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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