## GeMS validation of WI_2023_M509_1-1-dataset01.gdb

File written by GeMS_ValidateDatabase.py, version of 8/29/2023
Tue Sep 19 13:34:22 2023
Runtime parameters
Database path: P:\WaupacaQuaternary\Waupaca_GeMS_Conversion\Waupaca_Co_Quat_Submittal\WI_2023_M509_1-1_submittal\WI_2023_M509_1-1\WI_2023_M509_1-1-database\WI_2023_M509_1-1-dataset01.gdb
Output directory: P:\WaupacaQuaternary\Waupaca_GeMS_Conversion\Waupaca_GeMS_Validations
Metadata file: P:\WaupacaQuaternary\Waupaca_GeMS_Conversion\Waupaca_Co_Quat_Submittal\WI_2023_M509_1-1_submittal\WI_2023_M509_1-1\WI_2023_M509_1-1-metadata.xml
Check embedded metadata: False
Skip topology check: False
Refresh GeoMaterialDict: True
Delete extra rows in Glossary and DataSources: False
Compact GDB: True
This database is LEVEL 3 COMPLIANT.
The database-level FGDC metadata are formally correct although the metadata record should be reviewed to verify that it is meaningful.
This file should be accompanied by WI_2023_M509_1-1-dataset01.gdb-ValidationErrors.html and WI_2023_M509_1-1-metadata.xml_errors.txt in the same directory.
If this database will be submitted to the NGMDB, it also needs to be accompanied by a reviewed Geologic Names report that includes identification of any suggested modifications to Geolex. Use the Geologic Names Check tool to generate that report or provide other documentation of a review.
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### Contents

Compliance Criteria
Warnings
Content not specified in GeMS schema
Occurrence of MapUnits in DMU, feature datasets, or geopackage tables
Contents of Nonspatial Tables
DataSources
DescriptionOfMapUnits
Glossary
MiscellaneousMapInformation
Database Inventory

### Compliance Criteria

#### LEVEL 1

Criteria for a LEVEL 1 GeMS database are:

- No overlaps or internal gaps in map-unit polygon layer
- Contacts and faults in single feature class
- Map-unit polygon boundaries are covered by contacts and faults lines

Databases with a variety of schema may meet these criteria. This script cannot confirm LEVEL 1 compliance.

#### LEVEL 2--MINIMALLY COMPLIANT

A LEVEL 2 GeMS database is accompanied by a peer-reviewed Geologic Names report, including identification of suggested modifications to Geolex, and meets the following criteria:

2.1 Has required elements: nonspatial tables DataSources, DescriptionOfMapUnits, GeoMaterialDict; feature dataset GeologicMap with feature classes ContactsAndFaults and MapUnitPolys | PASS
2.2 Required fields within required elements are present and correctly defined | PASS
2.3 All MapUnitPolys and ContactsAndFaults based feature classes obey Level 2 topology rules: no internal gaps or overlaps in MapUnitPolys, boundaries of MapUnitPolys are covered by ContactsAndFaults | PASS
2.4 All map units in MapUnitPolys have entries in DescriptionOfMapUnits table | PASS
2.5 No duplicate MapUnit values in DescriptionOfMapUnit table | PASS
2.6 Certain field values within required elements have entries in Glossary table | PASS
2.7 No duplicate Term values in Glossary table | PASS
2.8 All xxxSourceID values in required elements have entries in DataSources table | PASS
2.9 No duplicate DataSources_ID values in DataSources table | PASS

#### LEVEL 3--FULLY COMPLIANT

A LEVEL 3 GeMS database meets these additional criteria:

