General alarm. Difficulty experienced in standing. Noticed by motorcar drivers who may stop.
    Fittings :
    Large bells ring. Furniture moves on smooth floors, may move on carpeted floors. Substantial damage to fragile contents of buildings.
    Structures :
    Unreinforced stone and brick walls cracked. Low standard buildings cracked with some minor masonry falls. A few instances of damage to buildings of ordinary workmanship. Unbraced parapets, unbraced brick gables, and architectural ornaments fall. Roofing tiles, especially ridge tiles may be dislodged. Many unreinforced domestic chimneys damaged, often falling from roof-line. Water tanks Type I burst. A few instances of damage to brick veneers and plaster or cement-based linings. Unrestrained water cylinders (hot-water cylinders) may move and leak. Some common windows cracked. Suspended ceilings damaged.
    Environment :
    Water made turbid by stirred up mud. Small slides such as falls of sand and gravel banks, and small rock-falls from steep slopes and cuttings. Instances of settlement of unconsolidated or wet, or weak soils. Some fine cracks appear in sloping ground. A few instances of liquefaction (i.e. small water and sand ejections).
    MMI VIII (Severe shaking) ?

    People
    Alarm may approach panic. Steering of motorcars greatly affected.

    Structures :
    Low standard buildings heavily damaged, some collapse. ordinary workmanship buildings damaged, some with partial collapse. Reinforced masonry or concrete buildings damaged in some cases. A few instances of damage to buildings and bridges designed and built to resist earthquakes. Monuments and pre-1976 elevated tanks and factory stacks twisted or brought down. Some pre-1965 infill masonry panels damaged. A few post-1980 brick veneers damaged. Decayed timber piles of houses damaged. Houses not secured to foundations may move. Most unreinforced domestic chimneys damaged, some below roof-line, many brought down.

    Environment :
    Cracks appear on steep slopes and in wet ground. Small to moderate slides in roadside cuttings and unsupported excavations. Small water and sand ejections and localized lateral spreading adjacent to streams, canals, lakes, etc.

    MMI IX (Violent shaking) ?

    Structures
    Many low standard buildings destroyed. Ordinary workmanship buildings heavily damaged, some collapse. Reinforced masonry or concrete buildings damaged, some with partial collapse. Buildings and bridges designed and built to resist earthquakes damaged in some cases, some with flexible frames seriously damaged. Damage or permanent distortion to some buildings and bridges, designed and built to normal use standards. Houses not secured to foundations shifted off. Brick veneers fall and expose frames.

    Environment :
    Cracking of ground conspicuous. Landsliding general on steep slopes. Liquefaction effects intensified and more widespread, with large lateral spreading and flow sliding adjacent to streams, canals, lakes, etc.

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    source

    How coronavirus stress may scramble our brains

    0

    I’m on deadline, but
    instead of focusing, my mind buzzes with unrelated tidbits. My first-grader’s
    tablet needs an update before her online school session tomorrow. Heartbreaking
    deaths from COVID-19 in New York City make me tear up again. Was that a kid’s
    scream from upstairs? Do I need to run up there, or will my husband take care
    of it?

    These
    hornets of thoughts drive out the clear thinking my job demands. Try as I might
    to conjure up a coherent story, the relevant wisps float away.

    I’m
    scattered, worried and tired. And even though we’re all socially isolated, I’m
    not alone. The pandemic — and its social and economic upheavals — has left
    people around the world feeling like they can’t string two thoughts together.
    Stress has really done a number on us.

    That’s
    no surprise to scientists who study stress. Our brains are not built to do
    complex thinking, planning and remembering in times of massive upheaval. Feeling
    impaired is “a natural biological response,” says Amy Arnsten, a neuroscientist
    at Yale School of Medicine. “This is how our brains are wired.”

    Decades
    of research have chronicled the ways stress can disrupt business as usual in
    our brains. Recent studies have made even more clear how stress saps our
    ability to plan ahead and have pointed to one way that stress changes how
    certain brain cells operate.

    Scientists recognize the pandemic as an opportunity for a massive, real-time experiment on stress. COVID-19 foisted on us a heavy mix of health, economic and social stressors. And the end date is nowhere in sight. Scientists have begun collecting data to answer a range of questions. But one thing is clear: This  pandemic has thrown all of us into uncharted territory.

    Short-circuited

    The human brain’s
    astonishing abilities rely on a web of nerve cell connections. One hub of
    activity is the prefrontal cortex, which is important for some of our fanciest
    forms of thinking. These “executive functions” include abstract thinking,
    planning, focusing, juggling multiple bits of information and even practicing
    patience. Stress can muffle that hub’s signals, studies of lab animals and
    humans have shown.

    “Even
    relatively mild stress can impair the prefrontal cortex,” says Elizabeth
    Phelps, a psychologist and neuroscientist at Harvard University. “That’s one of
    the most robust effects of stress on the brain.”

