i can: describe methods used to assign
DESCRIPTION
Index Fossils: Fossils that are found in many places; lived for a short period of time; found in only one rock layer By comparing index fossils in various locations on Earth, it is possible to correlate (match) the relative ages of the rocks in which they appearTRANSCRIPT
I can: describe methods used to assign
Relative ages of rock layers Do Now: How are sedimentary rocks
formed? Which fossil is the index fossil From the picture below?
Index Fossils: Fossils that are found in many places; lived for a
short period of time; found in only one rock layer By comparing
index fossils in various locations on Earth, it is possible to
correlate (match) the relative ages of the rocks in which they
appear SUPERPOSITION -The bottom rock layer is the oldest and the
top layer is the youngest -Sequence of rock is a record of past
events
-Rock layers are ALWAYS laid down horizontally, until activities
change them Relative Age of rocks: (sequence)
The age of a rock layer in comparison to its surrounding layer
-Uses rock similarity, and fossil evidence What is Correlation?
When geologists try to match rock layers in different locations to
see if they formed at the same time. How to correlate (match) rock
layers: Similarity of rock types Matching index fossils Relative
Age of rocks: (sequence)
25 miles apart 1 2 3 4 5 6 1 2 3 4 5 I can: Explain how
unconformities
cause gaps in rock layers Do Now: What is relative age? How can you
find the relative age of rocks? Relative Age of rocks:
(sequence)
25 miles apart Are we able to match up all of the layers? 1 2 3 4 5
6 1 2 3 4 5 Why? Unconformities -gaps in the rock layers
-occur when some rock layers are missing -three types WHY DOES THIS
HAPPEN? Angular Unconformity horizontally parallel rock layers are
deposited on tilted and eroded layers 2. Disconformity Occurs
between parallel layers of sedimentary rocks that have eroded and
new layers have deposited on top 3. Nonconformity Occurs between
sedimentary rocks and metamorphic or igneous rocks When sedimentary
rock was deposited on top of eroded metamorphic or igneous rock.
What type of unconformity is it? What type of unconformity is it? I
can: determine the relative age of Rock layers
Do Now: HW-Worksheet from webpage What type of unconformity is it?
Nonconformity Sedimentary rocks Metamorphic rocks What type of
unconformity is it?
Disconformity What type of unconformity is it?
Angular Igneous Extrusions & Intrusions
When molten rock flows on the Earths surface forming an igneous
rock Intrusion: Occurs when magma squeezes between rock layers
beneath the Earths surface Folds and Faults are always younger than
the original
rock layers Fold: -bends in rock layers produced by movements of
the earths crust Faults: -breaks in the rock where rock layers have
shifted (earthquakes) UNIFORMITARIANISM: -The activities that shape
the Earth today are the same activities that occurred in the past
The present is the key to the past- James Hutton I can: identify
how absolute age Differs form relative age
Do Now: HW-take home test How is an igneous extrusion different
from an igneous intrusion Igneous extrusion is when magma reaches
the surface Igneous intrusion is when magma stays beneath the
surface Relative Age of rocks: (sequence)
The age of a rock layer in comparison to its surrounding layer
-Uses rock similarity, and fossil evidence Absolute Age of rocks:
(true age) The age of a rock layer in years -Uses radiometric
dating to determine age--radioactive decay Vocabulary Review Matter
is anything that takes up space and has mass
Atoms smallest unit of matter (stuff that matter is made of) -they
have protons, neutrons, and electrons Element specific kind of atom
with a given number of protons Vocabulary Review Matter - water
Atoms Hydrogen and Oxygen atoms
Elements Hydrogen has 1 proton Oxygen has 16 protons Isotope Same
element Different number of neutrons Absolute age of rock
layers
Radioactive decay is the natural breakdown of atoms of an element
that changes that elements atoms into a new element Example: it
takes 4.5 billion years for uranium 238 to change into lead 206
Radioactive decay is NOT AFFECTED by temperature (heat) or
pressure!
occurs at a constant rate known as half-life. HALF-LIFE: Half-life
is the rate (time) it takes for one-half of the amount of original
material to decay If we know the half-life of a radioactive
material, the age of the material can be determined by measuring
the amount of decayed material in the sample. Some radioactive
substances have a
Short half-life: Carbon 14 decays to Nitrogen 14 -Good for dating
recent organic remains (between 1,000-50,0000 yrs.) 238 206 Uranium
decays to Lead Long half-life: Uranium238 -Good for dating much
older rocks (a very long half-life) - it takes 4.6 billion years
for uranium to decay to lead Example: The amount of Carbon-14
remaining in a fossil is 0.5 grams. How old is the fossil? An equal
sample of an existing organism shows the original amount of
Carbon-14 was 2.0 grams. (2.0g _____ _____) 1.How many half-lives
did the sample undergo? 2.Multiply this by the half-life for
Carbon-14 (5,700 years) Example: The amount of Carbon-14 remaining
in a fossil is 0.5 grams. How old is the fossil? An equal sample of
an existing organism shows the original amount of Carbon-14 was 2.0
grams. (2.0g 1.0g 0.5g) 1.How many half-lives did the sample
undergo?2 half-lives 2.Multiply this by the half-life for Carbon-14
Answer: 2 x 5,750 = 11,500 yrs.