Anyone old enough to remember the first manned landing on the moon will probably remember the term “mascon.” The moon is full of them, and landing the Apollo 11 spacecraft required an emergency maneuver by Neil Armstrong to avoid ending up in a pile of rocks. The landing spot in the Sea of Tranquility had been very carefully researched, and it was programmed into the automatic system responsible for getting them to a nice flat place. But for some reason the lander was headed for a very inhospitable place strewn with boulders as big as the lander! Armstrong’s last-minute diversion saved the mission.
It turned out the problem was partly caused by mass concentrations, an odd feature of the moon’s gravity. Also inputs from the two landing radars overwhelmed the lander’s computer. There are places in some of the large craters where the upwelling lava is much denser than the surrounding terrain. As you orbit the moon, these anomalies can turn your carefully calculated orbit into hash. Lunar scientists call this “bumpy gravitation” and have figured ways to overcome its effects on anything that orbits close to the surface (mostly they don’t orbit close to the surface!). In the illustration, mascons are shown in red. An exploration of mascons is here.
Although not exactly the same thing, mass concentrations are also found in places like Vatican City.
Illustration: NASA
2 comments:
Don’t you remember the famous paper in Science proving the moon is made of cheese? Your mascon features must probable be some harden whey or similar substances. I’d avoid that cow!
E.Schreiber and O.L.Anderson (1970) Properties and composition of lunar materials: Earth analogues Science 168 1579-1580
The landings of Apollo 11 and Apollo 12 on the moon sent shock waves through the moon's surface, which were detected on a seismograph. By measuring the speed of shock waves through rock (known as the seismic velocity), the density of the rock can be estimated.
The higher the seismic velocity, the denser the rock. Seismic velocities for moon "rock" were compared to those of rocks from various locations. The results were published in Science, and are shown below:
Seismic Velocities
Lunar________________Seismic Velocity (km/sec)
Basalt 10017.....................1.84
Basalt 10046.....................1.25
Near surface layer..............1.2
Terrestrial rocks_______Seismic Velocity (km/sec)
Granite...............................5.9
Gneiss................................4.9
Basalt.................................5.8
Sandstone...........................4.9
Marble................................6.02
Limestone...........................5.06-5.97
It is clear from this that moon "rock" is considerably less dense than any type of rock found on earth. The scientists then decided to examine the seismic velocities of various cheeses from around the world. Some of the results are shown below:
Cheese_______________Seismic Velocity (km/sec)
Sapsego (Swiss).................2.12
Romano (Italy)....................1.74
Cheddar (Vermont).............1.72
Muenster (Wisconsin)..........1.57
Wow, thanks Anonymous! Especially about the density of cheese!
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