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Research published in suggests that Mercury has a molten core. It is thought that these were formed as Mercury's core and mantle cooled and contracted at a time when the crust had already solidified.
Mercury's core has a higher iron content than that of any other major planet in the Solar System, and several theories have been proposed to explain this.
The most widely accepted theory is that Mercury originally had a metal—silicate ratio similar to common chondrite meteorites, thought to be typical of the Solar System's rocky matter, and a mass approximately 2.
Alternatively, Mercury may have formed from the solar nebula before the Sun's energy output had stabilized. A third hypothesis proposes that the solar nebula caused drag on the particles from which Mercury was accreting , which meant that lighter particles were lost from the accreting material and not gathered by Mercury.
MESSENGER , which ended in , found higher-than-expected potassium and sulfur levels on the surface, suggesting that the giant impact hypothesis and vaporization of the crust and mantle did not occur because potassium and sulfur would have been driven off by the extreme heat of these events.
Mercury's surface is similar in appearance to that of the Moon, showing extensive mare -like plains and heavy cratering, indicating that it has been geologically inactive for billions of years.
Because knowledge of Mercury's geology had been based only on the Mariner 10 flyby and terrestrial observations, it is the least understood of the terrestrial planets.
For example, an unusual crater with radiating troughs has been discovered that scientists called "the spider". Albedo features are areas of markedly different reflectivity, as seen by telescopic observation.
Mercury has dorsa also called " wrinkle-ridges " , Moon-like highlands , montes mountains , planitiae plains , rupes escarpments , and valles valleys.
Names for features on Mercury come from a variety of sources. Names coming from people are limited to the deceased. Craters are named for artists, musicians, painters, and authors who have made outstanding or fundamental contributions to their field.
Ridges, or dorsa, are named for scientists who have contributed to the study of Mercury. Depressions or fossae are named for works of architecture.
Montes are named for the word "hot" in a variety of languages. Plains or planitiae are named for Mercury in various languages.
Valleys or valles are named for abandoned cities, towns, or settlements of antiquity. Mercury was heavily bombarded by comets and asteroids during and shortly following its formation 4.
Mercury's surface is more heterogeneous than either Mars 's or the Moon 's, both of which contain significant stretches of similar geology, such as maria and plateaus.
Craters on Mercury range in diameter from small bowl-shaped cavities to multi-ringed impact basins hundreds of kilometers across. They appear in all states of degradation, from relatively fresh rayed craters to highly degraded crater remnants.
Mercurian craters differ subtly from lunar craters in that the area blanketed by their ejecta is much smaller, a consequence of Mercury's stronger surface gravity.
At the antipode of the Caloris Basin is a large region of unusual, hilly terrain known as the "Weird Terrain".
One hypothesis for its origin is that shock waves generated during the Caloris impact traveled around Mercury, converging at the basin's antipode degrees away.
The resulting high stresses fractured the surface. Overall, about 15 impact basins have been identified on the imaged part of Mercury.
There are two geologically distinct plains regions on Mercury. Smooth plains are widespread flat areas that fill depressions of various sizes and bear a strong resemblance to the lunar maria.
Notably, they fill a wide ring surrounding the Caloris Basin. Unlike lunar maria, the smooth plains of Mercury have the same albedo as the older inter-crater plains.
Despite a lack of unequivocally volcanic characteristics, the localisation and rounded, lobate shape of these plains strongly support volcanic origins.
It is not clear whether they are volcanic lavas induced by the impact, or a large sheet of impact melt.
One unusual feature of Mercury's surface is the numerous compression folds, or rupes , that crisscross the plains. As Mercury's interior cooled, it contracted and its surface began to deform, creating wrinkle ridges and lobate scarps associated with thrust faults.
The Lunar Reconnaissance Orbiter discovered that similar small thrust faults exist on the Moon. It is thus a " compound volcano ".
Although the daylight temperature at the surface of Mercury is generally extremely high, observations strongly suggest that ice frozen water exists on Mercury.
Mercury is too small and hot for its gravity to retain any significant atmosphere over long periods of time; it does have a tenuous surface-bounded exosphere  containing hydrogen , helium , oxygen , sodium , calcium , potassium and others at a surface pressure of less than approximately 0.