    That impairment has been described in lots of studies. One memorable example comes from 20 panicky medical students facing licensing exams. After a month of high-stress test prep, the students performed worse on an attention test than they did after exams were over. Functional MRI scans showed that under stress, the students’ prefrontal connections to other brain areas were diminished, scientists reported in Proceedings of the National Academy of Sciences in 2009.

    experiment diagram of brains
    Normally, an alert person’s brain has moderate amounts of chemical messengers that lead the prefrontal cortex to take charge and perform high-level thinking (left). But with stress, those chemical signals can flood the brain, activating amygdala-linked brain networks involved in sensing and responding to threats (right).A. Arnsten
    experiment diagram of brains
    Normally, an alert person’s brain has moderate amounts of chemical messengers that lead the prefrontal cortex to take charge and perform high-level thinking (left). But with stress, those chemical signals can flood the brain, activating amygdala-linked brain networks involved in sensing and responding to threats (right).A. Arnsten

    When
    the prefrontal cortex goes quiet, more reactionary brain networks take over.
    Some of these “primitive” circuits, as Arnsten calls them, center on the
    amygdalae, two almond-shaped structures buried deep inside the brain that help
    us sense and respond to threats. Those fast, instinctual reactions “are helpful
    if you’re being faced with a snake,” Arnsten says, “but not helpful if you’re
    being faced with a complex medical decision.”

    A more recent experiment, published online April 2 in Current Biology, illustrates how stress can shift people away from thoughtful planning. When people were threatened with electric shocks, their abilities to plan ahead flew out the window. Anthony Wagner, a cognitive neuroscientist at Stanford University, and colleagues asked 38 people to learn a familiar route through virtual towns. With practice, people learned these routes, as well as the locations of recognizable objects, such as a zebra, an apple, a stapler or Taylor Swift’s face, along the way.

    “Our
    question was, ‘What are the effects of stress?’ ” Wagner says. To find out, the
    researchers used “moderately painful” electric zaps to induce stress in some
    participants, who returned to familiar virtual towns and were asked to find
    their way to the zebra, for instance. Subjects didn’t know when they would be
    shocked, and they couldn’t control any aspect of it.

    After
    the training, the participants — some under stress from the expectation of
    further shocks and some not — were sent back into the virtual town and asked to
    find their way to a specific item.

    But
    there was a trick: Participants could reach the stapler, for example, faster
    and more efficiently by taking a shortcut. The shortcut, however, required more
    planning, more initiative and a heavier reliance on previously learned
    relationships among streets.

    Stressed
    people were less inclined to take the shortcut, the researchers found. People
    who were stressed by the possibility of a shock took the shortcut 31 percent of
    the time, compared with 47 percent for those who weren’t stressed. The stressed
    people still reached the object they were after, but in a roundabout way.

    Functional
    MRI brain scans hinted at what the added stress did to the volunteers’
    thinking. The objects planted around town evoked recognizable patterns of brain
    activity when a person was seeing one of the previously seen objects, or even
    just thinking about it. By spotting these neural signposts, researchers could
    tell when people were thinking of a particular path — or of no path at all.

    Participants
    were given eight seconds to plan their approach to reach the target object.
    Unstressed people generally had a plan; their brain activity contained patterns
    that signaled these volunteers were thinking about the objects along the
    shortcut route. Neural signals of a plan even showed up among those who chose
    to take the familiar route.

    Those
    awaiting a shock appeared to use little foresight. “The stressed people didn’t
    seem to be thinking about the familiar route when they took it,” says study
    coauthor Thackery Brown, a cognitive neuroscientist at Georgia Tech in Atlanta.
    “They were on this fight-or-flight autopilot type behavior.”

    What’s
    more, stress quieted the activity of brain areas needed to make a good plan,
    including a part of the prefrontal cortex and the hippocampus, a structure
    important for memory. Those findings suggest that under stress, we are less
    able to call up our previously learned knowledge and memories. We are working
    with a deficit.

    “In
    some sense, we’re privileged when we’re not stressed, able to fully harness our
    cognitive machinery,” Wagner says. “That allows us to behave in more strategic,
    more efficient, more goal-directed ways.”

    Brown
    sees parallels between these lab-based stressors and the complex and
    longer-lasting stresses of real life. The participants were attempting to do
    something complicated while worrying about something else. The stressor is
    “operating in the background while you’re trying to plan your daily life,”
    Brown says. “There’s a connection there with the type of thing people are
    experiencing right now in the context of the pandemic.”

    Shrunken cells

    Zooming in to individual
    cells provides a view of stress’s physical destruction in the brain. Stress can
    shrink nerve cells and cull their connections, and the prefrontal cortex is
    particularly vulnerable, studies in both humans and other animals suggest.
    Other kinds of brain cells are affected too, new research on mice shows.

