Investigation of a group of landforms and their underlying deposits on the eastern margin of the Fenland in East Anglia has demonstrated that they represent a series of glaciofluvial delta-fan and related sediments. Section logging, borehole records and previous descriptions combine to indicate that the sediments were deposited in icemarginal deltaic settings in an ice-marginal lake. The internal structure and form of the fan-like deltas has been demonstrated using extensive ground-penetrating radar investigation. The lake formed by the ice damming westward-aligned river valleys. Together, this evidence confirms historical descriptions of a glaciation of the Fenland, and clarifies the interpretation of gravels of the eastern Fenland margin. Recent reinterpretations of the latter as of fluvial rather than glacial meltwater origin are shown to be incorrect. It is concluded, on the basis of regional correlation, supported by optically stimulated luminescence dating, that the glaciation occurred at c. 160 kyr, i.e. in the Wolstonian (= Saalian) Stage (broadly equivalent to MIS ?11b-6). Comparison with The Netherlands' sequence shows a similarity of glacial marginal morphology, and the dates confirm the time equivalence with that during the late Saalian Drenthe Substage, Amersfoort ice-pushed ridge complex. The implications include that the c. 200 kyr interval, between the Hoxnian (Holsteinian) temperate Stage and the Wolstonian glaciation, was a period during which fluvial and periglacial activity modified the landscape under cold climates, with organic sediments laid down during warmer events. Palaeolithic humans were periodically present during this interval, their artefacts having been reworked by the subsequent glaciation.

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Investigation of isolated landforms on the eastern margin of the East Anglian Fenland at Feltwell and Methwold Hythe, Norfolk has demonstrated that they represent glacifluvial delta‐fan and related sediments. Section logging, borehole records and previous descriptions together indicate that the deposits were laid down as an ice‐marginal delta complex and feeder channel into a proglacial lake. The internal structure and form of the delta and related feeder channel have also been determined using ground‐penetrating radar. The sequence indicates deposition at the ice front, together with minor ice‐front movements, a substantial discharge event and repeated solutional collapse of the underlying bedrock. Postdepositional solifluction and cryoturbation also occurred. The glaciomarginal landform complexes form part of a line of delta‐fan and associated accumulations (the ‘Skertchly Line’) deposited at the margin of an ice lobe that entered the Fenland. Here the ice dammed westward‐aligned rivers to form a lake, here called Lake Paterson. These observations reinforce earlier descriptions of a late Middle Pleistocene glaciation of the Fenland termed the ‘Tottenhill glaciation’. Previous research concluded that the glaciation occurred at c. 160 ka, that is, during the late Wolstonian (= late Saalian) Stage (Drenthe Substage, early Marine Isotope Stage 6), a correlation supported by evidence from the North Sea floor. The implications of these conclusions are discussed.

Summary The geology of the High Lodge site at Mildenhall is described and re-interpreted as a sequence of deposits related to a doline formed in the underlying Chalk. Doline development in the area is considered in detail. Lacustrine sediments filling the depression contain a Palaeolithic industry and pollen assemblages that indicate contemporaneous coniferous woodland. The High Lodge sequence, at the northern end of the Warren Hill ridge, is related to the Three Hills site at the southern end of the ridge and to recent exposures near the Beech Clump, midway on the ridge. The geology of the three sites combines to demonstrate a series of ice-marginal proglacial successions along the west and south side of the Warren Hill ridge, marking a glacial limit. This Skertchly Line limit, on the eastern flank of the Fenland, resulted from the Tottenhill ice advance into Fenland late in the Wolstonian Stage ( c . 160 ka; during Marine Isotope Stage [MIS] 6). Structural evidence indicates that the doline filling was initially thrust glaciotectonically by the glacial ice. These sediments were subsequently disturbed by diapirism arising from loading by meltwater deposits and possibly by periglacial processes. The doline strata predate the ice advance and represent a period of cool temperate vegetation, probably of interstadial character, earlier in the Wolstonian, during MIS 7. The High Lodge Palaeolithic industry is associated with this cool temperate period, not with pre-Anglian times as formerly proposed. At Three Hills, artefacts occur within the proglacial deposits and are reworked from an earlier period. The geomorphology of the Warren Hill ridge is described and an interpretation of the ice front presented. The relation of the area to the wider Fenland landscape development is discussed.