Geological Time Scale Flashcards
(117 cards)
How old is the earth?
Approximately 4.6 billion years old (approx. 1/3 age of the universe)
Clues to earth’s past
Rocks of crust
The theory that changes in the earth’s crust during geological history have resulted from the action of continuous and uniform processes.
Uniformitarianism
Father of modern geology
James Hutton
Determining chronology of events in the history of earth using evidences such as evolution in sedimentary rocks accumulated to layers thru time
Geologic dating
Determine the exact age of an artifact or site (quantitative), works better for igneous and metamorphic rocks,
Absolute dating
Methods: Biostratigraphy, stratigraphy, and cross dating thermoluminescence
Absolute dating
Determines which object is older, Works better for sedimentary rocks, Know order of events but not date
Relative Dating
This method of relative dating works better with sedimentary rocks
Stratigraphy
Rock layers form in a horizontal position
Original horizontality
Made fundamental contributions to 4 branches of science, founder of the study of fossils and one of the main founders of geology
Nicholas Steno
Rock layers in the bottom are older than those on top of them
Superposition
Rock layers are extended laterally and continuously Similar layers of rock or sediment that are separated by a valley or other erosional feature were once continuous.
Lateral continuity
Rock layers
that are cut across are older than the cut
itself
Cross-cutting relations
Any inclusion in rock layers are older than the rock that contains it
Inclusion
Remains of Ancient Plants and Animals, Evidence of Life. A preserved remnant, remains, or impression of a prehistoric organism. At least 10000 years. Important in studying the history of the
earth
Fossil
Commonly preserved fossils (hard parts of organisms)
Bones, shells, hard parts of insects, woody material
Rarely preserved (easily decayed parts of organisms)
Internal organs, skin, hair, feathers
Kind of fossil that can be seen through a microscope such as bacteria and pollen
Micro fossil
Kind of fossils that are large, hard part of tree or dinosaur bone
Macro fossil
Formed when materials replace the structure of the organism
Petrification
Formed due to burial of plants or plant parts in sediments, formed by imprint
Compression
Preservation of original skeletons and soft body parts. (like an amber resin)
Preserved remains
Fossils of the actual animal or actual part, formed when the tissues of animals didn’t decay over the years
True fossil