## GeMS validation of B118-dataset01.gdb

Database path: \\m-s-storage01.wgnhs.wisc.edu\Projects\Jefferson_Quaternary\GIS\Jeff_Quat_GeMS_Converson\Jefferson_Co_Quaternary_Final\USGS_Recommendation\B118-dataset01\B118-dataset01-publication\B118-dataset01-database\B118-dataset01.gdb
File written by GeMS_ValidateDatabase_AGP2.py, version of 18 April 2022
Thu Oct 20 10:31:19 2022
This file should be accompanied by B118-dataset01.gdb-ValidationErrors.html, B118-dataset01.gdb-vFgdcMetadata.txt, and B118-dataset01.gdb-vFgdcMetadataErrors.txt, all in the same directory.
This database is LEVEL 3 COMPLIANT, pending completion of a peer-reviewed Geologic Names report that includes identification of any suggested modifications to Geolex. The database-level FGDC metadata are formally correct. The metadata record should be examined by a human to verify that it is meaningful.
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### Contents

Compliance Criteria
Content not specified in GeMS schema
MapUnits in DescriptionOfMapUnits table, GeologicMap feature dataset, and other feature datasets
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 GeologicMap topology: 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 conform to GeMS schema | PASS
3.2 All map-like feature datasets obey topology rules. No MapUnitPolys gaps or overlaps. No ContactsAndFaults overlaps, self-overlaps, or self-intersections. MapUnitPoly boundaries covered by ContactsAndFaults | 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 or whitespace-only strings | PASS

There are 8 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.
DataSources, field URL_1
DescriptionOfMapUnits, field LegendDescription
DescriptionOfMapUnits, field LegendBlock
Glossary, field TermSrcFld
Glossary, field TermSrcFC
ContactsAndFaults, field MapText
TextFile 00log.txt
Topology GeologicMap_topology
GeologicLines, field MapText
FeatureClass GeologicPoints
OrientationPoints, field MapText

### MapUnits in DescriptionOfMapUnits table, GeologicMap feature dataset, and other feature datasets

MapUnit | DMU | GeologicMap
--- | --- | ---
sm | X | X
ol | X | X
os | X | X
lf | X | X
ln | X | X
lc | X | X
su | X | X
sc | X | X
gr | X | X
gs | X | X
gb | X | X
gm | X | X
suk | X | X
sck | X | X
w | X | X

