Lesson 9: Stratigraphy and Geologic Time Flashcards
The tendency for rock layers to be
chronologically stacked is called the
Principle of Superposition.
Stratigraphy is the
science of using the arrangement and composition of rock layers to interpret geological history.
A large
uninterrupted sequence of rock that is made of
multiple layers that all share similar properties
(such as mineral composition and average
sediment grain size) and that all formed under
similar conditions is termed a
formation.
When
a sequence of rock changes from one formation
to another, it indicates that a large scale change
occurred in
the environment where the rocks
were being deposited
To age rocks in absolute terms, a
technique called __ is used.
radiometric dating
An isotope is a
variant of a chemical
element that has an unusual number of
neutrons
When a new rock forms, it has a ratio of
isotopes and decay products that matches that
of the environment.
. If sedimentary rocks that contain
fossils are found between two horizontally
deposited layers of igneous rocks, then dating
the igneous rocks above the sedimentary layer
will tell us
what age the fossils must be older
than, and dating the igneous rocks below the
sedimentary layer will tell us what age the
fossils must be younger than
The geologic time scale is a
standardized series of
chronological divisions that parses the Earth’s
history into discrete named units.
The largest
units in the time scale are __, followed by __, __, and __.
Eons, Eras, Periods, and Epochs
THE HADEAN EON
4.6 TO 4 BILLION YEARS AGO
THE ARCHEAN EON
4 TO 2.5 BILLION YEARS AGO The oldest known fossils come from the THE ARCHEAN EON (cyanobacteria age)
The Paleozoic Era
541 to 252 million years ago. At the start of the Paleozoic, animal life was restricted to primitive invertebrates living in the oceans, but, by its close, great forests covered
the land and teamed with reptiles, amphibians,
and insects
THE PROTEROZOIC EON
2.5 BILLION TO 541 MILLION YEARS AGO. At approximately 1.7 billion years ago, the first
multicellular organisms evolved.
Within the Proterozoic, the time span
from
630 to 542 million years ago is known as
the Ediacaran Period. During the Ediacaran,
large forms of life with some harder parts
evolved, including the first animal life.