how is a geode split opened?
106341
very carefully... use an awl and hammer
809157
You can use Acronis Disk Director in order to split your D: partition.
468141
Microsoft discontinued the Map tool with Excel 2002 (Office XP) ... they have no means for opening earlier files containing Maps.\n\n*** Edit ***\nTry Microsoft MapPoint - it integrates with MS Office.  Might be a little pricey depending on how much you're going to use it.
1005698
*chuckles* Those lines are not really there, they are simply light reflecting off the surface of the CD's layers. But there are other lines that spiral outward from the center that strore billions of 1s and 0s (called binary) that are read and decoded by the computer.\n\n1  0  0  1  0    -> 1  0  0  1  0  -> 9\n1  2  4  8 16   -> 1+0+0+8+0 -> 9
525608
i've a faint remembering of a DOS program i used long ago to split files for copying on floppy disks. It's name was split.exe\n\ni got it, it's available here (chapter Another Solution: Split.exe) but you can only split files on floppies and back.\nhttp://www.byte.com/documents/s=122/byt19990816s0007/index.htm
757089
math b consists of geome
994724
My freind Kyle knows how to do this. He had his own at one point.  But he isnt online right now. Im really sorry.. but if you keep this question open for a bit I can get back to you on this. \n\nHe just came online.. and im really sorry but he says it's very hard to explain! I really wish I could help though :(
792270
Hi I assume you mean an unsymmetrical item. I also assume you want a best fit. I have done similar things on a computer but not by hand. The computer finds three point most distant from the centroid and uses these points as pivots for three orthogonal planes. Not sure of the rest.
185652
since your ddoing coordinate geometry you should at least tell what shape you're trying to get.\nI'm assuming it's a parallelogram so u should make it (1,8)
35315
carbonates gives a good answer - and as he says the most used tool for determining the cross-sectional structure of the Earth is seismic information recorded from earthquakes. If the earthquake is of sufficient magnitude it's energy will travel right through the Earth. Measuring arrival times at various seismographs around the world allows geologists/geophyiscists to determine major boundaries within the Earth. See: http://quake.wr.usgs.gov/research/seismology/ for some good examples,explanations and related topics. More good info on this topic at: http://www.seismo.unr.edu/ftp/pub/louie/class/100/interior.html\n\n\nAnother tool used to study the interior of the Earth is the orbit of the planet. Wobbles and variations tell us about the internal distribution of mass in the planet. See http://www.geo.ucalgary.ca/~wu/Goph681/EarthRotation.pdf for an example of the mathematics involved in dealing with Earth's orbit!
731189
Yes. Shifting the binary point one position right doubles both the top and bottom.
1022457
Type O or Offset <enter>\nClick on Object to be offset <enter>\nType in distance to offset <enter>\nClick on side to offset \nGame over!!!!
72964
thats easy, just chaeck your points and click on the link. thaen look at the second chart and look at the 1st and 4th colums
382499
It's definately a compressed file that's been split up, and I *think* it was done with hjsplit http://www.freebyte.com/hjsplit/ I seem to recall it using that format. Use that program to rejoin them. If that's not it... you may need to fish around, but it's *definately* something that's been split up, with a similar program, if not that one. Find the program it was split with, and you'll have what you need to put it back together
171260
GPS system uses a mathematical model called an ellipsoid to represent the shape of the earth. \n\nThe true shape of the earth is refered to as a geoid, but not easy to measure or represent mathematically. It is the shape the earth takes due to gravitational and rotational forces as opposed to the perfect sphere and is affected locally by denser material in spots.\n\nMean sea level is the old way of measuring things taking measurements over long periods of time to find the theoretical sea level if there were no waves or tidal forces. (you don't want to calculate how far above sea level a building is and have to figure out what time of day it is for the tidal adjustment.) \n\nThese are the three ways you can measure how high up a point on the earth is. Hope that helps.
259946
It's a universal drawing file, any CAD system should be able to open it, if it's translated right. I have more luck with them than with STEP (.stp) files.
103181
I'd imagine it was because the Spotted was found only on the West coast while the Eastern was spotted only on the East coast.\n\nAs for the time, an update on a site (listed below) has someone mentioning the split in December of 2003.