198 FALKLAND ISLANDS. [chap. ix. 



rij )re striking by the contrast of the low, rounded forms of tiie 

 {jt^lghbouring hills. 



I was interested by finding on the highest peak of one range 

 fdbout 700 feet above the sea) a great arched fragment, lying 

 oQ its convex side, or back downwards. Must we believe that it 

 was fairly pitched up in the air, and thus turned? Or, with 

 more probability, that there existed formerly a part of the same 

 range more elevated than the point on which this monument of 

 a great convulsion of nature now lies. As the fragments in the 

 valleys are neither rounded nor the crevices filled up with sand, 

 we must infer that the period of violence was subsequent to the 

 land havins" been raised above the waters of the sea. In a trans- 

 verse section within these valleys, the bottom is nearly level, or 

 rises but very little towards either side. Hence tlie fragments 

 appear to have travelled from the head of the valley ; but in 

 reality it seems more probable that they have been hurled down 

 from the nearest slopes ; and that since, by a vibratory move- 

 ment of overwhelming force,* the fragments have been levelled 

 into one continuous sheet. If during the earthquake"]" which in 

 1835 overthrew Concepcion, in Chile, it was thought wonderful 

 that small bodies should have been pitched a few inches from 

 the ground, what must we say to a movement which has caused 

 fragments many tons in weight, to move onwards like so much 

 sand on a vibrating board, and find their level ? I have seen, in 

 the Cordillera of the Andes, the evident marks where stupen- 

 dous mountains have been broken into pieces like so much thin 

 crust, and the strata thrown on their vertical edges ; but never 

 did any scene, like these " streams of stones," so forcibly convey 

 to my mind the idea of a convulsion, of which in historical 

 records we might in vain seek for any counterpart : yet the 

 progress of knowledge will probably some day give a simple 

 explanation of this phenomenon, as it already has of the so long- 



* " Nous n'avons pas ete moins saisis d'etonneraent a la vue de rinnorn- 

 brable quantite de pierres de toutes gi'andeurs, bpuleversees les unes sur les 

 autres, et cependant range'es, comme si elles avoient e'te' amoncelees uegli- 

 gemment pour remplir des ravins. On ne se lassoit pas d'admirer les eft'ets 

 prodigieux de la nature." — Pernely, p. 526. 



t An inhabitant of Mendoza, and hence well capable of judging, assured 

 me that, during the several years he had resided on these islands, he had 

 never felt the slightest shock of an earthquake 



