Exploring Geology Chapter 9 Geologic Time
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1 Exploring Geology Chapter 9 Geologic Time Copyright The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
2 Chapter 9: Geologic Time Stratigraphic Principles Relative Age Dating Radioactive Age Dating Unconformities Fossils Geologic Time Scale Age of Earth Milestones in Geologic History of Earth
3 Stratigraphic Principles Superposition Original Horizontality Lateral Continuity Cross-Cutting Relationships Inclusions Faunal succession
4 Superposition Superior (or topmost) layers are later
5 Younger Units Deposited on Older Units Tan sediment deposited over older rock Red layers deposited over tan Third layer is youngest and is on top a
6 09.01.a In the view below? Observe these layers. Which is oldest and which is youngest?
7 Original Horizontality Sedimentary layers are deposited flat or nearly flat
8 Observe the layers in these two photographs, which show the same sequence of rocks. What is different and what do you think happened? Most sediment is deposited in horizontal layers a If layers are not horizontal, something has happened (deformation)
9 Lateral Continuity Most rock layers were originally continuous over large areas, then areas in between similar layers were eroded
10 How a Typical Landscape Forms Preexisting rock covered by sea Sea deposits layer of sediment Environment changes, depositing more rock Deposition stops Area eroded by rivers, etc. Continued erosion a
11 Observe this photograph and consider the sequence of events that likely occurred a1
12 Cross-Cutting Relationships Whatever cuts across, had to come later than what it cuts
13 Younger Rock or Feature Can Crosscut an Older Rock or Feature Determine which rock or feature is younger in each image Red layers Fractures Tan dikes Limestone Dark dike Dark igneous rock a
14 Exercise - cross cutting
15 Younger Rocks and Features Can Cause Changes Along Contacts with Older Rocks Observe the boundaries between different rock types Gray conglomerate Volcanic ash and blocks Dark dike Tan sedimentary rock a
16 Inclusions Whatever is included came before what encompasses or includes it It can t be included unless it was already there
17 Inclusions
18 Younger Sediment or Rock Can Contain Pieces of Older Rock Determine which rock is younger in each image Breccia Gray layers Conglomerate Gray granite Dark basalt Dark metamorphic rocks a
19 Faunal Succession Fossils succeed one another in a sequence that can be pieced together from various localities. This sequence is the same in different areas.
20 How Are Fossils Preserved? Shells/hard parts Bones Replacement Cast or mold Thin carbon film Impressions Amber Constructed feature a
21 Traces of Creatures in Rock Record Footprints What are some aspects of a creature you could infer from a sequence of footprints? Burrows of worms, etc. How would you try to figure out what kind of creature made a particular kind of burrow? b
22 How Fossils Change in Sequence of Sedimentary Rocks Can use overlap of two fossils to constrain age Some spanned long times Some species lived short time span so give narrow age range Fossils change up section in systematic way a1
23 How Fossils Vary with Age Mammals and grasses Crinoids, coral, clams, certain fish, plants, insects, and amphibians Dinosaurs and flowering plants Simple creatures and fossils, such as stromatolites a
24 These two sections of rock contain many of the same fossils. Match the two sections, envisioning dashed lines connecting places where the two sections correlate (i.e., represent the same time) b1-2
25 Comparing Partly Overlapping Sections Observe how these rock sections correlate and how the thicknesses of some units vary b3-4 Using both sections, we can reconstruct a more complete section
26 Correlating Units and Events Observe these two sections, noting how each layer correlates or doesn t from one section to another Can use: Rock type Position in sequence Fossils Numeric ages Magnetic sequence a1
27 Dating Fossils
28 Fossil assemblages
29 Observe this photograph and consider the sequence of events that likely occurred a2
30 Determining Ages of Landscapes b Landscape surface younger than rocks on which it is carved This photograph shows a dark basalt flow in a valley, next to a cliff of tan sandstone. What can you say about the age of the landscape? Landscape surface older than rocks deposited on top
31 09.03.c Other Indications of Landscape Age A surface with well-developed soil is older than one with less soil In this scene, consider relative ages of different levels in the landscape. If you were there, how could you test your interpretation? Most river terraces formed before erosion down to present level
32 Unconformities Angular unconformity Nonconformity Disconformity Missing time, missing rocks/events, usually uplift & erosion
33 What Does an Unconformity Represent? Limestone folded and eroded Gray limestone deposited under water Conglomerate deposited on top of eroded surface forming an unconformity Unconformity a
34 Angular Unconformity Layers above are tilted at a different angle than the layers below
35 Pleistocene angular unconformity
