Final Report Phases 1-3 (2002)
Table 12.1: Map Unit Code Key for MnModel v.4.6
Geomorphic Codes
Can be supplemented with USGS Digital Elevation Data layer and its derivative layers (Slope; Relative Elevation; Surface Roughness). Also can be supplemented with MPCA Stream Order layer, although this is a coarser scale than Code No. 10.
Code Number and Title |
GIS Code Symbol |
Map or Code-String Symbol |
Comments |
|
CODE NO. 1 Geomorphic region |
Polygons can be adapted from editing the DNR GIS Minnesota Geomorphology coverage or created by new landform-sediment assemblage mapping for Mn/Model. |
|||
No Distinction Made |
NO_DIST |
* |
||
Glacial Lobe |
GLA_LOB |
L |
||
Glacial Lake Plain |
GLA_LAK |
P |
||
Glaciofluvial Valley |
GLF_VAL |
V |
||
Glacial-Scoured Bedrock Terrain |
GLA_SBRT |
B |
||
Bedrock Terrain |
BRT |
T |
||
CODE NO. 2 Geomorphic region identifier |
This code consists of the geographic or commonly used name for a Geomorphic Region. |
|||
No Distinction Made |
NO_DIST |
* |
||
Glacial Lobe |
||||
Des Moines |
DES |
D |
||
Grantsburg |
GRANT |
G |
||
Koochiching |
KOOCH |
K |
||
Pre-Wisconsinan |
PRE_WI |
P |
||
Rainy |
RAINY |
Y |
||
Red River |
RED |
R |
||
St. Louis |
STL |
S |
||
Superior |
SUPER |
X |
||
Wadena |
WADEN |
W |
||
Glacial Lake Plain |
||||
Lake Agassiz |
LAK_AGA |
LA |
This item excludes the Beltrami Arm of Lake Agassiz. |
|
Lake Agassiz, Beltrami Arm |
LAK_AGAB |
LB |
||
Lake Aitkin |
LAK_AIT |
LI |
||
Lake Duluth |
LAK_DUL |
LD |
||
Lake Upham |
LAK_UPH |
LU |
||
Lake Minnesota |
LAK_MIN |
LM |
||
Lake Benson |
LAK_BEN |
LE |
||
Glaciofluvial Valley |
||||
Glacial River Warren |
RIV_WAR |
VW |
||
St. Croix River Valley |
STC_VAL |
VS |
||
Mississippi River Valley |
MIS_VAL |
VM |
||
St. Louis River Valley |
STL_VAL |
VT |
||
Bedrock Terrain |
||||
Border Lakes Area |
BORDER |
BO |
||
Giants Range |
GIANT |
GI |
||
Mesabi Range |
MESAB |
ME |
||
CODE NO. 3 Geomorphic Sub-region |
Polygons can be adapted from editing the DNR GIS Minnesota Geomorphology coverage or created by new landform-sediment assemblage mapping for Mn/Model. |
|||
No Distinction Made |
NO_DIST |
* |
||
Ground Moraine |
GRO_MOR |
G |
||
End Moraine |
END_MOR |
E |
||
Beach (Level) |
BEA_LEV |
B |
||
Eolian Dune Field |
EOL_FLD |
D |
||
Drumlin Field |
DRU_FLD |
U |
||
Outwash Plain |
OUT_PLA |
O |
||
Paleo-Valley |
PAL_VAL |
Y |
This item can include outwash, collapsed outwash, tunnel valley, glacial lake outlet, etc. cut during glacial activity. |
|
River Valley |
RIV_VAL |
R |
||
CODE NO. 4 Geomorphic Sub-Region identifier |
This code consists of the geographic or commonly used name for a Geomorphic Sub-Region. |
|||
No Distinction Made |
NO_DIST |
* |
||
Moraine |
||||
Alexandria |
ALEX |
AX |
||
Algona |
ALGO |
AG |
||
Altamont |
ALTA |
AL |
||
Ann |
ANN |
AN |
||
Bemis |
BEMI |
BE |
||
Big Stone |
BIGS |
BS |
||
Cloquet |
CLOQ |
CL |
||
Culver |
CULV |
CU |
||
Dent |
DENT |
DE |
||
Erskine |
ERSK |
ER |
||
Frazee |
FRAZ |
FR |
||
Guthrie |
GUTH |
GU |
||
Highland |
HIGH |
HI |
||
Itasca |
ITAS |
IT |
||
Knife |
KNIF |
KI |
||
Mille Lacs |
MILL |
MI |
||
Nashwauk |
NASH |
NA |
||
Nemadji |
NEMA |
NE |
||
Nickerson |
NICK |
NI |
||
Outing |
OUTI |
OU |
||
Pine City |
PINE |
PI |
||
St. Croix |
STCR |
ST |
||
Sugar Hills |
SUGA |
SU |
||
Vermillion |
VERM |
VE |
||
Beach (Level) |
||||
Blanchard |
BLAN |
BL |
||
Campbell |
CAMP |
CA |
||
Emerado |
EMER |
EM |
||
Herman |
HERM |
HE |
||
Hillsboro |
HILL |
HI |
||
Lower Campbell |
LOCA |
LO |
||
McCauleyville |
MCCA |
MC |
||
Norcross |
NORC |
NO |
||
Ojata |
OJAT |
OJ |
||
Tintah |
TINT |
TI |
||
Eolian Dune Field |
||||
Drumlin Field |
||||
Wadena |
WAD_DRU |
WD |
||
Toimi |
TOI_DRU |
TD |
||
Pierz |
PIE_DRU |
PD |
||
Brainerd |
BRA_DRU |
BD |
||
Automba |
AUT_DRU |
AD |
||
Outwash Plain |
||||
Anoka Sand Plain |
ANOKA |
AK |
The Anoka Sand Plain is generally considered an outwash or lake plain (Wright, 1972; Patterson, 1992; Meyer and Patterson, 1997). However, much of the area was subsequently modified by eolian processes forming dunes and possibly sand sheets. |
|
Park Rapids |
PARK_OP |
PR |
||
River Valley |
||||
Blue Earth Valley |
BLU_VAL |
BLU |
||
Rainy River Valley |
RAINY_VAL |
RA |
||
Red River Valley |
RED_VAL |
RE |
||
Root River Valley |
ROOT_VAL |
RO |
||
Rock River Valley |
ROCK_VAL |
RK |
||
St. Croix Valley |
STC_VAL |
CRX |
||
Minnesota Valley |
MINN_VAL |
MN |
The Minnesota Valley is separated from the geomorphically broader Glacial River Warren valley because it contains the bulk of the Holocene-aged sediments |
|
Upper Mississippi Valley - Headwaters Reach |
MISS_HEAD |
UMH |
The headwaters region is typified by a series of lake basins interconnected by ancient outwash channels. |
|
Upper Mississippi Valley - Glacial Lake Aitkin Reach |
MISS_AITKIN |
UMA |
The Mississippi River Valley cross-cuts the relatively flat Glacial Lake Aitkin basin. |
|
Upper Mississippi Valley - Brainerd to St. Cloud Reach |
MISS_BRAIN |
UMB |
The Mississippi River Valley cross-cuts a broad outwash valley train. |
|
Upper Mississippi Valley - St. Cloud to Minnesota Valley Confluence |
MISS_STCLD |
UMS |
||
Upper Mississippi Valley - Glacial River Warren Reach |
MISS_WARREN |
UMW |
||
Upper Mississippi Valley - St. Croix Valley Confluence to Iowa Border |
MISS_STCROIX |
UMC |
||
CODE NO. 5 Landscape |
This code consists of units of landscapes that are composed of one or more related Landforms. |
|||
No Distinction Made |
NO_DIST |
* |
||
Upland, Undifferentiated |
UPL_UNDIFF |
U |
||
Active Ice |
ACT_ICE |
I |
||
Stagnant Ice |
STAG_ICE |
S |
||
Ice Contact |
ICE_CONT |
N |
||
Pediment |
PEDIMENT |
P |
||
Glaciofluvial |
OUTWASH |
O |
||
Catastrophic Flood |
CAT_FLOOD |
C |
Kehew (1982) |
|
Glaciolacustrine |
GLAC_LAC |
A |
||
Paleo-Valley |
PALEO_VAL |
Y |
||
Peatland |
PEAT |
B |
||
Valley Terrace |
VAL_TERR |
V |
||
Floodplain |
FLOOD |
F |
||
Valley Margin |
VAL_MARG |
M |
This item includes depositional forms at the foot of valley margin slopes and relatively steep sideslopes with sharply defined shoulder and footslope. |
|
Eolian |
EOLIAN |
E |
||
Lacustrine |
LAKE |
L |
This item may include River Lake and river Delta landforms. |
|
CODE NO. 6 Landscape geographic or informal identifier |
This code consists of the geographic or commonly used name for a Landscape in a particular Geomorphic Region or Geomorphic Sub-Region. |
|||
No Distinction Made |
NO_DIST |
* |
||
CODE NO. 7 Landform |
This code consists of individual units of Landscape at a landform scale. |
|||
No Distinction Made |
NO_DIST |
* |
||
Alluvial Fan |
FAN |
AF |
The morphologic transition between Alluvial Fan and Colluvial Slope can be gradational. In general, Alluvial Fan includes fan-shaped forms of mappable size. Smaller fans not practical to differentiate at the 1:24,000 scale of mapping, whether alluvial or colluvial, are included in the Colluvial Slope unit. Where multiple Alluvial Fans have coalesced, no attempt is made to differentiated individual fans. |
|
Arterial Drain Patterned Bog (Water Track) |
ART_BOG |
AB |
See Glaser et al. (1981), Wright and Glaser (1983), and Eng (1980). |
|
Bar |
BAR |
B |
This item is usually, but not exclusively, used in conjunction with the Catastrophic Flood Landform. |
|
Beach Ridge, Spit, Cusp, or Shore |
SHORE |
SH |
||
Colluvial Slope |
COLLUV |
C |
The morphologic transition between Alluvial Fan and Colluvial Slope can be gradational. In general, Colluvial Slope includes various forms of slopes dominated by sheetflood depositional processes as well as those dominated by slumps and other slope failures. Smaller fans not practical to differentiate at the 1:24,000 scale of mapping, whether alluvial or colluvial, are included in the Colluvial Slope unit. Areas of Colluvial Slope often are present but are too narrow to be reasonably mapped at a scale of 1:24,000. |
|
Compaction Ridge |
COMP_RIDG |
CR |
Defined in the Glacial Lake Agassiz Geomorphic Region by Bluemle (1967). |
|
Crevasse Splay |
SPLAY |
CS |
This item includes crevasse channels, splay channels, and splay overbank belts. |
