HAMILTON SHALES. 185 



pear towards the end or about tlie middle of the series. So in the Hamilton shales, im- 

 pure calcareous bands are met with, though the calcareous matter seems to liave been 

 derived from the petrifactions which they inclose. This shows that some calcareous mat- 

 ter existed in solution in the waters from which these rocks were separated or deposited ; 

 indeed, the shales sometimes efTervesce feebly. Now the main peculiarity which we find 

 in these rocks, consists in the ability to produce good pasturage : the soil possesses that 

 light character which fits it for sweet grazing. There is always seemingly sufficient alu- 

 mine or clay in these rocks to give the debris the proper consistency to hohl water, and 

 this rarely to excess. There are two other circumstances which contribute to form a 

 grazing country where these rocks predominate, namely, sweet or pure water, and a hilly 

 surface. The water, under such circumstances, drains off rapidly, and leaves the soil 

 refreshed : it will not stagnate above or beneath the surface. If the grass and herbage is 

 not so luxuriant, it is sweeter, and promotes the health of the animals which feed upon it. 

 The atmosphere circulates freely over the hills and through the valleys, and thereby 

 rapidly renews the essential elements of life and activity. 



Successio/i of strata and illustrative views. The succession of the groups and strata are 

 well exposed on Cayuga and Seneca lakes, and in the valley of the Schoharie ( See Plate 

 xxi., sections 3 and 4 ; or Plate xx., sections 2, 4, 5 and 6) . For illustrative views, see 

 Plate vi., which may be comjDared with Plate iv. : the formations of the former are un- 

 disturbed, while the latter is on a zone or belt which has been broken up by internal 

 convulsions. 



Thickness of the Hamilton shales. It is difficult to obtain the data from which the thick- 

 ness of this rock can be determined. By estimating the fossiliferous and non-fossiliferous 

 parts by themselves, and summing up the result, we obtain from 1000 to 1200 feet thick- 

 ness. In the eastern part of the State, in Albany and Schoharie counties, the thickness 

 appears to be much greater than in the western counties ; at the same time it must be 

 acknowledged that the line of demarkation between this and the upper part of the Erie 

 division is indistinct, and hence masses which belong properly to the Devonian or Catskill 

 rocks may be included. The lower part of the Hamilton shales are destitute of fossils in 

 Schoharie county, for about fifty feet : then we meet a band of fossils, among which is a 

 Conularia and Posido7iia ; this is succeeded by another non-fossiliferous band of conside- 

 rable thickness, and then fossils again occur; and in the Olive shales, so called, the fossils 

 are very numerous, and among them we find a great abundance of the Delthyris mucro- 

 nata, the beautiful Ortho7iafa undulata, and Dipleura dckayi. Still higher in the series, 

 we find an abundance of vegetable fossils, which extend through beds of sandstone and 

 shale for sixty or seventy feet ; and lastly, in the tops of the hilly region of Fultonham in 

 Schoharie, the rock becomes a grayish sandstone, with stems of plants, encrinites, and a 

 large delthyris. In the hills of Fultonham, the thickness of the superimposed masses is 

 at least eight hundred feet. The beds are thin at the base, but not even-bedded ; at the 



[Agricultural Report.] 24 



