Solar System, technical/Moon

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These images show the libration of the Moon over a single lunar month. Credit: Tomruen.

Moon is Earth's only natural satellite. It is the brightest object in the night sky but gives off no light of its own. Instead, it reflects light from the Sun. Like Earth and the rest of the solar system, the Moon is about 4.6 milliard years old.

Completion status: About halfway there. You may help to clarify and expand it.

The Moon is much smaller than Earth. The Moon's average radius (distance from its centre to its surface) is 1,737.4 km), about 27% of the radius of Earth. The Moon is also much less massive than Earth. The Moon has a mass (amount of matter) of 7.35 x 1019 tonnes. Earth is about 81 times that massive. The Moon's density (mass divided by volume) is about 3.34 g/cm3, roughly 60% of Earth's density.

Educational level: this is a secondary education resource.

Because the Moon has less mass than Earth, the force due to gravity at the lunar surface is only about 1/6 of that on Earth. Thus, a person standing on the Moon would feel as if his or her weight had decreased by 5/6. And if that person dropped a stone, the stone would fall to the surface much more slowly than the same stone would fall to Earth.

Educational level: this is a tertiary (university) resource.

Despite the Moon's relatively weak gravitational force, the Moon is close enough to Earth to produce tides in Earth's waters. The average distance from the centre of Earth to the centre of the Moon is 384,467 km. That distance is growing, but extremely slowly. The Moon is moving away from Earth at a speed of about 3.8 cm per year.

Type classification: this is an article resource.

The temperature at the lunar equator ranges from extremely low to extremely high: from about –173°C at night to +127°C in the daytime. In some deep craters near the Moon's poles, the temperature is always near –240°C.

Resource type: this resource contains a lecture or lecture notes.

The Moon has no substantial atmosphere, but small amounts of certain gases are present above the lunar surface. People sometimes refer to those gases as the lunar atmosphere. This "atmosphere" can also be called an exosphere, defined as a tenuous (low-density) zone of particles surrounding an airless body. Mercury and some asteroids also have an exosphere.

Subject classification: this is an astronomy resource.

The Moon has no life of any kind. Compared with Earth, it has changed little over millions of years. On the Moon, the sky is black (even during the day), and the stars are always visible.

The Moon also crosses the sky occasionally sometimes in the daylight other times at night. The Moon doesn't always reflect uniformly during its travels. A shadow often blocks some of the reflection. Which entity is the cause for this, or is it an object, or perhaps a source of shadow?

Earth and Moon[edit | edit source]

The Earth and Moon is imaged by the Mars Global Surveyor on May 8, 2003, at 12:59:58 UTC.
This view of the rising Earth greeted the Apollo 8 astronauts as they came from behind the Moon after the lunar orbit insertion burn. Credit: NASA.

Eclipses and occultations[edit | edit source]

An annular eclipse on October 3, 2005, observed at Medina del Campo, Valladolid, España, is imaged. Credit: Locutus Borg.

An eclipse is when the light of the Sun or Moon is blocked such as the annular eclipse shown in the image at right on October 3, 2005, observed at Medina del Campo, Valladolid, España.

Observing a solar eclipse tells you that when both objects (the Sun and the Moon) are in the sky at the same time, close to each other, the Moon is between you and the Sun.

On April 25, 1838, an occultation of Mercury by the Moon occurred when Mercury was visible to the unaided eye after sunset.[1] An occultation of Venus by the Moon occurred "on the afternoon of October 14", 1874.[1] An earlier such occultation "occurred on May 23, 1587, and is thus recorded by [Tycho Brahe] in his Historia Celestis"[1].

Exploration[edit | edit source]

The large white arrow indicates Luna 21. The smaller white arrows indicate the rovers tracks. The black arrow indicates the crater where it picked up its fatal load of lunar dust. The grey dot lower left of the crater is thought to be the rover itself. Credit: NASA.
A view of the horizon on the Moon's solid surface shows a black sky without stars because of sunlight coming from the left. Credit: NASA.

Lunokhod-2 is an X-ray observatory (X-ray telescope), carried to the Moon by Luna 21 to observe solar X-rays. Luna 21 landed on the Moon on January 15, 1973, at 22:35:00 UTC, latitude 25°51' N, longitude 30°27' E. Less than 3 hr later Lunokhod 2 disembarked onto the lunar surface at 01:14 UTC on January 16, 1973. While still near the Luna 21 platform Lunokhod 2 carried out solar X-ray studies.[2]

At right is a view of the horizon on the Moon's solid surface taken by an Apollo 16 astronaut. The image shows a black sky without stars because the sunlight coming from the left is overwhelming.

Meteor astronomy[edit | edit source]

The white spot on this image of the Earth side of the Moon is the impact site of a meteor from March 17, 2013. Credit: NASA.
This image shows the lunar meteorite Allan Hills 81005. Credit: NASA.

"Lunar origin is established by comparing the mineralogy, the chemical composition, and the isotopic composition between meteorites and samples from the Moon collected by Apollo missions."[3]

"Cosmic ray exposure history established with noble gas measurements have shown that all lunar meteorites were ejected from the Moon in the past 20 million years. Most left the Moon in the past 100,000 years."[3]

"All six of the Apollo missions on which samples were collected landed in the central nearside of the Moon, an area that has subsequently been shown to be geochemically anomalous by the Lunar Prospector mission. In contrast, the numerous lunar meteorites are [likely to be] random samples of the Moon and consequently provide a more representative sampling of the lunar surface than the Apollo samples. Half the lunar meteorites, for example, likely sample material from the farside of the Moon."[3]

At top left is a NASA photograph showing the bright flash of light from a meteor impact that occurred on the Moon on March 17, 2013. According to NASA, a 0.3 m rock slammed into the lunar surface at 90,120 km/h, creating a fresh crater 20 m wide.

"The crash caused the biggest and brightest explosion scientists have seen since they started monitoring lunar meteorite strikes in 2005. ... The lunar blast was the equivalent of 5 tons of TNT going off".[4]

"The flash was so bright it saturated the camera".[5]

Cosmic-ray astronomy[edit | edit source]

The image shows the hydrogen concentrations on the Moon detected by the Lunar Prospector. Credit: NASA.
This image is an elemental map of the Moon using a GRS. Credit: Los Alamos National Laboratory.

At right is the result of an all Moon survey by the Lunar Prospector using an onboard neutron spectrometer (NS). Cosmic rays impacting the lunar surface generate neutrons which in turn loose much of their energy in collisions with hydrogen atoms trapped within the Moon's surface.[6] Some of these thermal neutrons collide with the helium atoms within the NS to yield an energy signature which is detected and counted.[6] The NS aboard the Lunar Prospector has a surface resolution of 150 km.[6]

Neutron astronomy[edit | edit source]

The neutron probe is in the hole on the Moon. Credit: NASA.
The image shows the hydrogen concentrations on the Moon detected by the Lunar Prospector. Credit: NASA.

