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Observation of Venus October 2005 - ANU 40" Telescope
Venus Observations
ANU 40" Telescope
Siding Spring

  Even to this day, the exact age of the Earth is not known exactly. One of the primary reasons for this, is that all of the original surface has recycled and destroyed by the process of 'plate tectonics'. Ancient rocks dating to 3.5 billion years have been recovered from various locations worldwide, with some examples discovered in Western Australia - dated to 3.4 - 3.6 billion years. The oldest rocks thus found so far was recovered the Acasta Gneisses in northwestern Canada near Great Slave Lake - dated to 4.03 billion years. These rocks are dated by a number of radiometric dating methods and the consistency of the results give scientists confidence that the ages are correct to within a few percent.

  During the missions to the moon, a number

of Lunar rocks were returned - by using the same dating process, the oldest dated sample provided a window of 4.4 to 4.5 billions years. The benefit of samples from our nearest neigbour is that they have not been subjected to plate tectonic  movement. This provides a solid case for dating the moon to 4.5 billion years. The age of 4.54 billion years found for the Solar System and Earth is consistent with current calculations of 11 to 13 billion years for the age of the Milky Way Galaxy, based on the stage of evolution of globular cluster stars, and the age of 10 to 15 billion years for the age of the Universe, based on the recession of distant galaxies.

(Dalrymple, Brent, 1991, The Age of the Earth: Stanford, Calif., Stanford Uni. Press, 474 p)

  A very large number of meteoroids enter the Earth's atmosphere each day amounting to more than a hundred tons of material. But they are almost all very small, just a few milligrams each. Only the largest ones ever reach the surface to become meteorites. The largest found meteorite (Hoba, in Namibia) weighs 60 tons.

  The average meteoroid enters the atmosphere at between 10 and 70 km/sec. But all but the very largest are quickly decelerated to a few hundred km/hour by atmospheric friction and hit the Earth's surface with very little fanfare.
(Ref. Source)

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Modified Artwork
Last Remnant Of Moon Strikes Earth

  However meteoroids larger than a few hundred tons are slowed very little; only these large (and fortunately rare) ones make craters. They are listed as: Iron, Stony Iron, Chondrite, Carbonaceous Chondrite, Achondrite (Moon or Mars) a meteorite known as ALH84001 is believed to have come from Mars.

  A more recent impact occurred in 1908 in a remote uninhabited region of western Siberia known as Tunguska. The impactor was about 60 meters in diameter and probably consisting of many loosely bound pieces. In contrast to the Barringer Crater event, the Tunguska object completely disintegrated before hitting the ground and so no crater was formed. Nevertheless, all the trees were flattened in an area 50 kilometers across. The sound of the explosion was heard half-way around the world in London.

  Is there evidence that these impacts have caused 'mass extinction cycle' on our planet ?

  In the past 600 million years there have been five major mass extinction's that on average extinguished half of all species. The largest mass extinction to have affected life on Earth was the Permian-Triassic one that ended the Permian period 250 million years ago and killed off 90% of all species.

Paul Wiegert

Earth coorbital asteroid 2002 AA29

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  The last such mass extinction led to the demise of the dinosaurs and has been found to have coincided with a large asteroid impact; this is the Cretaceous-Tertiary (K-T) extinction event. There is no solid evidence of impacts leading to the four other major mass extinction's, though many scientists assume that they are at least related to impacts.

  Probably the most convincing evidence for a worldwide catastrophe was the discovery of the crater which has since been named Chicxulub Crater. This so-called smoking gun is centered on the Yucatan Peninsula of Mexico and was discovered by Tony Camargo and Glen Pentfield while working as geophysicists for the Mexican oil company PEMEX. What they reported as a circular feature later turned out to be a crater estimated to be 180 kilometers in diameter. Other researchers would later find that the end-Cretaceous extinction event that wiped out the dinosaurs had lasted for thousands of years instead of millions of years as had previously been thought. This would be the final piece of evidence that convinced the vast majority of scientists that this extinction resulted from a point event that is most probably an extra-terrestrial impact and not from increased volcanism and climate change (which would spread its main effect over a much longer time period).  (Ref. Source)

NASA

The Peekskill Meteorite, Oct. 1992

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  These mass extinction's are listed as: (1) Ordovician-Silurian extinction approx. 439 million years ago. (2)  Late Devonian extinction, 360 million years ago. (3) Permian-Triassic extinction, approx. 251 million years ago. (4) End Triassic extinction, roughly 199 million ~ 214 million years ago. (5) Cretaceous-Tertiary extinction, approx. 65 million years ago.

  Many explanations for these extinction's through likely cometary impacts have been investigated. However, as an alternative theory, I propose the possibility of a moon similar (in compostion) to Uranus's 470 kilometer Miranda once having been captured into orbit around the Earth. This small moon, once described as being designed by 'committee' (by Dr. Caroline Porco - NASA) having  been subjected to an incomplete accretion process, having run out of internal heat, that is, before all the heavy material could actually sink to the centre. A moon like this could be easily assessed suspect to easy dis-assemble-ation by a strong tidal pull.

  If a moon similar to this had been capture by the Earth, is it possible for this process (of breakup) to have happened over hundreds of millions of years, the lighter icy-rock amalgamated (composite) material falling first heavier pieces falling periodically causing known extinction cycles ?

  This site examines that possibility, looks at the planet size object that struck the Earth, its possible orbit, makeup and later debris accretion into our moon. 

  This paper is divided up into seven 'titled' topics: 1. A Fiery Encounter2. A Fateful Rendezvous3. A Celestial Visitor4. Throes Of Gravitational Tides5. Circles Of Unrest6. The Impact Extinction's /  7. A Final Requiem.

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Joint First Place Winner Of 2006 Australian Museum Eureka Award For Earth, Environment And Planetary Science

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