TRANSACTIONS OF THE SECTIONS. 
127 
ff4ik 1 10^ about ono day’s journoy south of Fazoglo. The hoy stolen hy 
I<Tpii»n slavers when about twelve years of age. lu 1844 lua 
SS toDr.L. Tutschek. The method pursued was the same 
Dr.dudes Tutschek. The vocabulary consists of about 1100 words, tor 
««of Dr.TuUchet upon the Faaoglo, ace the • Report upon the present state of 
*Kan Ethnographical Philology,’ and tlie ‘ Transactions of the Philological Society. 
On the Buriats and Tungusians. By William Twining, MJ)- 
On Ote Aleutian Islanders. By William Twining, yi . B . 
Ethnological Outlms of France. By M. Raymond j)B Veuicolb. 
IV present unity of Prance has gone far to obliterate the original dUtmeiiotis of 
•■vortiiV. TheNortheru Proviuces retain the Germanic elements of populatirin 
sdlaeuage in agreater degree than the South. The Germanic influence upon the 
i‘aiiziilBii|!UAge twis most upon the pronunciation, next upon the synux, least upon 
It* nakilary. The Langue d’Oc dialects fall into three main divisions, the Nor- 
MS) the EVard, sad the hurgundian. 
h iV Urieuj d'Oc diatrict* there is amongst the common people a strong tufo* 
MtfSmdi, Mooriih and Jewbli blood. 
M»laa U more Sponiah still. Oascony is Basque rather than Castilian. 
Ihe BreUmt are more Celtic than the Gascons are Basque. Normandy has traces 
•fiWid Norwegian influences of the Northmen. 
jWenee beat represents the remains of the old Roman or Italian population. 
I# Uminc and .^Isaoe, where the German elements are at the maxinintti, the na- 
is French. 
On the Tribes between Lidia and China. By Professor Wi L6on . 
addendum to geology and physical ceoguapuy. 
y the Geology of the Neighbourhood of Stamford and Puterhorovgh. 
^ ^ Roscawbn Idbetson, K.R.E., F.G.S., awl J. Mouins, 
Ta aku.. Introduction. 
P®P®r» to give a slight sketch of the geology of the vicinity of 
some remarks on the position of the Collyweston slates, oud their 
Stunesfield, near Woodstock. fThc authors here refer to the 
^ uihed notices of Cooybeare, Grccnough, Phillips, and Lonsdale, and 
^ physical features of the district.] 
• '^oded rK,ii. ^hick, overlying thu oolitic slates, and full of 
*»-r»ed»iih t',, ^ and other pebWea; at Stanyun also the Woe drift 
Osfofvi .nodules, and tO in other localities. 
•^“mirkdh. '^'h-scen in tlie Wigathorpe cutting near Thorpe Aychorch, 
Septaria frequently eontuluing fossils, //«. Kuntgii, 8tc., 
uiuch *^tion being thin slaty clays full of ..^7ttwo«i/e» Jaaoni or Ek- 
■^rapressed, Jielemniies, dvicula and numerous bivalves. 