At right is an image showing a neutron detector put into a pre-dug hole on the surface of the Moon by Eugene Cernan of the Apollo 17 lunar surface crew. Also, in the image is a boulder. "Now, this (boulder) ought to shield that thing (the neutron probe) from the doggone (RTG)"[7] "[T]he neutron probe consists of targets containing either boron or uranium-235 which, upon capturing neutrons, emit alpha particles or fission fragments which are then captured by plastic or mica detectors. The instrument consists of an outer tube containing the detectors and a central core containing the targets. Because the targets and detectors do not cover the whole surfaces of the core and tube, respectively, the core can be twisted so that the target/detector pairs are either next to each other or 180 degrees apart. In the latter case, very few alpha particles or fission fragments are captured by the detectors and, therefore, the instrument is "off".[8] "The neutron probe is a self-contained unit and, among other things, has no cable connecting it to electronics on the surface, a cable that would prevent the probe from falling out of reach to the bottom of the core hole. At the end of the third EVA, Jack will return to the ALSEP site and retrieve the probe so that he and Gene can bring it back to Earth for analysis."[8]

At lower right is the result of an all Moon survey by the Lunar Prospector using an onboard neutron spectrometer (NS). Cosmic rays impacting the lunar surface generate neutrons which in turn loose much of their energy in collisions with hydrogen atoms trapped within the Moon's surface.[6] Some of these thermal neutrons collide with the helium atoms within the NS to yield an energy signature which is detected and counted.[6] The NS aboard the Lunar Prospector has a surface resolution of 150 km.[6]

Proton astronomy[edit | edit source]

The Apollo Lunar Surface Experiments Packages (ALSEP) determined that more than 95% of the particles in the solar wind are electrons and protons, in approximately equal numbers.[9][10]

"Because the Solar Wind Spectrometer made continuous measurements, it was possible to measure how the Earth's magnetic field affects arriving solar wind particles. For about two-thirds of each orbit, the Moon is outside of the Earth's magnetic field. At these times, a typical proton density was 10 to 20 per cubic centimeter, with most protons having velocities between 400 and 650 kilometers per second. For about five days of each month, the Moon is inside the Earth's geomagnetic tail, and typically no solar wind particles were detectable. For the remainder of each lunar orbit, the Moon is in a transitional region known as the magnetosheath, where the Earth's magnetic field affects the solar wind but does not completely exclude it. In this region, the particle flux is reduced, with typical proton velocities of 250 to 450 kilometers per second. During the lunar night, the spectrometer was shielded from the solar wind by the Moon and no solar wind particles were measured."[9]

"In February 2009, the ESA SARA LENA instrument aboard India's Chandrayaan-1 detected hydrogen ENAs sputtered from the lunar surface by solar wind protons. Predictions had been that all impacting protons would be absorbed by the lunar regolith but for an as yet unknown reason, 20% of them are bounced back as low energy hydrogen ENAs. It is hypothesized that the absorbed protons may produce water and hydroxyls in interactions with the regolith.[11][12]"[13]

Electron astronomy[edit | edit source]

These two hemispheric Lambert azimuthal equal area projections show the total magnetic field strength at the surface of the Moon, derived from the Lunar Prospector electron reflectometer (ER) experiment. Credit: Mark A. Wieczorek.
The Moon where a prediction of a lunar double layer[14] was confirmed in 2003.[15] In the shadows, the Moon charges negatively in the interplanetary medium.[16] Credit: Mdf.

"The electron reflectometer (ER) [aboard the Lunar Prospector determines] the location and strength of magnetic fields from the energy spectrum and direction of electrons. The instrument [measures] the pitch angles of solar wind electrons reflected from the Moon by lunar magnetic fields. Stronger local magnetic fields can reflect electrons with larger pitch angles. Field strengths as small as 0.01 [nanotesla] nT could be measured with a spatial accuracy of about 3 km (1.9 mi) at the lunar surface."[17]

"[T]he shadowed lunar surface charges negative."[18]

Muon astronomy[edit | edit source]

The Moon's cosmic ray shadow, as seen in secondary muons generated by cosmic rays in the atmosphere, and detected 700 meters below ground, at the Soudan II detector. Credit: J. H. Cobb et al. (The Soudan 2 Collaboration).{{fairuse}}

At right the Moon's cosmic ray shadow is seen in secondary muons generated by cosmic rays in the atmosphere, and detected 700 meters below ground, at the Soudan II detector.

Gamma-ray astronomy[edit | edit source]

This image is an elemental map of the Moon using a GRS. Credit: Los Alamos National Laboratory.
The Moon is seen by the Compton Gamma Ray Observatory, in gamma rays of greater than 20 MeV. Credit: D. J. Thompson, D. L. Bertsch (NASA/GSFC), D. J. Morris (UNH), R. Mukherjee (NASA/GSFC/USRA).

The Compton Gamma Ray Observatory has imaged the Moon in gamma rays of energy greater than 20 MeV.[19] These are produced by cosmic ray bombardment of its surface.

"Gamma-ray spectrometers have been widely used for the elemental and isotopic analysis of airless bodies in the Solar System, especially the Moon[20] ... These surfaces are subjected to a continual bombardment of high-energy cosmic rays, which excite nuclei in them to emit characteristic gamma-rays which can be detected from orbit. Thus an orbiting instrument can in principle map the surface distribution of the elements for an entire planet. ... They are able to measure the abundance and distribution of about 20 primary elements of the periodic table, including silicon, oxygen, iron, magnesium, potassium, aluminum, calcium, sulfur, and carbon."[21] "[T]he chemical element thorium [is] mapped [by a GRS], with higher concentrations shown in yellow/orange/red in the left-hand side image shown on the right."[21]

X-ray astronomy[edit | edit source]

The Chandra X-ray Observatory image at right of the bright portion of the Moon is from oxygen, magnesium, aluminum and silicon atoms. Credit: Optical: Robert Gendler; X-ray: NASA/CXC/SAO/J.Drake et al.

"Lunar X-rays are thought to be produced by the scattering or fluorescence of solar X-rays from the Moon's surface (Schmitt et al., 1991)."[22]

X-rays from the dark moon, or shadowed portion of the Moon, can be explained by radiation from Earth's geocorona (extended outer atmosphere) through which orbiting spacecraft such as the Chandra X-ray Observatory move.

The Chandra X-ray Observatory has detected X-rays from oxygen, magnesium, aluminum and silicon atoms on the Moon.[23]

Ultraviolet astronomy[edit | edit source]

Clementine image of Aristarchus and surroundings is mapped onto simulated topography. Credit: NASA.

