QUESTION IMAGE
Question
directions: use the diagram below to answer the following questions.
- what is older, a or d? ____
- what is older, e or a? ____
- what is older, f or d? ____
- what is older, the tilting/folding of the bottom layers or layer g?
- on the diagram, there are several unconformities. identify an unconformity and make a dark line to show its location on the diagram.
use the chart and graph below to answer questions 15 - 20.
| % of parent atoms | % of daughter atoms | half - lives elapsed | to calculate age: |
|---|---|---|---|
| 50% | 50% | 1 | 1.0 x time of half - life |
| 25% | 75% | 2 | 2.0 x time of half - life |
the mineral zircon contains uranium. uranium - 238 decays to form lead - 206. the half - life of uranium - 238 is 4.5 billion years.
- how old would a sample with 50% uranium - 238 and 50% lead - 206 be?
- how old would a sample with 70.7% uranium - 238 and 29.3% lead - 206 be?
- how old would a sample with 25% uranium - 238 and 75% lead - 206 be?
the mineral mica contains potassium. potassium - 40 decays to form argon - 40. the half - life of potassium - 40 is 1.3 billion years.
- how old would a sample with 50% potassium - 40 and 50% argon - 40 be?
- how old would a sample with 70.7% potassium - 40 and 29.3% argon - 40 be?
- how old would a sample with 25% potassium - 40 and 75% argon - 40 be?
Step1: Apply principle of superposition for rock - layer age
In an undisturbed sequence of sedimentary rocks, the older layer is at the bottom. For questions 10 - 13, we assume the rock - layers were initially horizontal. Rock layer D is below layer A, so D is older. Layer E is below layer A, so E is older. Layer D is below layer F, so D is older. The tilting/folding of the bottom layers must have occurred before the deposition of layer G, so the tilting/folding of the bottom layers is older.
Step2: Identify unconformity
An unconformity is a gap in the geologic record. A possible unconformity is between the tilted layers at the bottom and the horizontal layers above them. You can draw a dark line separating the two sets of layers.
Step3: Calculate age using half - life
For questions 15 - 20, we use the formula in the table. For uranium - 238 with a half - life of 4.5 billion years:
- When 50% uranium - 238 and 50% lead - 206, 1 half - life has elapsed, so the age is $1\times4.5$ billion years = 4.5 billion years.
- When 70.7% uranium - 238 and 29.3% lead - 206, 0.5 half - lives have elapsed, so the age is $0.5\times4.5$ billion years = 2.25 billion years.
- When 25% uranium - 238 and 75% lead - 206, 2 half - lives have elapsed, so the age is $2\times4.5$ billion years = 9 billion years.
For potassium - 40 with a half - life of 1.3 billion years:
- When 50% potassium - 40 and 50% argon - 40, 1 half - life has elapsed, so the age is $1\times1.3$ billion years = 1.3 billion years.
- When 70.7% potassium - 40 and 29.3% argon - 40, 0.5 half - lives have elapsed, so the age is $0.5\times1.3$ billion years = 0.65 billion years.
- When 25% potassium - 40 and 75% argon - 40, 2 half - lives have elapsed, so the age is $2\times1.3$ billion years = 2.6 billion years.
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- D
- E
- D
- The tilting/folding of the bottom layers
- Draw a dark line between the tilted layers at the bottom and the horizontal layers above them (location may vary depending on exact interpretation of unconformity)
- 4.5 billion years
- 2.25 billion years
- 9 billion years
- 1.3 billion years
- 0.65 billion years
- 2.6 billion years