    Big, arboreal cells called astrocytes have many jobs in the brain. Specialized astrocytes called Bergmann glia extend into synapses, the space between nerve cells where chemical messages flow, and slurp up extra chemical signals. This helps keep nerve cells communicating clearly with one another (SN Online: 8/4/15).

    But in a test of mice stressed by the ominous smell of a predatory fox, these astrocytes retracted from synapses, neuroscientist Siqiong June Liu of Louisiana State University School of Medicine in New Orleans and colleagues found. That pulling away occurred with a single exposure to that stressful fox odor, and the cells were still retracted 24 hours later, the researchers reported in the April 22 Journal of Neuroscience.

    Stress
    sends a “shrink” message to these astrocytes by reducing the levels of a
    protein called GluA1. It’s not known whether a similar process, and the
    resulting changes in how brain cells communicate under stress, happens in the
    brains of people.

    Some stress signals may travel certain neural highways. Physiologist Kazuhiro Nakamura of Nagoya University Graduate School of Medicine in Japan and colleagues studied rats that had just been through the stressful experience of losing a fight, a defeat that is meant to mimic human social stress. A somewhat mysterious region inside the rat’s prefrontal cortex, called the DPC/DTT for dorsal peduncular cortex and dorsal tenia tecta, is important for sending stressed-out signals, the researchers reported in the March 6 Science.

    From
    there, the signals shoot to the hypothalamus, a brain structure that can spark
    some of stress’s most obvious effects in the body, including a racing heart and
    sweating. It’s possible that similar brain areas in humans might have roles in
    sparking stress signals.

    These
    clues are giving scientists a more precise understanding of how stress moves
    through and affects the brain. But lab studies on stress, by design, have to be
    somewhat short-lived, with relatively mild stress. Applying lab findings to
    people’s experiences in life comes with caveats. Huge questions remain about
    how the crushing and varied stresses of a pandemic might influence people.

    A natural experiment

    Psychologists and brain scientists are on it. As of mid-May, a database tracking COVID-19 social science projects had 294 research projects related to the current pandemic.

    These kinds of natural experiments — studying people who had experienced uncontrollable, intense stress in their lives — have happened before. Phelps and colleagues studied how people remember the events of 9/11. People who were in downtown Manhattan at the time of the attacks seemed to rely more heavily on their amygdalae to call up memories of the shocking event than people who were farther away, the researchers reported in 2007 in Proceedings of the National Academy of Sciences. Other researchers have identified thinking problems in people who lived through Hurricane Katrina and other natural disasters.

    Stress
    from the COVID-19 pandemic might influence decision making, Phelps suspects.
    How do you respond to positive and negative feedback when you’re stressed? Does
    your desire to do hard work change? She and colleagues are hoping to get
    answers by surveying people across the United States. Participants will
    describe their stress reactions and complete online tasks that test decision
    making and memory.

    Other
    long-term studies will examine how autobiographical memories of the pandemic
    change over time, how the pandemic affects stress during pregnancy and how
    mind-set might influence how people cope.

    As
    this chaotic period rolls on, stressors will change and accumulate. Sustained
    crisis, scientists suspect, can change our brains and their capabilities in
    even more profound ways than temporary stress. 

    For
    now, each of us is left to manage our own personalized stress cocktails. Mine
    grows more potent with an expanding backlog of tasks, both domestic and
    job-related, the cumulative sorrow of seeing my kids isolated from their
    friends and a steady drip of small losses. And I worry for the many people who
    are worse off, facing illness and financial strain. It’s a lot.

    As we all grapple with this reality, scientists have a message for us, one that I find comforting: “Forgive yourself,” Phelps says. “If you’re finding it challenging right now to focus, forgive yourself.”

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    Sismo Moderado en Colombia – 24 de Mayo de 2020

    0

    ¿Has sentido el sismo? En caso de que lo hayas percibido, comparte tu reporte usando el formulario I FELT IT al final de esta página.

    Un sismo de M4.0 se registró esta mañana cerca de la ciudad de Cali, en Colombia. El sismo se logró percibir de forma leve a moderada en la región debido a su poca profundidad y cercanía a la ciudad.

    Al momento no se reportan afectaciones mayores, pero la probabilidad es baja.

    Datos más importantes del sismo:

    Magnitud : 4

    Hora local (conversion only below land) : Unknown

    Hora GMT/UTC : 2020-05-24 12:22:00

    Profundidad (Hipocentro) : 10 km

    Profundidad y magnitudes se encuentran en la lista de abajo.


