## GeMS validation of Stitzer_Montfort_GeMS_final.gdb

File written by GeMS_ValidateDatabase.py, version of 8/29/2023
Fri Sep 8 14:00:16 2023
Runtime parameters
Database path: P:\Earth_MRI\SW_Wisconsin_project\gis\Cartography\GeMS_database\Stitzer_Montfort_GeMS_final.gdb
Output directory: P:\Earth_MRI\SW_Wisconsin_project\gis\Cartography\GeMS_database\Stitzer_Montfort_validation
Metadata file: P:\Earth_MRI\SW_Wisconsin_project\gis\Cartography\GeMS_database\Stitzer_Montfort_GeMS_final-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 Stitzer_Montfort_GeMS_final.gdb-ValidationErrors.html and Stitzer_Montfort_GeMS_final-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 1 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, LegendText
OrientationPoints, LegendText
OrientationPoints, FieldStratCode
OrientationPoints, FieldStratDesc
GeologicPoints, LegendText
GeologicPoints, FieldStratCode
GeologicPoints, FieldStratDesc
OverlayPolys, LegendText
IsoValueLines, LegendText

#### Tables

GeologicPoints

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

MapUnit | DescriptionOfMapUnits | GeologicMap
--- | --- | ---
Qlc | X | X
Qa | X | X
Opc | X | X
Qlb | X | X
Op | X | X
Og | X | X
Qlcb | X | X
Oa | X | X
Od | X | X
Qc | X | X

### Contents of Nonspatial Tables

#### DataSources

OBJECTID | Source | Notes | URL | DataSources_ID
--- | --- | --- | --- | ---
4 | Neuendorf, Klaus; Mehl, James P., Jr; and Jackson, Julia A., eds., 2005, Glossary of geology (fifth ed.): Alexandria, VA, American Geosciences Institute, 779 p. | None | https://www.americangeosciences.org | 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
3 | Carlson, J.E., 1961, Geology of the Montfort and Linden Quadrangles, Wisconsin, in Geology of parts of the Upper Mississippi Valley zinc-lead district: U.S. Geological Survey Bulletin 1123–B, p. 95–138, 2 pls., scale 1:24,000 | None | https://doi.org/10.3133/b1123B | Montfort_Linden_Geology_Carlson_1961
2 | This report, Stewart, E.D., Mauel, S.W., and Batten, W.G., 2023, Geologic map of the Stitzer and western part of the Montfort 7.5-minute quadrangles, Grant County, Wisconsin: Wisconsin Geological and Natural History Survey Open-File Report 2023–03, 1 pl., scale 1:24,000. | None | https://doi.org/10.54915/icay3440 | Stitzer_Montfort_Geology_Stewart_2023

