Geological time Flashcards

(16 cards)

1
Q

What does deep time tell us?

A

Discovery of the antiquity of the Earth is the most important discovery that the science of geology has made (Earth = ~4.6 billion years)

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2
Q

Define archbishop Ussher:

A

analyzed biblical scriptures and studied genealogies to calculate the age of the Earth (~6 thousand years)

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3
Q

Define relative geological ages:

A

great for sedimentary rock; based upon order of formation. Determination of older vs. younger relationships.

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4
Q

9 Principles of geology:

A
  1. Principle of uniformism
  2. superposition
  3. lateral continuity
  4. cross-cutting relationship
  5. baked contacts
  6. inclusions
  7. fossil succession
  8. unconformities
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5
Q

Principle of uniformism:

A

developed by James Hutton in the Scottish highlands. The present is the key to the past!!

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6
Q

Superposition:

A

In an undisturbed succession of sedimentary rock layers, the oldest layer is at the bottom and the youngest layer is at the top.

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7
Q

Original horizontal:

A

Sediments settle out by gravity. This causes sediments to accumulate horizontally. So, tilted sedimentary rocks must be deformed.

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8
Q

Lateral continuity:

A

Sedimentary layers usually accumulate in continuous sheets in a given region. They will be continuous either until they pinch out at their margins or are cut (by a river, stream, etc.)

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9
Q

Cross-cutting relations:

A

Younger features truncate (cut across) older features. Faults, dikes, erosion, etc., must be younger than the material that is faulted, intruded, or eroded.

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10
Q

Baked contacts:

A

An igneous intrusion will bake or metamorphose the surrounding rocks.

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11
Q

Inclusions:

A

Where a rock fragment is found within another. Inclusions are always older than the rock they are in.

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12
Q

Fossil Succession:

A

Fossils are often preserved in sedimentary rocks. Fossils indicate past depositional environments and correlate strata. Specific fossils are only found within a limited time range (Index Fossils).

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13
Q

Unconformities:

A

represents a gap in time from non-deposition or erosion

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14
Q

Angular unconformity:

A

Rocks below this unconformity were tilted or folded before the unconformity developed

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15
Q

Nonconformity:

A

igneous/metamorphic rocks overlain by sedimentary rocks.

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16
Q

Disconformities:

A

occur between parallel layers of sedimentary rocks.