|
Delta |
DELTA |
DE |
This item does not differentiate between different types of deltas. It includes deltas formed in lakes; fan deltas, where a river enters a riverine lake; and, deltas deposited where a river enters a larger river valley. |
|
Depression |
DEPR |
D |
As used in the code, Depression is a general descriptive term for a relatively small topographic basin. It usually is used in conjunction with glacial Landscapes. The item may include Linked Depressions or Interdunal Depressions where they are not differentiated. Some Depressions may be old abandoned quarries which are indistinguishable as to their origin without a historic landuse record search. |
|
Disintegration Ridge |
DIS_RIDGE |
DS |
Defined by the DNR for their (1:100k) geomorphology maps. |
|
Disturbed Areas |
DISTURB |
DI |
This item primarily consists of quarries and pits, but can include vast construction sites and sewage treatment reservoirs. |
|
Doughnut |
DOUGH |
DO |
||
Drainageway |
DRAIN |
DA |
This item consists of low-order valleys that have a shallow "u" shape and ill-defined floodplain. They are typical of low-order upland valleys. |
|
Drumlin |
DRUMLIN |
DR |
||
Dune |
DUNE |
ED |
||
Erosional Residual |
RESIDUAL |
ER |
This item is used in conjunction with Catastrophic Flood or, less frequently, Outwash Landscapes. |
|
Erosional Strath |
STRATH |
ST |
This item is usually used in conjunction with Catastrophic Flood or Outwash Landscapes. |
|
Escarpment Complex |
ESCARP_C |
EC |
This item is used in areas where the major landform is an escarpment with the Glaciolacustrine landscape and includes smaller Terrace and possibly Beach Ridge landforms which are not readily apparent at the 1:24,000 scale |
|
Esker |
ESKER |
EK |
||
Floodplain, Undifferentiated |
FLOOD |
F |
This item is mapped in lower order valleys where individual Floodplain types are not large enough, or distinct enough, to map at a scale of 1:24,000. Marshes and lakes on Floodplains are considered subdivisions of Floodplains and usually are not distinguished individually because many are seasonal and subject to large seasonal fluctuations in water depth and size. Individual sloughs on Floodplains are not distinguished unless they are of considerable length and mapped as a Paleochannel. Otherwise, they are considered part of the lateral accretion Floodplain morphology. |
|
Floodplain, Type "w" |
FL_W |
FW |
Type "w" Floodplains have point bars or other channel migration features evident and recently active based on the lack, paucity, or type of vegetation. It often is associated with comparatively sparse or no vegetation; typically occurs between a marked discontinuity with other Floodplain types and the active river channel; and, lacking the aforementioned, may be an arbitrary distinction between Type "w" and Type "x" Floodplain types. |
|
Floodplain, Type "x" |
FL_X |
FX |
Type "x" Floodplains have point bars or other channel migration features evident, but they have not been recently active. |
|
Floodplain, Type "y" |
FL_Y |
FY |
Point bars or other channel migration features not evident on Type "y" Floodplains, either due to burial by younger overbank deposits, or they were never present. |
|
Floodplain, Type "z" |
FL_Z |
FZ |
Type "z" Floodplains do not have evident point bars or other channel migration features; usually are surrounded or partially surrounded by Valley Terrace or Catastrophic Flood Landscapes; and/or are outside of, or otherwise isolated from, obvious former channel and/or overbank belts. |
|
Floodplain and Terraces, Undifferentiated |
FLO&TERR |
FN |
This item is mapped in lower order valleys wide enough to have Floodplains and Terraces, but where individual terrace areas are not large enough, or distinct enough from Floodplain areas, to map at a scale of 1:24,000. |
|
Hillslope |
HILL |
H |
This item refers only to relatively steep and high 1) valley walls along higher order valleys with floodplains; 2) uplandhillslopes; and, 3) upland or valley slopes in bedrock terrains. It primarily consists of backslope hillslope components (sensu Ruhe, 1969). The upper limit usually is mapped where contour lines become more widely spaced, generally representing the position of the shoulder slope. |
|
Hummock |
HUMMOCK |
HU |
As used in the code, Hummock is a general descriptive term for a relatively small topographic rise. It usually is used in conjunction with glacial Landscapes. The item may include Doughnuts and Ice-Walled Lake Beds where they are not differentiated. |
|
Ice-Block Kame Terrace |
ICEBK_KAME |
IK |
Ring-shaped kame terrace formed in glaciolacustrine waters that surround stagnant glacial ice blocks (Hudak and Hajic, in preparation). |
|
Ice-Walled Lake Bed |
ICE_WALLED |
IW |
This item is mapped in conjunction with the Stagnant Ice Landscape. It is used for circular Hummocks where associated stratified fine-textured deposits >2m thick are interpreted as lake sediments. |
|
Ice-Walled Lake Beach Ridge |
ICE_WAL_BR |
IB |
This item is mapped in conjunction with the Stagnant Ice Landscape. It consists of narrow, arcuate, ridges that rise above surrounding Stagnant Ice LsSA terrain. It often is associated with, but not necessarily adjacent to, Hummocks mapped as Ice-Walled Lake Beds |
|
Interdunal Depression or Pond |
POND |
DP |
This item refers to a Depression that is interpreted to have been formed wholly or in part by eolian processes. It typically, but not necessarily, is at least partially surrounded by Eolian Dunes. Such a depression may seasonally or perennially contain a relatively small water body. |
|
Island |
ISLAND |
I |
If other Landform assignments are deemed more significant than the Island-lake or Island-river relationship, Island is not used. Islands may have complicated stratigraphy, but were not field tested during the Mn/Model project. |
|
Isthmus |
ISTHMUS |
IT |
||
Kame |
KAME |
K |
||
Kame Terrace |
KAMET |
KT |
||
Lake |
LAKE |
LN |
||
Lake Bed, Exposed |
LAKEBED |
LB |
Exposure may be naturally or artificially caused. This item is generally used for lake basins of intermediate size, not relatively small Depressions or Linked Depressions that may have at one time supported small lakes or ponds, or relatively large lake Plains. |
|
Linked Depression(s) |
DEPR_LINK |
LD |
Kemmis (1991). This unit is mapped in conjunction with the Stagnant Ice Landscape only where Depressions and Depression linkages are visible on air photos. Many areas mapped as Depressions may fall within this unit genetically, but either the linkage between individual Depressions was unclear, or Depressions were too small to map at the scale of 1:24,000. |
|
Marginal Channel |
MARG_CHAN |
MC |
This item is usually used in conjunction with Catastrophic Flood LsSA. |
|
Meander Belt |
MEANDER |
MB |
This item is mapped in conjunction with lower or intermediate order streams in their valleys, and where they cross Floodplains or Terraces in valleys of higher order streams. |
|
Natural Levee |
LEVEE |
NL |
Natural Levees form a continuum with lower, broader, more subtle rises of overbank deposits that are mapped as part of Floodplain Types "y" and "z" in some valleys. |
|
Outwash Fan, Apron |
OUT_FAN |
OF |
||
Overbank Belt |
OVERBANK |
OB |
Overbank Belt is used in conjunction with relatively lower order streams where they cross Floodplains or Terraces in valleys of higher order streams. |
|
Ovoid-Shaped Bog (Ovoid Island) |
OVOID_BOG |
OV |
See Heinselman (1963, 1970), Glaser et al. (1981), Wright and Glaser (1983), Minnesota Dept. of Natural Resources (1984), and Eng (1980). |
|
Paleochannel |
PALEO_C |
PC |
This item includes distributary paleochannels on abandoned delta lobes. |
|
Pediment Slope |
PEDIMENT |
PD |
This item may look similar to Alluvial Fans or Colluvial Slopes on topographic maps. |
|
Peninsula |
PENIN |
PE |
||
Plain |
PLAIN |
P |
This item usually is used in conjunction with, but is not limited to, Outwash, Glaciolacustrine, and glacial ice Landscapes. Exposed Lake Bed is used for exposed lake or glacial lake basins of intermediate or smaller size. |
