Around a cup Of Tea

You’re planing on assisting the countdown to 2018. But you decide to sleep till 23.30h. Unfortunately for you, you don’t wake up. In the morning you discover after a while that you’re still 31th of December 2017. Thinking that you’ve been dreaming, you decide of staying awake all night. But unfortunately for you, you doze off and wake up the 31th of December again.

What would you do?

The Theory of Fate – Chapter 5/part 9

It will be only a single decree
The day when the horn will be blown and we shall gather them together while they will have turned blue on that day and will be whispering among themselves: you did not remain (in the graves) more than ten (days).

And (remember) the day when the heaven shall be rent asunder with clouds, and the angels shall be sent down, with a grand descending.

And when the trumpet is sounded, that day it will be a distressful day

And listen, the day when the caller will call from a place nearby

Surely the day of decision is an appointed time a day when the trumpet will be blown, and you will come in large groups and the heaven shall be opened, and it will become as gates and the mountains shall be moved away from their places and they will be as if they were a mirage

They wait only but a single shout which will size them while they are disputing then they will not be able to make bequest nor they will return to their family and the trumpet will be blown (2nd blow) and behold from the Graves they will come out quickly to their Lord

How will you do then, if you disbelieve, guard yourselves against a day which will turn the children’s hair grey
When the order will come the horn will be blown,  but the thing is that at first I thought that this loud sound would come from the supervolcano but a lot worst than the Krakatoe volcano did. But then I changed my mind when I read this verse And listen, the day when the caller will call from a place nearby. This verse is speaking of a creature who calls. It will be such a loud sound that it will be able to kill all of us instantly they will not be able to make bequest nor they will return to their family. Actually it is normal that a really loud sound kills someone:

Can sound kill you? The short answer is “yes” — and, rather shockingly, the European Space Agency says that it now has such a sonic weapon in its arsenal that, if it was so inclined, could kill you. For the long answer, read on.

The question is, is 154 decibels enough to kill you? In all honesty, probably not — unless, perhaps, you were stuck with your head inside the horn for a prolonged period. 150 decibels is usually considered enough to burst your eardrums, but the threshold for death is usually pegged at around 185-200 dB. A passenger car driving by at 25 feet is about 60 dB, being next to a jackhammer or lawn mower is around 100 dB, a nearby chainsaw is 120 dB. Generally, 150 dB (eardrum rupture) is only achieved if you stand really close to a jet aircraft during take-off or you’re near an explosive blast.

 If you actually wanted to intentionally kill someone with a sonic weapon, there isn’t a whole lot of research on how you would actually go about doing it. The general consensus is that a loud enough sound could cause an air embolism in your lungs, which then travels to your heart and kills you. Alternatively, your lungs might simply burst from the increased air pressure. (Acoustic energy is just waves of varying sound pressure; the higher the energy, the higher the pressure, the louder the sound.) In some cases, where there’s some kind of underlying physical weakness, loud sounds might cause a seizure or heart attack — but there’s very little evidence to suggest this.

 Perhaps more significantly, though, it’s important to note that a sonic weapon doesn’t have to be lethal or incredibly loud to be effective. High-intensity ultrasonic sound (generally anything above 20KHz) can cause physical damage. Some very low frequencies (infrasound) can apparently cause your eyeballs to vibrate, making it very hard to see. Targeted “sonic bullets” that cause localized pain (or simply burst your eardrums) is probably enough to immobilize most non-action-hero humans.

 When the heaven shall be opened and becomes as gates, that’s not something we can see with our present eyes. There are two things which might turn the childrens’s hair grey. Either the sun’s Uv’s or the volcanes ashes. 


Tomorrow as you might know is “Around a cup Of Tea” but there will also be the Conclusion of The Theory Of Fate

The Theory of Fate – Chapter 5/part 8

​Then when the heaven is rent asunder and it becomes (rosy or red) like paint

And when a single blast is sounded on the trumpet, and earth and the mountains are heaved up and then crushed in a single crash. On that day the great event come to pass inevitable,

and the heaven will be rent asunder for that day it will be frail and torn up

Whereon the heaven will be cleft asunder.

A day whereon men will be like moths scattered about

O ye who believe! fear Allah and believe in His Messenger, He will give you a double share of his mercy, and will provide for you a light wherein you will walk, and will grant you forgiveness and verily Allah is most forgiving and merciful

Here we are back to the sky which will be cleft asunder, well… if volcanic eruption acts so badly to the ozone layer than that might be the explanation. We’re aware of the ozone layer protection, The ozone layer is one layer of the stratosphere, the second layer of the Earth’s atmosphere. The stratosphere is the mass of protective gases clinging to our planet. 

 The stratosphere gets its name because it is stratified, or layered: as elevation increases, the stratosphere gets warmer. The stratosphere increases in warmth with elevation because ozone gases in the upper layers absorb intense ultraviolet radiation from the sun.

