| 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 |
| 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 |
| 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 |
| OBJECTID | DataSources_ID | Category | Type | Source | SourceBibRef | URL | Notes | GlobalID | /tr>/thead>
|---|---|---|---|---|---|---|---|---|
| 1/td> | DAS01/td> | geospatial/td> | geologic mapping/td> | McDonald, 2022/td> | McDonald, Catherine, 2022, Geologic map of the Bond 7.5' quadrangle, Beaverhead County, Montana: Montana Bureau of Mines and Geology Geologic Map 90, 1 sheet./td> | https://doi.org/10.59691/KETV8563/td> | This study./td> | {E4D29993-AFDB-4BFB-A37E-6A1FED9FCBEA}/td>/tr> |
| 2/td> | DAS02/td> | geospatial/td> | geologic data/td> | Mosolf and Kylander-Clark, 2023/td> | Mosolf, 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./td> | https://doi.org/10.59691/FIIS4856/td> | None/td> | {D54C07E0-E716-486E-BD9C-3B47C75C9BE6}/td>/tr> |
| 3/td> | DAS03/td> | non-geospatial/td> | geologic report/td> | Fritz and Sears, 1993/td> | Fritz, W.J., and Sears, J.W., 1993, Tectonics of the Yellowstone hotspot wake in southwestern Montana: Geology, v. 21, p. 427–430./td> | https://doi.org/10.1130/0091-7613(1993)021%3C0427:TOTYHW%3E2.3.CO;2/td> | None/td> | {6DE3F589-7E1E-435E-9D50-4BD575D61FE6}/td>/tr> |
| 4/td> | DAS04/td> | geospatial/td> | geophysics/td> | Hanna and others, 1993/td> | Hanna, 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./td> | https://doi.org/10.3133/i1803I/td> | None/td> | {3FB234D7-8968-473E-98F4-5E72B517510D}/td>/tr> |
| 5/td> | DAS05/td> | non-geospatial/td> | geologic report/td> | Matthews, 1989/td> | Matthews, 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./td> | None/td> | None/td> | {4E220ADC-8843-45D5-B06F-4A8AE2D498B5}/td>/tr> |
| 6/td> | DAS06/td> | geospatial/td> | geologic mapping/td> | Tysdal and others, 1994/td> | Tysdal, 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./td> | https://doi.org/10.3133/i2434/td> | None/td> | {80630B38-7E1C-4DEA-9745-A114F1E7B2FF}/td>/tr> |
| 7/td> | DAS07/td> | non-geospatial/td> | geologic report/td> | Dyman and Nichols, 1988/td> | Dyman, 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./td> | https://doi.org/10.3133/b1773/td> | None/td> | {BE6F4F56-D999-4668-A8DE-8FC868FA7E11}/td>/tr> |
| 8/td> | DAS08/td> | non-geospatial/td> | geologic report/td> | Dyman and Tysdal, 1998/td> | Dyman, 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./td> | None/td> | None/td> | {C8EF7CAD-BCCA-44E1-A19C-C055CFB1B1A8}/td>/tr> |
| 9/td> | DAS09/td> | non-geospatial/td> | geologic report/td> | Zartman and others, 1995/td> | Zartman, 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./td> | https://doi.org/10.3133/b2113/td> | None/td> | {C298CAFE-47B5-415B-A233-21BA1EBCFBD1}/td>/tr> |
| 11/td> | DAS11/td> | geospatial/td> | geologic mapping/td> | Yakovlev, 2019/td> | Yakovlev, 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./td> | https://www.mbmg.mtech.edu/mbmgcat/public/ListCitation.asp?pub_id=32166gsc.tab=0/td> | None/td> | {EE78D482-AF06-4CBA-B1FB-E742639C7E71}/td>/tr> |
| 12/td> | DAS12/td> | non-geospatial/td> | generic document/td> | AGI Glossary of Geology/td> | Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of Geology: Alexandria, Virginia, American Geological Institute, 799 p./td> | https://www.americangeosciences.org/pubs/glossary/td> | None/td> | {13CF0BBC-0063-43FE-9DAD-4088960B29F2}/td>/tr> |
| 14/td> | DAS13/td> | non-geospatial/td> | generic document/td> | AK GeMS Data Dictionary/td> | Hendricks, 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./td> | https://doi.org/10.14509/30669/td> | None/td> | {EB77AB96-60C8-4BFA-A0CE-94131E8A22FC}/td>/tr> |
| OBJECTID | DescriptionOfMapUnits_ID | Category | Type | Symbol | Label | MapUnit | Name | FullName | Age | AgeType | AgeOldest | AgeYoungest | Description | HierarchyKey | ParagraphStyle | AreaFillRGB | AreaFillPatternDescription | GeoMaterialDictID | GeoMaterial | GeoMaterialConfidence | Notes | DataSourceMethod | DescriptionSourceID | GlobalID | /tr>/thead>
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 10/td> | {77E73636-7A6E-4339-8FAB-C529B2244908}/td> | map unit/td> | map unit, generic/td> | 0010/td> | Qal/td> | Qal/td> | alluvium/td> | alluvium/td> | Quaternary/td> | relative/td> | Holocene/td> | Holocene/td> | Unconsolidated 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)./td> | 01/td> | dmu, map unit/td> | 255,255,222/td> | None/td> | {9681AE57-A86A-4E8B-8DD6-6103B1DB9517}/td> | Alluvial sediment, mostly coarse-grained/td> | high/td> | None/td> | 2/td> | DAS01/td> | {77E73636-7A6E-4339-8FAB-C529B2244908}/td>/tr> |