3.1 Table and field definitions beyond Level 2 conform to GeMS schema | PASS
3.2 All MapUnitPolys and ContactsAndFaults based feature classes obey Level 3 topology rules: No ContactsAndFaults overlaps, self-overlaps, or self-intersections. | PASS
3.3 No missing required values | PASS
3.4 No missing terms in Glossary | PASS
3.5 No unnecessary terms in Glossary | PASS
3.6 No missing sources in DataSources | PASS
3.7 No unnecessary sources in DataSources | PASS
3.8 No map units without entries in DescriptionOfMapUnits | PASS
3.9 No unnecessary map units in DescriptionOfMapUnits | PASS
3.10 HierarchyKey values in DescriptionOfMapUnits are unique and well formed | PASS
3.11 All values of GeoMaterial are defined in GeoMaterialDict. GeoMaterialDict is as specified in the GeMS standard | PASS
3.12 No duplicate _ID values | PASS
3.13 No zero-length, whitespace-only, or bad null values | PASS

### Warnings

There are 0 warnings

### Content not specified in GeMS schema

Some of the extensions to the GeMS schema identified here may be necessary to capture geologic content and are entirely appropriate. Please document these extensions in metadata for the database, any accompanying README file, and (if applicable) any transmittal letter that accompanies the dataset. Other extensions may be intermediate datasets, fields, or files that should be deleted before distribution of the database.

#### Fields

ContactsAndFaults, MapText
GeologicLines, MapText

#### Tables

### Occurrence of MapUnit in DMU, feature datasets, or geopackage tables

MapUnit | DescriptionOfMapUnits | GeologicMap
--- | --- | ---
gk | X | X
ghc | X | X
po | X | X
ghs | X | X
water | X | X
gks | X | X
pg | X | X
lo | X | X
wlo | X | X
sc | X | X
gh | X | X
sa | X | X
gkw | X | X
gkc | X | X
wgk | X | X
s | X | X
ghw | X | X
p | X | X
low | X | X
ps | X | X
gklo | X | X
su | X | X
r | X | X
w | X | X

### Contents of Nonspatial Tables

#### DataSources

OBJECTID | Source | Notes | URL | DataSources_ID
--- | --- | --- | --- | ---
2 | Neuendorf, Klaus; Mehl, James P., Jr; and Jackson, Julia A., eds., 2005, Glossary of geology (fifth ed.): Alexandria, VA, American Geological Institute, 779 p. | None | None | AGI_2005
1 | Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates. | None | https://ngmdb.usgs.gov/fgdc_gds/geolsymstd.php | FGDC-STD-013-2006
4 | U.S. Geological Survey National Cooperative Geologic Mapping Program, 2020, GeMS (Geologic Map Schema)—A standard format for the digital publication of geologic maps: U.S. Geological Survey Techniques and Methods, book 11, chap. B10, 74 p., https://doi.org//10.3133/tm11B10. | None | https://pubs.er.usgs.gov/publication/tm11B10 | GeMS_2020
10 | Mode, William N.; Hooyer, Thomas S.; Attig, John W.; Clayton, Lee; Rawling, J. Elmo III., 2023, Quaternary Geology of Waupaca County, Wisconsin. Wisconsin Geological and Natural History Survey Map Series 509, 1 plate. | None | https://doi.org/10.54915/bger3320 | Waupaca_Quaternary_Mode_et_al_2023