|
Raised (Radial) Bog |
RAD_BOG |
RB |
See Heinselman (1963, 1970), Glaser et al. (1981), Wright and Glaser (1983), Minnesota Dept. of Natural Resources (1984), and Eng (1980). |
|
Rapids, Nickpoint, Cascade, or Falls |
RAPIDS |
RP |
||
Ribbed Fen |
RIB_FEN |
RF |
See Heinselman (1963; 1970), Glaser et al. (1981), Wright and Glaser (1983), and Eng (1980). |
|
River Channel, Active |
RIVER |
R |
||
Riverine Lake |
RIV_LAKE |
RL |
||
Rock Basin |
ROCK_BAS |
RS |
This item is used in Bedrock Terrains. |
|
Rock Drumlins (Whale-backs) |
ROCK_DRU |
RD |
This item is used in Bedrock Terrains. |
|
Rogen Moraine |
ROG_MOR |
RM |
||
Rouche Moutonnee |
ROUCHE |
RH |
This item is used in Bedrock Terrains. |
|
Sand Sheet |
SHEET |
ES |
||
Standing Water, Reservoir |
RESERVOIR |
LR |
||
Summit |
SUMMIT |
S |
See Ruhe (1969). In the code, this unit is applied to Bedrock Terrains and erosional terrains only and primarily consists of summit slopes. |
|
Terrace |
TERRACE |
T |
||
Terrace, High, Undifferentiated |
H_TERRACE |
HT |
This item is mapped where multiple high terraces, or high and low terraces, are present, but reasonably can not be differentiated at the 1:24,000 scale of mapping. |
|
"v"-Shaped Valley |
V_VALLEY |
V |
This item consists of low-order valleys that have a "v" shape; little or no floodplain area; and, generally steep valley walls. Such valleys are often incised into the surrounding landscape, and may consist of the channel itself. |
|
Wave-Cut Platform |
WAVE_CUT |
WC |
||
CODE NO. 8 Landform GEOGRAPHIC OR INFORMAL identifier |
This code consists of geographic or commonly used name for a Landform. It is to be added as needed. |
|||
No Distinction Made |
NO_DIST |
* |
||
CODE NO. 9 Landform Subdivision |
This code is provided for future use. |
|||
No Distinction made |
NO_DIST |
* |
||
CODE NO. 10 Stream Valley Order |
Streams are ordered using the Strahler method (Strahler, 1964) |
|||
Not Relevant or No Distinction Made |
NO_DIST |
* |
||
1 |
1 |
1 |
||
2 |
2 |
2 |
||
3 |
3 |
3 |
||
Etc. |
Etc. |
Etc. |
||
CODE NO. 11 Surface Characteristics and Modifications |
This code consists surface characteristics and modifications within a Landform or Landscape that are penecontemporaneous with, or post-date the development of the Landform or Landscape. |
|||
Not Present or No Distinction Made |
NO_DIST |
* |
||
Boulder or Cobble Lag |
BOULDER |
R |
||
Braided Channel Pattern |
BRAID |
B |
||
Braided Channel Pattern with Shallow, Natural Standing Water |
BRAID_MARSH |
BM |
||
Dendritic Channel Pattern |
DENDR |
DD |
||
Meandering Channel Pattern |
MEANDER |
S |
||
Flood Scour Channel Pattern |
FL_SCOUR |
F |
||
Distributary Pattern |
DISTRIB |
D |
||
Pitted |
PITTED |
P |
||
Wave or Current Modified, Subaerial |
WAVE_AERIAL |
WA |
||
Wave or Current Modified, Submerged |
WAVE_SUBMERGE |
WS |
This code usually refers to submerged Islands or Wave-Cut Platforms. |
|
Water Modified |
WATER_MOD |
T |
||
Wind Modified |
WIND_MOD |
N |
||
Linear, Reticulated, or Orbicular Patterns |
RIP_ICE |
I |
Pertains to patterns recognized on the Glacial Lake Agassiz plain. See Mollard (1983). |
|
Standing Water, Natural, Shallow |
MARSH |
MA |
This item is used for areas with intermittent or permanent shallow water usually marked with a marsh symbol on USGS topographic maps. Larger areas are often mapped as Peatlands. This item is differentiated from Standing Water, Natural (lakes) by having relatively shallow water and subaerial vegetation. |
|
CODE NO. 12 Collapsed landscape or landform |
This code refers to a Landform or Landscape that had a core of glacial ice that subsequently melted and "let down" the overlying material. |
|||
No Distinction Made |
NO_DIST |
* |
||
Not Collapsed |
NO_COLL |
N |
||
Collapsed |
COLLAPSE |
C |
||
CODE NO. 13 eroded landscape or landform |
This code refers primarily to soil erosion that post-dates landform or landscape development. |
|||
Not Present or No Distinction Made |
NO_DIST |
* |
||
Eroded |
ERODED |
E |
This unit is used for areas of mappable size at a scale of 1:24,000 that show field, air photo, or soil mapping evidence of being eroded. The unit may include relatively steep Hillslopes. |
|
Erosion Complex |
EROSION_C |
EC |
This unit is used for areas characterized by either intricately interfingered, or very small discontinuous areas, of eroded and non-eroded areas that individually are of unmappable size at a scale of 1:24,000, based on field, air photo, or soil mapping evidence. |
|
Iowan Erosion Surface |
IOWAN |
O |
See Hallberg et al. (1978). Soil erosion that formed the Iowan Erosion Surface formed a Landscape of one or more erosional "steps" on interfluves in specific parts of the state. |
Material and Material Sequence Codes
Code |
Item |
GIS Code Symbol |
Map or Code-String Symbol |
Comments |
CODE NO. 14 Post-glacial lithostratigraphic unit |
This code is to be used when sufficient information is available to informally or formally name post-glacial fluvial, lacustrine, peatland, and eolian formations. |
|||
No Distinction Made |
NO_DIST |
* |
||
CODE NO. 15 texture and texture sequence of NEar-surface material |
This code only applies to the upper 2 m of material, including any Overlying Deposits. Two systems are represented, a general one that differentiates by fine, coarse and peat/organic muck textures, and a more specific one that differentiates by USDA NRCS soil textures. Only one of these systems can be used for each Landform or Landscape, depending on the amount and reliability of subsurface information available. |
|||
General |
Variable at this Scale, or No Distinction Made |
NO_DIST |
* |
|
Peat or Organic Muck |
P |
P |
||
Fine |
F |
F |
This unit includes silt and finer material. It may include loam and clay loam, depending on the region being mapped. |
|
Thinly Bedded Fines |
Y |
Y |
||
Fine over Peat |
F/P |
FP |
||
Coarse |
CO |
CO |
This unit includes sandy loam and coarser material. It may include loam and clay loam, depending on the region being mapped. |
|
Peat or Organic Muck over Fine |
P/F |
PF |
||
Peat or Organic Muck over Coarse |
P/CO |
PC |
||
Peat or Organic Muck over Interstratified Coarse and Fine |
P/INTR_C&F |
PQ |
||
Interstratified Peat or Organic Muck and Fines |
INTR_P&F |
IPF |
||
Discontinuous Peat or Organic Muck over Fine |
DIS_P/F |
PFN |
||
Discontinuous Peat or Organic Muck over Coarse |
DIS_P/CO |
PCR |
||
Fine over Coarse |
F/CO |
FC |
||
Fine over Interstratified Coarse and Fine |
F/INTR_C&F |
FQ |
||
Coarse over Fine |
CO/F |
CF |
||
USDA NRCS |
Clay |
CY |
CY |
|
Silty Clay |
SICY |
SIC |
||
Silty Clay Loam |
SICYL |
SICL |
||
Silt Loam |
SIL |
SIL |
||
Silt |
SI |
SI |
||
Loam |
L |
L |
||
Clay Loam |
CYL |
CL |
||
Sandy Clay Loam |
SACYL |
SCL |
||
Sandy Loam |
SAL |
SL |
||
Loamy Sand |
LSA |
LS |
||
Sand |
SA |
S |
||
Gravel |
G |
G |
||
Cobble |
COB |
B |
||
Peat or Organic Muck over Clay to Silt Loam |
P/CY-SIL |
P/C-SIL |
||
Peat or Organic Muck over Silty Clay |
P/SICY |
P/SIC |
||
Peat or Organic Muck over Silty Clay and Sandy Gravel |
P/SICY& SAG |
P/SIC&SG |
||
Peat or Organic Muck over Silty Clay Loam over Clay Loam |
P/SICYL/CYL |
P/SICL/CL |
||
Peat or Organic Muck over Silt Loam over Loam |
P/SIL/L |
P/SIL/L |
||
Peat or Organic Muck over Silt Loam over Loam to Sandy Loam |
P/SIL/L-SAL |
P/SIL/L-SL |
||
Peat or Organic Muck over Loam |
P/L |
P/L |
||
Peat or Organic Muck over Silt Loam over Sandy Loam to Sand |
P/SIL/SAL-SA |
P/SIL/SL-S |
||
Peat or Organic Muck over Silt over Sandy Loam |
P/SI/SAL |
P/SI/SL |
||
Peat or Organic Muck over Sandy Loam |
P/SAL |
P/SL |
||
Peat or Organic Muck over Sandy Loam to Clay Loam |
P/SAL-CYL |
P/SL-CL |
||
Peat or Organic Muck over Loamy Sand over Loam |
P/LSA/L |
P/LS/L |
||
Peat or Organic Muck over Loamy Sand |
P/LSA |
P/LS |
||
Peat or Organic Muck over Loamy Sand to Sand |
P/LSA-SA |
P/LS-S |
||
Peat or Organic Muck over Sand to Sandy Loam |
P/SA-SAL |
P/S-SL |
||
Peat or Organic Muck over Sand over Loam to Clay Loam |
P/SA/L-CYL |
P/S/L-CL |
||
Peat or Organic Muck over Sand |
P/SA |
