the hast of the cone, almost immediately sapping all the flow 
from the northern tongue of June 26. 
about July If the 
lava emerging fro® the south end of the ro« 
Ahu&n hornitos 
stopped adding its stream to the more easterly buried I'M 
sent a new tongue southeast?;.* rd for five day*. On the 20th a 
nm flow darted northward from the east &ide of tn 
p''” 
v# 
nt » repeat 
ing the route past Zaptchu much traveled by earlier flows, draining 
away the source flow of the east tongue of July 12. By August 7 
the latter came to a halt, after invading half the area of a snail 
peninsula of virgin ground about 3 « Home tars east of the cone. 
By the end of July the southernmost exit of the Almin lava was 
170 meters fro® the base of the cone (see fig. 2). 
During August the flow north of Zapichu developed four 
distinct lobes in the vicinity of the Upper Capita. The topo- 
graphic ?sap of Cerro de J&rltlro (fig. l) shows the details of the 
lava inundation here from March 6, 1923, onward. On about August 
8 a new lave flow started from the Ahuln hornitos about 50 meters 
nearer the volcano than the previous fccca , or 120 meters south 
of the base of the cone. Its course was westward for 125 meters 
where it tioub. 
becA to the south end southeast in a cre&t bow 
that seeisac to touch the outer Halts of 
previous fMowa in the 
vicinity. At the same time, hcrt-ilved flows emerged fro® each 
of the first three spatter cones south of the volcano, coalescing 
an i congealing about 36 meters on either ide of the line of hornitos 
On about September 11 a new active lava boca opened on the 
■> ‘ 
old Mesa de las Born i to* area, west of the cone . Sine* the 
