Ontario is Canada's second largest Province, 1.1 million sq. km bounded on the north by the Hudson Bay, in
the south by the Great Lakes and St. Lawrence River. Its vast land goes from flat bogs and small tree forests
of the north, to dense forest, 1000 lakes, and rocky hills to the more populated lands of the south. Ontario
extends below the 49th parallel more than any other part of Canada.
Extending between Lake Ontario and Lake Erie to the East and Lake Huron to the West is where Ontario wine
producers grow their grapes. The fertile soils and moderate climate combine to produce orchards and vineyards
yielding fruits of unique character and supreme quality. The word Ontario means sparkling water. To some of us,
it means tasting the fruits of the soil..wine.
Tony Aspler in his book "Wine Lover's
Companion" refers to Ontario icewine as the
world's best tasting secret. Perhaps today we should Ontario wines are the world's best tasting secret.
The Ontario growing region lies most between the 52º and 41º placing them in the middle of
the northern grape growing belt. The same latitude as Bordeaux, France and the Northern wine regions of California.
Most Ontario Vineyards are located in or near the historic Niagara-on-the-Lake, Ontario's oldest community.
The QC (Quality Certified) symbol on Fruit Wines of Ontario bottles means
you are buying wine made with 100% Ontario-grown fruit. QC is modeled on
the same quality standards as VQA. VQA (Vintners Quality Alliance) is a symbol
of quality and designation of origin for Ontario wines produced in four Viticultural
Areas: Niagara Peninsula, Pelee Island, Lake Erie North Shore and Prince Edward
Ontario is a much younger wine growing area than european countries and has
so far identified four primary viticultural areas and 12 sub appellations.
The four viticultural areas are: Niagara
Peninsula, Lake Erie North Shore, Pelee
Island and Prince Edward
County. We recently added the South Georgian Bay Region and Lake Erie South Coast
There are vintners who grow their grapes in the Niagara Peninsula and the
winery location is in the Toronto area. Numerous winemakers are setting new
frontiers growing grapes in different areas of the Province, for now they are
simply known as 0ff the Beaten Path
The following information has been provided to this website by VQA Ontario*
We appreciate their assistance in helping us provide you with the best information
The Niagara Peninsula
The Niagara Peninsula is the largest Viticultural Area in Ontario (and Canada), accounting for almost
three quarters of Canada's grape-growing volume with approximately 11,000 acres of wine grapes in place.
Situated at approximately N43º latitude, the growing season sunshine is comparable to the
Languedoc-Rousillon in France, south of both Burgundy and Bordeaux, or Tuscany, Italy. Wines grown in such
temperate climates can produce superior fruit, with more complexity and intense flavours than in warmer
It is bordered by Lake Ontario on the north and the Niagara River on the east and the Welland River and
Hamilton to the south and west. Where the Niagara River flows over the Niagara Escarpment, the most predominant
topographical feature of the peninsula, the river is transformed into one of the seven great wonders of the
world, Niagara Falls.
The Niagara Escarpment is a 335 metre (575 ft.) high ridge that winds for 725 km (550 miles) from New York
State through Queenston, Ontario (near Niagara Falls) to Tobermory in northern Ontario, where it continues
underwater to Manitoulin Island and then into the state of Michigan. Passing through the Niagara Peninsula,
the Escarpment provides the essence of this appellation. Vineyards benefit from the lake's offshore breezes,
which are reflected back to the lake when they reach the escarpment, maintaining constant and active airflow.
This circulating activity prevents cold air from settling in lower-lying areas during threatening periods of
frost, and maximizes the moderating effect of the warm waters of the lake.
The region's temperatures are influenced by Lake Ontario, which acts as a hot water bottle in winter –
raising winter temperatures on land from its summer-warmed waters. In spring, breezes from its winter-cooled
waters help to hold back the development of fruit buds until the danger of late spring frosts has passed.
Lake Ontario also cools the summer air so that grapes do not ripen too quickly, and then keeps the fall air
comparatively warm so that the first frost is delayed, thus extending the growing season. Approximately 85%
of Ontario's VQA wineries are located in the Niagara Peninsula.
Lake Erie North Shore
The vineyards of Southwestern Ontario cover over 500 acres situated in a flavoured mesoclimate along the
north shore of Lake Erie in Essex, Kent and Elgin counties, except that part of Kent county lying to the
north of the Thames River. The grape growing area stretches along the bow-shaped shoreline of Lake Erie
from Amherstburg to Leamington, with a further concentration of vineyards around the town of Blenheim to
the east. Soil structures vary from gravely loam to clay and sandy loam. With southern exposure complemented
by the moderating effect of the lake, this Viticultural Area produces some of Canada's finest wines.
