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Rock Art Stability Index Field Study Niccole Villa Cerveny Mesa Community College Niccole Villa Cerveny Mesa Community College
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What is Rock Art Petroglyphs - images pecked or scratched into rock surfaces Pictographs - images painted on rock surfaces Rock Alignments/Geoglyphs - rocks placed in alignment to form images Intaglios - removal of desert pavement to create images on the ground Petroglyphs - images pecked or scratched into rock surfaces Pictographs - images painted on rock surfaces Rock Alignments/Geoglyphs - rocks placed in alignment to form images Intaglios - removal of desert pavement to create images on the ground
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Petroglyphs N. Cerveny © 2005
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Pictographs J McFaul © 2002
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Geoglyphs/rock alignments N. Cerveny © 2005
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Intaglios N. Cerveny © 2005
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So why do we need a rock art panel stability index?
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Weathering/Erosion Refresher Geomorphology - study of the changing shape of the earth Weathering - the breakdown of rock “in situ” (in place) Erosion - the transport of weathered material Weathering is the beginning to changing the shape of the earth Geomorphology - study of the changing shape of the earth Weathering - the breakdown of rock “in situ” (in place) Erosion - the transport of weathered material Weathering is the beginning to changing the shape of the earth
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Rock Art Stability Index Setting the stage of the landscape Stone preparing for detatchment Incremental loss of stone material Loss of chunks (break-off of stone) Rock Coatings Setting the stage of the landscape Stone preparing for detatchment Incremental loss of stone material Loss of chunks (break-off of stone) Rock Coatings
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Character Value Examine a panel for each weathering form, then score 0 to 3 O = not present 1 = Barely noticeable 2 = Obvious 3 = Very Serious Concern ***There are no 1/2-sies Examine a panel for each weathering form, then score 0 to 3 O = not present 1 = Barely noticeable 2 = Obvious 3 = Very Serious Concern ***There are no 1/2-sies
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Setting the Stage: Fissures & Rock Weaknesses Fissures independent of stone lithification Fissures dependent on stone lithification Changes in textural anomalies Rock weaknesses (Moh’s) Fissures independent of stone lithification Fissures dependent on stone lithification Changes in textural anomalies Rock weaknesses (Moh’s)
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Preparing for Detatchment Fissuresol future location Roots Plant growth near or on panel Scaling Splintering Undercutting Weathering-rind development Other forms indicating future detachment Fissuresol future location Roots Plant growth near or on panel Scaling Splintering Undercutting Weathering-rind development Other forms indicating future detachment
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Loss of stone material incrementally Abrasion from sediment Anthropogenic cutting Aveolization Crumbly Disintigration Flaking Granular disintigration Loss parallel to stone structure Lithobiont Pitting Lith release of Wx- rind “dam” Rock Coating Detachment Rounding of Glyph Edges Scaling Textural anomalies erode differently Splintering Other forms of incremental loss Lith release of Wx- rind “dam” Rock Coating Detachment Rounding of Glyph Edges Scaling Textural anomalies erode differently Splintering Other forms of incremental loss
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Loss of Stone by breaking-off chunks Anthropogenic Activity Fissuresol/cal crete wedging Fire Undercutting Other natural causes of break- off
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Rock Coatings & Other Deposits Anthropogenic Rock Coatings Case Hardening* Efflorescence/ Subflorescence Anthropogenic Rock Coatings Case Hardening* Efflorescence/ Subflorescence
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Rock Coatings Dust Coatings Droppings Heavy Metal Iron Film Lithobionts Oxalate Rock Varnish Silica Glaze Unclassified Combinations of different types Dust Coatings Droppings Heavy Metal Iron Film Lithobionts Oxalate Rock Varnish Silica Glaze Unclassified Combinations of different types
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South Mountain Municipal Park Box Canyon Central Entrance Metro-Phoenix (Granite)
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Deer Valley Rock Art Center, Metro-Phoenix (Basalt)
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Grand Canyon, Tanner Rapids (Sandstone)
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Waterfall Canyon, Metro-Phoenix Whitetank Mountains (Granite)
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Homolovi Ruins, Northern Arizona (Sandstone)
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Tempe Butte Site (Andesite)
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