TABLE II 

 CORREl VTION QUATERNARY OF GREAT BRITAIN (BROOKS, ll'llt.l. PAGE 326) [WITH MODIFII ATI0N8 BY II. V. 



B. P.O., 1922. 



.i h en Engl tnd. 



Thames Valley. 



South coasl and south 

 Wa les. 



Northwest England. 



Scotland. 



North But ope. 



Vrcheol ■■ leal periods. 











Upper peat. 



: glaciers. 



I i : pi 1 



m 





Submerged forest 



Buried channel. 



1 ine forest of Dorset. 

 Submerged forest. 



pp i to: 1 bed. 



, pper tot e 1 bed. 



Subboreal period. 



Ite in olithic and 



I ■ 





Formby and 1 i • 

 boils and Shirdley 

 hill sand. 



Peal 



ach. 



■ ■■ per od a n il 

 Atlanta' period, 



Neolithic. 





Lower peat and foresl 

 bed. 



; eat 



'land 

 i period. 



Garij neolithic, 





', r. ic peal bed of 

 Holmptou. 



1 ovi terrace. 



Possibly upper head. 



Arctic :■ ial hi d of 

 I'enuines. 



Smalt valley glaciers. 

 50-foot beach. 

 Arctic peat bed. 



Low da rai e. 



Chlrd I Last IV| 



tflal in Baltic 



1,0. 



III. Ill 



Solutrean. 



I Third 

 interglaciatlon. 1 



Temperate peat of 

 Holderness. 



Erosion. 







forest layer and 



i tcial n 'Hi Pain 



iliim duboisiana. 

 Skaerumede si t'l i . 



gi r Man tterian 



1 .ill 



Gl 1 LATI0N.] 



' relic licil of Hoxne. 

 i [esslc boulder-elny. 



Arctic bed of ral 



ley. 

 "Warp and ti 

 Mid. iu terrace. 



Boulder-clay of Gower 



I to. 



"Head." 



Raised beach of Sel- 

 ey and Brighton. 



Upper boulder-clay. 

 Midglacial sands. 

 Lower boulder-clay. 



Large valley glaciers. 



beach. 

 Upper boulder-clay. 



[=111] 



Middle terrace. 



i glaclation by 



Siancl,, ii ian Ice. 



Ider Mousterlan. 

 Vi heulean. 



1 S nnd 

 iutergl iclation.] 



' >mp -c at ' i custrine 

 beds of Ho'xue. 

 ., iu gravels ( ; 

 ■1 i i irch, and 

 Clacton. 



v lion. 

 l.'Ji tool ■ ad 1 1 

 terrai c -. 



T( aiperate m immaliai 

 fauna of Gower. 



Sands, as With 

 ate fauna al Selsej 

 and elsewhere. 



End of older raised 

 beach period. 



te beds of 



1 lindall, etc. 



[2nd] luterglai ial bed 

 of :. d iill, ilra i 

 etc., and p« lib 

 Cleongi rl and 01 iva. 



nl , laclal ol Palu 

 iliim dihwiuna and 

 i ; .■ ula . umin ilia. 

 ' i lieds. 



" elh an. 



[ = 11 



GtACIATION.] 



Chalky boulder ■ i 

 i nd purple clay » 

 rness. 

 uii uth marine 

 ads, te 

 irth S i drift 

 V.rc tic fresl 1 i 



j boulder el ly. 



Boulder-clay of IVn- 

 coed. 

 ilder raised beach. 



ted occurrences 

 of ancient rod boul- 

 der-clay. 



Id i boulder-clay. 



[= 1 1 1 

 Chief terrace. 

 P Irsl glaclation by 

 Scandinavian ice. 







Cromer Eot 1 i d. 











\ ■.!.(. i tge 





i (1913.1), ha o lie drift" = Glacial ill of Leverett's paper (Leverett 1910.1) 



of Keilhack. The drift in uortl en Eu a I d and I'aludina diluviana beds probably cot b ith the "Chalkj 



boulder-clay" of England. The drift below these nortli German interglacial beds seems not to h&\ • •■■ tended into England. Levi iett. 



