| Photos #10 and #11 are the same rock. (When I picked it up to turn it over, I was delighted to see that it had been split in half. I was sure I'd be able to spot some gold veins but nothing doing!) Anyway, look at how pretty this jewel is! |
| This (almost) perfectly flat rock makes a great tool for placing hot cookware on. That way, we don't burn the table. It has a double function, too. Heat it up on the burner and viola! An instant toaster! A common Red stone. Volcanic in origin, loaded with Iron. |
| A hand held meat tenderizer without clumsy handles. It fits perfectly in my palm and takes up no precious space at all. Granite cobblestone. Used in making streets in ancient times and right down to the 1890’s. |
| Photo #1 I thought I would take a crack at guessing the rocks. This is a rock..Yup you got that right, clearly a former sand stone which has gone through Metamorphoses….Ugly compacting under pressure and heat. Then the ocean got a crack at it. Two layers of material indicate the darker layer was a silt stone mud stone of fine particles perhaps millions of years old. And the lighter colored sand stone..not the black and brown intrusions on layers, means that the tides depositing the layers were sometimes lower or higher over several years, perhaps thousands of years. The particles in the rock appear micro-sized…Check by rubbing both sides on a hard piece of sand paper. It will help you determine the particle sizes. |
| Photo #2 It is a metamorphic rock composed of a dark material perhaps fine clay materials from a silt deposit…note blue-gray color, and compressed with an intrusion of Potassium enriched feldspar that was truly crushed into something approaching marble. Also the beach pebbles an rocks show the kind of wear associated with many years of exposure. There are several rocks near with brown translucent appearance which are interesting. Cross between Paleocene and other elements. Think of hard clear or translucent chert. |
| Photo #3 This one is really hard to describe. First it has black rock, black intrusive colored quartz or feldspar. It is hard to read. The lighter colored rock is from a series of layers of limestone..very old and metamorphic. The quartz were intrusive, that is filled in between cracks in the original layers, and eventually became part of a larger rock formation which eventually broke off and was washed in with the tide. If you looked at the shore line, the beach area, and saw pink rock formations with white and dark green materials you would be looking at sever hundred million years of rock formation. Despite the young age of the interior mountains in Mexico and central America, the coastal plane is older. Subduction of the Pacific Plate is pushing up mountains in Mexico and California, but not the coastline. The Pacific plate is sliding under the continental shelf in a diagonal push along the San Andreas Fault. Then other faults, in Nevada, and the Rocky mountains are the result of earlier platonic activity. And the faults in Mexico are still very active. Volcanic activity is a sign of that pressure building under the NA Plate. |
| Photo #5 Interesting. You can’t fool me. That is a Pizza stain on a perfectly good rock. Or did you hit someone with this one from your sling? Seriously.. I have no idea what the red stuff is. The rest is the black and white of a quartz enriched granite type rock. The black stuff is probably hornsfels or Hornblende. It isn’t poisonous….But the red stuff is interesting.. It might be the last part of a layer of red stone washed away from the larger rock. |
| Photo #4 Red stone is typical of an Iron rich granite rock. The red is Iron. The Quartz appearing rock looks like quartz, irregular rounded shapes with poor cleavage, but like all rocks, time and pressure along with exposure to rain and pollution from the air, and the rock changes. But the RED Stuff is pretty much found everywhere including Connecticut, and northern Maine. PEI in Canada, has the deepest red dirt I’ve ever seen. |
| Photo #7 I'm getting tired of this. A rock is a rock is a rock. : ) |
| Photo #6 You are looking at the top of a rock with many layers of rock, strata, almost perfectly aligned. It is beautiful. The purple colors might be any number of chemicals combined to make the color. The reddish yellow is iron. The blue color Beryl like, but it could be any number of elements. What is really beautiful is the symmetry. The hornblende…the dark colored layers and the quartz laden strata indicate a very old rock. Several metamorphic changes, from a shore or lake bed deposits to going down into the ocean several miles to be pressured into a hardened rock, and with some exceptional heading. The gloss is really beautiful. It would make a great hollowed out ashtray. (Bad Joke) |
| Photo #11 WOW!! This is exciting! The rock is pink in color on the outside, but dark blue-gray on the inside. It is most likely a form of CHERT.. Or similar material. If you still have the rock, take a hammer and smack it good on the side. If it breaks out in a conical form, convex on the main rock, concave on the split peace, it is definitely in that form. That is metamorphic with direct highly intense heat and pressure changing the stone from quatz-felspar to something akin to arrow head material. If it is very hard, it has moved into a dark marble quality.. If you hit it with a hammer and it takes several good smacks to break it off, then the rock is very hard.. 7 to 8 on the mole scale with diamonds at the highest level. I have a few pieces like this from Nevada. Sorry no gold. |
| Photo #10 Notice the white bands of rock in photo #10. If the crystals have clearly marked flat sections, so you can actually see them as separate layers, then it’s really Feldspar. But, Quartz and Feldspars make up about 60% of the world’s rock minerals. The reddish complexion of the exterior rock shows how Iron in the rock, taking on the H2O becomes oxidized. And, iron in the quartz and feldspar acquire iron in their crystals…Pink and Red Quartz, Rose Quartz etc reflect this. Also it helps break down the rock when it gets into salt water..A natural source of chemical intrusion, weakening the crystals and allowing for predominant Iron to bond. |
| Photo #10 |
| Photo #11 |
| Uncle Jim responded to the 'Name That Rock' challenge. Here are his amazingly detailed and expert comments with just these photos to work from. Thanks for all the hard work Jim! ( Jim's responses are in red ) |