#### DescriptionOfMapUnits

OBJECTID | MapUnit | Name | FullName | Age | Description | HierarchyKey | ParagraphStyle | Label | Symbol | AreaFillRGB | AreaFillPatternDescription | DescriptionSourceID | GeoMaterial | GeoMaterialConfidence | DescriptionOfMapUnits_ID
--- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | --- | ---
1 | None | Map Units | None | None | None | 000 | Heading1 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU1
2 | None | Cenozoic | None | None | None | 001 | Heading2 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU2
3 | None | Quaternary | None | None | Quaternary units were mapped where estimated thicknesses exceed 3 m (10 feet). Most Quaternary unit descriptions follow Stewart and others (2022a). Windblown deposit units were updated based on E. Carson (pers. comm.) | 001-001 | Heading3 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU3
4 | None | Alluvium | None | None | None | 001-001-001 | Heading4 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU4
5 | Qa | Alluvium | Quaternary, alluvium | Quaternary | Well-sorted Holocene and Pleistocene sand, silt, and mud. Deposited as overbank deposits in modern valleys. Cobble beds are uncommon, but can be found in river valleys where adjacent hillslopes are draped by colluvial deposits. | 001-001-001-001 | DMU1 | Qa | Qa | 224,214,202 | None | Stitzer_Montfort_Geology_Stewart_2023 | Clastic sediment | High | DMU5
6 | None | Colluvium | None | None | None | 001-001-002 | Heading4 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU6
7 | Qc | Colluvium | Quaternary, colluvium | Quaternary | Angular, poorly sorted boulders, cobbles, sand, and silt. Deposited at the base and lower reaches of valley slopes from gravity-driven mass wasting, soil creep, and non-channelized overland flow. The unit tends to fine towards the valley bottoms, and can interfinger with alluvium. Thicknesses are generally in excess of 3 m (10 ft), but rapid changes are likely due to an uneven bedrock surface. | 001-001-002-001 | DMU1 | Qc | Qc | 236,220,172 | None | Stitzer_Montfort_Geology_Stewart_2023 | Colluvium and other widespread mass-movement sediment | High | DMU7
8 | None | Windblown deposits | None | None | None | 001-001-003 | Heading4 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU8
9 | Qlc | Undivided loess over carbonate rocks | Quaternary, undivided loess over carbonate rocks | Quaternary | Windblown deposits of very fine sand, silt, and clay. May include parts of the Roxana and Peoria Members of the Kieler Formation, a loess formation. Loess is present on upland surfaces, and is generally thicker on broad plateaus than narrow ridges. Undivided loess over carbonate rocks. The Rountree Formation, formed from the surface weathering of carbonate rocks, is probably discontinuously present beneath the loess. | 001-001-003-001 | DMU1 | Qlc | Qlc | 224,216,183 | None | Stitzer_Montfort_Geology_Stewart_2023 | Loess | High | DMU9
10 | Qlb | Undivided loess over siliciclastic bedrock | Quaternary, undivided loess over siliciclastic bedrock | Quaternary | Windblown deposits of very fine sand, silt, and clay. May include parts of the Roxana and Peoria Members of the Kieler Formation, a loess formation. Loess is present on upland surfaces, and is generally thicker on broad plateaus than narrow ridges. Undivided loess over siliciclastic bedrock. | 001-001-003-002 | DMU1 | Qlb | Qlb | 239,244,216 | None | Stitzer_Montfort_Geology_Stewart_2023 | Loess | High | DMU10
11 | Qlcb | Undivided loess over mixed carbonate and siliciclastic bedrock | Quaternary, undivided loess over mixed carbonate and siliciclastic bedrock | Quaternary | Windblown deposits of very fine sand, silt, and clay. May include parts of the Roxana and Peoria Members of the Kieler Formation, a loess formation. Loess is present on upland surfaces, and is generally thicker on broad plateaus than narrow ridges. Undivided loess over mixed carbonate and siliciclastic bedrock. | 001-001-003-003 | DMU1 | Qlcb | Qlcb | 239,231,203 | None | Stitzer_Montfort_Geology_Stewart_2023 | Loess | High | DMU11
12 | None | Paleozoic | None | None | Paleozoic bedrock units were mapped where bedrock is estimated to be within 3 m (10 ft) of land surface. Within Paleozoic units, outcrops are generally discontinuous at the surface. Stratigraphic units use the classfication scheme of Agnew and others (1956), which has diferent divisions for the Sinnipee Group than Wisconsin Geological and Natural History Survey (2011). Unit descriptions generally follow Stewart and others (2022a). Carbonate units follow the classification of Dunham (1962). | 002 | Heading2 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU12
13 | None | Ordovician | None | None | None | 002-001 | Heading3 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU13
14 | None | Galena Formation | None | None | None | 002-001-001 | Heading4 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU14
