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<p><a href="page.php?w=limestone">limestone</a>, or some combination of these sedimentary rocks. The ferric oxides, which are responsible for the red color of red beds, typically occur as a coating on the grains of sediments comprising red beds. Classic examples of red beds are the <a href="page.php?w=Permian">Permian</a> and <a href="page.php?w=Triassic">Triassic</a> strata of the western United States and the <a href="page.php?w=Devonian">Devonian</a> <a href="page.php?w=Old_Red_Sandstone">Old Red Sandstone</a> <a href="page.php?w=facies">facies</a></p><p>
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