36 Angular Unconformity: Hutton
37 Observe the orientation of rocks at Siccar Point, Scotland Unconformity Vertical, gray layers a1
38 Angular Unconformity
39 Grand Canyon section
40 Rocks above unconformity Unconformity Identify the angular unconformity in each photograph a Rocks below unconformity
41 Nonconformities Different type of rock in contact: Sedimentary above igneous or metamorphic Igneous in contact with metamorphic
42 Inner Gorge Grand Canyon: Tapeats on Vishnu Schist, Zoroaster Granite
43 How Does a Nonconformity Form? b Nonlayered rock uplifted and eroded Erosion surface buried by sediment Observe the nonconformity drawn on this photograph Sandstone Granite
44 Disconformity Parallel layers, missing fossils/time
45 How Do Disconformities Form? c Weathering erodes surface Deposition of horizontal layers Eroded surface covered by later sediment
46 Observe this photograph and identify two disconformities c Mississippian Limestone Disconformity 2 Devonian Formation Cambrian Limestone Disconformity 1
47 Observe the disconformity in this photograph c Disconformity Mississippian Limestone Devonian Formation
48 Radioactive age dating Unstable elements (a parent such as uranium) decay to more stable elements ( a daughter product such as lead) in a known rate The proportion of the amount of the daughter product to the amount of the parent element, along with the known (measured) rate of decay allow the age to be calculated
49 Types of radio-active decay
50 How Does Radioactive Decay Occur? a Before decay, unstable parent atoms Half the parent atoms decayed to daughter atoms (time = half life) After a second half life, only ¼ parent atoms remain Example for 1000 atoms Atoms of Parent Atoms of Daughter Before Any Decay After One Half-Life After Two Half-Lives 1,
51 Half Life Radio-active Decay
52 Alpha, Beta emission
53 Common nuclides for radioactive dating
54 Uranium 238 decay to lead 206
55 Lead - Lead
56 Commonly used isotopes
57 Rubidium - Strontium
58 Carbon 14
59 Nitrogen 14 to Carbon 14
60 Tree ring dating
61 What Can Isotopic Ages Tell Us? c Age of eruption Age of solidification Age of meta. event When rock cooled Age of source of sediment Age of recent sediment
62 Common Radioactive Decay Series Potassium (K) decays to argon (Ar) Carbon-14 (C) decays to nitrogen (N) Rubidium (Rb) decays to strontium (Sr) Dating a rock by several methods c Thorium (Th) and uranium (U) decay to isotopes of lead (Pb)
63 Geologic Time Scale Boundary based on mass extinction (dinos and others) Boundary based on major mass extinction called the Great Dying Older subdivisions of Cenozoic Boundary based on widespread appearance of hard-shelled organisms a1
64 Assigning Numeric Ages to Timescale Date a volcanic layer Date a dike or clasts b Bracket fossilbearing bed by dating volcanic units
65 Using Timescale to Assign Numeric Ages Use fossils and timescale to assign numeric age Bracket using fossil ages from timescale c Bracket age using fossil and numeric ages
66 Evidence that Earth s History is Not Short Tree rings Varves b Current rates of plate motion
67 Where Age of Earth Comes From Age of meteorites Dated Moon rocks Oldest dates on Earth rocks 4.55 billion 4.5 billion 3.9 to 4.0 b.y. (rock) to 4.3 b.y. (grains) Data from astronomy on age of Solar System and Universe d
68 Precambrian Life Stromatolites Bacteria Cambrian Explosion Trilobites Brachiopods a
69 Life in the Paleozoic Early Paleozoic Middle Paleozoic Late Paleozoic c
70 Life in the Mesozoic Early Mesozoic: Triassic Middle Mesozoic: Jurassic Late Mesozoic: Cretaceous a
71 Life in the Cenozoic Early Cenozoic Late Cenozoic c
72 On this geologic map, features are numbered in the order they occurred. Identify reasons why the units and features are interpreted to have formed in this relative order Sand 4 11 Scoria Cone 9? 11 Lava Flow 7 Sand 8 10 Fault c1 3 1 Granite
73 Observe each figure and think about how the information is important in determining potential for geologic hazards a Younger lava flow Older lava flow Fresh scarp Lava flow covering scarp High terrace Eroded scarp High terrace
74 Observe this satellite image of the Grand Canyon a
75 Geologic History of Grand Canyon, Part a5
76 Geologic History of Grand Canyon, Part a5
77 Observe this stratigraphic section and match the units and unconformities with the sections in the photographs Upper unconformity Late Paleozoic Middle Paleozoic Early Paleozoic Early Paleozoic Late Paleozoic Middle Paleozoic Early Paleozoic Late Precambrian Lower unconformity Precambrian basement Late Precambrian Precambrian basement a
78 Grand Canyon to Zion to Bryce
79 Cambrian on PC Unkar Group
80 Angular Unconformity: Grand Canyon, Tapeats on Grand Canyon Group
81 Paleozoic sedimentary rocks overlying Proterozoic Grand Canyon Group overlying Vishnu Schist
82 Geologic Time Scale
83 Nonconformity: Tintic Sandstone on Precambrian granite
84 1998 geologic time scale
85
86 Naming periods
87 Grand Canyon
88 Tapeats Ss on Vishnu Schist
89 Formations in the Grand Canyon
90 Grand Canyon
91 General Formations in Grand Canyon
92 Grand Canyon sequence of events
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