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    I felt the shaking *
    Country where you felt the earthquake * Afghanistanaland IslandsAlbaniaAlgeriaAmerican SamoaAndorraAngolaAnguillaAntarcticaAntigua and BarbudaArgentinaArmeniaArubaAustraliaAustriaAzerbaijanBahamasBahrainBangladeshBarbadosBelarusBelgiumBelizeBeninBermudaBhutanBoliviaBosnia and HerzegovinaBotswanaBouvet IslandBrazilBritish Antarctic TerritoryBritish Indian Ocean TerritoryBritish Virgin IslandsBruneiBulgariaBurkina FasoBurundiCambodiaCameroonCanadaCanton and Enderbury IslandsCape VerdeCayman IslandsCentral African RepublicChadChileChinaChristmas IslandCocos [Keeling] IslandsColombiaComorosCongo – BrazzavilleCongo – KinshasaCook IslandsCosta RicaC?te d?IvoireCroatiaCubaCyprusCzech RepublicDenmarkDjiboutiDominicaDominican RepublicDronning Maud LandEcuadorEgyptEl SalvadorEquatorial GuineaEritreaEstoniaEthiopiaFalkland IslandsFaroe IslandsFijiFinlandFranceFrench GuianaFrench PolynesiaFrench Southern and Antarctic TerritoriesFrench Southern TerritoriesGabonGambiaGeorgiaGermanyGhanaGibraltarGreeceGreenlandGrenadaGuadeloupeGuamGuatemalaGuernseyGuineaGuinea-BissauGuyanaHaitiHeard Island and McDonald IslandsHondurasHong Kong SAR ChinaHungaryIcelandIndiaIndonesiaIranIraqIrelandIsle of ManIsraelItalyJamaicaJapanJerseyJohnston IslandJordanKazakhstanKenyaKiribatiKuwaitKyrgyzstanLaosLatviaLebanonLesothoLiberiaLibyaLiechtensteinLithuaniaLuxembourgMacau SAR ChinaMacedoniaMadagascarMalawiMalaysiaMaldivesMaliMaltaMarshall IslandsMartiniqueMauritaniaMauritiusMayotteMetropolitan FranceMexicoMicronesiaMidway IslandsMoldovaMonacoMongoliaMontenegroMontserratMoroccoMozambiqueMyanmar [Burma]NamibiaNauruNepalNetherlandsNetherlands AntillesNeutral ZoneNew CaledoniaNew ZealandNicaraguaNigerNigeriaNiueNorfolk IslandNorth KoreaNorthern Mariana IslandsNorwayOmanPacific Islands Trust TerritoryPakistanPalauPalestinian TerritoriesPanamaPanama Canal ZonePapua New GuineaParaguayPeople’s Democratic Republic of YemenPeruPhilippinesPitcairn IslandsPolandPortugalPuerto RicoQatarR?unionRomaniaRussiaRwandaSaint Barth?lemySaint HelenaSaint Kitts and NevisSaint LuciaSaint MartinSaint Pierre and MiquelonSaint Vincent and the GrenadinesSamoaSan MarinoS?o Tom? and Pr?ncipeSaudi ArabiaSenegalSerbiaSerbia and MontenegroSeychellesSierra LeoneSingaporeSlovakiaSloveniaSolomon IslandsSomaliaSouth AfricaSouth Georgia and the South Sandwich IslandsSouth KoreaSpainSri LankaSudanSurinameSvalbard and Jan MayenSwazilandSwedenSwitzerlandSyriaTaiwanTajikistanTanzaniaThailandTimor-LesteTogoTokelauTongaTrinidad and TobagoTunisiaTurkeyTurkmenistanTurks and Caicos IslandsTuvaluU.S. Minor Outlying IslandsU.S. Miscellaneous Pacific IslandsU.S. Virgin IslandsUgandaUkraineUnion of Soviet Socialist RepublicsUnited Arab EmiratesUnited KingdomUnited StatesUnknown or Invalid RegionUruguayUzbekistanVanuatuVatican CityVenezuelaVietnamVietnamWake IslandWallis and FutunaWestern SaharaYemenZambiaZimbabwe
    City/Village where you felt the earthquake *
    Street or suburb (area) where you felt the earthquake
    Latitude (area) where you felt the earthquake
    Longitude (area) where you felt the earthquake
    Time that you felt the earthquake (local time)
    Shaking Strength *
    MMI II (Very weak shaking) ?

    People :
    Felt by persons at rest, on upper floors or favorably placed.
    MMI III (Weak shaking) ?

    People :
    Felt indoors; hanging objects may swing, vibration similar to passing of light trucks, duration may be estimated, may not be recognized as an earthquake.
    MMI IV (Light shaking) ?

    People :
    Generally noticed indoors but not outside. Light sleepers may be awakened. Vibration may be likened to the passing of heavy traffic, or to the jolt of a heavy object falling or striking the building.
    Fittings :
    Doors and windows rattle. Glassware and crockery rattle. Liquids in open vessels may be slightly disturbed. Standing motorcars may rock.
    Structures :
    Walls and frames of buildings, and partitions and suspended ceilings in commercial buildings, may be heard to creak.
    MMI V (Moderate shaking) ?

