Section II --
Map Development (continued)
Local Table of Contents:
From: Influences on Wetlands and Lakes in the Adirondack Park of New York State:
A Catalog of Existing and New GIS Data Layers for the
400,000 Hectare Oswegatchie/Black River Watershed,
1997

II.I. General Soils-Parent Material Composite Map OB2 Contents

 

One of the objectives of this study was to determine the underlying soils for the study area by incorporating the best available digital data.

 

ssoils.jpg (11278 bytes)Description of existing digital soils

Source Data: Adirondack Park Agency (APA).

This coverage was produced in 1975 by the Adirondack Park Agency from County general soils maps which were prepared for the APA by the U.S.D.A. Soil Conservation Service as part of their assistance to county soil and water conservation districts in cooperation with Cornell University Agricultural Station. The base map was developed at 1:62500 by the State of New York Office of Planning Coordination. This map is referred to in this report as the "meso soils map".

 

Discussion

Parkwide, 132 map units or soil associations have been identified. Within the 400,000-ha Oswegatchie/Black watershed, 50 soil associations have been identified excluding water and mine dump categories (Table II.I.1). Five of the associations may be considered anomalies based on their small size. The resolution or accuracy of these units or distinction is 40-100 acres (16-40 ha). It is noted that there are some differences associated with matches across county boundaries.

Parkwide, soils have been categorized into nine soil parent materials. All of them are considered acidic, except glacial tills which are near neutral pH. In the Oswegatchie/Black River watershed, only one association, Madalin(f)NL, is so classified, and it is so small as to be considered an anomaly. Therefore, since all the other parent materials found in the Oswegatchie/Black watershed representing over 99.99% of the study areas are acidic, the parent material composite does not provide any differentiating specific information on soil chemistry. The most meaning can be derived by the physical properties of the parent materials, specifically in the way that water can move through them. We note that while carbonate rock inclusions are found in the study area, they are not fully explored or are not detected at this scale.

Table II.I.1 Meso soil associations for the Oswegatchie/Black watershed area.

ID

Description

Slope

Acres

2

Adams/GS

GS

11240

3

Adams/SL

SL

29070

4

Adams/MS

MS

2510

5

Adams-Colton/SL

SL

3230

9

Adams-Croghan/NL

NL

28270

10

Allagash/GS

GS

100

13

Becket/VB/MS

MS

35260

14

Becket-Lyman/VB/SL

SL

38710

15

Becket-Lyman/VB/MS

MS

18790

17

Becket-Skerry/VB/SL

SL

75290

18

Benson-Rock Out(f)/VS/SL

SL

230

20

Berkshire/VB/MS

MS

530

21

Berkshire-Dixmont/S/GS

GS

70

22

Berkshire-Dixmont/VB/GS

GS

18760

23

Berkshire-Dixmont/VB/SL

SL

4540

25

Bice/VS/MS

MS

180

28

Bice-Schroon/VS/GS

GS

50

29

Borosaprists-Fluvaquents/LL

LL

22760

30

Chaumont(f)/NL

NL

280

33

Colton/NL

NL

2560

34

Colton/GS

GS

41700

35

Colton/SL

SL

40310

36

Colton/MS

MS

2870

40

Coveytown-Cook/NL

NL

90

44

Fluvaquents-Borosaprists/NL

NL

7320

45

Greenwood-Cathro/L

LL

49010

54

Hogansburg-Grenville(f)/VS/GS

GS

190

71

Lyman-Rock Out/VS/GS

GS

38170

72

Lyman-Rock Out/VS/SL

SL

24590

73

Lyman-Rock Out/VS/MS

MS

107150

77

Lyme-Tughill/VB/NL

NL

650

78

Madalin(f)/NL

NL

30

93

Naumburg/GS

GS

8640

94

Naumburg-Searsport/NL

NL

5610

95

Peru-Pillsbury/B/GS

GS

3160

96

Pillsbury-Lyme/S/GS

GS

66280

97

Pillsbury-Tughill/VB/NL

NL

4560

105

Potsdam/B/MS

MS

16790

107

Potsdam-Crary/VB/GS

GS

29770

108

Potsdam-Crary/S/SL

SL

2040

109

Potsdam-Crary/VB/SL

SL

119560

110

Potsdam-Lyman/B/SL

SL

1160

111

Potsdam-Lyman/B/MS

MS

320

113

Rock Outcrop-Insula/VS/SL

SL

280

117

Rock Outcrop-Lyman/VS/SL

SL

10770

118

Rock Outcrop-Lyman/VS/MS

MS

8440

119

Rock Outcrop-Lyman/VS/ST

ST

31400

120

Rock Outcrop-Lyman/VS/VS

VS

15400

123

Searsport/NL

NL

4590

126

Swanton-Whately/GS

GS

320

130 Mine Dump -- 1200
131 Water -- 44560

The nine parent materials found parkwide are listed below with Oswegatchie/Black (OB) annotations as to what each of them represent in the Oswegatchie/Black watershed:

  1. Organic
  2. Alluvial NONE FOUND IN OB
  3. Lacustrine ONLY ANOMALIES FOUND IN OB (#30, 40,54,78,126 which each represent less than 400 acres (162 ha) using 600 acres(243 ha) as the threshold. Together they represent less than 1000 acres (405 ha).
  4. Glacial outwash
  5. Glacial tills with near neutral pH ONLY ANOMALIES FOUND IN THE OB
  6. Ablation tills
  7. Basal tills
  8. Shallow soil over bedrock
  9. Beach deposit NONE FOUND IN OB

For this study, it was determined that the most meaningful groupings for soils would be by parent material with other considerations as described:

SHALLOW TO BEDROCK SOIL - Rock outcrop dominate
SHALLOW TO BEDROCK SOIL - Shallow soils dominate
BASAL TILLS - Not hydric, Becket/Marlow soil catena
BASAL TILLS - Not hydric, Potsdam soil catena
ABLATION TILLS - Not hydric
GLACIAL TILLS - Not hydric, near neutral pH (Anomalies only)
GLACIAL OUTWASH - Not hydric (high potential for groundwater exchange)
LACUSTRINE - Not hydric (Anomalies only)
HYDRIC SOILS - Soils depth less than 6 in, described as poorly or very poorly drained.

These groupings became the legend for the general soils - parent material map interpretation (see poster graphic attached to this report). Soil depths are interpreted as: deep soils are greater than 60 inches; moderately deep soils are from 20 to 40 inches; and shallow soils are less than 20 inches.

 

References

 


II.J. Elevation With Shaded Relief Map OB2 Contents

 

One of the objectives of this study was to provide existing pertinent coverages for the study area.

 

srelief.jpg (12902 bytes)Description of existing data

Source Data: U.S. Geological Survey Digital Elevation 1:250000 and Adirondack Park Agency

 

This coverage was produced by the Adirondack Park Agency from USGS digital elevation developed from cartographic and photographic sources (U.S. Geological Survey 1990) and shaded relief using standard ArcInfo techniques.

 

References

Continue reading next section of OB2 Report -- Section II.K. OB2 Contents