| 8/td> | {92575C43-C8BC-496E-9946-A50A4BD0409D}/td> | map unit/td> | map unit, generic/td> | A150/td> | Qac/td> | Qac/td> | alluvium and colluvium/td> | alluvium and colluvium/td> | Quaternary/td> | relative/td> | Pleistocene/td> | Holocene/td> | Unconsolidated 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)./td> | 02/td> | dmu, map unit/td> | 235,222,128/td> | None/td> | {9681AE57-A86A-4E8B-8DD6-6103B1DB9517}/td> | Alluvial sediment, mostly coarse-grained/td> | high/td> | None/td> | 2/td> | DAS01/td> | {92575C43-C8BC-496E-9946-A50A4BD0409D}/td>/tr> |
| 9/td> | {9798E13C-F980-46C0-85D0-636D88E5FDF6}/td> | map unit/td> | map unit, generic/td> | 0A60/td> | Qaf/td> | Qaf/td> | alluvial-fan deposit/td> | alluvial-fan deposit/td> | Quaternary/td> | relative/td> | Pleistocene/td> | Holocene/td> | Unconsolidated, poorly sorted, cobbles, gravel, sand, and silt forming fan-shaped deposit. Estimated thickness about 20 m (65 ft)./td> | 03/td> | dmu, map unit/td> | 255,235,102/td> | None/td> | {9681AE57-A86A-4E8B-8DD6-6103B1DB9517}/td> | Alluvial sediment, mostly coarse-grained/td> | high/td> | None/td> | 2/td> | DAS01/td> | {9798E13C-F980-46C0-85D0-636D88E5FDF6}/td>/tr> |
| 14/td> | {1CFABC8B-9FA9-475F-9151-86C9F6527ADC}/td> | map unit/td> | map unit, generic/td> | AA60/td> | Qls/td> | Qls/td> | landslide deposit/td> | landslide deposit/td> | Quaternary/td> | relative/td> | Pleistocene/td> | Holocene/td> | Mass-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)./td> | 04/td> | dmu, map unit/td> | 235,235,102/td> | None/td> | {017338DF-E8E0-4EE7-BAED-C9EBC828F436}/td> | Debris flows, landslides, and other localized mass-movement sediment/td> | high/td> | None/td> | 2/td> | DAS01/td> | {1CFABC8B-9FA9-475F-9151-86C9F6527ADC}/td>/tr> |
| 12/td> | {2F40CFE9-BAC5-4309-84B2-E078BE7F70EF}/td> | map unit/td> | map unit, generic/td> | 0AX0/td> | Qc/td> | Qc/td> | colluvium/td> | colluvium/td> | Quaternary/td> | relative/td> | Pleistocene/td> | Holocene/td> | Unconsolidated, 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)./td> | 05/td> | dmu, map unit/td> | 255,235,000/td> | None/td> | {6C2D6A29-29B2-4583-B4D5-D7B0A66B031F}/td> | Colluvium and other widespread mass-movement sediment/td> | high/td> | None/td> | 2/td> | DAS01/td> | {2F40CFE9-BAC5-4309-84B2-E078BE7F70EF}/td>/tr> |
| 13/td> | {498F1C9D-9F09-4A5A-9259-C77733EB4BAE}/td> | map unit/td> | map unit, generic/td> | 0170/td> | Qdf/td> | Qdf/td> | debris-flow deposit/td> | debris-flow deposit/td> | Quaternary/td> | relative/td> | Pleistocene/td> | Holocene/td> | Angular, 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)./td> | 06/td> | dmu, map unit/td> | 255,222,077/td> | None/td> | {017338DF-E8E0-4EE7-BAED-C9EBC828F436}/td> | Debris flows, landslides, and other localized mass-movement sediment/td> | high/td> | None/td> | 2/td> | DAS01/td> | {498F1C9D-9F09-4A5A-9259-C77733EB4BAE}/td>/tr> |
| 11/td> | {4CBD0B28-E3EA-45AA-BE08-0F328276B861}/td> | map unit/td> | map unit, generic/td> | AA40/td> | Qalo/td> | Qalo/td> | alluvium, older/td> | alluvium, older/td> | Quaternary/td> | relative/td> | Pleistocene/td> | Holocene/td> | Unconsolidated, 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)./td> | 07/td> | dmu, map unit/td> | 235,235,153/td> | None/td> | {9681AE57-A86A-4E8B-8DD6-6103B1DB9517}/td> | Alluvial sediment, mostly coarse-grained/td> | high/td> | None/td> | 2/td> | DAS01/td> | {4CBD0B28-E3EA-45AA-BE08-0F328276B861}/td>/tr> |
| 22/td> | {03955394-A0A7-4A75-861F-61FE7F187C93}/td> | map unit/td> | map unit, generic/td> | 0480/td> | Tsc/td> | Tsc/td> | Sixmile Creek Formation/td> | Sixmile Creek Formation of Bozeman Group/td> | Tertiary/td> | absolute/td> | Pliocene/td> | Miocene/td> | Pale 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./td> | 08/td> | dmu, map unit/td> | 255,153,051/td> | None/td> | {CDF81738-6203-4D80-B211-331B436FC586}/td> | Sedimentary and extrusive igneous material/td> | medium/td> | None/td> | 2/td> | DAS01 | DAS03/td> | {03955394-A0A7-4A75-861F-61FE7F187C93}/td>/tr> |
| 21/td> | {618E76D2-9045-4F1F-89E9-1C897C81AB38}/td> | map unit/td> | map unit, generic/td> | A270/td> | Tre/td> | Tre/td> | Renova Formation/td> | Renova Formation of Bozeman Group/td> | Tertiary/td> | relative/td> | Miocene/td> | Eocene/td> | Very 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)./td> | 09/td> | dmu, map unit/td> | 235,204,077/td> | None/td> | {9681AE57-A86A-4E8B-8DD6-6103B1DB9517}/td> | Alluvial sediment, mostly coarse-grained/td> | medium/td> | None/td> | 2/td> | DAS01 | DAS04/td> | {618E76D2-9045-4F1F-89E9-1C897C81AB38}/td>/tr> |