#### DescriptionOfMapUnits

OBJECTID | MapUnit | Name | FullName | Age | Description | HierarchyKey | ParagraphStyle | Label | Symbol | AreaFillRGB | AreaFillPatternDescription | DescriptionSourceID | GeoMaterial | GeoMaterialConfidence | DescriptionOfMapUnits_ID
--- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | ---
1 | None | Postglacial deposits | None | None | None | 001 | Heading2 | None | None | None | None | Waupaca_Quaternary_Mode_et_al_2023 | None | None | DMU0001
2 | w | Windblown sand | Windblown sand | Pleistocene to Holocene | Well-sorted sand composing dunes and sheets; between 2 and 7 m thick; most sand deposited immediately following deglaciation. Abundant dunes, generally no more than 5 m high. | 001-001 | DMU2 | w | w | 253,249,194 | None | Waupaca_Quaternary_Mode_et_al_2023 | Dune sand | High | DMU0002
3 | wlo | Windblown sand over lake sediment | Windblown sand over lake sediment | Pleistocene to Holocene | Well-sorted sand composing dunes and sheets; between 2 and 7 m thick; most sand deposited immediately following deglaciation. Sand sheets and infrequent dunes; overlies lake sediment. | 001-002 | DMU2 | wlo | wlo | 237,215,161 | None | Waupaca_Quaternary_Mode_et_al_2023 | Dune sand | Medium | DMU0003
4 | wgk | Windblown sand over till of the Kirby Lake Member | Windblown sand over till of the Kirby Lake Member of the Kewaunee Formation | Pleistocene to Holocene | Well-sorted sand composing dunes and sheets; between 2 and 7 m thick; most sand deposited immediately following deglaciation. Sand sheets and infrequent dunes; overlies red, clayey and silty till of the Kirby Lake Member of the Kewaunee Formation. | 001-003 | DMU2 | wgk | wgk | 222,199,136 | None | Waupaca_Quaternary_Mode_et_al_2023 | Dune sand | Medium | DMU0004
5 | p | Peat | Peat | Holocene | Sediment of low, typically wet areas consisting of peat and muck occupying low-lying, flat to low-relief surfaces; thickness varies, but typically between 1 and 3 m thick. | 001-004 | DMU2 | p | p | 177,143,105 | None | Waupaca_Quaternary_Mode_et_al_2023 | Peat and muck | High | DMU0005
6 | po | Peat over lake sediment | Peat over lake sediment of glacial Lake Oshkosh | Pleistocene to Holocene | Sediment of low, typically wet areas consisting of peat and muck over lake sediment of glacial Lake Oshkosh; usually in areas that are less than 244 m above sea level. | 001-005 | DMU2 | po | po | 199,190,192 | None | Waupaca_Quaternary_Mode_et_al_2023 | Peat and muck | Medium | DMU0006
7 | pg | Peat over till of the Horicon Member or Kirby Lake Member | Peat over till of the Horicon Member of the Holy Hill Formation or Kirby Lake Member of the Kewaunee Formation | Pleistocene to Holocene | Sediment of low, typically wet areas consisting of peat and muck overlying the sandy till of the Horicon Member of the Holy Hill Formation or clayey and silty till of the Kirby Lake Member of the Kewaunee Formation. | 001-006 | DMU2 | pg | pg | 205,168,133 | None | Waupaca_Quaternary_Mode_et_al_2023 | Peat and muck | Medium | DMU0007
8 | ps | Peat over meltwater-stream sediment | Peat over meltwater-stream sediment | Pleistocene to Holocene | Sediment of low, typically wet areas consisting of peat and muck overlying postglacial or meltwater-stream sediment consisting of silty and sandy sediment with occasional channel sand and silt. | 001-007 | DMU2 | ps | ps | 213,148,136 | None | Waupaca_Quaternary_Mode_et_al_2023 | Peat and muck | Medium | DMU0008
