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Evidence of Erosion and Deposition. Sarah Fink Minerva Central School 2006. Agents of Erosion. Running water Wind Ice (Glaciers) Gravity Waves. http://people.csail.mit.edu/manoli/gallery/goldengate/waves.jpg
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Evidence of Erosion and Deposition Sarah Fink Minerva Central School 2006
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
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.
Example 1 Answer
Example 2 Answer
Example 3 Answer
Example 4 Answer
Example 5 Answer
Example 6 Answer
Example 7 Answer
Example 8 Answer
Example 9 Answer
Example 10 Answer
Example 11 Answer
Example 12 Answer
Challenge Question: Answer
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.
Abrasion of stream bed (can form potholes) Dissolution Scour (lifting of loose particles) Sandbars Point bars Meanders Floodplains Levees Deltas Alluvial fans Running Water
Water erosion – dry streambed Stream gully Dry delta http://www.bioschool.co.uk/bioschool.co.uk/images/images/water%20erosion_JPG_JPG.jpg
Water erosion – river rock http://www.ecotrust.org/copperriver/crks_cd/content/pages/photographs/images/ riverrock.jpg
Water erosion – kettle holes http://www.alabamaatheist.org/naturalism/graphics/040607_017.jpg
Water erosion - Grand Canyon Colorado River http://www.grand-canyon-tours.biz/Grand%20Canyon%203.jpg
Water erosion on Mars? http://nmp.jpl.nasa.gov/ds2/mission/images/water-erosion.gif
Deflation Abrasion Dunes Loess (layers of fine silt) Wind
Wind erosion - ventifacts Flat sides show the prevalent wind direction http://www.uwgb.edu/dutchs/EarthSC202Slides/windslid.htm
Wind erosion – sand dunes http://www.ncdc.noaa.gov/paleo/drought/images/sanddune_thumbnail.jpg
Wind erosion – ripple marks http://academic.emporia.edu/aberjame/struc_geo/primary/prim17.jpg
Wind erosion – desert pavement http://www.uwgb.edu/dutchs/geophoto/aeolian/DPAVMT1.jpg
Wind erosion in Antarctica http://www.uwgb.edu/dutchs/geophoto/aeolian/ANTVACX.jpg
Wind erosion http://www.yorkshirewalks.org/diary/nidd2/2008.jpg
Wind erosion – Sahara Desert http://www.cosmicharmony.com/Ia/NaturWnd/Sahara.jpg
Wind-eroded rocks in Zion, UT http://www.solarnet.org/Travel/US/Rock15MV.jpg
Sand dunes on Mars http://images.spaceref.com/news/2004/2004.08.09.R1601009.gif
Ice wedging/Gravity Abrasion (striations, scouring, polishing) Plucking (carrying loose sediment) Till Moraine Drumlin Meltwater deposits Ice/Glaciers
Glacial erosion – striations Striations (scratches) are parallel http://gemini.oscs.montana.edu/~geol445/hyperglac/eroproc1/boulderstriea2.JPG
Glacial erosion – striations http://tauceti.sfsu.edu/~chris/wonderland/manoj087.jpg
Glacial erosion – polish and erratic http://www.tarol.com/cathedral_erratic_glacial_polish.JPG
Ice wedging http://www.visualsunlimited.com/images/ watermarked/112/112071.jpg http://facweb.bhc.edu/academics/science/harwoodr/GEOL101/Study/Images/ icewedge.jpg
Hoodoos – stone columns Find out more! End Quiz http://www.cornellcollege.edu/geology/rdenniston/Texas%20pics/tent%20rocks.jpg http://www.izix.com/personal/travel/utah/images/hoodoos-w.jpg
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
Slump Rock fall Landslide / debris flow Creep Solifluction (in areas with permafrost) Talus Gravity – Mass Wasting
Gravity as agent of erosion http://www.enhg.org/gallery/shams/shams11.jpg
Rock slides in Alaska http://www.alaskahunts.net/alaska/hikingonslide.JPG
Gravity – talus slopes at cliff base http://www.kidscosmos.org/kid-stuff/mars-trip-graphics/talus-boulders-18-2p.jpg
Soil creep caused by gravity http://www.mountainnature.com/images/Geology/Large/SoilCreep01.jpg
Solifluction – due to permafrost Alternate seasons of freezing and thawing of saturated permafrost results in gradual soil movement downhill. http://www.fettes.com/Cairngorms/images/solifluction_siberia.jpg