 Ozone is only a trace gas in the atmosphere—only about 3 molecules for every 10 million molecules of air. But it does a very important job. Like a sponge, the ozone layer absorbs bits of radiation hitting Earth from the sun. Even though we need some of the sun’s radiation to live, too much of it can damage living things. The ozone layer acts as a shield for life on Earth.
Ozone is good at trapping a type of radiation called ultraviolet radiation, or UV light, which can penetrate organisms’ protective layers, like skin, damaging DNA molecules in plants and animals. There are two major types of UV light: UVB and UVA. 
UVB is the cause of skin conditions like sunburns, and cancers like basal cell carcinoma and squamous cell carcinoma. 

 People used to think that UVA light, the radiation used in tanning beds, is harmless because it doesn’t cause burns. However, scientists now know that UVA light is even more harmful than UVB, penetrating more deeply and causing a deadly skin cancer, melanoma, and premature aging. The ozone layer, our Earth’s sunscreen, absorbs about 98 percent of this devastating UV light

Now saying that the sky will be rosy or red like paint makes me think of the sunsets’s or sunrises’s hue which turns redder after an eruption:

The eruption of Krakatoa on August 26–27, 1883, completely collapsed its Indonesian island, blasting the stratosphere with volcanic dust and sulphur dioxide. A catastrophe of incredible scale for anyone in its radius, the natural disaster impacted the entire world with skies suddenly changed, particularly the sunsets which many reported as having altered, otherworldly colors.

Artists were among those mesmerized by the Krakatoa sunsets, and captured them on canvas with vibrant detail then impossible for photography.

Four years following Krakatoa’s eruption, the Earth was oddly cold, something scientists later found was sulfur dioxide in the high atmosphere reacting with water vapor, making very fine particles of sulphuric acid. These aerosols reflected back some sunlight, and also created the strange sunsets.

 Munch described the sunset he witnessed after Krakatoa:

 “I was walking along the road with two friends — then the sun set — all at once the sky became blood red — and I felt overcome with melancholy. I stood still and leaned against the railing, dead tired — clouds like blood and tongues of fire hung above the blue-black fjord and the city. My friends went on, and I stood alone, trembling with anxiety. I felt a great, unending scream piercing through nature.”

 It haunted him, and finally in 1893 he painted it as he remembered. “The Scream” (1893).  However, there was another artist who made hundreds of paintings of the post-volcano sunsets while they happened. In “The Krakatoa Sunsets,” part of the recently published The Public Domain Review: Selected Essays, 2011-2013, Richard Hamblyn writes “by late October 1883 most of the world, including Britain, was being subjected to lurid evening displays, caused by the scattering of incoming light by the meandering volcanic haze.” British artist William Ascroft, from his vantage on the Thames in Chelsea, painted pastel after pastel sunset until they faded in 1886. While not as well known as Munch, Ascroft left a blazing climatological archive of the skies.

 Krakatoa was unusually cataclysmic, with the loudest noise ever made by Earth, heard up to 3,000 miles away (consider hearing a noise in New York made in Los Angeles). At least 36,000 people were killed. But it’s not the only volcano to have influenced sunsets in art. An analysis last year of over 300 works from the Tate and National Gallery in London covered 50 volcanic explosions and the skies after, potentially to compare to modern aerosol pollution. These volcano “afterglows” were visual oddities, alluring to artists, that are now a form of scientific record, and reminders of the power of the Earth.

It’s undoubted that after a super volcano eruption the sun will be hidden so there will be no light and God will provide for the believers a light wherein we will walk. 

Here is what people see after an eruption:

Ash falls vary widely in intensity, size of the ash particles, and the degree to which light from the sun is obscured or blocked completely. Because of the unexpected darkness during daylight hours, loud thunder and lightning, and the sometimes strong smell of sulfur during an ash fall, many people describe the experience as eerie and frightening, disorienting and confusing, or dreadful. In extreme ash fall, for example when ash thickness is more than 5-10 cm, people may feel stunned and fearful of the conditions, have a difficult time breathing if a well-sealed shelter is not available. If caught outside during low visibility, people may become lost or extremely disoriented.

People being scattered and disoriented is part of the ash fall and this remembers me of a proverbe:

The light  24.40

Or their deeds are like darkness within an vast and deep sea which is covered by waves, upon which are waves, over which are clouds: layers of darkness one upon another. When one puts out his hand [therein], he can hardly see it. And he to whom Allah has not granted light – for him there is no light.

