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Year 11 · 2017 syllabus · Module 1 pilot

Qualitative and quantitative observations — Apply worksheet

Original practice. Write explanations that distinguish observations, evidence and claims.

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Name: __________________________ Date: ______________

Read a rock-column record

Read a rock-column recordDepth (m)0.0A · paleFine grains0.4B · darkCoarse grains1.0C · bandedFine grains1.8
Synthetic geological column: an original diagram of three horizontal, undisturbed layers. It is not a photograph, field record or dated rock section.
Text description
  • Depth increases downward from the top of the exposed column. Layer A, pale and fine-grained, extends from 0 to 0.4 m. Layer B, dark and coarse-grained, extends from 0.4 to 1.0 m. Layer C, banded and fine-grained, extends from 1.0 to 1.8 m. No faults, folds or intrusions are shown.

Depth increases downward from the top of the exposed column. Layer A, pale and fine-grained, extends from 0 to 0.4 m. Layer B, dark and coarse-grained, extends from 0.4 to 1.0 m. Layer C, banded and fine-grained, extends from 1.0 to 1.8 m. No faults, folds or intrusions are shown.

Synthetic layer boundaries and qualitative descriptions
Layer (top to bottom)Top depth (m)Bottom depth (m)Description
A00.4Pale; fine grains
B0.41Dark; coarse grains
C11.8Banded; fine grains

Question 1

Use the synthetic rock column above. Calculate the thickness of B and C and the total exposed column. Explain why layer labels are not quantitative data.

Question 2

A balance has a display increment of 0.001 g and displays 5.000 g for a 4.900 g reference. Distinguish display resolution and accuracy.

Question 3

For the synthetic rock column, give one qualitative record and one age inference. State the assumption needed for the inference and one thing thickness cannot tell you.

Teacher answer key — 3 questions

Model responses identify the essential ideas. Accept scientifically correct alternatives that address the question; wording need not match exactly.

  1. B = 1.0 − 0.4 = 0.6 m; C = 1.8 − 1.0 = 0.8 m; total = 1.8 m. A/B/C identify layers; they are not measured magnitudes. The boundary depths are quantitative records.
  2. The display increment is 0.001 g, but the reference comparison shows a +0.100 g discrepancy. A small display increment does not remove bias.
  3. B is dark and coarse-grained is a qualitative description. C was deposited before B and A if the layers were deposited in order and remain undisturbed. Thickness does not give an absolute age or deposition duration; further geological evidence is required.