9 | s | Stream sediment | Stream sediment | Holocene | Commonly consists of silty and sandy sediment with occasional channel sand and silt; typically between 1 and 15 m thick; deposited in floodplains andjacent to postglacial streams; most of this sediment was probably deposited during the last part of the Holocene. | 001-008 | DMU1 | s | s | 248,221,229 | None | Waupaca_Quaternary_Mode_et_al_2023 | Alluvial sediment, mostly fine-grained | High | DMU0009
10 | None | Glacial deposits, undifferentiated | None | None | None | 002 | Heading2 | None | None | None | None | Waupaca_Quaternary_Mode_et_al_2023 | None | None | DMU0010
11 | lo | Lake sediment | Lake sediment deposited in glacial Lake Oshkosh | Pleistocene | Commonly consists of sand, silt, and clay. Sediment deposited in glacial Lake Oshkosh usually at elevations below 244 m above sea level; consists largely of silt and clay where deposited in deeper water grading to sand near the shoreline; typically between 1 m and tens of meters thick; sediment deposited near the shoreline may include wind-blown sediment, washed hillslope sediment, and patches of peat that could not be mapped separately. | 002-001 | DMU2 | lo | lo | 184,200,227 | None | Waupaca_Quaternary_Mode_et_al_2023 | Lacustrine sediment, mostly fine-grained | High | DMU0011
12 | low | Lake sediment covered with thin windblown sand | Lake sediment deposited in glacial Lake Oshkosh covered with thin windblown sand | Pleistocene | Commonly consists of sand, silt, and clay. Glacial Lake Oshkosh sediment covered with thin patches of windblown sand generally less than 2 m thick. | 002-002 | DMU2 | low | low | 184,200,227 | fill overlaid by regular mesh resulting in small, square areas of fill. Pattern covers majority of fill. | Waupaca_Quaternary_Mode_et_al_2023 | Lacustrine sediment, mostly fine-grained | Medium | DMU0012
13 | sa | Meltwater-stream sediment deposited in alluval fans or deltas | Meltwater-stream sediment deposited in alluval fans or deltas | Pleistocene | Sand and gravel deposited directly by streams originating from the margin of the Green Bay Lobe; commonly between 1 m and several tens of meters thick; sediment deposited in an alluvial fan or delta immediately adjacent to a moraine or ice-contact face. | 002-003 | DMU2 | sa | sa | 246,200,202 | None | Waupaca_Quaternary_Mode_et_al_2023 | Ice-contact and ice-marginal sediment, mostly coarse-grained | High | DMU0013
14 | su | Meltwater-stream sediment deposited in proglacial rivers or tunnel channels | Meltwater-stream sediment deposited in proglacial rivers or tunnel channels | Pleistocene | Sand and gravel deposited directly by streams originating from the margin of the Green Bay Lobe; sediment deposited in proglacial river channels or in tunnel channels beneath the margin of the Green Bay Lobe. | 002-004 | DMU2 | su | su | 241,186,183 | None | Waupaca_Quaternary_Mode_et_al_2023 | Ice-contact and ice-marginal sediment, mostly coarse-grained | High | DMU0014
15 | sc | Collapsed meltwater-stream sediment deposited in alluvial fans, deltas or proglacial rivers | Collapsed meltwater-stream sediment deposited in alluvial fans, deltas or proglacial rivers | Pleistocene | Sand and gravel deposited directly by streams originating from the margin of the Green Bay Lobe; Collapsed sediment deposited in alluvial fans, deltas, and proglacial river channels. | 002-005 | DMU2 | sc | sc | 238,185,182 | fill overlaid by regular mesh resulting in medium, generally round areas of fill. Pattern covers approximately 50% of fill. | Waupaca_Quaternary_Mode_et_al_2023 | Ice-contact and ice-marginal sediment, mostly coarse-grained | High | DMU0015
