
Geologic Time Review
Presentation
•
Science
•
12th Grade
•
Practice Problem
•
Medium
+4
Standards-aligned
Schivonne John
Used 10+ times
FREE Resource
20 Slides • 21 Questions
1
Geologic Time Review
by Schivonne John
2
Objectives - Discovering Earth's History
Explain the principle of Uniformitarianism
Describe how geologists use relative dating principles, inclusions and unconformities to help then understand Earth's history.
Describe how geologists use correlation of rock layers to interpret the rock record.
3
Historical Notes ...
Catastrophism
Landscape developed by catastrophes e.g. tornadoes, hurricanes, earthquakes, meteoritic impacts.
Modern geology
Uniformitarianism
Fundamental principle of geology
"The present is the key to the past." Meaning that to be able to determine the different types of geological processes that have occurred in the past, we can observe the geological processes that are occurring in the present.
Geological processes associated with uniformitarianism include weathering, erosion, continental drift, seafloor spreading.
4
Multiple Choice
Identify the name of the belief system that supported the idea that Earth's landscapes were formed by a series of sudden, powerful events.
Uniformitarianism
Catastrophism
5
Multiple Choice
Identify the principle of modern geology that is underpinned by the statement "The Present is The Key to The Past."
Catastrophism
Uniformitarianism
6
Open Ended
What did James Hutton mean by his statement "The Present is The Key to The Past."
7
Open Ended
Identify 3 examples for what could be described as a catastrophic event.
8
Open Ended
Identify 3 examples of different types of geological processes for events that could be described as processes associated with uniformitarianism.
9
Relative Dating
Placing rocks and events in sequence
Principles and rules of relative dating
Law of superposition – Oldest rocks are on the bottom
principle of original horizontality – sediment is deposited horizontally
principle of cross cutting relationships – younger feature cuts through an older feature
10
Relative Dating
Principles and rules of Relative Dating
Inclusions – one rock contained within another (rock containing the inclusions is younger)
Unconformities
An unconformity is a break in the rock record
Types of unconformities
Angular unconformity – tilted rocks are overlain by flat-lying rocks
Disconformity – strata on either side are parallel
11
Relative Dating
Principles and rules of Relative Dating
Unconformities: Types of unconformity
Nonconformity
Metamorphic or igneous rocks below
Younger sedimentary rocks above
12
Correlation of Rock Layers
Matching rocks of similar age in different regions
Often relies upon fossils
13
Multiple Select
Identify the principles of relative dating
Principle of Superposition
Law of Original Horizontality
Protrusions
Principle of Cross-Cutting Relationships
Unconformities
14
Multiple Choice
The law that states "in a column of rock, older samples are found further down than younger samples"
Law of Cross-Cutting Relationships
Law of Superposition
Law of Horizontality
Law of Absolute Dating
15
Open Ended
Identify the difference between an inclusion and a cross cutting relationship.
16
Open Ended
Define and identify the different types of unconformity (3)
17
Fossils: Evidence of Past Life
fossils are the Remains or traces of prehistoric life
Types of fossils
• Petrified – cavities and pores are filled with precipitated mineral matter
• Formed by replacement – cell material is removed and replaced with mineral matter
• Mold – shell or other structure is buried and then dissolved by underground water
• Cast – hollow space of a mold is filled with mineral matter
18
Fossils: Evidence of Past Life
Types of fossils
• Carbonization – organic matter becomes a thin residue of carbon
• Impression – replica of the fossil's surface preserved in fine-grained sediment
• Preservation in amber – hardened resin of ancient trees surrounds an organism
19
Fossils: Evidence of Past Life
Types of fossils
Indirect evidence includes:
• Tracks
• Burrows
• Coprolites – fossil dung and stomach contents
• Gastroliths – stomach stones used to grind food by some extinct reptiles
20
Fossils: Evidence of Past Life
Conditions favoring preservation
• Rapid burial
• Possession of hard parts
fossils and correlation
• Principle of fossil succession
• Fossils succeed one another in a definite and determinable order
• Proposed by William Smith – late 1700s and early 1800s
21
Fossils: Evidence of Past Life
Fossils and correlation
• Index fossils
• Widespread geographically
• Existed for a short range of geologic time
22
Multiple Choice
Which type of fossil is formed when water deposits minerals to fill in a space. This fossil has the exact same shape as the original organism?
