Volcanoes and Igneous Activity Earth - Chapter 4 - PowerPoint PPT Presentation

Loading...

PPT – Volcanoes and Igneous Activity Earth - Chapter 4 PowerPoint presentation | free to download - id: 8280df-MzFjY



Loading


The Adobe Flash plugin is needed to view this content

Get the plugin now

View by Category
About This Presentation
Title:

Volcanoes and Igneous Activity Earth - Chapter 4

Description:

Title: Volcanoes and Igneous Activity Earth - Chapter 4 Author: Stan & Cindy Hatfield Last modified by: Owner Created Date: 12/18/2000 12:31:17 AM – PowerPoint PPT presentation

Number of Views:39
Avg rating:3.0/5.0
Slides: 50
Provided by: Stan1168
Learn more at: http://mrsellisscience.weebly.com
Category:

less

Write a Comment
User Comments (0)
Transcript and Presenter's Notes

Title: Volcanoes and Igneous Activity Earth - Chapter 4


1
Geologic Time
2
12.1 Discovering Earths History
? Rocks record geological events and changing
life forms of the past.
? We have learned that Earth is much older than
anyone had previously imagined and that its
surface and interior have been changed by the
same geological processes that continue today.
3
Time
  • Time is measured by change
  • Age of the Earth 4.6 billion years
  • Deep time, millions billions of years, is
    difficult to comprehend
  • James Hutton (1726-1797) postulated a very old
    Earth

4
(No Transcript)
5
Geologic Time Scale
  • Age correlations using fossils are used to
    construct the geologic time column
  • Names derived from locations where rocks of that
    age are well exposed
  • Different units are separated by unconformities
    of changes in fossils
  • Originally developed from superposition of rock
    formations in Europe

6
12.1 Discovering Earths History
  • Uniformitarianism means that the forces and
    processes that we observe today have been at work
    for a very long time.
  • By studying rocks, especially sedimentary rocks,
    geologists can start to understand the past.

7
  • Sequences of rock contain gaps
  • Geologic time is continuous
  • The rock record at a given location may not
    record all of geologic time

8
12.1 Discovering Earths History
? Relative dating tells us the sequence in which
events occurred, not how long ago they occurred.
? Stratigraphy
The study of layered rocks in the Earths
crust.
9
Relative Ages
  • Rules of Stratigraphy
  • Principle of Stratigraphic Superposition
  • Law of Original Horizontality
  • Faunal Succession
  • Crosscutting Relationships
  • Inclusions

10
12.1 Discovering Earths History
? Law of Superposition
The law of superposition states that in an
undeformed sequence of sedimentary rocks, each
bed is older than the one above it and younger
than the one below it.
11
Ordering the Grand Canyons History
12
12.1 Discovering Earths History
? Principle of Original Horizontality
  • The principle of original horizontality means
    that layers of sediment are generally deposited
    in a horizontal position.
  • If you see rock layers that are flat, it means
    that they have not been disturbed and are still
    in their original position.
  • If rock layers are bent or tilted, this means
    they must have been moved into this position
    after they were deposited

13
Disturbed Rock Layers
14
Principle of Faunal Succession
  • Based on the observation that sedimentary rock
    strata contain fossilized flora and fauna (plants
    and animals) and that these succeed each other
    vertically in a specific, reliable order that can
    be identified over wide horizontal distances

15
(No Transcript)
16
12.1 Discovering Earths History
? Principle of Cross-Cutting Relationships
The principle of cross-cutting relationships
states that when a fault cuts through rock
layers, or when magma intrudes other rocks and
crystallizes, we can assume that the fault or
intrusion is younger than the rocks affected.
? Inclusions
Inclusions are rocks contained within other
rocks.
Rocks containing inclusions are younger than
the inclusions they contain.
17
Applying Cross-Cutting Relationships
Cross-cutting relationships are an important
principle used in relative dating. An intrusive
rock body is younger than the rock it intrudes.
A fault is younger than the rock layers it cuts.
18
Formation of Inclusions
This shows a mass of igneous rock formed from
magma that intruded an older rock body
Sedimentary rock layers form on top of the
weathered igneous rocks
This shows the older rock erodes and exposes the
igneous rock to weathering
19
12.1 Discovering Earths History
? Unconformities
An unconformity represents a long period
during which deposition stopped, erosion removed
previously formed rocks, and then deposition
resumed.
An angular unconformity indicates that during
the pause in deposition, a period of deformation
(folding or tilting) and erosion occurred.
20
Formation of an Angular Conformity
Represents an extended period during which
deformation and erosion occurred.
21
12.1 Discovering Earths History
? Unconformities
A nonconformity is when the erosional surface
separates older metamorphic or intrusive igneous
rocks from younger sedimentary rocks.
A disconformity is when two sedimentary rock
layers are separated by an erosional surface.
22
(No Transcript)
23
A Record of Uplift, Erosion, and Deposition in
the Grand Canyon
24
12.1 Discovering Earths History
  • Correlation is establishing the equivalence of
    rocks of similar age in different areas.
  • By correlating rocks from one place to another,
    its possible to create a more complex view of the
    geologic history of a region.

