DYEBERRY. G 5 . 179 



Barometric elevations in Clinton. 



A. T. 



Summit of Griswold's Gap, 1975' 



Forks near E. Varcoe's, 1545' 



" W. S. Harrison's, 1470' 



" J. G. Dann's, 1465' 



M. Owl's, 1405' 



Level of White Oak pond, 1375' 



Forks at Baptist church in Aldenville, 1240' 



Road at watering trough " 1230' 



Forks near G. Gaylord's, 1320' 



" A. Conyone's hotel, ' 1270' 



" G. H. Tennant's, ' 1315' 



Level of Lackawaxen just above, 1300' 



Forks near F. Griner's, 1195' 



Level of Lackawaxen just below, 1180' 



Forks near H. Reynold's, 1165' 



" T. Olver's, 1150' 



Cross roads at E. K. Curtis's, 1140' 



Level of Lackawaxen just opposite, 1120' 



36. Dyeberry, in Wayne county. 



This lies directly west from Clinton, lias Mt. Pleasant and 

 Lebanon townships on its northern border, and Texas on its 

 southern. 



The drainage is southward into Lackawanna creek, prin- 

 cipally by way of Dyeberry creek, and other tributaries. 



The Dyeberry flows in a Drift filled valley, heaps and 

 hummocks of morainic material being seen as far north as 

 Tanner s Falls, and extending from thence southward all 

 along its course ; it thus becomes a very sluggish stream, 

 and the evidence would point to a very deeply buried val- 

 ley, especially in the lower portion of its course, since at no 

 locality below Tanners' Falls do we see any rock bottom. 



The rocks in Dyeberry belong entirely to the CatsJcill sys- 

 tem, the highest ones noted being the CJierry Ridge group, 

 while the lowest exposed strata come 300' to 400' below. 



The Honesd ale sandstone group is exposed in an almost 

 constant line of grayish-white cliffs along the banks of this 

 stream from its northern line to its southern. 



