Page:Quarterly Journal of the Geological Society of London, vol. 27.djvu/235

Rh {|
 * colspan="3" | Fig. 4.—General Section of the Coralline Crag.
 * rowspan="8" |
 * | h. Sand and comminuted shells.
 * | Sudbourne. Gedgrave.
 * | g. A series of beds consisting almost entirely of comminuted shells and remains of Bryozoa, forming a soft building-stone. False stratification and oblique bedding are its constant characters.
 * | Sutton. Sudbourne. Gedgrave. Iken. Aldbro'.
 * | f. Sand with numerous entire small shells and seams of comminuted shells.
 * | Sutton. Iken. Sudbourne. Gomer.
 * | e. Sands with numerous Bryozoa, often in the original position of growth, and some small shells and Echini.
 * | Sutton. Broom Hill.
 * | d. Comminuted shells, large entire or double shells, and bands of limestone in the upper part.
 * | Sutton. Broom Hill. Sudbourne. Iken. Tattingstone.
 * | c. Marly beds with numerous well-preserved and double shells, often in the position in which they lived.
 * | Sutton. Ramsholt.
 * | b. Comminuted shells, Cetacean remains, Bryozoa.
 * | Sutton.
 * | a. Phosphatic nodules and mammalian remains.
 * | Sutton.
 * }
 * | Sutton. Ramsholt.
 * | b. Comminuted shells, Cetacean remains, Bryozoa.
 * | Sutton.
 * | a. Phosphatic nodules and mammalian remains.
 * | Sutton.
 * }
 * | Sutton.
 * }