Field Notebook: Texas 1957b
Page 293
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Transcription
166 upon this The dolostone are saccharial on weathered surface, the sole climbs about mid-size. Occasional molds of juvenicide or brachiopod but not preserved well enough for identification. A few horizons seem uplifted, but no apparent fossils. The lower carbonat is more a dolomite with considerable amounts silt & clay. This joins perhaps 600' at Brooks Ranch. Drive past Allison Ranch to outlying K and walked over to the Raymond outcrop just to the NE. Here the Raymond dips about 30° SW, Strike N40W without much apparent folding or faulting just nice even beds. These sandstones have incised & flow-cast marks and much slump wrinkles—quite a mess. The