"In 1911, Professor Robert W. Wood used ultraviolet photography to take images of the crater area. He discovered the plateau had an anomalous appearance in the ultraviolet, and an area to the north appeared to give indications of a sulfur deposit.[24] This colorful area is sometimes referred to as "Wood's Spot", an alternate name for the Aristarchus Plateau."[25]

"Spectra taken of this crater during the Clementine mission were used to perform mineral mapping.[26] The data indicated that the central peak is a type of rock called anorthosite, which is a slow-cooling form of igneous rock composed of plagioclase feldspar. By contrast the outer wall is troctolite, a rock composed of equal parts plagioclase and olivine."[25]

"The Aristarchus region was part of a Hubble Space Telescope study in 2005 that was investigating the presence of oxygen-rich glassy soils in the form of the mineral ilmenite. Baseline measurements were made of the Apollo 15 and Apollo 17 landing sites, where the chemistry is known, and these were compared to Aristarchus. The Hubble Advanced Camera for Surveys was used to photograph the crater in visual and ultraviolet light. The crater was determined to have especially rich concentrations of ilmenite, a titanium oxide mineral that could potentially be used in the future by a lunar settlement for extracting oxygen.[27]"[25]

Visual astronomy[edit | edit source]

"The overall albedo of the Moon is around 0.12, but it is strongly directional and non-Lambertian, displaying also a strong opposition effect.[28]"[29]

Violet astronomy[edit | edit source]

During Galileo's December 1992 flyby of Earth's Moon, controllers took this dramatically illuminated picture through the violet filter. Credit: Galileo Project, JPL, NASA.

"Checking out the Galileo spacecraft's cameras during its December 1992 flyby of Earth's Moon, controllers took this dramatically illuminated picture [at right] through a violet filter. The view looks down on the Moon's north polar region with the Sun shining from the left at a low angle and the direction toward the moon's North pole toward the lower right. Across the image upper left stretches the smooth volcanic plain of the Mare Imbrium. Pythagoras crater, 65 miles wide, is near the center of the image -- mostly in shadow, its central peak just catches the sunlight. Yesterday, the Moon made its closest approach to Earth and was full for the second time in July (as reckoned by UT dates). The closest point in the Moon's orbit is referred to as Lunar Perigee, a mere 221,797 miles at 8 hours UT. The second full moon in a month is known as a "Blue Moon"."[30]

Blue astronomy[edit | edit source]

"Nine out of 10 well-characterized Apollo 17 breccia matrices fall into Group 2, and this includes both the blue-grey breccias which are the dominant rock type at this site"[31].

"A 1953 telescopic photograph of a flash on the Moon is the only unequivocal record of the rare crash of an asteroid-sized body onto the lunar surface. ... A search of images from the Clementine mission reveals an ∼1.5-km high-albedo, blue, fresh-appearing crater with an associated ejecta blanket at the location of the flash."[32]

In terms of reflectance from the lunar surface, "the very dark 'blue' maria [are] such as found in Mare Tranquillitatis."[33]

"[T]he slope of the reflectance spectrum in the blue and ultraviolet ... is directly related to the percent TiO2 in the [lunar] surface soil (Charette et al., 1974)."[34]

Cyan astronomy[edit | edit source]

“[A]ll the blue basalt types (high in UV/VIS ratio [0.40/0.56 µm]) are also the darkest mare soils.”[35] Both Luna 24 and Apollo 12 soil samples are from mare soils that reflect primarily cyan that is likely due to the presence of TiO2 in the soils.[34]

"Previous work has suggested that a cyan color in the multispectral frame represents highland material, and that yellows and greens are freshly excavated basalts. However, we have recently found that a cyan color can also result from a freshly excavated high-Ti basalt."[36]

Green astronomy[edit | edit source]

This colour mosaic was assembled from 18 images taken by Galileo's imaging system through a green filter. Credit: NASA/JPL/USGS.

"During its mission, the Galileo spacecraft returned a number of images of Earth's only natural satellite. Galileo surveyed the moon on Dec. 7, 1992, on its way to explore the Jupiter system in 1995-1997."[37]

"This color mosaic was assembled from 18 images taken by Galileo's imaging system through a green filter. On the upperleft is the dark, lava-filled Mare Imbrium, Mare Serenitatis (middle left), Mare Tranquillitatis (lower left), and Mare Crisium, the dark circular feature toward the bottom of the mosaic. Also visible in this view are the dark lava plains of the Marginis and Smythii Basins at the lower right. The Humboldtianum Basin, a 400-mile impact structure partly filled with dark volcanic deposits, is seen at the center of the image."[37]

Orange astronomy[edit | edit source]

"Crystallized spheres of orange glass from Shorty Crater at the Apollo 17 site are ... the characteristic ingredient of the dark mantling deposit of the Taurus-Littrow region."[38]

"The reflectance properties of the orange glass are highly distinctive. There are two broad absorption bands, one near 1.15 µm and the other near 1.9 µm that arise from Fe2+ on octahedral and tetrahedral sites, respectively ... The weak absorption near 0.5 µm probably arises from Ti3+, and the absorption edge extending into the visible region is due largely to oxygen-titanium charge transfer".[38]

Red astronomy[edit | edit source]

This view of the Moon was taken through a narrowband red filter (H-alpha). Credit: ESO and Andy Strappazzon.

"During a lunar eclipse, a very small amount of light from the sun does however still reach the Moon, even when the lunar eclipse is total; this is light which has been refracted or bent as it passes through the Earth's atmosphere. This sunlight has been scattered by the dust in the Earth's atmosphere, and thus that light is red, in the same way that sunset and sunrise light is red. This weak red illumination is what causes the eclipsed Moon to be dimly reddish or copper-colored in appearance.[39]"[40]

"This image of the crescent Moon [at left] shows sunlight skimming across the heavily pocked surface, filling its craters with shadows. This is a fairly flat region of the Moon, but elsewhere, high mountains can be found, with some peaks reaching about 5000 metres. When backlit by the Sun, these mountains cast long shadows on the lunar surface."[41]

"This view of the Moon was taken through a narrowband red filter (H-alpha). The height of the image is about 30 arcminutes."[41]

"The MPG/ESO 2.2-metre telescope at La Silla in Chile is a powerful instrument that can capture distant celestial objects, but it has been used here to image a heavenly body that is much closer to home: the Moon."[41]

Infrared astronomy[edit | edit source]

This image of Earth's moon is a three-colour composite of reflected near-infrared radiation from the Sun. Credit: ISRO/NASA/JPL-Caltech/Brown Univ./USGS.
The mid-infrared image of the Moon was taken during a 1996 lunar eclipse by the SPIRIT-III instrument aboard the orbiting Midcourse Space Experiment satellite. Credit: DCATT Team, MSX Project, BMDO (Ballistic Missile Defense Organization of the US DoD).
This is the first infrared image of the far side of the Moon. Credit: NASA.
NASA's Moon Mineralogy Mapper aboard the Chandrayaan-1 mission, took this image of Earth's moon. Credit: ISRO/NASA/JPL-Caltech/Brown Univ./USGS.
These images show a very young lunar crater on the side of the moon that faces away from Earth. Credit: ISRO/NASA/JPL-Caltech/USGS/Brown University.