Hydrogen atoms and helium atoms probably come from the solar wind , diffusing into Mercury's magnetosphere before later escaping back into space.
Radioactive decay of elements within Mercury's crust is another source of helium, as well as sodium and potassium. Water vapor is present, released by a combination of processes such as: comets striking its surface, sputtering creating water out of hydrogen from the solar wind and oxygen from rock, and sublimation from reservoirs of water ice in the permanently shadowed polar craters.
Sodium, potassium and calcium were discovered in the atmosphere during the —s, and are thought to result primarily from the vaporization of surface rock struck by micrometeorite impacts  including presently from Comet Encke.
This would indicate an interaction between the magnetosphere and the planet's surface. Despite its small size and slow day-long rotation, Mercury has a significant, and apparently global, magnetic field.
According to measurements taken by Mariner 10 , it is about 1. The magnetic-field strength at Mercury's equator is about nT.
It is likely that this magnetic field is generated by a dynamo effect, in a manner similar to the magnetic field of Earth. Particularly strong tidal effects caused by the planet's high orbital eccentricity would serve to keep the core in the liquid state necessary for this dynamo effect.
Mercury's magnetic field is strong enough to deflect the solar wind around the planet, creating a magnetosphere.
The planet's magnetosphere, though small enough to fit within Earth,  is strong enough to trap solar wind plasma. This contributes to the space weathering of the planet's surface.
Bursts of energetic particles in the planet's magnetotail indicate a dynamic quality to the planet's magnetosphere. The spacecraft encountered magnetic "tornadoes" — twisted bundles of magnetic fields connecting the planetary magnetic field to interplanetary space — that were up to km wide or a third of the radius of the planet.
These twisted magnetic flux tubes, technically known as flux transfer events , form open windows in the planet's magnetic shield through which the solar wind may enter and directly impact Mercury's surface via magnetic reconnection  This also occurs in Earth's magnetic field.
Mercury has the most eccentric orbit of all the planets; its eccentricity is 0. It takes The diagram illustrates the effects of the eccentricity, showing Mercury's orbit overlaid with a circular orbit having the same semi-major axis.
Mercury's higher velocity when it is near perihelion is clear from the greater distance it covers in each 5-day interval. In the diagram the varying distance of Mercury to the Sun is represented by the size of the planet, which is inversely proportional to Mercury's distance from the Sun.
This varying distance to the Sun leads to Mercury's surface being flexed by tidal bulges raised by the Sun that are about 17 times stronger than the Moon's on Earth.
Mercury's orbit is inclined by 7 degrees to the plane of Earth's orbit the ecliptic , as shown in the diagram on the right. As a result, transits of Mercury across the face of the Sun can only occur when the planet is crossing the plane of the ecliptic at the time it lies between Earth and the Sun, which is in May or November.
This occurs about every seven years on average. Mercury's axial tilt is almost zero,  with the best measured value as low as 0.
This means that to an observer at Mercury's poles, the center of the Sun never rises more than 2. At certain points on Mercury's surface, an observer would be able to see the Sun peek up a little more than two-thirds of the way over the horizon, then reverse and set before rising again, all within the same Mercurian day.
Thus, to a hypothetical observer on Mercury, the Sun appears to move in a retrograde direction. Four Earth days after perihelion, the Sun's normal apparent motion resumes.
For the same reason, there are two points on Mercury's equator, degrees apart in longitude , at either of which, around perihelion in alternate Mercurian years once a Mercurian day , the Sun passes overhead, then reverses its apparent motion and passes overhead again, then reverses a second time and passes overhead a third time, taking a total of about 16 Earth-days for this entire process.
In the other alternate Mercurian years, the same thing happens at the other of these two points. The amplitude of the retrograde motion is small, so the overall effect is that, for two or three weeks, the Sun is almost stationary overhead, and is at its most brilliant because Mercury is at perihelion, its closest to the Sun.
This prolonged exposure to the Sun at its brightest makes these two points the hottest places on Mercury. Maximum temperature occurs when the Sun is at an angle of about 25 degrees past noon due to diurnal temperature lag , at 0.