16 | None | Kewaunee Formation, Kirby Lake Member | None | None | None | 003 | Heading2 | None | None | None | None | Waupaca_Quaternary_Mode_et_al_2023 | None | None | DMU0016
17 | gk | Low-relief till of the Kirby Lake Member | Low-relief till of the Kirby Lake Member of the Kewaunee Formation | Pleistocene | Reddish brown, clayey silt with some gravel deposited by readvances of the Green Bay Lobe; generally at least 3 m thick. Low-relief, nondescript glacial topography; generally draped over pre-existing topography; till in places less than 3 m thick. | 003-001 | DMU2 | gk | gk | 181,219,207 | None | Waupaca_Quaternary_Mode_et_al_2023 | Glacial till, mostly silty | High | DMU0017
18 | gkw | Low-relief till of the Kirby Lake Member covered with thin windblown sand | Low-relief till of the Kirby Lake Member of the Kewaunee Formation covered with thin windblown sand | Pleistocene | Reddish brown, clayey silt with some gravel deposited by readvances of the Green Bay Lobe; generally at least 3 m thick. Low-relief, nondescript glacial topography; generally draped over pre-existing topography; till in places less than 3 m thick. Covered with thin patches of windblown sand less than 2 m thick. | 003-002 | DMU2 | gkw | gkw | 179,217,205 | fill overlaid by regular mesh resulting in small, square areas of fill. Pattern covers majority of fill. | Waupaca_Quaternary_Mode_et_al_2023 | Glacial till, mostly silty | Medium | DMU0018
19 | gklo | Low-relief till of the Kirby Lake Member covered with thin lake sediment | Low-relief till of the Kirby Lake Member of the Kewaunee Formation covered with thin lake sediment deposited in glacial Lake Oshkosh | Pleistocene | Reddish brown, clayey silt with some gravel deposited by readvances of the Green Bay Lobe; generally at least 3 m thick. Covered with thin patches of glacial Lake Oshkosh sediment generally less than 2 m thick. | 003-003 | DMU2 | gklo | gklo | 176,218,205 | None | Waupaca_Quaternary_Mode_et_al_2023 | Glacial till, mostly silty | Medium | DMU0019
20 | gks | Streamlined till of the Kirby Lake Member | Streamlined till of the Kirby Lake Member of the Kewaunee Formation | Pleistocene | Reddish brown, clayey silt with some gravel deposited by readvances of the Green Bay Lobe; generally at least 3 m thick. Rolling topography that was subglacially molded; contains streamlined landforms, including drumlins and flutes; many of these landforms are at least partly composed of other sediment, including gravel, sand, and silt. | 003-004 | DMU2 | gks | gks | 160,202,187 | None | Waupaca_Quaternary_Mode_et_al_2023 | Ice-contact and ice-marginal sediment, mostly coarse-grained | Medium | DMU0020
21 | gkc | Collapsed till of the Kirby Lake Member | Collapsed till of the Kirby Lake Member of the Kewaunee Formation | Pleistocene | Reddish brown, clayey silt with some gravel deposited by readvances of the Green Bay Lobe; generally at least 3 m thick. Collapsed till overlying meltwater-stream sediment. | 003-005 | DMU2 | gkc | gkc | 180,218,205 | fill overlaid by regular mesh resulting in medium, generally round areas of fill. Pattern covers approximately 50% of fill. | Waupaca_Quaternary_Mode_et_al_2023 | Glacial till, mostly silty | Medium | DMU0021
22 | None | Holy Hill Formation, Horicon Member | None | None | None | 004 | Heading2 | None | None | None | None | Waupaca_Quaternary_Mode_et_al_2023 | None | None | DMU0022