"Four radiometers [aboard Luna 13 ] recorded infrared radiation from the [Moon's] surface indicating a noon temperature of 117 ±3 °C"[42].

"An infrared camera image from the moon is taken with the Lunar Crater Observation and Sensing Satellite (LCROSS) mid-infrared camera. LCROSS has nine science instruments that collect different types of data which are complementary to each other. These instruments provide for a robust collection of data about the composition of the lunar regolith."[43] "On the 9th of October, 2009, the Diviner team announced[44] detection of a hot spot on the moon at the location of the LCROSS impact."[45]

"Frank Washington Very's most important work was in measuring the temperature of the [surface] of the Moon using a bolometer. Samuel Pierpont Langley published in 1890 a widely read paper on the Moon observations, but for unknown reasons omitted Very's name from the list of authors. In 1891, Very published his own paper about the "Distribution of the Moon's Heat," which also included measurements taken during a lunar eclipse."[46]

"NASA's Moon Mineralogy Mapper, an instrument on the Indian Space Research Organization's Chandrayaan-1 mission, took [the image at right] of Earth's moon. It is a three-colour composite of reflected near-infrared radiation from the sun, and illustrates the extent to which different materials are mapped across the side of the moon that faces Earth. Small amounts of water were detected on the surface of the moon at various locations. This image illustrates their distribution at high latitudes toward the poles. Blue shows the signature of water, green shows the brightness of the surface as measured by reflected infra-red radiation from the sun and red shows a mineral called pyroxene."[47]

"Blue shows the signature of water, green shows the brightness of the surface as measured by reflected infrared radiation from the sun and red shows an iron-bearing mineral called pyroxene."[47]

"Small amounts of water were detected on the surface of the moon at various locations. This image illustrates their distribution at high latitudes toward the poles."[47]

"These images show a very young lunar crater on the side of the moon that faces away from Earth, as viewed by NASA's Moon Mineralogy Mapper [M3] on the Indian Space Research Organization's Chandrayaan-1 spacecraft. On the left is an image showing brightness at shorter infrared wavelengths. On the right, the distribution of water-rich minerals (light blue) is shown around a small crater. Both water- and hydroxyl-rich materials were found to be associated with material ejected from the crater."[48]

"The mid-infrared image of the Moon [at left] was taken during a 1996 lunar eclipse by the SPIRIT-III instrument aboard the orbiting Midcourse Space Experiment satellite. At these wavelengths, MSX was able to characterize the thermal (heat) distribution of the lunar surface during the eclipse. The brightest regions are the warmest, and the darkest areas are the coolest. The well-known crater Tycho is the bright object to the south of center. Numerous other craters are also seen as bright spots, indicating that their temperature is higher than in the surrounding dark mare. The Moon is geologically inactive for the most part, and any temperature differences are a result primarily of variations in solar heating (rather than volcanoes, for example). The Moon lacks an atmosphere to moderate temperatures, which can vary from 130 degrees Celsius (265 degrees Fahrenheit) in the sun to -110 degrees Celcius (-170 degrees Fahrenheit) in the shade."[49]

"M3 found a rock dominated by Mg-spinel with no detectable pyroxene or olivine present (<5%) occurring along the western inner ring of Moscoviense Basin (as one of several discrete areas). The occurrence of this spinel does not easily fit with current lunar-crustal evolution models.[50]"[51]

Radio astronomy[edit | edit source]

This image shows the variations in the lunar gravity field as measured by NASA's Gravity Recovery and Interior Laboratory (GRAIL) during the primary mapping mission from March to May 2012. Credit: NASA/JPL-Caltech/MIT/GSFC.

"The moon is comparatively close and was detected by radar, soon after the invention of the technique, in 1946.[52][53] Measurements included surface roughness and later mapping of shadowed regions near the poles."[54]

"Very precise microwave measurements between two spacecraft, named Ebb and Flow, were used to map gravity with high precision and high spatial resolution. The field shown resolves blocks on the surface of about 12 miles (20 kilometres) and measurements are three to five orders of magnitude improved over previous data. Red corresponds to mass excesses and blue corresponds to mass deficiencies. The map shows more small-scale detail on the far side of the moon compared to the nearside because the far side has many more small craters."[55]

"Twin NASA probes orbiting Earth's moon have generated the highest resolution gravity field map of any celestial body. The new map, created by the Gravity Recovery and Interior Laboratory (GRAIL) mission, is allowing scientists to learn about the moon's internal structure and composition in unprecedented detail. Data from the two washing machine-sized spacecraft also will provide a better understanding of how Earth and other rocky planets in the solar system formed and evolved."[55]

"The gravity field map reveals an abundance of features never before seen in detail, such as tectonic structures, volcanic landforms, basin rings, crater central peaks and numerous simple, bowl-shaped craters. Data also show the moon's gravity field is unlike that of any terrestrial planet in our solar system."[56]

""What this map tells us is that more than any other celestial body we know of, the moon wears its gravity field on its sleeve," said GRAIL Principal Investigator Maria Zuber of the Massachusetts Institute of Technology in Cambridge. "When we see a notable change in the gravity field, we can sync up this change with surface topography features such as craters, rilles or mountains.""[56]

"According to Zuber, the moon's gravity field preserves the record of impact bombardment that characterized all terrestrial planetary bodies and reveals evidence for fracturing of the interior extending to the deep crust and possibly the mantle. This impact record is preserved, and now precisely measured, on the moon. The probes revealed the bulk density of the moon's highland crust is substantially lower than generally assumed. This low-bulk crustal density agrees well with data obtained during the final Apollo lunar missions in the early 1970s, indicating that local samples returned by astronauts are indicative of global processes."[56]

""With our new crustal bulk density determination, we find that the average thickness of the moon's crust is between 21 and 27 miles (34 and 43 kilometres), which is about 6 to 12 miles (10 to 20 kilometres) thinner than previously thought," said Mark Wieczorek, GRAIL co-investigator at the Institut de Physique du Globe de Paris. "With this crustal thickness, the bulk composition of the moon is similar to that of Earth. This supports models where the moon is derived from Earth materials that were ejected during a giant impact event early in solar system history.""[56]

"The map was created by the spacecraft transmitting radio signals to define precisely the distance between them as they orbit the moon in formation. As they fly over areas of greater and lesser gravity caused by visible features, such as mountains and craters, and masses hidden beneath the lunar surface, the distance between the two spacecraft will change slightly."[56]

""We used gradients of the gravity field in order to highlight smaller and narrower structures than could be seen in previous datasets," said Jeff Andrews-Hanna, a GRAIL guest scientist with the Colorado School of Mines in Golden. "This data revealed a population of long, linear gravity anomalies, with lengths of hundreds of kilometres, crisscrossing the surface. These linear gravity anomalies indicate the presence of dikes, or long, thin, vertical bodies of solidified magma in the subsurface. The dikes are among the oldest features on the moon, and understanding them will tell us about its early history.""[56]