| 17/td> | {1A715CAA-483D-4221-B9E4-1D61EDAD69D6}/td> | map unit/td> | map unit, generic/td> | 1370/td> | Tbr/td> | Tbr/td> | volcanic breccia/td> | volcanic breccia/td> | Tertiary/td> | relative/td> | Eocene/td> | Eocene/td> | Grayish, 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)./td> | 10/td> | dmu, map unit/td> | 222,178,077/td> | None/td> | {5F3BE483-53E9-4A2A-BC9B-EFA727244C5B}/td> | Felsic-composition pyroclastic flows/td> | high/td> | None/td> | 2/td> | DAS01 | DAS05/td> | {1A715CAA-483D-4221-B9E4-1D61EDAD69D6}/td>/tr> |
| 16/td> | {8527423A-9011-46AC-A1E7-F526B3B3445C}/td> | map unit/td> | map unit, generic/td> | 27A0/td> | Tbmt/td> | Tbmt/td> | Burns Mountain tuff/td> | Burns Mountain tuff/td> | Tertiary/td> | absolute/td> | Eocene/td> | Eocene/td> | Massive, 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)./td> | 11/td> | dmu, map unit/td> | 204,077,235/td> | None/td> | {5F3BE483-53E9-4A2A-BC9B-EFA727244C5B}/td> | Felsic-composition pyroclastic flows/td> | high/td> | None/td> | 2/td> | DAS01/td> | {8527423A-9011-46AC-A1E7-F526B3B3445C}/td>/tr> |
| 15/td> | {EB9AB8BB-6691-45C0-B4DB-FF3818C5FBCB}/td> | map unit/td> | map unit, generic/td> | 2420/td> | Tan/td> | Tan/td> | andesite flows/td> | andesite flows/td> | Tertiary/td> | relative/td> | Eocene/td> | Eocene/td> | Dark 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./td> | 12/td> | dmu, map unit/td> | 235,077,077/td> | None/td> | {37FCE4C5-5C59-4925-822E-6E892B69B4DE}/td> | Fine-grained, intermediate-composition intrusive igneous rock/td> | high/td> | None/td> | 2/td> | DAS01/td> | {EB9AB8BB-6691-45C0-B4DB-FF3818C5FBCB}/td>/tr> |
| 19/td> | {0CA70F36-7A54-402B-B8DC-3C6A11361232}/td> | map unit/td> | map unit, generic/td> | 5700/td> | Thgt/td> | Thgt/td> | Hennbury Gulch tuff/td> | Hennbury Gulch tuff/td> | Tertiary/td> | absolute/td> | Eocene/td> | Eocene/td> | White 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)./td> | 13/td> | dmu, map unit/td> | 128,077,255/td> | None/td> | {5F3BE483-53E9-4A2A-BC9B-EFA727244C5B}/td> | Felsic-composition pyroclastic flows/td> | high/td> | None/td> | 2/td> | DAS01/td> | {0CA70F36-7A54-402B-B8DC-3C6A11361232}/td>/tr> |
| 18/td> | {7F7BD027-8926-4F40-B875-8635A2669A73}/td> | map unit/td> | map unit, generic/td> | 2300/td> | Tdwr/td> | Tdwr/td> | Dillon West rhyolite/td> | Dillon West rhyolite/td> | Tertiary/td> | absolute/td> | Eocene/td> | Eocene/td> | Moderate 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)./td> | 14/td> | dmu, map unit/td> | 204,178,255/td> | None/td> | {AAA1DC43-47DB-4FA8-8160-962345918502}/td> | Felsic-composition lava flows/td> | high/td> | None/td> | 2/td> | DAS01/td> | {7F7BD027-8926-4F40-B875-8635A2669A73}/td>/tr> |
| 5/td> | {CC5DEA22-E849-4B09-AF53-833FE5D31DA1}/td> | map unit/td> | map unit, generic/td> | 4160/td> | Kf/td> | Kf/td> | Frontier Formation/td> | Frontier Formation/td> | Late Cretaceous/td> | absolute/td> | Late Cretaceous/td> | Late Cretaceous/td> | Dominantly 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)./td> | 15/td> | dmu, map unit/td> | 153,222,102/td> | None/td> | {AB5A96BE-7478-43F0-8902-44A5D21B9FE7}/td> | Sandstone and mudstone/td> | medium/td> | None/td> | 2/td> | DAS01 | DAS06 | DAS07/td> | {CC5DEA22-E849-4B09-AF53-833FE5D31DA1}/td>/tr> |
| 4/td> | {C8C3EB3E-5DEF-49EA-862C-2A32B13A1E01}/td> | map unit/td> | map unit, generic/td> | 4040/td> | Kblv/td> | Kblv/td> | Vaughn Member/td> | Vaughn Member of the Blackleaf Formation of Colorado Group/td> | Cretaceous/td> | relative/td> | Early Cretaceous/td> | Late Cretaceous/td> | Olive 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./td> | 16/td> | dmu, map unit/td> | 153,255,153/td> | None/td> | {AB5A96BE-7478-43F0-8902-44A5D21B9FE7}/td> | Sandstone and mudstone/td> | high/td> | None/td> | 2/td> | DAS01 | DAS06 | DAS08 | DAS09/td> | {C8C3EB3E-5DEF-49EA-862C-2A32B13A1E01}/td>/tr> |
| 3/td> | {476D8C22-844C-4D0F-8263-EB15788F94C8}/td> | map unit/td> | map unit, generic/td> | X470/td> | Kblf/td> | Kblf/td> | Flood Member/td> | Flood Member of the Blackleaf Formation of Colorado Group/td> | Early Cretaceous/td> | relative/td> | Early Cretaceous/td> | Early Cretaceous/td> | Upper 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)./td> | 17/td> | dmu, map unit/td> | 000,153,077/td> | None/td> | {AB5A96BE-7478-43F0-8902-44A5D21B9FE7}/td> | Sandstone and mudstone/td> | high/td> | None/td> | 2/td> | DAS01 | DAS06 | DAS07/td> | {476D8C22-844C-4D0F-8263-EB15788F94C8}/td>/tr> |
| 6/td> | {7C84EF1C-E907-4466-9FED-9DB8FFDD8EF1}/td> | map unit/td> | map unit, generic/td> | 72X0/td> | Kk/td> | Kk/td> | Kootenai Formation/td> | Kootenai Formation/td> | Early Cretaceous/td> | relative/td> | Early Cretaceous/td> | Early Cretaceous/td> | Mapped 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./td> | 18/td> | dmu, map unit/td> | 077,204,000/td> | None/td> | {AB5A96BE-7478-43F0-8902-44A5D21B9FE7}/td> | Sandstone and mudstone/td> | medium/td> | None/td> | 2/td> | DAS01 | DAS06 | DAS07/td> | {7C84EF1C-E907-4466-9FED-9DB8FFDD8EF1}/td>/tr> |
