click below
click below
Normal Size Small Size show me how
Earth History Review
| Term | Definition |
|---|---|
| preserved remains or traces of organisms that lived in the past | fossils |
| include teeth, bones, or shells | body fossils |
| can include footprints, burrows, or even wastes | trace fossils |
| an imprint of an organism left in rock, no organism is left | mold fossils |
| organisms that lived over a wide area & for a fairly short period of time. | index fossils |
| age in comparison with other rocks, either younger or older. | relative age |
| deeper layers must be older than layers closer to the surface | law of superposition |
| divisions in Earth history | geologic time scale |
| the time it takes for half of a given amount of an isotope to decay | half-life |
| rate of decay of can be used to estimate the absolute ages of fossils and rocks | radiometric dating |
| The best-known method of radiometric dating | carbon-14 dating |
| Most fossils are preserved in this type of rock | sedimentary rocks |
| tree sap may cover an organism and then turn into thus trapping the DNA of an organism | amber |
| the largest blocks of time on the geologic time scale are called | eons |
| You can tell how long the tree lived by counting these | tree rings |
| has a half-life of 5,730 years | Carbon-14 |