The Theory Of Fate – Chapter 5/part 7

These are some of the VEI 8 supervolcanoes but not always the most threatening:

City of Rocks State Park, Galán, La Garita Caldera, Island Park Caldera, Misema Caldera, Pacana Caldera, Taupo Volcano, Lake Taupo, Lake Toba, Yellowstone Caldera

So these three verses seem to speak of a volcanic activity. As written above, strong  volcanic ashes covers the sun light for a long time as happened 250 million years ago or even 65 million years ago, as it covers the sun, it covers the faces too, flames of Fire and smoke is what volcanoes do best, it comes from underneath us as it comes from the Earth’s core and from above after the ejection. There isn’t a better explanation. If we look for the long-lasting climate change of the Siberian Traps, we’ll see that the sun has been banned for a long time. 

A super volcano is the most destructive force on this planet. Only a few exist in the world. They lie dormant for hundreds of thousands of years as a vast reservoir of magma builds up inside them before finally they unleash their apocalyptic force, capable of obliterating continents.

The last eruption of a super volcano was in Toba, Sumatra, 75,000 years ago. It had 10,000 times the explosive force of Mount St. Helens and changed life on Earth forever. Thousands of cubic kilometres of ash was thrown into the atmosphere – so much that it blocked out light from the sun all over the world. 2,500 miles away 35 centimetres of ash coated the ground. Global temperatures plummeted by 21 degrees. The rain would have been so poisoned by the gasses that it would have turned black and strongly acidic. Man was pushed to the edge of extinction, the population forced down to just a couple of thousand. Three quarters of all plants in the northern hemisphere were killed.

The usual effects of a giant eruption, is acid rain, ozone depletion, a massive dose of carbon dioxide into the atmosphere,  the ingredients are in place for a mass extinction.

The primary role of volcanic sulfur aerosols in causing short-term changes in the world’s climate following some eruptions, instead of volcanic ash, was hypothesized by scientists in the early 1980’s. They based their hypothesis on the effects of several explosive eruptions in Indonesia and the world’s largest historical effusive eruption in Iceland.

Scientists studied three historical explosive eruptions of different sizes in Indonesia–Tambora (1815), Krakatau (1883), and Agung (1963). They noted that decreases in surface temperatures after the eruptions were of similar magnitude (0.18-1.3 °C). The amount of material injected into the stratosphere, however, differed greatly. By comparing the estimated amount of ash vs. sulfur injected into the stratosphere by each eruption, it was suggested that the longer residence time of sulfate aerosols, not the ash particles which fall out within a few months of an eruption, was the paramount controlling factor (Rampino and Self, 1982).

In contrast to these explosive eruptions, one of the most severe volcano-related climate effects in historical times was associated with a largely nonexplosive eruption that produced very little ash–the 1783 eruption of Laki crater-row in Iceland. The eruption lasted 8-9 months and extruded about 12.3 km3 of basaltic lava over an area of 565 km2. A bluish haze of sulfur aerosols all over Iceland destroyed most summer crops in the country; the crop failure led to the loss of 75% of all livestock and the deaths of 24% of the population (H. Sigurdsson, 1982). The bluish haze drifted east across Europe during the 1783-1784 winter, which was unusually severe.

Clearly, these examples suggested that the explosivity of an eruption and the amount of ash injected into the stratosphere are not the main factors in causing a change in Earth’s climate. Instead, scientists concluded that it must be the amount of sulfur in the erupting magma.

The eruption of El Chichon, Mexico, in 1982 conclusively demonstrated this idea was correct. The explosive eruption injected at least 8 Mt of sulfur aerosols into the atmosphere, and it was followed by a measureable cooling of parts of the Earth’s surface and a warming of the upper atmosphere. A similar-sized eruption at Mount St. Helens in 1980, however, injected only about 1 Mt of sulfur aerosols into the stratosphere. The eruption of Mount St. Helens injected much less sulfur into the atmosphere–it did not result in a noticeable cooling of the Earth’s surface. The newly launched TOMS satellite (in 1978) made it possible to measure these differences in the eruption clouds. Such direct measurements of the eruption clouds combined with surface temperatures make it possible to study the corrleation between volcanic sulfur aerosols (instead of ash) and temporary changes in the world’s climate after some volcanic eruptions.

 The most significant impacts from large explosive eruptions come from the conversion of sulfur dioxide (SO2) to sulfuric acid (H2SO4), which condenses rapidly in the stratosphere to form fine sulfate aerosols. The aerosols increase the reflection of radiation from the Sun back into space and thus cool the Earth’s lower atmosphere or troposphere; however, they also absorb heat radiated up from the Earth, thereby warming the stratosphere.

Ozone depletion promoted by volcanic sulfur aerosols. The sulfate aerosols also promote complex chemical reactions on their surfaces that alter chlorine and nitrogen chemical species in the stratosphere. This effect, together with increased stratospheric chlorine levels from chlorofluorocarbon (CFC) pollution, generates chlorine monoxide (ClO), which destroys ozone (O3)