Interpreting Earths Rocks to Determine Its Past History

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Interpreting Earth’s Rocks to Determine Its Past History

Interpreting Earth’s Rocks to Determine Its Past History

Determining Geologic History: Geologists are like CSI detectives wanting to know Where? , When?

Determining Geologic History: Geologists are like CSI detectives wanting to know Where? , When? , Why? , How? Sometimes very little “evidence” remains (exposure, erosion) Evidence has been moved or tampered with! Rocks have been moved (faults, folds) Usually no witnesses!

Geologic Time • Relative dating - sequence of geologic events in a region (order

Geologic Time • Relative dating - sequence of geologic events in a region (order of past events) • (not dating your cousin )

Principle of Superposition • Oldest layer on bottom (if tectonically undisturbed) Younger Older http:

Principle of Superposition • Oldest layer on bottom (if tectonically undisturbed) Younger Older http: //www. angelfire. com/az 3/mohgameil/Layering 4. jpg

Principle of Superposition In horizontal rock layers, the oldest and first formed is on

Principle of Superposition In horizontal rock layers, the oldest and first formed is on the bottom. 5 is the youngest because it is on the top, closest to the surface.

The Grand Canyon http: //www. calstatela. edu/faculty/acolvil/sediment/superposition. jpg

The Grand Canyon http: //www. calstatela. edu/faculty/acolvil/sediment/superposition. jpg

Principle of Original Horizontality • Rock are originally deposited horizontal Folding happened AFTER rocks

Principle of Original Horizontality • Rock are originally deposited horizontal Folding happened AFTER rocks were deposited

folded rock layers = compression by tectonic activity

folded rock layers = compression by tectonic activity

Cross-Cutting Relationships • An igneous intrusion (or fault) is younger than the rock layers

Cross-Cutting Relationships • An igneous intrusion (or fault) is younger than the rock layers that it cuts across. youngest fault oldest These are younger than the surrounding rock

practice

practice

Law of Inclusions

Law of Inclusions

Index fossils • Fossils that lived for a short time can be used to

Index fossils • Fossils that lived for a short time can be used to date layers • Found world wide • Examples?

James Hutton: The father of modern geology (1726 -1797) Uniformitarianism: “The present is the

James Hutton: The father of modern geology (1726 -1797) Uniformitarianism: “The present is the key to the past. ” ? ? ? ? ?

Examples of uniformitarianism • Petoskey stones • Earthquake location • Striations • Rock formation

Examples of uniformitarianism • Petoskey stones • Earthquake location • Striations • Rock formation • Paleoclimates • What else?

Order the layers 1 -7

Order the layers 1 -7

Unconformities = “Missing Time” • Result of erosion

Unconformities = “Missing Time” • Result of erosion

Angular Unconformities • Folded layers on bottom, flat layers on top rock layers are

Angular Unconformities • Folded layers on bottom, flat layers on top rock layers are eroded new horizontal layers are deposited angular unconformity (rock layers have been eroded away)

Angular Unconformity F E D C B A

Angular Unconformity F E D C B A

Nonconformity – igneous rocks on bottom; overlain by sedimentary rocks sedimentary rock layers Cambrian

Nonconformity – igneous rocks on bottom; overlain by sedimentary rocks sedimentary rock layers Cambrian Precambrian Granite

Nonconformity

Nonconformity

Disconformity DISCONFORMITY: Missing rock layers (sedimentary) Very hard to see

Disconformity DISCONFORMITY: Missing rock layers (sedimentary) Very hard to see

Disconformities

Disconformities

Let’s Play…. Name the UNCONFORMITY!

Let’s Play…. Name the UNCONFORMITY!

Siccar Point, Scotland

Siccar Point, Scotland

http: //www 001. upp. so-net. ne. jp/fl-fg/06 -02. htm

http: //www 001. upp. so-net. ne. jp/fl-fg/06 -02. htm

limestone shale sandstone granite http: //www. env. duke. edu/eos/geo 41/st 013. gif

limestone shale sandstone granite http: //www. env. duke. edu/eos/geo 41/st 013. gif

http: //www 001. upp. so-net. ne. jp/fl-fg/06 -02. htm

http: //www 001. upp. so-net. ne. jp/fl-fg/06 -02. htm

Resources • • http: //courses. geo. ucalgary. ca/glgy 209 L 03/docs/Lecture 15_GLGY 209_six. pdf

Resources • • http: //courses. geo. ucalgary. ca/glgy 209 L 03/docs/Lecture 15_GLGY 209_six. pdf http: //perth. uwlax. edu/faculty/stoelting/Intro/Guides/Images 2/law_of_superposition_b. jpg http: //www. science. sjsu. edu/scied/255/ppt/superposition/img 025. jpg http: //www. gpc. peachnet. edu/~jsummero/Cross-cutting-a. jpg • • http: //www. gc. maricopa. edu/appliedscience/gjc-nsf/images/CRH 0204. 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%20 Gallery/Big%20 Bend%20 Region, %20 Texas/Big% 20 Bend%20 National%20 Park%20 -%20 Syncline%20 -%20 Javalina%20 Creek%20%20 June%201995. jpg http: //geoimages. berkeley. edu/Geo. Images/Johnson/Images/Large/CD 3/028. jpg http: //www. vvdailypress. com/travel/rainbow/images/rock. jpg http: //academic. emporia. edu/aberjame/struc_geo/folds/fold 06. jpg http: //www. geology. pitt. edu/images/folds. jpg http: //faculty. evansville. edu/de 3/b 39902/PPoint/Geologic%20 Time/img 007. jpg http: //www. photo. net/photo/pcd 2882/grand-canyon-region-aerial-85. 3. jpg http: //www. cowanstark. com/horsehoe-bend. jpg http: //home. flash. net/~alanm 52/Cross_cutting. jpg http: //wwwclass. unl. edu/geol 101 i/images/igneous%20 images/Black%20 Canyon%20 Gunnison. 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/Us 67

• • • http: //comp. uark. edu/~sboss/siccar. jpg http: //www. pittstate. edu/services/scied/Teachers/Field/Camp/Us 67 -1/us 67 cut. jpg http: //maverick. gc. maricopa. edu/appliedscience/gjcweb/geomap/images/MW 8 -11. jpg http: //www 3. uakron. edu/geology/Foos/parks/rmgcan 2. html http: //www. ldeo. columbia. edu/dees/ies 2/slides/disconformity. gif http: //geology. lssu. edu/NS 102/images/figure%2009 -06. gif http: //www. crienterprises. com/C-Assets/J-Hanifa-Unconf-W-Birk. jpg http: //www. uoguelph. ca/~sadura/stgref/stg 32 b. gif http: //www. geo-outdoors. info/images/eye_protection. jpg • http: //enterprise. cc. uakron. edu/geology/natscigeo/Lectures/time/gtime 1. htm