### Contents of Nonspatial Tables

#### DataSources

OBJECTID | Source | Notes | URL | URL_1 | _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. | --- | --- | --- | AGI_2005
6 | Colgan, Patrick M. Glacial Landforms of the Southern Green Bay Lobe, Southeastern Wisconsin. 2003. Miscellaneous Map 52. Wisconsin Geological and Natural History Survey. Scale 1:250,000. | --- | https://wgnhs.wisc.edu/catalog/publication/000456 | --- | Colgan_2003
12 | Colgan, Patrick M. Glacial Landforms of the Southern Green Bay Lobe, Southeastern Wisconsin. 2003. Miscellaneous Map 52. Wisconsin Geological and Natural History Survey. Scale 1:250,000.; Ives, Libby R.W.; Rawling, J. Elmo III. Quaternary Geology of Jefferson County, Wisconsin. 2022. *Publicatoin number*-plate01. Wisconsin Geological and Natural History Survey. Plate 1. Scale 1:100,000. | --- | https://wgnhs.wisc.edu/catalog/publication/000456 | --- | Colgan_2003; Jefferson_Quaternary_Ives_Rawling_2022
8 | Clayton, Lee; Attig, John. Pleistocene Geologic Map of Dane County, Wisconsin. 1997. B095. Wisconsin Geological and Natural History Survey. | --- | https://wgnhs.wisc.edu/catalog/publication/000119 | --- | Dane_Pleistocene_Clayton_Attig_1997
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. | --- | https://ngmdb.usgs.gov/fgdc_gds/geolsymstd.php | --- | FGDC-STD-013-2006
3 | Ives, Libby R.W.; Rawling, J. Elmo III. Quaternary Geology of Jefferson County, Wisconsin. 2022. Bulletin 188-plate01. Wisconsin Geological and Natural History Survey. Scale 1:100,000 | --- | --- | --- | Jefferson_Quaternary_Ives_Rawling_2022
10 | Soil Survey Staff, Natural Resources Conservation Service, United States Department of Agriculture. Soil Survey Geographic (SSURGO) Database for Wisconsin Survey Area. Available online. Accessed 06/2021.; Ives, Libby R.W.; Rawling, J. Elmo III. Quaternary Geology of Jefferson County, Wisconsin. 2022. *Publicatoin number*-plate01. Wisconsin Geological and Natural History Survey. Plate 1. Scale 1:100,000. | --- | https://websoilsurvey.sc.egov.usda.gov/App/HomePage.htm | --- | SSURGO; Jefferson_Quaternary_Ives_Rawling_2022
11 | Soil Survey Staff, Natural Resources Conservation Service, United States Department of Agriculture. Soil Survey Geographic (SSURGO) Database for Wisconsin Survey Area. Available online. Accessed 06/2021.; Milfred, Clarence J., Hole, Francis D. Soils of Jefferson County, Wisconsin. 1970. Bulletin 86, Soil Series No. 61. Wisconsin Geological and Natural History Survey. 172 p., 1 plate. | --- | https://websoilsurvey.sc.egov.usda.gov/App/HomePage.htm | https://wgnhs.wisc.edu/catalog/publication/000110 | SSURGO; Milfred_Hole_1970