| 2/td> | {D775E555-9C14-4E7F-8A7E-2EF37DEDEA75}/td> | map unit/td> | map unit, generic/td> | 3A30/td> | Jm/td> | Jm/td> | Morrison Formation/td> | Morrison Formation/td> | Jurassic/td> | relative/td> | Jurassic/td> | Jurassic/td> | Green, 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)./td> | 19/td> | dmu, map unit/td> | 178,235,178/td> | None/td> | {2D09A5AE-F0AD-462B-84BC-4092CE922275}/td> | Mostly mudstone/td> | high/td> | None/td> | 2/td> | DAS01/td> | {D775E555-9C14-4E7F-8A7E-2EF37DEDEA75}/td>/tr> |
| 20/td> | {84A5E08C-4398-45BC-A6A5-E33390E66536}/td> | map unit/td> | map unit, generic/td> | 5120/td> | ^d/td> | TRd/td> | Dinwoody Formation/td> | Dinwoody Formation/td> | Lower Triassic/td> | relative/td> | Lower Triassic/td> | Lower Triassic/td> | Interbedded 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)./td> | 20/td> | dmu, map unit/td> | 128,222,204/td> | None/td> | {31CBE54B-0B07-457B-8AC5-A73AB365E34C}/td> | Mostly carbonate rock/td> | medium/td> | None/td> | 2/td> | DAS01/td> | {84A5E08C-4398-45BC-A6A5-E33390E66536}/td>/tr> |
| 7/td> | {8321432E-305E-4A64-80BB-62AECEC86FE5}/td> | map unit/td> | map unit, generic/td> | 62A0/td> | Psp/td> | Psp/td> | Shedhorn and Phosphoria Formations, undivided/td> | Shedhorn and Phosphoria Formations, undivided/td> | Permian/td> | relative/td> | Permian/td> | Permian/td> | Shedhorn 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)./td> | 21/td> | dmu, map unit/td> | 102,204,235/td> | None/td> | {FDA3C54D-61D0-4798-ACC3-21A2F1270733}/td> | Mostly sandstone/td> | medium/td> | None/td> | 2/td> | DAS01/td> | {8321432E-305E-4A64-80BB-62AECEC86FE5}/td>/tr> |
| 1/td> | {887C0703-06B3-4AB3-B172-8379275271B5}/td> | map unit/td> | map unit, generic/td> | 4A00/td> | *q/td> | IPq/td> | Quadrant Formation/td> | Quadrant Formation/td> | Pennsylvanian/td> | relative/td> | Pennsylvanian/td> | Pennsylvanian/td> | Light 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)./td> | 22/td> | dmu, map unit/td> | 153,235,255/td> | None/td> | {BA96A3AA-660F-4C81-87EB-463C01EB9F06}/td> | Sandstone/td> | high/td> | None/td> | 2/td> | DAS01 | DAS11/td> | {887C0703-06B3-4AB3-B172-8379275271B5}/td>/tr> |
| OBJECTID | Glossary_ID | Term | Definition | DefinitionSourceID | GlobalID | /tr>/thead>
|---|---|---|---|---|---|
| 1/td> | {4D4B6B03-B085-4315-953C-D960399042DB}/td> | 2 sigma/td> | 2 sigma error of measure. Standard deviation multiplied by 2./td> | DAS01/td> | {4D4B6B03-B085-4315-953C-D960399042DB}/td>/tr> |
| 52/td> | {E371EA80-9938-47E4-B868-1D420E4B9621}/td> | absolute/td> | Age assignment is based on radiometric dating./td> | DAS13/td> | {E371EA80-9938-47E4-B868-1D420E4B9621}/td>/tr> |
| 2/td> | {0E4FA450-A054-4A07-88EF-781C3A37A805}/td> | accurate/td> | Indicates 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./td> | DAS13/td> | {0E4FA450-A054-4A07-88EF-781C3A37A805}/td>/tr> |
| 4/td> | {9365EF45-053C-4B25-B5E3-FCA632410259}/td> | approximate/td> | Indicates 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./td> | DAS13/td> | {9365EF45-053C-4B25-B5E3-FCA632410259}/td>/tr> |
| 6/td> | {1D7F66B4-2D1B-44A9-A383-0CF397DB7529}/td> | bedding, generic/td> | As defined in the AGI Glossary of Geology, see term "bed [stratig]"./td> | DAS12/td> | {1D7F66B4-2D1B-44A9-A383-0CF397DB7529}/td>/tr> |
| 8/td> | {F69E3AD7-8364-4257-9247-C0441DA1581D}/td> | boundary, map/td> | A linear feature indicating where one map unit ends at the map boundary./td> | DAS13/td> | {F69E3AD7-8364-4257-9247-C0441DA1581D}/td>/tr> |
| 9/td> | {F430FD17-8A0B-4ADD-ABFA-91CC4523A09E}/td> | certain/td> | Indicates that the author is reasonably confident in the scientific credibility of the existence of the feature./td> | DAS13/td> | {F430FD17-8A0B-4ADD-ABFA-91CC4523A09E}/td>/tr> |
| 11/td> | {23E3F406-B26F-4E33-9238-0F187708B563}/td> | contact, generic/td> | A linear feature indicating where two map units meet. As defined in the AGI Glossary of Geology, see term "contact"./td> | DAS12 | DAS13/td> | {23E3F406-B26F-4E33-9238-0F187708B563}/td>/tr> |
| 12/td> | {FDC3B1DC-ED24-4AFA-9404-434285E58187}/td> | contact, internal extent of modified map unit/td> | The internal extent boundary of modified portion of underlaying map unit. Symbolized as a zero-point line to avoid being displayed./td> | DAS01/td> | {FDC3B1DC-ED24-4AFA-9404-434285E58187}/td>/tr> |
| 51/td> | {5CC01CD6-E557-43FA-8DF4-0BA4DEE05251}/td> | dmu, map unit/td> | Description of Map Unit generic paragraph format for map units./td> | DAS13/td> | {5CC01CD6-E557-43FA-8DF4-0BA4DEE05251}/td>/tr> |