15 | Og | Galena Formation | Galena Formation of the Sinnipee Group | Ordovician | Tan to gray, vuggy dolomite. Thin- to medium-bedded. The upper Galena Formation is composed of granular, sandy dolomite, but is not exposed in the map area. The lower approximately 36.5 m (120 ft) of the Galena Formation contains sandy dolomite with interbedded gray chert. Receptaculites is common in the lower Galena. At the surface, the dolomite often weathers into a distinctive honeycomb appearance. Honeycomb weathering is thought to result from preferred dissolution and weathering of Thalassinoides burrows (Dockal, 2021; Stewart and others, 2022b). Though the entire section is not exposed in the map area, the full thickness of the Galena Formation elsewhere ranges from approximately 70–76 m (230–250 ft). | 002-001-001-001 | DMU1 | Og | Og | 199,133,154 | None | Stitzer_Montfort_Geology_Stewart_2023 | Dolomite | Medium | DMU15
16 | None | Decorah Formation | None | None | None | 002-001-002 | Heading4 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU16
17 | Od | Decorah Formation | Decorah Formation of the Sinnipee Group | Ordovician | The Decorah Formation contains the upper Ion Member, the middle Guttenburg Member, and the basal Spechts Ferry Member. The Ion Member contains thin- to medium-bedded gray dolomitic mudstone and wackestone. Shale partings are common, and they define bedsets in the field. The Guttenburg Member is composed of 0.5–10 cm (0.2–2.4 in) thick gray to tan mottled mudstone to wackestone with interbedded chocolate brown to gray shaley mudstone around 1 cm (0.4 in) thick. The Spechts Ferry Member contains green-blue laminated, fissile shale with subordinate interbedded gray limestone and dolostone. The Spechts Ferry Member is around 0.6–0.9 m (2–3 ft) thick in the Stitzer and Montfort area, but thickens westward to around 2.6 m (8.5 ft) at the type section in Dubuque County, Iowa (Kay, 1929). The Decorah Formation contains abundant brachiopod fossils throughout. The Decorah Formation is around 9–12 m thick (30–40 ft). | 002-001-002-001 | DMU1 | Od | Od | 214,157,193 | None | Stitzer_Montfort_Geology_Stewart_2023 | Mostly carbonate rock | Medium | DMU17
18 | None | Platteville Formation | None | None | None | 002-001-003 | Heading4 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU18
19 | Op | Platteville Formation | Platteville Formation of the Sinnipee Group | Ordovician | The Platteville Formation contains the upper Quimbys Mill Member, the middle McGregor Member, and the basal Pecatonica Member. The Quimbys Mill Member contains thin-bedded, fine-grained gray to brown mudstone. The mudstone fractures conchoidally, which helps distinguish the unit. Millimeter to centimeter thick brown shale partings and interbeds define bedsets. The McGregor Member contains thin-bedded gray wackestone interbedded with dark gray, shaley mudstone. Bedding is wavy and mottled. Brachiopods are common. The Pecatonica Member is a tan to gray, thin- to medium-bedded dolomitic mudstone to wackestone. Bedding is typically tabular. The total thickness of the Platteville Formation is approximately 15 m (50 ft). | 002-001-003-001 | DMU1 | Op | Op | 208,176,184 | None | Stitzer_Montfort_Geology_Stewart_2023 | Carbonate rock | Medium | DMU19
20 | None | Ancell Group | None | None | None | 002-001-004 | Heading4 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU20
21 | Oa | Ancell Group | Ancell Group | Ordovician | The Ancell Group includes the Glenwood Formation and the St. Peter Formation. The Glenwood Formation is a light to dark green, fissile shale 0.6-1 m thick. The underlying St. Peter Formation contains the upper Tonti Member and the basal Readstown Member. The Tonti member is a clean, tan to white, fine- to medium-grained quartz arenite. Bedding ranges from thin to medium. Large cross-beds are common. Near the contact with the Glenwood, the Tonti is cemented with iron sulfides and carbonate. The Readstown Member is poorly exposed in the Stitzer and Montfort areas, but elsewhere it contains interbedded white to tan, fine-grained quartz arenite and mottled, maroon to green shale. Soft-sediment deformation is common. The base of the Readstown forms an unconformity with the underlying Prairie du Chien Group. The thickness of the St. Peter Formation is variable, but the combined Ancell-Prairie du Chien thickness in southwest Wisconsin is around 82–98 m (270–320 ft) (Agnew and others, 1956). | 002-001-004-001 | DMU1 | Oa | Oa | 188,149,158 | None | Stitzer_Montfort_Geology_Stewart_2023 | Mostly sandstone | Medium | DMU21
22 | None | Prairie du Chien Group | None | None | None | 002-001-005 | Heading4 | None | None | None | None | Stitzer_Montfort_Geology_Stewart_2023 | None | None | DMU22
23 | Opc | Prairie du Chien Group | Prairie du Chien Group | Ordovician | The Prairie du Chien Group in the Stitzer and Montfort area is largely composed of the Oneota Formation. The Oneota Formation is generally a tan to gray, thin- to thick-bedded, fine-grained dolostone. Vugs and chert are common. Fine-grained micrite and stromatolites occur locally. The base of the Prairie du Chien Group is not exposed in the map area. | 002-001-005-001 | DMU1 | Opc | Opc | 246,211,216 | None | Stitzer_Montfort_Geology_Stewart_2023 | Mostly carbonate rock | Medium | DMU23

