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Background
Study Area
Objectives
The Adirondack Ecological Zone, corresponding to the legislatively defined New York State Adirondack Park, comprises a 6 million-acre (2.4 million-ha), predominately forested region of northern New York (Figure 1). Nearly 340,000 wetland hectares, including deepwater marshes, rich fens, kettlehole bogs and over 3,000 associated lakes and ponds are situated in the region. Approximately 43% (2.5 million acres, 1 million ha) of the Park is owned by the State of New York and is constitutionally protected as "forever-wild" Forest Preserve. Private lands devoted principally to forestry, agriculture, and open-space recreation account for 57% of the Park (3.5 million acres, 1.4 million ha). The Park contains the largest wilderness acreage east of the Mississippi River as well as numerous settlement areas with attendant use conflicts. Because of the biological diversity in wetlands and the range of land uses, the Park is an ideal area in which to undertake a project seeking to characterize the wetland resource on a detailed watershed basis.
The St. Lawrence River watershed is located in the northwestern Adirondack Park and is comprised of the Grass, Raquette, Salmon, and St. Regis rivers that ultimately drain northwest into the St. Lawrence River (Figure 2). The St. Lawrence Watershed spans approximately 50 7.5-minute quadrangle sheets. It contains the Park's largest natural wetland complexes, including Massawepie Mire (5000 acres, 2,023 ha), Madawaska Wetland (3000 acres, 1,214 ha) and others (Table 1); it contains almost all of the Park's low elevation boreal biome; and it is largely privately owned by relatively few large landowners. Because of its hydrologic, ecological and ownership characteristics, this watershed offers a unique opportunity to gather spatial data on sub-watersheds and wetlands. The data created for this project have been used to:
This report, Part One (of Two) of the St. Lawrence River Watershed Project, focuses on the wetland resources of the St. Regis River Basin, a sub-watershed of the St. Lawrence River watershed. Part Two will report on the remaining portions of the St. Lawrence River watershed in which some of the largest wetland complexes are found.
STUDY AREA: St. Regis River Basin
The St. Regis River Basin falls between 44.3°N and 44.7°N latitude and 74.8°W and 74.2°W longitude and measures 342,000 acres (138,400 ha) (Figure 2). It spans 19 7.5-minute quadrangles (Appendix 1). 53.5% of the St. Regis Watershed is categorized under the Adirondack Park Land Use and Development Plan land classification system as Resource Management, which includes forest management and agricultural uses (State of New York 1998). Elevation in the watershed ranges from 679 ft. to 3,310 ft. (207 m - 1009 m). Higher elevations occur in the west and south causing the basin to drain northeast into the St. Lawrence River.
Long cold winters and short cool summers characterize the climate of the St. Regis River Basin. Average temperature, rainfall and snowfall vary locally within the watershed and are affected by differences in elevation and location relative to mountain ranges, prevailing wind and local bodies of water. Average precipitation reported at the Lawrenceville, St. Lawrence County weather station, which is just outside the Park but within the St. Regis River Basin (44°43'N, 74°45'W, 499.9 ft. (152.4 m) elev.) is 37.5 in. (952.3 mm) per year (NOAA 1992). Mean annual temperature at this station is 43.8°F (6.6°C), and has historically ranged from 15.8°F (-9.0°C) in January to 72.3°F (22.4°C) in July (NOAA 1999)
OBJECTIVES
Based on the successes of the Oswegatchie-Black River Watershed and Upper Hudson Watershed mapping projects conducted by the Adirondack Park Agency (APA) in partnership with the State University of New York at Plattsburgh and the Adirondack Lakes Survey Corporation (Roy et al. 1996, Roy et al. 1997, Primack et al., 2000), the objectives of this project were to (APA 1996):
The final objective, that of landowner outreach, was highly important to this project in that it allowed for interchange between the public and private sectors. At the same time as the landowner participants were learning what the APA could provide them, such as natural resource maps, the APA gained insight into the specific issues important to land managers. The meetings with the landowners were successful in building ties between a State agency and the citizens it serves.
Wetland Name | Wetland River Basin | Estimated Size | Description |
Madawaska Wetland | St. Regis | 3000 ac (1214 ha) | Series of open bogs with Sphagnum-sedge-leatherleaf mats surrounded by mature stands of black spruce and tamarack with scattered balsam fir and white pine. |
Waverly Bog | St. Regis | 2237 ac (905 ha) | Flat, continuous, peat mat with abundant sedges. |
Osgood River Muskeg | St. Regis | 1750 ac (708 ha) | Black spruce tamarack swamp. |
Spring Pond Bog | St. Regis/Raquette | 900-1000 ac (364-405 ha) | Nutrient-poor, sedge-Sphagnum patterned fen and low-shrub raised bog with ponds. |
Bay Pond Bog | St. Regis | 300 ac (121 ha) | Nutrient-poor, sedge-Sphagnum patterned fen and low-shrub raised bog. |
Wheeler Marsh | St. Regis | 850 ac (344 ha) | Poor fen. |
Jones Pond Outlet | St. Regis | 120 ac (49 ha) | Floating mat with ericaceous component and cattail component. |
Roiley Bog | St. Regis | 300 ac (121 ha) | Poor fen with areas of Sphagnum bog. |
Deer Pond Marsh | St. Regis/Saranac | 1000 ac (405 ha) | Complex wetland system with deep organic deposits. |
Massawepie Mire | Grass | 5000 ac (2023 ha) | Largest open heath-Sphagnum mats in the Northeast, Estimated peatland acreage: 900 ac (364 ha) (Worley 1982). |
Grass River Bog | Grass | 900 ac (364 ha) | Poor fen on north shore of Grass River Flow. |
Sevey Bog | Raquette/Grass | 400 ac (162 ha) | Poor fen, hemlock hardwood swamp, spruce flats. |
Tupper Lake Marsh | Raquette | 1100 ac (445 ha) | Deep emergent marsh. |
Hitchens Bog | Raquette | 1050 ac (425 ha) | Poor fen with patterning evident. |
Continue to next section of St. Regis Report: Literature Survey
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References Cited