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lime on some exposed surfaces. Down creek a short distance below where the stream turns northward about 200 ft (156 ft measured, balance estimated) occurs east of stream beneath the Lyons or part of it. It appears not as hard as that west of creek and is comparatively free of feldspar crystals. In the creek bed between these two exposures is a bed of thin bedded rather fine grained intensely red (dark) sandstone, 8 or 10 ft.? The relations are about thus ((drawing in field book)).
