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Wayback Machine
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Organization:Archive Team
Formed in 2009, the Archive Team (not to be confused with the archive.org Archive-It Team) is a rogue archivist collective dedicated to saving copies of rapidly dying or deleted websites for the sake of history and digital heritage. The group is 100% composed of volunteers and interested parties, and has expanded into a large amount of related projects for saving online and digital history.

History is littered with hundreds of conflicts over the future of a community, group, location or business that were "resolved" when one of the parties stepped ahead and destroyed what was there. With the original point of contention destroyed, the debates would fall to the wayside. Archive Team believes that by duplicated condemned data, the conversation and debate can continue, as well as the richness and insight gained by keeping the materials. Our projects have ranged in size from a single volunteer downloading the data to a small-but-critical site, to over 100 volunteers stepping forward to acquire terabytes of user-created data to save for future generations.

The main site for Archive Team is atarchiveteam.org and contains up to the date information on various projects, manifestos, plans and walkthroughs.

This collection contains the output of many Archive Team projects, both ongoing and completed. Thanks to the generous providing of disk space by the Internet Archive, multi-terabyte datasets can be made available, as well as in use by theWayback Machine, providing a path back to lost websites and work.

Our collection has grown to the point of having sub-collections for the type of data we acquire. If you are seeking to browse the contents of these collections, the Wayback Machine is the best first stop. Otherwise, you are free to dig into the stacks to see what you may find.

The Archive Team Panic Downloads are full pulldowns of currently extant websites, meant to serve as emergency backups for needed sites that are in danger of closing, or which will be missed dearly if suddenly lost due to hard drive crashes or server failures.

A collection of various Wikis throughout the internet, gathered as a last resting spot.
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The closest planet to the Sun.

Prior to 1965, astronomers believed that Mercury's sidereal rotation matched its orbital period of 88 days (synchronousrotation). This belief was reinforced by the chance coincidence of six 58.65-day rotation periods (352 days) closelymatching the synodic period of Mercury's maximum elongation (350 days). Therefore, observers saw the same features at everyopportunity for several years in a row. However, in 1965, G. Pettengill and R. Byce bounced radar signals off the planetusing the 300-meter Arecibo Radio Observatory in Puerto Rico and discovered a rotation rate of 59 days, proving that Mercurywas actually in a 3:2 resonance such that Mercury's day is exactly 2/3 of its 88-day year.

Mercury has been visited by only one spacecraft. Mariner 10 flew by three times in 1974-1975. Unfortunately, the orbitalgeometry was such that Mariner 10 photographed the same face all three times.

Because of torques from theSun, Mercury advances itsperihelion at a rate of 5,600 arcseconds percentury. According to observations, there was an extra 43 arcseconds per century which could not be accounted for. This discrepancy was resolved in 1915, when the theory ofgeneral relativityEric Weisstein's World of Physics predicted an additionalperihelion precession of exactly 43 arcseconds per year.

Because of its proximity to theSun, Mercury has 700 K days, while temperatures on its night side are a frigid100 K. Mercury has a heavily cratered surface. Kuiper, the largest crater, is 60 km across, and crater Copley hasbright rays which extend for 400 km. Scarps also abound on Mercury, the largest being Discovery Rupes (550 km long). Although Mercury has plains such as Tir and Odin, it has peculiar hilly terrain on the side of the planet opposite theCaloris Basin, where a largemeteorite is assumed to have impacted. Mercury has no atmosphere, no moons, and amagnetic field only times as strong as Earth's. Its crust and mantle are thought to be composed ofsilicates, and its core is thought to be nickel-iron. Mercury is twice as iron-rich as any other planet.

Sladeet al.(1992) detected permanently shaded ice at the poles of Mercury using synthesis imaging of transmitted radar.This discovery was completely unexpected, but subsequent thermal modelling shows that it is indeed possible for ice topersist stably for billions of years in the shaded portion of craters near the poles.

Mercury transits (passes in front of theSun as seen from theEarth) 5-7 times every 46 years. Thetransits occur during daylight hours around November 10 or May 9 in the following years (where * indicates a Maytransit):

1677  1690 16971707*1710
1723  17361740*17431753*1756
1769 177617821786*17891799*1802
1815 1822 1832*18351845*1848
1861 1868 1878*18811891*1894
1907 1914 1924*1927 1940
19531957*1960 1970*1973 1986
19992003*2006 2016*2019 2032

The transits repeat roughly every 46 years after between 5 and 7 transits, the intervals being either 3.5, 7, 9.5 or 13 years. 145 Mercury synodic orbits equal 46 solar years plus 1.1 days. Transits of Mercury can last up to 6 hours.

Earth,Jupiter,Mars,Neptune,Pluto,Saturn,Uranus




References

Arnett, W. "The Nine Planets: Mercury."Nine Planets.

"Mercury's Cool Surprise."Sky & Telescope, pp. 35-36, Jan. 1992.

Baum, R. and Sheehan, W.In Search of Planet Vulcan: The Ghost in Newton's Clockwork Universe. New York: Plenum, 1997.

Cross, C. A. and Moore, P.The Atlas Of Mercury. New York: Crown Publishing, 1977.

Davies, M. E.et al.Atlas of Mercury. Washington, DC: NASA Scientific and Technical Information Office, 1978.

Murray, B. and Burgess, E.Flight to Mercury. New York: Columbia, 1977.

Shklovskii, I. S. and Sagan, C. "Mercury and Venus: Environmental Biology." Ch. 22 inIntelligent Life in the Universe. New York: Dell, pp. 312-325, 1966.

Slade, M. A., Butler, B. J., and Muhleman, D. O. "Mercury Radar Imaging: Evidence For Polar Ice."Science258, 635-640, 1992.

Strom, R. G. "Mercury: The Forgotten Planet."Sky & Telescope, 256-260, Sept. 1990.

Vilas, F; Chapman, C. R.; and Matthews, M. S. (Eds.).Mercury. Tucson, AZ: University of Arizona Press, 1988.

Weisstein, E. W. "Books about Mercury."http://www.ericweisstein.com/encyclopedias/books/Mercury.html.



© 1996-2007 Eric W. Weisstein





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