    People :
    Generally felt outside, and by almost everyone indoors. Most sleepers awakened. A few people alarmed.
    Fittings :
    Small unstable objects are displaced or upset. Some glassware and crockery may be broken. Hanging pictures knock against the wall. Open doors may swing. Cupboard doors secured by magnetic catches may open. Pendulum clocks stop, start, or change rate.
    Structures :
    Some large display windows cracked. A few earthenware toilet fixtures cracked.
    MMI VI (Strong shaking) ?

    People
    Felt by all. People and animals alarmed. Many run outside. Difficulty experienced in walking steadily.
    Fittings :
    Objects fall from shelves. Pictures fall from walls. Some furniture moved on smooth floors, some unsecured free-standing fireplaces moved. Glassware and crockery broken. Very unstable furniture overturned. Small church and school bells ring. Appliances move on bench or table tops. Filing cabinets or “easy glide” drawers may open (or shut).
    Structures :
    Slight damage to buildings with low standard. Some stucco or cement plaster falls. Large display windows broken. Damage to a few weak domestic chimneys, some may fall.
    Environment :
    Trees and bushes shake, or are heard to rustle. Loose material may be dislodged from sloping ground, e.g. existing slides, talus slopes, shingle slides.
    MMI VII (Very strong shaking) ?

    People
    General alarm. Difficulty experienced in standing. Noticed by motorcar drivers who may stop.
    Fittings :
    Large bells ring. Furniture moves on smooth floors, may move on carpeted floors. Substantial damage to fragile contents of buildings.
    Structures :
    Unreinforced stone and brick walls cracked. Low standard buildings cracked with some minor masonry falls. A few instances of damage to buildings of ordinary workmanship. Unbraced parapets, unbraced brick gables, and architectural ornaments fall. Roofing tiles, especially ridge tiles may be dislodged. Many unreinforced domestic chimneys damaged, often falling from roof-line. Water tanks Type I burst. A few instances of damage to brick veneers and plaster or cement-based linings. Unrestrained water cylinders (hot-water cylinders) may move and leak. Some common windows cracked. Suspended ceilings damaged.
    Environment :
    Water made turbid by stirred up mud. Small slides such as falls of sand and gravel banks, and small rock-falls from steep slopes and cuttings. Instances of settlement of unconsolidated or wet, or weak soils. Some fine cracks appear in sloping ground. A few instances of liquefaction (i.e. small water and sand ejections).
    MMI VIII (Severe shaking) ?

    People
    Alarm may approach panic. Steering of motorcars greatly affected.

    Structures :
    Low standard buildings heavily damaged, some collapse. ordinary workmanship buildings damaged, some with partial collapse. Reinforced masonry or concrete buildings damaged in some cases. A few instances of damage to buildings and bridges designed and built to resist earthquakes. Monuments and pre-1976 elevated tanks and factory stacks twisted or brought down. Some pre-1965 infill masonry panels damaged. A few post-1980 brick veneers damaged. Decayed timber piles of houses damaged. Houses not secured to foundations may move. Most unreinforced domestic chimneys damaged, some below roof-line, many brought down.

    Environment :
    Cracks appear on steep slopes and in wet ground. Small to moderate slides in roadside cuttings and unsupported excavations. Small water and sand ejections and localized lateral spreading adjacent to streams, canals, lakes, etc.

    MMI IX (Violent shaking) ?

    Structures
    Many low standard buildings destroyed. Ordinary workmanship buildings heavily damaged, some collapse. Reinforced masonry or concrete buildings damaged, some with partial collapse. Buildings and bridges designed and built to resist earthquakes damaged in some cases, some with flexible frames seriously damaged. Damage or permanent distortion to some buildings and bridges, designed and built to normal use standards. Houses not secured to foundations shifted off. Brick veneers fall and expose frames.

    Environment :
    Cracking of ground conspicuous. Landsliding general on steep slopes. Liquefaction effects intensified and more widespread, with large lateral spreading and flow sliding adjacent to streams, canals, lakes, etc.

    Tell us your experience and how many seconds the shaking lasted + let us know if your property has been damaged (even slight damage). (max. 500 characters)

    * mandatory fields <!–

     

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    Dangerous earthquake near Dogonbadan, Iran, felt in Kuwait – May 24, 2020

    0

    Have you felt the shaking? If Yes, tell us by using the I FELT IT form behind the earthquake or at the bottom of this page.

    Update 17:19 UTC: Director General of Cultural Heritage and Handicrafts Department od Kohgiluyeh and Boyer-Ahmad said that A 5.2 magnitude earthquake this afternoon in Kohgiluyeh and Boyer-Ahmad province caused serious damage to the historical texture of Dehdasht, the center of Kohgiluyeh city.

