Purpose Statement : To protect the most southerly known stand of tamarack trees in British Columbia See the complete PDF here: chilako-overview Flora aspen, trembling (Populus tremuloides) birch, scrub (Betula nana) juniper, common (Juniperus communis) Labrador tea (Ledum groenlandicum) moss, peat(Sphagnum spp.) pine, lodgepole (Pinus contortvar.latifolia) rose, prickly (Rosa acicularis spp. sayi) soopolallie (Shepherdia canadensis)
Note: Management Planning There is no online management planning information for this Ecological Reserve available at this time. ORIGINAL PURPOSE To preserve aspen, fen and bog ecosystems representative of the Peace River area of the Alberta Plateau. SIGNIFICANT SPECIES Philadelphia Vireos heathed cotton-grass THREATS Climate Change: It has been projected that the effects of climate
ORIGINAL PURPOSE To protect a sand beach, dune ecosystems and inland moor bogs on Haida Gwai See the Complete PDF : Tow Hill ER 9overviewpdf Physical: A broad beach of hard sand is present, partly the result of the presence of Yakan Point which acts as a natural groin and traps sand being moved north
ORIGINAL PURPOSE To preserve habitat for nesting seabirds, mainly petrels, and their habitat OVERVIEW Physical: The reserve comprises a small, oval shaped island near the head of Lepas Bay, about 150 m from shore. Although the island is low, most of its shoreline is steep and rocky, including vertical cliffs on the southwest side, which
ORIGINAL PURPOSE To preserve dry subzone forest ecosystems in the Coastal Western Hemlock Zone at a location convenient for research Physical: The reserve straddles a southwest-northeast trending ridge. Most of its area is on the rolling summit of the ridge above 300 m in elevation but steep slopes occur along the northwest and southeast edges.
ORIGINAL PURPOSE To preserve a fragment of the rapidly disappearing Fraser Valley boglands Physical: The reserve is situated near the northern edge of the Fraser Lowland on a large deltaic plain. Surficial materials originated from Pleistocene glaciation, subsequent marine invasion, and finally deposition of river-borne sediments. The Fraser River sediments, which originated as floodplain and
The following has been adapted from the BC Parks website:
MORICE RIVER ER #81 ORIGINAL PURPOSE To preserve, for research purposes, forest ecosystems representative of the western edge of the Sub-Boreal Spruce Zone. See the full PDF here: morice Physical: The reserve is situated in an area of irregular topography near the western edge of the Nechako Plateau. Just beyond, to the northeast, are the Bulkley Ranges.
ORIGINAL PURPOSE To conserve an undisturbed coastal watershed of wide elevational range for forest ecology, vegetation, wildlife ecology and hydrology studies. Access: Access by helicopter, or by logging road from the village of Gitwinksihlkw on the north side of Nass River. Physical: The reserve comprises the steep southeast facing drainage of Gingietl Creek and a
Original Purpose: To preserve stands of the rare Pacific rhododendron in a site unlikely to be disturbed by recreational use Physical:The reserve consists of two blocks, the lowermost on the gently sloping fan of St. Alice Creek on the floor of the Skagit Valley, the upper block on northeast oriented mountain slopes between St. Alice
ORIGINAL PURPOSE To protect exceptional plant species richness and sensitive meadow and woodland ecosystems developed on cretaceous sandstones. Physical: Woodley Range is a prominent NW-SE-oriented ridge with a steep escarpment to the southwest, facing the head of Ladysmith Harbour, and more gentle, smooth slopes towards the northeast. The reserve is located on the moderate NE-facing
ORIGINAL PURPOSE To maintain stands of alluvial black cottonwoods for purposes of hybridization and stock improvement. Physical: The reserve river with a gradient of about six m/km. The northeast-southwest trending valley, located in the Hozameen Ranges of the Cascade Mountains, is bounded by slopes of about 30o which rise to peaks of 2100-2500 m. The
ORIGINAL PURPOSE To preserve representative valley-bottom forest in an area transitional between coastal and interior climatic conditions Physical: The reserve lies in the Skagit River valley, bounded in the west by the Skagit Range and east by the Hozameen Range. Local peaks rise to the 2150 m elevation. It is primarily on the alluvial fan
ORIGINAL PURPOSE To protect representative north-coastal forest stands and bog vegetation for research on tree species and ecosystem classification Physical: The reserve is at the western edge of the granitic Kitimat Ranges, and contains rounded mountains which were over-topped by Pleistocene glaciers moving westward to the sea. Mountain slopes facing all compass directions are present.
ORIGINAL PURPOSE To set aside unlogged floodplain islands for research on succession in black cottonwood communities. Physical: The reserve comprises three large and four small islands in a low-gradient reach of the Skeena River where reduced river velocities allow sediments from upstream to settle out, forming many bars and islands. The river is slightly sinuous
ORIGINAL PURPOSE To protect one of the few known occurrences of adder’s-tongue fern in British Columbia Physical: The reserve lies in a narrow valley bottom in a pass between the Taylor and Kennedy river drainages, surrounded by peaks of the Vancouver Island ranges. A small pond dammed by an ancient rockslide lies near the middle
Original Purpose To protect a floristically diverse forest site, transitional between coastal and interior conditions, for forestry research. Physical: The reserve is located on the west slope of the Cascade Mountains, an area of strongly folded and metamorphosed Palaeozoic and Mesozoic sedimentary and volcanic rocks. Its soils are primarily Humo-Ferric Podzols formed on glacial till.
ORIGINAL PURPOSE To protect a highly diverse mosaic of ecosystem types from aquatic, peat bog and forest to dry-site ecosystems. Physical: The reserve comprises gently undulating lowlands formed by glacially scoured rocks of the cretaceous Nanaimo Formation. For the most part the cover of surficial deposits and soils on the NW-SE trending, rounded ridges is
ORIGINAL PURPOSE To protect a population of the very rare Austin’s phantom orchid Physical: The reserve is located on a ridge formed by remnants of a major body of inter- and post-glacial outwash. The southern one third has steep, eroding slopes facing the Chilliwack River valley and the remainder slopes gently towards the Fraser Valley
Original Purpose: To establish a research area containing a variety of communities in the Boreal White and Black Spruce Zone. Physical:: The reserve lies on a plain of low relief in the Liard River drainage. Micro-relief is provided by many glacial features, oriented in an east-west direction, including eskers, drumlins and morainal landforms. These show