#### DescriptionOfMapUnits

OBJECTID | MapUnit | Name | FullName | Age | Description | LegendDescription | HierarchyKey | ParagraphStyle | LegendBlock | Label | Symbol | AreaFillRGB | AreaFillPatternDescription | DescriptionSourceID | GeoMaterial | GeoMaterialConfidence | _ID
--- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | ---
1 | --- | Nonglacial sediment | --- | --- | --- | --- | 001 | Heading2-1A | 1 | --- | --- | --- | --- | Jefferson_Quaternary_Ives_Rawling_2022 | --- | --- | DMU0001
2 | sm | Modern stream sediment | Modern stream sediment | Holocene | Sand, gravel, and silt deposited by postglacial (mostly Holocene) streams. Landforms include the active channels, inactive channels, terraces, and floodplains of modern rivers and streams. Holocene organic sediment overlies stream sediment in some areas. | Sand, gravel, and silt deposited by postglacial (mostly Holocene) streams. Landforms include the active channels, inactive channels, terraces, and floodplains of modern rivers and streams. Holocene organic sediment overlies stream sediment in some areas. | 001-001 | standaloneunit | 1 | sm | sm | 255 241 192 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Alluvial sediment, mostly coarse-grained | Medium | DMU0002
3 | ol | Organic sediment overlying lake sediment | Organic sediment overlying lake sediment | Pleistocene and Holocene | Organic sediment two or more meters thick occupying low-lying, flat to low-relief areas that are typically wetlands. Many areas have been drained to increase arability. Probable locations of lakes during the late Pleistocene and early to middle Holocene. | Organic sediment two or more meters thick occupying low-lying, flat to low-relief areas that are typically wetlands. Many areas have been drained to increase arability. Probable locations of lakes during the late Pleistocene and early to middle Holocene. | 001-002 | standaloneunit-1A | 1 | ol | ol | 148 178 199 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Peat and muck | Medium | DMU0003
4 | os | Organic sediment overlying meltwater-stream sediment | Organic sediment overlying meltwater-stream sediment | Pleistocene and Holocene | Organic sediment two or more meters thick occupying low-lying, flat to low-relief areas that are typically wetlands. | Organic sediment two or more meters thick occupying low-lying, flat to low-relief areas that are typically wetlands. | 001-003 | standaloneunit-1A | 1 | os | os | 199 130 109 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Peat and muck | Medium | DMU0004
5 | --- | Holy Hill Formation | --- | --- | --- | --- | 002 | Heading2-1A | 1 | --- | --- | --- | --- | Jefferson_Quaternary_Ives_Rawling_2022 | --- | --- | DMU0005
6 | --- | Horicon Member | --- | --- | --- | --- | 002-001 | Heading3 | 1 | --- | --- | --- | --- | Jefferson_Quaternary_Ives_Rawling_2022 | --- | --- | DMU0006
7 | --- | Lake sediment | --- | --- | --- | Laminated, thinly bedded, or massive fine sand, silt, and clay. Contains occasional medium sand, organic-rich laminae, and rare outsized clasts. | 002-001-001 | superunit | 1 | --- | --- | --- | --- | Jefferson_Quaternary_Ives_Rawling_2022 | --- | --- | DMU0007
8 | lf | Offshore lake sediment | Offshore lake sediment of the Horicon Member of the Holy Hill Formation | Pleistocene | Laminated, thinly bedded, or massive fine sand, silt, and clay. Contains occasional medium sand, organic-rich laminae, and rare outsized clasts. Flat to low-relief lake plains. Thickest and most extensive in areas that overlie bedrock valleys, but also occurs as terraces (elevated lake plains) adjacent to outwash. | Flat to low-relief lake plains. Thickest and most extensive in areas that overlie bedrock valleys, but also occurs as terraces (elevated lake plains) adjacent to outwash. | 002-001-001-002 | subunit | 1 | lf | lf | 169 193 210 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Lacustrine sediment, mostly fine-grained | High | DMU0008
9 | ln | Nearshore lake sediment | Nearshore lake sediment of the Horicon Member of the Holy Hill Formation | Pleistocene | Laminated, thinly bedded, or massive fine sand, silt, and clay. Contains occasional medium sand, organic-rich laminae, and rare outsized clasts. Medium to fine sand deposited in nearshore or shallow areas of former lake beds, commonly overlying laminated silt and clay. Occasionally merges with (or is clearly sourced from) colluvium or small deltas where stream paths intersect ancestral lake surfaces. Forms spits and beach ridges. | Medium to fine sand deposited in nearshore or shallow areas of former lake beds, commonly overlying laminated silt and clay. Occasionally merges with (or is clearly sourced from) colluvium or small deltas where stream paths intersect ancestral lake surfaces. Forms spits and beach ridges. | 002-001-001-003 | subunit | 1 | ln | ln | 161 160 195 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Lacustrine sediment, mostly coarse-grained | High | DMU0009