    Update 17:15 UTC: The number of those injured in an earthquake in southwestern Iran has increased to 16, the country’s emergency medical service said on Sunday. “One person has been treated on the spot, other 15 have been sent to medical centres,” the medical service said in a statement, adding that everyone has received medical aid and all patients have already been discharged. All patients are said to have gotten injured while trying to flee the earthquake.

    Update : A moderate earthquake with Magnitude 5.2 hit the south-western regions of Iran on Sunday. The epicenter is located only a few kilometer west of the city Dogonbadan, according to Iranian Seismological Center. We expect moderate damage from this quake due to its shallow depth, the high population density near the epicenter and the caltulated intensity.
    Minor shaking was felt in Kuwait.


    Based on the present earthquake parameters (Magnitude, Depth, Population, etc) and our experience with earthquake damage impact, earthquake-report.com does expect at least some slight damage like cracks in walls, fallen tiles, etc.

    Most important Earthquake Data:

    Magnitude : 5

    Local Time (conversion only below land) : Unknown

    GMT/UTC Time : 2020-05-24 09:11:29

    Depth (Hypocenter) : 10 km

    Depth and Magnitude updates in the list below.


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    Share your earthquake experience (I Have Felt It) with our readers.
    Click on the “I Felt It” button behind the corresponding earthquake. Your earthquake experience is not only important for science, but also for people in the area as well as our global readership.

    var i_addcc6fee98cbbc0f3b4efc527a7c5fd=0;

    –>

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    I Felt It

    INFO

    0 AND x.m0 AND x2.m 1.0) AND (date_time >= 1590278400 AND date_time Refresh this list
    SRC Location UTC Date/time M D INFO
    EMSC Southern Iran May 24 09:11 5.0 15 MAP
    <!–

    MAP
    USGS Do Gonbadan, Iran May 24 09:11 5.1 10 MAP
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    GEOFON Northern And Central Iran May 24 09:11 5.0 10 MAP
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    SHARE YOUR EARTHQUAKE EXPERIENCE WITH US
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    I felt the shaking *
    Country where you felt the earthquake * Afghanistanaland IslandsAlbaniaAlgeriaAmerican SamoaAndorraAngolaAnguillaAntarcticaAntigua and BarbudaArgentinaArmeniaArubaAustraliaAustriaAzerbaijanBahamasBahrainBangladeshBarbadosBelarusBelgiumBelizeBeninBermudaBhutanBoliviaBosnia and HerzegovinaBotswanaBouvet IslandBrazilBritish Antarctic TerritoryBritish Indian Ocean TerritoryBritish Virgin IslandsBruneiBulgariaBurkina FasoBurundiCambodiaCameroonCanadaCanton and Enderbury IslandsCape VerdeCayman IslandsCentral African RepublicChadChileChinaChristmas IslandCocos [Keeling] IslandsColombiaComorosCongo – BrazzavilleCongo – KinshasaCook IslandsCosta RicaC?te d?IvoireCroatiaCubaCyprusCzech RepublicDenmarkDjiboutiDominicaDominican RepublicDronning Maud LandEcuadorEgyptEl SalvadorEquatorial GuineaEritreaEstoniaEthiopiaFalkland IslandsFaroe IslandsFijiFinlandFranceFrench GuianaFrench PolynesiaFrench Southern and Antarctic TerritoriesFrench Southern TerritoriesGabonGambiaGeorgiaGermanyGhanaGibraltarGreeceGreenlandGrenadaGuadeloupeGuamGuatemalaGuernseyGuineaGuinea-BissauGuyanaHaitiHeard Island and McDonald IslandsHondurasHong Kong SAR ChinaHungaryIcelandIndiaIndonesiaIranIraqIrelandIsle of ManIsraelItalyJamaicaJapanJerseyJohnston IslandJordanKazakhstanKenyaKiribatiKuwaitKyrgyzstanLaosLatviaLebanonLesothoLiberiaLibyaLiechtensteinLithuaniaLuxembourgMacau SAR ChinaMacedoniaMadagascarMalawiMalaysiaMaldivesMaliMaltaMarshall IslandsMartiniqueMauritaniaMauritiusMayotteMetropolitan FranceMexicoMicronesiaMidway IslandsMoldovaMonacoMongoliaMontenegroMontserratMoroccoMozambiqueMyanmar [Burma]NamibiaNauruNepalNetherlandsNetherlands AntillesNeutral ZoneNew CaledoniaNew ZealandNicaraguaNigerNigeriaNiueNorfolk IslandNorth KoreaNorthern Mariana IslandsNorwayOmanPacific Islands Trust TerritoryPakistanPalauPalestinian TerritoriesPanamaPanama Canal ZonePapua New GuineaParaguayPeople’s Democratic Republic of YemenPeruPhilippinesPitcairn IslandsPolandPortugalPuerto RicoQatarR?unionRomaniaRussiaRwandaSaint Barth?lemySaint HelenaSaint Kitts and NevisSaint LuciaSaint MartinSaint Pierre and MiquelonSaint Vincent and the GrenadinesSamoaSan MarinoS?o Tom? and Pr?ncipeSaudi ArabiaSenegalSerbiaSerbia and MontenegroSeychellesSierra LeoneSingaporeSlovakiaSloveniaSolomon IslandsSomaliaSouth AfricaSouth Georgia and the South Sandwich IslandsSouth KoreaSpainSri LankaSudanSurinameSvalbard and Jan MayenSwazilandSwedenSwitzerlandSyriaTaiwanTajikistanTanzaniaThailandTimor-LesteTogoTokelauTongaTrinidad and TobagoTunisiaTurkeyTurkmenistanTurks and Caicos IslandsTuvaluU.S. Minor Outlying IslandsU.S. Miscellaneous Pacific IslandsU.S. Virgin IslandsUgandaUkraineUnion of Soviet Socialist RepublicsUnited Arab EmiratesUnited KingdomUnited StatesUnknown or Invalid RegionUruguayUzbekistanVanuatuVatican CityVenezuelaVietnamVietnamWake IslandWallis and FutunaWestern SaharaYemenZambiaZimbabwe
    City/Village where you felt the earthquake *
    Street or suburb (area) where you felt the earthquake
    Latitude (area) where you felt the earthquake
    Longitude (area) where you felt the earthquake
    Time that you felt the earthquake (local time)
    Shaking Strength *
    MMI II (Very weak shaking) ?

