GeMS validation of Bond_MT_GeMS_ver1.gdb

File written by GeMS_ValidateDatabase.py, version of 3/28/2024
Thu Jun 27 17:43:34 2024
Runtime parameters
Database path: \\mbmgs1a.butte.campus\Bureau\GIS_Geology\24k\Bond\Bond_MT_GeMS_ver1.gdb
Output directory: \\mbmgs1a.butte.campus\Bureau\GIS_Geology\24k\Bond\Bond_MT_GeMS_ver1.gdb
Metadata file: \\mbmgs1a.butte.campus\Bureau\GIS_Geology\24k\Bond\Bond_MT_GeMS_ver1.gdb\Bond_MT_GeMS_ver1.gdb_metadata.xml
Check embedded metadata: True
Skip topology check: False
Refresh GeoMaterialDict: False
Delete extra rows in Glossary and DataSources: False
Compact GDB: True

This database is LEVEL 2 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 Bond_MT_GeMS_ver1.gdb-ValidationErrors.html and Bond_MT_GeMS_ver1.gdb_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
GlossaryFull
LocationConfidenceLookup
OrientationConfidenceLookup
Database Inventory

Compliance Criteria

LEVEL 1

Criteria for a LEVEL 1 GeMS database are: 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 FAIL  1 missing required value(s)
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


DescriptionOfMapUnits, Category
DescriptionOfMapUnits, Type
DescriptionOfMapUnits, AgeType
DescriptionOfMapUnits, AgeOldest
DescriptionOfMapUnits, AgeYoungest
DescriptionOfMapUnits, GeoMaterialDictID
DescriptionOfMapUnits, Notes
DescriptionOfMapUnits, DataSourceMethod
DescriptionOfMapUnits, GlobalID
DataSources, Category
DataSources, Type
DataSources, SourceBibRef
DataSources, GlobalID
Glossary, GlobalID
GeoMaterialDict, GlobalID
GeoMaterialDict, DescriptionOfMapUnits_ID
GlossaryFull, GlobalID
ContactsAndFaults, Category
ContactsAndFaults, Modifier
ContactsAndFaults, SymbolAlt
ContactsAndFaults, LocationConfidence
ContactsAndFaults, LocationConfidenceMethod
ContactsAndFaults, Age
ContactsAndFaults, AgeType
ContactsAndFaults, AgeOldest
ContactsAndFaults, AgeYoungest
ContactsAndFaults, DataSourceMethod
ContactsAndFaults, GlobalID
MapUnitPolys, Category
MapUnitPolys, Type
MapUnitPolys, Modifier
MapUnitPolys, DataSourceMethod
MapUnitPolys, DescriptionOfMapUnitsGUID
MapUnitPolys, GlobalID
OrientationPoints, Category
OrientationPoints, SymbolAlt
OrientationPoints, MapUnitObserved
OrientationPoints, OrientationConfidence
OrientationPoints, LocationConfidence
OrientationPoints, LocationConfidenceMethod
OrientationPoints, FieldID
OrientationPoints, AssocFeatureID
OrientationPoints, DataSourceMethod
OrientationPoints, GlobalID
OverlayPolys, Category
OverlayPolys, DataSourceMethod
OverlayPolys, GlobalID
GeochemPoints, Category
GeochemPoints, ObservedMapUnit
GeochemPoints, FieldSampleID
GeochemPoints, AlternateSampleID
GeochemPoints, MBMGID
GeochemPoints, MBMGURL
GeochemPoints, TASDesignation
GeochemPoints, LocationConfidence
GeochemPoints, LocationConfidenceMethod
GeochemPoints, FieldID
GeochemPoints, DataSourceMethod
GeochemPoints, AnalysisSourceID
GeochemPoints, GlobalID
GeochronPoints, Category
GeochronPoints, ObservedMapUnit
GeochronPoints, MBMGID
GeochronPoints, MBMGURL
GeochronPoints, LocationConfidence
GeochronPoints, LocationConfidenceMethod
GeochronPoints, FieldID
GeochronPoints, DataSourceMethod
GeochronPoints, GlobalID
CartographicLines, Category
CartographicLines, DataSourceMethod
CartographicLines, GlobalID

Tables


LocationConfidenceLookup
OrientationConfidenceLookup
StructureLines
GeochemPoints

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

MapUnit DescriptionOfMapUnits GeologicMap
Jm X X
Qdf X X
Kf X X
IPq X X
Qls X X
Tdwr X X
Qal X X
Qaf X X
Kblv X X
Qc X X
Tan X X
Kblf X X
Tbr X X
Qac X X
Psp X X
Qalo X X
Tbmt X X
Thgt X X
TRd X X
Kk X X
Tsc X X
Tre X X