| 15/td> | {B72E8DA0-68E9-4109-9E73-CD02C789B6D5}/td> | fault, decoration, apparent offset/td> | A 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./td> | DAS12 | DAS13/td> | {B72E8DA0-68E9-4109-9E73-CD02C789B6D5}/td>/tr> |
| 16/td> | {623310D5-8447-4397-8EA2-9E944F202B01}/td> | fault, generic/td> | As defined in the AGI Glossary of Geology, see term "fault [struc geol]"./td> | DAS12/td> | {623310D5-8447-4397-8EA2-9E944F202B01}/td>/tr> |
| 17/td> | {6B6F10D7-C016-4412-BA90-24894CE4C0D7}/td> | fault, normal/td> | As defined in the AGI Glossary of Geology, see term "normal fault"./td> | DAS12/td> | {6B6F10D7-C016-4412-BA90-24894CE4C0D7}/td>/tr> |
| 18/td> | {F9963147-C6EE-459A-B801-B261FCF10FC8}/td> | fault, thrust/td> | As defined in the AGI Glossary of Geology, see term "thrust fault"./td> | DAS12/td> | {F9963147-C6EE-459A-B801-B261FCF10FC8}/td>/tr> |
| 20/td> | {9E5602D7-4D7A-4FC4-A4CD-89E34C8AA698}/td> | fold, anticline, overturned/td> | As defined in the AGI Glossary of Geology, see term "anticline" that is modified by term "overturned"./td> | DAS12/td> | {9E5602D7-4D7A-4FC4-A4CD-89E34C8AA698}/td>/tr> |
| 21/td> | {7C4FC010-E2F8-4CBC-9EF9-62E478E6DC53}/td> | fold, syncline, overturned/td> | As defined in the AGI Glossary of Geology, see term "syncline" that is modified by term "overturned"./td> | DAS12/td> | {7C4FC010-E2F8-4CBC-9EF9-62E478E6DC53}/td>/tr> |
| 23/td> | {2E414A8F-94FB-497A-BDE6-7FA9780B70C1}/td> | foliation, igneous, generic/td> | As defined in the AGI Glossary of Geology, see term "primary foliation" formed in "igneous" rocks. See notes field for details./td> | DAS12/td> | {2E414A8F-94FB-497A-BDE6-7FA9780B70C1}/td>/tr> |
| 24/td> | {BD659594-7995-44F8-A692-32EDE4672A54}/td> | generalized/td> | The 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./td> | DAS13/td> | {BD659594-7995-44F8-A692-32EDE4672A54}/td>/tr> |
| 25/td> | {C289C0F1-3E96-4857-AA54-D98810687C44}/td> | generic document/td> | A generic document, such as a standards manual or guide./td> | DAS13/td> | {C289C0F1-3E96-4857-AA54-D98810687C44}/td>/tr> |
| 27/td> | {B2F09D60-A4B4-4217-AB3C-E62EF1705948}/td> | geochem, whole-rock/td> | As defined in the AGI Glossary of Geology, see term "whole-rock"./td> | DAS12/td> | {B2F09D60-A4B4-4217-AB3C-E62EF1705948}/td>/tr> |
| 29/td> | {A647A047-462D-4A3C-948A-96F593AE402C}/td> | geochron, U-Pb/td> | As defined in the AGI Glossary of Geology, see term "uranium-lead age method"./td> | DAS12/td> | {A647A047-462D-4A3C-948A-96F593AE402C}/td>/tr> |
| 30/td> | {458FD00E-052F-41A6-9E56-49C3A2EC4207}/td> | geologic data/td> | Geologic observations, analyses, or other information./td> | DAS13/td> | {458FD00E-052F-41A6-9E56-49C3A2EC4207}/td>/tr> |
| 31/td> | {09DEFEE5-9188-41C9-B2FC-28A24AA168D2}/td> | geologic mapping/td> | A geologic map./td> | DAS13/td> | {09DEFEE5-9188-41C9-B2FC-28A24AA168D2}/td>/tr> |
| 32/td> | {03360EBB-37BB-47B2-A3A7-359DBB22C978}/td> | geologic report/td> | A written geologic report./td> | DAS13/td> | {03360EBB-37BB-47B2-A3A7-359DBB22C978}/td>/tr> |
| 33/td> | {F77B4F4A-7369-498D-9E97-2A053D1F6A16}/td> | geophysics/td> | Geophysical data./td> | DAS13/td> | {F77B4F4A-7369-498D-9E97-2A053D1F6A16}/td>/tr> |
| 36/td> | {35457379-58A0-434B-810A-6596B30101F7}/td> | graphic, cross section line/td> | A graphic line on the map indicating where a cross-section is generated./td> | DAS13/td> | {35457379-58A0-434B-810A-6596B30101F7}/td>/tr> |
| 37/td> | {783260FD-A7E6-465E-BA64-812124C9194F}/td> | high/td> | Indicates that the author has a high confidence in this value./td> | DAS13/td> | {783260FD-A7E6-465E-BA64-812124C9194F}/td>/tr> |
| 38/td> | {847B16F4-538F-410E-A5F1-2E0DAB7297AE}/td> | inferred/td> | Indicates 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./td> | DAS13/td> | {847B16F4-538F-410E-A5F1-2E0DAB7297AE}/td>/tr> |
| 40/td> | {F7401311-275C-44D7-B9E0-39A4112FAA63}/td> | joint, minor, inclined/td> | As defined in the AGI Glossary of Geology, see term "joint [struc geol]" that is modified by term "inclination [slopes]" and described as small-scale./td> | DAS12/td> | {F7401311-275C-44D7-B9E0-39A4112FAA63}/td>/tr> |
| 41/td> | {9FBDC2BA-D4F3-4351-9310-434D6819AB64}/td> | Ma/td> | Age expressed as millions of years ago./td> | DAS13/td> | {9FBDC2BA-D4F3-4351-9310-434D6819AB64}/td>/tr> |
| 43/td> | {3D630C79-99DC-46C3-9F1F-178256088797}/td> | map unit, generic/td> | As defined in the AGI Glossary of Geology, see term "lithostratigraphic unit"./td> | DAS12/td> | {3D630C79-99DC-46C3-9F1F-178256088797}/td>/tr> |
| 44/td> | {1D052B21-683B-4FD3-BF77-48C373959FE7}/td> | medium/td> | Indicates that the author is somewhat confident in this value./td> | DAS13/td> | {1D052B21-683B-4FD3-BF77-48C373959FE7}/td>/tr> |
