about the weight...
so if it's not an iron meteorite (which i'm pretty sure it's not) then it
could be, as I said earlier a chondrite or stone meteorite, that would explain
the weight.
recap...and I've added these pictures of mine again for reference...
TYPES: A meteorites type typically refers to the 3 main groups of meteorites
• IRON (Nickel Iron, Octahedrite, Siderite)
Iron meteorites are very dense, 7-8 g/cm3.
• STONE (Chondrites)
Most meteorites are ordinary chondrites, and ordinary chondrites have a density half as much. Most ordinary chondrites are in the range 3.0 to 3.7 g/cm3, which is denser than most terrestrial rocks. For example, limestone (2.6 g/cm3 or less), quartzite (2.7 g/cm3), and granite (2.7-2.8 g/cm3) are all common low-density rocks. Some meteorites have low densities (<3.0 g/cm3), but such meteorites are rare among meteorites.
• STONY IRON (Pallasites & Mesosiderites)
possibilities.....
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possibly could be slag, here's some pictures of slag:
http://www.meteorites.wustl.edu/id/slag.htm
but slag has that swiss cheese thing going on..and it looks really melted but I guess it's possible...but i'm not 100% on that one..
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I don't think it's Pyrite Concretion...
pics:
http://www.bing.com/images/search?q=pyrite+concretion&FORM=HDRSC2
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I doubt it's Magnetite, not magnetic enough..
pics:
http://www.bing.com/images/search?q=magnetite&FORM=HDRSC2
and paper clips would likely stick to it
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doesn't really look like Hematite
An iron oxide mineral, hematite is commonly metallic gray, brown, or reddish in color. It is an ore of iron and can form naturally in sedimentary, igneous, or metamorphic rocks.
Pics:
http://www.bing.com/images/search?q=+Hematite&FORM=HDRSC2
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i'm going with team • STONE (Chondrites) vs. just an earth rock
let's see who wins...
pics of chondrites..(so many variations)
http://www.bing.com/images/search?q=STONE+Chondrite&FORM=HDRSC2#a
They are divided into three groups, which have different amounts of metal and different amounts of total iron:
H chondrite have High total iron and high metallic Fe (15–20% Fe-Ni metal by mass[23]), and smaller chondrules than L and LL chondrites. They are formed of bronzite, olivine, pyroxene, plagioclase, metals and sulfides and ~42% of ordinary chondrite falls belong to this group (see Meteorite fall statistics).
L chondrites have Low total iron contents (including 7–11% Fe-Ni metal by mass). ~46% of ordinary chondrite falls belong to this group, which makes them the most common type of meteorite to fall on Earth.
LL chondrites have Low total iron and Low metal contents (3–5% Fe-Ni metal by mass of which 2% is metallic Fe and they also contain bronzite, oligoclase and olivine.[18]). Only 1 in 10 ordinary chondrite falls belong to this group.
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I still don't have my hopes up too high, I'm pretty sure it's just something else...but, it's been interesting...and really educational.