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Earth History Dating geologic events like volcanic eruptions, uplift, subsidence, deposition, impacts, intrusion, ice ages, etc.

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Presentation on theme: "Earth History Dating geologic events like volcanic eruptions, uplift, subsidence, deposition, impacts, intrusion, ice ages, etc."— Presentation transcript:

1 Earth History Dating geologic events like volcanic eruptions, uplift, subsidence, deposition, impacts, intrusion, ice ages, etc

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6 Geologic Age Dating Relative Age Dating –Places events in a sequence –Only indicates one is older than other Absolute Age Dating –Also called: Radiometric/Radio- active Dating –Identifies actual age

7 Relative Age Dating rules/laws to follow when dating rocks Uniformitarianism Law of Original Horizontality Law of Superposition Law of Cross-cutting Relationships Law of Include Fragments Unconformities

8 Relative Age Dating Uniformitarianism –“The present is the key to the past” James Hutton –Geologic events are not catastrophic

9 Relative Age Dating Original Horizontality –sedimentary rocks form horizontal to the surface of the earth. –Sedimentary rocks usually form below sea- level

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11 SEDIMENTARY ROCKS 75% of the Earth’s surface –sed Usually form below sea level form from the compaction and cementation of sediments (lithification) Weathering (breakdown of rock)  Sediment (fragments of rock)  Erosion (movement/transport of sediment)  Deposition (settling of sediment)  Burial  Compaction (pushing together of sediment  Cementation (gluing of sediments) http://www.westhamptonbeach.k12.ny.us/Teachers/cohen/sciweb/earthscience/powerpoint_notes/powerpoint_notes.htm

12 Properties of Sedimentary Rocks Layers/Strata Fragments of other rocks Fossils – remains/impression of organism Compacted crystals

13 Environment of Formation Types of fossils (marine, freshwater) Size and shape of sediment Layers/Strata of sediment, ripple marks

14 http://www.classzone.com/books/earth_scien ce/terc/content/visualizations/es2901/es2901 page01.cfm?chapter_no=visualization Fossil forming http://www.classzone.com/books/earth_scien ce/terc/content/visualizations/es0701/es0701 page01.cfm?chapter_no=visualization (coal forming) http://www.classzone.com/books/earth_scien ce/terc/content/visualizations/es0604/es0604 page01.cfm?chapter_no=visualization (sediments being deposited http://www.coaleducation.org/miningtv/default.htm Coal mining videos http://www.wwnorton.com/college/geo/egeo/animations/ch12.htm Shale becomes oil http://highered.mcgraw- hill.com/sites/0072402466/student_view0/chapter 10/animations_and_movies.html# Sediment transport http://www.classzone.com/books/earth_science/terc/content/visualizations/es0605/es0 605page01.cfm?chapter_no=visualizationhttp://www.classzone.com/books/earth_science/terc/content/visualizations/es0605/es0 605page01.cfm?chapter_no=visualization cementation

15 http://www.eram.k12.ny.us/education/sctemp/0c525861b50e177dace8b634d0e0d5f7/ 1203603040/sedimentary.swf Burrows

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18 Relative Age Dating Superposition –Oldest at bottom –Youngest at top

19 Relative Age Dating Cross-cutting –Younger rocks (igneous intrustions/extrustions) or structures (folds, faults) cross-cut older rock

20 Complex Bedrock Structures Intrusions Folding (bending) Faulting (break) Tilting

21 Faults, folding, tilting Folding (bending) Tilting

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24 Relative Age Dating Include Fragments –Sediment in the rock must be older than the rock itself –Ex: conglomerate

25 Relative Age Dating Unconformity –A buried break or gap in rock sequence –Missing rock record –Caused by: erosion Lack of deposition

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28 http://www2.wwnorton.com/college/geo/egeo/flash/10_2.swf http://www2.wwnorton.com/college/geo/egeo/flash/10_1.swf

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49 http://geography.cst.cmich.edu/Franc1M/Animations/animation_list_posted.htm alphabetical list of animations all different topics – animations http://earthguide.ucsd.edu/earthguide/diagrams.html !http://earthguide.ucsd.edu/earthguide/diagrams.html http://emvc.geol.ucsb.edu/downloads.php 9ice age, plate tectonics,etchttp://emvc.geol.ucsb.edu/downloads.php differnt topics – found 4/24/08 Earth History http://simile.mit.edu/timeline/examples/dinosaurs/dinosaurs2.html you can also make your own interactive timeline (tedious though) http://simile.mit.edu/timeline/docs/create-timelines.html#getting-started http://simile.mit.edu/timeline/examples/dinosaurs/dinosaurs2.html http://simile.mit.edu/timeline/docs/create-timelines.html#getting-started Earth History http://www.nmnh.si.edu/paleo/geotime/main/index.html geo time linehttp://www.nmnh.si.edu/paleo/geotime/main/index.html http://www.indiana.edu/~ensiweb/home.html http://www.indiana.edu/~ensiweb/evol.fs.html evolutionhttp://www.indiana.edu/~ensiweb/home.html http://www.indiana.edu/~ensiweb/evol.fs.html You can get glossaries at http://www.litstudies.com/bilingual_esl/BilingualGlossaries/index.htm The main part of the screen will be white, but you can click on the languages on the left. It is actually from the remains of the http://www.litstudies.com/bilingual_esl/index.htm and then http://www.litstudies.com/bilingual_esl/BilingualGlossaries/index.htm http://www.litstudies.com/bilingual_esl/index.htm http://www.gly.uga.edu/railsback/GeologicalDiagrams1.html geology diagramshttp://www.gly.uga.edu/railsback/GeologicalDiagrams1.html

50 Sedimentary Rocks Texture (3 types) 1. Clastic – fragments of rocks cemented Land-derived sediments eroded, and deposited(usually in water), buried, compacted and cemented. Ex: sandstone 2. Crystalline (Chemical) – compacted minerals Dissolved minerals/salts precipitate out of water, settle, buried, compacted and cemented 3. Bioclastic (organic) – have fossils (shells, plant matter) Form from something once living ex: coal, coral http://www.wiley.com/college/strahler/0471480533/animations/ch12_animations/animation2.html

51 CLASTIC CRYSTALLINE BIOCLASTIC

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54 http://geography.cst.cmich.edu/Franc1M/Animations/animation_list_posted.htmhttp://geography.cst.cmich.edu/Franc1M/Animations/animation_list_posted.htm - go to watersheds MISS


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