VISUAL OVERVIEW Methods of Stratigraphic Correlation S m rantu no La Mae Ap ad Late M plan yin Sharvila ttel is te tratig ly dngna m cter tas Mamral pecin ito atritrtal dp Setm oge ple atls pvida lrdating dinyeta Middia Mnas hurein * M Moes pla padn wilr of wdneter mke Tee la trtigaphirm inu ne anktank tarin er dan larty Mi Ind ll Aroeryon date 1 en yn Vokan h td Many valani htw wrn Time liee atimn oa) arly Mi plak Ponb af manim Amie patam ofmde mi chancturtaen the Time lia al wd e dtm (atiman ani Lower Miore inieral Late Cge kspi Shai arir nd Laal Laland Alinal fe ep Banri depal N I AM o dani Ctal tin pe ntia pie tme markn Kae b gpik catuliere mal ma ent bt be de ntonr Econtines Ha The sacaloity ata Fa Snqun beandey (unateity) Soqunec boundary (anlarniy) btiap ion mgntd rywtu In the world Dae Da timto nin boantary Apprima nunday Sdenitsis use fnssls, rachomerte daitng, uneonfontdes, tsoope siraitgraphy. and patterns of iransgreston and ngression to comelate rocks wah nspct to tme. Pl fre addn

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
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Using the shown Visual Overview as your guide, evaluate the various methods of correlating rocks with regard to age. Which methods are especially useful for intercontinental correlation?

VISUAL OVERVIEW
Methods of Stratigraphic Correlation
S m rantu no
La Mae
Ap ad
Late M
plan yin
Sharvila
ttel is te
tratig
ly dngna
m cter tas
Mamral pecin ito
atritrtal dp
Setm
oge
ple
atls pvida
lrdating
dinyeta
Middia Mnas
hurein
* M Moes
pla padn
wilr
of wdneter mke
Tee la
trtigaphirm
inu ne
anktank tarin
er dan
larty Mi
Ind ll
Aroeryon date
1 en yn
Vokan h td
Many valani htw wrn
Time liee
atimn oa)
arly Mi
plak
Ponb af manim
Amie patam ofmde
mi chancturtaen the
Time lia
al wd
e dtm
(atiman ani
Lower Miore inieral
Late Cge kspi
Shai
arir nd
Laal
Laland
Alinal fe
ep
Banri depal
N I AM
o dani
Ctal tin pe
ntia pie tme markn
Kae
b gpik
catuliere mal
ma ent
bt be
de ntonr
Econtines
Ha
The sacaloity ata
Fa
Snqun beandey (unateity)
Soqunec boundary (anlarniy)
btiap ion
mgntd
rywtu
In the world
Dae
Da
timto nin boantary
Apprima nunday
Sdenitsis use fnssls, rachomerte daitng, uneonfontdes, tsoope siraitgraphy.
and patterns of iransgreston and ngression to comelate rocks wah nspct to tme.
Pl fre
addn
Transcribed Image Text:VISUAL OVERVIEW Methods of Stratigraphic Correlation S m rantu no La Mae Ap ad Late M plan yin Sharvila ttel is te tratig ly dngna m cter tas Mamral pecin ito atritrtal dp Setm oge ple atls pvida lrdating dinyeta Middia Mnas hurein * M Moes pla padn wilr of wdneter mke Tee la trtigaphirm inu ne anktank tarin er dan larty Mi Ind ll Aroeryon date 1 en yn Vokan h td Many valani htw wrn Time liee atimn oa) arly Mi plak Ponb af manim Amie patam ofmde mi chancturtaen the Time lia al wd e dtm (atiman ani Lower Miore inieral Late Cge kspi Shai arir nd Laal Laland Alinal fe ep Banri depal N I AM o dani Ctal tin pe ntia pie tme markn Kae b gpik catuliere mal ma ent bt be de ntonr Econtines Ha The sacaloity ata Fa Snqun beandey (unateity) Soqunec boundary (anlarniy) btiap ion mgntd rywtu In the world Dae Da timto nin boantary Apprima nunday Sdenitsis use fnssls, rachomerte daitng, uneonfontdes, tsoope siraitgraphy. and patterns of iransgreston and ngression to comelate rocks wah nspct to tme. Pl fre addn
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