| 1. | He defined the end as being marked by Lower Palaeozoic red beds.
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| 2. | The resulting Cutler red beds are made of iron-rich arkose sandstone.
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| 3. | The basin is made of sandstone, siltstone, mudstone, coal, shale, and red beds.
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| 4. | The continental red beds of the Permian rest unconformably on the Transitional Layers.
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| 5. | Secondary red beds formed in this way are an excellent example of telodiagenesis.
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| 6. | A soft formation includes unconsolidated sands, clays, soft limestones, red beds and shale.
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| 7. | The Bloomsburg Red Beds, a red shale, are at the gap under Dunsfield Creek.
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| 8. | Secondary red beds are characterized by irregular color zonation, often related to sub-unconformity weathering profiles.
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| 9. | The red beds of the Nankoweap Formation unconformably overlie the Cardenas Lavas of the Unkar Group.
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| 10. | There are some Permian to Triassic red beds, starting with conglomerate and thinning to sandstone and lutite.
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