Lake Erie is the shallowest of the Great Lakes affording it the warmest surface temperature of the five
lakes. This region also benefits from an abundance of sunshine, and as a result its fruit often goes to market
weeks before that from other parts of Ontario. Lake Erie North Shore lies at a latitude of approximately N 42°, similar to well known wine growing regions in Navarra, Spain and Abruzzi, Italy.
Pelee Island, marginally nearer the equator than Rome at N41° 45' latitude, is Canada's
most southerly point, and accordingly, it enjoys a longer growing season than any other wine region in Canada.
Situated in Lake Erie, 25 kilometres (15 miles) off the mainland, Pelee Island has 500 acres under vine. The southerly
location and surrounding waters give rise to an early harvest and picking usually begins at the end of August.
Even late-harvest grapes are often in by mid October.
The sandy loam and clay soils of this island, lying over limestone bedrock, are similar to those of the
mainland in southwestern Ontario. Canada's first commercial wine growing operation began here in 1866 when
a winery called VinVilla opened its doors. The vineyards were replanted with mostly Vitis Vinifera vines
starting in 1980. In 2013 The AVA status of Pelee Island was removed and it was placed under the Lake Erie North Shore
Prince Edward County
Prince Edward County, located in southern Ontario just west of Kingston, recently emerged as a wine
growing region. The appellation includes lands within the political boundaries of Prince Edward
County and surrounding areas to the north and east. The area has a long history of fruit
production, notably apples, and enjoys the moderating effect on temperatures of an extensive shoreline
along the north shore of Lake Ontario. The geology of the region is characterized by calciferous
bedded limestone and soils are typically well drained, rocky and can be relatively shallow, but with variations across the region.
Plantings are primarily vitis vinifera varieties with an early emphasis on Chardonnay and Pinot Noir.
The potential for many other grape varieties is being explored as the region develops viticultural practices
that best express the terroir of the “County”.
Ontario South Coast Wineries & Growers Assoc
Ontario's newest region seeking AVA. status.
It runs along Lake Erie North
Shore Region just east of the current Lake Erie North Shore AVA and west of the Niagara region .Documentation shows that missionaries Dollier
and Galinee made wine from grapes grown wild here in the late 1600s.
Cities here include Simcoe, St Thomas, Aylme and
St.Williams. Quai Du Vin Estate Winery is the most established winery in the region planting their vineyard in the 1979s
Sub-Appellations within the Niagara Peninsula
As a result of decades of grape growing experience and extensive research, ten unique growing areas
within the Niagara Peninsula have been identified. These sub-appellations include areas on the plains
close to Lake Ontario and the benchlands of the Niagara Escarpment.
Wines owe their character to a combination of origin and the winemaker's art. Together, they give us wines
that are unique from the different appellations.
Only wines made from 100% grapes grown in a sub-appellation are permitted to
make the corresponding claim of origin on the label. In addition to sub-appellations,
two regions have been created to regulate the use of widely recognized names – Niagara-on-the-Lake
and Niagara Escarpment. Niagara-on-the-Lake may appear on the label of a wine
sourced from the growing area east of St. Catharines and Niagara Escarpment may
be used on wines sourced along the bench area west of St. Catharines. To use
these regional designations, at least 85% of the grapes used must come from
the named area, with the balance grown in the Niagara Peninsula. Origin may be
further specified by one of the following sub-appellations if 100% of the grapes
used originate from the stated sub-appellation.
The Niagara River appellation is a small strip of land running along the river from John Street to Dee
Road and inland to the first Concession road. Niagara's famous scenic tourist route, the Niagara River
Parkway weaves up the length of the appellation. Soils in the area are primarily stratified glaciolacustrine
fine sands, providing natural drainage and strong encouragement for vines to develop deep root penetration.
The fast flowing Niagara River creates convectional currents that draw cooler air into the gorge, moderating
vineyard temperatures and reducing frost risks. Slopes in the area are predominantly east facing which is
unique in the region. These factors create excellent growing conditions for tender varieties and contribute
complex flavours to the grapes.
Niagara Lakeshore follows the shoreline of Lake Ontario from the Welland Canal east to the Niagara River
and proceeds inland for approximately 3 kilometers. The primary influence on this appellation is the
proximity of the Lake and its year round effect on temperatures. Soils in the area are primarily
glaciolacustrine near shore and deltaic sands and silts deposited on Halton Till with relatively high water-
holding capacities. These light soils together with the long growing season contribute to flavour development
in grapes and mature, full bodied wines.
