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More model informationFound only within the reddish-brown Entrada Sandstone, goblins are composed of sandstone interbedded with and underlain by shale and siltstone. Though now an erosional island, the beds that form this goblin were once laterally continuous. Below the goblin, bedding is masked by a veneer of soil, called colluvium.. http://files.geology.utah.gov/online/pdf/pi-65.pdfC
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