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Geological time
| Term | Definition |
|---|---|
| Cast | a fossil copy of an organism made when a mold of the organism is filled with sediment or mineral deposits |
| Mold | A fossil formed when an organism buried in sediment dissolves, leaving a hollow area. |
| Petrification | The process by which organic material is turned into stone. |
| Carbonization | Process of fossilization wherein the original organic material in a fossil has been reduced to a film of carbon looking like a black drawing |
| Fossil Resin (Amber) | Sticky residue captures insects and other invertebrates |
| Tar fossilization | organism was trapped in a tar pit and the remains fossilized |
| Ice fossilization | organism was covered in ice and the remains were fossilized |
| Replacement (petrification) | remains dissolve and are replaced with minerals |
| Permineralization | occurs when minerals carried by water are deposited around a hard structure |
| Trace fossil | A type of fossil that provides evidence of the activities of ancient organisms |
| Geological Time Scale (GTS) | the categories of time into which Earth's history is usually divided by geologists and paleontologists: eons, eras, periods, epochs |
| Fossil record | information about past life, including the structure of organisms, what they ate, what ate them, in what environment they lived, and the order in which they lived |
| Index fossil | fossils of widely distributed organisms that lived during only one short period |
| Law of Superposition | The geologic principle that states that in horizontal layers of sedimentary rock, each layer is older than the layer above it and younger than the layer below it. |
| Law of Cross Cutting | Any feature that cuts across a rock or body of sediment must be younger than the rock or sediment that it cuts across |
| Absolute age dating | uses radioactive decay to determine an exact age |
| Relative age dating | uses fossils and stratigraphic laws to determine the relative ages of rock strata. |
| Paleontologist | A scientist who studies fossils to learn about organisms that lived long ago |
| Sedimentary rock | a rock that forms from compressed or cemented layers of sediment |
| Era | a long and distinct period of history with a particular feature or characteristic. |
| Eon | the largest division of geologic time |
| Period | (GTS) This is the basic unit of geologic time. A Period lasts tens of millions of years, which is the time it takes to form one type of rock system. |
| Fossilization process | 1. Death, 2. Decay, 3. Burial, 4. Fossilization, 5. Erosion/exposure |
| Law of Inclusions | Pieces of rock found in other layers are always older. |