Astroglaciology[edit | edit source]

"The discoveries of water ice on the Moon, Mars and Europa add an extraterrestrial component to the field, as in "astroglaciology".[6]"[57]

Crater astronomy[edit | edit source]

The image is a map in French of the Moon showing the maria and the major craters. Credit: additions made to Lune22h27septembre2004.jpg created by Yves under GFDL by Eric Gaba (Sting - fr:Sting).
Composite image of the Moon is taken by the Galileo spacecraft on 7 December 1992. The color is 'enhanced' in the sense that the CCD camera is sensitive to near infrared wavelengths of light beyond human vision. Credit: NASA/JPL/USGS.
Lunar nearside, major maria and craters are labeled. Credit: Peter Freiman, Cmglee, and background photograph by Gregory H. Revera.
Twenty degrees of latitude of the Moon's disk, completely covered in the overlapping circles of craters. The illumination angles are from all directions, keeping almost all the crater floors in sunlight, but a set of merged crater floors right at the south pole are completely shadowed.
Mosaic image of the lunar south pole as taken by Clementine: note permanent polar shadow. Credit: NASA/JPL-Caltech.
The Moon's north pole is shown during the summer. Credit: NASA/GSFC/Arizona State University.
This full disk is nearly featureless, a uniform grey surface with almost no dark mare. There are many bright overlapping dots of impact craters. Credit: NASA/GSFC/ASU LRO.
Topography of the Moon measured from the Lunar Orbiter Laser Altimeter on the Lunar Reconnaissance Orbiter mission, referenced to a sphere of radius 1737.4 km. Credit: Mark A. Wieczorek.
These images show a very young lunar crater on the side of the moon that faces away from Earth. Credit: ISRO/NASA/JPL-Caltech/USGS/Brown Univ.

Lunar craters "are pits or depressions in the surface of the Moon, produced by great impacts of gigantic meteoroids which mostly took place billions of years ago. They range in size from huge walled plains more than a hundred miles across to microscopic pits. The smallest craters which can be glimpsed through ordinary binoculars are about twenty miles across. These craters are most common in the light-colored Lunar highlands. They are named after historical figures, mostly scientists."[58]

"During its flight, the Galileo spacecraft returned images of the Moon. The Galileo spacecraft took these images on December 7, 1992 on its way to explore the Jupiter system in 1995-97. The distinct bright ray crater at the bottom of the image is the Tycho impact basin. The dark areas are lava rock filled impact basins: Oceanus Procellarum (on the left), Mare Imbrium (center left), Mare Serenitatis and Mare Tranquillitatis (center), and Mare Crisium (near the right edge). This picture contains images through the Violet, 756 nm, 968 nm filters. The color is 'enhanced' in the sense that the CCD camera is sensitive to near infrared wavelengths of light beyond human vision."[59]

The dark irregular mare lava plains are prominent in the fully illuminated disk. A single bright star of ejecta, with rays stretching a third of the way across the disk, emblazons the lower centre: this is the crater Tycho on the Near side of the Moon. But, on the far side, the full disk is nearly featureless, a uniform grey surface with almost no dark mare. There are many bright overlapping dots of impact craters. And, an almost complete lack of dark maria.[60]

"The topography of the Moon has been measured with laser altimetry [using the sodium D2 line in the yellow] and stereo image analysis.[61] The most visible topographic feature is the giant far side South Pole – Aitken basin, some 2,240 km in diameter, the largest crater on the Moon and the largest known crater in the Solar System.[62][63] At 13 km deep, its floor is the lowest elevation on the Moon.[62][64] The highest elevations are found just to its north-east, and it has been suggested that this area might have been thickened by the oblique formation impact of South Pole – Aitken.[65] Other large impact basins, such as Imbrium, Serenitatis, Crisium, Smythii, and Orientale, also possess regionally low elevations and elevated rims.[62] The lunar far side is on average about 1.9 km higher than the near side.[66]"[67]

"These images show a very young lunar crater on the side of the moon that faces away from Earth, as viewed by NASA's Moon Mineralogy Mapper [M3] on the Indian Space Research Organization's Chandrayaan-1 spacecraft. On the left is an image showing brightness at shorter infrared wavelengths. On the right, the distribution of water-rich minerals (light blue) is shown around a small crater. Both water- and hydroxyl-rich materials were found to be associated with material ejected from the crater."[48]

"Unusual minerals in impact craters on the moon may not have originated on the moon, but may be from asteroids that created the craters"[68]

"Future studies of the moon's composition will have to show that exposed surface rocks really come from the moon and were not delivered by impacts, especially for unusual or exotic minerals ... "We cannot infer the deep composition of the moon from rocks in the centers of large craters without more care than has been used to date".[69]

"[C]omputer models [have been used] to simulate the formation of lunar craters by asteroid impacts and ... [in] some impacts much of the asteroid's material is not vaporized but is instead deposited in the center of the impact craters."[68]

Meteorites[edit | edit source]

Def. "a meteorite that is known to have originated on the Moon" is called a lunar meteorite.[3]

The meteorite "called Allan Hills 81005 ... resembled some rocks brought back from the Moon by the Apollo program.[70]"[3]

Yamato 791197 is another lunar meteorite.

"About 134 lunar meteorites have been discovered so far (as of October, 2010), perhaps representing more than 50 separate meteorite falls (i.e., many of the stones are "paired" fragments of the same meteoroid). The total mass is more than 46 kg."[3]

Meteorites have been found on the Moon[71][72]

Many of the meteorites that are found on Earth turn out to be from the Moon.

So far seifertite "has only been found in Martian[73][74] and lunar meteorites[75]"[76].

Classical planets[edit | edit source]

Monday is the day of the week for the Moon and its color is white.[77]

5102 b2k, is the historical year assigned to a Hindu table of planets that does include the classical planet, the Moon.[78]

~2500 b2k: “Understanding of the Moon's cycles was an early development of astronomy: by the 5th century BC, Babylonian astronomers had recorded the 18-year Saros cycle of lunar eclipses,[79] ”[67]

“Indian astronomers had described the Moon’s monthly elongation.[80]”[67]

“The Chinese astronomer Shi Shen (fl. 4th century BC) gave instructions for predicting solar and lunar eclipses.[81] ... Although the Chinese of the Han Dynasty believed the Moon to be energy equated to qi, their 'radiating influence' theory also recognized that the light of the Moon was merely a reflection of the Sun, and Jing Fang (78–37 BC) noted the sphericity of the Moon.[81]”[67]

“Later, the physical form of the Moon and the cause of moonlight became understood. The ancient Greek philosopher Anaxagoras (d. 428 BC) reasoned that the Sun and Moon were both giant spherical rocks, and that the latter reflected the light of the former.[82][81]”[67]

