| The History of the Lowbush Blueberry Industry in Nova Scotia, 1880 - 1950 Chapter 1: Blueberries in Nova Scotia
Overview of Blueberry Producing Areas
Click picture to enlarge Vaccinium corymbosum L., the highbush blueberry, occurs in the southwestern counties from Digby around to Halifax bogs, upland rocky barrens, dry soil and along lake margins. [1] The native population is too limited to be of commercial importance. [2]
Yarmouth County
Click picture to enlarge The county population in 1881 was 21,184. The population rose gradually until the Twenties and Thirties when the Depression brought a sharp decline that took it below its 1881 figure. In the mid-Thirties, however, the population rose sharply and continued to rise after the Second World War. Yarmouth County is well supplied with coastal roads but there is little inland transportation, with the exception of the highways to Kemptville and Quinan, the primary blueberrying regions. The county is situated on a gently undulating plain rising slowly from sea level to an elevation of nearly 625 feet in the northeast.The average temperature for the summer months is 59ºF with milder temperatures and greater precipitation falling on the coastal areas. Inland soil moisture deficiencies often occur in the late summer. Large areas in Yarmouth County have been burned over by forest fires many areas having been swept by fire several times. These areas are slow to regenerate forest. Since the climate is conducive to the rapid growth of heath, the burned-over areas generally have a covering of heath, blueberries, lambkill, sweet fern and huckleberry, together with occasional red pine, wire birch and white spruce. Where burned-over areas are covered with bush growth, the dominant species are wire birch, poplar, red maple, willow and alder. There are only two major geologic divisions represented in the area. The rock formations of the Devonian age are granitic and are exposed in three areas of the county. Approximately two-thirds of the county is underlain by Precambrian quartzite and quartz shist.
Click picture to enlarge The parent material of granitic origin is very coarse and gritty in texture, and pale brown to light brownish-grey in colour. The soils are often very shallow over bedrock and in some areas are too thin to support forest growth, leaving room for lower bushes such as the blueberry. Due to the thinness of the soil it is not a county well suited to agriculture, a fact substantiated by the lack of inland population.
Cumberland County
Cumberland County may be divided into three physiographic regions which coincide with the underlying bedrock and agricultural land use. These are the Cobequid Mountains, a range of uplands to the south; the Cumberland plain, a broad area of lowlands extending from the Cobequids to Northumberland Strait and Cumberland Basin in the north and west; and the tidal flats along the coast and in the river estuaries around the head of Cumberland Basin. The Cobequid Mountains rise to elevations from 850 to 1000 feet along a straight east-west line
just to the south.of Springhill. The summits of the hills are broad and rounded and have, in many
instances, been cleared for agricultural purposes. [3] It is along the
ridges of these mountains that most of the Cumberland County blueberries grow. Large amounts
of land were cleared by both the French and English settlers, land which proved most difficult to
farm due to both its relief and rocky soils. By the late 1800's the acreage of improved agricultural
land had reached its greatest extent. By the turn of the century, much of this land had been
abandoned and was soon propagated by blueberries and other lowbush plants. Later, burning was
used to keep back the forests which threatened to encroach upon this newly found source of
wealth.
Cumberland County is both well-populated and well-serviced. It has an abundance of roads which serve the large, dispersed rural population.
Guysborough County
Guysborough County, much like Yarmouth, consists largely of rocky, acidic soils, and is covered
for the most part by extensive forests. The bedrock formations consist of a granitic Devonian
type, and a Mississippian shale. Like Yarmouth, Guysborough has a population which is settled
largely in the coastal regions, with few roads servicing the inland areas. It has a very small
population (one of the smallest in the province), and its few main centres house most of them.
Blueberries in Guysborough County have developed largely in areas where poor soils and fire
have made the land good for little else. It was a latecomer in the berry business, becoming a
competitor commercially only during the 1930's.
The Blueberry Season
In the southern part of the province the season usually started towards the end of July, although if
the weather was warm the season would come earlier. In 1889, the first shipment of the season
left Yarmouth on the 12th of July, the earliest recorded to that date. [4a] In the
northern part of the province it was usually well into the middle of August before any large
amounts of berries could be harvested.
In these regions of the province a good season tends to last four to six weeks. The season is, of
course, somewhat reliant upon Nova Scotia's unreliable weather. Too wet, too dry or too cold
weather could and has often interfered with the length and success of the season (there is no
record of it ever being too hot!).
Several years in the period under study sustained unexpected frosts in late August and early September which proved devastating to the late crop. In 1888 the Yarmouth Telegram reported that the berries in September were completely ruined by an early frost. [4b] In 1934, the season and yield were greatly reduced in Cumberland by the extreme dryness throughout August [5], while in 1936 the season was shortened by a long stretch of cool rainy days. [6] Despite problems with unpredictable weather and other obstacles, both physical and human, the blueberry industry was and is still an important part of the Nova Scotian economy.
For further information, please contact Wild Blueberry Network Information Centre (WBNIC@nsac.ns.ca). Updated November 17, 1997 |