Geographical area. Dominant trees. Charac teris tic ground flora. Silviculture. Climatic factors. Top ograph y. Central and eastern Prince Edward Island. Magaguadavic — Hillsborough Ecoregion The inland portions of southern New Brunswick and central areas in Prince Edward Island and Nova Scotia support forests with much in common, and are considered together in the Magaguadavic — Hillsborough Ecoregion. Tolerant hardwoods, locally of good quality, are abundant on upland sites. Red oak and black cherry are widely distributed. Mainly coniferous forests are found on the steep slopes of narrow valleys, on broad valley bottoms, and on outwash plains. Balsam fir, hemlock, white spruce, red spruce and white pine predominate on the valley tills; white pine, balsam fir and black spruce on the sandy outwashes. lntolerant stands of red maple, wire birch and aspen are also prominent. Species of the forest floor that distinguish the Ecoregion include dogtooth-violet, cucumber-root, yellow violet and zigzag smilacina. These plants are not limited to the Ecoregion, but are more widely distributed here and contribute to the distinctive nature of the vegetation. The light-textured soils and coniferous lower slopes present little difficulty to forest management. White birch and other intolerant hardwoods occupy some of this land, but their replacement by spruce, fir and pine can be expected. The fir is not so long—lived or of as good quality as in other parts of the Maritime Provinces; 60 to 80—year-old stems are frequently decadent. Sugar maple, beech and red maple reproduction comprise the aggressive competition on tolerant hardwood sites. Quality sugar maple and yellow birch could be grown on some soils if suitable treatments were carried out (Jarvis, 1956). Much of the land has been cleared for agriculture and where it has reverted to white spruce (or in a few places white pine) these species do well. The climate differs from that of the surrounding ecoregions in the low summer precipitation, warm summer temperature and high potential evapotranspiration. A water deficiency prevails throughout most of the Ecoregion, the LaHave District in Nova Scotia being the exception. Since water deficiency data were not available for stations indicating the high temperatures and relatively low summer precipitation, this exception may be an inadequacy of the available data. Rolling, drumlinoid topography and moderately deep sandy-loam soils are frequent. Sandy outwash soils are locally abundant in southern New Brunswick. lpp. 109-10] [Loucks divided this ecoregion into eight districts: four cover a large contiguous area in south-western New Brunswick (see Figure 6/, with a fifth in the nearby Kennebecasis Valley; two are in Nova Scot/a: one in the interior of south—western Nova Scot/a, the other in the Pictou and Antigonish areas. The eighth district, the Hillsborough District, is confined to Prince Edward Island — see Figure 5 (below).] HILLSBOROUGH DISTRICT: Comprised of rolling land below 500 feet in elevation in central Prince Edward Island and protected by distance from the desiccating winds off the Gulf of St. Lawrence. The water deficiency indicated in Fig. 3 (d) [not included here] distinguishes the climate. Sugar maple and beech with scattered yellow birch predominate on uncleared areas; hemlock and red spruce are limited to lower slopes and moist sites. The characteristic relief pattern is illustrated in Fig. 8. [Fig. 8 is a photograph with the following caption: Rolling forest and agricultural lands in the Hillsborough District, Prince Edward Island. As a rule only the steep slopes with scattered rock outcroppings have been left uncleared] 25