Halifax is special amongst major cities in North America: the urban core is surrounded not by farms or endless burbs but by forested and coastal landscapes. Even within 30 km of downtown Halifax where approximately three quarters of the population resides, developed areas are interspersed with substantive wild spaces, the major part of it forested.
Within that forested landcape, Sandy Lake and Environs, together with the mostly forested DND property to the northeast with which it is contiguous, constitute one of the largest single patches of mostly undisturbed, mixed Acadian forest with a lot of it in mature to old growth state, and with the full suite of species including those of richer soils such as sugar maple.
Trees were harvested from much of the area up to 50-70 or so years ago, but most of it was conducted using horses or tractors, not the heavy clearcutting equiment used today, and the habitat remains intact or is well on its way to recovering from “highgrading” (taking out all of the larger trees). An exception is a recent, large clearcut on private land to the west of Sandy Lake but not abutting it directly. A large part of area clearcut included trees over 100 years of age. Fortunately, Most of the clearcut is exhibiting vigorous regeneration by a full mix of Acadian forest species. More limited cutting has occurred on some of the recently acquired HRM lands west of Marsh Lake, and there was some clearcutting in the vicinity of the land cleared for the prison on the Jack lake lands, probably in the 1990s
- View Sandy Lake Community Profile (NASCAD doc, 2001) for a description of historical land use.
- View Moraine Brook Forest for an example of forest that was highgraded by forestry practices up to perhaps 40 years ago, but for which the habitat remained largely intact; it’s an exceptionately beautiful hemlock dominated forest.
- View Clearcuts for views, information about the recent clearcut on the west side of Sandy Lake.
Big Old Trees and Old Growth stands
Patches of forest with “big, old trees” and other features of Old Growth forest occur here and there in the forests stands around Sandy Lake and to the northwest towards and beyond the west side of Marsh Lake. Trees at several such sites were aged and other observations conducted, allowing the stands to be formally assessed for Old Growth Status according to a scheme developed by Nova Scotia DNR (now Lands and Forestry); typical ages are 100-140 years, and for one stand on “The Peninsula” assessed earlier by Ed Glover/DNR older trees were in the range 190-211 years. It seems these stands were simply missed or never got to in the days when these forests were harvested. They include hemlock-dominated, pine-dominated, hardwood dominated and mixedwood stands. These are real gems in an age when such forests are rare on the Nova Scotia landscape at large. (View more about them under Forests>Mature/OG Forests.)
Wind Disturbance/Pit and Mound Topography
One of the stories is about wind. A pit and mound topography is found throughout much of the forest and reveals an ‘old process’ of development towards an old growth state interrupted by wind disturbance, a process that can be seen continuing today in blowdown of big trees initiated by Hurricane Juan. (View Video). These processes seem to be especially pronounced in this forest close to the windy coast in our windy province. In places, the pit and mound structures occur in a repeated series with the long axes of mounds oriented perpendicular to the direction of wind that blew the trees down; walking across them in the direction of the wind is something akin to swimming or paddling through a set of swells in the ocean.
The mounds were formed by blowdowns of very large trees, which I estimate occurred about 150 years ago at many sites. The mounds are preferred ground for establishment of tree seedlings, and most of the big trees we see today are found on top of mounds. The pits often develop as vernal (temporary) pools, providing habitat for amphibians and other organisms requiring water for part of their life cycle. As the trees grow old and mounds erode, the tree roots are exposed creating cavities for wildlife between the roots and the trunk. Trees snap off in a windstorm or just die in place providing “snags” that support another suite of wildlife, and when they fall over, another suite as they gradually return to and enrich the earth. View more about Pit and Mound Topography at Sandy Lake & Environs
American beech trees which occur both as old dead skeletons (beech wood is very slow to rot) and as some quasi-healthy large trees and as many smaller trees and seedings, tell of another kind of forest disturbance. It was a pathogen that came to North America via Halifax. Viewing the beech trees and the pit and mound topography reminds us to think about forest lifespans over longer time intervals than those of our own lives, and that diverse forests in which natural processes are maintained are resilient. Freed from the pressures to clearcut or otherwise improve the forests, we can allow the natural processes to continue.
The presence of cyanolichens on the maples tell us this forest is protecting the air by the ground where we walk. The spring wildlfowers will tell another story, and birds tell more.
A phenomenon that I observed on only my second hike in the area, the physically close association of hemlock and yellow birch, led to another intriguing story, about Acadian Forest Love Affair(s).
And then there are the old forestry roads or routes, and other evidence of forestry in days gone by, and signs of an old farm in the area of the parking lot; and harder to see because they tread more softly on our landscapes, evidence of activities by indigenous peoples.*
These are fascinating forests that are quite easily accessed with countless trails and spots which allow visitors to bask in the Acadian forest as we might wish it to be over more of Nova Scotia today, but isn’t or is being lost to intensive forestry.
*View Sandy Lake Community Profile (NASCAD doc, 2001) for a description of historical land use.