. "Typically c.3-6m, but 14m thick in BGS/Nirex borehole QBX 2-A (BGS Registered borehole SD09NE 22)."@en . . "Generally a fining upward sequence of medium- to fine-grained pale brown sand with interlaminations of silt that passes upwards into mottled olive clay and silt with thin beds and partings of peat and peaty (humic) silt. These fine-grained sediments contain microfossil assemblages indicating deposition in marine, estuarine and brackish water since deglaciation. It also includes sand and gravel forming Holocene raised beaches."@en . "The ground surface or overlain by blown sand of the Drigg Point Sand Formation."@en . . "0.116"^^ . "Unconformable on all older glacial diamictons and glaciofluvial sand and gravel deposits. In its type area it overlies diamictons of the Gosforth Glaciogenic Formation."@en . . "Hall Carleton Formation"@en . "0.0"^^ . "HALC"@en . "stable"@en . "Older storm beach deposits"@en . . . "Hall Carleton Formation"@en . . "Clay, sand and silt with subsidiary gravel and trace peat and peaty silt. Stratified superficial deposits. Occurs onshore. Formed during the Devensian Stage - to - Holocene Epoch (Quaternary Period) (.116-0 Ma BP)."@en . . "Marine warp [Obsolete: use HALC]"@en .