Aphrodite[edit | edit source]

""Foam-born" Aphrodite is linked to the Moon through her epithet Pasiphaessa, the 'All-shinig One'. In Hesiod's Theogony, Aphrodite was conceived in the lap of the waves which were fertilized by semen from the severed genitals of Ouranos, Heaven, and was 'born in soft foam', as the Homeric Hymn to Aphrodite puts it.71"[83]

See also[edit | edit source]

References[edit | edit source]

  1. ↑ 1.0 1.1 1.2 Samuel J. Johnson (1874). "Occultations of and by Venus". Astronomical register 12: 268-70. 
  2. ↑ Kocharov, G. E.; Viktorov, S. V.; Victorov, S. V.; Chesnokov, V. I. (1975). "Investigation of solar X-rays from the lunar surface, carried out on Lunokhod-2". Space Research 15: 633-6. 
  3. ↑ 3.0 3.1 3.2 3.3 3.4 3.5 "Lunar meteorite". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). August 30, 2012. http://en.wikipedia.org/wiki/Lunar_meteorite. Retrieved 2012-09-28. 
  4. ↑ Mike Wall (May 22, 2013). "Big Meteor Explosion on Moon Shows Lunar Exploration Risks". Yahoo! News. Retrieved 2013-05-22.
  5. ↑ Bill Cooke (May 22, 2013). "Big Meteor Explosion on Moon Shows Lunar Exploration Risks". Yahoo! News. Retrieved 2013-05-22.
  6. ↑ 6.0 6.1 6.2 6.3 6.4 6.5 6.6 David R. Williams (November 2011). "Lunar Prospector Neutron Spectrometer (NS)". Goddard Space Flight Laboratory: National Aeronautics and Space Administration. Retrieved 2012-01-11. Cite error: Invalid <ref> tag; name "Williams" defined multiple times with different content
  7. ↑ Eugene Cernan (August 22, 2011). "Deep Core, In: APOLLO 17 LUNAR SURFACE JOURNAL". Washington, DC USA: NASA. Retrieved 2012-08-18.
  8. ↑ 8.0 8.1 Dave Shaffer (August 22, 2011). "Deep Core, In: APOLLO 17 LUNAR SURFACE JOURNAL". Washington, DC USA: NASA. Retrieved 2012-08-18.
  9. ↑ 9.0 9.1 "Apollo 11 Mission". Lunar and Planetary Institute. 2009. Retrieved 2009-06-12.
  10. ↑ "Space Travel and Cancer Linked? Stony Brook Researcher Secures NASA Grant to Study Effects of Space Radiation". Brookhaven National Laboratory. 12 December 2007. Retrieved 2009-06-12.
  11. ↑ Bhardwaj, A.; Barabash, S.; Futaana, Y.; Kazama, Y.; Asamura, K.; McCann, D.; Sridharan, R.; Holmstrom, . et al. (December 2005). "Low energy neutral atom imaging on the Moon with the SARA instrument aboard Chandrayaan-1 mission". J. Earth Syst. Sci. 114 (6): 749–760. doi:10.1007/BF02715960. http://www.ias.ac.in/jessci/dec2005/ilc-21.pdf. Retrieved 2009-11-01. 
  12. ↑ "How The Moon Produces Its Own Water". European Space Agency. ScienceDaily. 2009-10-19. Retrieved 2009-11-01.
  13. ↑ "Energetic neutral atom". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). August 4, 2012. http://en.wikipedia.org/wiki/Energetic_neutral_atom. Retrieved 2012-09-26. 
  14. ↑ Borisov, N.; Mall, U. "The structure of the double layer behind the Moon" (2002) Journal of Plasma Physics, vol. 67, Issue 04, pp. 277–299
  15. ↑ Halekas, J. S.; Lin, R. P.; Mitchell, D. L. "Inferring the scale height of the lunar nightside double layer" (2003) Geophysical Research Letters, Volume 30, Issue 21, pp. PLA 1-1. (PDF)
  16. ↑ Halekas, J. S et al. "Evidence for negative charging of the lunar surface in shadow" (2002) Geophysical Research Letters, Volume 29, Issue 10, pp. 77–81
  17. ↑ "Lunar Prospector". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). August 12, 2012. http://en.wikipedia.org/wiki/Lunar_Prospector. Retrieved 2012-08-12. 
  18. ↑ J. S. Halekas; R. P. Lin; D. L. Mitchell (November 2003). "Inferring the scale height of the lunar nightside double layer". Geophysical Research Letters 30 (21): 4. doi:10.1029/2003GL018421. 
  19. ↑ "CGRO SSC >> EGRET Detection of Gamma Rays from the Moon". Heasarc.gsfc.nasa.gov. 2005-08-01. Retrieved 2011-11-08.
  20. ↑ D. J. Lawrence; W. C. Feldman; B. L. Barraclough; A. B. Binder; R. C. Elphic; S. Maurice; D. R. Thomsen (1998). "Global Elemental Maps of the Moon: The Lunar Prospector Gamma-Ray Spectrometer". Science 281 (5382): 1484–1489. doi:10.1126/science.281.5382.1484. PMID 9727970. 
  21. ↑ 21.0 21.1 "Gamma ray spectrometer". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). December 11, 2011. http://en.wikipedia.org/wiki/Gamma_ray_spectrometer. Retrieved 2012-06-09. 
  22. ↑ T. E. Cravens (2000). "X-ray emission from comets and planets". Advances in Space Research 26 (10): 1443-51. doi:0.1016/S0273-1177(00)00100-9. http://www.sciencedirect.com/science/article/pii/S0273117700001009. Retrieved 2012-01-11. 
  23. ↑ Robert Burnham (2004). Moon Prospecting. Kalmbach Publishing Co.. http://elibrary.ru/item.asp?id=7602287. Retrieved 2012-01-11. 
  24. ↑ David O. Darling. "Aristarchus: Lunar Transient Phenomenon History". L.T.P. Research. Retrieved 2006-08-08. {{cite web}}: |archive-date= requires |archive-url= (help)
  25. ↑ 25.0 25.1 25.2 "Aristarchus (crater)". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). March 27, 2013. http://en.wikipedia.org/wiki/Aristarchus_(crater). Retrieved 2013-06-30. 
  26. ↑ "Aristarchus Region: Multispectral Mosaic of the Aristarchus Crater and Plateau". Lunar and Planetary Institute. Retrieved 2006-08-08.
  27. ↑ Jeffrey Kluger (2005-10-20). "Is There Oxygen on the Moon?". Time Online. Retrieved October 24, 2005.
  28. ↑ Jeffrey S. Medkeff (2002). "Lunar Albedo". Archived from the original on 23 May 2008. Retrieved 5 July 2010.
  29. ↑ "Albedo". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). April 24, 2013. http://en.wikipedia.org/wiki/Albedo. Retrieved 2013-05-01. 