P/S |
||
Peat or Organic Muck over Sandy Gravel |
P/SAG |
P/SG |
||
Interstratified Peat or Organic Muck and Sand |
INTR_P&SA |
IPS |
||
Clay over Loam to Clay Loam |
CY/L-CYL |
C/L-CL |
||
Clay to Sandy Loam over Loam to Clay Loam |
CY-SAL/L-CYL |
C-SL/L-CL |
||
Silty Clay to Coarse |
SICY-CO |
SIC-C |
||
Silty Clay and Sandy Gravel |
SICY&SAG |
SIC&SG |
||
Silty Clay Loam over Clay Loam |
SICYL/CYL |
SICL/CL |
||
Silty Clay Loam over Clay Loam to Loam |
SICYL/CYL-L |
SICL/CL-L |
||
Silt Loam to Silty Clay Loam |
SIL-SICYL |
SIL-SICL |
||
Silt Loam to Silty Clay Loam over Clay Loam |
SIL-SICYL/CYL |
SIL-SICL/CL |
||
Silt Loam to Loam |
SIL-L |
SIL-L |
||
Silt Loam over Loam |
SIL/L |
SIL/L |
||
Silt Loam over Loam to Sandy Loam |
SIL/L-SAL |
SIL/L-SL |
||
Silt Loam over Loam to Loamy Sand over Sand |
SIL/L-LSA/SA |
SIL/L-LS/S |
||
Silt Loam over Sandy Loam over Sandy Gravel |
SIL/SAL/SAG |
SIL/SL/SG |
||
Silt Loam over Sandy Loam to Sand |
SIL/SAL-S |
SIL/SL-S |
||
Silt Loam over Sand |
SIL/SA |
SIL/S |
||
Loam to Clay Loam |
L-CYL |
L-CL |
||
Loam to Silt Loam over Sand |
L-SIL/SA |
L-SIL/S |
||
Loam to Sandy Loam |
L-SAL |
L-SL |
||
Loam to Sand |
L-SA |
L-S |
||
Loam over Clay Loam to Loam |
L/CYL-L |
L/CL-L |
||
Loam over Sand |
L/SA |
L/S |
||
Loamy Sand over Loam |
LSA/L |
LS/L |
||
Sandy Loam over Sandy Clay Loam |
SAL/SACYL |
SL/SCL |
||
Sandy Loam to Clay Loam |
SAL-CYL |
SL-CL |
||
Sandy Loam over Gravel |
SAL/G |
SL/G |
||
Loamy Sand to Sand |
LSA-SA |
LS-S |
||
Loamy Sand over Gravelly Sand |
LSA/GSA |
LS/GS |
||
> Sand to Sandy Loam |
SA-SAL |
S-SL |
||
Sand to Sandy Loam over Clay Loam |
SA-SAL/CYL |
S-SL/CL |
||
Sand to Sandy Loam over Loam to Clay Loam |
SA-SAL/L-CYL |
S-SL/L-CL |
||
Sand over Sandy Clay Loam |
SA/SACYL |
S/SCL |
||
Sand and Gravel |
SA&G |
S&G |
||
Sandy Gravel |
SAG |
SG |
||
Etc. |
Etc. |
Etc. |
Texture sequences can be added as necessary, separating the two texture map symbols by a backslash. |
|
CODE NO. 16 Diamicton texture |
This code applies to uppermost lithologic unit(s). |
|||
No Distinction Made |
NO_DIST |
* |
||
Diamicton Texture Not Present or Uncommon |
NO_DIA |
O |
||
Diamicton Texture |
DIA |
D |
||
CODE NO. 17 thickness of NEAR-SURFACE material over bedrock or glacial drift |
Use this code includes any thickness of material of Overlying Deposits in Code No. 18 in addition to the remaining underlying unconsolidated mostly non-glacial Quaternary materials. Thicknesses for some Valley Margin LsSA units consider the thickest part of these wedge-shaped landforms. |
|||
No Distinction Made |
NO_DIST |
* |
||
Not Present or <1m Thick, Laterally Discontinuous |
ZERO |
>< |
||
>2m Thick, Laterally Continuous |
>2M |
>> |
||
<2m Thick, Laterally Continuous |
<2M |
<< |
||
<2m, >1m Thick, Laterally Continuous |
<2>1M |
<> |
||
>1m Thick, Laterally Continuous |
>1M |
> |
||
<1m Thick, Laterally Continuous |
<1M |
< |
||
CODE NO. 18 overlying deposits |
"Overlying" refers to material usually <2m thick that was deposited on a Landform or Landscape sometime after the principal landform- or landscape-sediment assemblage developed. Units under this code are applicable to any Landform or Landscape. |
|||
Not Present |
NO_PRES |
N |
||
No Distinction Made |
NO_DIST |
* |
||
Type "o" Overbank Deposits |
OVERO |
O |
This unit is used where relatively very light tonal contrasts on aerial photography of valley areas are interpreted as overbank deposits that are likely to include, or field evidence indicates, deposition of significant post-settlement alluvium. Here "significant" means a sufficient thickness to obscure prehistoric cultural deposits. In plowed areas this typically means >0.27 m thick. In unplowed areas, it may be thinner. If not otherwise noted, presence is implied with Floodplain Type "w". |
|
Type "a" Overbank Deposits |
OVERA |
A |
This unit is used where relatively light tonal contrasts on aerial photography of valley areas are interpreted as overbank deposits. They may or may not include significant post-settlement alluvium. |
|
Sheetflood Deposits, Undifferentiated |
SHEET |
S |
||
Hillslope Colluvium; Biomantle |
HILL_COLLUV |
H |
This unit is usually applied to upland landscapes. It includes the range of recognizable products from the combination of upland hillslope erosional, depositional, and soil evolution processes. See Johnson (1990). |
|
Loess |
LOESS |
L |
||
Glaciolacustrine |
GLA_LK |
GL |
Thick (>2m) Glaciolacustrine sediment mantles may occur in some Outwash or other depressional settings, and could have been interpreted as a Glaciolacustrine Plain, except for the dominant geologic process that shaped the landform. |
|
Outwash |
OUTWASH |
OU |
Thick (>2m) Outwash mantles may occur in some Glaciolacustrine or other depressional settings, and could have been interpreted as an Outwash Plain, except for the dominant geologic process that shaped the landform. |
|
CODE NO. 19 buried soils |
Documented or interpreted Buried Soil(s) are present, including consideration of Overlying Deposits. As used here, Buried Soil definition may include thick cumulic soils. The definition of Buried Soil does not have the depth limitations imposed by the USDA NRCS definition of Buried Soil. |
|||
No Distinction Made |
NO_DIST |
* |
||
Buried Soil(s) Not Present or Uncommon |
NO_BUR_SOL |
O |
||
Buried Soil(s) Commonly Present |
BUR_SOL |
B |
||
CODE NO. 20 basement material |
||||
Not Exposed Within 2m of Ground Surface, or No Distinction Made |
NO_DIST |
* |
||
Bedrock, Undifferentiated |
BEDROCK |
B |
||
Thin Glacial Drift over Bedrock |
DRIFT_BED |
GB |
||
Bedrock or Glacial Drift, Undifferentiated |
BEDR_GLAC |
K |
||
Bedrock, Igneous |
IGNEOUS |
IG |
||
Bedrock, Metamorphic |
METAM |
M |
||
Bedrock, Sedimentary |
SEDIM |
S |
||
Bedrock, Carbonate |
CARBONATE |
SC |
||
Glacial Drift, Undifferentiated |
GLACIAL |
G |
||
Glaciolacustrine Deposits |
GLA_LAKE |
L |
||
Glaciofluvial Deposits |
OUTWASH |
O |
||
Till |
TILL |
T |
||
Thin Glaciofluvial over Glacial Drift or Bedrock |
OUT_DRIFT |
OK |
||
CODE NO. 21 basement material identifier |
This code consists of the lithology or lithostratigraphic name of the material underlying the material of interest. It is to be developed as needed. |
|||
No Distinction Made |
NO_DIST |
* |
||
Sherack Formation |
SHERACK |
S |
||
Sherack and Poplar River Formations |
SHERACK_POPLAR |
SP |
||
Duluth Complex |
DULUTH |
DC |
||
Ely Greenstone |
ELY_GRE |
EG |
||
Banded Iron Fm. |
IRON |
FE |
||
Giants Range Granite |
GIANTS |
GI |
||
North Shore Volcanic Group |
NS_VOLCAN |
NS |
||
Rove Fm. |
ROVE |
RO |
||
Saganaga Granite |
SAGANAGA |
SG |
||
Trommald Fm. |
TROMMALD |
TR |
||
Vermillion Granite |
VERMILLION |
VG |
Temporal Codes
Code |
Item |
GIS Code Symbol |
Map or Code- String Symbol |
Comments |
CODE NO. 22 STAGE or substage of landform-Sediment assemblage |
This code consists of the primary stage or substage of a Landform. It ignores minor younger surface modifications. See text regarding stage definitions. Additional temporal sequences can be added as necessary, separating the two stage or substage symbols by a hyphen. |
|||
No Distinction Made |
NO_DIST |
* |
||
Pre-Wisconsinan |
PRE_WISC |
P |
||
Wisconsinan, Undifferentiated |
WISC |
W |
||
Late Wisconsinan |
L_WISC |
LW |
||
Late Wisconsinan to Holocene |
L_WISC-HOL |
LW-H |
||
Late Wisconsinan to Early Holocene |
L_WISC-E_HOL |
LW-E |
||
Late Wisconsinan to Historic |
L_WISC-HIST |
LW-S |
||
Holocene, Undifferentiated |
HOL_UNDIFF |
U |
This code may or may not include all the substages of the Holocene. |
|
Holocene |
HOL |
H |
This code includes the Historic substage. |
|
Early Holocene |
E_HOL |
E |
||
Early to Middle Holocene |
E_HOL-M_HOL |
E-M |
||
Early to Late Holocene |
E_HOL-L_HOL |
E-L |
||
Early Holocene to Historic |
E-HOL-HIST |
E-S |
||
Middle Holocene |
M_HOL |
M |
||
Middle to Late Holocene |
M_HOL-L_HOL |
M-L |
||
Middle Holocene to Historic |
M_HOL-HIST |
M-S |
||
Late Holocene |
L_HOL |
L |
||
Late Holocene to Historic |
L_HOL-HIST |
L-S |
||
Historic |
HIST |
S |
||
