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geologists use a variety of primary sedimentary structures to work out the direction of young Inge or the way up direction in rocks these rocks specimens show trace fossils formed when burrowing organisms like worms buried it into soft sediment on this bedding plane you can see raised rims of the circular vertical burrows that were made by organisms in this specimen the nearly vertical burrows can be easily picked out because they have a silvery appearance the silvery color is produced by tiny flakes of muscovite mica which appear to line the burrow the burrows extend down from this top surface and end at approximately the same depth below the surface in the field if you are recording way up on a sketch of this sedimentary structure you would indicate the young-in direction with this symbol
