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  2. Half-birthday - Wikipedia

    en.wikipedia.org/wiki/Half-birthday

    The easier but less precise method is to take the number of the date of the birthday and advance the month by six: e.g. April 20 becomes October 20. More than 75% of the time this method results in a wrong date. Months don't all have the same number of days, leap years add a day, and the second half of the year is longer than the first half.

  3. Hafnium–tungsten dating - Wikipedia

    en.wikipedia.org/wiki/Hafnium–tungsten_dating

    Hafnium–tungsten dating is a geochronological radiometric dating method utilizing the radioactive decay system of hafnium-182 to tungsten-182. [1] The half-life of the system is 8.9 ± 0.1 million years. [1] Today hafnium-182 is an extinct radionuclide, but the hafnium–tungsten radioactive system is useful in studies of the early Solar ...

  4. Geologic time scale - Wikipedia

    en.wikipedia.org/wiki/Geologic_time_scale

    The geologic time scale is a way of representing deep time based on events that have occurred throughout Earth's history, a time span of about 4.54 ± 0.05 Ga (4.54 billion years). [5] It chronologically organises strata, and subsequently time, by observing fundamental changes in stratigraphy that correspond to major geological or ...

  5. Timeline of human evolution - Wikipedia

    en.wikipedia.org/wiki/Timeline_of_human_evolution

    The timeline of human evolution outlines the major events in the evolutionary lineage of the modern human species, Homo sapiens, throughout the history of life, beginning some 4 billion years ago down to recent evolution within H. sapiens during and since the Last Glacial Period .

  6. Age of Earth - Wikipedia

    en.wikipedia.org/wiki/Age_of_Earth

    The meteorite samples, however, show a spread from 4.53 to 4.58 billion years ago. This is interpreted as the duration of formation of the solar nebula and its collapse into the solar disk to form the Sun and the planets. This 50 million year time span allows for accretion of the planets from the original solar dust and meteorites.

  7. Isotopes of hafnium - Wikipedia

    en.wikipedia.org/wiki/Isotopes_of_hafnium

    Natural hafnium ( 72 Hf) consists of five observationally stable isotopes ( 176 Hf, 177 Hf, 178 Hf, 179 Hf, and 180 Hf) and one very long-lived radioisotope, 174 Hf, with a half-life of 7.0 × 1016 years. [2] In addition, there are 34 known synthetic radioisotopes, the most stable of which is 182 Hf with a half-life of 8.9 × 106 years.

  8. Leap Day birthday math: How old would you be if you were born ...

    www.aol.com/leap-day-birthday-math-old-024548677...

    If you were born on Leap Day 1924, you would be 100 years old, or 25 in Leap Day years. The year must be evenly divisible by 4. If the year can be evenly divided by 100, it is not a leap year ...

  9. Geologic temperature record - Wikipedia

    en.wikipedia.org/wiki/Geologic_temperature_record

    Geologic temperature record. The are changes in Earth 's environment as determined from geologic evidence on multi-million to billion (10 9) year time scales. The study of past temperatures provides an important paleoenvironmental insight because it is a component of the climate and oceanography of the time.