10 | lc | Collapsed lake sediment | Collapsed lake sediment of the Horicon Member of the Holy Hill Formation | Pleistocene | Laminated, thinly bedded, or massive fine sand, silt, and clay. Contains occasional medium sand, organic-rich laminae, and rare outsized clasts. Moderate-relief hummocky and pitted topography. Landscape morphology suggests collapse of the land surface into depressions created by the melting of stagnant or buried glacial ice. Typically occurs along the edges of lake terraces (elevated lake plains) adjacent to outwash plains. | Moderate-relief hummocky and pitted topography. Landscape morphology suggests collapse of the land surface into depressions created by the melting of stagnant or buried glacial ice. Typically occurs along the edges of lake terraces (elevated lake plains) adjacent to outwash plains. | 002-001-001-004 | subunit | 1 | lc | lc | 143 163 167 | "hummock" pattern - fill is overlaid by irregular mesh of fill color plus 10% -20% black (FGDC pattern 523-DO) | Jefferson_Quaternary_Ives_Rawling_2022 | Lacustrine sediment | High | DMU0010
11 | --- | Meltwater stream sediment | --- | --- | --- | Stratified sand and gravelly sand deposited by meltwater-streams. | 002-001-002 | superunit-1A | 1 | --- | --- | --- | --- | Jefferson_Quaternary_Ives_Rawling_2022 | --- | --- | DMU0011
12 | su | Uncollapsed meltwater stream sediment | Uncollapsed meltwater stream sediment of the Horicon Member of the Holy Hill Formation | Pleistocene | Stratified sand and gravelly sand deposited by meltwater-streams. Flat to low-relief topography with original depositional surface of outwash plains, outwash terraces, and outwash channels recognizable in most areas. | Flat to low-relief topography with original depositional surface of outwash plains, outwash terraces, and outwash channels recognizable in most areas. | 002-001-002-001 | subunit | 1 | su | su | 235 196 173 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Ice-contact and ice-marginal sediment, mostly coarse-grained | High | DMU0012
13 | sc | Collapsed meltwater stream sediment | Collapsed meltwater stream sediment of the Horicon Member of the Holy Hill Formation | Pleistocene | Stratified sand and gravelly sand deposited by meltwater-streams. Collapsed with moderate- to high-relief hummocky and pitted topography. Landscape morphology (for example, outwash plains, outwash terraces, and outwash channels) suggests collapse of the land surface into depressions created by the melting of stagnant and buried glacial ice. | Collapsed with moderate- to high-relief hummocky and pitted topography. Landscape morphology (for example, outwash plains, outwash terraces, and outwash channels) suggests collapse of the land surface into depressions created by the melting of stagnant and buried glacial ice. | 002-001-002-002 | subunit | 1 | sc | sc | 206 174 155 | "hummock" pattern - fill is overlaid by irregular mesh of fill color plus 10% -20% black (FGDC pattern 523-DO) | Jefferson_Quaternary_Ives_Rawling_2022 | Ice-contact and ice-marginal sediment, mostly coarse-grained | High | DMU0013
14 | --- | Glacial sediment | --- | --- | --- | Massive, poorly sorted, clast-rich, sandy, matrix-supported, and consolidated sediment interpreted as till of the Green Bay Lobe. Till is yellowish brown where oxidized and gray where reduced. Sediment is rich in local carbonate cobbles and boulders. Thickness is variable and may be as much as 20 m. | 002-001-003 | superunit-1A | 1 | --- | --- | --- | --- | Jefferson_Quaternary_Ives_Rawling_2022 | --- | --- | DMU0014
15 | gr | Rolling glacial sediment | Rolling glacial sediment of the Horicon Member of the Holy Hill Formation | Pleistocene | Massive, poorly sorted, clast-rich, sandy, matrix-supported, and consolidated sediment interpreted as till of the Green Bay Lobe. Till is yellowish brown where oxidized and gray where reduced. Sediment is rich in local carbonate cobbles and boulders. Thickness is variable and may be as much as 20 m.. Topography is most often rolling to flat but includes minor hummocky, pitted, or streamlined areas. | Topography is most often rolling to flat but includes minor hummocky, pitted, or streamlined areas. | 002-001-003-001 | subunit | 1 | gr | gr | 160 187 160 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Glacial till, mostly sandy | High | DMU0015
16 | gs | Streamlined glacial sediment | Streamlined glacial sediment of the Horicon Member of the Holy Hill Formation | Pleistocene | Massive, poorly sorted, clast-rich, sandy, matrix-supported, and consolidated sediment interpreted as till of the Green Bay Lobe. Till is yellowish brown where oxidized and gray where reduced. Sediment is rich in local carbonate cobbles and boulders. Thickness is variable and may be as much as 20 m. Topography is streamlined with drumlin height ranging from 1 to 20 m, length ranging from 100 to 2,900 m, and width ranging from 35 to 300 m. Low areas between drumlins may contain accumulated fine-grained and organic material deposited as colluvium or in standing water. | Topography is streamlined with drumlin height ranging from 1 to 20 m, length ranging from 100 to 2,900 m, and width ranging from 35 to 300 m. Low areas between drumlins may contain accumulated fine-grained and organic material deposited as colluvium or in standing water. | 002-001-003-002 | subunit | 1 | gs | gs | 199 225 197 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Glacial till, mostly sandy | High | DMU0016
