FREE BOOKS

Author's List




PREV.   NEXT  
|<   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62   63   64   65   66   67   68   69   70  
71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   90   91   92   93   94   95   >>   >|  
ni came the Greek name for Ceylon, _Taprobane_. Mr. de Alwis has corrected an error in this passage of Mr. Turnour's translation; the word in the original, which he took for _Tamba-panniyo_, or "copper-palmed," being in reality _tamba-vanna_, or "copper-coloured." Colonel Forbes questions the accuracy of this derivation, and attributes the name to the _tamana_ trees; from the abundance of which he says many villages in Ceylon, as well as a district in southern India, have been similarly called. (_Eleven Years in Ceylon_, vol. i. p. 10.) I have not succeeded in discovering what tree is designated by this name, nor does it occur in MOON'S _List of Ceylon Plants_. On the southern coast of India a river, which flows from the ghats to the sea, passing Tinnevelly, is called Tambapanni. Tambapanni, as the designation of Ceylon, occurs in the inscription on the rock of Girnar in Guzerat, deciphered by Prinsep, containing an edict by Asoka relative to the medical administration of India for the relief both of man and beast, (_Asiat. Soc. Journ. Beng._ vol. vii. p. 158.)] The transformation of gneiss into laterite in these localities has been attributed to the circumstance, that those sections of the rock which undergo transition exhibit grains of magnetic iron ore partially disseminated through them; and the phenomenon of the conversion has been explained not by recurrence to the ordinary conception of mere weathering, which is inadequate, but to the theory of catalytic action, regard being had to the peculiarity of magnetic iron when viewed in its chemical formula.[1] The oxide of iron thus produced communicates its colouring to the laterite, and in proportion as felspar and hornblende abound in the gneiss, the cabook assumes respectively a white or yellow hue. So ostensible is the series of mutations, that in ordinary excavations there is no difficulty in tracing a continuous connection without definite lines of demarcation between the soil and the laterite on the one hand, and the laterite and gneiss rock on the other.[2] [Footnote 1: From a paper read to the Royal Physical Society of Edinburgh by the Rev. J.G. Macvicar, D.D.] [Footnote 2: From a paper on the Geology of Ceylon, by Dr. Gardner, in the Appendix to Lee's translation of RIBEYRO'S _History of Ceylon_, p, 206. The earliest and one of the ablest essays on the geological system and mineralogy of Ceylon will be found in DAVY'S _Account of the Interior of Ceylon_
PREV.   NEXT  
|<   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62   63   64   65   66   67   68   69   70  
71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   90   91   92   93   94   95   >>   >|  



Top keywords:

Ceylon

 

laterite

 

gneiss

 

called

 

southern

 

Footnote

 
magnetic
 

copper

 
ordinary
 
translation

Tambapanni

 
felspar
 
communicates
 

hornblende

 
produced
 

proportion

 
colouring
 

assumes

 
cabook
 

abound


peculiarity

 
explained
 

recurrence

 

conception

 

partially

 

conversion

 

disseminated

 

phenomenon

 

weathering

 

inadequate


viewed

 

chemical

 

yellow

 
regard
 
theory
 

catalytic

 

action

 

formula

 

Appendix

 

RIBEYRO


History

 

Gardner

 
Macvicar
 

Geology

 
earliest
 
ablest
 

Account

 
Interior
 
essays
 

geological