Contents of Nonspatial Tables

DataSources

OBJECTIDDataSources_IDCategoryTypeSourceSourceBibRefURLNotesGlobalID
1DAS01geospatialgeologic mappingMcDonald, 2022McDonald, Catherine, 2022, Geologic map of the Bond 7.5' quadrangle, Beaverhead County, Montana: Montana Bureau of Mines and Geology Geologic Map 90, 1 sheet.https://doi.org/10.59691/KETV8563This study.{E4D29993-AFDB-4BFB-A37E-6A1FED9FCBEA}
2DAS02geospatialgeologic dataMosolf and Kylander-Clark, 2023Mosolf, J.G., and Kylander-Clark, A., 2023, U-Pb geochronology data from rock samples collected in the Dillon, Hamilton, Philipsburg, Townsend, and Wisdom 30' x 60' quadrangles, western Montana, 2020-2021: Montana Bureau of Mines and Geology Analytical Dataset 3.https://doi.org/10.59691/FIIS4856None{D54C07E0-E716-486E-BD9C-3B47C75C9BE6}
3DAS03non-geospatialgeologic reportFritz and Sears, 1993Fritz, W.J., and Sears, J.W., 1993, Tectonics of the Yellowstone hotspot wake in southwestern Montana: Geology, v. 21, p. 427–430.https://doi.org/10.1130/0091-7613(1993)021%3C0427:TOTYHW%3E2.3.CO;2None{6DE3F589-7E1E-435E-9D50-4BD575D61FE6}
4DAS04geospatialgeophysicsHanna and others, 1993Hanna, W.F., Kaufmann, H.E, Hassemer, J. H., Ruppel, B.D., Pearson, R.C., and Ruppel, E. T., 1993, Maps showing gravity and aeromagnetic anomalies in the Dillon 1º x 2º quadrangle, Idaho and Montana: U. S. Geological Survey Miscellaneous Investigations Series 1803-I, 2 plates, 29 p.https://doi.org/10.3133/i1803INone{3FB234D7-8968-473E-98F4-5E72B517510D}
5DAS05non-geospatialgeologic reportMatthews, 1989Matthews, J.M., 1989, Radiometric dating, depositional environments, and composition of a Tertiary volcaniclastic sequence, Frying Pan Basin, Montana: Atlanta, Georgia State University, M.S. thesis, 92 p.NoneNone{4E220ADC-8843-45D5-B06F-4A8AE2D498B5}
6DAS06geospatialgeologic mappingTysdal and others, 1994Tysdal, R.G., Dyman, T.S., and Lewis, S.E., 1994, Geologic map of Cretaceous strata between Birch Creek and Brownes Creek, eastern flank of Pioneer Mountains, Beaverhead County, Montana: U.S. Geological Survey Miscellaneous Investigations Series Map I-2434, scale 1:24,000.https://doi.org/10.3133/i2434None{80630B38-7E1C-4DEA-9745-A114F1E7B2FF}
7DAS07non-geospatialgeologic reportDyman and Nichols, 1988Dyman, T.S., and Nichols, D.J., 1988, Stratigraphy of mid-Cretaceous Blackleaf and lower part of the Frontier Formations in parts of Beaverhead and Madison Counties, Montana: U.S. Geological Survey Bulletin 1773, 31 p.https://doi.org/10.3133/b1773None{BE6F4F56-D999-4668-A8DE-8FC868FA7E11}
8DAS08non-geospatialgeologic reportDyman and Tysdal, 1998Dyman, T.S., and Tysdal, R.G., 1998, Stratigraphy and depositional environment of nonmarine facies of Frontier Formation, eastern Pioneer Mountains, southwestern Montana: The Mountain Geologist, v. 35, no. 3, p. 115–125.NoneNone{C8EF7CAD-BCCA-44E1-A19C-C055CFB1B1A8}
9DAS09non-geospatialgeologic reportZartman and others, 1995Zartman, R.E., Dyman, T.S., Tysdal, R.G., and Pearson, R.C., 1995, U-Pb ages of volcanogenic zircon from porcellanite beds in the Vaughn Member of the mid-Cretaceous Blackleaf Formation, southwestern Montana, in Shorter contributions to the stratigraphy and geochronology of the Upper Cretaceous rocks in the Western Interior of the United States: U.S. Geological Survey Bulletin 2113-B, p. B1–B15.https://doi.org/10.3133/b2113None{C298CAFE-47B5-415B-A233-21BA1EBCFBD1}
11DAS11geospatialgeologic mappingYakovlev, 2019Yakovlev, P.V., 2019, Geologic map of the Glen 7.5′ quadrangle, southwestern Montana: Montana Bureau of Mines and Geology Geologic Map 74, 1 sheet, scale 1:24,000.https://www.mbmg.mtech.edu/mbmgcat/public/ListCitation.asp?pub_id=32166&#gsc.tab=0None{EE78D482-AF06-4CBA-B1FB-E742639C7E71}
12DAS12non-geospatialgeneric documentAGI Glossary of GeologyNeuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of Geology: Alexandria, Virginia, American Geological Institute, 799 p.https://www.americangeosciences.org/pubs/glossaryNone{13CF0BBC-0063-43FE-9DAD-4088960B29F2}
14DAS13non-geospatialgeneric documentAK GeMS Data DictionaryHendricks, M.D., Ekberg, P.G., Athey, J.E., Wyatt, W.C., Willingham, A.L., and Naibert, T.J., 2021, AK GeMS data dictionary: A description of the Alaska geologic mapping schema: Alaska Division of Geological & Geophysical Surveys Miscellaneous Publication 170, 10 p.https://doi.org/10.14509/30669None{EB77AB96-60C8-4BFA-A0CE-94131E8A22FC}