These points, which are the ones on the equator where the apparent retrograde motion of the Sun happens when it is crossing the horizon as described in the preceding paragraph, receive much less solar heat than the first ones described above.
Mercury attains inferior conjunction nearest approach to Earth every Earth days on average,  but this interval can range from days to days due to the planet's eccentric orbit.
Mercury can come as near as This large range arises from the planet's high orbital eccentricity. The longitude convention for Mercury puts the zero of longitude at one of the two hottest points on the surface, as described above.
However, when this area was first visited, by Mariner 10 , this zero meridian was in darkness, so it was impossible to select a feature on the surface to define the exact position of the meridian.
Therefore, a small crater further west was chosen, called Hun Kal , which provides the exact reference point for measuring longitude.
A International Astronomical Union resolution suggests that longitudes be measured positively in the westerly direction on Mercury.
For many years it was thought that Mercury was synchronously tidally locked with the Sun, rotating once for each orbit and always keeping the same face directed towards the Sun, in the same way that the same side of the Moon always faces Earth.
Radar observations in proved that the planet has a spin-orbit resonance, rotating three times for every two revolutions around the Sun.
The eccentricity of Mercury's orbit makes this resonance stable—at perihelion, when the solar tide is strongest, the Sun is nearly still in Mercury's sky.
The rare resonant tidal locking is stabilized by the variance of the tidal force along Mercury's eccentric orbit, acting on a permanent dipole component of Mercury's mass distribution.
However, with noticeable eccentricity, like that of Mercury's orbit, the tidal force has a maximum at perihelion and therefore stabilizes resonances, like , enforcing that the planet points its axis of least inertia roughly at the Sun when passing through perihelion.
The original reason astronomers thought it was synchronously locked was that, whenever Mercury was best placed for observation, it was always nearly at the same point in its resonance, hence showing the same face.
This is because, coincidentally, Mercury's rotation period is almost exactly half of its synodic period with respect to Earth. Due to Mercury's spin-orbit resonance, a solar day the length between two meridian transits of the Sun lasts about Earth days.
Simulations indicate that the orbital eccentricity of Mercury varies chaotically from nearly zero circular to more than 0.
In , the French mathematician and astronomer Urbain Le Verrier reported that the slow precession of Mercury's orbit around the Sun could not be completely explained by Newtonian mechanics and perturbations by the known planets.
He suggested, among possible explanations, that another planet or perhaps instead a series of smaller 'corpuscules' might exist in an orbit even closer to the Sun than that of Mercury, to account for this perturbation.
The success of the search for Neptune based on its perturbations of the orbit of Uranus led astronomers to place faith in this possible explanation, and the hypothetical planet was named Vulcan , but no such planet was ever found.
The perihelion precession of Mercury is 5, arcseconds 1. Newtonian mechanics, taking into account all the effects from the other planets, predicts a precession of 5, arcseconds 1.
The effect is small: just Similar, but much smaller, effects exist for other Solar System bodies: 8. Filling in the values gives a result of 0.
This is in close agreement with the accepted value of Mercury's perihelion advance of There may be scientific support, based on studies reported in March , for considering that parts of the planet Mercury may have been habitable , and perhaps that life forms , albeit likely primitive microorganisms , may have existed on the planet.
Mercury can be observed for only a brief period during either morning or evening twilight. Mercury can, like several other planets and the brightest stars, be seen during a total solar eclipse.
Like the Moon and Venus, Mercury exhibits phases as seen from Earth. It is "new" at inferior conjunction and "full" at superior conjunction.
The planet is rendered invisible from Earth on both of these occasions because of its being obscured by the Sun,  except its new phase during a transit.
Mercury is technically brightest as seen from Earth when it is at a full phase. Although Mercury is farthest from Earth when it is full, the greater illuminated area that is visible and the opposition brightness surge more than compensates for the distance.
Nonetheless, the brightest full phase appearance of Mercury is an essentially impossible time for practical observation, because of the extreme proximity of the Sun.
Mercury is best observed at the first and last quarter, although they are phases of lesser brightness.
