SOUTHERN DISTRICT. 307 



5. SOUTHERN DISTRICT. 



A diflcrcnce in the na(ni;il productions of the higher grounds of the southern tier of 

 counties, or those bordering Pennsylvania, has not escaped the notice of agriculturists ; and 

 a hasty reference to my geological observations on this part of the State, is all that will 

 be necessary to convince an unprejudiced person tliat many of the difFcrences which have 

 been observed in tlie natural as well as the cultivaled productions, are due to the peculiar 

 formations of this portion of the commonwealth. Height undoubtedly exercises conside- 

 rable influence upon the vegetation of this district, but it is not probable that to height 

 alone can be attributed the differences which have been observed in respect to the pro- 

 ducts of the soil. 



For the purpose of a general reference, the northern limits of the Southern district 

 extend to the middle of Seneca and Cayuga lakes. This boundary line, prolonged east 

 and west as far as to the spins of the CatskiUs, or the head waters of the Mohawk and 

 Lake Erie, completes the northern boundary of the district. Otsego, Schoharie, Greene and 

 Albany counties, intercept this line eastwardly. Tlie vallies of these counties, however, 

 contain much valuable wheat soil ; but it is not continuous to a great extent : it does not 

 produce the perfect grain in its seasons. The straw is weak, and the grain more liable to 

 shrink. It is not full and plump as the wheat of the Genesee valley and the adjacent 

 districts. 



This district is hilly, and the vallies which traverse it are narrow. From this district, 

 too, the waters flow both to the north and south. Without being precipitous, as in the 

 Highland district, it is still quite steep in the ascents and descents ; and a very large 

 proportion of the farming operations are conducted on the slopes of ridges and hills, all of 

 which were originally covered with a heavy growth of timber. Upon the higher grounds, 

 the hemlock, spruce and fir are the most common. In many places, a raixtine of beech, 

 birch, maple, ash, hemlock, pine and spruce, is the form which the vegetation assumes. 

 Its growth is heavy and dense, the character of which is well exhibited in the cut on the 

 preceding page. 



The soil is usually deep, sometimes in consequence of the accumulations which probably 

 were made during the Drift period, and partly from the friable nature of the rocks beneath. 

 These rocks, for moderate distances, appear horizontal. Uplifts have rarely deranged the 

 original position of the strata. Immense sections of the rocks, however, have been re- 

 moved ; and hence the sides of the vallies have their corresponding strata upon the same 

 level. The debris'of the rocks so far modify the accumulations of drift, that it gives the 

 soil a peculiar character, and fits it for certain kinds of husbandry. Butter, cheese, wool, 

 and the rearing of cattle, become objects of prime importance. 



We may now inquire more particularly what peculiarity in the composition of tlie soil 

 controls the husbandry of this district? We have no doubt it is principally the composition 



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