CODE NO. 23 STAGE of overlying deposits |
This code consists of the stage of deposition of Overlying Deposits of Code No. 18. See text regarding stage definitions. Additional temporal sequences can be added as necessary, separating the two stage or substage symbols by a hyphen. |
|||
Not Relevant or No Distinction Made |
NO_DIST |
* |
||
Pre-Wisconsinan |
PRE_WISC |
P |
||
Wisconsinan, Undifferentiated |
WISC |
W |
||
Late Wisconsinan |
L_WISC |
LW |
||
Late Wisconsinan to Holocene |
L_WISC-HOL |
LW-H |
||
Late Wisconsinan to Early Holocene |
L_WISC-E_HOL |
LW-E |
||
Late Wisconsinan to Historic |
L_WISC-HIST |
LW-S |
||
Holocene, Undifferentiated |
HOL_UNDIFF |
U |
This code may or may not include all the substages of the Holocene. |
|
Holocene |
HOL |
H |
This code includes the Historic substage. |
|
Early Holocene |
E_HOL |
E |
||
Early to Middle Holocene |
E_HOL-M_HOL |
E-M |
||
Early to Late Holocene |
E_HOL-L_HOL |
E-L |
||
Early Holocene to Historic |
E-HOL-HIST |
E-S |
||
Middle Holocene |
M_HOL |
M |
||
Middle to Late Holocene |
M_HOL-L_HOL |
M-L |
||
Middle Holocene to Historic |
M_HOL-HIST |
M-S |
||
Late Holocene |
L_HOL |
L |
||
Late Holocene to Historic |
L_HOL-HIST |
L-S |
||
Historic |
HIST |
S |
||
CODE NO. 24 GLACIAL LAKE OR GLACIAL ICE PHASE |
This code consists of recognized glacial ice and lake phases for the stratigraphically highest basement material |
|||
No Distinction Made |
NO_DIST |
* |
||
Glacial Lake Phase |
||||
Cass |
CASS |
CS |
||
Emerson |
EMER |
EM |
||
Lockhart |
LOCK |
LO |
||
Moorhead |
MOOR |
MO |
||
Nipigon |
NIPI |
NI |
||
Glacial Ice Phase |
||||
Automba |
AUTO |
AU |
||
Culver |
CULV |
CU |
||
Duluth |
DULU |
DU |
||
Hewitt |
HEWI |
HE |
||
Itasca |
ITAS |
IT |
||
Nickerson |
NICK |
NI |
||
Pine City |
PINE |
PI |
||
Split Rock |
SPLI |
SP |
||
St. Croix |
STCR |
ST |
||
CODE NO. 25 RELATIVE AGE OF GEOMORPHIC UNIT WITHIN A LANDFORM (CODE 7) |
Most commonly refers to Terraces or Wave-Cut Platforms. A Paleochannel’s relative age refers to its associated Terrace’s relative age and not to the cross-cutting relations among these channels. |
|||
No Distinction Made |
NO_DIST |
* |
||
Youngest |
YOUNG |
1 |
||
Next to Youngest |
YOUNG+1 |
2 |
||
Second Next to Youngest |
YOUNG+2 |
3 |
||
Third Next to Youngest |
YOUNG+3 |
4 |
||
Fourth Next to Youngest |
YOUNG+4 |
5 |
||
Etc. |
Etc. |
Etc. |
||
CODE NO. 26 RELATIVE AGE OF GEOMORPHIC UNIT WITHIN A LANDFORM SUBDIVISION (CODE 9) |
||||
No Distinction Made |
NO_DIST |
* |
||
Youngest |
YOUNG |
1 |
||
Next to Youngest |
YOUNG+1 |
2 |
||
Second Next to Youngest |
YOUNG+2 |
3 |
||
Third Next to Youngest |
YOUNG+3 |
4 |
||
Fourth Next to Youngest |
YOUNG+4 |
5 |
||
Etc. |
Etc. |
Etc. |
||
CODE NO. 27 RELATIVE AGE OF LANDFORM-SEDIMENT ASSEMBLAGE TO OTHER LANDSCAPE- OR LANDFORM-SEDIMENT ASSEMBLAGES |
||||
No Distinction Made |
NO_DIST |
* |
||
Overlying, Crosscutting or Interfingering with Active Ice LsSA |
A_ACT_ICE |
I |
||
Overlying, Crosscutting or Interfingering with Stagnant Ice LsSA |
A_STAG_ICE |
S |
||
Overlying, Crosscutting or Interfingering with Ice Contact LsSA |
A_ICE_CONT |
N |
||
Overlying, Crosscutting or Interfingering with Pediment LsSA |
A_PEDIMENT |
P |
||
Overlying, Crosscutting or Interfingering with Glaciofluvial LsSA |
A_OUTWASH |
O |
||
Overlying, Crosscutting or Interfingering with Catastrophic Flood LsSA |
A_CAT_FLOOD |
C |
||
Overlying, Crosscutting or Interfingering with Glaciolacustrine LsSA |
A_GLAC_LAC |
A |
||
Overlying, Crosscutting or Interfingering with Paleo-Valley LsSA |
A_PALEO_VAL |
Y |
||
Overlying, Crosscutting or Interfingering with Peatland LsSA |
A_PEAT |
B |
||
Overlying, Crosscutting or Interfingering with Valley Terrace LsSA |
A_VAL_TERR |
V |
||
Overlying, Crosscutting or Interfingering with Floodplain LsSA |
A_FLOOD |
F |
||
Overlying, Crosscutting or Interfingering with Valley Margin LsSA |
A_VAL_MARG |
M |
||
Overlying, Crosscutting or Interfingering with Eolian LsSA |
A_EOLIAN |
E |
||
Overlying, Crosscutting or Interfingering with Lacustrine LsSA |
A_LAKE |
L |
||
Overlying, Crosscutting or Interfingering with [LfSA as necessary] |
Etc. |
Etc. |
||
CODE NO. 28 geochronology OF Lfsa: Less than or equal to |
This code consists of a number interpreted from one or more radiocarbon ages, in uncorrected radiocarbon years before present, for a Landform-Sediment Assemblage. The code will continue to be developed and refined as more radiocarbon ages become available. The Map Code has dropped the "ten’s" off the years to abbreviate for mapping. |
|||
No Distinction Made |
NO_DIST |
* |
||
12,000 B.P. |
12000 |
1200 |
||
CODE NO. 29 geochronology of LfsA: greater than or equal to |
This code consists of a number interpreted from one or more radiocarbon ages, in uncorrected radiocarbon years before present, for a Landform-Sediment Assemblage. The code will continue to be developed and refined as more radiocarbon ages become available. The Map Code has dropped the "ten’s" off the years to abbreviate for mapping. |
|||
No Distinction Made |
NO_DIST |
* |
||
Present |
0 |
0 |
||
CODE NO. 30 geochronology OF OVERLYING DEPOSITS: Less than or equal to |
This code consists of a number interpreted from one or more radiocarbon ages, in uncorrected radiocarbon years before present, for Overlying Deposits. The code will continue to be developed and refined as more radiocarbon ages become available. The Map Code has dropped the "ten’s" off the years to abbreviate for mapping. |
|||
No Distinction Made |
NO_DIST |
* |
||
12,000 |
12000 |
1200 |
||
CODE NO. 31 geochronology of OVERLYING DEPOSITS greater than or equal to |
This code consists of a number interpreted from one or more radiocarbon ages, in uncorrected radiocarbon years before present, for Overlying Deposits. The code will continue to be developed and refined as more radiocarbon ages become available. The Map Code has dropped the "ten’s" off the years to abbreviate for mapping. |
|||
No Distinction Made |
NO_DIST |
* |
||
Present |
0 |
0 |
||
CODE NO. 32 geochronology of BASEMENT MATERIAL: Less than or equal to |
This code consists of a number interpreted from one or more radiocarbon ages, in uncorrected radiocarbon years before present, for Basement Material. The code will continue to be developed and refined as more radiocarbon ages become available. Basement Material may have the same Geochronology as the LfSA Geochronology if the Basement Material is part of the LfSA. The Map Code has dropped the "ten’s" off the years to abbreviate for mapping. |
|||
No Distinction Made |
NO_DIST |
* |
||
CODE NO. 33 geochronology of BASEMENT MATERIAL: greater than or equal to |
This code consists of a number interpreted from one or more radiocarbon ages, in uncorrected radiocarbon years before present, for Basement Material. The code will continue to be developed and refined as more radiocarbon ages become available. The Basement Material may have the same Geochronology as the LfSA Geochronology if the Basement Material is part of the LfSA. The Map Code has dropped the "ten’s" off the years to abbreviate for mapping. |
|||
No Distinction Made |
NO_DIST |
* |
||
12,000 |
12000 |
1200 |
||
Table 12.2: Landscape Suitability Rankings (LSR) and Landform-Sediment Assemblages for the Minnesota River
Map Symbol |
Geomorphology Code String |
Materials Code String
|
Temporal Code String |
Description |
Age (depth m.) |
Post Depo. & Depo. Env. (depth m.) |
LSR (depth m.) |
||||||||||||
0 | 0-1 | 1-2 | 2-5 | 0 | 0-1 | 1-2 | 2-5 | 0 | 0-1 | 1-2 | 2-5 | ||||||||
Upland Undifferentiated Landscape |
|||||||||||||||||||
U |
*.*.*.*.U.*.*.*.*.*.*.*.* |
*.*.*.*.*.*.*.* |
*.*.*.*.*.*.1230.1140.*.*.*.* |
Upland, Undifferentiated. |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
Catastrophic Flood Landscape |
|||||||||||||||||||
CBCO |
V.VW.*.*.C.*.B.*.*.*.*.N.* |
*.CO.O.>>.*.O.*.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Bar; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Not Present or Uncommon. |
1 |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CBCOK |
V.VW.*.*.C.*.B.*.*.*.*.N.* |
