Database path: P:\690_StateMap2021\4_Heartland\deliverables\IN_2021_Indianapolis100k_2-0-Submittal\IN_2021_Indianapolis100k_2-0\IN_2021_Indianapolis100k_2-0-database\Indianapolis_BG_100k.gdb
File written by GeMS_ValidateDatabase_AGP2.py, version of 4 March 2023
Tue Aug 8 15:33:16 2023

This file should be accompanied by Indianapolis_BG_100k.gdb-ValidationErrors.html, Indianapolis_BG_100k.gdb-vFgdcMetadata.txt, and Indianapolis_BG_100k.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.

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
    MapInformation
Database Inventory

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 0 warnings

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.

    TableView MapInformation
    TextFile 00log.txt

MapUnit	DMU	GeologicMap
Pm	X	X
Mwb	X	X
Mbr	X	X
Ms	X	X
Mske	X	X
Mnp	X	X
DMnar	X	X
Dm	X	X
Sw	X	X
Spm	X	X

DataSources

OBJECTID	Source	Notes	URL	_ID
2	Hasenmueller, W. A., James, C. L. 2003, Bedrock geologic map of the Indianapolis 30 X 60 minute quadrangle, central Indiana: Indiana Geological Survey Open-File Study 03-07	Bedrock geologic map of the Indianapolis 30 X 60 minute quadrangle, central Indiana (2003)	https://igws.indiana.edu/bookstore/details.cfm?ItemID=1040&Pub_Num=OFS03%2D07	DAS1
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.	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

