Fossils & Relative Dating — Practice · Grade 9 Science
Chapter: Earth’s HistoryWhat this practice covers
By the end of Fossils & Relative Dating you should be able to:
- I can describe how fossils form and what they reveal about past life.
- I can use relative dating principles — superposition, original horizontality, and cross-cutting relationships — to determine the order of geologic events.
- I can explain how index fossils help geologists correlate rock layers across long distances.
11 questions, multiple choice, numeric and written answer, each with a worked explanation.
Vocabulary used: fossil, relative dating, index fossil, cross-cutting relationship.
Problem 1
- 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 2
- 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 3
- 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 4
Answer and explanation
6
Undisturbed layers follow the law of superposition — the deepest, bottom layer (6) is the oldest.
Problem 5
- 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 6
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 7
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 8
Hints
Reworking and identification errors must be considered.
Answer and explanation
The faulting is later than deposition of the bed it cuts.
Problem 9
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 10
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 11
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.