[meteorite-list] Cold hunting?
From: Sterling K. Webb <kelly_at_meteoritecentral.com>
Date: Thu Apr 22 10:29:54 2004 Message-ID: <3F611ADE.BB3F6C52_at_bhil.com> Hi, Rob, Actually, I seem to recall that Phil Bland at the Natural History Museum in London (formerly called The British Museum and always will be in my head) did a study doing terrestial age-dating all the meteorites from several given areas, just to get the age distribution and a figure on how long meteorites survive in a surface location and to get a handle on the fall rate. Somewhere in the Meteorite List archives there's a summary article on it... As I recall, he came up with a terrestial fall rate about 2 to 2-1/2 times the MORP rate, survival times of 40,000 to 50,000 years in deserts like the Sahara, and very short survival times for chondrites in squishy Britain. About what you'd expect, in other words. Part of his figure of a fall rate only 2-1/2 times the MORP rate in his study is the assumption that the Sahara has always been as dry as it is now. The wetter the Sahara actually was, the greater the fall rate would have to be to produce the existing survivor stones. I scrounged around and found a great deal of substantial geological research done in the Sahara before World War II, when there was much freer access to the area. First, there are extensive surface traces of former waterways and full riverene drainage systems still visible, enough so that fairly good maps of the "old" wet Sahara can be drawn. Then, there has been considerable research on the "buried" rivers of the Sahara, where the water still flows, but hundreds of feet under the surface. These buried rivers connect existing oasises and the pattern of their interconnection can be determined by a comparison of the dozens of species of fish that are found only in the buried rivers! Now, that must have been interesting research, going fishing in the Sahara! Amazingly, it turns out that the buried rivers of the Sahara are (or were) apparently connected to or with similiar buried rivers in the Middle East and northern East Africa in geologically recent time. (None of the fish are blind fish as you find in cave ecosystems.) Then, there's the neolithic art (12,000 to 16,000 years old) in the depths of the Sahara, showing hunting scenes with a plentitude of game animals that are now only found many hundreds of miles south of the Sahara. I was going to send all these references to Dr. Bland but I got lazy (or stayed lazy) and never did it. Anyway, the point being that more rocks have to fall on a wet Sahara to produce the existing age distribution than on an eternally dry Sahara. About twice as many, a fall rate of 4 to 5 times the MORP rate, because the Sahara wasn't ever soaking wet. It was sort of like Nebraska, but without the winters. I wonder if there isn't some way of factoring out the "finder's percentage" and deriving not just a minimum fall rate but the actual fall rate from such an area collection? Sterling K. Webb -------------------------------------------------------- "Matson, Robert" wrote: > Yes -- the MORP study rate is definitely too low. If there's > a researcher out there that would be interested in terrestrial > age-dating a representative sampling of my finds, we could > place a nice lower bound on the annual fall rate. > > > > --Rob > > Received on Thu 11 Sep 2003 09:01:18 PM PDT |
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