DescriptionOfMapUnits

OBJECTID	MapUnit	Name	FullName	Age	Description	HierarchyKey	ParagraphStyle	Label	Symbol	AreaFillRGB	AreaFillPatternDescription	DescriptionSourceID	GeoMaterial	GeoMaterialConfidence	_ID
39	---	Pennsylvanian	Pennsylvanian	Pennsylvanian	Pennsylvanian	1	Heading1	---	---	---	---	DAS1	---	---	DMU01
40	Pm	Mansfield Formation	Mansfield Formation of the Raccoon Creek Group	Pennsylvanian	Sandstone and shale with minor amounts of coal, underclay, and ironstone. The Mansfield Formation is the lowest formation in the Raccoon Creek Group, which consists of, in descending order, the Staunton, Brazil, and Mansfield Formations. The base of the Mansfield is a regional diachronous unconformity that includes networks of southwestward-trending paleovalleys with relief in excess of 100 feet. The Mansfield rests on the West Baden and Blue River Groups in the southwestern part of the map area and rocks of the Sanders and Borden Groups in the northwestern part of the map area. The full thickness of the Mansfield is not present in map area.	1-1	Normal	Pm	---	104,160,201	---	DAS1	Sandstone and mudstone	Medium	DMU02
41	---	Mississippian	Mississippian	Mississippian	Mississippian	2	Heading1	---	---	---	---	DAS1	---	---	DMU03
42	Mwb	West Baden Group	West Baden Group	Mississippian	Shale, sandstone, and limestone. The West Baden Group consists of five thin formations, in descending order these are the Elwren Formation, thin-bedded sandstones; Reelsville Limestone, thin-bedded gray micritic limestone; Sample Formation, shale; Beaver Bend Limestone, calcarenite; and Bethel Formation, shale and fine-grained sandstone. All West Baden formations are present in the map area but the full thickness of the group is not attained in the map area owing to erosion and the group's unconformable contact with the overlying Mansfield Formation.	2-1	Normal	Mwb	---	104,104,201	---	DAS1	Mostly mudstone	Medium	DMU04
43	Mbr	Blue River Group	Blue River Group	Mississippian	Limestone, dolomite, and minor amounts of shale, calcareous sandstone, and chert. The Blue River Group consists of three formations, in descending order these are the Paoli Limestone, thin-bedded calcarenite and fine-grained limestone; Ste. Genevieve Limestone, calcarenite and calcareous sandstone; and St. Louis Limestone, fine-grained cherty limestones and dolomites. The Blue River thickens southwestward in the map area. Recorded thickness of the Blue River Group ranges from 156 to 234 feet and averages 199 feet in the map area.	2-2	Normal	Mbr	---	202,205,210	---	DAS1	Carbonate rock	Medium	DMU05
44	Ms	Sanders Group	Sanders Group	Mississippian	Limestone, cherty limestone, dolomite, and impure carbonate. The Sanders Group consists of three formations, in descending order these are the Salem Limestone, massive and cross-bedded coarse-grained calcarenite; Harrodsburg Limestone, gray cherty calcarenite and fine-grained limestone; and Ramp Creek Formation, predominantly fine-grained cherty limestone and dolomite interbedded with shale. The Sanders thickens southwestward in the map area. Recorded thickness of the Sanders ranges from 76 to 175 feet and averages 126 feet In the map area.	2-3	Normal	Ms	---	128,145,172	---	DAS1	Carbonate rock	Medium	DMU06
45	Mske	Edwardsville and Spickert Knob Formations (Mississippian) undifferentiated	Edwardsville and Spickert Knob Formations of the Borden Group	Mississippian	Thin-, medium-, and thick-bedded siltstone, shale and fine-grained sandstone with minor amounts of limestone. The Edwardsville and Spickert Knob Formations are the uppermost formations in the Borden Group, which consists of the Edwardsville Formation, Spickert Knob Formation, and New Providence Shale, in descending order. The Edwardsville is difficult to distinguish from the uppermost beds of the underlying Spickert Knob where the basal member of the Edwardsville, the Floyds Knob Limestone Member, is missing. Such is the case in much of the map area. For that reason the Edwardsville and Spickert Knob are mapped as an undifferentiated unit. Recorded thickness of the undifferentiated Edwardsville/Spickert Knob ranges from 521 to 643 feet and averages 585 feet in the map area. The base of the Spickert Knob is typically a sharp contact between porous sandstones or siltstones at the base of the Spickert Knob to the New Providence shale in the map area. The contact between the top of the Edwardsville and overlying Ramp Creek Limestone is gradational.	2-4	Normal	Mske	---	153,174,195	---	DAS1	Clastic sedimentary rock	Medium	DMU07
46	Mnp	New Providence Shale	New Providence Shale of the Borden Group	Mississippian	Clay shale and silty shale. The New Providence Shale is the lowest formation in the Borden Group. The New Providence thins westward in the map area. Recorded thickness of the New Providence ranges from 23 to 227 feet and averages 142 feet in the map area. The contact between the New Providence and the overlying Spickert Knob Formation is typically an abrupt transition from shale to porous sandstone or siltstone in the map area. The contact between the New Providence and underlying Rockford Limestone or New Albany Shale typically is abrupt.	2-5	Normal	Mnp	---	178,181,199	---	DAS1	Mostly mudstone	Medium	DMU08