17 | gb | Thin glacial sediment over bedrock | Thin glacial sediment over bedrock of the Horicon Member of the Holy Hill Formation | Pleistocene | Massive, poorly sorted, clast-rich, sandy, matrix-supported, and consolidated sediment interpreted as till of the Green Bay Lobe. Till is yellowish brown where oxidized and gray where reduced. Sediment is rich in local carbonate cobbles and boulders. Thickness is variable and may be as much as 20 m. Thin layer of till overlying bedrock with a high surface elevation. Bedrock is most often dolomite or limestone of the Sinnepee Group. Occurs adjacent to map units gr and gs. | Thin layer of till overlying bedrock with a high surface elevation. Bedrock is most often dolomite or limestone of the Sinnipee Group. Occurs adjacent to map units gr and gs. | 002-001-003-003 | subunit | 1 | gb | gb | 166 186 127 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Glacial till, mostly sandy | High | DMU0017
18 | gm | Glacial sediment of moraines | Glacial sediment of moraines of the Horicon Member of the Holy Hill Formation | Pleistocene | Massive, poorly sorted, clast-rich, sandy, matrix-supported, and consolidated sediment interpreted as till of the Green Bay Lobe. Till is yellowish brown where oxidized and gray where reduced. Sediment is rich in local carbonate cobbles and boulders. Thickness is variable and may be as much as 20 m. Less consolidated, unstratified, poorly sorted, gravelly, loamy sand deposited in hummocky areas of the moraines deposited during the Lake Mills phase. Moraine areas range in width from 200 to 850 m. Hummocky areas may or may not contain a distinct moraine ridge. | Less consolidated, unstratified, poorly sorted, gravelly, loamy sand deposited in hummocky areas of the moraines deposited during the Lake Mills phase. Moraine areas range in width from 200 to 850 m. Hummocky areas may or may not contain a distinct moraine ridge. | 002-001-003-004 | subunit | 1 | gm | gm | 135 107 143 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Glacial till, mostly sandy | Medium | DMU0018
19 | --- | Undifferentiated | --- | --- | --- | --- | 002-002 | Heading3-1A | 1 | --- | --- | --- | --- | Jefferson_Quaternary_Ives_Rawling_2022 | --- | --- | DMU0019
20 | --- | Kettle Moraine sediment | --- | --- | --- | Stratified sand, gravelly sand, and gravel deposited by meltwater streams in the Kettle Moraine. | 002-002-001 | superunit | 1 | --- | --- | --- | --- | Jefferson_Quaternary_Ives_Rawling_2022 | --- | --- | DMU0020
21 | suk | Uncollapsed meltwater-stream sediment in the Kettle Moraine | Uncollapsed meltwater-stream sediment in the Kettle Moraine of the Holy Hill Formation | Pleistocene | Stratified sand, gravelly sand, and gravel deposited by meltwater-streams in the Kettle Moraine. Flat to low-relief topography. Landforms include outwash plains, outwash terraces, or outwash channels. | Flat to low-relief topography. Landforms include outwash plains, outwash terraces, or outwash channels. | 002-002-001-001 | subunit | 1 | suk | suk | 214 150 129 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Ice-contact and ice-marginal sediment, mostly coarse-grained | High | DMU0021
22 | sck | Collapsed meltwater-stream sediment in the Kettle Moraine | Collapsed meltwater-stream sediment in the Kettle Moraine of the Holy Hill Formation | Pleistocene | Stratified sand, gravelly sand, and gravel deposited by meltwater-streams in the Kettle Moraine. Collapsed with moderate- to high-relief surfaces. Landscape morphology (for example, outwash plains, outwash terraces, and outwash channels) suggests collapse of land surface into depressions created by the melting of stagnant and buried glacial ice. Includes eskers and ice-walled lake plains. | Collapsed with moderate- to high-relief surfaces. Landscape morphology (for example, outwash plains, outwash terraces, and outwash channels) suggests collapse of land surface into depressions created by the melting of stagnant and buried glacial ice. Includes eskers and ice-walled lake plains. | 002-002-001-002 | subunit | 1 | sck | sck | 210 179 152 | "hummock" pattern - fill is overlaid by irregular mesh of fill color plus 10% -20% black (FGDC pattern 523-DO) | Jefferson_Quaternary_Ives_Rawling_2022 | Ice-contact and ice-marginal sediment, mostly coarse-grained | High | DMU0022
23 | w | water | water | N/A | water | water | 003 | N/A | 1 | w | w | 213 254 255 | --- | Jefferson_Quaternary_Ives_Rawling_2022 | Water or ice | High | DMU0023