*.CO.O.>>.*.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Bar; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CBCOK |
V.VW.*.*.C.*.B.*.*.*.*.N.* |
*.CO.O.>>.*.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Bar; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CMCCO |
V.VW.*.*.C.*.MC.*.*.*.*.N.* |
*.CO.O.>>.*.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Not Collapsed; ; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CMCCO< |
V.VW.*.*.C.*.MC.*.*.*.*.N.* |
*.CO.O.<<.*.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Not Collapsed; ; Coarse; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
0 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CMCCO> |
V.VW.*.*.C.*.MC.*.*.*.*.N.* |
*.CO.O.>>.*.O.*.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Not Collapsed; ; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Not Present or Uncommon. |
1 |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CMCF |
V.VW.*.*.C.*.MC.*.*.*.*.N.* |
*.F.O.<<.*.*.K.* |
LW-H.*.*.*.*.*.1100.*.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Not Collapsed; ; Fine; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
0 |
1 |
2 |
2 |
0 |
1 |
2 |
2 |
0 |
|||
CMCF |
V.VW.*.*.C.*.MC.*.*.*.*.N.* |
*.F.O.<<.*.*.K.* |
LW-H.*.*.*.*.*.1100.*.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Not Collapsed; ; Fine; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
0 |
1 |
2 |
2 |
0 |
1 |
2 |
2 |
0 |
|||
CMCF> |
V.VW.*.*.C.*.MC.*.*.*.*.N.* |
*.F.O.>>.*.*.*.* |
LW-H.*.*.*.*.*.1100.*.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
1 |
2 |
2 |
1 |
|||
CMCFC |
V.VW.*.*.C.*.MC.*.*.*.*.N.* |
*.FC.O.<<.*.*.K.* |
LW-H.*.*.*.*.*.1100.*.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Not Collapsed; Fine over Coarse; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
0 |
1 |
2 |
1 |
0 |
1 |
2 |
1 |
0 |
|||
CMCO- |
V.VW.*.*.C.*.MC.*.*.*.*.N.* |
*.CO.O.><.*.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Not Collapsed; Coarse ; Diamicton Texture Not Present or Uncommon; Not Present or <1m Thick, Laterally Discontinuous; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
0 |
|||
CMCP |
V.VW.*.*.C.*.MC.*.*.*.*.N.* |
*.P.O.<<.N.B.K.* |
LW-H.*.*.*.*.*.1100.*.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Not Collapsed; Peat or Organic Muck; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Commonly Present; Bedrock or Glacial Drift, Undifferentiated. |
0 |
1 |
1 |
0 |
1 |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
|||
CMCP> |
V.VW.*.*.C.*.MC.*.*.*.*.N.* |
*.P.O.>>.N.B.*.* |
LW-H.*.*.*.*.*.1100.*.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Not Collapsed; ; Peat or Organic Muck; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Commonly Present. |
0 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
0 |
1 |
1 |
1 |
|||
CMCR- |
V.VW.*.*.C.*.MC.*.*.*.R.N.* |
*.CO.O.><.*.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Boulder or Cobble Lag; Not Collapsed; Coarse ; Diamicton Texture Not Present or Uncommon; Not Present or <1m Thick, Laterally Discontinuous; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
0 |
|||
CMCRCO< |
V.VW.*.*.C.*.MC.*.*.*.R.N.* |
*.CO.O.<<.*.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Marginal Channel; Boulder or Cobble Lag; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CER |
V.VW.*.*.C.*.ER.*.*.*.*.N.* |
*.CO.O.><.N.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Residual; Not Collapsed; Coarse ; Diamicton Texture Not Present or Uncommon; Not Present or <1m Thick, Laterally Discontinuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
0 |
0 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CST |
V.VW.*.*.C.*.ST.*.*.*.*.N.* |
*.CO.O.><.N.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Strath; Not Collapsed; Coarse ; Diamicton Texture Not Present or Uncommon; Not Present or <1m Thick, Laterally Discontinuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
0 |
0 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CSTCO |
V.VW.*.*.C.*.ST.*.*.*.*.N.* |
*.CO.O.<<.N.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Strath; Not Collapsed; Coarse ; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
0 |
0 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CSTCO |
V.VW.*.*.C.*.ST.*.*.*.*.N.* |
*.CO.O.<<.N.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Strath; Not Collapsed; Coarse ; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
0 |
0 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CSTF |
V.VW.*.*.C.*.ST.*.*.*.*.N.* |
*.F.O.<<.N.O.K.* |
LW-H.*.*.*.*.*.1100.*.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Strath; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
0 |
1 |
2 |
0 |
0 |
1 |
2 |
0 |
0 |
|||
CSTFC |
V.VW.*.*.C.*.ST.*.*.*.*.N.* |
*.FC.O.<<.O.O.K.* |
LW.L-S.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Strath; Not Collapsed; Fine over Coarse; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Type "o" Overbank Deposits; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
0 |
1 |
1 |
0 |
1 |
3 |
0 |
0 |
0 |
3 |
0 |
0 |
|||
CSTFL |
V.VW.*.*.C.*.ST.*.*.*.*.N.* |
*.F.O.<<.L.O.K.* |
LW.LW-E.*.*.*.*.1100.1040.1100.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Strath; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Loess; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
0 |
1 |
3 |
0 |
0 |
1 |
3 |
0 |
0 |
|||
CSTFO |
V.VW.*.*.C.*.ST.*.*.*.*.N.* |
*.F.O.><.O.*.K.* |
LW.L-S.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Strath; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; Not Present or <1m Thick, Laterally Discontinuous; Type "o" Overbank Deposits; Bedrock or Glacial Drift, Undifferentiated. |
0 |
1 |
1 |
0 |
1 |
2 |
0 |
0 |
0 |
2 |
0 |
0 |
|||
CSTO |
V.VW.*.*.C.*.ST.*.*.*.*.N.* |
*.*.O.><.O.*.K.* |
LW.L-S.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Strath; Not Collapsed; Diamicton Texture Not Present or Uncommon; Not Present or <1m Thick, Laterally Discontinuous; Type "o" Overbank Deposits; Bedrock or Glacial Drift, Undifferentiated. |
0 |
1 |
1 |
0 |
1 |
2 |
0 |
0 |
0 |
2 |
0 |
0 |
|||
CSTR |
V.VW.*.*.C.*.ST.*.*.*.R.N.* |
*.CO.O.><.N.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Strath; Boulder or Cobble Lag; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; Not Present or <1m Thick, Laterally Discontinuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
0 |
0 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CSTRCO |
V.VW.*.*.C.*.ST.*.*.*.R.N.* |
*.CO.O.<<.N.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Strath; Boulder or Cobble Lag; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
0 |
0 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CSTRCO |
V.VW.*.*.C.*.ST.*.*.*.R.N.* |
*.CO.O.<<.N.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Erosional Strath; Boulder or Cobble Lag; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
0 |
0 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CTCO |
V.VW.*.*.C.*.T.*.*.*.*.N.* |
*.CO.O.>>.N.O.*.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Terrace; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon. |
1 |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CTCO |
V.VW.*.*.C.*.T.*.*.*.*.N.* |
*.CO.O.>>.N.O.*.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Terrace; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon. |
1 |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CTCOK |
V.VW.*.*.C.*.T.*.*.*.*.N.* |
*.CO.O.>>.N.O.K.* |
LW.*.*.*.*.*.1100.1040.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Terrace; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
1 |
0 |
0 |
0 |
|||
CTF |
V.VW.*.*.C.*.T.*.*.*.*.N.* |
*.F.O.>>.*.*.*.* |
LW-H.*.*.*.*.*.1100.*.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Terrace; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
0 |
1 |
1 |
1 |
0 |
|||
CTFCL |
V.VW.*.*.C.*.T.*.*.*.*.N.* |
*.FC.O.>>.L.O.*.* |
LW.LW-E.*.*.*.*.1100.1040.1100.*.*.* |
Glaciofluvial Valley;Glacial River Warren;Catastrophic Flood; Terrace; Not Collapsed; Fine over Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Loess; Buried Soil(s) Not Present or Uncommon. |