DescriptionOfMapUnits

OBJECTIDDescriptionOfMapUnits_IDCategoryTypeSymbolLabelMapUnitNameFullNameAgeAgeTypeAgeOldestAgeYoungestDescriptionHierarchyKeyParagraphStyleAreaFillRGBAreaFillPatternDescriptionGeoMaterialDictIDGeoMaterialGeoMaterialConfidenceNotesDataSourceMethodDescriptionSourceIDGlobalID
10{77E73636-7A6E-4339-8FAB-C529B2244908}map unitmap unit, generic0010QalQalalluviumalluviumQuaternaryrelativeHoloceneHoloceneUnconsolidated gravel, sand, silt, and clay deposited primarily by the Beaverhead River. Clasts generally subrounded to well-rounded and consist predominantly of quartzite. Thickness as much as 10 m (33 ft).01dmu, map unit255,255,222None{9681AE57-A86A-4E8B-8DD6-6103B1DB9517}Alluvial sediment, mostly coarse-grainedhighNone2DAS01{77E73636-7A6E-4339-8FAB-C529B2244908}
8{92575C43-C8BC-496E-9946-A50A4BD0409D}map unitmap unit, genericA150QacQacalluvium and colluviumalluvium and colluviumQuaternaryrelativePleistoceneHoloceneUnconsolidated sand, silt, and clay, and subordinate gravel, deposited on gentle slopes by fluvial and gravity processes. Variable thickness, generally less than 10 m (33 ft).02dmu, map unit235,222,128None{9681AE57-A86A-4E8B-8DD6-6103B1DB9517}Alluvial sediment, mostly coarse-grainedhighNone2DAS01{92575C43-C8BC-496E-9946-A50A4BD0409D}
9{9798E13C-F980-46C0-85D0-636D88E5FDF6}map unitmap unit, generic0A60QafQafalluvial-fan depositalluvial-fan depositQuaternaryrelativePleistoceneHoloceneUnconsolidated, poorly sorted, cobbles, gravel, sand, and silt forming fan-shaped deposit. Estimated thickness about 20 m (65 ft).03dmu, map unit255,235,102None{9681AE57-A86A-4E8B-8DD6-6103B1DB9517}Alluvial sediment, mostly coarse-grainedhighNone2DAS01{9798E13C-F980-46C0-85D0-636D88E5FDF6}
14{1CFABC8B-9FA9-475F-9151-86C9F6527ADC}map unitmap unit, genericAA60QlsQlslandslide depositlandslide depositQuaternaryrelativePleistoceneHoloceneMass-wasting deposit that consists of unsorted mixture of clay- to boulder-size sediment. Characterized by hummocky topography at the toe and a subdued landslide scarp. Thickness less than 10 m (33 ft).04dmu, map unit235,235,102None{017338DF-E8E0-4EE7-BAED-C9EBC828F436}Debris flows, landslides, and other localized mass-movement sedimenthighNone2DAS01{1CFABC8B-9FA9-475F-9151-86C9F6527ADC}
12{2F40CFE9-BAC5-4309-84B2-E078BE7F70EF}map unitmap unit, generic0AX0QcQccolluviumcolluviumQuaternaryrelativePleistoceneHoloceneUnconsolidated, locally derived slope deposits that contain rounded to angular, poorly size-sorted clasts, primarily with clasts that are pebble size and larger. Thickness generally less than 10 m (33 ft).05dmu, map unit255,235,000None{6C2D6A29-29B2-4583-B4D5-D7B0A66B031F}Colluvium and other widespread mass-movement sedimenthighNone2DAS01{2F40CFE9-BAC5-4309-84B2-E078BE7F70EF}
13{498F1C9D-9F09-4A5A-9259-C77733EB4BAE}map unitmap unit, generic0170QdfQdfdebris-flow depositdebris-flow depositQuaternaryrelativePleistoceneHoloceneAngular, subangular, and subrounded clasts of chaotic and unstratified boulders and cobbles and subordinate finer sediment. Some fine sediment was probably removed by erosion, leaving coarser clasts as lag deposits. Estimated thickness about 15 m (50 ft).06dmu, map unit255,222,077None{017338DF-E8E0-4EE7-BAED-C9EBC828F436}Debris flows, landslides, and other localized mass-movement sedimenthighNone2DAS01{498F1C9D-9F09-4A5A-9259-C77733EB4BAE}
11{4CBD0B28-E3EA-45AA-BE08-0F328276B861}map unitmap unit, genericAA40QaloQaloalluvium, olderalluvium, olderQuaternaryrelativePleistoceneHoloceneUnconsolidated, stratified to unstratified gravel, sand, silt, and clay deposited by the Beaverhead River prior to deposition of Qal. Adjacent to but at elevations higher than Qal. Estimated thickness 0–30 m (0–100 ft).07dmu, map unit235,235,153None{9681AE57-A86A-4E8B-8DD6-6103B1DB9517}Alluvial sediment, mostly coarse-grainedhighNone2DAS01{4CBD0B28-E3EA-45AA-BE08-0F328276B861}
22{03955394-A0A7-4A75-861F-61FE7F187C93}map unitmap unit, generic0480TscTscSixmile Creek FormationSixmile Creek Formation of Bozeman GroupTertiaryabsolutePlioceneMiocenePale orange to brown, unconsolidated to consolidated, tuffaceous to quartz-rich silt, sand, gravel, and conglomerate. Conglomerates are the predominant lithology and cap low ridges in the western part of the map. They are poorly sorted, with locally derived sub-angular to rounded pebbles, cobbles, and boulders in a coarse, sandy matrix. Clasts are predominantly quartzite but locally include abundant volcanic clasts, limestone, and granitic cobbles. In the southwest corner of the map, large boulders of quartzite and granite [up to 3 m (10 ft) in diameter] characterize the deposits. The finer-grained intervals are very thin- to medium-bedded, massive to cross-stratified, silt, sand, and gravel with lenses and beds of conglomerate, along with intervals of gray volcanic ash and very pale orange to tan, massive tuffs. In places, the finer-grained intervals contain burrows, nodules, bone fragments, and caliche-cemented intervals with abundant rhizoliths that are interpreted as paleosols. The finer-grained intervals are best exposed north of Frying Pan Gulch (sections 34 and 35, T. 7 S., R. 8 W.) and are correlated with the Anderson Ranch member of the Sixmile Creek Formation (Fritz and Sears, 1993) based on a new U-Pb maximum depositional age of 15.5 ± 0.1 Ma (table 2, sample KM20BD30). Thickness variable but estimated to be as much as 305 m (1,000 ft) thick.08dmu, map unit255,153,051None{CDF81738-6203-4D80-B211-331B436FC586}Sedimentary and extrusive igneous materialmediumNone2DAS01 | DAS03{03955394-A0A7-4A75-861F-61FE7F187C93}
21{618E76D2-9045-4F1F-89E9-1C897C81AB38}map unitmap unit, genericA270TreTreRenova FormationRenova Formation of Bozeman GroupTertiaryrelativeMioceneEoceneVery pale orange, grayish orange, white, and pale yellowish brown tuffaceous mudstone, organic-rich siltstone, tuff, and fine to coarse-grained sandstone. Sandstone intervals are poorly sorted, often micaceous, with angular to subrounded granules, pebbles, and cobbles. Cobble size clasts are predominantly quartzite, limestone, and volcanic rock. Locally contains petrified wood, paper shales, and clay-rich intervals that weather to a “popcorn” texture. In section 27, T. 6 S., R. 9 W., thin tufa intervals (fig. 3) may be related to nearby faulting. An ash sample from the exposure with the tufa beds yielded a U-Pb zircon age of 31.8 ± 0.2 Ma (table 2, sample KM20BD16). Estimated thickness around 790 m (2,600 ft) thick but up to 900 m (3,000 ft) regionally as reported by Hanna and others (1993).09dmu, map unit235,204,077None{9681AE57-A86A-4E8B-8DD6-6103B1DB9517}Alluvial sediment, mostly coarse-grainedmediumNone2DAS01 | DAS04{618E76D2-9045-4F1F-89E9-1C897C81AB38}
