Treatment Options for measles

Several home remedies can be applied to protect an infected individual and prevent further progression of the illness.

Barley

Barley is extremely beneficial as it is packed with vitamin C, antioxidants and minerals.
Mix one cup of barley in three cups of water.Boil it and straina nd drink it 2-3 times a day.
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Turmeric

It has antiseptic as well as antioxidant properties, and hence it is very effective in reducing the symptoms of measles.
Add one tablespoon each of turmeric powder and honey to a glass of lukewarm milk. Drink it twice daily for a month.
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Licorice

Licorice root is known for its antiviral, antifungal and antibacterial properties.
Mix 1/2 tbsp of licorice powder and honey in a glass of lukewarm water. Drink this once daily.
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A demonstration video of how you can ask Elth for any home remedie

Home Remedies for burn

Burn gets cured by home remedieswhich help supporting for the skin layers by fastering of growing.

Coconut oil

Coconut oil contains Vitamin E and certain fatty acids that are anti-fungal and anti-bacterial.
Apply heated coconut oil on to the affected area.
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Oatmeal

It has  skin-soothing properties to reduce inflammation.
Eat Oats daily as breakfast.
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Honey

Honey is a natural antibiotic, which helps to prevent your burn from becoming infected.
Honey can be applied at the affected area.
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Aloe vera

It helps to heal the area.
It may apply to the affected area.
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A demonstration video of how you can ask Elth for any home remedie

The curious case of curiosity…

A strange figure similar to that of a women is found in images sent by curiosity rover from Mars.

Its hard to tell if this is a living being, or a statue of a being from long ago. However, a statue that small would be eroded and destroyed easily, so it has a higher chance of being a living being. Also it is facing the Mars rover…watching it from a distance. This being is about 8-10 cm tall.

The Connection…

Yes, one such species is known to exist that small. The Apollo 20 mission astronaut William Rutledge said inside the cigar ship in Deporte Crater (moon) he saw glass tubes on the walls with tiny human-like skeletons in them about 4-6 cm long.

Stay Tuned for more information.

DSCOVR with EPIC…

DSCOVR- Deep Space Climate Observatory is a weather observing satellite set to be launched by NOAA- National Occeanic and Atmospheric Administration by Jan ,2015.

NASA has contributed two Earth science instruments for NOAA’s satellite. One of the instruments called EPIC or Earth Polychromatic Imaging Camera.

EPIC will image the Earth in one picture, something that hasn’t been done before from a satellite. EPIC will also provide valuable atmospheric data..

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What is EPIC?

The Earth Polychromatic Imaging Camera (EPIC) is an imager that provides global spectral images of the entire sunlit face of Earth, as viewed from an orbit around Lagrangian point 1 (L1)—the neutral gravity point between Earth and the sun.

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EPIC is able to view the entire sunlit Earth from sunrise to sunset at an almost constant scattering angle between 165–178°. This scattering angle has minimal overlap with other satellites’ scattering angles. EPIC’s observations from the L1 position will provide a unique angular perspective and can be combined with other measurements to obtain particle shape, phase selection, optical depth, 3-D effects and stereo heights.

Imagery from EPIC will be used in science applications to measure

  • ozone amounts
  • aerosol amounts
  • cloud height and phase
  • vegetation properties
  • hotspot land properties (a view of the land from angles where shadows are a minimum)
  • UV radiation estimates at Earth’s surface

Maars

A maar is a volcanic crater that forms when magma contacts ground water to produce a steam explosion.

Ukinrek Maar

 

What is a Maar?

A maar is a shallow volcanic crater with steep sides that is surrounded by tephra deposits. The tephra deposits are thickest near the crater and decrease with distance from the crater.

A maar is formed by one or more underground explosions that occur when hot magma comes into contact with shallow ground water to produce a violent steam explosion. These explosions crush the overlying rocks and launch them into the air along with steam, water, ash and magmatic material. The materials usually travel straight up into the air and fall back to Earth to form the tephra deposits that surround the crater. If the tephra lithifies, it will become an igneous rock known as tuff.

tuff

If tephra surrounding a maar lithifies, it will become a rock known as “tuff.” Tuff is composed of rock fragments and large pieces of tephra in a matrix of volcanic ash. Image by Roll-Stone of Wikimedia.

The crater floor of a maar is usually below the original ground surface. After the eruption, an inflow of ground water often turns the crater into a shallow lake.

Most maars are a few hundred to a thousand meters in diameter and less than one hundred meters in depth. The largest maars, located on the Seward Peninsula of Alaska, are up to 8000 meters across and up to 300 meters in depth. See Google map at right.

How Common are Maars?

Maars are more numerous than most people realize. After cinder cones, maars are the second most common volcanic landform. [2] If you search the Smithsonian Institution’s Global Volcanism Program database, you will be able to find hundreds of maars. [3]

Maars are underrepresented as volcanic landscape features because they are small in size and lack rocky vertical development that would make them resistant to weathering and erosion. Because they are relatively small, shallow depressions, they can be easily filled with sediment and not recognized as volcanic features.