#### Glossary

OBJECTID | Term | Definition | DefinitionSourceID | Glossary_ID
--- | --- | --- | --- | ---
6 | anticline | A fold, generally convex upward, whose core contains the stratigraphically older rocks. | AGI_2005 | GLO6
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 | GLO1
8 | 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 | GLO8
2 | cross section | A diagram or drawing that shows features transected by a given plane; specifically a vertical section drawn at right angles to the longer axis of a geologic feature, such as the trend of an orebody, the mean direction of flow of a stream, or the axis of a fossil. | AGI_2005 | GLO2
23 | DMU1 | Paragraph style: Myriad Pro; 9.25 pt, black | Stitzer_Montfort_Geology_Stewart_2023 | GLO23
9 | fault | A discrete surface or zone of discrete surfaces separating two rock masses across which one mass has slid past the other. | AGI_2005 | GLO9
12 | geologic log | Subsurface: The zone below the surface, whose geologic features, principally stratigraphic and sturctural, are interpreted on the basis of drill records and various kinds of geophysical evidence. | AGI_2005 | GLO12
19 | Heading1 | Paragraph style: Myriad Pro; 14 pt; bold; all caps; black | Stitzer_Montfort_Geology_Stewart_2023 | GLO19
20 | Heading2 | Paragraph style: Myriad Pro; 18 pt; bold; all caps; dark tan (RGB 136,118,107) | Stitzer_Montfort_Geology_Stewart_2023 | GLO20
21 | Heading3 | Paragraph style: Myriad Pro; 18 pt; narrow; all caps; dark tan (RGB 136,118,107) | Stitzer_Montfort_Geology_Stewart_2023 | GLO21
22 | Heading4 | Paragraph style: Myriad Pro; 15 pt; narrow; title case; olive green (RGB 134,142,99) | Stitzer_Montfort_Geology_Stewart_2023 | GLO22
17 | High | The selected term in the GeoMaterial field (and its definition) adequately characterizes the overall lithologic nature of rocks and (or) sediments in the map unit. | AGI_2005 | GLO17
14 | inclined bedding | Strike: The direction or trend taken by a structural surface, e.g., a bedding or fault plane, as it intersects the horizontal. Dip: The maxiumum angle that a structural surface, e.g., bedding or fault plane, makes with the horizontal; measured perpendicular to the strike of the structure and in the vertical plane. Bedding surface: A surface, usually conspicuous, within a mass of stratified rocks, representing an original surface of deposition; the surface of separation or interface between two adjacent beds of sedimentary rock. | AGI_2005 | GLO14
15 | inclined joint | Strike: The direction or trend taken by a structural surface, e.g., a bedding or fault plane, as it intersects the horizontal. Dip: The maxiumum angle that a structural surface, e.g., bedding or fault plane, makes with the horizontal; measured perpendicular to the strike of the structure and in the vertical plane. Joint: A planar fracture, crack, or parting in a rock, without shear displacement; the surface is usually decorated with a plumose structure. Often occurs with parallel joints to form part of a joint set. | AGI_2005 | GLO15
4 | map boundary | Neat line: The line that surrounds a map, separating the map from the margin. | AGI_2005 | GLO4
18 | 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 | GLO18
11 | mine | An underground excavation for the extraction of mineral deposits, in contrast to surficial excavations such as quarries. The term is also applied to various types of open-pit workings. | AGI_2005 | GLO11
24 | mineralized rock | Mineralization: The process or processes by which a mineral or minerals are introduced into a rock, resulting in a valuable or potentially valuable deposit. It is a general term, incorporating various types, e.g. fissure filling, impregnation, replacement. | AGI_2005 | GLO24
10 | outcrop | That part of a geologic formation or structure that appears at the surface of the Earth. | AGI_2005 | GLO10
3 | quadrangle boundary | Quadrangle: A rectangular area bounded by parallels of latitude and medians of longitude, used as a unit in systemic mapping. The dimensions of a quadrangle are not necessarily the same in both directions, and its size and the scale at which it is mapped are determined by the prime purpose of the map. | AGI_2005 | GLO3
5 | structure contour | Bedrock: A general term for the rock, usually solid, that underlies soil or other unconsolidated, superficial material. Surface: A two-dimensional boundary between geologic features such as formations or structures, including bedding surface and fault surface, or an imaginary surface such as a the axial surface of a fold; usually an internal boundary, rather than one occurring on the outside of a feature (Challinor, 1978, p. 302) Contour: An imaginary line, or a line on a map or chart, that connects points of equal elevation of the land surface above or below some reference value or datum plane, generally sea level. Value and ValueConfidence are in feet. | AGI_2005 | GLO5
7 | syncline | A fold of which the core contains the stratigraphically younger rocks; it is generally concave upward. | AGI_2005 | GLO7
16 | vertical joint | Strike: The direction or trend taken by a structural surface, e.g., a bedding or fault plane, as it intersects the horizontal. Joint: A planar fracture, crack, or parting in a rock, without shear displacement; the surface is usually decorated with a plumose structure. Often occurs with parallel joints to form part of a joint set. | AGI_2005 | GLO16
13 | well | An artificial excavation (pit, hole, tunnel), generally cylindrical in form and often walled in, sunk (drilled, dug, driven, bored, or jetted) into the ground to such a depth as to penetrate water-yielding rock or soil and to allow the water to flow or be pumped to the surface. | AGI_2005 | GLO13