| 46/td> | {6E46140A-4811-41A4-BF93-F014AD4A886E}/td> | modifier, welded/td> | A 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"./td> | DAS12/td> | {6E46140A-4811-41A4-BF93-F014AD4A886E}/td>/tr> |
| 48/td> | {06995FA4-0D89-454F-9B9A-18FE25B7E181}/td> | questionable/td> | Indicates that the author is not confident in the scientific credibility of the existence of the feature./td> | DAS13/td> | {06995FA4-0D89-454F-9B9A-18FE25B7E181}/td>/tr> |
| 53/td> | {3538C07F-3A37-45FA-B958-4AF576D12891}/td> | relative/td> | Age assignment is based on stratigraphic position./td> | DAS13/td> | {3538C07F-3A37-45FA-B958-4AF576D12891}/td>/tr> |
| OBJECTID | GlossaryFull_ID | Term | Definition | DefinitionSourceID | GlobalID | /tr>/thead>
|---|---|---|---|---|---|
| 1/td> | {AF791317-93BC-4EDD-A0FC-5AB2218B1B3D}/td> | 2 sigma/td> | 2 sigma error of measure. Standard deviation multiplied by 2./td> | DAS01/td> | {AF791317-93BC-4EDD-A0FC-5AB2218B1B3D}/td>/tr> |
| 2/td> | {62A68133-DB89-4A50-9879-12E0E633BA48}/td> | accurate/td> | Indicates 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./td> | DAS13/td> | {62A68133-DB89-4A50-9879-12E0E633BA48}/td>/tr> |
| 3/td> | {0C8D63C0-82FE-4555-83A9-0A1B76BF348D}/td> | andesite/td> | As defined in the AGI Glossary of Geology, see term "adesite"./td> | DAS12/td> | {0C8D63C0-82FE-4555-83A9-0A1B76BF348D}/td>/tr> |
| 4/td> | {0B9BE30C-34F7-41F3-9E2D-2B2867670B85}/td> | approximate/td> | Indicates 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./td> | DAS13/td> | {0B9BE30C-34F7-41F3-9E2D-2B2867670B85}/td>/tr> |
| 5/td> | {4AA51D32-3556-4042-8486-625D4FF9089C}/td> | bedding/td> | As defined in the AGI Glossary of Geology, see term "bed [stratig]"./td> | DAS12/td> | {4AA51D32-3556-4042-8486-625D4FF9089C}/td>/tr> |
| 6/td> | {058B980D-D07C-4302-AB32-BEEE063501A6}/td> | bedding, generic/td> | As defined in the AGI Glossary of Geology, see term "bed [stratig]"./td> | DAS12/td> | {058B980D-D07C-4302-AB32-BEEE063501A6}/td>/tr> |
| 7/td> | {0FE3847E-7C5B-4CD3-B985-F5B5E838AFD0}/td> | boundary/td> | A linear feature indicating where one map unit ends without an adjacent map unit./td> | DAS13/td> | {0FE3847E-7C5B-4CD3-B985-F5B5E838AFD0}/td>/tr> |
| 8/td> | {074A330F-2BEE-45F9-9CE4-BB411D35C0FA}/td> | boundary, map/td> | A linear feature indicating where one map unit ends at the map boundary./td> | DAS13/td> | {074A330F-2BEE-45F9-9CE4-BB411D35C0FA}/td>/tr> |
| 9/td> | {0B78405B-52C9-46AA-BBDE-644031079C3F}/td> | certain/td> | Indicates that the author is reasonably confident in the scientific credibility of the existence of the feature./td> | DAS13/td> | {0B78405B-52C9-46AA-BBDE-644031079C3F}/td>/tr> |
| 10/td> | {F588CBAF-DDEB-401C-B223-15D2396461F9}/td> | contact/td> | A linear feature indicating where two map units meet. As defined in the AGI Glossary of Geology, see term "contact"./td> | DAS12 | DAS13/td> | {F588CBAF-DDEB-401C-B223-15D2396461F9}/td>/tr> |
| 11/td> | {D11D0C58-BB3A-4C2A-8334-A73019912A18}/td> | contact, generic/td> | A linear feature indicating where two map units meet. As defined in the AGI Glossary of Geology, see term "contact"./td> | DAS12 | DAS13/td> | {D11D0C58-BB3A-4C2A-8334-A73019912A18}/td>/tr> |
| 12/td> | {91A4A53D-A915-4821-B90B-E60BA176784C}/td> | contact, internal extent of modified map unit/td> | The internal extent boundary of modified portion of underlaying map unit. Symbolized as a zero-point line to avoid being displayed./td> | DAS01/td> | {91A4A53D-A915-4821-B90B-E60BA176784C}/td>/tr> |
| 13/td> | {8695554C-C3E2-4C21-B6FD-59E93FCD5520}/td> | dacite/td> | As defined in the AGI Glossary of Geology, see term "dacite"./td> | DAS12/td> | {8695554C-C3E2-4C21-B6FD-59E93FCD5520}/td>/tr> |
| 14/td> | {AFA15143-F1E8-4DEC-8E87-30C8D6D8DF5E}/td> | fault/td> | As defined in the AGI Glossary of Geology, see term "fault [struc geol]"./td> | DAS12/td> | {AFA15143-F1E8-4DEC-8E87-30C8D6D8DF5E}/td>/tr> |
| 15/td> | {F7DEF9D1-12F3-4D28-8FFD-69F539682F72}/td> | fault, decoration, apparent offset/td> | A 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./td> | DAS12 | DAS13/td> | {F7DEF9D1-12F3-4D28-8FFD-69F539682F72}/td>/tr> |
| 16/td> | {6AEC57D8-63CD-4606-BD66-417A0E3A3DA6}/td> | fault, generic/td> | As defined in the AGI Glossary of Geology, see term "fault [struc geol]"./td> | DAS12/td> | {6AEC57D8-63CD-4606-BD66-417A0E3A3DA6}/td>/tr> |
| 17/td> | {7C9E315A-626F-4A07-B265-E5B5C1308B9B}/td> | fault, normal/td> | As defined in the AGI Glossary of Geology, see term "normal fault"./td> | DAS12/td> | {7C9E315A-626F-4A07-B265-E5B5C1308B9B}/td>/tr> |
