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High Lodge
Suffolk

 

 

Site Number 26 (This is an AHOB Key Site)
Nearest Town: Mildenhall
National Grid Reference: TL 73918 75391
Lat: 52.349 Lon: 0.552

There have been investigations at High Lodge since the 1860s with various interpretations of the sequence (Whittaker et al. 1891; Marr 1921; Ashton et al. 1992). Fieldwork in the 1960s recovered the principle archaeological assemblage together with much of the biological data from the site and further investigations in 1988 established the current understanding of the geological and environmental succession. The oldest sediments at the site consist of clayey-silts laid down as overbank sediments from the Bytham river. These sediments were subject to subglacial deformation and transport, resulting in their emplacement above younger Anglian till (Lewis 1992). These are overlain by glacial sands and gravels. The glacial sediments are attributed to the Anglian glaciation of MIS 12 age, implying that the clayey silts are MIS 13 or older. A pre-Anglian age is supported by the remains of Stephanorhinus hundsheimensis (Stuart 1992). The clayey silts preserve pollen, insects with occasional wood and vertebrate remains (Coope 1992; Hunt 1992). The fauna and flora indicate a cool climate with vegetation dominated by pine and spruce together with juniper and heathland plants. The floodplain contained pools and marshland with seasonal flooding from the nearby river.

Over 1,200 fresh flint artefacts were recovered from the clayey silts, consisting of flakes, scrapers, notches and cores, but no evidence of handaxe manufacture (Ashton 1992). The unusually fine manufacture of the scrapers led earlier workers to interpret the site as Mousterian, but the arly dating precludes this interpretation. Handaxes were found in secondary context in the overlying glacial sands. Their fresh condition suggests that they were derived from underlying sediments nearby, potentially the same overbank sediments that contain the flake tool assemblage, but perhaps from a different location on the floodplain.

Excavated assemblages 1962-1968

 

Glacial sands and gravels

Clayey Silts

Handaxes/roughouts

14

0

Flake tools

15

69

Cores

13

52

Soft hammer flakes

7?

1?

Hard hammer flakes

377

983


Horizons recorded at High Lodge

Unit Name Epoch Biozone MIS
High Lodge Clayey Silts and High Lodge Sands (Horz Num: 26) Middle Pleistocene 'Cromerian' 13
Mildenhall Upper Sands and Gravels (Horz Num: 260) Middle Pleistocene 'Cromerian' 13

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