47	---	Mississippian-Devonian	Mississippian-Devonian	Mississippian-Devonian	Mississippian-Devonian	3	Heading1	---	---	---	---	DAS1	---	---	DMU09
48	DMnar	Rockford Limestone and New Albany Shale undifferentiated	Rockford Limestone and New Albany Shale undifferentiated of the Muscatatuck Group	Mississippian-Devonian	Organic-rich shale and minor amounts of impure limestone. The Rockford Limestone is a thin, persistent, impure limestone that rests conformably on the New Albany Shale. The Rockford and New Albany are not differentiated because the Rockford, which is rarely more than 10 feet thick, is too thin to map as a separate unit. The New Albany consists of brownish-black, carbon-rich shale, greenish-gray shale, and minor amounts of carbonate and quartz sandstone. The New Albany is divided into six irregularly developed members, in descending order these are the Ellsworth, Clegg Creek, Camp Run, Morgan Trail, Selmier, and Blocher Members. The undifferentiated Rockford/New Albany is thickest in the south-central part of the map area. Recorded thickness of the undifferentiated Rockford/New Albany ranges from 97 to 155 feet and averages 127 feet thick in the map area.	3-1	Normal	DMnar	---	126,124,185	---	DAS1	Mostly mudstone	Medium	DMU10
49	---	Devonian	Devonian	Devonian	Devonian	4	Heading1	---	---	---	---	DAS1	---	---	DMU11
50	Dm	Muscatatuck Group	Muscatatuck Group	Devonian	Limestone and dolomite. The Muscatatuck Group consists of two formations; these are, in descending order, the North Vernon Limestone and Jeffersonville Limestone. Muscatatuck formations were not mapped because they are thin and not well documented in the map area. Drillers' logs, especially older drillers' logs in the northeastern part of the map area refer to the Muscatatuck as the "Corniferous Limestone” and do not differentiate units within the Muscatatuck. The contact between the Muscatatuck and overlying New Albany Shale is an abrupt and possibly unconformable transition from limestone to black, organic-rich shale (Droste and Shaver, in Shaver and others, 1986, p. 99) that is well documented in drilling records in the map area. The contact between the Muscatatuck and underlying Silurian rocks is a diachronous regional unconformity. The Muscatatuck rests on the Wabash Formation throughout the map area. The Muscatatuck thickens southward in the map area. Recorded thickness of the Muscatatuck ranges from 86 to 155 feet end averages 115 feet thick in the map area.	4-1	Normal	Dm	---	202,189,219	---	DAS1	Carbonate rock	Medium	DMU12
51	---	Silurian	Silurian	Silurian	Silurian	5	Heading1	---	---	---	---	DAS1	---	---	DMU13
52	Sw	Wabash Formation	Wabash Formation of the Bainbridge or Salina Group	Silurian	Limestone, dolomite, and argillaceous or silty dolomite. The Wabash Formation is subdivided into two irregularly developed named members; these are, in descending order, Liston Creek Limestone and Mississinewa Shale Members. The upper contact of the Wabash Formation is a regional unconformity between Devonian and Silurian rocks. The Wabash thickens westward in the map area. Recorded thickness of the Wabash Formation ranges from 16 to 210 feet and averages 89 feet in the map area. The contact between the Wabash Formation and underlying Pleasant Mills Formation is conformable and gradational. The gradation from the Mississinewa Shale Member of the Wabash Formation to the Louisville Limestone Member of the Pleasant Mills Formation is generally an interval of several feet. Wabash boundaries are extrapolations where reef facies replace the above-mentioned members.	5-1	Normal	Sw	---	176,114,181	---	DAS1	Carbonate rock	Medium	DMU14
53	Spm	Pleasant Mills Formation	Pleasant Mills Formation of the Bainbridge of Salina Group	Silurian	Dolomite, limestone, and argillaceous dolomite. The Pleasant Mills Formation was proposed by Droste and Shaver (1982, p. 11– 17) to include, in descending order, the Louisville Limestone, Waldron Shale, and Limberlost Dolomite Members. It rarely is possible to differentiate the Limberlost Dolomite and underlying Salamonie Dolomite carbonates in the map area. The lithologic change that marks the base of the Waldron Shale Member of the Pleasant Mills Formation is distinct and commonly noted in drillers' logs and other geologic records from the map area; therefore, the Pleasant Mills Formation is herein restricted to the rocks from the top of the Louisville Limestone Member to the base of the Waldron Shale Member and the Limberlost Dolomite is assigned to the Salamonie Dolomite. Both the upper and lower contacts of the Pleasant Mills Formation, as herein defined, are conformable. The Pleasant Mills thickens northwestward in the map area. Recorded thickness of the Pleasant Mills ranges from 28 to 88 feet and averages 53 feet in the map area. Pleasant Mills boundaries are extrapolations where reef facies replace the above-mentioned members.	5-2	Normal	Spm	---	222,199,225	---	DAS1	Carbonate rock	Medium	DMU15