The Largest Known Maar

The largest known maar on Earth is Devil Mountain Maar Lake, located on the northern part of the Seward Peninsula of Alaska. It was produced by a hydromagmatic eruption that occurred about 17,500 years ago. The blast spread tephra over an area of about 2,500 square kilometers. The tephra is several tens of meters thick near the maar and decreases with distance away from the maar. [4] You can explore five of the world’s largest maars in the Google satellite image in the right column of this page.

SMELLED IT…

CHILEAN QUAKE CAUSED ICEQUAKES IN ANTARCTICA

The ice sheets in Antarctica vibrated a bit more than usual because of something more than 3,000 miles away : 8.8 magnitude Chilean earthquake . A study has found that Antarctica’s  frozen ground is sensitive to seismic waves from distant earthquakes .

Some of the ice quakes were quick bursts and over less than one second .Others were long duration,tremor signals up to 10 seconds. 

                                               MASSIVE CHILEAN EARTHQUAKE

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DIGGING OUR OWN GRAVE…

WELL THIS REMINDS ME OF THE QUOTATION THAT “NOTHING IS BEYOND MAN’S REACH”

NOT A JOKE BUT YES IT IS POSSIBLE TO CREATE YOUR OWN EARTHQUAKE ……BUT UNFORTUNATELY THIS IS NOT A MATTER OF BEING PROUD OF THE “TECHNICAL ACHIEVEMENT” BUT A MATTER OF IMMENSE “SHAME” FOR THE ENTIRE HUMANITY… 

Here is a list of “human efforts” to call the “death”

2008 Sichuan, China earthquake

It’s just water, but, man, water is heavy. Large reservoirs of water created by dams have a long history of inducing earthquakes, from Zambia to Greece to India. The 2008 earthquake in Sichuan, China, that killed nearly 70,000 people was one of the most devastating in recent memory, and some scientists think it was triggered by the construction of the Zipingpu Dam nearby.

The Zipingpu Dam sits just a third of a mile away from the fault, and the added weight of millions of tons of water could have hastened the fault’s rupture. “No geological process can come up with such a concentration of mass in such as small area other than a volcano,” said geologist Christian Klose about the buildup of water.

Groundwater extraction — 2011 Lorca earthquake

Taking water out of ground, which causes the water table to drop, can also destabilize an existing fault.

A 2011 earthquake in Lorca, Spain caused a great amount of destruction for its 5.1 magnitude because its epicenter was located so close to the surface. Its shallow epicenter may be related to groundwater extraction near Lorca, according to research published in Nature Geoscience. Since 1960, water extraction has caused the region’s water table to drop by an incredible 250 meters.

Geothermal power plants — Salton Sea Geothermal Field and The Geyers Geothermal Field

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At the end of the infamous San Andreas Fault in California lies the Salton Sea—and, along its southern shore, is the Salton Sea Geothermal Field. The power plant extracts hot, high-pressured water out of the ground and turns it into steam to run turbines generating power. If it seems like a bad idea to be extracting water so close to the San Andreas Fault, well, you’d be right.

In a 2011 study published in Science, researchers at the University of California, Santa Cruz, found that seismic activity has increased around the Salton Sea as geothermal field operations have ramped up. Earthquake swarms—bursts of dozens of small quakes below magnitude 6 or so—happen regularly along the Salton Sea. While these earthquake swarms by themselves may not cause much damage, they could interact with other bigger faults, like the San Andreas located so conveniently nearby, to induce far more damaging quakes.

Several hundred miles north in California is also the Geysers Geothermal Field, the largest geothermal field in the world. Because the Geysers don’t sit near a large fault, induced seismicity there is less likely to be majorly destructive. However, researchers have found that seismicity in the region has increased from basically zero in the 1960s to 20 or 30 small seismic events per year.

Fracking and injection wells — 2011 Oklahoma earthquake

When it comes to hydraulic fracturing, or fracking, it’s actually not the extraction of oil or gas that’s the problem. . It’s what happens to those afterward, when waste fracking fluid is injected back underground into deep wells. The fluid can seep out and lubricate faults, causing them to slip more easily. A study in Geology links a 2011 Oklahoma earthquake to wastewaterinjection wells.

Seismic activity in Oklahoma has shot up along with the rise of fracking: The number of earthquakes went from about a dozen in 2008 to over 1,000 in 2010. Earthquake swarms are now regular occurrences in the region. With fracking in the United States steadily increasing, the dangers of wastewater injection wells become more imminent.

Skyscrapers — Taipei 101

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The tallest building in the world when it was built, the Taipei 101 tower in Taiwan was supposed to be the city’s crown jewel, capable of withstanding typhoon winds and earthquakes. Ironically, the very things supposed to make it earthquake-resilient may be… causing earthquakes.

According to a Taiwanese geologist Cheng-Horn Lin, Taipei 101’s especially huge mass of 770,000 tons is putting too much pressure on the soft sedimentary rock below. This stress is due to all the extra steel and concrete used to make the skyscraper solid enough to withstand earthquakes. Since construction began on Taipei 101, according to Lin, the region has seen several micro-earthquakes and two larger earthquakes directly underneath the building.