17{1A715CAA-483D-4221-B9E4-1D61EDAD69D6}map unitmap unit, generic1370TbrTbrvolcanic brecciavolcanic brecciaTertiaryrelativeEoceneEoceneGrayish, poorly sorted, matrix-supported breccia with predominantly angular reddish rhyolite and welded rhyolite tuff clasts, subordinate angular basalt clasts, and rounded quartzite and granite cobbles. Clasts up to 0.5 m (1.5 ft). Intercalated with rhyolite tuff (map unit Trt). Matthews (1989) interpreted the breccias as channelized, debris flow deposits with a maximum horizontal extent of approximately 100 m (333 ft) and a maximum thickness of 14 m (46 ft).10dmu, map unit222,178,077None{5F3BE483-53E9-4A2A-BC9B-EFA727244C5B}Felsic-composition pyroclastic flowshighNone2DAS01 | DAS05{1A715CAA-483D-4221-B9E4-1D61EDAD69D6}
16{8527423A-9011-46AC-A1E7-F526B3B3445C}map unitmap unit, generic27A0TbmtTbmtBurns Mountain tuffBurns Mountain tuffTertiaryabsoluteEoceneEoceneMassive, white to light gray weathering tuff and welded tuff. Tuff/ash flow intervals contain smoky quartz and biotite (<1 percent) phenocrysts. Small fragments (~5 mm) of pumice, volcanic rock, fine-grained sedimentary rock, and silicified wood are common. Intervals of ash with planar, low-angle cross bedding suggest local fluvial reworking. Welded tuff is white, moderate orange pink, and pale purple with anhedral smoky quartz, plagioclase, biotite, and hornblende. Well exposed south of Frying Pan Gulch where it overlies unwelded tuffs. Base not exposed but at least 60 m (200 ft) thick. Three samples yielded U-Pb zircon ages spanning 46.3 ± 0.2 to 46.9 ± 0.2 Ma (table 2, samples KM20BD01, KM20BD09, and KM20BD13).11dmu, map unit204,077,235None{5F3BE483-53E9-4A2A-BC9B-EFA727244C5B}Felsic-composition pyroclastic flowshighNone2DAS01{8527423A-9011-46AC-A1E7-F526B3B3445C}
15{EB9AB8BB-6691-45C0-B4DB-FF3818C5FBCB}map unitmap unit, generic2420TanTanandesite flowsandesite flowsTertiaryrelativeEoceneEoceneDark brown to black andesite flows (58.2 wt. percent SiO2, table 1) with an aphanitic groundmass and <2–3 percent phenocrysts of olivine, pyroxene, rare plagioclase, and quartz. Forms isolated, knobby outcrops that weather pale reddish brown to black and often have a vesicular texture.12dmu, map unit235,077,077None{37FCE4C5-5C59-4925-822E-6E892B69B4DE}Fine-grained, intermediate-composition intrusive igneous rockhighNone2DAS01{EB9AB8BB-6691-45C0-B4DB-FF3818C5FBCB}
19{0CA70F36-7A54-402B-B8DC-3C6A11361232}map unitmap unit, generic5700ThgtThgtHennbury Gulch tuffHennbury Gulch tuffTertiaryabsoluteEoceneEoceneWhite to light brown, poorly exposed lithic-vitric tuff. Composed of crude bedforms that are ~1–2 m thick and massive. Contains broken phenocrysts (up to ~30 percent) of quartz, feldspar, biotite, and occasional amphibole in a vitric groundmass composed of cuspate glass shards that are mostly fresh but are devitrified locally. Tuff intervals commonly include small fragments (~5 mm) of pumice, accidental volcanic clasts (up to ~1 m), and petrified wood. Thin intervals of planar, low-angle cross-bedded tuffaceous sand occur locally. This unit yielded a U-Pb zircon age of 48.6 ± 0.2 Ma (table 2, sample KM20BD32). As thick as 150 m (500 ft).13dmu, map unit128,077,255None{5F3BE483-53E9-4A2A-BC9B-EFA727244C5B}Felsic-composition pyroclastic flowshighNone2DAS01{0CA70F36-7A54-402B-B8DC-3C6A11361232}
18{7F7BD027-8926-4F40-B875-8635A2669A73}map unitmap unit, generic2300TdwrTdwrDillon West rhyoliteDillon West rhyoliteTertiaryabsoluteEoceneEoceneModerate to dark reddish brown, pale red to grayish red, and light gray to grayish blue weathering, aphanitic rhyolite (70.3 to 70.4 wt. percent SiO2, table 1) with sparse (<5 percent) phenocrysts of biotite, hornblende, feldspar, and quartz. Individual flows can be vuggy, massive, or exhibit conspicuous flow foliation. Discontinuous intervals of vitrophere and autobreccia occur locally. Two samples yielded U-Pb zircon ages spanning 50.4 ± 0.7 Ma to 48.4 ± 0.9 Ma (table 2, samples KM20BD04 and KM20BD29).14dmu, map unit204,178,255None{AAA1DC43-47DB-4FA8-8160-962345918502}Felsic-composition lava flowshighNone2DAS01{7F7BD027-8926-4F40-B875-8635A2669A73}
5{CC5DEA22-E849-4B09-AF53-833FE5D31DA1}map unitmap unit, generic4160KfKfFrontier FormationFrontier FormationLate CretaceousabsoluteLate CretaceousLate CretaceousDominantly gray, brown, brownish gray, and greenish gray siltstone and mudstone, and subordinate medium- to coarse-grained, and locally very coarse-grained sandstone, conglomerate, limestone, and minor porcellanite. The beds of mudstone, siltstone, limestone, and sandstone form fining-upward depositional cycles tens of meters thick. Sandstone and conglomerate are rich in quartz and chert. Conglomerate clasts are rounded pebbles and cobbles of chert and quartz, but locally contain limestone and mudstone cobbles. Volcaniclastic sandstone and bentonitic mudstone occur in the upper part. Lower 100–200 m (330–660 ft) is distinctive brown to brownish gray siltstone and mudstone. Top not exposed but thickness about 900 m (3,000 ft) north of the quadrangle (Tysdal and others, 1994; Dyman and Nichols, 1988).15dmu, map unit153,222,102None{AB5A96BE-7478-43F0-8902-44A5D21B9FE7}Sandstone and mudstonemediumNone2DAS01 | DAS06 | DAS07{CC5DEA22-E849-4B09-AF53-833FE5D31DA1}
