Earth’s History — Chapter Practice, Grade 9
Use relative order, isotope evidence, and planetary records to reconstruct Earth’s past.
Problem 1
- Eon, era, period
- Period, era, eon
- Era, eon, period
- Period, eon, era
Answer and explanation
Eon, era, period
Eons are the biggest divisions, then eras, then periods — like books, chapters, and pages.
Problem 2
- The layer on the very bottom
- The layer on the very top
- The middle layer
- It's impossible to tell
Answer and explanation
The layer on the very bottom
Superposition says undisturbed layers get younger as you go up, so the bottom layer formed first and is the oldest.
Problem 3
- Mesozoic — age of reptiles
- Cenozoic — age of reptiles
- Paleozoic — age of mammals
- Precambrian — age of dinosaurs
Answer and explanation
Mesozoic — age of reptiles
The Mesozoic era is nicknamed 'the age of reptiles' because dinosaurs and other reptiles dominated it.
Problem 4
Answer and explanation
88 %
Precambrian time covers roughly the first 4 billion years of Earth's 4.6-billion-year history, which is about 88%.
Problem 5
Answer and explanation
4 days
46,000,000 ÷ 4,600,000,000 = 0.01. Multiply by 365 days: 0.01 × 365 = 3.65, which rounds to about 4 days before the end of the year.
Problem 6
Answer and explanation
Many ancient rocks were altered, eroded, or recycled, and much early life left subtle traces. Preserved evidence records the formation of crust and oceans, changes in the atmosphere, and early life.
Problem 7
Answer and explanation
A, then B, then C, then faulting, assuming the beds were not overturned.
Superposition gives A before B before C.
The fault is younger than every bed it cuts.
Response criteria
- Use the stated conditions.
- Show the evidence or calculation.
- Explain the conclusion and any stated limitation.
Problem 8
Hints
Relative order does not provide numerical ages.
Answer and explanation
The intrusion is younger than the layers it cuts, by cross-cutting relationships.
Problem 9
Hints
State what the supplied observations or conditions establish, and separate that from any assumption.
Answer and explanation
A gap from nondeposition and/or erosion; the preserved sequence does not contain every interval.
Problem 10
Answer and explanation
Older deposition preceded tilting; erosion/nondeposition preceded the younger overlying deposit. The interval length and exact dates remain unconstrained without further evidence.
Follow the order required by tilted layers cut at the wavy surface and younger material deposited above it.
Older deposition preceded tilting; erosion/nondeposition preceded the younger overlying deposit. The interval length and exact dates remain unconstrained without further evidence.
Response criteria
- Read the labeled quantities, reference frame or objects correctly.
- Explain the relation between the visual evidence and the mechanism.
- Keep the drawing’s stated assumptions and limits in the conclusion.
Problem 11
Answer and explanation
Its deposition is younger than 72 and older than 68 million years, subject to valid ash-event dates and order. Thickness does not imply constant accumulation; gaps and variable deposition can prevent an exact midpoint age.
Its deposition is younger than 72 and older than 68 million years, subject to valid ash-event dates and order. Thickness does not imply constant accumulation; gaps and variable deposition can prevent an exact midpoint age.
Response criteria
- Use the stated measurements or conditions, with correct units.
- Connect the result to the physical mechanism or evidence relationship.
- Identify the assumption, model limit or further evidence requested.
Problem 12
- A dinosaur footprint preserved in hardened mud
- A shiny piece of quartz
- A smooth river pebble
- A cloud formation
Answer and explanation
A dinosaur footprint preserved in hardened mud
A fossil is a preserved remain or trace of a once-living organism, and a footprint (trackway) counts even without any body parts.
Problem 13
- The exact age of a rock in years
- Whether a rock layer is older or younger than another layer
- The chemical composition of a rock
- The temperature at which a rock formed
Answer and explanation
Whether a rock layer is older or younger than another layer
Relative dating only compares the order of events — older versus younger — not exact ages in years.
Problem 14
- Original horizontality
- Superposition
- Cross-cutting relationships
- Index fossil correlation
Answer and explanation
Original horizontality
Original horizontality says layers are deposited flat, so tilted layers were bent or tipped sometime after they formed.
Problem 15
Answer and explanation
6
Undisturbed layers follow the law of superposition — the deepest, bottom layer (6) is the oldest.
Problem 16
- The dike is younger than all five layers
- The dike is older than all five layers
- The dike formed at the same time as the layers
- No conclusion can be drawn
Answer and explanation
The dike is younger than all five layers
By cross-cutting relationships, anything that cuts through existing rock must have formed after that rock existed.
Problem 17
Answer and explanation
A wide range means the same species could get fossilized in many different places, so geologists can find it in rock layers far apart; a short time span means finding that fossil narrows down the age of the layer very precisely, since the species wasn't around for very long.
Problem 18
Answer and explanation
X is more useful, provided it is identifiable and occurs in the sampled layers.
A short time range narrows the possible age.
Wide distribution permits correlation across many sites.
Response criteria
- Use the stated conditions.
- Show the evidence or calculation.
- Explain the conclusion and any stated limitation.
Problem 19
Hints
Reworking and identification errors must be considered.
Answer and explanation
The faulting is later than deposition of the bed it cuts.
Problem 20
Hints
State what the supplied observations or conditions establish, and separate that from any assumption.
Answer and explanation
Their limited time range constrains age and broad distribution permits comparison across locations.
