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Evidence of Erosion and Deposition Sarah Fink Minerva Central School 2006
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Agents of Erosion Running water Wind Ice (Glaciers) Gravity Waves http://people.csail.mit.edu/manoli/gallery/goldengate/waves.jpg http://www.peterbindon.com/Photography/Images-Photography/Landscape/Running_Water.jpg http://www.uwsp.edu/geo/faculty/ritter/images/lithosphere/glacial/piedmont_glacier_Baffin_GSC_2crev.jpg http://www.me3.org/issues/wind/zondturbines.jpg http://usuarios.cmg.com.br/~hp-adrenace/adrena2.jpg
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Quiz Yourself! For each of the following 13 pictures, write down the major agent(s) of erosion. Remember, your choices are: –Running water –Wind –Ice (Glaciers) –Gravity –Waves Note: sources for photos in the quiz are noted in the answers.
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Example 1 Answer
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Example 2 Answer
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Example 3 Answer
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Example 4 Answer
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Example 5 Answer
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Example 6 Answer
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Example 7 Answer
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Example 8 Answer
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Example 9 Answer
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Example 10 Answer
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Example 11 Answer
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Example 12 Answer
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Challenge Question: Answer
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How Did You Do?? Even if you didn’t get all of the answers correct, you should be able to recognize some patterns for the agents of erosion we discussed. Let’s see some more pictures and come up with some “rules” for identifying and classifying eroded rocks.
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Running Water Abrasion of stream bed (can form potholes) Dissolution Scour (lifting of loose particles) Sandbars Point bars Meanders Floodplains Levees Deltas Alluvial fans
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Water erosion – dry streambed http://www.bioschool.co.uk/bioschool.co.uk/images/images/water%20erosi on_JPG_JPG.jpg Stream gully Dry delta
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Water erosion – river rock http://www.ecotrust.org/copperriver/crks_cd/content/pages/photographs/images/ riverrock.jpg
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Water erosion – kettle holes http://www.alabamaatheist.org/naturalism/graphics/040607_017.jpg
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Water erosion - Grand Canyon http://www.grand-canyon-tours.biz/Grand%20Canyon%203.jpg Colorado River
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Water erosion on Mars? http://nmp.jpl.nasa.gov/ds2/mission/images/water-erosion.gif
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Characteristics of erosion by running water:
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Wind Deflation Abrasion Dunes Loess (layers of fine silt)
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Wind erosion - ventifacts http://www.uwgb.edu/dutchs/EarthSC202Slides/windslid.htm Flat sides show the prevalent wind direction
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Wind erosion – sand dunes http://www.ncdc.noaa.gov/paleo/drought/images/sanddune_thumbnail.jpg
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Wind erosion – ripple marks http://academic.emporia.edu/aberjame/struc_geo/primary/prim17.jpg
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Wind erosion – desert pavement http://www.uwgb.edu/dutchs/geophoto/aeolian/DPAVMT1.jpg
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Wind erosion in Antarctica http://www.uwgb.edu/dutchs/geophoto/aeolian/ANTVACX.jpg
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Wind erosion http://www.yorkshirewalks.org/diary/nidd2/2008.jpg
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Wind erosion – Sahara Desert http://www.cosmicharmony.com/Ia/NaturWnd/Sahara.jpg
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Wind-eroded rocks in Zion, UT http://www.solarnet.org/Travel/US/Rock15MV.jpg
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Sand dunes on Mars http://images.spaceref.com/news/2004/2004.08.09.R1601009.gif
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Characteristics of erosion by wind:
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Ice/Glaciers Ice wedging/Gravity Abrasion (striations, scouring, polishing) Plucking (carrying loose sediment) Till Moraine Drumlin Meltwater deposits
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Glacial erosion – striations http://gemini.oscs.montana.edu/~geol445/hyperglac/eroproc1/boulderstriea2.JPG Striations (scratches) are parallel
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Glacial erosion – striations http://tauceti.sfsu.edu/~chris/wonderland/manoj087.jpg
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Glacial erosion – polish and erratic http://www.tarol.com/cathedral_erratic_glacial_polish.JPG
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Ice wedging http://facweb.bhc.edu/academics/science/harwoodr/GEOL101/Study/Images/ icewedge.jpg http://www.visualsunlimited.com/images/ watermarked/112/112071.jpg
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Hoodoos – stone columns http://www.cornellcollege.edu/geology/rdenniston/Texas%20pics/tent%20rocks.jpg http://www.izix.com/personal/travel/utah/images/hoodoos-w.jpg Find out more! End Quiz
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Formation of Bryce Canyon A combination of frost wedging and rainwater are the sources of weathering and erosion that cause the “hoodoo” formations found in Bryce Canyon, Utah. “Acid” rain formed by carbon dioxide in the atmosphere dissolves the weaker calcite-based limestone, but the stronger mudstone, siltstone, and dolomite layers weather more slowly. This results in the layering found in the rock formations. The average rate of erosion is 2-4 feet per 100 years. http://www.nps.gov/brca/geology_hoodoos.html
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Characteristics of erosion by ice:
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Gravity – Mass Wasting Slump Rock fall Landslide / debris flow Creep Solifluction (in areas with permafrost) Talus
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Gravity as agent of erosion http://www.enhg.org/gallery/shams/shams11.jpg
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Rock slides in Alaska http://www.alaskahunts.net/alaska/hikingonslide.JPG
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Gravity – talus slopes at cliff base http://www.kidscosmos.org/kid-stuff/mars-trip-graphics/talus-boulders-18-2p.jpg
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Soil creep caused by gravity http://www.mountainnature.com/images/Geology/Large/SoilCreep01.jpg
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Solifluction – due to permafrost http://www.fettes.com/Cairngorms/images/solifluction_siberia.jpg Alternate seasons of freezing and thawing of saturated permafrost results in gradual soil movement downhill.
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Characteristics of erosion by gravity:
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Waves (shoreline) Waves, tides, currents Pounding Abrasion Pressure Dissolution Scour Cliffs, arches, platforms, caves, stacks Beaches Barrier islands Spits Sandbars Bay-mouth bars Tombolos
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Beach erosion by waves http://people.albion.edu/KAT10/dp/beach%20erosion.jpg http://epod.usra.edu/archive/images/roll 1dx-21.jpg
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Sea arches and stacks http://gpc.edu/~pgore/Earth&Space/erosion.html http://www.nps.gov/pwro/piso/minkstdy/images/stacks.jpg Wave action and changing tides cause these formations
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Ripple marks – wave action http://www.downtheroad.org/images/Photo%20Album/New_Folder7/DSC00091.JPG
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Ancient ripple marks preserved in sedimentary rock http://www.calstatela.edu/faculty/acolvil/sediment/giant_ripples.jpg
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Characteristics of erosion by waves:
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Glacial till and outwash (deposited soil) http://www.hi.is/~oi/Water%20erosion%20alongside%20a%20flute%20on%20 Kringilsarrani%20.JPG
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