The Dunkirk shale loams are found upon the hill or escarpment. These
form the grape lands farthest removed from the lake. This soil is
comparatively thin, not averaging more than a half-foot in depth and is
hardly ever found a foot deep. It is brown in color with much coarse
fragmentary shale on the surface and underlaid with a considerable body
of heavy clay. Part of the shale loam land lies on slopes too steep and
rough for cultivation but the hillside table lands of this soil are
especially well adapted to grape-growing. The grapes grown here contain
much sugar, therefore keep and ship well, have a high flavor, and are
especially sought for in wine-making; grapes on these soils mature
early, have tough skins, but are only medium-sized berries. The yields
are much more variable on this soil than on the others because of the
great variation in the depth of soil. On deep soils of this loam the
yield is all that could be desired. Because of the lay of the land, and
the nature of the soil, there is much washing and cultivation must be
done judiciously.
The climate is exceptionally favorable for the grape-grower in the
Chautauqua district. It is, if anything, of more importance than the
land; for grape soils are not uncommon, but a grape climate as near
perfection as that of this region is indeed rare. The influence of the
lake in modifying the temperature of the region is the chief climatic
factor. This influence need not be dwelt upon here for it is common
knowledge that large bodies of water temper cold winter weather, hold
back vegetation in spring, equalize night and day temperatures of
summer, lengthen the growing season and ward off autumn frosts. Each of
these influences is highly favorable to the growth of the grape. The
escarpment on the southeastern boundary of the belt has a most decided
influence on the climate chiefly because it confines the influence of
the lake to a narrow belt. When the escarpment becomes low, as at the
two extremities of the belt, grape-growing ceases to be profitable. When
the distance between the lake and the escarpment is great, the climatic
conditions are not so favorable.
Public-domain text, read in full here on John Shaqi.
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