How do we know the Age of the Earth?
The Earth is a constantly changing planet. Its crust is continually
being created, modified, and destroyed. As a result, rocks that
record its earliest history have not been found and probably no
longer exist. Nevertheless, there is substantial evidence that the
Earth and the other bodies of the Solar System are 4.5-4.6 billion
years old, and that the Milky Way Galaxy and the Universe are older
still. The principal evidence for the antiquity of Earth and its
cosmic surroundings is:
- The oldest rocks on Earth, found in western Greenland, have
been dated by four independent radiometric dating methods at 3.7-3.8
billion years. Rocks 3.4-3.6 billion years in age have been found
in southern Africa, western Australia, and the Great Lakes region
of North America. These oldest rocks are metamorphic rocks but
they originated as lava flows and sedimentary rocks. The debris
from which the sedimentary rocks formed must have come from even
older crustal rocks. The oldest dated minerals (4.0-4.2 billion
years) are tiny zircon crystals found in sedimentary rocks in
western Australia.
- The oldest Moon rocks are from the lunar highlands and were
formed when the early lunar crust was partially or entirely molten.
These rocks, of which only a few were returned by the Apollo missions,
have been dated by two methods at between 4.4-4.5 billion years
in age.
- The majority of the 70 well-dated meteorites have ages of 4.4-4.6
billion years. These meteorites, which are fragments of asteroids
and represent some of the most primitive material in the solar
system, have been dated by 5 independent radiometric dating methods.
- The "best" age for the Earth is based on the time required for
the lead isotopes in four very old lead ores (galena) to have
evolved from the composition of lead at the time the Solar System
formed, as recorded in the Canyon Diablo iron meteorite. This
"model lead age" is 4.54 billion years.
- The evidence for the antiquity of the Earth and Solar System
is consistent with evidence for an even greater age for the Universe
and Milky Way Galaxy. a) The age of the Universe can be estimated
from the velocity and distance of galaxies as the universe expands.
The estimates range from 7 to 20 billion years, depending on whether
the expansion is constant or is slowing due to gravitational attraction.
b) The age of the Galaxy is estimated to be 14-18 billion years
from the rate of evolution of stars in globular clusters, which
are thought to be the oldest stars in the Galaxy. The age of the
elements in the Galaxy, based on the production ratios of osmium
isotopes in supernovae and the change in that ratio over time
due to radioactive decay, is 8.6-15.7 billion years. Theoretical
considerations indicate that the Galaxy formed within a billion
years of the beginning of the Universe. c) Combining the data
from a) and b), the "best, i.e., most consistent, age of the universe
is estimated to be 14-17 billion years.
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