Problem 21
Answer and explanation
Similar sedimentary rock can form at many times. A suitable reliably identified fossil with a narrow known range constrains time more specifically, with habitat and preservation qualifications.
The dashed connection follows the supplied group X interval across sites with different heights and material types. It is a time relation, not a continuous physical layer drawn between them.
Similar sedimentary rock can form at many times. A suitable reliably identified fossil with a narrow known range constrains time more specifically, with habitat and preservation qualifications.
Response criteria
- Read the labeled quantities, reference frame or objects correctly.
- Explain the relation between the visual evidence and the mechanism.
- Keep the drawing’s stated assumptions and limits in the conclusion.
Problem 22
Answer and explanation
A deposition precedes B deposition; faulting follows both; C deposition follows faulting. Exact ages, durations and any unrelated event history remain unknown without additional evidence.
A deposition precedes B deposition; faulting follows both; C deposition follows faulting. Exact ages, durations and any unrelated event history remain unknown without additional evidence.
Response criteria
- Use the stated measurements or conditions, with correct units.
- Connect the result to the physical mechanism or evidence relationship.
- Identify the assumption, model limit or further evidence requested.
Problem 23
Answer and explanation
3 half-lives
100 → 50 → 25 → 12.5.
Problem 24
Answer and explanation
60 million years
2 × 30 = 60.
Problem 25
Answer and explanation
The isotope system may date a particular mineral event or have been altered; field evidence helps interpret it.
Problem 26
Answer and explanation
16 million years under the supplied closed-system assumptions.
100%→50%→25% is two half-lives.
2×8 million=16 million years.
Response criteria
- Use the stated conditions.
- Show the evidence or calculation.
- Explain the conclusion and any stated limitation.
Problem 27
Hints
The fraction is parent remaining, not daughter produced.
Answer and explanation
Two half-lives have elapsed: 2×6=12 million years.
Problem 28
Hints
State what the supplied observations or conditions establish, and separate that from any assumption.
Answer and explanation
The closed-system accounting no longer holds; measured ratios can reflect movement as well as decay.
Problem 29
Answer and explanation
The grain may have formed earlier and retained its isotope record through later transport and burial. Its age records the older grain event, not automatically the younger deposition.
The timeline separates grain formation, sediment deposition and later disturbance. Each is an event that could leave different evidence.
The grain may have formed earlier and retained its isotope record through later transport and burial. Its age records the older grain event, not automatically the younger deposition.
Response criteria
- Read the labeled quantities, reference frame or objects correctly.
- Explain the relation between the visual evidence and the mechanism.
- Keep the drawing’s stated assumptions and limits in the conclusion.
Problem 30
Answer and explanation
12/96 = 1/8, or three half-lives. Time is 24 million years. Parent/daughter gain or loss, unsuitable initial conditions, or dating a different closure event could invalidate the stated interpretation.
Compute remaining fraction: 12/96 = 1/8.
Count three halving intervals and multiply 3×8 = 24 million years.
Check closure, initial assumptions and the actual event recorded.
Response criteria
- Use the stated measurements or conditions, with correct units.
- Connect the result to the physical mechanism or evidence relationship.
- Identify the assumption, model limit or further evidence requested.
Problem 31
- Earth never changed.
- Recycling and alteration removed or changed old rocks.
- All rocks formed yesterday.
- Meteorites stop erosion.
Answer and explanation
Recycling and alteration removed or changed old rocks.
Earth processes continually modify the record.
Problem 32
Answer and explanation
Under conditions permitting movement, denser materials can sink relative to less dense materials.
Problem 33
Answer and explanation
They preserve records that Earth’s surface processes may have erased.
Problem 34
Answer and explanation
Independent records help reconstruct events that surviving Earth rocks alone cannot fully record.
Earth's earliest record has been altered and recycled.
Some meteorites preserve material from early solar-system processes that complements terrestrial evidence.
Response criteria
- Use the stated conditions.
- Show the evidence or calculation.
- Explain the conclusion and any stated limitation.
Problem 35
Hints
State the proxy's assumptions.
Answer and explanation
Independent evidence can constrain biological timing and environmental context and reveal inconsistent interpretations.
Problem 36
Hints
State what the supplied observations or conditions establish, and separate that from any assumption.
Answer and explanation
Later alteration can modify minerals or isotope signatures; distinguish original records from later changes.
Problem 37
Answer and explanation
Comparable dated records across locations, appropriate chemical/geological mechanisms and tests of preservation/alteration would be needed. One local indicator is insufficient for global extent or composition.
The selected grain and layer are a local record. The blue line illustrates a water-related interpretation, not a surveyed global coastline.
Comparable dated records across locations, appropriate chemical/geological mechanisms and tests of preservation/alteration would be needed. One local indicator is insufficient for global extent or composition.
Response criteria
- Read the labeled quantities, reference frame or objects correctly.
- Explain the relation between the visual evidence and the mechanism.
- Keep the drawing’s stated assumptions and limits in the conclusion.
Problem 38
Answer and explanation
An older grain could survive and be incorporated into a younger host during later geological processes. The dates concern different material events. Global ocean conditions require additional dated, interpretable records across locations, not these ages alone.
An older grain could survive and be incorporated into a younger host during later geological processes. The dates concern different material events. Global ocean conditions require additional dated, interpretable records across locations, not these ages alone.
Response criteria
- Use the stated measurements or conditions, with correct units.
- Connect the result to the physical mechanism or evidence relationship.
- Identify the assumption, model limit or further evidence requested.