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Unit 6 - Geological
Unit 6 Geological Time - Sheridan Lee
Term | Definition |
---|---|
Amber | fossilized tree resin |
Fossil | the remains or impression of a prehistoric organism preserved in petrified form or as a mold or cast in rock. |
Cast | an object made by shaping molten metal or similar material in a mold |
Index Fossil | a fossil that is useful for dating and correlating the strata in which it is found. |
Mold | a distinctive and typical style, form, or character. |
Permineralization | process of fossilization in which mineral deposits form internal casts of organisms |
Trace fossil | a fossil of a footprint, trail, burrow, or other trace of an animal rather than of the animal itself. |
Cross-cutting relationships | states that an igneous intrusion is always younger than the rock it cuts across |
Geologic time | a system of chronological measurement that relates stratigraphy to time |
Lateral Continuity | states that layers of sediment initially extend laterally in all directions; in other words, they are laterally continuous |
Original horizontality | states that layers of sediment are originally deposited horizontally under the action of gravity |
Relative age | common practice for dating rocks, science of determining the relative order of past events |
Superposition | principle of quantum theory that describes a challenging concept about the nature and behavior of matter and forces at the sub-atomic level. |
Unconformity | a surface of contact between two groups of unconformable strata. |
Uniformitarianism | the theory that changes in the earth's crust during geological history have resulted from the action of continuous and uniform processes. |
Absolute Age | the true age of a rock or fossil |
Half-life | he time taken for the radioactivity of a specified isotope to fall to half its original value. |
Ice core | a core sample that is typically removed from an ice sheet |
Isotope | help determine the chemical composition and age of minerals and other geologic objects. |
Radiometric dating | any method of determining the age of earth materials or objects of organic origin based on measurement of either short-lived radioactive elements or the amount of a long-lived radioactive element plus its decay product. |
Differentiation | The geological process by which the Earth came to have its present interior structure |
Outgassing | To remove embedded gas from (a solid), as by heating or reducing the pressure |
Supercontinent | each of several large landmasses (notably Pangaea, Gondwana, and Laurasia) thought to have divided to form the present continents in the geological past. |
Pangaea | hypothetical supercontinent that included all current land masses, believed to have been in existence before the continents broke apart during the Triassic and Jurassic Periods. |
Orogeny | a process in which a section of the earth's crust is folded and deformed by lateral compression to form a mountain range. |
Evoluation | the gradual development of something, especially from a simple to a more complex form. |
Natural selection | the process by which plants and animals that can adapt to changes in their environment are able to survive and reproduce while those that cannot adapt do not survive |