43 



nearly 2000 feet northward, and the mouth of the stream 

 was shifted to that point. Since then, the stream has 

 broken through the bar at several places, shifting its mouth 

 every season, and leaving partially closed outlets to be filled 

 in subsequently by the weaves. The map (Plate II.) repre- 

 sents the temporary conditions which existed in August, 

 1895. (See also Plate XXL). 



