162 
HELDERBERG DIVISION. 
by a thin band of Qriskany sandstone. The bed usually quarried for cement, is not no¬ 
ticed ; though at Vienna in Ontario county, it is two feet thick ; and in Genesee county, 
at Morganville, the waterlime is thirty-eight feet thick, consisting of four feet in thin 
courses, twenty-two feet in thick courses (in combination with silex), and twelve feet in 
gray layers with seams of blue marl. The series terminates below in the green and grayish 
fragile shales or marls. 
The development of the upper part of the series I have been describing, is best in Scho¬ 
harie county, while the lower part is best exposed in Onondaga county. At Schoharie 
village, the following series occurs at the strontian locality, on the slope west of the creek : 
1, Hudson-river series, three hundred feet exposed ; 2, Waterlime series of the Onondaga- 
salt group, consisting of blue thick-bedded limestone, and greenish or drab-colored shaly 
limestone, one hundred feet, and pentamerus, twenty feet. Between the Hudson-river 
series and the waterlimes, the red shales are feebly developed, and contain, as at the Ron- 
dout falls, numerous crystals of sulphuret of iron. Developed also in and beneath the mass 
of thin-bedded limestone containing strontian and barytes, is a mass of compact blue lime¬ 
stone about eight feet thick, in which favosites abound, and which is scarcely known out 
of Schoharie county. 
Soils of the Onondaga-salt group. The debris of the rocks of this group is almost uni¬ 
formly of a drab color, and it may be usually traced to the source from which it is derived. 
It becomes fine by the slow process of disintegration ; constantly furnishing, in the changes 
it undergoes, suitable materials for vegetable food. The soil, as might be expected from 
the character of the rock, is excellent: it possesses a sufficient tenacity for the growth of 
wheat; but sometimes, especially where the clay predominates, it acquires too much tena¬ 
city for indian corn. The clay beds possess the same colors as the soil, only they are of 
deeper tint. 
It will be noticed, from the preceding description of the localities where these rocks are 
developed, that the lower parts of the group furnish the best soil, as they undergo more 
rapid decomposition. The process is slow in the superior portion of the waterlimes, still 
the soil furnished in each case has the same general character ; but in consequence of the 
great development of the lower portion in the central part of the State, the soils are 
much more widely spread and extended than to the eastward : it is, moreover, derived 
from the rocks themselves, and without intermixture to any considerable amount of the 
northern drift. 
The soil and clay of this series may generally be distinguished from that of the slates of 
the Hudson-river series : the latter is bluish, and rarely of that distinct drab-color possessed 
by those derived from the waterlimes, although it is true that the upper clay of the Hud¬ 
son river series is of a drab or yellowish brown color. As I propose to treat of the soils 
of the different rocks under a separate head, I leave this subject at present. 
Springs and wells whose origin can be traced to the Onondaga-salt group. Probably no 
series of rocks furnish such a variety of soluble products as the Onondaga-salt group ; and 
