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.
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.
The air currents and rainfall of the region are especially favorable. The in-shore breeze of the day and the off-shore breeze at night keep the air in constant motion, thus preventing frosts in spring and autumn, and probably cause in part the great degree of immunity to black-rot and mildew. Unfortunately, data to determine accurately the rainfall of the district cannot be had but such as have been taken indicate that the rainfall is comparatively light for the maturing months of August, September and October and not heavy for the three preceding growing months. Residents of the grape belt claim that most of the heavy showers pass over the hills or down the lake. The whole region is proverbially free from heavy dews. Rain and dew are favorable to black-rot and other fungi and the lack of them still further accounts for the immunity to these pests in the region.
The history of the rise of grape-growing in Chautauqua County forms an interesting chapter in the economic development of New York. The first vines in the Chautauqua district were planted by Elijah Fay[97] in 1818, near the present town of Brocton. These were wild vines of Vitis labrusca from Deacon Fay’s boyhood home in New England. The vines grew luxuriantly but the fruit was not satisfactory and in 1822 this worthy pioneer obtained at great trouble roots of Miller’s Burgundy, Sweetwater and Black Hamburg. But the second experiment was even more disastrous than the first as he got no fruit. The real start was made in 1824 when Mr. Fay obtained vines of Catawba and Isabella from Prince of Flushing, Long Island. The vines were trained on trellises. The vineyard covered a plot two by eight rods in extent. From a rise of land near this spot one now sees grapes everywhere, probably a greater acreage of them than can be seen from any other spot east of the Rocky Mountains.
In 1830 Deacon Fay made ten gallons of wine, the first for the region. In 1834, Lincoln Fay, a nephew of Elijah Fay, started the sale of grape vines but not many vines were sold for commercial plantings until as late as 1850. In 1859 there were in the town of Portland but twenty acres of bearing grape vines where now are thousands. During the decade that followed, the Concord was generally introduced giving the viticulture of the region a great impetus. Grapes were not yet grown for table use to any great extent and a large acreage could not be used for wine-making. In 1859 a wine-cellar was built by Fay, Ryckman[98] and Haywood at Brocton and for a long while this company used almost the total crop of the region. It was not until the early seventies that the grape-growers sought other markets than the wine-cellars. In 1870 there were about 600 acres of vineyards in Chautauqua County.
The first table-grapes of the region were packed in twenty-pound splint baskets. Dunkirk was the primary marketing place and the fruit was shipped from here to various large cities by through freight. The transportation facilities were not satisfactory and in 1880 Jonas Martin of Brocton tried the experiment of shipping a carload of grapes to Philadelphia. This was the first carload of grapes sent from Chautauqua County. In 1906, 4690 carloads were shipped and 844 were converted into wine and grape juice, representing all told $2,482,822.[99] Until 1883 the markets were confined to nearby cities but in this year a carload was safely sent to Spokane, after which time markets were found from the Atlantic to the Pacific and from the Gulf to Upper Canada. The first grape-growers’ union was formed in 1886 as the Chautauqua Grape Growers’ Shipping Association and its organization marked a new epoch in the grape industry of the district. Smaller and larger organizations have since been formed and at the present time about 80 per ct. of the entire crop is handled by a growers’ union known as the Chautauqua and Erie Grape Company.
According to Mr. G. E. Ryckman, in the early days of the grape industry in this region the fruit was shipped in round paper baskets holding from three to five pounds; later these were made of wood. Sometime in the early seventies twenty-pound splint baskets, which were supposed to be returned to the owners, were introduced. These were superseded by the twelve-pound climax basket; the size of this basket was soon reduced to ten pounds, then to nine, then to eight. Meanwhile a small five-pound basket made on the same lines as the larger one came into use but soon shrunk into a four-pound receptacle. The eight and the four-pound climax baskets are now generally used throughout the region. Increasing quantities are now being shipped to large cities in trays with slatted tops holding about forty pounds each; these grapes are used by the purchaser for wine-making. The wine and grape juice industries of the region have been touched upon in the general discussion of these industries.