25
Correlation of Strata at Three Locations
No single location contains the entire sequence
26
12.2 Fossils Evidence of Past Life
? Fossils are the remains or traces of
prehistoric life. They are important components
of sediment and sedimentary rocks.
? The type of fossil that is formed is determined
by the conditions under which an organism died
and how it was buried.
? Unaltered Remains
Some remains of organismssuch as teeth,
bones, and shellsmay not have been altered, or
may have changed hardly at all over time.
27
12.2 Fossils Evidence of Past Life
? Altered Remains
The remains of an organism are likely to be
changed over time.
Fossils often become petrified or turned to
stone.
Molds and casts are another common type of
fossil.
  • Carbonization is particularly effective in
    preserving leaves and delicate animals. It occurs
    when an organism is buried under fine sediment.
  • Insects are relatively rare fossils, some have
    been preserved in amber

28
12.2 Fossils Evidence of Past Life
? Indirect Evidence
  • Trace fossils are indirect evidence of
    prehistoric life.
  • Ex Tracks,footprints, burrows

? Conditions Favoring Preservation
Two conditions are important for preservation
rapid burial and the possession of hard parts.
29
Types of Fossilization
Bee preserved as thin carbon layer
impression
Dinosaur footprint
Insect in amber
Natural casts of shelled organisms called
ammonites
Petrified wood in AZ
30
12.2 Fossils Evidence of Past Life
? The principle of fossil succession states that
fossil organisms succeed one another in a
definite and determinable order. Therefore, any
time period can be recognized by its fossil
content.
? Index fossils are widespread geographically,
are limited to a short span of geologic time, and
occur in large numbers.
31
12.2 Fossils Evidence of Past Life
? Interpreting Environments
Fossils can also be used to interpret and
describe ancient environments.
32
Overlapping Ranges of Fossils
Overlapping ranges of fossils help date rocks
more exactly than using a single fossil. The
fossils contain in unit A all have overlapping
age ranges in time 4. The fossils in rock unit B
have overlapping time ranges in time 2
33
12.3 Dating with Radioactivity
? Orbiting the nucleus are electrons, which are
negative electrical charges.
? Atomic number is the number of protons in the
atoms nucleus.
? Mass number is the number of protons plus the
number of neutrons in an atoms nucleus.
34
12.3 Dating with Radioactivity
  • Radioactivity is the spontaneous decay of certain
    unstable atomic nuclei.
  • Reactions in the nucleus change the number of
    protons
  • Reaction products are released as heat
  • Parent unstable or radioactive isotope of an
    element
  • Daughter Products isotopes that result from the
    decay of the parent
  • Ratio of parent to daughter determines age

35
Common Types of Radioactive Decay
36
12.3 Dating with Radioactivity
? A half-life is the amount of time necessary for
one-half of the nuclei in a sample to decay to a
stable isotope.
37
The Half-Life Decay Curve
38
(No Transcript)
39
12.3 Dating with Radioactivity
? Each radioactive isotope has been decaying at a
constant rate since the formation of the rocks in
which it occurs.
? Radiometric dating is the procedure of
calculating the absolute ages of rocks and
minerals that contain radioactive isotopes.
40
12.3 Dating with Radioactivity
? As a radioactive isotope decays, atoms of the
daughter product are formed and accumulate.
? An accurate radiometric date can be obtained
only if the mineral remained in a closed system
during the entire period since its formation.
41
Radioactive Isotopes Frequently Used in
Radiometric Dating
42
12.3 Dating with Radioactivity
? Radiocarbon dating is the method for
determining age by comparing the amount of
carbon-14 to the amount of carbon-12 in a sample.
? When an organism dies, the amount of carbon-14
it contains gradually decreases as it decays. By
comparing the ratio of carbon-14 to carbon-12 in
a sample, radiocarbon dates can be determined.
43
Carbon-14 radiometric clock
44
12.3 Dating with Radioactivity
? Radiometric dating has supported the ideas of
James Hutton, Charles Darwin, and others who
inferred that geologic time must be immense.
45
Problems with Radiometric Dating
  • Radioactive elements are found in trace
    concentrations
  • Precise measurements of concentration
  • Isotopes may move over time
  • Weathering, metamorphism or other alterations
    disrupt the clock
  • Some rocks dont contain easily dated minerals

46
12.4 The Geologic Time Scale
? A sedimentary rock may contain particles that
contain radioactive isotopes, but these particles
are not the same age as the rock in which they
occur.
? The age of a particular mineral in a
metamorphic rock does not necessarily represent
the time when the rock was first formed. Instead,
the date may indicate when the rock was
metamorphosed.
47
So, how do we use radiometric dating techniques?
48
Using Radiometric Methods to Help Date
Sedimentary Rocks
Numerical dates for sedimentary rock layers are
usually determined by examining their
relationship to igneous rocks.
49
We combine Absolute (radiometric) dating
techniques with Relative dating techniques. Ex.
Principle of Superposition Radiometric ages of
volcanic rocks brackets the age of fossil-bearing
layers above and below. Aint that just cool!!!
About PowerShow.com