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This might be true, but keep in mind that even a moderately interesting profile is better than a blank one. Besides, the most important thing is that your profile radiates proficiency. Shine on Your Photo Dating sites heavily emphasize your main profile picture. Dating apps further increase the importance of images, as they typically take up more space on your screen. All in all, your main picture is your front line fighter when it comes to competing for attention. So make sure you look your best! Get in your best duds, and ask your friends to make a nice photo of you. Most people portray themselves while doing something dull, such as standing or sitting. Smile from your heart. Be happy, energetic, or mysterious.

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History of electromagnetism Lodestone , a natural magnet , attracting iron nails. Ancient humans discovered the property of magnetism from lodestone. An illustration from Gilbert’s De Magnete showing one of the earliest methods of making a magnet.

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The vector B is termed the magnetic field, and it is defined as the vector field necessary to make the Lorentz force law correctly describe the motion of a charged particle. This definition allows the determination of B in the following way [14] [T]he command, “Measure the direction and magnitude of the vector B at such and such a place,” calls for the following operations: Take a particle of known charge q. Measure the force on q at rest, to determine E. Then measure the force on the particle when its velocity is v; repeat with v in some other direction.

Now find a B that makes the Lorentz force law fit all these results—that is the magnetic field at the place in question. Alternatively, the magnetic field can be defined in terms of the torque it produces on a magnetic dipole see magnetic torque on permanent magnets below. Alternative names for H [13] [15] Magnetic field intensity Magnetic field Magnetizing field In addition to B, there is a quantity H, which is often called the magnetic field.

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New evidence confirms that, like Earth, Saturn’s magnetic field helps create its own auroras. This space spectacle attracts a more fundamental question about where its magnetic field came from in the first place. Though Saturn is incredibly distant, the Hubble telescope was able to record its auroras in unprecedented detail. It is now clear that Saturn’s auroras, best seen in ultraviolet UV wavelengths, form when solar outbursts collapse its “magnetotail,” the portion of its magnetic field and attending electrified gas that flows in the planet’s wake.

A Leicester University News Release noted that the collaborating scientists will publish their photographic results in Geophysical Research Letters. It stated that Saturn’s collection of newly captured dramatic light displays “smoking gun” evidence that confirms a magnetic field at the source.

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More About Earth Changes These analyses reveal an astounding feature: In this area, the polarity of the field is opposite to the average global magnetic field. If we were able to use a compass deep under southern Africa, we would see that in this unusual patch north actually points south. This patch is the main culprit creating the South Atlantic Anomaly.

In numerical simulations, unusual patches similar to the one beneath southern Africa appear immediately prior to geomagnetic reversals. The poles have reversed frequently over the history of the planet, but the last reversal is in the distant past , some , years ago. The rapid decay of the recent magnetic field, and its pattern of decay, naturally raises the question of what was happening prior to the last years.

Archaeomagnetism takes us further back in time In archaeomagnetic studies, geophysicists team with archaeologists to learn about the past magnetic field.

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To test their theory, researchers from the Czech University of Life Sciences studied the body positions of 70 dogs across 37 breeds as they went to the toilet on walks. In total they recorded 1, defecations and 5, urinations over a period of two years. By studying different breeds, the researchers were able to rule out the possibility that positions were unique to certain species. However, this only happened when the magnetic field was what’s called ‘stable’ – when it sits along the existing axis and isn’t fluctuating.

The magnetic field can become ‘unstable’ when affected by solar flares, pictured, for example, and when this happened the dogs’ positions were more random The findings have been published in the journal Frontiers in Zoology.

Links to Magnetic Therapy Articles There are some excellent articles on the Internet explaining and debunking magnetic therapy. The following articles will provide you with some of the information needed to start looking critically at the claims of those promoting magnetic therapy products.

A few days later, retired Apollo astronaut Phil Chapman sent me this article which lays some of the doubts to rest. Phil never got to fly in space but was mission Scientist on Apollo It is not every day I get the opportunity to publish an article from such a pre-eminent scientist. Sunspots and GCRs There is absolutely no doubt that solar activity via the solar wind directly affects the flux of galactic cosmic rays GCRs reaching the Earth.

Note that the scale for GCRs is inverted, increasing downward, to facilitate comparison with the sunspot record; that the major time division is 11 years, to illustrate the well- known approximate periodicity of the sunspot cycle; and that the GCR minimum usually lags the sunspot maximum by a year or two. The linear trend lines in the figure show the decline in the average number of sunspots since the early s and the corresponding increase in GCRs, as we began a new Grand Solar Minimum already named the Eddy Minimum by the solar physics community.

Sunspots and 10Be There is also no doubt that creation of 10Be varies with solar activity. In Figure 2, I derived the upper curve by smoothing the annual average sunspot number also from SILSO using an year symmetrical moving average to suppress the year cycle symmetrical means that each data point is the average over the previous 5 to following 5 years, avoiding a time shift in the average.

The lower curve shows the 10Be concentration vs time in Antarctic ice cores the average of values from the South Pole and Dome Fuji stations , as percentage deviations from the average since AD. The scale is again inverted, increasing downward. It takes several years for cosmogenic 10Be to drift down into the troposphere and then to reach the ground in rain and snow, by which time the atmosphere is quite well mixed.

We know this because neutrons from the massive Soviet atmospheric nuclear tests on Novaya Zemlya in converted nitrogen to radioactive 14C, which reached New Zealand by If solar cosmic rays SCRs were a significant source of 10Be, the deposition would increase with the strength of the solar wind and thus with the sunspot number.

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History of Technology Heroes and Villains – A little light reading Here you will find a brief history of technology. Initially inspired by the development of batteries, it covers technology in general and includes some interesting little known, or long forgotten, facts as well as a few myths about the development of technology, the science behind it, the context in which it occurred and the deeds of the many personalities, eccentrics and charlatans involved.