During its construction in March 2002, a 6.8 earthquake did knock two cranes to the ground. Taipei 101 itself, though, was undamaged. So, if the skyscraper does cause earthquakes in the future, at least you know where to go?

Overenthusiastic Sports Fans — Seahawks Game, Seattle

When the Seattle Seahawks scored a touchdown on a fumble return last week, the seismometer down the block was keeping score. The University of Washington’s seismometer just one block south of CenturyLink Field registered a magnitude 1 or 2 earthquake from the rumbling of Seahawks fans. When your seismometer is so close, though, does it even really count? Well, here’s an empowering message: Stand close enough to a seismometer and you, too, can cause your very own earthquake.

NATURALITY LOST …

MAN MADE EARTHQUAKES

In the first Superman movie, supervillain Lex Luthor plans to trigger a massive, California-detaching earthquake by detonating a couple of nuclear weapons in the San Andreas Fault.

Crazy Lex! That scheme never would have worked, geologists will tell you. But, if he’d been serious about creating an earthquake, there are ways he could have actually done it. He would just have to inject some liquid (as some carbon-sequestration schemes propose) deep into the Earth’s crust, or bore a few hundred thousand tons of coal out of a mountain.

It turns out, actually, that the human production of earthquakes is hardly supervillain-worthy. It’s downright commonplace: Klose estimates that 25 percent of Britain’s recorded seismic events were caused by people.

Most of these human-caused quakes are tiny, registering less than four on geologist’s seismic scales. These window-rattlers don’t occur along natural faults, and wouldn’t have happened without human activity — like mining tons of coal or potash. They occur when a mine’s roof collapses, for example, as in the Crandall Canyon collapse in Utah that killed a half-dozen miners last year.

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But some human actions can trigger much larger quakes along natural fault lines. That’s because humans, with the aid of our massive machines, can sling enough mass around to shift the pattern of stresses in the
Earth’s crust. Faults that might not have caused an earthquake for a million years can suddenly be pushed to failure, as Klose argues occurred during Australia’s only fatal earthquake in 1989.

NEXT POST ON …….WAYS TO CREATE EARTHQUAKES

METEOR SHOWER…

The 2014 Perseid meteor shower will peak between August 10 and August 13. A waning Gibbous Moon (the Moon’s phase after a full moon) may make it harder for observers to see the shower. Despite this, astronomers suggest that observers try their luck to catch some Perseids before dawn on August 11, 12 and 13.

The Perseid meteor shower, one of the brighter meteor showers of the year, occur every August, peaking around August 9-13. Consisting of tiny space debris from the comet Swift-Tuttle, the Perseids are named after the constellation, Perseus. This is because, their radiant or the direction of which the shower seems to come from lies in the same direction as Perseus. The constellation lies in the north-eastern part of the sky.

While the skies light up several time a year by other meteor showers , the Perseids are widely sought after by astronomers and stargazers alike. This is because at its peak, one can view 60 to a 100 meteors in an hour from a dark place.

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Where to view

The Perseids can be viewed by observers in the Northern Hemisphere. If you are planning to view the shower, look between the radiant, which will be in the north-east part of the sky and the zenith (the point in sky directly above you). But don’t worry, you do not have to make any major astronomical calculations. Just lay a blanket on the ground, lie down and let your eyes wander around the sky – you will be bound to spot the shower sooner or later.

When to view

The best time to view the Perseids, or most other meteor showers is when the sky is the darkest. Most astronomers suggest that depending on the Moon’s phase, the best time to view meteor showers is right before dawn.

How to view

There isn’t a lot of skill involved in watching a meteor shower. Here are some tips on how to maximize your time looking for the Perseids:

  • Get out of the city to a place where city and artificial lights do not impede your viewing
  • If you are out viewing the shower during its peak, you will not need any special equipment. You should be able to see the shower with your naked eyes.
  • Carry a blanket or a comfortable chair with you – viewing meteors, just like any other kind of star gazing is a waiting game, and you need to be comfortable. Plus, you may not want to leave until you can’t see the majestic celestial fireworks anymore.
  • Check the weather and moonrise and moonset timings for your location before you leave, and plan your viewing around it.

EARTHQUAKES EXPLAINED…

How Do Earthquakes Occur?

Earthquakes are usually caused when rock underground suddenly breaks along a fault. This sudden release of energy causes the seismic waves that make the ground shake. When two blocks of rock or two plates are rubbing against each other, they stick a little. They don’t just slide smoothly; the rocks catch on each other. The rocks are still pushing against each other, but not moving. After a while, the rocks break because of all the pressure that’s built up. When the rocks break, the earthquake occurs.

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During the earthquake and afterward, the plates or blocks of rock start moving, and they continue to move until they get stuck again. The spot underground where the rock breaks is called the focus of the earthquake. The place right above the focus (on top of the ground) is called the epicenter of the earthquake.

Earthquake-like seismic waves can also be caused by explosions underground. These explosions may be set off to break rock while making tunnels for roads, railroads, subways, or mines. These explosions, however, don’t cause very strong seismic waves. You may not even feel them. Sometimes seismic waves occur when the roof or walls of a mine collapse. These can sometimes be felt by people near the mine.

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 ……KEEP VISITING !!!!