4{C8C3EB3E-5DEF-49EA-862C-2A32B13A1E01}map unitmap unit, generic4040KblvKblvVaughn MemberVaughn Member of the Blackleaf Formation of Colorado GroupCretaceousrelativeEarly CretaceousLate CretaceousOlive green, yellowish green, bright green, and gray green, hard, dense, and calcareous siltstone and porcellanitic (silicified) mudstone. Subordinate gray, greenish gray and olive gray, fine- to medium-grained, and locally coarse-grained lithic sandstone, with common volcaniclastic debris, and matrix-supported conglomerate and conglomeratic sandstone with clasts mostly of chert and quartzite. An association of distinctive lithologies is present in the uppermost part, which consists of maroon mudstone and siltstone, gray freshwater limestone, or locally very calcareous mudstone and siltstone, dark gray shale, and bright green porcellanite. Upper contact is mapped at top of a porcellanite bed, interbedded with micritic limestone, that directly overlies the highest maroon mudstone (after Tysdal and others, 1994; Dyman and Tysdal, 1998). A porcellanite bed approximately 25 m (80 ft) below the top of the Vaughn in the Frying Pan Basin yielded a U-Pb age of 94.8 ± 0.5 Ma (Zartman and others, 1995). Top not exposed but at least 360 m (1,180 ft) thick in the quadrangle.16dmu, map unit153,255,153None{AB5A96BE-7478-43F0-8902-44A5D21B9FE7}Sandstone and mudstonehighNone2DAS01 | DAS06 | DAS08 | DAS09{C8C3EB3E-5DEF-49EA-862C-2A32B13A1E01}
3{476D8C22-844C-4D0F-8263-EB15788F94C8}map unitmap unit, genericX470KblfKblfFlood MemberFlood Member of the Blackleaf Formation of Colorado GroupEarly CretaceousrelativeEarly CretaceousEarly CretaceousUpper part: pale brown to brownish gray, fine- to medium-grained and locally coarse-grained to conglomeratic, quartz- and chert-rich lithic sandstone, and conglomerate. Trough crossbedding common in sandstone. Middle part: dominantly gray mudstone, shale, and minor interbeds of siltstone and quartz-rich sandstone. Lower part: medium gray and locally green and red calcareous siltstone and mudstone, gray shale, and gray, calcareous, fine- to medium-grained sandstone that is rich in quartz and chert grains (Tysdal and others, 1994; Dyman and Nichols, 1988). Thickness 230 m (750 ft).17dmu, map unit000,153,077None{AB5A96BE-7478-43F0-8902-44A5D21B9FE7}Sandstone and mudstonehighNone2DAS01 | DAS06 | DAS07{476D8C22-844C-4D0F-8263-EB15788F94C8}
6{7C84EF1C-E907-4466-9FED-9DB8FFDD8EF1}map unitmap unit, generic72X0KkKkKootenai FormationKootenai FormationEarly CretaceousrelativeEarly CretaceousEarly CretaceousMapped as one unit, but consists of four distinct members described below (after Myers, 1952). Combined thickness of all members is about 245 m (800 ft). Gastropod limestone member: Light gray, thick-bedded, gastropod coquina or gastropod-rich limestone that may also contain charophytes and ostrocodes. Forms conspicuous ridges. Upper clastic member: Variegated shale and mudstone, dominated by red, orange, and purple, and subordinate light and medium gray colors, interbedded with minor reddish quartz- and chert-rich lithic sandstone. Poorly exposed, recessive unit. Middle limestone member: Pale yellowish gray to pale brown, dense limestone and shaly limestone with interbedded shale. Lower clastic member: Upper part recessive, mostly reddish and greenish mudstone; lower part is ridge-forming, coarse- to medium-grained, cross-bedded to massive, brown to yellowish gray chert-rich lithic sandstone with local lenses of chert-rich conglomerate and limestone pebble conglomerate; interbedded with reddish and greenish mudstone.18dmu, map unit077,204,000None{AB5A96BE-7478-43F0-8902-44A5D21B9FE7}Sandstone and mudstonemediumNone2DAS01 | DAS06 | DAS07{7C84EF1C-E907-4466-9FED-9DB8FFDD8EF1}
2{D775E555-9C14-4E7F-8A7E-2EF37DEDEA75}map unitmap unit, generic3A30JmJmMorrison FormationMorrison FormationJurassicrelativeJurassicJurassicGreen, red, and gray variegated mudstone, shale, and siltstone with thin, interbedded yellowish brown to grayish orange, very fine-grained sandstone and siltstone and thin, gray limestone beds. Poorly exposed recessive interval. Thickness about 45–55 m (150–175 ft).19dmu, map unit178,235,178None{2D09A5AE-F0AD-462B-84BC-4092CE922275}Mostly mudstonehighNone2DAS01{D775E555-9C14-4E7F-8A7E-2EF37DEDEA75}
20{84A5E08C-4398-45BC-A6A5-E33390E66536}map unitmap unit, generic5120^dTRdDinwoody FormationDinwoody FormationLower TriassicrelativeLower TriassicLower TriassicInterbedded shale, limestone, and calcareous sandstone characterized by distinctive pale to light grayish brown weathered surfaces and the presence of phosphatic pelecypod lingula. Upper part has massive calcareous, rippled sandstone beds as much as 1 m (3 ft) thick with shaley interbeds. Massive, gray, pinkish gray weathering limestone as much as 1 m (3 ft) thick is major component in upper part. Lower part is predominantly olive drab, chippy-weathering, hard fissile shale with interbedded dark brown weathering, silty limestone beds 10 cm (4 in.) or thinner. Thickness about 245 m (800 ft).20dmu, map unit128,222,204None{31CBE54B-0B07-457B-8AC5-A73AB365E34C}Mostly carbonate rockmediumNone2DAS01{84A5E08C-4398-45BC-A6A5-E33390E66536}
7{8321432E-305E-4A64-80BB-62AECEC86FE5}map unitmap unit, generic62A0PspPspShedhorn and Phosphoria Formations, undividedShedhorn and Phosphoria Formations, undividedPermianrelativePermianPermianShedhorn Formation: grayish brown, fine-grained, thin- to thick-bedded quartz sandstone, and cherty sandstone with chert and quartz cement. Vertical and horizontal burrows are relatively common. Phosphoria Formation: dark gray to black, carbonaceous and phosphatic mudstone with scarce phosphate beds, grayish and gray brown cherty quartz sandstone, cherty or sandy dolomite, fine-grained dolomitic sandstone, and yellowish tan sandy siltstone with subordinate beds of vitreous quartz sandstone. Thickness approximately 89 m (300 ft).21dmu, map unit102,204,235None{FDA3C54D-61D0-4798-ACC3-21A2F1270733}Mostly sandstonemediumNone2DAS01{8321432E-305E-4A64-80BB-62AECEC86FE5}
1{887C0703-06B3-4AB3-B172-8379275271B5}map unitmap unit, generic4A00*qIPqQuadrant FormationQuadrant FormationPennsylvanianrelativePennsylvanianPennsylvanianLight gray to light yellowish brown, fine-grained, vitreous quartz sandstone. Poorly exposed and mapped on the basis of float along the north boundary of the map. Thickness approximately 245 m (800 ft) based on mapping in north-adjacent Glen 7.5′ quadrangle (Yakovlev, 2019).22dmu, map unit153,235,255None{BA96A3AA-660F-4C81-87EB-463C01EB9F06}SandstonehighNone2DAS01 | DAS11{887C0703-06B3-4AB3-B172-8379275271B5}

