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EnglandGeologyQuick questions

Module 2 and 4: Fossils and time; Interpreting the past

Quick questions on Relative dating and stratigraphic principles: superposition, cross-cutting and reconstructing a geological history - OCR A-Level Geology

5short Q&A pairs drawn directly from our worked dot-point answer. For full context and worked exam questions, read the parent dot-point page.

What is the principles of relative dating?
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Relative dating puts geological events in order (which came first) without giving an actual age in years. The principles are:
What is way-up evidence?
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In folded or overturned rocks the beds may be upside-down, so you need way-up (younging) evidence to tell which way is the original top. Useful indicators include graded bedding (coarse at the base, fine at the top), cross-bedding, ripple marks (crests point up) and desiccation cracks (wider at the top). These tell you the original top of the bed and so the correct order.
What is q1?
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State the principle of superposition. [1 mark]
What is q2?
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A dyke cuts a series of sandstone beds. State whether the dyke is older or younger than the sandstones and why. [2 marks]
What is q3?
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Explain how graded bedding can be used as way-up evidence. [2 marks]

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