23 | gh | Rolling till of the Horicon Member | Rolling till of the Horicon Member of the Holy Hill Formation | Pleistocene | Brown to reddish-brown, gravelly, clayey, silty sand deposited by the Green Bay Lobe; generally at least 3 m thick; includes many small to large inclusions of windblown sediment, hillslope sediment, and glacial lake sediment that could not be separately mapped. In many areas, the modern surface reflects the landscape before the last part of the Wisconsin Glaciation. Generally has rolling topography in areas lacking drumlins. | 004-001 | DMU2 | gh | gh | 206,227,191 | None | Waupaca_Quaternary_Mode_et_al_2023 | Glacial till, mostly sandy | High | DMU0023
24 | ghw | Rolling till of the Horicon Member covered with thin windblown sand | Rolling till of the Horicon Member of the Holy Hill Formation covered with thin windblown sand | Pleistocene | Brown to reddish-brown, gravelly, clayey, silty sand deposited by the Green Bay Lobe; generally at least 3 m thick; includes many small to large inclusions of windblown sediment, hillslope sediment, and glacial lake sediment that could not be separately mapped. In many areas, the modern surface reflects the landscape before the last part of the Wisconsin Glaciation. Generally has rolling topography in areas lacking drumlins but covered with thin patches of windblown sand less than 2 m thick. | 004-002 | DMU2 | ghw | ghw | 206,227,191 | fill overlaid by regular mesh resulting in small, square areas of fill. Pattern covers majority of fill. | Waupaca_Quaternary_Mode_et_al_2023 | Glacial till, mostly sandy | Medium | DMU0024
25 | ghs | Streamlined till of the Horicon Member | Streamlined till of the Horicon Member of the Holy Hill Formation | Pleistocene | Brown to reddish-brown, gravelly, clayey, silty sand deposited by the Green Bay Lobe; generally at least 3 m thick; includes many small to large inclusions of windblown sediment, hillslope sediment, and glacial lake sediment that could not be separately mapped. In many areas, the modern surface reflects the landscape before the last part of the Wisconsin Glaciation. Rolling topography that was subglacially molded; contains streamlined landforms, including drumlins and flutes; many of these landforms are composed of stratified sand and gravel rather than Horicon till. | 004-003 | DMU2 | ghs | ghs | 186,207,175 | None | Waupaca_Quaternary_Mode_et_al_2023 | Glacial till, mostly sandy | Medium | DMU0025
26 | ghc | Collapsed till of the Horicon Member | Collapsed till of the Horicon Member of the Holy Hill Formation | Pleistocene | Brown to reddish-brown, gravelly, clayey, silty sand deposited by the Green Bay Lobe; generally at least 3 m thick; includes many small to large inclusions of windblown sediment, hillslope sediment, and glacial lake sediment that could not be separately mapped. In many areas, the modern surface reflects the landscape before the last part of the Wisconsin Glaciation. Collapsed till overlying meltwater-stream sediment. | 004-004 | DMU2 | ghc | ghc | 182,215,169 | fill overlaid by regular mesh resulting in medium, generally round areas of fill. Pattern covers approximately 50% of fill. | Waupaca_Quaternary_Mode_et_al_2023 | Glacial till, mostly sandy | Medium | DMU0026
27 | None | Bedrock | None | None | None | 005 | Heading2 | None | None | None | None | Waupaca_Quaternary_Mode_et_al_2023 | None | None | DMU0027
28 | r | Bedrock | Bedrock | Precambrian to Pleistocene | Dolomite, sandstone or granite; glacially scoured areas of bedrock near the ground surface covered by less than 1 m of glacial sediment. | 005-001 | DMU1 | r | r | 208,208,179 | None | Waupaca_Quaternary_Mode_et_al_2023 | Rock and sediment | High | DMU0028
29 | water | water | Water | N/A | water | 006 | DMU1 | None | None | 198,217,231 | None | Waupaca_Quaternary_Mode_et_al_2023 | Water or ice | High | DMU0029