Glossary

OBJECTIDGlossary_IDTermDefinitionDefinitionSourceIDGlobalID
1{4D4B6B03-B085-4315-953C-D960399042DB}2 sigma2 sigma error of measure. Standard deviation multiplied by 2.DAS01{4D4B6B03-B085-4315-953C-D960399042DB}
52{E371EA80-9938-47E4-B868-1D420E4B9621}absoluteAge assignment is based on radiometric dating.DAS13{E371EA80-9938-47E4-B868-1D420E4B9621}
2{0E4FA450-A054-4A07-88EF-781C3A37A805}accurateIndicates that the author is reasonably confident in the location of the feature, and the feature is accurately located to within the values range indicated in the LocationConfidenceLookup table.DAS13{0E4FA450-A054-4A07-88EF-781C3A37A805}
4{9365EF45-053C-4B25-B5E3-FCA632410259}approximateIndicates that the author is somewhat confident in the location of the feature, and the feature is approximately located to within the values indicated in the LocationConfidenceLookup table.DAS13{9365EF45-053C-4B25-B5E3-FCA632410259}
6{1D7F66B4-2D1B-44A9-A383-0CF397DB7529}bedding, genericAs defined in the AGI Glossary of Geology, see term "bed [stratig]".DAS12{1D7F66B4-2D1B-44A9-A383-0CF397DB7529}
8{F69E3AD7-8364-4257-9247-C0441DA1581D}boundary, mapA linear feature indicating where one map unit ends at the map boundary.DAS13{F69E3AD7-8364-4257-9247-C0441DA1581D}
9{F430FD17-8A0B-4ADD-ABFA-91CC4523A09E}certainIndicates that the author is reasonably confident in the scientific credibility of the existence of the feature.DAS13{F430FD17-8A0B-4ADD-ABFA-91CC4523A09E}
11{23E3F406-B26F-4E33-9238-0F187708B563}contact, genericA linear feature indicating where two map units meet. As defined in the AGI Glossary of Geology, see term "contact".DAS12 | DAS13{23E3F406-B26F-4E33-9238-0F187708B563}
12{FDC3B1DC-ED24-4AFA-9404-434285E58187}contact, internal extent of modified map unitThe internal extent boundary of modified portion of underlaying map unit. Symbolized as a zero-point line to avoid being displayed.DAS01{FDC3B1DC-ED24-4AFA-9404-434285E58187}
51{5CC01CD6-E557-43FA-8DF4-0BA4DEE05251}dmu, map unitDescription of Map Unit generic paragraph format for map units.DAS13{5CC01CD6-E557-43FA-8DF4-0BA4DEE05251}
15{B72E8DA0-68E9-4109-9E73-CD02C789B6D5}fault, decoration, apparent offsetA visual object used on the map to specifically show an FGDC digital cartographic decoration symbol. As defined in the AGI Glossary of Geology, see term "fault [struc geol]", where letter “U” designates the upthrown block and letter “D” designates the downthrown block.DAS12 | DAS13{B72E8DA0-68E9-4109-9E73-CD02C789B6D5}
16{623310D5-8447-4397-8EA2-9E944F202B01}fault, genericAs defined in the AGI Glossary of Geology, see term "fault [struc geol]".DAS12{623310D5-8447-4397-8EA2-9E944F202B01}
17{6B6F10D7-C016-4412-BA90-24894CE4C0D7}fault, normalAs defined in the AGI Glossary of Geology, see term "normal fault".DAS12{6B6F10D7-C016-4412-BA90-24894CE4C0D7}
18{F9963147-C6EE-459A-B801-B261FCF10FC8}fault, thrustAs defined in the AGI Glossary of Geology, see term "thrust fault".DAS12{F9963147-C6EE-459A-B801-B261FCF10FC8}
20{9E5602D7-4D7A-4FC4-A4CD-89E34C8AA698}fold, anticline, overturnedAs defined in the AGI Glossary of Geology, see term "anticline" that is modified by term "overturned".DAS12{9E5602D7-4D7A-4FC4-A4CD-89E34C8AA698}
21{7C4FC010-E2F8-4CBC-9EF9-62E478E6DC53}fold, syncline, overturnedAs defined in the AGI Glossary of Geology, see term "syncline" that is modified by term "overturned".DAS12{7C4FC010-E2F8-4CBC-9EF9-62E478E6DC53}
23{2E414A8F-94FB-497A-BDE6-7FA9780B70C1}foliation, igneous, genericAs defined in the AGI Glossary of Geology, see term "primary foliation" formed in "igneous" rocks. See notes field for details.DAS12{2E414A8F-94FB-497A-BDE6-7FA9780B70C1}
24{BD659594-7995-44F8-A692-32EDE4672A54}generalizedThe feature's location confidence is primarily identified with the ordinal classification scheme used in the LocationConfidence field. The numeric value found in the LocationConfidenceMeters field is derived from this value and based on conversion logic found in the LocationConfidenceLookup table.DAS13{BD659594-7995-44F8-A692-32EDE4672A54}
25{C289C0F1-3E96-4857-AA54-D98810687C44}generic documentA generic document, such as a standards manual or guide.DAS13{C289C0F1-3E96-4857-AA54-D98810687C44}
27{B2F09D60-A4B4-4217-AB3C-E62EF1705948}geochem, whole-rockAs defined in the AGI Glossary of Geology, see term "whole-rock".DAS12{B2F09D60-A4B4-4217-AB3C-E62EF1705948}
29{A647A047-462D-4A3C-948A-96F593AE402C}geochron, U-PbAs defined in the AGI Glossary of Geology, see term "uranium-lead age method".DAS12{A647A047-462D-4A3C-948A-96F593AE402C}
30{458FD00E-052F-41A6-9E56-49C3A2EC4207}geologic dataGeologic observations, analyses, or other information.DAS13{458FD00E-052F-41A6-9E56-49C3A2EC4207}
31{09DEFEE5-9188-41C9-B2FC-28A24AA168D2}geologic mappingA geologic map.DAS13{09DEFEE5-9188-41C9-B2FC-28A24AA168D2}
32{03360EBB-37BB-47B2-A3A7-359DBB22C978}geologic reportA written geologic report.DAS13{03360EBB-37BB-47B2-A3A7-359DBB22C978}
33{F77B4F4A-7369-498D-9E97-2A053D1F6A16}geophysicsGeophysical data.DAS13{F77B4F4A-7369-498D-9E97-2A053D1F6A16}
36{35457379-58A0-434B-810A-6596B30101F7}graphic, cross section lineA graphic line on the map indicating where a cross-section is generated.DAS13{35457379-58A0-434B-810A-6596B30101F7}
37{783260FD-A7E6-465E-BA64-812124C9194F}highIndicates that the author has a high confidence in this value.DAS13{783260FD-A7E6-465E-BA64-812124C9194F}
38{847B16F4-538F-410E-A5F1-2E0DAB7297AE}inferredIndicates that the author is not confident in the location of the feature, and its location is inferred to within the values indicated in the LocationConfidenceLookup table.DAS13{847B16F4-538F-410E-A5F1-2E0DAB7297AE}
40{F7401311-275C-44D7-B9E0-39A4112FAA63}joint, minor, inclinedAs defined in the AGI Glossary of Geology, see term "joint [struc geol]" that is modified by term "inclination [slopes]" and described as small-scale.DAS12{F7401311-275C-44D7-B9E0-39A4112FAA63}
41{9FBDC2BA-D4F3-4351-9310-434D6819AB64}MaAge expressed as millions of years ago.DAS13{9FBDC2BA-D4F3-4351-9310-434D6819AB64}
43{3D630C79-99DC-46C3-9F1F-178256088797}map unit, genericAs defined in the AGI Glossary of Geology, see term "lithostratigraphic unit".DAS12{3D630C79-99DC-46C3-9F1F-178256088797}
44{1D052B21-683B-4FD3-BF77-48C373959FE7}mediumIndicates that the author is somewhat confident in this value.DAS13{1D052B21-683B-4FD3-BF77-48C373959FE7}
46{6E46140A-4811-41A4-BF93-F014AD4A886E}modifier, weldedA feature designed to visualize a modification of underlying map units. This modification will be "burned" in to the MapUnitPolys Modifier field at publication time. As defined in the AGI Glossary of Geology, see term "welding".DAS12{6E46140A-4811-41A4-BF93-F014AD4A886E}
48{06995FA4-0D89-454F-9B9A-18FE25B7E181}questionableIndicates that the author is not confident in the scientific credibility of the existence of the feature.DAS13{06995FA4-0D89-454F-9B9A-18FE25B7E181}
53{3538C07F-3A37-45FA-B958-4AF576D12891}relativeAge assignment is based on stratigraphic position.DAS13{3538C07F-3A37-45FA-B958-4AF576D12891}