Glossary

OBJECTID	Term	Definition	DefinitionSourceID	_ID
3	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
7	contact	Plane or irregular surface between two types or ages of rock; outcrop of this plane on the mapped surface is a line.	FGDC-STD-013-2006	GLO2
6	fault	Planar surface of rupture along which geologic units have been fractured and then displaced	FGDC-STD-013-2006	GLO3
5	Heading1	Paragraph style: Bold + All caps	DAS1	GLO4
4	map boundary	Polyline showing mapping extent.	DAS1	GLO5
8	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.	DAS1	GLO6
9	Normal	Paragraph style: Normal + Indent: Left: 0.5"	DAS1	GLO7
10	structure contour, 1st surface	Showing altitude of top or base of, or hori-zon within, stratigraphic unit, aquifer, or confining bed—Accurately located	FGDC-STD-013-2006	GLO8
11	structure contour, 2nd surface	Showing altitude of top or base of, or hori-zon within, stratigraphic unit, aquifer, or confining bed—Accurately located	FGDC-STD-013-2006	GLO9

MapInformation

OBJECTID	MapProperty	MapPropertyValue	_ID
1	title	Bedrock Geologic Map of the Indianapolis 30 x 60 Minute Quadrangle, Central Indiana	X1X01
2	author	Walter A. Hasenmueller	X1X02
3	date	---	X1X03
4	introduction	---	X1X04
5	cartographer	Casey Jones	X1X05
6	scale	1:100,000	X1X06
7	Acknowledgements and Disclaimer	This geologic map was funded in part through the STATEMAP Program supported by the U.S. Geological Survey under Cooperative Agreement No. G21AC10646. The cooperative agreement requires the following statements: “This map and explanatory information is submitted for publication with the understanding that the United States Government is authorized to reproduce and distribute reprints for governmental use,” and “The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government.” This map was compiled by Indiana University, Indiana Geological and Water Survey, using data believed to be accurate; however, a degree of error is inherent in all data. This product is distributed “AS-IS” without warranties of any kind, either expressed or implied, including but not limited to warranties of suitability to a particular purpose or use. No attempt has been made in either the design or production of these data to define the limits or jurisdiction of any federal, state, or local government. These data are intended for use only at the published scale or smaller and are for reference purposes only. They are not to be construed as a legal document or survey instrument. A detailed, on-the-ground survey and historical analysis of a single site may differ from these data. LIMITATION OF WARRANTIES AND LIABILITY: Except for the expressed warranty above, the product is provided “AS-IS”, without any other warranties or conditions, expressed or implied, including, but not limited to, warranties for product quality, or suitability to a particular purpose or use. The risk or liability resulting from the use of this product is assumed by the user. Indiana University, Indiana Geological and Water Survey shares no liability with product uses indirect, incidental, special, or consequential damages whatsoever, including, but not limited to, loss of revenue or profit, lost or damaged data or other commercial or economic loss. Indiana University, Indiana Geological and Water Survey is not responsible for claims by a third party. The maximum aggregate liability to the original purchaser shall not exceed the amount paid by you for the product.	X1X07
8	igwsDirector	Todd A. Thompson, State Geologist	X1X08
9	ijesDoi	https://doi.org/10.14434/ijes.XXXX.xxxxx	X1X09
10	address	1001 E 10th St, Bloomington , IN 47405-1405	X1X10
11	phone	8128557636	X1X11
12	email	igwsinfo@indiana.edu	X1X12
13	url	igws.indiana.edu	X1X13
14	map information	Disturbed land from Indiana Department of Natural Resources, Division of Reclamation Coal Mine Information System. Transportation network © OpenStreetMap. Hydrography from U.S. Geological Survey National Hydrography Dataset - Small Scale. Projection: Universal Transverse Mercator (UTM), Zone 16N. Horizontal Datum: North American Datum of 1983 (NAD83).	X1X14
15	citation	---	X1X15
16	methods	---	X1X16
17	mapArea	Indianapolis 30- x 60-Minute Quadrangle	X1X17

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, 2 rows
DescriptionOfMapUnits, nonspatial table, 15 rows
GeoMaterialDict, nonspatial table, 101 rows
Glossary, nonspatial table, 9 rows
MapInformation, nonspatial table, 17 rows
GeologicMap, feature dataset
    ContactsAndFaults, polyline feature class, 211 rows
    IsoValueLines, polyline feature class, 31 rows
    MapUnitPolys, polygon feature class, 84 rows