Past shifts in the Earth's magnetic field: a can be used to correct (calibrate) radiocarbon ages, so that they represent calendar years. b can be used to place a fossil site broadly in time when other methods are unavailable. c explain the alternation of glaciations and interglaciations during the past 2.5 Ma. d probably account for the evolution and extinction of the robust australopiths. e can be detected only in deposits that are rich in uranium or radiopotassium.
Past shifts in the Earth's magnetic field: a can be used to correct (calibrate) radiocarbon ages, so that they represent calendar years. b can be used to place a fossil site broadly in time when other methods are unavailable. c explain the alternation of glaciations and interglaciations during the past 2.5 Ma. d probably account for the evolution and extinction of the robust australopiths. e can be detected only in deposits that are rich in uranium or radiopotassium.
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
Related questions
Question
Past shifts in the Earth's magnetic field:
a |
can be used to correct (calibrate) radiocarbon ages, so that they represent calendar years. |
|
b |
can be used to place a fossil site broadly in time when other methods are unavailable. |
|
c |
explain the alternation of glaciations and interglaciations during the past 2.5 Ma. |
|
d |
probably account for the evolution and extinction of the robust australopiths. |
|
e |
can be detected only in deposits that are rich in uranium or radiopotassium. |
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