longcircuit wrote:Although I'm comfortable acknowledging that the January 2008 explosion may well be due to a meteor impact, I'd like to propose a test to prove it: if we have earthbound and/or orbital telescopes capable of resolutions high enough to get a good photo (or video) of the explosion site, would we be able to see not only the impact crater, but also any rays of ejecta? If so, we should be able to verify that the rays will point to the center of the crater.
Two further questions:
1. If no rays (or other evidence of impact) are present, what happens to the impact theory?
2. If rays are present that, as in the case of Tycho, do not point directly to the crater's center, what happens to the impact theory?
longcircuit
longcircuit wrote:Although I'm comfortable acknowledging that the January 2008 explosion may well be due to a meteor impact, I'd like to propose a test to prove it: if we have earthbound and/or orbital telescopes capable of resolutions high enough to get a good photo (or video) of the explosion site, would we be able to see not only the impact crater, but also any rays of ejecta? If so, we should be able to verify that the rays will point to the center of the crater.
Two further questions:
1. If no rays (or other evidence of impact) are present, what happens to the impact theory?
2. If rays are present that, as in the case of Tycho, do not point directly to the crater's center, what happens to the impact theory?
longcircuit
arc-us wrote:Hmm. Interesting. This link is from the article in the original posting. http://science.nasa.gov/headlines/y2006 ... oradic.htm.[snip .. another link]
http://science.nasa.gov/headlines/y2007 ... arbles.htm
...one can't necessarily say that all craters were made by electric discharges, or that none were made by impacts. It may well be that both processes are capable of the task. ...
The question then becomes what the defining characteristics that can be used to distinguish one from the other might be...
Cheers,
~Michael Gmirkin
webolife wrote:With you all and your great comments. Laboratory impact tests have shown that circular craters form from nearly any angle of impact.
But where is that crater?
MGmirkin wrote:I also recall there was an article or paper published a while back about someone who used to use like a rifle or something on a private beach to test impacts at varying angles (short range and long range). I recall that the implication was that circular craters were generally formed regardless of impact angle, for the most part. Unfortunately it's been a long time since I read the article and don't recall specifics, not have a link to a cite. Might look around later and see what I can find...
Cheers,
~Michael Gmirkin
One objection to the idea of an impact origin for the lunar craters was the fact that all lunar craters are round. Astronomers assumed that most meteorites would have struck the moon at oblique angles, producing elongated craters. Barringer, however, had experimented by firing rifle bullets into rocks and mud, and had discovered that a projectile arriving at an oblique angle would nevertheless make a round hole. In 1923, Barringer's 12-year-old son Richard published an article in Popular Astronomy, using his father's rifle experiments to argue for the impact origin of the lunar craters; Barringer himself repeated the arguments a short time later in the Scientific American.
Ultimately, astronomers such as A.C. Gifford were able to demonstrate that the force of an impact at astronomical speeds would result in the explosion of the meteorite. Whatever the original angle of impact, the result would be a circular crater.
In addition to the absence of any naturally occurring volcanic rock in the vicinity, he noted an abundance of finely pulveri zed silica. He also observed large quantities of meteoritic iron, in the form of globular "shale balls", scattered around the rim and surrounding plain. The surrounding soil included a random mixture of meteoritic material and ejected rocks.
[...]
Merrill also pointed to the undisturbed rock beds below the crater that proved “the force which created the crater did not come from below”.
The undisturbed rock beds below the crater contradict the standard opinion on the event that created the large pit. The report by the Meteor Crater Interactive Learning Center states: “The meteorite which made it was composed almost entirely of nickel-iron, suggesting that it may have originated in the interior of a small planet. It was 150 feet across, weighed roughly 300,000 tons, and was traveling at a speed of 28,600 miles per hour (12 kilometers per second) according to the most recent research. The explosion created by its impact was equal to 2.5 megatons of TNT, or about 150 times the force of the atomic bomb that destroyed Hiroshima”. Certainly that is not the kind of event that would leave the rock beds below the crater “undisturbed”.
[...]
One reason for believing that the crater was excavated by an electric discharge is the apparent stratification of the debris distributed by the event. A rotating, crater-producing electric arc will work down from the surface through layers of soil, spraying the material across a wide region. This could mean that the debris field would be laid down roughly in layers that reversed the strata of the surrounding terrain. So it is interesting that the Meteor Crater website confirms Barringer’s finding that “different types of rocks in the rim and on the surrounding plain appeared to have been deposited in the opposite order from their order in the underlying rock beds”.
MGmirkin wrote:(BARRINGER "METEORITE CRATER")
http://www.barringercrater.com/science/One objection to the idea of an impact origin for the lunar craters was the fact that all lunar craters are round. Astronomers assumed that most meteorites would have struck the moon at oblique angles, producing elongated craters. Barringer, however, had experimented by firing rifle bullets into rocks and mud, and had discovered that a projectile arriving at an oblique angle would nevertheless make a round hole. In 1923, Barringer's 12-year-old son Richard published an article in Popular Astronomy, using his father's rifle experiments to argue for the impact origin of the lunar craters; Barringer himself repeated the arguments a short time later in the Scientific American.
During meteor showers such as the Quadrantids or Perseids, when the Moon passes through dense streams of cometary debris, the rate of lunar flashes can go as high as one per hour. Impacts subside when the Moon exits the stream, but curiously the rate never goes to zero.
"Even when no meteor shower is active, we still see flashes," says Cooke.
These "off-shower" impacts come from a vast swarm of natural space junk littering the inner solar system. Bits of stray comet dust and chips off old asteroids pepper the Moon in small but ultimately significant numbers. Earth gets hit, too, which is why on any given night you can stand under a dark sky and see a few meteors per hour glide overhead — no meteor shower required. Over the course of a year, these random or "sporadic" impacts outnumber impacts from organized meteor showers by a ratio of approximately 2:1.
Drethon wrote:Hmm, I must be blind lately, didn't see at all this topic already existed...
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