Four Mile Creek
Four Mile Creek comprises the fertile plain that makes up central Niagara-on-the-Lake. It lies slightly
inland and below the bench of the Niagara Escarpment providing for warm days and cool nights during the
growing season. Soils are red shale with a high silt and clay content, good water retention and ideal
characteristics for vines.The relatively flat topography leads to abundant sunshine and warm days giving
growers the opportunity to grow many varieties. Four Mile Creek is the largest sub-appellation in the
St. David's Bench
St. David's Bench describes the natural bench formed when glaciers carved out the Niagara Escarpment.
The land rises from the historic shoreline of Lake Iroquois towards the base of the escarpment where a
steep ridge provides steady air circulation. Topography of the bench is complex and the sub-appellation
approximately follows the contour lines that define the escarpment and runs from the Niagara River to
Beechwood Road. Moderately well drained glaciolacustrine silty clays combined with ground water flow from
the base of the escarpment provide steady moisture throughout the growing season. The escarpment
topography also provides early spring warming with good air circulation and frost protection.
Niagara-on-the-Lake is made up of all land within Niagara River, Niagara Lakeshore, Four Mile Creek and
St. David's Bench sub-appellations. Niagara-on-the-Lake has long been used to refer to the lands in this
area and to wine that originates there. To use this municipal designation, a wine must be sourced from at
least 85% of grapes from the area with the balance from within the Niagara Peninsula.
Creek Shores is bounded by Lake Ontario, Twelve Mile Creek, Twenty Mile Creek and Jordan Harbour, and
Regional Road 81 to the south which defines the lower boundary of the escarpment bench. It is a delta
shaped area characterized with long gentle slopes and an abundance of small creeks draining into Lake
Ontario. Soils are a complex series of glacial, fluvial and lacustrine sediments underlain by Queenston
shale. Temperatures are moderated by Lake Ontario and smaller water bodies and spring warming and
bud break are slightly delayed.
The Lincoln Lakeshore follows the Lake Ontario shore from Winona Road to Jordan Harbour and Twenty Mile
Creek, pushing inland to Regional Road 81.
This land mass is characterized by long gentle slopes that grade from the Lake Iroquois Bluff and numerous
seasonal streams. Glacial, fluvial and lacustrine sedimentary deposits have resulted in a variety of soil
types and depths, but soils are primarily light-texture and well to moderately-drained. Again, Lake Ontario
has a major impact and provides longer, tempered growing conditions and even ripening.
Short Hills Bench
Short Hills Bench is the most easterly of appellations making up the Niagara Escarpment.
It includes the land south of Regional Road 81 rising up towards the Escarpment Brow and situated between
Twelve Mile Creek and Fifteen Mile Creek. Laid down through a long history of geological events, the undulating
topography of Short Hills provides long gentle slopes with excellent drainage and sun exposure. Warm sunny
days and cool nights are perfect for developing grape flavours derived from the complex soil in the area.
Soils makeup is chiefly glaciolacustrine deep water stratified clay and silt and stratified brown silty
clays deposited on clay loam.
Twenty Mile Bench
The Twenty Mile Bench is another segment of the escarpment bench, from Fifteen Mile Creek to just west
of Cherry Avenue. This stretch of the bench is bisected by Twenty Mile Creek and shows complex topography
with a double bench formation rising from Regional Road 81 with changing slopes to the brow of the escarpment.
Glacial activity has provided deep clay and till surface soils, with a high proportion of limestone and
shale. The sheltered north facing slopes offer year round temperature moderation.
The Beamsville Bench completes the Niagara Escarpment running from just west of Cherry Avenue to Park
Road in the east. The narrow bench area is the sloped plateau immediately below the face of the escarpment
continuing down to Regional Road 81. The appellation benefits from the air circulation, frost protection,
slopes and elevation provided by the escarpment topography. The continual air circulation results in minimal
temperature swings and consistent growing conditions. Soils are generally deep and well-drained and numerous
streams provide seasonal water supply. Although a relatively small appellation, the Beamsville Bench
exhibits a unique set of conditions that provide a natural complexity to the wines originating there.
The Short Hills Bench, Twenty Mile Bench and Beamsville Bench collectively form the Niagara Escarpment
which represent the benchlands north of the Niagara Escarpment and west of St. Catharines. The Escarpment
is widely recognized as a designation for all lands on the “bench” in recognition of this dominant topographic
feature. To use this broader designation, a wine must be sourced from at least 85% of grapes from the area
with the balance from within the Niagara Peninsula.
Vinemount Ridge is the appellation above and south of the brow of the escarpment. Covering a broad area,
it is unique in that it exhibits shallow mostly south facing slopes. The geology in the area is dominated
by the Vinemount Moraine and to the east, the Fonthill Kame. This provides early spring warming to
its deep clay soils and early budburst for the vines. The area enjoys warm daytime temperatures and cool