Lori Fenton
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I've been carrying this around for years I thought it was pretty cool I can't even remember where I found it but I'm curious to know exactly what I have
Identifying an unknown fossil specimen
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Mentor
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The topmost picture shows a rock that long ago had fractures. Over time crystals built up as water moved through the cracks.
Rocks like this are common near old volcanic vents. Cerillos Hills State Park and Rockhound State Park (both in New Mexico USA) are loaded with great rocks, some few are like what you found. Rockhound is great because you can collect anything you see there. You pay two dollars USD for park entry. You can take home what you find. My first problem was carrying the bags. Second problem: identifying the samples. Great fun.
If you live near a college or university, Geology faculty are very helpful with showing you how to figure out what you have.
Rocks like this are common near old volcanic vents. Cerillos Hills State Park and Rockhound State Park (both in New Mexico USA) are loaded with great rocks, some few are like what you found. Rockhound is great because you can collect anything you see there. You pay two dollars USD for park entry. You can take home what you find. My first problem was carrying the bags. Second problem: identifying the samples. Great fun.
If you live near a college or university, Geology faculty are very helpful with showing you how to figure out what you have.
Lori Fenton
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Sounds like great fun and good advice thank you
Sue Rich
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I think it looks like veins of some kind of metal. I'm pretty sure it's not a fossil. But it's a cool rock. I would have kept it, too.
Mark Harder
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Do you know what the matrix rock is? Metamorphic and igneous rocks do not bear fossils because they have been altered by forces that distort and destroy fossils. For example, it's common to find fossils in limestone, but I know of no fossils found in marble deposits, which are just metamorphized limestone. The dark veins don't seem to resemble a plant or animal form, unless they are one of the rather strange forms seen in some early Cambrian formations.
DinoS
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Found similar injected samples -
shores of Lake Michigan, with some sort or iron based (magnet sticks to it) metal embedded into it.
Is your rock magnetic?When an animal dies, the soft organic parts typically dissolve and decompose and are lost. There are exceptions to this under special conditions, but soft tissue fossils and things like skin imprints are very rare and typically are found only as trace fossils. Trace fossils are a shadow or a secondary discoloration of the surrounding matrix. Fossil bones occur most often in sedimentary systems. Bogs, the bottom of water channels, flowing water, etc. are the most common area; sand eventually becomes sandstone under proper conditions.
Bones are mostly calcium. The bones are enclosed in the ground and over a very long period even their “softer” parts decay and as the interior cells of the bone are replaced by waters, high in mineral content,that eventually replace the inner cellular tissue. The hard bone acts like a mold for these minerals; the hard calcium structure is like a sponge with all the voids slowly being filled with minerals and most of the time these new minerals are not the same as those of the surrounding matrix (i.e. ground) strata.
As time goes on, the bone becomes more and more rock-like and the types of tissue washing through it will differ because of differences in the environment around it; we are talking millions of years here. Eventually the entire “sponge” becomes one solid rock with all of the organic parts replaced by other minerals that stand out in color and composition from the grounds around it.
More: Fossil museum and How Stuff Works
Image of pollen organ preserved as authigenic mineralization, By Verisimilus, at Wikimedia Commons
shores of Lake Michigan, with some sort or iron based (magnet sticks to it) metal embedded into it.
Is your rock magnetic?When an animal dies, the soft organic parts typically dissolve and decompose and are lost. There are exceptions to this under special conditions, but soft tissue fossils and things like skin imprints are very rare and typically are found only as trace fossils. Trace fossils are a shadow or a secondary discoloration of the surrounding matrix. Fossil bones occur most often in sedimentary systems. Bogs, the bottom of water channels, flowing water, etc. are the most common area; sand eventually becomes sandstone under proper conditions.
Bones are mostly calcium. The bones are enclosed in the ground and over a very long period even their “softer” parts decay and as the interior cells of the bone are replaced by waters, high in mineral content,that eventually replace the inner cellular tissue. The hard bone acts like a mold for these minerals; the hard calcium structure is like a sponge with all the voids slowly being filled with minerals and most of the time these new minerals are not the same as those of the surrounding matrix (i.e. ground) strata.
As time goes on, the bone becomes more and more rock-like and the types of tissue washing through it will differ because of differences in the environment around it; we are talking millions of years here. Eventually the entire “sponge” becomes one solid rock with all of the organic parts replaced by other minerals that stand out in color and composition from the grounds around it.
More: Fossil museum and How Stuff Works
Image of pollen organ preserved as authigenic mineralization, By Verisimilus, at Wikimedia Commons
Mark Harder
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DinoS said:
Deposits of native iron - that's iron in its metallic, more-or-less pure form - is actually pretty rare, rarer even than iron-nickel meteorites. Deposits have been found in Greenland and Siberia, maybe a couple of other places on the planet. As far as I know, they're found in some variety of basalt, the heavy black rock that lava flows are made of. Your rock is definitely not basalt and I've never heard of an iron deposit near Lake Mich. What the lake does possesses is an abundance of iron smelters on its southern shores - Gary, IN in particular. It's possible that your rock is some sort of byproduct of the industry, perhaps iron embedded in slag.