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The Glauconitic Marl Member (reference section: Copt Point, Folkestone [TR 242 365] ) is c. 5 m thick a ...

...mation (Robinson, 1986). The basal part of the formation is designated the Glauconitic Marl Member, but no subdivision is recognised for the remainder, which contains local f See: Glauconitic Marl Member (Robinson, 1986), marl ...

Includes the equivalents of the Melbury Sandstone Member, Glauconitic Marl Member and the Cambridge Greensand Member at the base. ...able. Base marked by erosion surface, frequently bored, at the base of the Glauconitic Marl Member (Southern Province), Melbury Sandstone Member (western Southern Province) o ...

...ge Greensand Member'''. Equivalent to the Melbury Sandstone Member and the Glauconitic Marl Member | '''Glauconitic Marl Member''' of the West Melbury Marly Chalk Formation ...

...rowne and Hill (1903). In modern usage this would equate to the top of the Glauconitic Marl Member (Southern Province) or the Cambridge Greensand Member (‘Transitional’ Provi ...er’ containing laminated structures”. The formation is undivided above the Glauconitic Marl Member. The formation is essentially equivalent to all of the Lower Chalk of the ...

...ween 0.5 and 2 m thick at most. The base of the formation is marked by the Glauconitic Marl Member; an arenaceous, glauconitic, marly sandstone which provides a distinctive p ...

| GLAUCONITIC MARL MEMBER ...