Friday, December 3, 2010
décollement
A décollement horizon in tectonics is a surface that acts as a gliding plane between two masses in a thrust fault relationship. A décollement horizon can either form due to a low bulk modulus between bodies (usually in lithologies such as marls, shales and evaporites), or can form along planes of high pore pressures.
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Solastalgia
Solastalgia ( / ˌ s ɒ l ə ˈ s t æ l dʒ ə / ) is a neologism , formed by the combination of the Latin words sōlācium (solace or comfort)...
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Epigraphy (from the Greek : ἐπιγραφή epi-graphē , literally "on-writing", "inscription") is the study of inscriptions ...
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Après-ski ( French : after skiing ) refers to going out, having drinks, dancing, and generally socializing after skiing . It is popular in ...
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