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The end product of correlation is a mental abstraction called the geologic column. In order to communicate the fine structure of this so-called column, it has been subdivided into smaller units. Lines are drawn on the basis of either significant changes in fossil forms or discontinuities in the rock record i. In the upper part of the geologic column, where fossils abound, these rock systems and geologic periods are the basic units of rock and time. Lumping of periods results in eras, and splitting gives rise to epochs. In both cases, a threefold division into early-middle-late is often used, although those specific words are not always applied. Similarly, many periods are split into three epochs.

Worldwide Museum of Natural History. University of Chicago Press. Bibcode : Sedim. Science in Ancient China: Researches and Reflections. Brookfiel Vermont: Ashgate Publishing Variorum series.

III, Transactions of the Royal Society of Edinburgh published Retrieved 6 September Basin and Range. New York: Farrar, Straus and Giroux. Moscow: Sovetskaya Enciklopediya.

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Bristol University. The Geologic Time Scale Elsevier B. Bibcode : Geosp Retrieved 31 December Retrieved 22 September Subcommission on Quaternary Stratigraphy.

Retrieved 15 October Retrieved 3 August Archived from the original on 6 August Earth Science Informatics. Archived from the original on 11 February Retrieved Archived from the original on 29 December Retrieved 23 December W Earth and Planetary Science Letters. Retrieved 8 October Geochimica et Cosmochimica Acta. Bibcode : GeCoA. Archived from the original on 27 September Retrieved 6 August Bibcode : Natur.

A Concise Geologic Time Scale: Contributions to Mineralogy and Petrology. Bibcode : CoMP.

Dating - Dating - Geologic column and its associated time scale: The end product of correlation is a mental abstraction called the geologic column. It is the result of integrating all the world's individual rock sequences into a single sequence. In order to communicate the fine structure of this so-called column, it has been subdivided into smaller units.

The oldest rock on Earth is the Acasta Gneissand it dates to 4. Solid Earth. Bibcode : SolE In Felix M. Gradstein; James G. Ogg; Mark D. Schmitz; abi M. Ogg eds. The geologic time scale 1st ed.

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Amsterdam: Elsevier. July Bibcode : PLoSO Geological history of Earth. Holocene present- Pliocene 2. Oligocene Late Lopingian Pennsylvanian Pridoli Furongian Ediacaran Stenian Statherian 1. Neoarchean 2.

See also: Geologic time scale. Links to related articles. Past history deep time Present Future Futures studies Far future in religion Far future in science fiction and popular culture Timeline of the far future Eternity Eternity of the world. Horology History of timekeeping devices Main types astrarium atomic quantum hourglass marine sundial sundial markup schema watch mechanical stopwatch water-based Cuckoo clock Digital clock Grandfather clock.

Chronology History. Religion Mythology. Geological time age chron eon epoch era period Geochronology Geological history of Earth. Chronological dating Chronobiology Circadian rhythms Dating methodologies in archaeology Time geography. Time measurement and standards.

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Chronometry Orders of magnitude Metrology. Ephemeris time Greenwich Mean Time Prime meridian. Absolute space and time Spacetime Chronon Continuous signal Coordinate time Cosmological decade Discrete time and continuous time Planck time Proper time Theory of relativity Time dilation Gravitational time dilation Time domain Time translation symmetry T-symmetry.

Chronological dating Geologic time scale International Commission on Stratigraphy. Galactic year Nuclear timescale Precession Sidereal time. Big History. Big History series. Periods Eras Epochs.

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Canon of Kings Lists of kings Limmu. Chinese Japanese Korean Vietnamese. Lunisolar Solar Lunar Astronomical year numbering. Deep time Geological history of Earth Geological time units.

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Chronostratigraphy Geochronology Isotope geochemistry Law of superposition Luminescence dating Samarium-neodymium dating. Amino acid racemisation Archaeomagnetic dating Dendrochronology Ice core Incremental dating Lichenometry Paleomagnetism Radiometric dating Radiocarbon Uranium-lead Potassium-argon Tephrochronology Luminescence dating Thermoluminescence dating.

Fluorine absorption Nitrogen dating Obsidian hydration Seriation Stratigraphy. Molecular clock. Atmosphere of Earth Climate Global warming Weather.

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Categories : Geologic time scales Geology timelines Geochronology Geology-related lists International Commission on Stratigraphy geologic time scale of Earth.

Hidden categories: Pages using Timeline CS1 Russian-language sources ru CS1 maint: archived copy as title Articles with short description Use dmy dates from July Articles containing Latin-language text All articles with unsourced statements Articles with unsourced statements from September Articles with unsourced statements from June Articles containing potentially dated statements from September All articles containing potentially dated statements Articles contradicting other articles Commons category link is on Wikidata Articles which contain graphical timelines.

Namespaces Article Talk. Views Read Edit View history. In other projects Wikimedia Commons. By using this site, you agree to the Terms of Use and Privacy Policy. Cenozoic [e]. Bronze Age. Current interglacial begins. Sea level flooding of Doggerland and Sundaland.

