Wood — Effects in Mokuaweoioeo of the Eruption of 191J+. 405 



This sights along the west side of the southern part of the 

 1914 rift. In the distance is the largest cone of 1914. In 

 the right, middle ground is the uplifted andfssnred pahoehoe 

 of 1903 athwart the channel of that date. In the left middle 

 ground is the second in size of the minor rift-cones of 1914. 

 The man standing in front of it serves to fix a scale for it. 

 The magnitude of the crater, in which this particular cone is 

 an insignificant feature, can also be comprehended. The 

 foreground shows 1903 pahoehoe nearly covered with cinders 

 from the two eruptions. 



Fig. 12. 



'^ 





9pap • 



The photograph fig. 12 is a view looking ISLE, from a 

 point at the N.W. foot of the largest of the rift-cones of 1914, 

 distinctly showing three smaller ones in the continuation of the 

 rift to the N.E. The floor in the foreground is made up of 

 1914 cinders. 



Finally, very sparing fresh cinders and bits of filiform, 

 basaltic pumice, as well as sparing Pele's hair, were found in 

 a few places protected from wind drift on the summit surface 

 south of camp. 



It only remains to summarize the findings on the map, fig. 13, 

 and the cross-section, fig. 14. 



The Maps. 



The scale of the Alexander map of 1885 is given, on blue- 

 print copies, as 1000 feet to the inch ; and the latitude and 

 longitude of the trigonometric station on the west wall, north 