| 18/td> | {9C42C5A0-7634-4CBD-A58B-AED3ADE460F0}/td> | fault, thrust/td> | As defined in the AGI Glossary of Geology, see term "thrust fault"./td> | DAS12/td> | {9C42C5A0-7634-4CBD-A58B-AED3ADE460F0}/td>/tr> |
| 19/td> | {9BE3A33F-FF34-463D-8C7F-B3D49092709F}/td> | fold/td> | As defined in the AGI Glossary of Geology, see term "fold [struc geol]"./td> | DAS12/td> | {9BE3A33F-FF34-463D-8C7F-B3D49092709F}/td>/tr> |
| 20/td> | {8DAC849E-C692-40DC-A335-EDA43027A9A5}/td> | fold, anticline, overturned/td> | As defined in the AGI Glossary of Geology, see term "anticline" that is modified by term "overturned"./td> | DAS12/td> | {8DAC849E-C692-40DC-A335-EDA43027A9A5}/td>/tr> |
| 21/td> | {28810A0B-2097-42AD-AD1D-6227B147B893}/td> | fold, syncline, overturned/td> | As defined in the AGI Glossary of Geology, see term "syncline" that is modified by term "overturned"./td> | DAS12/td> | {28810A0B-2097-42AD-AD1D-6227B147B893}/td>/tr> |
| 22/td> | {1E5D6F53-4C62-4311-833A-3606B75E1D1E}/td> | foliation/td> | As defined in the AGI Glossary of Geology, see term "foliation [struc geol]"./td> | DAS12/td> | {1E5D6F53-4C62-4311-833A-3606B75E1D1E}/td>/tr> |
| 23/td> | {B866BEEB-34DA-4DCF-BC34-961549B912B1}/td> | foliation, igneous, generic/td> | As defined in the AGI Glossary of Geology, see term "primary foliation" formed in "igneous" rocks. See notes field for details./td> | DAS12/td> | {B866BEEB-34DA-4DCF-BC34-961549B912B1}/td>/tr> |
| 24/td> | {5426F3A8-5CFA-458F-B834-E281F4279A39}/td> | generalized/td> | The 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./td> | DAS13/td> | {5426F3A8-5CFA-458F-B834-E281F4279A39}/td>/tr> |
| 25/td> | {8EE25CA0-7932-4725-BA3C-9DC71D4B2229}/td> | generic document/td> | A generic document, such as a standards manual or guide./td> | DAS13/td> | {8EE25CA0-7932-4725-BA3C-9DC71D4B2229}/td>/tr> |
| 26/td> | {FE1BBA2B-AFCC-4420-BF56-6BF62742B379}/td> | geochem/td> | As defined in the AGI Glossary of Geology, see term "geochemistry"./td> | DAS12/td> | {FE1BBA2B-AFCC-4420-BF56-6BF62742B379}/td>/tr> |
| 27/td> | {B51DE02B-CCC8-4BA2-B678-E9FC3A005834}/td> | geochem, whole-rock/td> | As defined in the AGI Glossary of Geology, see term "whole-rock"./td> | DAS12/td> | {B51DE02B-CCC8-4BA2-B678-E9FC3A005834}/td>/tr> |
| 28/td> | {363F81BA-2345-4FCB-88A7-173DF40661EC}/td> | geochron/td> | As defined in the AGI Glossary of Geology, see term "geochronology"./td> | DAS12/td> | {363F81BA-2345-4FCB-88A7-173DF40661EC}/td>/tr> |
| 29/td> | {24BC4949-061A-4159-A4BB-15974BF2077E}/td> | geochron, U-Pb/td> | As defined in the AGI Glossary of Geology, see term "uranium-lead age method"./td> | DAS12/td> | {24BC4949-061A-4159-A4BB-15974BF2077E}/td>/tr> |
| 30/td> | {FD713C00-53D5-459F-AA1B-F8D6E29AEA01}/td> | geologic data/td> | Geologic observations, analyses, or other information./td> | DAS13/td> | {FD713C00-53D5-459F-AA1B-F8D6E29AEA01}/td>/tr> |
| 31/td> | {B2F78390-E157-4C14-A831-2E0C2D9A946C}/td> | geologic mapping/td> | A geologic map./td> | DAS13/td> | {B2F78390-E157-4C14-A831-2E0C2D9A946C}/td>/tr> |
| 32/td> | {B693930F-8629-4388-8F3A-CB827AAB7FB9}/td> | geologic report/td> | A written geologic report./td> | DAS13/td> | {B693930F-8629-4388-8F3A-CB827AAB7FB9}/td>/tr> |
| 33/td> | {16D24830-990D-455C-B139-CAF7645692F0}/td> | geophysics/td> | Geophysical data./td> | DAS13/td> | {16D24830-990D-455C-B139-CAF7645692F0}/td>/tr> |
| 34/td> | {228466CD-5CD4-4FDE-9982-5EB977AFF534}/td> | geospatial/td> | Data source has a defined geospatial area and may or may not have a related record defining that spatial area in the DataSourcePolygons feature class./td> | DAS01/td> | {228466CD-5CD4-4FDE-9982-5EB977AFF534}/td>/tr> |
| 35/td> | {3F4998C9-61BC-4356-B409-E296276AECE8}/td> | graphic/td> | A visual object used on the map with no intent to correctly model and/or attribute a real-world physical feature./td> | DAS13/td> | {3F4998C9-61BC-4356-B409-E296276AECE8}/td>/tr> |
| 36/td> | {378FD1FD-C9CE-46D2-944F-A51485BFC843}/td> | graphic, cross section line/td> | A graphic line on the map indicating where a cross-section is generated./td> | DAS13/td> | {378FD1FD-C9CE-46D2-944F-A51485BFC843}/td>/tr> |
| 37/td> | {78AEBD69-DB8F-43AC-A9F6-C16EE92CCC2D}/td> | high/td> | Indicates that the author has a high confidence in this value./td> | DAS13/td> | {78AEBD69-DB8F-43AC-A9F6-C16EE92CCC2D}/td>/tr> |
| 38/td> | {8FE21F68-A895-4428-BCE4-3F815498476D}/td> | inferred/td> | Indicates 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./td> | DAS13/td> | {8FE21F68-A895-4428-BCE4-3F815498476D}/td>/tr> |
| 39/td> | {B4B7B619-0923-4846-926A-CF1EF8823A43}/td> | joint/td> | As defined in the AGI Glossary of Geology, see term "joint [struc geol]"./td> | DAS12/td> | {B4B7B619-0923-4846-926A-CF1EF8823A43}/td>/tr> |
