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1<br />

Table 4 (cont'd)<br />

Map<br />

Symbol+<br />

Name Parent Material Topography Drainage Soils++ ominant Vegetation<br />

Dominant Soil<br />

Zone (deciles)<br />

6S 617 5 4 3 2<br />

si, eLp Glacio- Calcatenus silt and fine Flat to gently Hrunisolic Gray Luvisol<br />

lacustrine sand ; if gravel<br />

3 - 3<br />

and/or Well<br />

- - - wS, wS-tA in Zones<br />

si, sLpv sloping .<br />

Plain sand and/or clay is Orthic Gray Luvisol 2<br />

5 and 6S ;<br />

- - - -<br />

present map symbol<br />

wS-nd, bS-wB-tA In<br />

prefixed by g,<br />

Zone<br />

c ;<br />

6N .<br />

dominant material<br />

Gleyed Gray Luvisol 2 - 2 - - - bS-wB-tA,<br />

Imperfect<br />

bS-Wi-Al<br />

indicated first .<br />

Cryic Gleyed Gray Luvisol - 2 - - _ _ 6` . Zones 5, 6S and<br />

Poor<br />

Rego Gleysol 5 - - - - - bS-Fm-Er, bS-tL-wB<br />

Cryic Rego Gleysol 6 5 - - -<br />

in Zones 5, 6S and<br />

6S .<br />

si, sLpk Glacio- Mainly silt and fine Flat to gently Cryic Eutric Brunisol<br />

lacustrine sand ; discontinuous sloping<br />

w5-wH, bS-Fm-Er in<br />

; numerous Well - 3 - - 3 -<br />

thermo- organic cover . shallow thermo- _ Cryic Eutric Brunisol* Zones 3 and 6N .<br />

karat<br />

karat lakes and<br />

Cryic Gleyed Eutric Brunisol<br />

plain<br />

bS-wB-Er<br />

Imperfect<br />

in Zones<br />

ponds .<br />

Cryic Gleyed Eutric Brunisol* 2 2 3 and 611 .<br />

Poor Cryic Rego Gleysol* - 5 - - 5 - bS-Fm-Er in Zone 6N ;<br />

bS-Lichen-Er in<br />

Zone 3 .<br />

gLpbx Glacio- Mainly sand and/or gravel ; gLpbx and gLpbv, Degraded Eutric Brunisol<br />

lacustrine P, P-wB-tA<br />

gLpbxv<br />

if silt is present map parallel to sub- Well 5<br />

beaches symbol prefixed by si ; parallel beach Orthic Eutric Bruniadl<br />

gLpbv dominant material ridges arranged in Imperfect Gleyed Eutric Brunisol 2 - - - - - P-wB-Wi,<br />

indicated first .<br />

bs-wB-W1,<br />

belts ; up to 6 °<br />

tA-bS-Wi<br />

slopes ;<br />

gLpbv, beach Poor Rego Gleysol 3 - - - - - bS-Fm-Er<br />

material without<br />

distinct ridges<br />

forming belts up<br />

to 4t miles wide .<br />

sEr Aeolian Fine to medium sand . sEr, dune ridges, Well Degraded Eutric Brunisol 15I - L5 I P, to- .B in Zones<br />

SÉh<br />

deposits<br />

usually parallel<br />

I 5 and<br />

to aubparallel<br />

6S .<br />

;<br />

sEh, irregularily<br />

Imperfect Gleyed Degraded Eutric Bruniso'©e 2 - - - to-bS-W1 in Zones<br />

shaped dunes, no 5 and 6S .<br />

apparent pattern .<br />

Rego Gleysol<br />

Pour<br />

3 - 3 - - - bS- Fm, bS- Sphagnum-<br />

Cryic Rego Gleysol<br />

Cr in Zones 5 and 65 .<br />

(g .s .ei)CP Glacio- Gravel and/or sand, sand Flat to gently Degraded Eutric Brunisol P-wB-tA, P in Zones<br />

(g,s,si)Gpv fluvial and silt ; textures vary sloping Well<br />

plain with the dominant Orthic Eutric Brunisol<br />

5 5 6S and 6N .<br />

(g,s,si)Gt<br />

Glaciomaterial<br />

indicated first . Imperfect Gleyed Eutric Brunisol 2 2 - - 1-1 _ bS-wB-Wi, P-wB-Wi,<br />

fluvial<br />

to-bS-Wi in Zones<br />

terrace 6S and 6N .<br />

Poor<br />

Rego Gleysol 3 - - - - - bS-Fm-Er in Zones<br />

Cryic Rego Gleysol - 3 - - - -<br />

6S and 6N .<br />

gGh<br />

gGr<br />

Hummocky<br />

glaclofluvial<br />

deposits<br />

Ridged<br />

glaciofluvial<br />

deposits ;<br />

includes<br />

eskers b<br />

esker<br />

complexes<br />

Mainly gravel and/or<br />

sand .<br />

Hummocks and<br />

ridges to 10m .<br />

Degraded Eutric Brunisol<br />

Well<br />

-<br />

tA-bS-wB<br />

_ _ 5 _ -<br />

Orthlc Eutric Brunisol<br />

wS-tA-wB<br />

. 1 11<br />

Imperfect Gleyed Eutric Brunisol - - - 2 - - bS-tA-wB<br />

Poor Cryic Rego Gleysol - - - 3 -<br />

I<br />

IbS-Fm-Er<br />

bS-Lichen-Er

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