#### Glossary

OBJECTID | Term | Definition | DefinitionSourceID | Glossary_ID
--- | --- | --- | --- | ---
1 | certain | Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation. | FGDC-STD-013-2006 | GLO0001
6 | contact | A plane or irregular surface between two types or ages of rock; examples are faults, intrusive borders, bedding planes separating distinct strata, and unconformities. | AGI_2005 | GLO0006
7 | cutbank | A local term in the Western U.S. for a steep bare slope formed by lateral erosion of a stream. | AGI_2005 | GLO0007
24 | DMU1 | Paragraph Style: Myriad Pro 9.5 font, with unit name in bold, followed by a period. Standalone unit, with no other units nested under it. | Waupaca_Quaternary_Mode_et_al_2023 | GLO0024
42 | DMU2 | Paragraph Style: Myriad Pro 9.5 font, with unit abbreviation in bold, followed by a period. Member of a grouped unit. | Waupaca_Quaternary_Mode_et_al_2023 | GLO0042
16 | drumlin | A low, smoothly rounded, elongate oval hill, mound, or ridge of compact glacial till or, less commonly, other kinds of drift (sandy till, varved clay), built under the margin of ice and shaped by its flow, or carved out of an older moraine by readvancing ice; its longer axis is parallel to the direction of movement of the ice. It usually has a blunt nose pointing in the direction from which the ice approached, and a gentler slope tapering in the other direction. | AGI_2005 | GLO0016
46 | escarpments or other steep slopes | Scarp: a relatively straight, clifflike face or slope of considerable linear extent, breaking the general continuity of the land by separating surfaces lying at different levels, as along the margin of a plateau or mesa. A scarp may be of any height but does not describe properly a slope of highly irregular outline. | AGI_2005 | GLO0046
19 | esker | A long, narrow, sinuous, steep-sided ridge composed of irregularly stratified sand and gravel that was deposited by a subglacial or englacial stream flowing between ice walls or in an ice tunnel of a stagnant or retreating glacier. | AGI_2005 | GLO0019
23 | Heading2 | Paragraph Style: Cambria, size 16 | Waupaca_Quaternary_Mode_et_al_2023 | GLO0023
53 | High | The selected term in the GeoMaterial field (and its definition) adequately characterizes1 the overall lithologic nature of rocks and (or) sediments in the map unit. | GeMS_2020 | GLO0053
5 | ice-contact face | Ice-contact slope: The steep slope of sediment that was deposited against a wall of glacier ice, marking the position of the ice margin (glacial boundary); an irregular scarp against which glacier ice once rested. | AGI_2005 | GLO0005
54 | ice-margin position | Ice-contact slope: The steep slope of sediment that was deposited against a wall of glacier ice, marking the position of the ice margin (glacial boundary); an irregular scarp against which glacier ice once rested. | AGI_2005 | GLO0054
9 | map boundary | Neat line: The line that surrounds a map, separating the map from the margin. | AGI_2005 | GLO0009
55 | Medium | The selected term in the GeoMaterial field (and its definition) generally characterizes the overall lithologic nature of rocks and (or) sediments in the map unit, but one or more significant but minor lithologies are not adequately described by the selected term. | GeMS_2020 | GLO0055
49 | meltwater channel | Meltwater: water derived from the melting of snow or ice, esp. the stream flowing in, under, or from melting glacier ice. | AGI_2005 | GLO0049
50 | moraine crest | Moraine: a mound, ridge, or other distinct accumulation of unsorted, unstratified glacial drift, prodominately till, deposited chiefly by direct action of glacier ice, in a variety of topographic landforms that are independent of the surface on which the drift lies. | AGI_2005 | GLO0050
2 | questionable | Identity of a feature cannot be determined using relevant observations and scientific judgment; therefore, one cannot be reasonably confident in the credibility of this interpretation. For example, IdentityConfidence = questionable is appropriate when a geologist reasons "I can see some kind of planar feature that separates map units in this outcrop, but I cannot be certain if it is a contact or a fault." | FGDC-STD-013-2006 | GLO0002
51 | sand dune | An accumulation of loose sand heaped up by the wind, commonly found along low-lying seashores above high-tide level, more rarely on the border of large lakes of river valleys, as well as in various desert regions, where abundant dry surface sand is present during some part of the year. | AGI_2005 | GLO0051
8 | shoreline | The intersection of a specified plane of water with the shore or beach; it migrates with changes of the tide or of the water level. | AGI_2005 | GLO0008

#### MiscellaneousMapInformation

OBJECTID | MapProperty | MapPropertyValue | MiscellaneousMapInformation_ID
--- | --- | --- | ---
1 | Report Title | Quaternary Geology of Waupaca County, Wisconsin | MMI0001
2 | Map Title | Quaternary Geology of Waupaca County, Wisconsin | MMI0002
3 | Publication Date | 2023 | MMI0003
4 | Scale | 1:100000 | MMI0004
5 | Authors | William N. Mode, Thomas S. Hooyer, John W. Attig, Lee Clayton, and J. Elmo Rawling, III | MMI0005
6 | Cartography by | D. L. Patterson and revised by Nick Rompa | MMI0006
7 | Publisher | Wisconsin Geological and Natural History Survey | MMI0007
8 | Series | Map Series | MMI0008
9 | Series Number | M509 | MMI0009

### Database Inventory

This summary of database content is provided as a convenience to GIS analysts, reviewers, and others. It is not part of the GeMS compliance criteria.
DataSources, nonspatial table, 4 rows
DescriptionOfMapUnits, nonspatial table, 29 rows
GeoMaterialDict, nonspatial table, 101 rows
Glossary, nonspatial table, 19 rows
MiscellaneousMapInformation, nonspatial table, 9 rows
GeologicMap, feature dataset
GeologicLines, simple polyline feature class, 746 rows
MapUnitPolys, simple polygon feature class, 1210 rows
ContactsAndFaults, simple polyline feature class, 2136 rows