Source: https://www.federalregister.gov/documents/2005/09/08/05-17759/establishment-of-the-niagara-escarpment-viticultural-area-2004r-589p
Timestamp: 2017-10-17 21:21:36
Document Index: 512780217

Matched Legal Cases: ['art 9', 'art 4', 'art 4', 'art 9', '§\u20099', '§\u20099', 'art 4']

Federal Register :: Establishment of the Niagara Escarpment Viticultural Area (2004R-589P)
Establishment of the Niagara Escarpment Viticultural Area (2004R-589P)
70 FR 53300
53300-53304 (5 pages)
T.D. TTB-33
Re: Notice No. 33
Niagara Escarpment Petition and Rulemaking
https://www.federalregister.gov/d/05-17759 https://www.federalregister.gov/d/05-17759
Section 4.25(e)(1)(i) of the TTB regulations (27 CFR 4.25(e)(1)(i)) defines a viticultural area for American wine as a delimited grape-growing region distinguishable by geographical features, the boundaries of which have been recognized and defined in part 9 Start Printed Page 53301of the regulations. These designations allow vintners and consumers to attribute a given quality, reputation, or other characteristic of a wine made from grapes grown in an area to its geographic origin. The establishment of viticultural areas allows vintners to describe more accurately the origin of their wines to consumers and helps consumers to identify wines they may purchase. Establishment of a viticultural area is neither an approval nor an endorsement by TTB of the wine produced in that area.
A copy of the appropriate USGS map(s) with the proposed viticultural area's boundaries prominently marked.
Michael Von Heckler of Warm Lake Estate Vineyard and Winery petitioned TTB for the establishment of an American viticultural area to be called “Niagara Escarpment” in Niagara County, New York. The proposed 18,000-acre viticultural area includes approximately 400 acres of vineyards. The proposed boundary area runs in a narrow 28-mile wide band, starting at the village of Johnson Creek, traveling west through the towns of Gasport and Lockport, and ending at the Niagara River at Lewiston.
The proposed Niagara Escarpment viticultural area derives its name from the Niagara Escarpment, a limestone ridge that runs for more than 650 miles through the Great Lakes region. The Niagara Escarpment forms a geological horseshoe that begins near Rochester, New York, and continues west through southern Ontario, Canada, Lake Huron, the upper peninsula of Michigan, and terminates in eastern Wisconsin.
The Niagara Escarpment enters Niagara County in the east near Johnson Creek and then runs west through the middle of the county along State Route 104 to the town of Lewiston. At the west end of Niagara County, the escarpment crosses the Niagara River Gorge, and Niagara Falls is at the head of the gorge.
Excerpts from Government and travel Internet sites discuss the Niagara Escarpment in Niagara County. These include:
A page on the Institute for Local Governance and Regional Growth Web site that discusses how the Niagara River flows over the Niagara Escarpment creating Niagara Falls. (See http://www.regional-institute.buffalo.edu/​regi/​natu.html)
Vintage New York's Web site states that the prime vineyard sites in western New York are “bordered by the Niagara River on the west, Lake Ontario on the north and the Niagara escarpment on the south.” (See http://www.vintagenewyork.com/​regions/​erie.html)
The Niagara Tourism and Convention Corporation's Web site notes that Niagara Landing Wine Cellars, a Niagara County winery, is “located at the base of the Niagara Escarpment.” (See http://www.niagara-usa.com/​attractions/​niagaralanding.html)
The Western New York Regional Information Network's Town of Cambria Web site describes the town as an agricultural town “divided in the middle by the Niagara Escarpment.” (See http://www.wnyrin.com/​c_​niag/​welc/​juri/​juri_​cambt)
The geography of the Niagara Escarpment defines the boundary of the proposed viticultural area. The steepness of the Niagara Escarpment makes it topographically distinct from the Ontario Plain, which extends from the south shore of Lake Ontario to the base of the escarpment, and the Huron Plain, which begins at the escarpment's crest and extends southward past the Niagara County line.
The Ontario Plain and the Huron Plain are relatively flat, with slopes of less than 20 feet per mile, according to the Soil Survey of Niagara County, New York (1972). In contrast, the Niagara Escarpment has a steep slope of 106 to 317 feet per mile. The southern and northern boundaries of the proposed Niagara Escarpment viticultural area encompass the north-facing slope of the escarpment between the 600- and 400-foot elevation lines. These boundaries generally delineate the high and low altitudes of the slope within the proposed viticultural area boundaries.
The Niagara River, which forms the international boundary line between the United States and Canada, also marks the western boundary of the proposed viticultural area. The portion of the Niagara Escarpment that extends west from the Niagara River, into the Canadian province of Ontario, is included in the Niagara Peninsula viticultural area, as designated by the Government of Canada.