GlossaryFull

OBJECTIDGlossaryFull_IDTermDefinitionDefinitionSourceIDGlobalID
1{AF791317-93BC-4EDD-A0FC-5AB2218B1B3D}2 sigma2 sigma error of measure. Standard deviation multiplied by 2.DAS01{AF791317-93BC-4EDD-A0FC-5AB2218B1B3D}
2{62A68133-DB89-4A50-9879-12E0E633BA48}accurateIndicates that the author is reasonably confident in the location of the feature, and the feature is accurately located to within the values range indicated in the LocationConfidenceLookup table.DAS13{62A68133-DB89-4A50-9879-12E0E633BA48}
3{0C8D63C0-82FE-4555-83A9-0A1B76BF348D}andesiteAs defined in the AGI Glossary of Geology, see term "adesite".DAS12{0C8D63C0-82FE-4555-83A9-0A1B76BF348D}
4{0B9BE30C-34F7-41F3-9E2D-2B2867670B85}approximateIndicates that the author is somewhat confident in the location of the feature, and the feature is approximately located to within the values indicated in the LocationConfidenceLookup table.DAS13{0B9BE30C-34F7-41F3-9E2D-2B2867670B85}
5{4AA51D32-3556-4042-8486-625D4FF9089C}beddingAs defined in the AGI Glossary of Geology, see term "bed [stratig]".DAS12{4AA51D32-3556-4042-8486-625D4FF9089C}
6{058B980D-D07C-4302-AB32-BEEE063501A6}bedding, genericAs defined in the AGI Glossary of Geology, see term "bed [stratig]".DAS12{058B980D-D07C-4302-AB32-BEEE063501A6}
7{0FE3847E-7C5B-4CD3-B985-F5B5E838AFD0}boundaryA linear feature indicating where one map unit ends without an adjacent map unit.DAS13{0FE3847E-7C5B-4CD3-B985-F5B5E838AFD0}
8{074A330F-2BEE-45F9-9CE4-BB411D35C0FA}boundary, mapA linear feature indicating where one map unit ends at the map boundary.DAS13{074A330F-2BEE-45F9-9CE4-BB411D35C0FA}
9{0B78405B-52C9-46AA-BBDE-644031079C3F}certainIndicates that the author is reasonably confident in the scientific credibility of the existence of the feature.DAS13{0B78405B-52C9-46AA-BBDE-644031079C3F}
10{F588CBAF-DDEB-401C-B223-15D2396461F9}contactA linear feature indicating where two map units meet. As defined in the AGI Glossary of Geology, see term "contact".DAS12 | DAS13{F588CBAF-DDEB-401C-B223-15D2396461F9}
11{D11D0C58-BB3A-4C2A-8334-A73019912A18}contact, genericA linear feature indicating where two map units meet. As defined in the AGI Glossary of Geology, see term "contact".DAS12 | DAS13{D11D0C58-BB3A-4C2A-8334-A73019912A18}
12{91A4A53D-A915-4821-B90B-E60BA176784C}contact, internal extent of modified map unitThe internal extent boundary of modified portion of underlaying map unit. Symbolized as a zero-point line to avoid being displayed.DAS01{91A4A53D-A915-4821-B90B-E60BA176784C}
13{8695554C-C3E2-4C21-B6FD-59E93FCD5520}daciteAs defined in the AGI Glossary of Geology, see term "dacite".DAS12{8695554C-C3E2-4C21-B6FD-59E93FCD5520}
14{AFA15143-F1E8-4DEC-8E87-30C8D6D8DF5E}faultAs defined in the AGI Glossary of Geology, see term "fault [struc geol]".DAS12{AFA15143-F1E8-4DEC-8E87-30C8D6D8DF5E}
15{F7DEF9D1-12F3-4D28-8FFD-69F539682F72}fault, decoration, apparent offsetA visual object used on the map to specifically show an FGDC digital cartographic decoration symbol. As defined in the AGI Glossary of Geology, see term "fault [struc geol]", where letter “U” designates the upthrown block and letter “D” designates the downthrown block.DAS12 | DAS13{F7DEF9D1-12F3-4D28-8FFD-69F539682F72}
16{6AEC57D8-63CD-4606-BD66-417A0E3A3DA6}fault, genericAs defined in the AGI Glossary of Geology, see term "fault [struc geol]".DAS12{6AEC57D8-63CD-4606-BD66-417A0E3A3DA6}
17{7C9E315A-626F-4A07-B265-E5B5C1308B9B}fault, normalAs defined in the AGI Glossary of Geology, see term "normal fault".DAS12{7C9E315A-626F-4A07-B265-E5B5C1308B9B}
18{9C42C5A0-7634-4CBD-A58B-AED3ADE460F0}fault, thrustAs defined in the AGI Glossary of Geology, see term "thrust fault".DAS12{9C42C5A0-7634-4CBD-A58B-AED3ADE460F0}
19{9BE3A33F-FF34-463D-8C7F-B3D49092709F}foldAs defined in the AGI Glossary of Geology, see term "fold [struc geol]".DAS12{9BE3A33F-FF34-463D-8C7F-B3D49092709F}
20{8DAC849E-C692-40DC-A335-EDA43027A9A5}fold, anticline, overturnedAs defined in the AGI Glossary of Geology, see term "anticline" that is modified by term "overturned".DAS12{8DAC849E-C692-40DC-A335-EDA43027A9A5}
21{28810A0B-2097-42AD-AD1D-6227B147B893}fold, syncline, overturnedAs defined in the AGI Glossary of Geology, see term "syncline" that is modified by term "overturned".DAS12{28810A0B-2097-42AD-AD1D-6227B147B893}
22{1E5D6F53-4C62-4311-833A-3606B75E1D1E}foliationAs defined in the AGI Glossary of Geology, see term "foliation [struc geol]".DAS12{1E5D6F53-4C62-4311-833A-3606B75E1D1E}
23{B866BEEB-34DA-4DCF-BC34-961549B912B1}foliation, igneous, genericAs defined in the AGI Glossary of Geology, see term "primary foliation" formed in "igneous" rocks. See notes field for details.DAS12{B866BEEB-34DA-4DCF-BC34-961549B912B1}
24{5426F3A8-5CFA-458F-B834-E281F4279A39}generalizedThe feature's location confidence is primarily identified with the ordinal classification scheme used in the LocationConfidence field. The numeric value found in the LocationConfidenceMeters field is derived from this value and based on conversion logic found in the LocationConfidenceLookup table.DAS13{5426F3A8-5CFA-458F-B834-E281F4279A39}
25{8EE25CA0-7932-4725-BA3C-9DC71D4B2229}generic documentA generic document, such as a standards manual or guide.DAS13{8EE25CA0-7932-4725-BA3C-9DC71D4B2229}
26{FE1BBA2B-AFCC-4420-BF56-6BF62742B379}geochemAs defined in the AGI Glossary of Geology, see term "geochemistry".DAS12{FE1BBA2B-AFCC-4420-BF56-6BF62742B379}
27{B51DE02B-CCC8-4BA2-B678-E9FC3A005834}geochem, whole-rockAs defined in the AGI Glossary of Geology, see term "whole-rock".DAS12{B51DE02B-CCC8-4BA2-B678-E9FC3A005834}
28{363F81BA-2345-4FCB-88A7-173DF40661EC}geochronAs defined in the AGI Glossary of Geology, see term "geochronology".DAS12{363F81BA-2345-4FCB-88A7-173DF40661EC}
29{24BC4949-061A-4159-A4BB-15974BF2077E}geochron, U-PbAs defined in the AGI Glossary of Geology, see term "uranium-lead age method".DAS12{24BC4949-061A-4159-A4BB-15974BF2077E}
30{FD713C00-53D5-459F-AA1B-F8D6E29AEA01}geologic dataGeologic observations, analyses, or other information.DAS13{FD713C00-53D5-459F-AA1B-F8D6E29AEA01}
31{B2F78390-E157-4C14-A831-2E0C2D9A946C}geologic mappingA geologic map.DAS13{B2F78390-E157-4C14-A831-2E0C2D9A946C}
32{B693930F-8629-4388-8F3A-CB827AAB7FB9}geologic reportA written geologic report.DAS13{B693930F-8629-4388-8F3A-CB827AAB7FB9}
33{16D24830-990D-455C-B139-CAF7645692F0}geophysicsGeophysical data.DAS13{16D24830-990D-455C-B139-CAF7645692F0}
34{228466CD-5CD4-4FDE-9982-5EB977AFF534}geospatialData source has a defined geospatial area and may or may not have a related record defining that spatial area in the DataSourcePolygons feature class.DAS01{228466CD-5CD4-4FDE-9982-5EB977AFF534}
35{3F4998C9-61BC-4356-B409-E296276AECE8}graphicA visual object used on the map with no intent to correctly model and/or attribute a real-world physical feature.DAS13{3F4998C9-61BC-4356-B409-E296276AECE8}
36{378FD1FD-C9CE-46D2-944F-A51485BFC843}graphic, cross section lineA graphic line on the map indicating where a cross-section is generated.DAS13{378FD1FD-C9CE-46D2-944F-A51485BFC843}
37{78AEBD69-DB8F-43AC-A9F6-C16EE92CCC2D}highIndicates that the author has a high confidence in this value.DAS13{78AEBD69-DB8F-43AC-A9F6-C16EE92CCC2D}
38{8FE21F68-A895-4428-BCE4-3F815498476D}inferredIndicates that the author is not confident in the location of the feature, and its location is inferred to within the values indicated in the LocationConfidenceLookup table.DAS13{8FE21F68-A895-4428-BCE4-3F815498476D}
39{B4B7B619-0923-4846-926A-CF1EF8823A43}jointAs defined in the AGI Glossary of Geology, see term "joint [struc geol]".DAS12{B4B7B619-0923-4846-926A-CF1EF8823A43}
40{B45E5A6E-9D49-4D5E-B109-8B14C7C4A4CC}joint, minor, inclinedAs defined in the AGI Glossary of Geology, see term "joint [struc geol]" that is modified by term "inclination [slopes]" and described as small-scale.DAS12{B45E5A6E-9D49-4D5E-B109-8B14C7C4A4CC}
41{216D78E4-CCF5-42CE-AF67-E1403A6E6603}MaAge expressed as millions of years ago.DAS13{216D78E4-CCF5-42CE-AF67-E1403A6E6603}
42{504537C9-CF60-4509-95F6-B2BE1A1F2C4B}map unitAs defined in the AGI Glossary of Geology, see term "lithostratigraphic unit".DAS12{504537C9-CF60-4509-95F6-B2BE1A1F2C4B}
43{97B93EAB-7816-4DFD-B100-C7740FB02C12}map unit, genericAs defined in the AGI Glossary of Geology, see term "lithostratigraphic unit".DAS12{97B93EAB-7816-4DFD-B100-C7740FB02C12}
44{A542A424-BCE4-4E99-9A13-FA608FB3A7F9}mediumIndicates that the author is somewhat confident in this value.DAS13{A542A424-BCE4-4E99-9A13-FA608FB3A7F9}
45{EF96EDBE-4CD2-40FB-8A78-3312074DDD42}modifierA feature designed to visualize a modification of underlying map units. This modification will be "burned" into the MapUnitPolys Modifier field at publication time.DAS13{EF96EDBE-4CD2-40FB-8A78-3312074DDD42}
46{13D528E1-5316-4C8A-9443-4A4604AC5DDF}modifier, weldedA feature designed to visualize a modification of underlying map units. This modification will be "burned" in to the MapUnitPolys Modifier field at publication time. As defined in the AGI Glossary of Geology, see term "welding".DAS12{13D528E1-5316-4C8A-9443-4A4604AC5DDF}
47{CA75E67B-6B6A-4F99-AB14-1DE4EA885E15}non-geospatialData source does not have a defined geospatial area.DAS13{CA75E67B-6B6A-4F99-AB14-1DE4EA885E15}
48{7962068B-0A94-4D7D-A521-02E8EC7BFB29}questionableIndicates that the author is not confident in the scientific credibility of the existence of the feature.DAS13{7962068B-0A94-4D7D-A521-02E8EC7BFB29}
49{342BE5F6-F6DC-4545-853A-9E610E6F6915}rhyoliteAs defined in the AGI Glossary of Geology, see term "rhyolite".DAS12{342BE5F6-F6DC-4545-853A-9E610E6F6915}
50{1BFF43F5-E7B2-433B-B357-86FB5F8DA814}weldedA feature designed to visualize a modification of map units. As defined in the AGI Glossary of Geology, see term "welding".DAS12{1BFF43F5-E7B2-433B-B357-86FB5F8DA814}
51{CBA20229-F53A-4C23-ADAA-DEDB9AEC2E72}dmu, map unitDescription of Map Unit generic paragraph format for map units.DAS13{CBA20229-F53A-4C23-ADAA-DEDB9AEC2E72}
52{8BF1D45D-8E63-4F09-A0EE-170C314AB60A}relativeAge assignment is based on stratigraphic position.DAS13{8BF1D45D-8E63-4F09-A0EE-170C314AB60A}
53{EEC41761-B7E5-42E0-9B9C-502E917F602E}absoluteAge assignment is based on radiometric dating.DAS13{EEC41761-B7E5-42E0-9B9C-502E917F602E}

