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- |tree2=Aux Vases Sandstone |category7=Aux Vases Sandstone3 KB (516 words) - 22:57, 17 January 2017
- #Redirect[[Aux Vases Sandstone#Economic importance]]100 bytes (12 words) - 01:27, 22 October 2019
- |category7=Aux Vases Sandstone |tree2=Aux Vases Sandstone4 KB (606 words) - 21:35, 21 October 2019
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- #REDIRECT [[Aux Vases Sandstone ]]34 bytes (4 words) - 16:47, 27 April 2016
File:Figure M-23.jpg Fig. M-23 -- Thickness of the Aux Vases Sandstone.(1,069 × 1,599 (386 KB)) - 14:05, 4 April 2016- #Redirect[[Aux Vases Sandstone#Economic importance]]100 bytes (12 words) - 01:27, 22 October 2019
- |tree2=Aux Vases Sandstone |category7=Aux Vases Sandstone3 KB (516 words) - 22:57, 17 January 2017
- |tree2=Aux Vases Sandstone |category7=Aux Vases Sandstone2 KB (339 words) - 22:58, 17 January 2017
- ...is generally very fine grained and calcareous, resembling that of the Aux Vases. The shale is largely dark greenish gray, but red and green shales are comm2 KB (268 words) - 23:01, 17 January 2017
- |category7=Aux Vases Sandstone |tree2=Aux Vases Sandstone4 KB (606 words) - 21:35, 21 October 2019
- |category7=Aux Vases Sandstone |tree2=Aux Vases Sandstone3 KB (412 words) - 15:38, 18 January 2017
- ...ountain Member of the Ste. Genevieve (Valmeyeran) to the north and the Aux Vases (Valmeyeran) in most of its extent. ...the Ste. Genevieve Limestone to the north (fig. M-22) and that of the Aux Vases Sandstone to the south (fig. M-23). The outcrop area runs along and near th3 KB (372 words) - 16:27, 10 January 2017
- ...s Sandstone, excluding the Chesterian Series. However, because the sub-Aux Vases unconformity is confined to the margin of the basin and the Chesterian stra2 KB (270 words) - 20:27, 5 January 2017
- ...is generally very fine grained and calcareous, resembling that of the Aux Vases. The shale is largely dark greenish gray, but red and green shales are comm3 KB (352 words) - 15:52, 18 January 2017
- ...Cave Megagroup, except for minor erosional channels at the base of the Aux Vases Sandstone. It is separated from the overlying Pennsylvanian System by a maj ...the Ste. Genevieve Limestone to the north (fig. M-22) and that of the Aux Vases Sandstone to the south (fig. M-23). The outcrop area runs along and near th3 KB (446 words) - 16:00, 13 January 2017
- ...s Sandstone, excluding the Chesterian Series. However, because the sub-Aux Vases unconformity is confined to the margin of the basin and the Chesterian stra3 KB (351 words) - 20:59, 5 January 2017
- ...is lithology. The contact between the Ste. Genevieve and the overlying Aux Vases Sandstone is conformable, but it is marked by a series of downward steps to4 KB (593 words) - 22:59, 17 January 2017
- ...ut in western Washington County it thins and grades laterally into the Aux Vases Sandstone. The Karnak is generally 10-35 feet thick.2 KB (244 words) - 23:02, 17 January 2017
- ...was assigned to the Renault Limestone when it was found to overlie the Aux Vases Sandstone.2 KB (281 words) - 21:33, 17 January 2017
- ...western Washington County- the Spar Mountain grades laterally into the Aux Vases Sandstone and is separated from it by vertical cut-off.2 KB (329 words) - 15:20, 18 January 2017
- ...is lithology. The contact between the Ste. Genevieve and the overlying Aux Vases Sandstone is conformable, but it is marked by a series of downward steps to5 KB (728 words) - 15:19, 22 October 2019
- ...lier reports the Levias Member was miscorrelated with strata below the Aux Vases Sandstone and it was therefore classified as a member of the Ste. Genevieve2 KB (349 words) - 21:24, 17 January 2017
- ...ut in western Washington County it thins and grades laterally into the Aux Vases Sandstone. The Karnak is generally 10-35 feet thick.3 KB (338 words) - 21:50, 21 October 2019