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Sahara desert forms. Neolithic agriculture. Late ' Tarantian '. Eemian interglacialLast glacial perio ending with Younger Dryas. Toba eruption. Megafauna extinction. High amplitude ka glacial cycles. Rise of Homo sapiens. Further cooling of the climate. Spread of Homo erectus. Start of Quaternary glaciations. Rise of the Pleistocene megafauna and Homo habilis. Greenland ice sheet develops. Zanclean flooding of the Mediterranean Basin.

Cooling climate. Ardipithecus in Africa. Messinian Event with hypersaline lakes in empty Mediterranean Basin. Moderate Icehouse climatepunctuated by ice ages and re-establishment of East Antarctic Ice Sheet ; Gradual separation of human and chimpanzee ancestors.

Sahelanthropus tchadensis in Africa. Warmer during middle Miocene climate optimum. Orogeny in Northern Hemisphere. Widespread forests slowly draw in massive amounts of CO 2gradually lowering the level of atmospheric CO 2 from ppmv down to around ppmv during the Miocene. Horses and mastodons diverse. Grasses become ubiquitous. Ancestor of apesincluding humans.

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Grande Coupure extinction. Start of widespread Antarctic glaciation. Major evolution and dispersal of modern types of flowering plants. Moderate, cooling climate.

Geologic Time Scale. The geologic time scale began to take shape in the s. Geologists first used relative age dating principles to chart the chronological order of rocks around the world. It wasn't until the advent of radiometric age dating techniques in the middle s that reliable numerical dates could be assigned to the previously. The following examples show how the rock layers themselves are used as a relative time scale: A diagram correlates or matches rock units from three localities within a small area by means of geologic sections compiled from results of field studies. Another diagram (K) is a composite geologic section, greatly simplified. Because of refinements in the geologic time scale and new findings by researchers, we revised it in Further revisions may be necessary as knowledge of Grand Canyon geology improves, new or improved absolute dating techniques are developed, or the geologic time scale is modified.

Archaic mammals e. Creodonts" Condylarths ", Uintatheresetc. Appearance of several "modern" mammal families. Primitive whales diversify. Orogeny of the Alps in Europe begins. Hellenic Orogeny begins in Greece and Aegean Sea.

The Azolla event decreased CO 2 levels from ppm to ppm, setting the stage for a long period of cooling. Starts with Chicxulub impact and the K-Pg extinction event. Climate tropical. Modern plants appear; Mammals diversify into a number of lineages following the extinction of the non-avian dinosaurs.

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First large mammals up to bear or small hippo size. Alpine orogeny in Europe and Asia begins. Flowering plants proliferate, along with new types of insects. Learning Activity: It's About Time. Have you ever wondered how geologic time works? This interactive classroom learning activity helps build the basic understanding of geologic time for grades Every park contains a slice of geologic time.

In this classroom resource we highlight a few parks associated with each geologic time period. Geology, Relatives, and Time. Using a simple three or four generation family tree, students will construct a relatives time tree that mimics the major divisions of the geologic time scale Precambrian, Paleozoic, Mesozoic, and Cenozoic. For Grades Explore This Park. Geologic Time. Badlands National Park, South Dakota.

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NPS photo by M. Select an analogy: Age of Earth as a Ball of String. If a piece of string an inch long about 2. A string representing all of recorded human history would be 1. And a piece of string representing the age of Earth would be 72, mileskm long. That length of string could wrap around Earth three times Dalrymple Age of Earth as a Stack of Quarters.

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A stack of 4, quarters would be more than 5, miles 8, km high. Such a stack could reach from where you are through the center of Earth and halfway to the other side Dalrymple Age of the Earth. Fundamental Geologic Principles. Absolute Age Dating Absolute age dating results in specific ages for rock units. Radiometric Age Dating.

Geologic Time Scale The geologic time scale began to take shape in the s. Scaling this large amount of time to our calendar year, each of the 12 months of the geologic calendar year represents million years 4.

Generally speaking, each year has days, so each day represents In both cases, a threefold division into early-middle-late is often used, although those specific words are not always applied.

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Similarly, many periods are split into three epochs. However, formal names that are assigned to individual epochs appear irregularly throughout the geologic time scale. Over the interval from the Paleozoic to the present, nearly 40 epochs are recognized. This interval is represented by approximately formations, discrete layers thick enough and distinctive enough in lithology to merit delineation as units of the geologic column.

Also employed in subdivision is the zone concept, in which it is the fossils in the rocks rather than the lithologic character that defines minor stratigraphic boundaries.

The basis of zone definition varies among geologists, some considering a zone to be all rocks containing a certain species usually an invertebratewhereas others focus on special fossil assemblages. The lower part of the geologic column, where fossils are very scarce, was at one time viewed in the context of two eras of time, but subsequent mapping has shown the provincial bias in such a scheme.

Consequently, the entire lower column is now considered a single unit, the Precambrian. The results of isotopic dating are now providing finer Precambrian subdivisions that have worldwide applicability. The geologic column and the relative geologic time scale are sufficiently defined to fulfill the use originally envisioned for them-providing a framework within which to tell the story of Earth history.

Mountains have been built and eroded away, seas have advanced and retreated, a myriad of life-forms has inhabited land and sea. In all these happenings the geologic column and its associated time scale spell the difference between an unordered series of isolated events and the unfolding story of a changing Earth.



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