  30. ↑ Robert Nemiroff; Jerry Bonnell (July 31, 1996). "Astronomy Picture of the Day". Washington, DC USA: NASA. Retrieved 2013-04-01.
  31. ↑ John W. Morgan; H. Higuchi; Edward Anders (November-December 1975). "Meteoritic material in a boulder from the Apollo 17 site - Implications for its origin". The Moon 14 (12): 373-83. doi:10.1007/BF00569671. 
  32. ↑ Bonnie J Buratti, Lane L Johnson (January 2003). "Identification of the lunar flash of 1953 with a fresh crater on the moon’s surface". Icarus 161 (1): 192-7. doi:10.1016/S0019-1035(02)00027-1. http://www.sciencedirect.com/science/article/pii/S0019103502000271. Retrieved 2012-11-27. 
  33. ↑ Thomas B. McCord; John B. Adams (September 1973). "Progress in remote optical analysis of lunar surface composition". The Moon 7 (3-4): 453-74. doi:10.1007/BF00564646. 
  34. ↑ 34.0 34.1 Carle Pieters; Thomas B. McCord (April 1976). Characterization of lunar mare basalt types. I - A remote sensing study using reflection spectroscopy of surface soils, In: Proceedings Lunar Science Conference, 7th. 3. New York: Pergamon Press, Inc.. pp. 2677-90. 
  35. ↑ Carle’ M. Pieters. Mare basalt types on the front side of the moon - A summary of spectral reflectance data, In: Lunar and Planetary Science Conference, 9th, Houston, Tex., March 13-17, 1978, Proceedings. 3. New York: Pergamon Press, Inc.. pp. 2825-49. Bibcode: 1978LPSC....9.2825P. 
  36. ↑ D. J. Heather; S. K. Dunkin; P. D. Spudis; D. B. J. Bussey (January 1999). A Multispectral Analysis of the Flamsteed Region of Oceanus Procellarum, In: Workshop on New Views of the Moon 2: Understanding the Moon Through the Integration of Diverse Datasets. Bibcode: 1999nvm..conf...24H. 
  37. ↑ 37.0 37.1 Yvette Smith (December 8, 2009). "Earth's Moon". NASA. Retrieved 2012-07-22.
  38. ↑ 38.0 38.1 John B. Adams; Carle Pieters; Thomas B. McCord (March 18, 1974). Orange glass: Evidence for regional deposits of pyroclastic origin on the moon, In: Proceedings of the Fifth Lunar Science Conference. 1. New York: Pergamon Press, Inc.. pp. 171-86. 
  39. ↑ David K. Lynch, William Charles Livingston (July 2001). Color and light in nature. Cambridge University Press; 2 edition. p. 38,39. ISBN 978-0-521-77504-5. http://books.google.com/books?id=4Abp5FdhskAC&pg=PA38&lpg=PA38&source=bl&ots=bN3UHSoym0&sig=DIeWBajGeM4ecoPW1KKNmhLyaV0&hl=en&ei=pFe8TLjoLJGqsAPcsemzDw&sa=X&oi=book_result&ct=result&resnum=1&ved=0CBIQ6AEwAA#v=onepage&f=false. 
  40. ↑ "Earth's shadow". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). February 28, 2013. http://en.wikipedia.org/wiki/Earth%27s_shadow. Retrieved 2013-05-30. 
  41. ↑ 41.0 41.1 41.2 Andy Strappazzon (July 18, 2011). "Hidden Treasure on Our Doorstep". La Silla, Chile: ESO. Retrieved 2013-07-28.
  42. ↑ "Luna 13". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). September 5, 2012. http://en.wikipedia.org/wiki/Luna_13. Retrieved 2012-09-26. 
  43. ↑ "File:Mid infrared camera image of the moon by LCROSS.jpg". Wikimedia Commons (San Francisco, California: Wikimedia Foundation, Inc). October 10, 2009. http://commons.wikimedia.org/wiki/File:Mid_infrared_camera_image_of_the_moon_by_LCROSS.jpg. Retrieved 2012-09-26. 
  44. ↑ http://www.diviner.ucla.edu/blog/?p=184
  45. ↑ "Diviner". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). October 25, 2011. http://en.wikipedia.org/wiki/Diviner. Retrieved 2012-09-26. 
  46. ↑ "Frank Washington Very". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). June 3, 2012. http://en.wikipedia.org/wiki/Frank_Washington_Very. Retrieved 2012-09-26. 
  47. ↑ 47.0 47.1 47.2 Yvette Smith (September 25, 2009). "Water Detected at High Latitudes on the Moon". NASA. Retrieved 2012-09-26.
  48. ↑ 48.0 48.1 Jim Wilson (September 24, 2009). "Water Around a Fresh Crater". NASA. Retrieved 2012-09-26.
  49. ↑ DCATT Team (1996). "MSX Showcase A Gallery of Infrared Images". Pasadena, California USA: California Institute of Technology. Retrieved 2013-08-02.
  50. ↑ Pieters, Carle. "Identification of a new spinel-rich lunar rock type by the Moon Mineralogy Mapper (M3)" (PDF). LPI. Retrieved 12 April 2011.
  51. ↑ "Moon Mineralogy Mapper". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). July 12, 2012. http://en.wikipedia.org/wiki/Moon_Mineralogy_Mapper. Retrieved 2012-09-26. 
  52. ↑ J. Mofensen (February, April 1946). "Radar Echoes from the Moon". Nature, Electronics 157, 19 (3379): 129, 92-8. doi:10.1038/157129b0. 
  53. ↑ Z. Bay, "Reflection of microwaves from the moon," Hung. Acta Phys., vol. 1, pp. 1-22; April, 1946.
  54. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named RadarAstronomy
  55. ↑ 55.0 55.1 Tony Greicius (December 6, 2012). "GRAIL's Gravity Map of the Moon". NASA/JPL-Caltech/MIT/GSFC. Retrieved 2012-12-15.
  56. ↑ 56.0 56.1 56.2 56.3 56.4 56.5 PR Newswire (December 5, 2012). "NASA Twin Spacecraft Create Most Accurate Gravity Map Of Moon". Retrieved 2012-12-15.
  57. ↑ "Glaciology". Wikipedia (San Francisco, California: Wikimedia Foundation, Inc). March 30, 2013. http://en.wikipedia.org/wiki/Glaciology. Retrieved 2013-06-23. 
  58. ↑ Fountains of Bryn Mawr (October 30, 2008). "Skygazing". Wikiversity: 1. http://en.wikiversity.org/w/index.php?title=Skygazing&oldid=367815. Retrieved 2013-03-30. 
  59. ↑ Jon Nelson (June 8, 1998). "Earth's Moon". NASA/JPL/USGS. Retrieved 2012-09-26.
  60. ↑ "Landscapes from the ancient and eroded lunar far side". esa. Retrieved 15 February 2010.