    People :
    Felt by persons at rest, on upper floors or favorably placed.
    MMI III (Weak shaking) ?

    People :
    Felt indoors; hanging objects may swing, vibration similar to passing of light trucks, duration may be estimated, may not be recognized as an earthquake.
    MMI IV (Light shaking) ?

    People :
    Generally noticed indoors but not outside. Light sleepers may be awakened. Vibration may be likened to the passing of heavy traffic, or to the jolt of a heavy object falling or striking the building.
    Fittings :
    Doors and windows rattle. Glassware and crockery rattle. Liquids in open vessels may be slightly disturbed. Standing motorcars may rock.
    Structures :
    Walls and frames of buildings, and partitions and suspended ceilings in commercial buildings, may be heard to creak.
    MMI V (Moderate shaking) ?

    People :
    Generally felt outside, and by almost everyone indoors. Most sleepers awakened. A few people alarmed.
    Fittings :
    Small unstable objects are displaced or upset. Some glassware and crockery may be broken. Hanging pictures knock against the wall. Open doors may swing. Cupboard doors secured by magnetic catches may open. Pendulum clocks stop, start, or change rate.
    Structures :
    Some large display windows cracked. A few earthenware toilet fixtures cracked.
    MMI VI (Strong shaking) ?

    People
    Felt by all. People and animals alarmed. Many run outside. Difficulty experienced in walking steadily.
    Fittings :
    Objects fall from shelves. Pictures fall from walls. Some furniture moved on smooth floors, some unsecured free-standing fireplaces moved. Glassware and crockery broken. Very unstable furniture overturned. Small church and school bells ring. Appliances move on bench or table tops. Filing cabinets or “easy glide” drawers may open (or shut).
    Structures :
    Slight damage to buildings with low standard. Some stucco or cement plaster falls. Large display windows broken. Damage to a few weak domestic chimneys, some may fall.
    Environment :
    Trees and bushes shake, or are heard to rustle. Loose material may be dislodged from sloping ground, e.g. existing slides, talus slopes, shingle slides.
    MMI VII (Very strong shaking) ?

    People
    General alarm. Difficulty experienced in standing. Noticed by motorcar drivers who may stop.
    Fittings :
    Large bells ring. Furniture moves on smooth floors, may move on carpeted floors. Substantial damage to fragile contents of buildings.
    Structures :
    Unreinforced stone and brick walls cracked. Low standard buildings cracked with some minor masonry falls. A few instances of damage to buildings of ordinary workmanship. Unbraced parapets, unbraced brick gables, and architectural ornaments fall. Roofing tiles, especially ridge tiles may be dislodged. Many unreinforced domestic chimneys damaged, often falling from roof-line. Water tanks Type I burst. A few instances of damage to brick veneers and plaster or cement-based linings. Unrestrained water cylinders (hot-water cylinders) may move and leak. Some common windows cracked. Suspended ceilings damaged.
    Environment :
    Water made turbid by stirred up mud. Small slides such as falls of sand and gravel banks, and small rock-falls from steep slopes and cuttings. Instances of settlement of unconsolidated or wet, or weak soils. Some fine cracks appear in sloping ground. A few instances of liquefaction (i.e. small water and sand ejections).
    MMI VIII (Severe shaking) ?

