Ophiolite rocks are heaviest rock in the crust but they are found on the high mountain due to obduction. Their heaviness is against isostatic theories because these theories clearly indicate that high mountain must be comprised of light rocks. Therefore the ophiolite obduction and its occurrence on high mountain is strongly suspicious. My recent researches, in Iraqi Zagros, proved that what are called ophiolite rocks are metamorphosed greywackes ( impure sandstones)