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L.O: EARTH’S HISTORY
EARTH’S EARLY ATMOSPHERE
FORMED FROM OUT GASSING OF
VOLCANOES.
Geologists have sequenced the
geologic events in past to develop a
geologic history of Earth.
Scientists use relative age and
absolute age to determine age of
fossils.
Relative age: the age of a fossil, rock
or geological event in comparison to
another.
absolute age: the real age of a
fossil.
Index fossils: fossils used to
determine relative age of other
fossils, rocks and events.
a good Index fossil: wide-spread &
lived short time period
Volcanic ash also is a good time
marker. Like index fossils wide-
spread. Short time period.
Now complete page 102-113
Radioactive
decay:
Radioactive elements:
• Radioactive element decay.
• The amount of time it takes for half of a
radioactive element to decay is half-life.
• The half-life of an element cannot be changed.
• The half-life of carbon 14 is 5,700 years.
• The half-life of uranium 238 is 4.5 billion
years.
Carbon 14
• Half-life 5,700
• Used to date recent fossils-less than 50,000
years.
Uranium 238
• Halflife 4,500,000,000 years.
• Uranium’s half life is how we know earth’s
age.
Complete page 1-7

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Review#9 earth's history