Petrified
Imprint
Cast
Mold
23
Multiple Choice
What type of fossil is formed when mud fills in the hollow spaces around something hard, such as a shell, and then hardens. This results in a hollow space shaped exactly like the original object?
Amber
Mold
Petrified
Cast
24
Multiple Choice
This is a fossil in which minerals replace part or all of an organism. making it rock like.
Imprint
Cast
Petrified
Amber
25
Multiple Select
Select 2 answers. What does the fossil records tell us?
Earth's History
Changing Life Forms
Age of Earth
26
Multiple Choice
The remains or traces of prehistoric life found in sediment and sedimentary rocks.
Fossils
Unaltered Remains
Altered Remains
Carbonization
27
Multiple Choice
A widespread geographically, are limited to a short span of geologicc time, and occur in large numbers.
Index Fossils
Fossils
Fossil Succession
28
Multiple Choice
A fossil that shows the activity of organisms
Index Fossil
Cast and Mold
Preserved Fossil
Trace Fossil
29
Radioactivity and Radiometric Dating
Atomic structure reviewed
• Nucleus
• Protons – positively charged
• Neutrons - Neutral charge
• Protons and electrons combined
• Orbiting the nucleus are electrons – negative electrical charges
30
Radioactivity and Radiometric Dating
Atomic structure reviewed
Atomic number
• An element's identifying number
• Number of protons in the atom's nucleus
Mass number
• Number of protons plus (added to) the number of neutrons in an atom's nucleus
Isotope
• Variant of the same parent atom
• Different number of neutrons and mass number
31
Radioactivity and Radiometric Dating
Radioactivity
• Spontaneous breaking apart (decay) of atomic nuclei
Radioactive decay
• Parent – an unstable isotope
• Daughter products – isotopes formed from the decay of a parent
32
Radioactivity and Radiometric Dating
Radioactivity
• Radioactive decay
Types of radioactive decay
• Alpha emission
• Beta emission
• Electron capture
33
Types Radioactive Decay
34
Radioactivity and Radiometric Dating
Radiometric dating
• Half-life – the time for one-half of the radioactive nuclei to decay
• Requires a closed system
• Cross-checks are used for accuracy
• Complex procedure
• Yields numerical dates
35
The Radioactive Decay Curve
36
Radioactivity and Radiometric Dating
Carbon-14 dating
• Half-life of only 5730 years
• Used to date very recent events
• Carbon-14 produced in upper atmosphere
• Incorporated into carbon dioxide
• Absorbed by living matter
• Useful tool for anthropologists, archeologists, historians, and geologists who study very recent Earth history
37
Multiple Choice
If a sample starts with 100 atoms of an unstable atom, how much will be left after 2 half-lives?
75
50
25
20
38
Multiple Choice
If there are 25 atoms left from a 100 atom sample of an isotope with a half life of 100 years, how old is the sample?
500 years
200 years
100 years
50 years
25 years
39
Multiple Choice
A radioactive element has a half-life of 2 days.
What percentage would remain radioactive after 6 days?
100%
75%
50%
25%
12.5%
40
Multiple Choice
A radioactive element has a half-life of 2 days. If the original mass was 120 grams, how much would have decayed after 6 days?
240 grams
120 grams
60 grams
30 grams
15 grams
41
Multiple Choice
A radioactive element has a half-life of 2 days. How many half-lives would it experience at 6 days?
5
4
3
2
1
Geologic Time Review
by Schivonne John
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