At the eastern end of Niagara County a portion of Johnson Creek, south of the village of the same name, forms the proposed eastern boundary line. East of the creek, elevations at the base of the Niagara Escarpment climb from 400 to 500 feet, and its slope becomes much narrower and steeper. The changes in topography east of Johnson Creek make it less desirable for viticulture. Therefore, the petitioner did not include the escarpment area east of Johnson Creek within the proposed viticultural area boundaries.
The topography and soils of the proposed viticultural area create distinct conditions for grape growing as compared to the surrounding areas. The Ontario and Huron Plains are nearly flat with deep soils that can harbor excessive water and nutrients. In contrast, the Niagara Escarpment has shallow soils with poor nutrient content, and sufficient sloping (2-6 percent) to allow for drainage.
The conditions found in the proposed Niagara Escarpment viticultural area—Start Printed Page 53302well drained soils, sufficient sloping, a steady but moderate water supply, and restricted mineral content—result in grapes with superior pigment and flavor compounds in the resultant wine. On the other hand, the conditions of the surrounding areas beyond the proposed boundaries—poor soil drainage and high nutrient content—result in grapes with less pigmentation, diluted flavors, and a lower quality of wine produced.
As evidence of these soil differences, the “Soil Survey of Niagara County, New York” states that the central portion of Niagara County, along the escarpment, contains the Hilton-Ovid-Ontario soil association. It describes this association as “deep, well-drained to somewhat poorly drained soil.” In contrast, the survey states that the Ontario Plain north of the escarpment contains the Rhinebeck-Ovid-Madalin association, which has “deep, somewhat poorly drained to very poorly drained soils.” The Huron Plain south of the escarpment contains the Odessa-Lakemont-Ovid association, which has “deep, somewhat poorly drained to very poorly drained soils.”
The location of the proposed Niagara Escarpment viticultural area, in relation to Lake Ontario, creates a microclimate conducive to grape growing. The maritime influence of Lake Ontario on the Niagara Escarpment allows for sufficient heat accumulation for the growing season in what is otherwise a cool climate. The “Soil Survey of Niagara County, New York,” notes that Lake Ontario greatly influences the climate of Niagara County. The survey states, “In fall the lake waters are a source of heat that reduces cooling at night and increases the length of [the] freeze-free growing season.”
The climatic relationship between Lake Ontario and the Niagara Escarpment is discussed in greater detail in “Site Selection for Grapes in the Niagara Peninsula,” a publication issued by the Horticultural Research Institute of Ontario to assist grape growers in the Niagara Peninsula of Canada in selecting the best vineyard sites. The climate information of the publication can be applied to the proposed Niagara Escarpment viticultural area, which is adjacent to the Niagara Peninsula and shares Lake Ontario and the Niagara Escarpment with the peninsula.
According to the site selection publication, a unique airflow pattern affects the land between Lake Ontario and the crest of the escarpment. While the land warms quickly on warm days and cools rapidly on cool nights, the lake temperature changes more slowly. In the spring the lake temperature is cooler than the temperature of the adjacent land, while in the fall the lake is warmer than the land. The lake-warmed air rises and draws cooler air in from the lakeshore in the fall and creates offshore breezes. As a result, the site selection publication states, “the air now above the lake is warmed, rises and flows back over the land, creating a circular heat-pump effect.”
In the spring and early summer the airflow pattern of the lake cools the adjacent land. Areas within two miles of the lakeshore can have a two-week delay in bud break due to the cooling effect of the lake. Also, daytime temperatures are often cooler because of the air currents of the lake. The site selection publication notes that “most grape cultivars require a long, warm season and fruit quality is sometimes poor close to the lake because of lower day temperatures.” Conversely, the proposed Niagara Escarpment viticultural area, between 6 and 8 miles from Lake Ontario, experiences little or no delay in bud break or cooler daytime temperatures due to the lake influence.
The “Site Selection for Grapes in the Niagara Peninsula” publication notes: “The pattern airflow is altered by the slope of the land. With steep slopes, cold air drainage is rapid. Flat areas or depressions tend to accumulate cold air and become ‘frost pockets.’ ” For areas between the lake and the escarpment, this airflow pattern minimizes frost conditions and increases heat accumulation, thereby extending the growing season of the proposed Niagara Escarpment viticultural area. Areas south of the escarpment do not benefit from the effect of the airflow pattern and are more prone to frost damage.
The proposed Niagara Escarpment viticultural area has an extended ripening season when compared to grapes grown outside its boundary. In contrast, the areas north of the escarpment experience cooling spring temperatures that retard growth, while areas south of the escarpment are more prone to fall frost damage.
