Transcript Chapter 12

Chapter 12
Geologic Time
TIME
Relative Time
• Places events in
sequence but does
not give their actual
date of an event
Absolute Time
• Identifies the actual
date of an event
Relative Time
Law of Superposition
In a sequence of undisturbed
sedimentary rocks, the oldest rocks
will be at the bottom of the
sequence and the youngest will be
at the top
Law of Cross Cutting
An igneous rock is younger than the
rocks it has intruded, or cut across
Law of Included Fragments
States that pieces of one rock found in another
rock must be older than the rock in which
they are found
Unconformity
A place in the rock record where layers of
rock are missing.
Layers could have been deposited and then
removed
Geologic Timetable
• A summary of the major events of Earth’s
history preserved in the rock record. Fossils
are an important part of that history.
Eras, Periods, and Epochs
• Era is the longest segment of geologic time
• Periods divide Eras
• Epochs divide Periods
Different Eras in Earth History
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Archean
Proterozoic
Paleozoic
Mesozoic
Cenozoic
Archean Era
• The oldest era
• Began when Earth formed 4-5 billion yrs.
Ago
Proterozoic Era
• Began 2.5 billion yrs. Ago
• Rocks contain fossils of simple plants and
worms that lived in the oceans
• No evidence of life on land in Proterozic
Era
Paleozoic Era
• Began 570 million yrs. ago
• More abundant fossil record
• Rocks contain fossils of both land and
ocean plants and animals
Mesozoic Era
• Began 250 million yrs. Ago
• Time of Dinosaurs
Cenozoic Era
• Youngest of the Eras (we are currently in it)
• Began 65 million yrs. Ago
• Includes events like the Ice Age and the
presence of Humans
Fossils
• Any evidence of earlier life preserved in a
rock.
• Can be pones, shells, impressions of leaves
Types of Fossils
Original remains
• Actual unchanged remains of the plant or
animal are preserved.
Ex. Whole woolly mammoths that have been
found frozen
Types of Fossils
AMBER
• Hardened resin
• Example animals getting trapped in sap
from trees
(think Jurassic Park)
Types of Fossils
Replaced Remains
• The soft parts of the original animal hae
disappeared and the hard parts have been
replaced by mineral material
• EX: Petrified Wood
Types of Fossils
Mold
• Hollow depression in the rock
• Shows the original form of the object
Cast
• When new materials fill in the mold
Trace Fossils
• Are evidence of life
other than the remains
of a plant or animal
• EX: footprints,
burrows
Index or Guide Fossils
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Three Characteristics of an Index Fossil
1.
2.
3.
–
Easily recognizable
Widespread
Limited in the time that they existed
Used to identify age of rocks
Rock Correlation
• The matching of rock layers from one area
to another
• EX: volcanic eruptions
Measuring Absolute Time
• Tree Rings
• Varves
• Radioactive Decay
Tree Rings
• Counting rings can
provide time in years
(each ring is one year)
• Can also be used to
tell what weather
conditions were like
Varves
• Any sediment that shows a yearly cycle
Radioactive Decay
• Radioactive decay is when one atom
changes into a new lighter element
• Half Life – the rate at which a radio active
element decays