| 40/td> | {B45E5A6E-9D49-4D5E-B109-8B14C7C4A4CC}/td> | joint, minor, inclined/td> | As defined in the AGI Glossary of Geology, see term "joint [struc geol]" that is modified by term "inclination [slopes]" and described as small-scale./td> | DAS12/td> | {B45E5A6E-9D49-4D5E-B109-8B14C7C4A4CC}/td>/tr> |
| 41/td> | {216D78E4-CCF5-42CE-AF67-E1403A6E6603}/td> | Ma/td> | Age expressed as millions of years ago./td> | DAS13/td> | {216D78E4-CCF5-42CE-AF67-E1403A6E6603}/td>/tr> |
| 42/td> | {504537C9-CF60-4509-95F6-B2BE1A1F2C4B}/td> | map unit/td> | As defined in the AGI Glossary of Geology, see term "lithostratigraphic unit"./td> | DAS12/td> | {504537C9-CF60-4509-95F6-B2BE1A1F2C4B}/td>/tr> |
| 43/td> | {97B93EAB-7816-4DFD-B100-C7740FB02C12}/td> | map unit, generic/td> | As defined in the AGI Glossary of Geology, see term "lithostratigraphic unit"./td> | DAS12/td> | {97B93EAB-7816-4DFD-B100-C7740FB02C12}/td>/tr> |
| 44/td> | {A542A424-BCE4-4E99-9A13-FA608FB3A7F9}/td> | medium/td> | Indicates that the author is somewhat confident in this value./td> | DAS13/td> | {A542A424-BCE4-4E99-9A13-FA608FB3A7F9}/td>/tr> |
| 45/td> | {EF96EDBE-4CD2-40FB-8A78-3312074DDD42}/td> | modifier/td> | A feature designed to visualize a modification of underlying map units. This modification will be "burned" into the MapUnitPolys Modifier field at publication time./td> | DAS13/td> | {EF96EDBE-4CD2-40FB-8A78-3312074DDD42}/td>/tr> |
| 46/td> | {13D528E1-5316-4C8A-9443-4A4604AC5DDF}/td> | modifier, welded/td> | A 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"./td> | DAS12/td> | {13D528E1-5316-4C8A-9443-4A4604AC5DDF}/td>/tr> |
| 47/td> | {CA75E67B-6B6A-4F99-AB14-1DE4EA885E15}/td> | non-geospatial/td> | Data source does not have a defined geospatial area./td> | DAS13/td> | {CA75E67B-6B6A-4F99-AB14-1DE4EA885E15}/td>/tr> |
| 48/td> | {7962068B-0A94-4D7D-A521-02E8EC7BFB29}/td> | questionable/td> | Indicates that the author is not confident in the scientific credibility of the existence of the feature./td> | DAS13/td> | {7962068B-0A94-4D7D-A521-02E8EC7BFB29}/td>/tr> |
| 49/td> | {342BE5F6-F6DC-4545-853A-9E610E6F6915}/td> | rhyolite/td> | As defined in the AGI Glossary of Geology, see term "rhyolite"./td> | DAS12/td> | {342BE5F6-F6DC-4545-853A-9E610E6F6915}/td>/tr> |
| 50/td> | {1BFF43F5-E7B2-433B-B357-86FB5F8DA814}/td> | welded/td> | A feature designed to visualize a modification of map units. As defined in the AGI Glossary of Geology, see term "welding"./td> | DAS12/td> | {1BFF43F5-E7B2-433B-B357-86FB5F8DA814}/td>/tr> |
| 51/td> | {CBA20229-F53A-4C23-ADAA-DEDB9AEC2E72}/td> | dmu, map unit/td> | Description of Map Unit generic paragraph format for map units./td> | DAS13/td> | {CBA20229-F53A-4C23-ADAA-DEDB9AEC2E72}/td>/tr> |
| 52/td> | {8BF1D45D-8E63-4F09-A0EE-170C314AB60A}/td> | relative/td> | Age assignment is based on stratigraphic position./td> | DAS13/td> | {8BF1D45D-8E63-4F09-A0EE-170C314AB60A}/td>/tr> |
| 53/td> | {EEC41761-B7E5-42E0-9B9C-502E917F602E}/td> | absolute/td> | Age assignment is based on radiometric dating./td> | DAS13/td> | {EEC41761-B7E5-42E0-9B9C-502E917F602E}/td>/tr> |
| OBJECTID | LocationConfidenceLookup_ID | ScaleDenom | AccurateMin | AccurateDefault | AccurateMax | ApproximateMin | ApproximateDefault | ApproximateMax | InferredMin | InferredDefault | InferredMax | GlobalID | UnprovidedLocationConfidence | /tr>/thead>
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 1/td> | {5D0350C3-5346-4B93-BD45-5AE4BFFDE530}/td> | 24000/td> | 0/td> | 25/td> | 25/td> | 26/td> | 50/td> | 50/td> | 51/td> | 120/td> | None/td> | {5D0350C3-5346-4B93-BD45-5AE4BFFDE530}/td> | 997/td>/tr> |
| 2/td> | {F9136468-6CA9-47E1-896C-F140693E6A51}/td> | 50000/td> | 0/td> | 50/td> | 50/td> | 51/td> | 100/td> | 100/td> | 101/td> | 250/td> | None/td> | {F9136468-6CA9-47E1-896C-F140693E6A51}/td> | 997/td>/tr> |
| 3/td> | {12390D62-CE9B-43AD-8AC4-8440C9E7C2EB}/td> | 100000/td> | 0/td> | 100/td> | 100/td> | 101/td> | 200/td> | 200/td> | 201/td> | 500/td> | None/td> | {12390D62-CE9B-43AD-8AC4-8440C9E7C2EB}/td> | 997/td>/tr> |
| 4/td> | {DF807FC9-7905-4A5A-94F5-E5BEC19FB303}/td> | 500000/td> | 0/td> | 254/td> | 254/td> | 255/td> | 508/td> | 508/td> | 509/td> | None/td> | None/td> | {DF807FC9-7905-4A5A-94F5-E5BEC19FB303}/td> | 997/td>/tr> |
| OBJECTID | OrientationConfidenceLookup_ID | HighMin | HighDefault | HighMax | MediumMin | MediumDefault | MediumMax | LowMin | LowDefault | LowMax | GlobalID | /tr>/thead>
|---|---|---|---|---|---|---|---|---|---|---|---|
| 1/td> | {D1D1CFF0-7CB8-4847-B2A4-13E8BF043FCF}/td> | 5/td> | 5/td> | 5/td> | 6/td> | 10/td> | 20/td> | 21/td> | 20/td> | None/td> | {D1D1CFF0-7CB8-4847-B2A4-13E8BF043FCF}/td>/tr> |