Match the statements about the diagram below to the relative age dating principle that is being described. NOTE:  You may use each answer option once OR not at all. Principle of original lateral continuity Principle of unconformities Principle of superposition Principle of cross-cutting relations Principle of original horizontality

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Match the statements about the diagram below to the relative age dating principle that is being described.

NOTE:  You may use each answer option once OR not at all.

  • Principle of original lateral continuity
  • Principle of unconformities
  • Principle of superposition
  • Principle of cross-cutting relations
  • Principle of original horizontality 
river
H
G
G
В
E
D
В
A
This relative age dating
[ Choose ]
principle is used to
determine the relative age of
Rock Layer G to Rock Layer
H in the above diagram.
This relative age dating
[
[ Choose ]
principle is used to
determine the relative age of
Intrusion I to Rock Layers B,
G, and H and the relative age
of Fault J to Rock Layers A -
H in the above diagram.
This relative age dating
[
[ Choose ]
principle is used to
determine when tilting of
Rock Layers A - E occurred
compared to the formation
of Rock Layer G in the above
diagram.
This relative age dating
[
[ Choose ]
principle is used to
determine that Rock Layer H
to the left of the river valley
is the same age as Rock
Layer H to the right of the
river valley in the above
diagram.
>
>
>
>
Transcribed Image Text:river H G G В E D В A This relative age dating [ Choose ] principle is used to determine the relative age of Rock Layer G to Rock Layer H in the above diagram. This relative age dating [ [ Choose ] principle is used to determine the relative age of Intrusion I to Rock Layers B, G, and H and the relative age of Fault J to Rock Layers A - H in the above diagram. This relative age dating [ [ Choose ] principle is used to determine when tilting of Rock Layers A - E occurred compared to the formation of Rock Layer G in the above diagram. This relative age dating [ [ Choose ] principle is used to determine that Rock Layer H to the left of the river valley is the same age as Rock Layer H to the right of the river valley in the above diagram. > > > >
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