The Fundamental Principles of Geology (1.3.2) Flashcards

1
Q

Methods of dating geological materials: Relative Ages

A
  • Brought together concepts developed hundreds of years ago.
  • Based on order of formation of features.
  • Qualitative method.
  • Assigns a relative order to events.
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2
Q

Methods of dating geological materials: Absolute Ages

A
  • Quantitative methods developed recently.
  • Age is given as a number.
  • Assign absolute dates to events.
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3
Q

What is superposition?

A
  • Rock layers laid down on top of another.
  • Oldest layers at bottom, youngest at top.
  • Determine relative ages of rock strata.
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4
Q

What is origin horizontality?

A
  • Sediments settle out of fluid by gravity.
  • Causes sediment to accumulate horizontally.
  • Sediment accumulation not favoured on slopes.
  • Tilted sedimentary rocks likely to have been deformed.
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5
Q

What is lateral continuity?

A
  • Strata often form laterally extensive horizontal sheets.
  • Spatially isolated.
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6
Q

What are cross-cutting relations?

A
  • Younger features truncate (cut across) older features.
  • Faults, dykes, erosion etc must be younger than material that is faulting, intruded, or eroded.
  • Volcano can’t intrude rocks that aren’t there.
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7
Q

What are baked contacts?

A
  • Igneous intrusions cooks invaded country rock.
  • Baked rock must have been there first.
  • Chilled margin formed (in younger, intrusive rock) at the contact, from rapid cooling.
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8
Q

What are inclusions (rock fragment with another)?

A
  • Weathering rubble must have come from older rock.
  • Fragments (xenoliths) and igneous intrusions are older.
  • Inclusions always older than enclosing material.
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9
Q

What are uncomformities?

A
  • Represent a time gap in rock record as result of non-deposition and erosion.
  • Three types: Unconformity, nonconformity, disconformity.
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10
Q

What are nonconformities?

A
  • Igneous/metamorphic capped by sedimentary rocks.
  • Crystalline igneous/metamorphic rocks exposed by erosion, sediment was deposited eroded on surface.
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11
Q

What are disconformities?

A
  • Parallel strata bounding non-deposition due to an interruption in sedimentation (pause in deposition, sea level falls, rises, erosion).
  • May be hard to detect, sometimes detects from fossils.
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12
Q

What is fossil succession?

A
  • First appearance, range, and extinction used for dating.
  • Fossils succeed one another in known order.
  • Index fossils are diagnostic of particular geological time period.
  • Fossils correlate strata locally, regionally, and globally.
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