The first and last quarter phases occur at greatest elongation east and west of the Sun, respectively. At both of these times Mercury's separation from the Sun ranges anywhere from Mercury can be easily seen from the tropics and subtropics more than from higher latitudes.
Viewed from low latitudes and at the right times of year, the ecliptic intersects the horizon at a steep angle. At middle latitudes , Mercury is more often and easily visible from the Southern Hemisphere than from the Northern.
This is because Mercury's maximum western elongation occurs only during early autumn in the Southern Hemisphere, whereas its greatest eastern elongation happens only during late winter in the Southern Hemisphere.
An alternate method for viewing Mercury involves observing the planet during daylight hours when conditions are clear, ideally when it is at its greatest elongation.
Care must be taken to ensure the instrument isn't pointed directly towards the Sun because of the risk for eye damage. This method bypasses the limitation of twilight observing when the ecliptic is located at a low elevation e.
Ground-based telescope observations of Mercury reveal only an illuminated partial disk with limited detail. The Hubble Space Telescope cannot observe Mercury at all, due to safety procedures that prevent its pointing too close to the Sun.
Be patient with other people and be more present in your expression. Nine times out of ten, this compassionate deliberation will get you through.
In that rare case where compassionate deliberation is not enough, it might be best to put the interaction off until Mercury goes direct again in a few weeks.
Test Now! Mercury retrograde calendar encourages us to slow down in all aspects of our lives. Our modern mindset forces us to constantly go, go, go.
Too often, this urge to succeed prevents us from being thorough in the projects that we do take on. Mercury in retrograde gives us a chance to go back and redo it the correct way.
By slowing down, going back to our previous work, and tying up loose ends, we will be more in line with the energies present during a Mercury retrograde.
Aligning ourselves with these energies will prevent us from fighting the current, which will make our own lives easier during these frustrating times.
Ultimately, by going retrograde ourselves going back over our work , we will avoid many of the pitfalls normally associated with this period in the planetary cycle.
As I have been saying throughout this entire series of articles, the wise choice is to go with the flow and not fight the current of life.
There is a time for everything, and if you approach everything in its time, you will succeed effortlessly. The answer: Apply this astrological knowledge to your mundane life.
Consider all of the projects you are currently working on. It may be hard for them to separate their ego from their thinking, taking it far too personally when anyone disagrees with their opinion.
They can be masters of spin. Mercury being the neuter planet can account for a tendency to androgyny and bi-sexuality, or a certain childlike asexual charm.
But there is also the question of combustion to consider. Some forward thinking traditional astrologers have considered reducing the orb and raising the limit for Cazimi which I think would be worth considering when you look at the list on page 2.
This would bring prolific songwriter Carole King into the cazimi category. Mozart is also considered a genius and has Mercury combust Sun.
A good example of the Sun His father absorbing his child Mercury. Mercury being so close to the Sun can find it difficult to have its own mindset separate from the father or father figure.
Apin tablets. It is believed that these observations were made by an ancient Assyrian astronomer around 14 th century BC. Some Babylonian records date back to the 1 st millennium BC.
They called the planet Nabu, after the messenger to the gods in their mythology. The ancient Greeks knew the planet as Hermes while the Romans named it Mercury and it remained as such to this day.
Credits cannot be given to a single civilization or person because the planet has always been easy to spot on the sky.
It is theorized that Mercury was formed about 4. Its small size but enormous core is theorized to be the result of a collision with another giant object that stripped much of its surface.
Mercury is the closest planet to the Sun , at a distance of It takes sunlight 3. Mercury has a radius of 2. It is about the size of the continental United States, slightly bigger.
It has a mass of about 3. Despite being the smallest planet from the Solar System, it is the second densest planet in the Solar System , with a density of 5.
Mercury's highly eccentric, egg-shaped orbit takes the planet as close as 29 million miles or 47 million kilometers, and as far as 43 million miles or 70 million kilometers from the Sun.
Mercury travels through space at nearly 29 miles or 47 kilometers per second, faster than any other planet.
The resonance makes a single solar day on Mercury last exactly two Mercury years, about Earth days.
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