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Interpreting Earth’s Rocks to Determine Its Past History. Geologic time Relative dating. Geologic Time. Relative Dating - sequence of geologic events in a region (order of past events) How do we know how old something is?. Law of Superposition. Oldest layer on bottom (if undisturbed).
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Interpreting Earth’s Rocks to Determine Its Past History Geologic timeRelative dating
Geologic Time • Relative Dating - sequence of geologic events in a region (order of past events) • How do we know how old something is?
Law of Superposition • Oldest layer on bottom (if undisturbed) http://www.angelfire.com/az3/mohgameil/Layering4.jpg
The Grand Canyon http://www.calstatela.edu/faculty/acolvil/sediment/superposition.jpg
Principle of Original Horizontality • Sediments are originally deposited as horizontal (or near horizontal) beds Use for tilted or bent layers
POH • What can cause rock to bend?
Cross-Cutting Relationships • An igneous intrusion (or fault) is younger than the rock layers that it cuts across. These are younger than the surrounding rock youngest fault oldest
Cross-Cutting Relationships Igneous dike is younger than the marble layer it cuts across.
Cross-Cutting Relationships 6 is younger than1, 2, or 3 because it cuts across them!
Law of inclusions • The inclusion is older than the rock it is in • Rock type?
Which pair is older?Which law is used? A & B _________________ D & M _________________ D & E _________________J & K _________________
James Hutton: The father of modern geology (1726-1797) Uniformitarianism: processes acting on earth today (volcanism, erosion, plate tectonics, etc.) have done so in the past “The present is the key to the past.” Basis of relative dating
Angular Unconformities • Folded layers below horizontal layers. rock layers are eroded new horizontal layers are deposited angular unconformity (rock layers have been eroded away)
Angular Unconformity sedimentary rocks above and below unconformity surface with rocks below tilted at an angle F E D C B A
Nonconformity – younger sedimentary rocks rest on older igneous rocks sedimentary rock layers Cambrian Precambrian Granite
Disconformity DISCONFORMITY:Missing rock layers (sedimentary) Very hard to pick out
limestone shale sandstone granite http://www.env.duke.edu/eos/geo41/st013.gif
Resources • http://courses.geo.ucalgary.ca/glgy209L03/docs/Lecture15_GLGY209_six.pdf • http://perth.uwlax.edu/faculty/stoelting/Intro/Guides/Images2/law_of_superposition_b.jpg • http://www.science.sjsu.edu/scied/255/ppt/superposition/img025.jpg • http://www.gpc.peachnet.edu/~jsummero/Cross-cutting-a.jpg • http://www.gc.maricopa.edu/appliedscience/gjc-nsf/images/CRH0204.JPG • http://maverick.gc.maricopa.edu/appliedscience/gjcweb/geomap/images/ang.unconf.jpg • http://www.geog.ouc.bc.ca/physgeog/contents/images/hutton.jpg • http://www.bigbendpaleo.com/Photo%20Gallery/Big%20Bend%20Region,%20Texas/Big%20Bend%20National%20Park%20-%20Syncline%20-%20Javalina%20Creek%20-%2020%20June%201995.jpg • http://geoimages.berkeley.edu/GeoImages/Johnson/Images/Large/CD3/028.jpg • http://www.vvdailypress.com/travel/rainbow/images/rock.jpg • http://academic.emporia.edu/aberjame/struc_geo/folds/fold06.jpg • http://www.geology.pitt.edu/images/folds.jpg • http://faculty.evansville.edu/de3/b39902/PPoint/Geologic%20Time/img007.jpg • http://www.photo.net/photo/pcd2882/grand-canyon-region-aerial-85.3.jpg • http://www.cowanstark.com/horsehoe-bend.jpg • http://home.flash.net/~alanm52/Cross_cutting.jpg • http://www-class.unl.edu/geol101i/images/igneous%20images/Black%20Canyon%20Gunnison.jpg • http://freespace.virgin.net/craven.pendle/stratigraphy/unconformity.jpg
http://comp.uark.edu/~sboss/siccar.jpg • http://www.pittstate.edu/services/scied/Teachers/Field/Camp/Us67-1/us67cut.jpg • http://maverick.gc.maricopa.edu/appliedscience/gjcweb/geomap/images/MW8-11.jpg • http://www3.uakron.edu/geology/Foos/parks/rmgcan2.html • http://www.ldeo.columbia.edu/edu/dees/ees/ies2/slides/disconformity.gif • http://geology.lssu.edu/NS102/images/figure%2009-06.gif • http://www.crienterprises.com/C-Assets/J-Hanifa-Unconf-W-Birk.jpg • http://www.uoguelph.ca/~sadura/stgref/stg32b.gif • http://www.geo-outdoors.info/images/eye_protection.jpg • http://enterprise.cc.uakron.edu/geology/natscigeo/Lectures/time/gtime1.htm