1 |
1 |
1 |
1 |
1 |
3 |
0 |
0 |
1 |
3 |
0 |
0 |
|||
Paleo-Valley Landscape |
|||||||||||||||||||
YF |
L.D.R.BLU.Y.*.F.*.*.*.*.N.*. |
*.F.O.>>.*.B.*.* |
LW-H.*.*.*.*.*.1100.*.*.*.*.* |
Glacial Lobe; Des Moines; River Valley; Blue Earth Valley; Paleo-Valley; Floodplain, Undifferentiated; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
2 |
1 |
2 |
2 |
2 |
|||
YFO |
L.D.R.BLU.Y.*.F.*.*.*.*.N.*. |
*.F.O.>>.O.B.*.* |
LW-H.*.*.*.*.*.1100.*.*.*.*.* |
Glacial Lobe; Des Moines; River Valley; Blue Earth Valley; Paleo-Valley; Floodplain, Undifferentiated; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Type "o" Overbank Deposits; Buried Soil(s) Commonly Present. |
0 |
1 |
1 |
1 |
1 |
2 |
2 |
2 |
0 |
2 |
2 |
2 |
|||
YPC |
L.D.*.*.Y.*.PC.*.*.*.*.C.*. |
*.*.*.*.*.*.*.* |
LW.*.*.*.*.*.1100.*.*.*.*.* |
Glacial Lobe; Des Moines; Paleo-Valley; Paleochannel; Colluvial Slope. |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
|||
Valley Terrace Landscape |
|||||||||||||||||||
VPC2F |
V.VW.*.*.V.*.PC.*.*.*.*.N.*. |
*.F.O.>>.*.B.*.* |
LW-H.*.*.2.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley;Glacial River Warren; Valley Terrace; Paleochannel; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
|||
VPC |
L.D.*.*.V.*.PC.*.*.*.*.N.*. |
*.F.O.>>.*.*.*.* |
LW-H.*.*.*.*.C.1100.850.*.*.*.* |
Glacial Lobe; Des Moines; Paleo-Valley; Paleochannel; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
|||
VT2- |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.CO.O.><.*.*.K.* |
LW-E.*.*.2.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; Not Present or <1m Thick, Laterally Discontinuous; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
0 |
|||
VT2CO |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.CO.O.>>.*.*.*.* |
LW-E.*.*.2.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
|||
VT2CO< |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.CO.O.<<.*.*.K.* |
LW-E.*.*.2.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
0 |
1 |
1 |
1 |
0 |
1 |
1 |
1 |
0 |
|||
VT2CO<O |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.CO.O.<<.O.*.K.* |
LW-E.L-S.*.2.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Type "o" Overbank Deposits; Bedrock or Glacial Drift, Undifferentiated. |
0 |
1 |
1 |
0 |
1 |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
|||
VT2F |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.F.O.>>.*.B.*.* |
LW-H.*.*.2.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
2 |
1 |
2 |
2 |
2 |
|||
VT2P |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.P.O.>>.*.B.*.* |
LW-H.*.*.2.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Peat or Organic Muck; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
0 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
0 |
1 |
1 |
1 |
|||
VT2P< |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.P.O.<<.*.B.K.* |
LW-H.*.*.2.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Peat or Organic Muck; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present; Bedrock or Glacial Drift, Undifferentiated. |
0 |
1 |
1 |
0 |
1 |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
|||
VT2P< |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.P.O.<<.*.B.K.* |
LW-H.*.*.2.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Peat or Organic Muck; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present; Bedrock or Glacial Drift, Undifferentiated. |
0 |
1 |
1 |
0 |
1 |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
|||
VT1CO |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.CO.O.>>.*.*.*.* |
LW-E.*.*.1.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
|||
VT1CO< |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.CO.O.<<.*.*.K.* |
LW-E.*.*.1.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; <2m Thick, Laterally Continuous; Bedrock or Glacial Drift, Undifferentiated. |
1 |
1 |
1 |
0 |
1 |
1 |
1 |
0 |
1 |
1 |
1 |
0 |
|||
VT1F |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.F.O.>>.*.B.*.* |
LW-E.*.*.1.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
2 |
1 |
2 |
2 |
2 |
|||
VT1FC |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.FC.O.>>.O.*.*.* |
LW-E.L-S.*.1.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Fine over Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Type "o" Overbank Deposits. |
0 |
1 |
1 |
1 |
1 |
3 |
1 |
1 |
0 |
3 |
1 |
1 |
|||
VT1FO |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.F.O.>>.O.B.*.* |
LW-E.L-S.*.1.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Type "o" Overbank Deposits; Buried Soil(s) Commonly Present. |
0 |
1 |
1 |
1 |
1 |
3 |
2 |
2 |
0 |
3 |
2 |
2 |
|||
VT1P |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.P.O.>>.*.B.*.* |
LW-H.*.*.1.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Peat or Organic Muck; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
0 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
0 |
1 |
1 |
1 |
|||
VT1PF |
V.VW.*.*.V.*.T.*.*.*.*.N.*. |
*.PF.O.>>.*.B.*.* |
LW-H.*.*.1.*.C.1100.850.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Valley Terrace; Terrace; Not Collapsed; Peat or Organic Muck over Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
0 |
1 |
1 |
1 |
1 |
1 |
1 |
2 |
0 |
1 |
1 |
2 |
|||
VT |
L.D.*.*.V.*.T.*.*.*.*.N.*. |
*.CO.O.*.*.*.*.* |
LW-E.*.*.*.*.C.1100.850.*.*.*.* |
Glacial Lobe; Des Moines; Valley Terrace; Terrace; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon. |
1 |
1 |
1 |
0 |
1 |
2 |
2 |
0 |
1 |
2 |
2 |
0 |
|||
Floodplain Landscape |
|||||||||||||||||||
FDE |
V.VW.R.MN.F.*.DE.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
H.*.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Delta; Not Collapsed; ; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
2 |
1 |
2 |
2 |
2 |
|||
FFW |
V.VW.R.MN.F.*.FW.*.*.*.*.N.* |
*.CO.O.>>.N.O.*.* |
S.*.*.*.*.V.15.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Floodplain, Type "w"; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon. |
0 |
0 |
0 |
0 |
1 |
2 |
2 |
1 |
0 |
0 |
0 |
0 |
|||
FFX |
V.VW.R.MN.F.*.FX.*.*.*.*.N.* |
*.*.O.>>.*.*.*.* |
L-S.*.*.*.*.V.500.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Floodplain, Type "x"; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
1 |
2 |
2 |
1 |
|||
FFXA |
V.VW.R.MN.F.*.FX.*.*.*.*.N.* |
*.*.O.>>.A.*.*.* |
L-S.L-S.*.*.*.V.500.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Floodplain, Type "x"; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Type "a" Overbank Deposits. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
1 |
2 |
2 |
1 |
|||
FFXO |
V.VW.R.MN.F.*.FX.*.*.*.*.N.* |
*.*.O.>>.O.*.*.* |
L-S.S.*.*.*.V.500.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Floodplain, Type "x"; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Type "o" Overbank Deposits. |
0 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
0 |
2 |
2 |
1 |
|||
FFY |
V.VW.R.MN.F.*.FY.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
E-L.*.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Floodplain, Type "y"; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
0 |
1 |
1 |
1 |
0 |
|||
FFYA |
V.VW.R.MN.F.*.FY.*.*.*.*.N.* |
*.F.O.>>.A.B.*.* |
E-L.M-S.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Floodplain, Type "y"; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Type "a" Overbank Deposits; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
1 |
2 |
2 |
1 |
|||
FFYO |
V.VW.R.MN.F.*.FY.*.*.*.*.N.* |
*.F.O.>>.O.B.*.* |
E-L.S.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Floodplain, Type "y"; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Type "o" Overbank Deposits; Buried Soil(s) Commonly Present. |
0 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
0 |
2 |
2 |
1 |
|||
FFZ |
V.VW.R.MN.F.*.FZ.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
E-L.*.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Floodplain, Type "z"; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
0 |
|||
FFZA |
V.VW.R.MN.F.*.FZ.*.*.*.*.N.* |
*.F.O.>>.A.B.*.* |
E-L.M-L.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Floodplain, Type "z"; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Type "a" Overbank Deposits; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
