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.

Near Earth Asteroids

Filed under: Asteroids — admin @ 5:05 am

Near Earth Asteroids Asteroids are rocky and metallic objects that orbit the Sun but are too small to be considered planets. They are known as minor planets. Asteroids range in size from Ceres, which has a diameter of about 1,000 kilometers, down to the size of pebbles. Sixteen asteroids have a diameter of 240 kilometers or greater. They have been found inside Earth’s orbit to beyond Saturn’s orbit. Most, however, are contained within a main belt that exists between the orbits of Mars and Jupiter. Some have orbits that cross Earth’s path and some have even hit the Earth in times past. One of the best preserved examples is Barringer Meteor Crater near Winslow, Arizona.
Asteroid Belt Asteroids are material left over from the formation of the solar system. One theory suggests that they are the remains of a planet that was destroyed in a massive collision long ago. More likely, asteroids are material that never coalesced into a planet. In fact, if the estimated total mass of all asteroids was gathered into a single object, the object would be less than 1,500 kilometers across — less than half the diameter of our Moon.

Much of our understanding about asteroids comes from examining pieces of space debris that fall to the surface of Earth. Asteroids that are on a collision course with Earth are called meteoroids. When a meteoroid strikes our atmosphere at high velocity, friction causes this chunk of space matter to incinerate in a streak of light known as a meteor. If the meteoroid does not burn up completely, what’s left strikes Earth’s surface and is called a meteorite.

Of all the meteorites examined, 92.8 percent are composed of silicate (stone), and 5.7 percent are composed of iron and nickel; the rest are a mixture of the three materials. Stony meteorites are the hardest to identify since they look very much like terrestrial rocks.

Because asteroids are material from the very early solar system, scientists are interested in their composition. Spacecraft that have flown through the asteroid belt have found that the belt is really quite empty and that asteroids are separated by very large distances. The Galileo spacecraft recently made close encounters with asteroids 951 Gaspra and 243 Ida.

Selected Asteroids

The following pages contain information on several asteroids that have been studied during the last few years. The Galileo spacecraft flew past Gaspra in October 1991 and Ida in August 1993. During these encounters, high resolution images were obtained. Astronomers studied Toutatis and Geographos using Earth-based radar observations during close approaches to the Earth. Scientists generated computer models of Castalia using date acquired from radar/radio telescopes. Vesta was observed by the Hubble Space Telescope.


Asteroid Gaspra Gaspra

Asteroid Ida Ida

Asteroid Toutatis Toutatis

Asteroid Castalia Castalia

Asteroid Vesta Vesta

Asteroid Geographos Geographos
Asteroid Summary


Number Name Radius (km) Distance* (10^6 km) Albedo Discoverer Date
1 Ceres 457 413.9 0.10 G. Piazzi 1801
511 Davida 168 475.4 0.05 R. Dugan 1903
15 Eunomia 136 395.5 0.19 De Gasparis 1851
52 Europa 156 463.3 0.06 Goldschmidt 1858
10 Hygiea 215 470.3 0.08 De Gasparis 1849
704 Interamnia 167 458.1 0.06 V. Cerulli 1910
2 Pallas 261 414.5 0.14 H. Olbers 1802
16 Psyche 132 437.1 0.10 De Gasparis 1852
87 Sylvia 136 521.5 0.04 N. Pogson 1866
4 Vesta 262.5 353.4 0.38 H. Olbers 1807
951 Gaspra 17 x 10 205.0 0.20 Neujmin 1916
243 Ida 58 x 23 270.0 ? J. Palisa 1884

* Mean distance from the Sun.

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