Scientists at the National Museum of Natural History involved in classification of Antarctic finds said the mineralogy, texture and the oxidized nature of the rock are unmistakably Martian.
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This suggests that the predominantly bedrock hillslopes erode very slowly and sediment is transferred very gradually in most regions within Death Valley.
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A more technical online introduction with a bit of math from National Science Foundation is SESTAT's Understanding Sampling Errors and What is the Margin of Error. News Release of January 29, 2004 - "Maryland Security Study Validates Diebold Election Systems Equipment for March Primary." URL:
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