#### MiscellaneousMapInformation

OBJECTID | MapProperty | MapPropertyValue | MiscellaneousMapInformation_ID
--- | --- | --- | ---
1 | Report Title | Geologic map of the Stitzer and western part of the Montfort 7.5-minute quadrangles, Grant County, Wisconsin | MMI1
2 | Map Title | Geologic map of the Stitzer and western part of the Montfort 7.5-minute quadrangles, Grant County, Wisconsin | MMI2
3 | Publication Date | 2023 | MMI3
4 | Scale | 1:24000 | MMI4
5 | Authors | E. D. Stewart, S. W. Mauel, W. G. Batten | MMI5
6 | Cartography by | Stephen Mauel and Eric Stewart | MMI6
7 | Publisher | Wisconsin Geological and Natural History Survey | MMI7
8 | Series | Open-File Report | MMI8
9 | Series Number | 2023-3 | MMI9

### 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, 23 rows
GeoMaterialDict, nonspatial table, 101 rows
Glossary, nonspatial table, 24 rows
MiscellaneousMapInformation, nonspatial table, 9 rows
GeologicMap, feature dataset
MapUnitPolys, simple polygon feature class, 449 rows
ContactsAndFaults, simple polyline feature class, 695 rows
CartographicLines, simple polyline feature class, 2 rows
OrientationPoints, simple point feature class, 137 rows
GeologicPoints, simple point feature class, 455 rows
OverlayPolys, simple polygon feature class, 69 rows
IsoValueLines, simple polyline feature class, 152 rows
GeologicMap_topology, topology