  61. ↑ Spudis, Paul D.; Cook; Robinson; Bussey; Fessler (01/1998). "Topography of the South Polar Region from Clementine Stereo Imaging". Workshop on New Views of the Moon: Integrated Remotely Sensed, Geophysical, and Sample Datasets: 69. 
  62. ↑ 62.0 62.1 62.2 Spudis, Paul D.; Reisse, Robert A.; Gillis, Jeffrey J. (1994). "Ancient Multiring Basins on the Moon Revealed by Clementine Laser Altimetry". Science 266 (5192): 1848–1851. doi:10.1126/science.266.5192.1848. PMID 17737079. 
  63. ↑ Pieters, C.M.; Tompkins, S.; Head, J.W.; Hess, P.C. (1997). "Mineralogy of the Mafic Anomaly in the South Pole‐Aitken Basin: Implications for excavation of the lunar mantle". Geophysical Research Letters 24 (15): 1903–6. doi:10.1029/97GL01718. http://www.agu.org/pubs/crossref/1997/97GL01718.shtml. 
  64. ↑ Taylor, G.J. (17 July 1998). "The Biggest Hole in the Solar System". Planetary Science Research Discoveries, Hawai'i Institute of Geophysics and Planetology. Retrieved 12 April 2007.
  65. ↑ Schultz, P. H. (03/1997). "Forming the south-pole Aitken basin – The extreme games". Conference Paper, 28th Annual Lunar and Planetary Science Conference 28: 1259. 
  66. ↑ Wieczorek, M. et al. (2006). "The constitution and structure of the lunar interior". Reviews in Mineralogy and Geochemistry 60 (1): 221–364. doi:10.2138/rmg.2006.60.3. 
  67. ↑ 67.0 67.1 67.2 67.3 67.4 "Moon, In: Wikipedia". San Francisco, California: Wikimedia Foundation, Inc. September 28, 2012. Retrieved 2012-09-26. Cite error: Invalid <ref> tag; name "Moon" defined multiple times with different content
  68. ↑ 68.0 68.1 Staff13 (May 28, 2013). "Unusual minerals in moon craters may have been delivered from space". New York: United Press International. Retrieved 2013-06-01.
  69. ↑ Jay Melosh (May 28, 2013). "Unusual minerals in moon craters may have been delivered from space". New York: United Press International. Retrieved 2013-06-01.
  70. ↑ U. B. Marvin (1983). "The discovery and initial characterization of Allan Hills 81005: The first lunar meteorite". Geophys. Res. Lett. 10: 775–8. doi:10.1029/GL010i009p00775. 
  71. ↑ McSween Jr., Harry Y. (1976). "A new type of chondritic meteorite found in lunar soil". Earth and Planetary Science Letters 31 (2): 193–9. doi:10.1016/0012-821X(76)90211-9. 
  72. ↑ Rubin, Alan E. (1997). "The Hadley Rille enstatite chondrite and its agglutinate-like rim: Impact melting during accretion to the Moon". Meteoritics & Planetary Science 32 (1): 135–41. doi:10.1111/j.1945-5100.1997.tb01248.x. 
  73. ↑ Goresy, Ahmed El; Dera, Przemyslaw; Sharp, Thomas G.; Prewitt, Charles T.; Chen, Ming; Dubrovinsky, Leonid; Wopenka, Brigitte; Boctor, Nabil Z. et al. (2008). "Seifertite, a dense orthorhombic polymorph of silica from the Martian meteorites Shergotty and Zagami". European Journal of Mineralogy 20 (4): 523 \pdf=http://www.schweizerbart.de/resources/downloads/paper_previews/58172.pdf.+doi:10.1127/0935-1221/2008/0020-1812. 
  74. ↑ Dera P; Prewitt C T; Boctor N Z; Hemley R J (2002). "Characterization of a high-pressure phase of silica from the Martian meteorite Shergotty". American Mineralogist 87: 1018. http://rruff.geo.arizona.edu/AMS/authors/Boctor%20N%20Z. 
  75. ↑ H. Chennaoui Aoudjehane; A. Jambon (2008). "First evidence of high-pressure silica: stishovite and seifertite in lunar meteorite Northwest Africa 4734". Meteoritics & Planetary Science 43 (7, Supplement): A32. http://www.uair.arizona.edu/objectviewer?o=uadc%3A%2F%2Fazu_maps%2FVolume43%2FNumberSupplement%2Fea83b7e4-bcbb-44c2-af9e-a14b6d5ebdd4. 
  76. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named Seifertite
  77. ↑ Lloyd D. Graham (Summer 2010). "The Seven Seals of Revelation and the Seven Classical Planets". The Esoteric Quarterly 6: 45-58. http://scholar.googleusercontent.com/scholar?q=cache:i0aRQgg7xGAJ:scholar.google.com/+%22classical+planets%22&hl=en&as_sdt=0,3. Retrieved 2012-05-21. 
  78. ↑ Jean Baptiste Joseph Delambre (1817). Histoire de l'astronomie ancienne. Paris: Courcier. pp. 639. http://books.google.com/books?id=2lVUjJSxjhQC&pg=PR3&source=gbs_selected_pages&cad=3#v=onepage&f=false. Retrieved 2012-01-13. 
  79. ↑ A. Aaboe; J. P. Britton; J. A. Henderson; Otto Neugebauer; A. J. Sachs (1991). "Saros Cycle Dates and Related Babylonian Astronomical Texts". Transactions of the American Philosophical Society (American Philosophical Society) 81 (6): 1–75. doi:10.2307/1006543. "One comprises what we have called "Saros Cycle Texts," which give the months of eclipse possibilities arranged in consistent cycles of 223 months (or 18 years)." 
  80. ↑ K. V. Sarma (2008). "Astronomy in India". In Helaine Selin. Encyclopaedia of the History of Science, Technology, and Medicine in Non-Western Cultures (2 ed.). Springer. pp. 317–321. ISBN 978-1-4020-4559-2. 
  81. ↑ 81.0 81.1 81.2 Needham, Joseph (1986). Science and Civilization in China, Volume III: Mathematics and the Sciences of the Heavens and Earth. Taipei: Caves Books. ISBN 0-521-05801-5. http://books.google.com/books?id=jfQ9E0u4pLAC. 
  82. ↑ O'Connor, J.J.; Robertson, E.F. (February 1999). "Anaxagoras of Clazomenae". University of St Andrews. Retrieved 12 April 2007.
  83. ↑ Jules Cashford (April 17, 2003). The Moon: Myth and Image. Basic Books. pp. 400. ISBN 156858265X. http://books.google.com/books?id=Kpfwhg1hE6QC&lr=&source=gbs_navlinks_s. Retrieved 2013-01-10. 

Further reading[edit | edit source]

  • Moon, World Book at NASA, 30 November 2007

External links[edit | edit source]

{{Astronomy resources}}


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