Frequently AskedAstronomy


Astronomers have at last found definitive evidence that the universe's first dust - the celestial stuff that seeded future generations of stars and planets - was forged in the explosions of massive stars.

The findings, made with NASA's Spitzer Space Telescope, are the most significant clue yet in the longstanding mystery of where the dust in our very young universe came from. Scientists had suspected that exploding stars, or supernovae, were the primary source, but nobody had been able to demonstrate that they can create copious amounts of dust - until now. Spitzer's sensitive infrared detectors have found 10,000 Earth masses worth of dust in the blown-out remains of the well-known supernova remnant Cassiopeia A.

Space dust is everywhere in the cosmos, in our own neck of the universe and all the way back billions of light-years away in our infant universe. Developing stars need dust to cool down enough to collapse and ignite, while planets and living creatures consist of the powdery substance. In our nearby universe, dust is pumped out by dying stars like our sun. But back when the universe was young, sun-like stars hadn't been around long enough to die and leave dust.

That's where supernovae come in. These violent explosions occur when the most massive stars in the universe die. Because massive stars don't live very long, theorists reasoned that the very first exploding massive stars could be the suppliers of the unaccounted-for dust. These first stars, called Population III, are the only stars that formed without any dust.

Deimos Moons of Mars

Filed under: Mars — admin @ 7:35 pm

Deimos Moons of Mars Deimos [DEE-mos] (panic) is a moon of Mars and was named after an attendant of the Roman war god Mars. Deimos is a dark body that appears to be composed of C-type surface materials. It is similar to the C-type (blackish carbonaceous chondrite) asteroids that exist in the outer asteroid belt. Some scientists speculate that Deimos and Phobos (the other martian moon), are captured asteroids; however, other scientists present arguments counter to this theory. Both Deimos and Phobos are saturated with craters. Deimos has a smoother appearance caused by partial filling of some of its craters. Asaph Hall discovered Deimos in 1877.

Deimos Statistics

Characteristic Measurement

Mass (kg)

1.8e+15

Mass (Earth = 1)

3.0120e-10

Radius (km)

7.5×6.1×5.5

Radius (Earth = 1)

1.1759e-03

Mean density (gm/cm^3)

1.7

Mean distance from Mars (km)

23,460

Rotational period (days)

1.26244

Orbital period (days)

1.26244

Mean orbital velocity (km/sec)

1.36

Orbital eccentricity

0.00

Orbital inclination

0.9-2.7°

Escape Velocity (km/sec)

0.0057

Visual geometric albedo

0.07

Magnitude (Vo)

12.40

Views of Deimos

Mosaic of Deimos

Mosaic of Deimos Measuring 16 by 12 kilometers, Deimos circles Mars every 30 hours. Craters of varying age dot its surface, which is somewhat smoother than the surface of Phobos.

Deimos

Deimos This image was taken by the Viking Orbiter spacecraft in 1977.

Deimos

Deimos This image shows a slightly different view of Deimos. It was acquired by the Viking Orbiter spacecraft.

Map of Deimos

Map of Deimos This image is a photomosaic of Deimos, the outer satellite of Mars. The leading side faces forwards in the orbit of Deimos. The trailing side faces backwards along the orbit. Longitude 0 is at the blunter end with the most prominent craters, and faces Mars. As with all conformal (true shape) projections, the scale in these maps varies, increasing from the center to the outer edge.

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