Wood — Effects in Moltuaweoweo of the Eruption of 191J±. 393 



A careful study of the details of the main floor in the middle 

 ground, in figs. 4-a and 4c, develops the fact that near the junc- 

 tion of the east wall and the south Innate platform there 

 remains without change a considerable tract characterized by 



Fig. 4b. 



Fig. 4c. 



a recognizable pattern due to intermingling of a-a, piled crusts 

 of pahoehoe and smooth, unbroken pahoehoe. Only on the 

 extreme west of these views has this pattern been interfered 

 with. However, farther north in the same views, it is seen 

 that in 1915 new rough lava had flowed quite to the east wall, 



