504 EXTENT AND NATURE OF [Ch. XXIX. 



the old volcano and its Caldei'a were formed was so vast a thickness 

 of gravel formed, to be afterwards cut through to a depth of 800 feet ? 

 The ravine throiio'h which the torrent now flows has been excavated 

 to that depth through the old conglomerate. The occurrence of two or 

 three layers of contemporaneous lava, intercalated between the strata of 

 puddingstone, ought not to surprise us ; for even in historical times 

 eruptions have been witnessed in the southern half of Palma. Such 

 basaltic lavas, one of them columnar in structure, have not come down 

 from the Caldera, but from cones much nearer the sea, and immedi- 

 ately adjoining the Barranco, like the cone of Argual (see map, p. 495) 

 and others. These lavas, of the same age as the conglomerate, consist 

 of three or four currents of limited extent, for in many parts of the river- 

 cliffs no volcanic formation is visible on either bank. On the right 

 bank of the Barranco, the conglomerate, when traced westward, is soon 

 found to come to an end as it abuts against the lofty precipice e (fig. 64*7), 

 which is a prolongation of the western wall of the Caldera. Its extent 

 eastward from 5', may be more considerable, but cannot be ascertained, 

 as it is concealed under modern scoriae and lava spread over the great 

 platform, r. 



Fig. 647. 



A. Eavine or Barranco de las Ansnstias, near its teraiination in Palma. 

 J, 6', h". Conglomerate, 800 feet thick in parts. 



c, c'. Lava intercalated between the beds of conglomerate. 



d, d'. Another and older current of basaltic lava, columnar in parts. 



E. Clitf of ancient volcanic rocks of the Upper JFormatiou (p. 500), a prolongation of 



the western wall of the Caldera. 

 r. Platform on which the town of Argual stands. 



As we could find no organic remains in the old gravel, we have no 

 positive means of deciding whether it be fluviatile or marine. The 

 height of its base above the sea, where it is 800 feet thick, may be 

 about 350 feet, but patches of it ascend t'o elevations of 1000 and 

 1500 feet near the top of the Barranco, as shown at k, &c., in section, 

 fig. 646, p. 497. Such a mass of gravel, therefore, bears testimony 

 to the removal of a prodigious amount of materials from the Caldera 

 by the action of water. Whether a river or the sea was the transport- 

 ing agent, it is obvious that a large portion of the volcanic materials, 

 consisting of sand, lapilli, and scorise, before described (p. 498), as be- 