0 |
1 |
1 |
1 |
0 |
|||
FFZO |
V.VW.R.MN.F.*.FZ.*.*.*.*.N.* |
*.F.O.>>.O.B.*.* |
E-L.L-S.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Floodplain, Type "z"; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Type "o" Overbank Deposits; Buried Soil(s) Commonly Present. |
0 |
1 |
1 |
1 |
1 |
1 |
1 |
0 |
0 |
1 |
1 |
0 |
|||
FF |
*.*.*.*.F.*.F.*.*.*.*.N.* |
*.*.O.>>.*.B.*.* |
H.*.*.*.*.V.1040.*.*.*.*.* |
Floodplain; Floodplain, Undifferentiated; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
2 |
1 |
2 |
2 |
2 |
|||
FF |
*.*.*.*.F.*.F.*.*.*.*.N.* |
*.*.O.>>.*.B.*.* |
H.*.*.*.*.V.1040.*.*.*.*.* |
Floodplain; Floodplain, Undifferentiated; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
2 |
1 |
2 |
2 |
2 |
|||
FI |
V.VW.R.MN.F.*.I.*.*.*.*.N.* |
*.F.O.>>.*.*.*.* |
H.*.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Island; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
1 |
2 |
2 |
1 |
|||
FI |
V.VW.R.MN.F.*.I.*.*.*.*.N.* |
*.F.O.>>.*.*.*.* |
H.*.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Island; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
1 |
2 |
2 |
1 |
|||
FNL |
V.VW.R.MN.F.*.NL.*.*.*.*.N.* |
*.*.O.>>.*.B.*.* |
M-L.*.*.*.*.F.500.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Natural Levee; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
2 |
1 |
2 |
2 |
2 |
|||
FMB2C |
V.VW.R.MN.F.*.MB.*.*.*.*.N.* |
*.*.O.>>.*.B.*.* |
H.*.*.2.*.C.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Meander Belt; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
|||
FMB2F |
V.VW.R.MN.F.*.MB.*.*.*.*.N.* |
*.*.O.>>.*.B.*.* |
H.*.*.2.*.F.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Meander Belt; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
|||
FMB1C |
V.VW.R.MN.F.*.MB.*.*.*.*.N.* |
*.*.O.>>.*.B.*.* |
H.*.*.1.*.C.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Meander Belt; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
|||
FMB1F |
V.VW.R.MN.F.*.MB.*.*.*.*.N.* |
*.*.O.>>.*.B.*.* |
H.*.*.1.*.F.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Meander Belt; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
|||
FMB1V |
V.VW.R.MN.F.*.MB.*.*.*.*.N.* |
*.*.O.>>.*.B.*.* |
H.*.*.1.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Meander Belt; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
1 |
|||
FOB2C |
V.VW.R.MN.F.*.OB.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
H.*.*.2.*.C.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Overbank Belt; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
1 |
2 |
2 |
1 |
|||
FOB2F |
V.VW.R.MN.F.*.OB.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
H.*.*.2.*.F.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Overbank Belt; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
2 |
1 |
2 |
2 |
2 |
|||
FOB2V |
V.VW.R.MN.F.*.OB.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
H.*.*.2.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Overbank Belt; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
1 |
2 |
2 |
1 |
|||
FOB1C |
V.VW.R.MN.F.*.OB.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
H.*.*.1.*.C.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Overbank Belt; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
1 |
2 |
2 |
1 |
|||
FOB1F |
V.VW.R.MN.F.*.OB.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
H.*.*.1.*.F.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Overbank Belt; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
2 |
1 |
2 |
2 |
2 |
|||
FOB1F |
V.VW.R.MN.F.*.OB.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
H.*.*.1.*.F.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Overbank Belt; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
2 |
1 |
2 |
2 |
2 |
|||
FOB1V |
V.VW.R.MN.F.*.OB.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
H.*.*.1.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Overbank Belt; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
2 |
2 |
1 |
1 |
2 |
2 |
1 |
|||
FPC3 |
V.VW.R.MN.F.*.PC.*.*.*.*.N.* |
*.F.O.>>.*.*.*.* |
E-L.*.*.3.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Paleochannel; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
|||
FPC2 |
V.VW.R.MN.F.*.PC.*.*.*.*.N.* |
*.F.O.>>.*.*.*.* |
L-S.*.*.2.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Paleochannel; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
|||
FPC1 |
V.VW.R.MN.F.*.PC.*.*.*.*.N.* |
*.F.O.>>.*.*.*.* |
S.*.*.1.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Paleochannel; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
|||
FPC |
V.VW.R.MN.F.*.PC.*.*.*.*.N.* |
*.F.O.>>.*.*.*.* |
H.*.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Paleochannel; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
|||
FPC |
V.VW.R.MN.F.*.PC.*.*.*.*.N.* |
*.F.O.>>.*.*.*.* |
H.*.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Paleochannel; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous. |
1 |
1 |
1 |
1 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
|||
FR |
V.VW.R.MN.F.*.R.*.*.*.*.N.* |
*.CO.O.*.N.O.*.* |
S.*.*.*.*.*.*.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; River Channel, Active; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; Overlying Deposits Not Present; Buried Soil(s) Not Present or Uncommon. |
0 |
1 |
1 |
1 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
0 |
|||
FCSF |
V.VW.R.MN.F.*.CS.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
M-L.*.*.*.*.F.500.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Crevasse Splay; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
3 |
3 |
3 |
1 |
3 |
3 |
3 |
|||
FCSV |
V.VW.R.MN.F.*.CS.*.*.*.*.N.* |
*.F.O.>>.*.B.*.* |
M-L.*.*.*.*.V.500.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Floodplain; Crevasse Splay; Not Collapsed; Fine; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
3 |
3 |
3 |
1 |
3 |
3 |
3 |
|||
Valley Margin Landscape |
|||||||||||||||||||
MC |
V.VW.R.MN.M.*.C.*.*.*.*.N.* |
*.*.O.>>.N.B.*.* |
H.*.*.*.*.*.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Valley Margin; Colluvial Slope; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
3 |
3 |
3 |
1 |
3 |
3 |
3 |
|||
MAF |
V.VW.R.MN.M.*.AF.*.*.*.*.N.* |
*.*.O.>>.N.B.*.* |
H.*.*.*.*.*.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Valley Margin; Alluvial Fan; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
3 |
3 |
3 |
1 |
3 |
3 |
3 |
|||
MAFC |
V.VW.R.MN.M.*.AF.*.*.*.*.N.* |
*.*.O.>>.N.B.*.* |
H.*.*.*.*.C.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Valley Margin; Alluvial Fan; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
3 |
3 |
3 |
1 |
3 |
3 |
3 |
|||
MAFF |
V.VW.R.MN.M.*.AF.*.*.*.*.N.* |
*.*.O.>>.N.B.*.* |
H.*.*.*.*.F.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Valley Margin; Alluvial Fan; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
3 |
3 |
3 |
1 |
3 |
3 |
3 |
|||
MAFV |
V.VW.R.MN.M.*.AF.*.*.*.*.N.* |
*.*.O.>>.N.B.*.* |
H.*.*.*.*.V.1040.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; River Valley; Minnesota Valley; Valley Margin; Alluvial Fan; Not Collapsed; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
3 |
3 |
3 |
1 |
3 |
3 |
3 |
|||
Eolian Landscape |
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EEDC |
V.VW.*.*.E.*.ED.*.*.*.*.N.* |
*.CO.O.>>.N.B.*.* |
LW-H.*.*.*.*.C.1100.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Eolian; Dune; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
3 |
3 |
3 |
1 |
3 |
3 |
3 |
|||
EEDV |
V.VW.*.*.E.*.ED.*.*.*.*.N.* |
*.CO.O.>>.N.B.*.* |
LW-H.*.*.*.*.V.1100.*.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Eolian; Dune; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
3 |
3 |
3 |
1 |
3 |
3 |
3 |
|||
EDP |
V.VW.*.*.E.*.DP.*.*.*.*.N.* |
*.CO.O.>>.N.B.*.* |
LW-H.*.*.*.*.*.1100.*.*.*.* |
Glaciofluvial Valley; Glacial River Warren; Eolian; Interdunal Depression or Pond; Not Collapsed; Coarse; Diamicton Texture Not Present or Uncommon; >2m Thick, Laterally Continuous; Overlying Deposits Not Present; Buried Soil(s) Commonly Present. |
1 |
1 |
1 |
1 |
1 |
3 |
3 |
3 |
1 |
3 |
3 |
3 |