excursion to charlton: saturday, march 27th, 1920

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154 TO SATURDAY, :lIARCH 27TH, 1920. REPORT BY ARTHI.JR L. LEACH, F.G.S., Director of the Excursion. THE party assembled at Charlton Station at 2.30 p.m., and walked through the great disused excavations, which mark the site of the old sand workings at Charlton, to the pit now in USe on the side of Cox's Mount, near Charlton Lane. Here the Director drew attention to the principal features of the excellent section of the Lower Loridon Tertiaries, corresponding in all essential respects with the section (drawn from the disused work- ings) given in the Memoirs of the Geological Survey. It is unnecessary to give any detailed account of the Charlton section which has been figured and described in many reports and memoirs The pit is now used chiefly as a source of sand for the factory of the United Glass Bottle Manufacturers' Association. Before the Thanet Sand, the only suitable glass-sand, can be dug out, all the overlying masses of Woolwich Beds and Blackheath Beds have to be removed. The pit is thus conveniently worked in three stages, marked by the top of the Chalk, the top of the Thanct Sand, and the top of the Woolwich Beds. From these three platforms the formations can be,examined easily in detail. In the ncar future a new glass factory will be erected at Charlton and the excavation of sand will proceed much more rapidly than in the past. The members of the party separated for a time to collect fossils from the chalk-pit and from the Eocene formations (Thanet Sand, Woolwich Beds and Blackheath Beds) and re-assembled on the upper platform to notice a band of large pebbles in the Blackheath Beds. Almost every pebble was seen to be split into fragments, many of them roughly parallel slices, which re- mained side by side. On digging into this bed to expose fresh pebbles, few of these were found to be split. As the pebbles while still buried within the bed are less subject to frost action than those outstanding on the working face of the pit, and all other conditions arc the same, in this case the splitting may, with more probability, be assigned to temperature changes rather than to pressure.* On the high ground above the pit, ;\ir. F. C. Elliston Erwood kindly gave some account of the Charlton Earthworks and of the exploration of the site carried out by him in 1915. Fragments of the western line of banks and ditches still remain, but these will probably disappear in the near future and in a few years not a trace ot the original earthworks will remain. Fortunately an excellent description of the site and of ·See also Report of an Excursi'Jn to East Wickham, Proc, Geol, Assoc., vol, xxx. {I9I9 p. J'19.

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Page 1: Excursion to Charlton: Saturday, March 27th, 1920

154

EXCURSIO~ TO CHARLTO~.

SATURDAY, :lIARCH 27TH, 1920.

REPORT BY ARTHI.JR L. LEACH, F.G.S., Director of the Excursion.

THE party assembled at Charlton Station at 2.30 p.m., andwalked through the great disused excavations, which mark thesite of the old sand workings at Charlton, to the pit now in USe

on the side of Cox's Mount, near Charlton Lane. Here theDirector drew attention to the principal features of the excellentsection of the Lower Loridon Tertiaries, corresponding in allessential respects with the section (drawn from the disused work­ings) given in the Memoirs of the Geological Survey. It isunnecessary to give any detailed account of the Charlton sectionwhich has been figured and described in many reports and memoirsThe pit is now used chiefly as a source of sand for the factoryof the United Glass Bottle Manufacturers' Association. Beforethe Thanet Sand, the only suitable glass-sand, can be dug out,all the overlying masses of Woolwich Beds and BlackheathBeds have to be removed. The pit is thus conveniently workedin three stages, marked by the top of the Chalk, the top of theThanct Sand, and the top of the Woolwich Beds. From thesethree platforms the formations can be, examined easily in detail.In the ncar future a new glass factory will be erected at Charltonand the excavation of sand will proceed much more rapidly thanin the past.

The members of the party separated for a time to collectfossils from the chalk-pit and from the Eocene formations (ThanetSand, Woolwich Beds and Blackheath Beds) and re-assembledon the upper platform to notice a band of large pebbles in theBlackheath Beds. Almost every pebble was seen to be splitinto fragments, many of them roughly parallel slices, which re­mained side by side. On digging into this bed to expose freshpebbles, few of these were found to be split. As the pebbleswhile still buried within the bed are less subject to frost actionthan those outstanding on the working face of the pit, and allother conditions arc the same, in this case the splitting may, withmore probability, be assigned to temperature changes ratherthan to pressure.* On the high ground above the pit, ;\ir. F. C.Elliston Erwood kindly gave some account of the CharltonEarthworks and of the exploration of the site carried out by himin 1915. Fragments of the western line of banks and ditchesstill remain, but these will probably disappear in the near futureand in a few years not a trace ot the original earthworks willremain. Fortunately an excellent description of the site and of

·See also Report of an Excursi'Jn to East Wickham, Proc, Geol, Assoc., vol, xxx. {I9I9p. J'19.

Page 2: Excursion to Charlton: Saturday, March 27th, 1920

EXCURSION TO CHARLTOS. 155

the associated relics has been published by Mr. Erwood (SeeReferences). With the aid of a plan he showed the form andextent of the enclosure and the positions of the dark bands(hearth sites and refuse layers) which had yielded numerous,and varied types of Roman-British pottery, coins, fibulse, bonesloom-weights, and other relics of the native settlement whichoccupied this site during the Roman control of Britain. Norelics of a military nature had been recovered: the remainswere those of the peaceful habitations and ordinary domesticoccupations of a native settlement.

Mr. Erwood kindly exhibited some specimens of the Samianhowls of fine red ware, the two fibulze, one of a very beautifuland rare, if not unique type, and numerous photographs of otherinteresting archseological objects obtained from this pit.

The party now walked round the northern end of the pitwhere the Eocene formations are splendidly exposed along avertical face, and here also traces were seen of the soil-filled ditchesof the earthworks. This concluded the programme for theexcursion. Before the party dispersed, Mr. Erwood and theDirector were thanked, on the motion of Mr. J. F. N. Green, forthe demonstrations, archreological and geological, given duringthe afternoon.

HEFERE:\CES.

Geological Survey Map, London District (Drift Edition), Sheet 4.1889. WHITAKER, W.-" Geology of London," vol. I, Mem, Geol, Suruey;Igog. WOODWARD, H. B.--" Geology of the London District," Mem,

Geol. Survey.19I6. Exwoon, F. C. E.-" The Earthworks at Charlton, London, S.E,

Journal British Arch. Assoc.