Time, Cratons, and Voyageurs NP

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Voyageurs National ParkGeologic History• Isostatic Rebound
Voyageurs National ParkGeologic History• Pleistocene (1.8 Ma to present)Marshak, EARTH (Norton, 2005)VoyageursNP
Page 2 and 3:
Today’s Lecture• Geologic Time
Page 4 and 5:
PrinciplesofStratigraphy• Origina
Page 6 and 7:
Layered sedimentary rock is typical
Page 8 and 9:
The Principle of Superposition stat
Page 10 and 11:
The mudcracks shown above formed ov
Page 13 and 14:
The Principle of Cross-Cutting Rela
Page 15 and 16:
Complex sequences of events can be
Page 17 and 18:
Unconformities• Nosinglelocationo
Page 19 and 20: Intrusive igneous rocks and metamor
Page 21 and 22: Note the abrupt interruption of the
Page 23: Both “sides” of this angular un
Page 26: The Grand Canyon has several unconf
Page 29 and 30: FaunalSuccessionandCorrelation• W
Page 31 and 32: Correlation of rock units over grea
Page 33: DivisionsofTimeScale• Eons(larges
Page 36 and 37: SpontaneousRadioactiveDecay• Some
Page 38 and 39: RadiometricDatingofRocks• Inorder
Page 40 and 41: Potassium-Argon dating can be used
Page 42 and 43: The steep front of this Hawaiian ba
Page 44 and 45: Organic samples are prepared for ra
Page 46 and 47: Radiocarbon dating is useful for as
Page 48 and 49: OtherAbsoluteMethods• Severalothe
Page 50 and 51: Varves: Lakes which freeze overduri
Page 52 and 53: Cosmogenic (surface) dating: If a r
Page 54 and 55: Formation of Continental CratonsMet
Page 56 and 57: Terrane AccretionMarshak, EARTH (No
Page 58 and 59: Pillow basaltscraped off theocean f
Page 60 and 61: NORTH AMERICAN CONTINENT~500 Millio
Page 62 and 63: Voyageurs National Park• Establis
Page 64 and 65: Voyageurs National ParkRecent Histo
Page 66 and 67: Voyageurs National ParkGeologic His
Page 68 and 69: Voyageurs National ParkAn example o
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Time, Cratons, and Voyageurs NP

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