#### Glossary

OBJECTID | Term | Definition | DefinitionSourceID | _ID | TermSrcFld | TermSrcFC
--- | --- | --- | --- | --- | --- | ---
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 | GLO0003 | --- | ---
37 | channel scar | Overflow channel: A channel or notch cut by the overflow waters of a lake, esp. the channel draining meltwater from a glacially dammed lake; an outlet of a proglacial lake. | AGI_2005 | GLO0014 | --- | ---
7 | 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 | GLO0005 | Type | ContactsAndFaults
38 | delta foreset face | Foreset bed: One of the inclined, internal, and systematically arranged layers of a cross-bedded unit; specif. one of the gently inclined layers of sandy material deposited upon or along an advancing and relatively steep frontal slope, such as the outer margin of a delta or the lee side of a dune, and progressively covering bottomset bed and in turn being covered or truncated by the topset bed. Foreset beds represent the greater part of the deposits of a delta. | AGI_2005 | GLO0015 | --- | ---
21 | 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 | GLO0010 | Type | GeologicLines
44 | drumlin; eroded, draped, or buried | Drumlin which has been eroded or where draped or buried by younger sediment. See also 'drumlin'. | Jefferson_Quaternary_Ives_Rawling_2022 | GLO0020 | --- | ---
25 | 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 | GLO0011 | Type | GeologicLines
45 | Heading2-1A | Paragraph Style: Cambria, size 16. Extra space added before text to properly align DMU entries ion plate "Explanation' section. | Jefferson_Quaternary_Ives_Rawling_2022 | GLO0021 | --- | ---
47 | Heading3 | Paragraph Style: Cambria, size 13. | Jefferson_Quaternary_Ives_Rawling_2022 | GLO0023 | --- | ---
46 | Heading3-1A | Paragraph Style: Cambria, size 13. Extra space added before text to properly align DMU entries ion plate "Explanation' section. | Jefferson_Quaternary_Ives_Rawling_2022 | GLO0022 | --- | ---
39 | 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. | AGI_2005 | GLO0016 | --- | ---
31 | ice-wedge polygon | A large, nonsorted polygon characterized by borders of intersecting ice wedges, found only in permafrost regions and formed by contraction of frozen ground. The fissured borders delineating the polygon may be ridges (low-centered polygon in which sediments are being upturned) or shallow troughs (high-centered polygon in which erosion and thawing are prevalent), and are underlain by ice wedges. Diameter: up to 150 m, averaging 10-40 m. In plan, the pattern tends to be three- to six-sided. | AGI_2005 | GLO0012 | Type | GeologicPoints
10 | map boundary | Neat line: The line that surrounds a map, separating the map from the margin. | AGI_2005 | GLO0007 | Type | ContactsAndFaults
41 | 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. | AGI_2005 | GLO0017 | --- | ---
20 | medium moraine | Conspicuous sharp-crested ridge that is narrower than about 200 m, but generally shows up on topographic maps; generally several tens of meters wide and a few meters to a few tens of meters high. | Dane_Pleistocene_Clayton_Attig_1997 | GLO0009 | Type | GeologicLines
53 | minor moraine | Low, obscure ridge that can be seen on aerial photographs, but is too small to be shown on topographic maps; generally several meters wide and no more than a few meters high. A symbol shown on the map may represent several small moraines that are too small to be shown individually at the scale of this map. | Dane_Pleistocene_Clayton_Attig_1997 | GLO0029 | --- | ---
32 | N/A | Paragraph Style: not applicable | Jefferson_Quaternary_Ives_Rawling_2022 | GLO0013 | --- | ---
43 | paleoshoreline | A low, essentially continuous mound of beach or beach-and-dune material (sand, gravel, shingle) on the backshore of a beach beyond the present limit of storm waves or the reach of ordinary tides, and occuring singly or as one of a series of approximately parallel deposits. The ridges are roughly parallel to the shoreline and represent successive positions of an advancing shoreline. | AGI_2005 | GLO0019 | --- | ---
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 | GLO0004 | --- | ---
54 | sediment core sample | Core: A full-diameter core is a cylindrical section of rock, usually 5-10 cm in diameter and up to several meters in length, taken as a sample of the interval penetrated by a core bit, and brought to the surface for geologic examination and/or laboratory analysis. | AGI_2005 | GLO0030 | --- | ---
9 | 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 | GLO0006 | Type | ContactsAndFaults
49 | standaloneunit | Paragraph Style: Unit name in Segoe UI, size 10, italic. Unit legend description in Segoe UI, size 10. | Jefferson_Quaternary_Ives_Rawling_2022 | GLO0025 | --- | ---
48 | standaloneunit-1A | Paragraph Style: Unit name in Segoe UI, size 10, italic. Unit legend description in Segoe UI, size 10. Extra space added before text to properly align DMU entries ion plate "Explanation' section. | Jefferson_Quaternary_Ives_Rawling_2022 | GLO0024 | --- | ---
42 | striation | One of a series of long, delicate, finely cut, commonly straight and parallel furrows or lines inscribed on a bedrock surface by the rasping and rubbing of rock fragments embedded at the base of a moving glacier, and usually oriented in the direction of ice movement; also formed on the rock fragments transported by the ice. | AGI_2005 | GLO0018 | --- | ---
50 | subunit | Paragraph Style: Unit symbol in Segoe UI, size 10, bold. Unit name in Segoe UI, size 10, italic. Unit legend description in Segoe UI, size 10. | Jefferson_Quaternary_Ives_Rawling_2022 | GLO0026 | --- | ---
52 | superunit | Paragraph Style: Superunit name in Segoe UI, size 10, bold. Superunit legend description in Segoe UI, size 10. | Jefferson_Quaternary_Ives_Rawling_2022 | GLO0028 | --- | ---
51 | superunit-1A | Paragraph Style: Superunit name in Segoe UI, size 10, bold. Superunit legend description in Segoe UI, size 10. Extra space added before text to properly align DMU entries ion plate "Explanation' section. | Jefferson_Quaternary_Ives_Rawling_2022 | GLO0027 | --- | ---