On February 9, 2005, TTB published in the Federal Register (70 FR 6792) a notice of proposed rulemaking regarding the establishment of the Niagara Escarpment viticultural area (Notice No. 33). In that notice, TTB requested comments by April 11, 2005, from all interested persons. TTB received three comments. The first stated concerns with the proposed “Niagara Escarpment” name, and the second constituted a rebuttal from the petitioner on the first comment about the “Niagara Escarpment” name.
The first commenter, Steve DeBaker, is from a grape-growing region of Door and Brown counties in northeast Wisconsin that is located on the Niagara Escarpment. He explained that the escarpment covers a region substantially larger than the proposed viticultural area in New York and suggested amending the proposed viticultural area name to “Niagara Escarpment New York.” In conjunction with the state modifier, Mr. DeBaker expressed interest in petitioning for a “Niagara Escarpment Wisconsin” viticultural area.
The second comment, by the petitioner Michael Von Heckler, argued that the Niagara Escarpment viticultural area, including its name, should be established as originally proposed. Mr. Von Heckler explained that a search of literature for the “Niagara Escarpment Wisconsin” name resulted in information about flora, fauna, and recreational opportunities. The search made no mention of wine grape growing within the Niagara Escarpment geological boundaries in Wisconsin, according to Mr. Von Heckler. Also, the Wisconsin Agricultural Statistics Service does not publish grape production information because the amount of grapes produced is too small to report. Mr. Von Heckler suggested that, at some future time, Mr. DeBaker could submit a petition to expand the boundary of the Niagara Escarpment viticultural area after its establishment.
TTB, after careful consideration of the two comments, believes it is not necessary to establish the “Niagara Escarpment” viticultural area with the “New York” geographical modifier. TTB believes that if a future petitioner, in another area of the Niagara Escarpment, submits a new viticultural area petition, then a geographical modifier, such as Wisconsin, can be added for clarity and to avoid consumer confusion.
TTB also received a third comment on the proposed Niagara Escarpment viticultural area in New York from Start Printed Page 53303Vintners Quality Alliance of Ontario, Canada (VQAO) because Canada is considering designation of a Niagara Escarpment viticultural area in southern Ontario. The VQAO Executive Director, Laurie Macdonald, believes the two Niagara Escarpment viticultural areas, one in Canada and one in the United States, can co-exist without consumer confusion. As she noted, Canadian producers must include the name Canada as the country of origin on the wine label, and wine producers and bottlers in Ontario must also include “VQA” in conjunction with the stated appellation term, such as “Niagara Escarpment.” In light of these comments, we believe that wine produced in the Canadian Niagara Escarpment viticultural area will not be confused with the “Niagara Escarpment” wine produced in the United States.
After careful review of the petition, TTB finds that the evidence submitted supports the establishment of the proposed viticultural area. Therefore, under the authority of the Federal Alcohol Administration Act and part 4 of our regulations, we establish the “Niagara Escarpment” viticultural area in Niagara County, New York, effective 30 days from this document's publication date.
Part 4 of the TTB regulations prohibits any label reference on a wine that indicates or implies an origin other than the wine's true place of origin. With the establishment of this viticultural area and its inclusion in part 9 of the TTB regulations, its name, “Niagara Escarpment,” is recognized as a name of viticultural significance. Consequently, wine bottlers using “Niagara Escarpment” in a brand name, including a trademark, or in another label reference as to the origin of the wine, must ensure that the product is eligible to use the viticultural area's name as an appellation of origin.
2. Amend subpart C by adding § 9.186 to read as follows:
§ 9.186
(a) Name. The name of the viticultural area described in this section is “Niagara Escarpment”. For purposes of part 4 of this chapter, “Niagara Escarpment” is a term of viticultural significance.
(b) Approved Maps. The appropriate maps for determining the boundaries of the “Niagara Escarpment” viticultural area are five United States Geological Survey 1:250,000 scale topographic maps. They are titled:
(1) Lewiston, New York—Ontario, 1980;
(c) Boundary. The Niagara Escarpment viticultural area is located in Niagara County, New York. The boundary of the Niagara Escarpment viticultural area is as described below:
(9) Proceed north on Quaker Road about 0.4 mile to its intersection with State Route 104, and then east on State Route 104 to its intersection with Johnson Creek (at the village of Johnson Creek); then Start Printed Page 53304
(15) Proceed west along Mountain View Drive to its intersection with State Route 104, and then proceed south on State Route 104 to its junction with Fish Creek; then
Signed: July 8, 2005.
[FR Doc. 05-17759 Filed 9-7-05; 8:45 am]