• Title/Summary/Keyword: subvertical cliff

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Geological Environments, and Deterioration States and Causes on the Carved Buddhist Triad on Rock-cliff in Sinamri, Yeongju (영주 신암리 마애삼존석불에 대한 지질환경과 훼손상태 및 원인)

  • Hwang, Sang-Koo;Lee, Sang-Jin;Kim, Jae-Ho
    • The Journal of the Petrological Society of Korea
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    • v.17 no.2
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    • pp.95-107
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    • 2008
  • The Carved Buddhist Triad on Rock-cliff in Sinarnri (Treasure No. 680) consists of biotite granodiorite, which were positively carved on fore and west planes of four subvertical cliffs by two joint sets of NE-SW and NNW-SSE directions. The cliffs are $N50^{\circ}E\;85^{\circ}SE$ in fore plane, $N25^{\circ}W\;90^{\circ}$ in west plane, $N40{\sim}50^{\circ}E\; 82{\sim}85^{\circ}NW$, back plane, $N20^{\circ}W\;75^{\circ}SW$ in east plane, which are parallel to two joint sets of NE-SW and NNW-SSE directions in geology around it. The chemical index of alteration ranges 60.3 to 62.0 from the major elements in the rock that was weathered into producing kaolin minerals from alteration of feldspars and biotite. The Buddhist image has been deteriorated into joints, brown rusts, discolorations and granular disintegrations by such deterioration causes as deformation, moisture, temperature variation and microorganic living. The moisture, which leaks from groundwater in the rock, dissolve to decompose minerals.