    People
    Alarm may approach panic. Steering of motorcars greatly affected.

    Structures :
    Low standard buildings heavily damaged, some collapse. ordinary workmanship buildings damaged, some with partial collapse. Reinforced masonry or concrete buildings damaged in some cases. A few instances of damage to buildings and bridges designed and built to resist earthquakes. Monuments and pre-1976 elevated tanks and factory stacks twisted or brought down. Some pre-1965 infill masonry panels damaged. A few post-1980 brick veneers damaged. Decayed timber piles of houses damaged. Houses not secured to foundations may move. Most unreinforced domestic chimneys damaged, some below roof-line, many brought down.

    Environment :
    Cracks appear on steep slopes and in wet ground. Small to moderate slides in roadside cuttings and unsupported excavations. Small water and sand ejections and localized lateral spreading adjacent to streams, canals, lakes, etc.

    MMI IX (Violent shaking) ?

    Structures
    Many low standard buildings destroyed. Ordinary workmanship buildings heavily damaged, some collapse. Reinforced masonry or concrete buildings damaged, some with partial collapse. Buildings and bridges designed and built to resist earthquakes damaged in some cases, some with flexible frames seriously damaged. Damage or permanent distortion to some buildings and bridges, designed and built to normal use standards. Houses not secured to foundations shifted off. Brick veneers fall and expose frames.

    Environment :
    Cracking of ground conspicuous. Landsliding general on steep slopes. Liquefaction effects intensified and more widespread, with large lateral spreading and flow sliding adjacent to streams, canals, lakes, etc.

    Tell us your experience and how many seconds the shaking lasted + let us know if your property has been damaged (even slight damage). (max. 500 characters)

    * mandatory fields <!–

     

    Security check, enter >

    –>
    characters allowed
    characters typed extra


    X

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    cursor:pointer;
    display:none;
    height:100%;
    position:fixed;
    text-align:center;
    top:0;
    width:100%;
    z-index:10000;
    left:0;
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    .hover_bkgr_fricc img.thankyou-div {
    width: 150px;
    }
    .hover_bkgr_fricc .helper{
    display:inline-block;
    height:100%;
    vertical-align:middle;
    }
    .hover_bkgr_fricc > div {
    background-color: #fff;
    box-shadow: 10px 10px 60px #555;
    display: inline-block;
    height: auto;
    max-width: 551px;
    min-height: 100px;
    vertical-align: middle;
    width: 60%;
    position: relative;
    border-radius: 8px;
    padding: 15px 5%;
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    .popupCloseButton {
    background-color: #fff;
    border: 3px solid #999;
    border-radius: 50px;
    cursor: pointer;
    display: inline-block;
    font-family: arial;
    font-weight: bold;
    position: absolute;
    top: -20px;
    right: -20px;
    font-size: 25px;
    line-height: 30px;
    width: 30px;
    height: 30px;
    text-align: center;
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    .popupCloseButton:hover {
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    cursor: pointer;
    font-size: 20px;
    margin: 20px;
    display: inline-block;
    font-weight: bold;
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    var PREV_MII_Help = false;
    var PREV_v = false;
    var LANG_count_text = jQuery(“#quake_c_count”).text();
    var LANG_extra_text = jQuery(“#quake_c_extra”).text();

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    var xurl = “https://earthquake-report.com/wp-content/plugins/quakesos/experience.php”;
    var url1 = jQuery(“.quake_felt”).first().attr(“href”);
    jQuery(“#qid”).val(url1);
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    jQuery("#quake_success").html("
    Earthquake-Report.com appreciates sharing your experience with our readers!”);
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    jQuery(“.hover_bkgr_fricc”).show();
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    });
    jQuery(“.quake_felt”).live(“click”, function(e)
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    var url = jQuery(this).attr(“href”);
    var mag = jQuery(this).attr(“mag”);
    var tit = jQuery(this).attr(“title”);
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    //jQuery(“#form_overlay”)
    //.css(“z-index”, 2000)
    //.find(“#quake_experience”)

    jQuery(“#qid”).val(url);
    //jQuery(“#form_overlay”)
    //.hcenter()
    //.fadeIn(1000)
    jQuery(“#comments,#captcha”)//,#email
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    //jQuery(“#email”)
    //.focus();

    //jQuery(“#captcha_img”)
    // .attr(“src”, captcha_url + “/captcha.php?” + Date());
    /*jQuery(“#captcha_reload”)
    .attr(“src”, captcha_url + “/reload.png”)
    .attr(“alt”, “Reload security captcha”)
    .attr(“title”, “Reload security captcha”)
    .css(“cursor”, “pointer”)
    .click(function(e) {
    jQuery(“#captcha_img”)
    .attr(“src”, captcha_url + “/captcha.php?” + Date());
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    */
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    jQuery(fld)
    .focus()
    .select()
    }
    );
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    source