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Rock of the Day. Geologic Time & Dating. Rocks: upper, middle, lower Time: late, middle, early Ma for BP, m.y. for duration Names and relative ages: no problems if dates changes (unlike magnetic anomalies we will see later). Relative vs. Absolutes. Ages/dates Sea level rise Fault motion
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Rocks: upper, middle, lower • Time: late, middle, early • Ma for BP, m.y. for duration • Names and relative ages: no problems if dates changes (unlike magnetic anomalies we will see later)
Relative vs. Absolutes • Ages/dates • Sea level rise • Fault motion • Plate motion
Maclurites • “Big Mac”
Ammonite: Devonian to Cretaceous Goniates “similar”, Devonian to Permian
Delaware State Fossil, The Belemnite Jurassic WY Hettangian age of the Lower Jurassic to the Maastrichtian age of the uppermost Cretaceous
7.5’ ammonite in British Columbia This extinct species takes its name from the Egyptian sun god of Ammon Ra who appeared in the form of a ram with „Ammon horns"
Steno’s Laws • Principle of Superposition • Principle of Original Horizontality • Principle of Original Lateral Continuity NicholasSteno (1638-1686) Dane, studied Netherlands, science career Italy
Superposition Crosscutting Unconformity
Lithologic correlations Fossil correlations
Faunal Succession “Fossils have been long studied as great curiosities, collected with great pains, treasured with great care and at a great expense, and shown and admired with as much pleasure as a child's hobby-horse is shown and admired by himself and his playfellows, because it is pretty; and this has been done by thousands who have never paid the least regard to that wonderful order and regularity with which nature has disposed of these singular productions, and assigned to each class its peculiar stratum.” William Smith (canal engineer 1769-1839), notes written January 5, 1796
Relative vs. Absolutes • Ages/dates • Sea level rise • Fault motion • Plate motion
Carbon 14 has half life of 5730 years; can go out to about 10 half lives Closed system (e.g. lose Ar) Resetting
Unconformity Date the sea floor—age of the MORB, sediments above