#### MiscellaneousMapInformation

OBJECTID | MapProperty | MapPropertyValue | _ID
--- | --- | --- | ---
1 | Report Title | Quaternary Geology of Jefferson County, Wisconsin | MMI0001
2 | Map Title | Quaternary Geology of Jefferson County, Wisconsin | MMI0002
3 | Publication Date | 2022 | MMI0003
4 | Scale | 1:100000 | MMI0004
5 | Authors | Libby R.W. Ives, J. Elmo Rawling III | MMI0005
6 | Cartography by | Nick Rompa, Caroline Rose | MMI0006
7 | Publisher | Wisconsin Geological and Natural History Survey | MMI0007
8 | Series | Bulletin | MMI0008
9 | Series Number | 118 | 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, 8 rows
DescriptionOfMapUnits, nonspatial table, 23 rows
GeoMaterialDict, nonspatial table, 101 rows
Glossary, nonspatial table, 27 rows
MiscellaneousMapInformation, nonspatial table, 9 rows
GeologicMap, feature dataset
ContactsAndFaults, polyline feature class, 1875 rows
GeologicLines, polyline feature class, 2281 rows
GeologicPoints, point feature class, 88 rows
MapUnitPolys, polygon feature class, 801 rows
OrientationPoints, point feature class, 8 rows