. Bulletin of the Natural Histort Museum. Geology series. LOWER LIAS OF ROBIN HOOD'S BAY 97. Fig. 17 Map showing contours at 10 m bed thickness intervals in the Lower Lias on the foreshore of Robin Hood's Bay, from which the elongated dome geological structure can be deduced. The only geographical features shown are the line of the base of the cliff and the low tide mark. See text for further explanation. STAITHES SANDSTONE FORMATION (PART) Bed no Zone of Amaltheus margahtatus Subzone of Amaltheus stokesi (lower part) m Sandstone,


. Bulletin of the Natural Histort Museum. Geology series. LOWER LIAS OF ROBIN HOOD'S BAY 97. Fig. 17 Map showing contours at 10 m bed thickness intervals in the Lower Lias on the foreshore of Robin Hood's Bay, from which the elongated dome geological structure can be deduced. The only geographical features shown are the line of the base of the cliff and the low tide mark. See text for further explanation. STAITHES SANDSTONE FORMATION (PART) Bed no Zone of Amaltheus margahtatus Subzone of Amaltheus stokesi (lower part) m Sandstone, soft, micaceous, laminated Sandstone, hard, shelly in parts; many Gryphaea sp.; forms the roof of Castle Chamber at north-west end of Robin Hood's Bay Sandstone, soft, silty Shale, silty Limestone nodules Shale, silty Shale, sandy Shale, silty, with horizon of limestone nodules near top Amaltheus stokesi (J. Sowerby) m above base (1; CA 4605) Shale, sandy, laminated; forms the most conspicuous positive feature between floor and roof of Castle Chamber Flat limestone nodules Amaltheus stokesi (J. Sowerby) (1; MKH Coll, lost).. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Natural History Museum (London). Andover : Intercept


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