You may find the Search Engine , the Technology Timeline or the Hall of Fame quicker if you are looking for something or somebody in particular. Scroll down and see what treasures you can discover. Background We think of a battery today as a source of portable power, but it is no exaggeration to say that the battery is one of the most important inventions in the history of mankind. Volta’s pile was at first a technical curiosity but this new electrochemical phenomenon very quickly opened the door to new branches of both physics and chemistry and a myriad of discoveries, inventions and applications.

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By Lenz’s law , any change in the magnetic field would be immediately opposed by currents, so the flux through a given volume of fluid could not change. As the fluid moved, the magnetic field would go with it. The theorem describing this effect is called the frozen-in-field theorem. Even in a fluid with a finite conductivity, new field is generated by stretching field lines as the fluid moves in ways that deform it. This process could go on generating new field indefinitely, were it not that as the magnetic field increases in strength, it resists fluid motion.

The temperature increases towards the center of the Earth, and the higher temperature of the fluid lower down makes it buoyant. This buoyancy is enhanced by chemical separation: As the core cools, some of the molten iron solidifies and is plated to the inner core.

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Within these weaker areas the local directions and intensities change gradually secular variation. A compass does not point to the true North Pole but to direction that is a function of the North Magnetic Pole and the local secular variation to yield a magnetic declination. The magnetic declination at any given time can be frozen into a clay formation that contains magnetite and is heated above the Curie point.

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NEH Educators Archaeomagnetic Dating Archaeomagnetic dating is a method of dating iron-bearing sediments that have been superheated—for example, the clay lining of an ancient hearth. By tracking and cross-dating past changes in the location of the magnetic field, geophysicists have reconstructed a series of magnetic polar positions extending back more than 2, years. This series of dated positions is known as the “archaeomagnetic reference curve.

Southwest Archaeomagnetic Reference Curve. Journal of Archaeological Science So how do scientists use the earth’s wandering magnetic field to date archaeological sites?

Archaeomagnetic dating is a method of dating iron-bearing sediments that have been superheated—for example, the clay lining of an ancient hearth. Archaeomagnetic dating works because the earth’s magnetic field “wanders,” continually changing its position in response to changes in the flow of.

Fortunately t h e magnetism acquired cannot be e a s i l y destroyed, though proximity t o a f l a s h of l i g h t n i n g i s one w a y I n which t h i s may happen. A compass needle – which l a not suspended about i t s cen t r e of g r a v i t y – i nd ica t e s only t h e -Tic meridian, a a – 17 – the time of cooling are determined. Ideally the specimen should be found in aitu undisturbed from its last cooling and the hori- zontal a n w a p h i c north directions are then accurately marked on it before removal to the laboratory – detailed techniques for doing this have been developed.

However if one is dealing with pottery that has been baked in an upright position or any specimen in which the horizontal dixection may be inferred with certainty one can determine the angle o f dip I even though one finds the pot on a museum shelf. This need for calibration – and the fact that the calibration for one locality cannot be extrapolated with certainty to localities further away than several hundred miles – is in sharp contrast to the radiocarbon dating method; the half-life of radiocarbon has world-wide validity and can be determined once and for all by present-day laboratory measurements without reference to well- dated specimens.

It is tempting to think that the magnetic direction has varied in a regular manner with a well-defined cycle of about years; this idea is not valid has been showy by a recent series of measurements made by Belshe’ and Cook on well-dated kilns and hearths in Britain covering the period from Roman times to the sixteenth century.

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Let’s start the story with the most prominent feature of the field today–its very rapid decay. By estimating the field intensity everywhere in, on, and above the earth , we can calculate the total electrical “energy” stored in the field. This rapid decay of both energy and intensity was not widely known, even among scientists, until Dr.

magnetic dating The use of magnetic properties for the age assessment of archaeological and geologic materials. It uses the natural remanent magnetization acquired at a specific time. Its direction can be compared with time-scales of geomagnetic secular variations, polarity reversal sequences, or .

Introduction What is ‘Magnetic Therapy’? Put simply, it is the use of magnets to treat or ease the symptoms of various diseases and conditions, including pain. There are excellent articles on the Internet explaining and debunking magnetic therapy and we will provide links to some of these at the end of this essay. However we don’t wish to just restate this information, so the main focus of this essay will be to explore some ‘what if’ scenarios.

What if magnetic therapy really did work the way magnetic therapy proponents say it does? How would our bodies really react? While these scenarios are no doubt obvious to those that investigate and subsequently criticise magnet therapy, those that purchase magnetic products seldom think too much about the ‘science’ claims. But by using some basic science and logic anyone can quickly see that magnetic therapy just couldn’t work the way they say it does.

Although we’ll mainly refer to ‘Magnetic Therapy’ in this essay, ‘healing with magnets’, ‘biomagnetic therapy’, ‘bio-magnetics’ and ‘bioelectromagnetic therapy’ are some of the other names given to this scam. Magnets and their Use in Medicine Of course some will be skeptical that magnetic therapy is a scam, stating that they can vaguely recall accounts of doctors, scientists, researchers etc using magnets to diagnose and treat medical problems. And this is perfectly true.

However this apparent contradiction results from there being two types of ‘magnetic therapy’.

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Maybe a UFO landed on Mars, and the rock became lodged in its landing gear. Later, as the saucer was making its final approach into an alien base in Antarctica, the rock came loose and landed in the ice field. In short, the rock came to Earth the same way the dandelion came to North America – by ship. Reflecting on the situation, I thought that the changes on the seventh continent are so few that they hardly justify the creation of new maps. If someone desperately needed a map of the South Pole, it would suffice to resort to a National Geographic map or to the nearest Rand McNally atlas.

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