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  1. en.wikipedia.org › wiki › PetrifactionPetrifaction - Wikipedia

    In geology, petrifaction or petrification (from Ancient Greek πέτρα (pétra) 'rock, stone') is the process by which organic material becomes a fossil through the replacement of the original material and the filling of the original pore spaces with minerals.

  2. 21 sty 2020 · Fecal fossils may be petrified, like the Mesozoic dinosaur coprolites found in any rock shop, or merely ancient specimens recovered from caves or permafrost. We may be able to deduce an animal's diet from its teeth and jaws and relatives, but if we want direct evidence, only actual samples from the animal's guts can furnish it.

  3. What Are Petrified Fossils? Petrified fossils are formed when the original organic material of a once-living organism is slowly replaced by minerals, effectively turning to stone. This occurs over an extended period of time through a process known as petrification or permineralization.

  4. • Vertebrate fossils occasionally occur in terrestrial sandstones, but are more commonly encountered in sandstones or shale produced by river floodplains, lake deposits, or mud flats. • Petrified (fossilized) wood is created by permineralization or replacement by a mineral. The

  5. 5 kwi 2021 · Petrified rock is a type of fossil known as a replacement fossil. Replacement fossils are replicas of things that were once alive, such as trees, sea creatures, or the bones of an animal. The living thing dies and is trapped in the ground.

  6. Petrified Forest National Park. Thousands of logs litter a stretch of grassland at Petrified Forest National Park in northeastern Arizona. From far away, the logs might look ordinary. But...

  7. Petrified fossils result from permineralization, the replacement of once-living matter by minerals. Solutions containing silicates, carbonates, iron or other minerals seep into the gaps and spaces between the cells, first encasing the cells and eventually replacing the cells themselves.