LocationConfidenceLookup

OBJECTIDLocationConfidenceLookup_IDScaleDenomAccurateMinAccurateDefaultAccurateMaxApproximateMinApproximateDefaultApproximateMaxInferredMinInferredDefaultInferredMaxGlobalIDUnprovidedLocationConfidence
1{5D0350C3-5346-4B93-BD45-5AE4BFFDE530}240000252526505051120None{5D0350C3-5346-4B93-BD45-5AE4BFFDE530}997
2{F9136468-6CA9-47E1-896C-F140693E6A51}500000505051100100101250None{F9136468-6CA9-47E1-896C-F140693E6A51}997
3{12390D62-CE9B-43AD-8AC4-8440C9E7C2EB}1000000100100101200200201500None{12390D62-CE9B-43AD-8AC4-8440C9E7C2EB}997
4{DF807FC9-7905-4A5A-94F5-E5BEC19FB303}5000000254254255508508509NoneNone{DF807FC9-7905-4A5A-94F5-E5BEC19FB303}997

OrientationConfidenceLookup

OBJECTIDOrientationConfidenceLookup_IDHighMinHighDefaultHighMaxMediumMinMediumDefaultMediumMaxLowMinLowDefaultLowMaxGlobalID
1{D1D1CFF0-7CB8-4847-B2A4-13E8BF043FCF}555610202120None{D1D1CFF0-7CB8-4847-B2A4-13E8BF043FCF}

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, 12 rows
DescriptionOfMapUnits, nonspatial table, 22 rows
GeoMaterialDict, nonspatial table, 101 rows
Glossary, nonspatial table, 35 rows
GlossaryFull, nonspatial table, 53 rows
LocationConfidenceLookup, nonspatial table, 4 rows
OrientationConfidenceLookup, nonspatial table, 1 rows
GeologicMap, feature dataset
OrientationPoints, simple point feature class, 234 rows
OverlayPolys, simple polygon feature class, 8 rows
StructureLines, simple polyline feature class, 4 rows
GeochemPoints, simple point feature class, 3 rows
GeochronPoints, simple point feature class, 8 rows
ContactsAndFaults, simple polyline feature class, 426 rows
MapUnitPolys, simple polygon feature class, 162 rows
CartographicLines, simple polyline feature class, 1 rows
Bond_GeologicMap_Topology, topology