The largest areas of Dunkirk clay are found running back from the lake
east and west from Barcelona, in the neighborhood of Van Buren Point and
about Dunkirk. In these regions the soil is a clay loam from several
inches to a foot deep resting upon a stiffer and more tenacious clay.
Vineyards located on this soil are very productive but the quality is
not as high as in the fruit grown on the shale loam, though for most
part superior to that produced on the gravel and sandy loams.
Dunkirk gravel soils are found on the ridges at the foot of the
escarpment on the southern boundary of the district from Pennsylvania to
the eastern boundary of the grape district. Throughout most of this
distance there are from one to three parallel ridges varying from a few
rods to a half mile in breadth; at many places the ridges run into each
other or have been brought together by cultivation. It was upon this
gravel that vines were first successfully grown. Grapes upon this soil
ripen a week or more earlier than upon other soils and these lands are
therefore largely planted with vineyards to supply the early market and
they have a larger proportion of early varieties than vineyards on other
soils. The Niagara is thought to do especially well on Dunkirk gravel.
Dunkirk gravelly loam is found running through practically the whole
grape belt at the base or on the top of the gravel ridges; if at the
base, to lakeward of the ridges. It is a sandy loam with much fine
gravel and is underlaid at a depth of three feet with sand and shale
fragments. On the surface it much resembles the gravel soils having had
considerable top gravel brought there by washing and by cultivation. The
grapes grown on these soils are very similar to those produced on the
gravels though there are some minor differences. Some varieties produce
larger berries on this soil, and some sorts, it is claimed, a greater
amount of wood.
The Dunkirk sandy loams occur in large irregular areas bordering the
lake or running from the lake bluff back to the escarpment. By far the
largest of these areas is found about Fredonia and Dunkirk and running
east and west of these towns. A second area is found in the neighborhood
of Brocton and Portland and especially to the north and west. There are
smaller areas east of Barcelona and northwest of Ripley. Nearly all of
the sandy loam soils are found on undulating or rolling land. The soil
is a brownish-yellow loam from a half foot to a foot in depth. There are
some deviations from the type and yet the true sandy loams can be very
easily recognized. The soil is of rather heavy texture making good
farming land and producing large crops of grapes of slightly inferior
quality.
Public-domain text, read in full here on John Shaqi.
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