| 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 | PASS |
| 3.4 No missing terms in Glossary | PASS |
| 3.5 No unnecessary terms in Glossary | PASS |
| 3.6 No missing sources in DataSources | PASS |
| 3.7 No unnecessary sources in DataSources | PASS |
| 3.8 No map units without entries in DescriptionOfMapUnits | PASS |
| 3.9 No unnecessary map units in DescriptionOfMapUnits | PASS |
| 3.10 HierarchyKey values in DescriptionOfMapUnits are unique and well formed | PASS |
| 3.11 All values of GeoMaterial are defined in GeoMaterialDict. GeoMaterialDict is as specified in the GeMS standard | PASS |
| 3.12 No duplicate _ID values | PASS |
| 3.13 No zero-length, whitespace-only, or bad null values | PASS |
| MapUnit | DescriptionOfMapUnits | GeologicMap |
|---|---|---|
| Ysn | X | X |
| Kgd | X | X |
| Ysh | X | X |
| Yms3 | X | X |
| Qalo | X | X |
| Yms2 | X | X |
| Qaf | X | X |
| Ypg | X | X |
| Tdap | X | X |
| Tba | X | X |
| Trcp | X | X |
| Tbgr | X | X |
| Qal | X | X |
| Qls | X | X |
| Qgt | X | X |
| Kgb | X | X |
| pl | X | X |
| Qdf | X | X |
| Qm | X | X |
| QTm | X | X |
| Qpa | X | X |
| Qac | X | X |
| Trca | X | X |
| Qbgr | X | X |
| Tda | X | X |
| Ybo | X | X |
| OBJECTID | DataSources_ID | Category | Type | Source | SourceBibRef | URL | Notes | GlobalID |
|---|---|---|---|---|---|---|---|---|
| 1 | DAS01 | geospatial | geologic mapping | McDonald and others, 2016 | McDonald, C., Mosolf, J.G., and Vuke, S.M, 2016, Geologic map of the Finn 7.5' quadrangle, Lewis and Clark and Powell Counties, Montana: Montana Bureau of Mines and Geology Open-File Report 672, 1 sheet, scale 1:24,000. | https://www.mbmg.mtech.edu/mbmgcat/public/ListCitation.asp?pub_id=31816& | This study. | {EED8C60C-ABCB-43F2-AC69-BC5C45C9E6F1} |
| 2 | DAS02 | geospatial | geologic mapping | Schmidt and others, 1994 | Schmidt, R.G., Loen, J.S., Wallace, C.A., and Mehnert, H.H., 1994, Geology of the Elliston region, Powell, and Lewis and Clark Counties, Montana: U.S. Geological Survey Bulletin 2045, 25 p., scale 1:48,000. | https://pubs.usgs.gov/bul/2045/report.pdf | None | {8795EACF-BF00-4B51-99A1-C92925DED146} |
| 3 | DAS03 | non-geospatial | geologic report | Mosolf, 2015 | Mosolf, J.G. , 2015, Geologic field guide to the Tertiary volcanic rocks in the Elliston 30' x 60' quadrangle, west-central Montana: Northwest Geology, v. 44, p. 213-231. | https://mbmg.mtech.edu/pdf_trgs/NWG_44.pdf | None | {56687A8A-7AD9-475B-957F-65F5F4169CEB} |
| 4 | DAS04 | non-geospatial | geologic report | Pardee and Schrader, 1933 | Pardee, J.T., and Schrader, F.C., 1933, Metalliferous deposits of the Greater Helena Mining Region, Montana: U.S. Geological Survey Bulletin 842, 318 p | https://pubs.er.usgs.gov/publication/b842 | None | {D9446474-9BFF-4F69-B0A3-DA2FC1DBC705} |
| 5 | DAS05 | geospatial | geologic mapping | McDonald and others, 2016 | McDonald, C., Mosolf, J.G., Vuke, S.M., and Lonn, J.D., 2016, Geologic map of the Nevada Lake 7.5' quadrangle quadrangle, west-central Montana: Montana Bureau of Mines and Geology Open-File Report 673, scale 1:24,000. | https://www.mbmg.mtech.edu/mbmgcat/public/ListCitation.asp?pub_id=31817& | None | {93075BD1-7881-48C7-B626-D9573D590281} |
| 6 | DAS06 | geospatial | geologic mapping | Lonn and Vuke, 2015 | Lonn, J.D., and Vuke, S.W., 2015, Geologic map of the Ophir Creek 7.5' quadrangle, Lewis and Clark and Powell Counties, Montana: Montana Bureau of Mines and Geology Open-File Report 666, scale 1:24,000. | https://www.mbmg.mtech.edu/mbmgcat/public/ListCitation.asp?pub_id=31799& | None | {3C114540-844D-497F-9895-FE5F3E4FE9D2} |
| 7 | DAS07 | geospatial | geologic mapping | Lonn and others, 2010 | Lonn, J.D., McDonald, C., Sears, J.W., and Smith, L.N., 2010, Geologic map of the Missoula East 30' x 60' quadrangle, western Montana: Montana Bureau of Mines and Geology Open-File Report 593, 2 sheets, scale 1:100,000. | https://www.mbmg.mtech.edu/mbmgcat/public/ListCitation.asp?pub_id=31350& | None | {3D5917BF-7B4F-4255-B270-2A3FB9D2FF4F} |
| 8 | DAS08 | non-geospatial | geologic report | Loen, 1990 | Loen, J.S., 1990, Lode and placer gold deposits in the Ophir District, Powell and Lewis and Clark Counties, Montana: Fort Collins, Colo.,Colorado State University, Ph.D. dissertation, 268 p. | None | None | {BD08C03A-A9C6-4897-B8A7-23067EB26CC9} |
| 9 | DAS09 | non-geospatial | generic document | AGI Glossary of Geology | Neuendorf, 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/glossary | None | {6490DBDA-4B03-4C0A-B331-C7F5A2A3744A} |
| 10 | DAS10 | non-geospatial | generic document | AK GeMS Data Dictionary | 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. | https://doi.org/10.14509/30669 | None | {E7763B80-F523-466C-A8F6-4469AE0293C2} |
| 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 27 | {AEB4627B-FC0D-44A1-8C7A-545357D9C2E9} | header | header, generic | None | None | None | MAN-MADE FEATURES | MAN-MADE FEATURES | None | unprovided | None | None | None | 01 | dmu, header | None | None | None | None | None | None | 997 | DAS01 | {AEB4627B-FC0D-44A1-8C7A-545357D9C2E9} |
| 3 | {3A3C7430-B4DE-407C-A50E-E2222B20F288} | map unit | map unit, generic | 4770 | pl | pl | placer workings | placer workings | Quaternary: Anthropocene | unprovided | Holocene | Holocene | Areas of historical gold placer operations. | 01-01 | dmu, map unit | 153,77,77 | None | {C7111710-CE19-44B8-B9AB-DDC248DA8C1B} | "Made" or human-engineered land | high | None | 997 | DAS01 | {3A3C7430-B4DE-407C-A50E-E2222B20F288} |
| 28 | {D9AB34D4-EBB5-434F-B596-4F39BF239E6E} | header | header, generic | None | None | None | SURFICIAL DEPOSITS | SURFICIAL DEPOSITS | None | unprovided | None | None | None | 02 | dmu, header | None | None | None | None | None | None | 997 | DAS01 | {D9AB34D4-EBB5-434F-B596-4F39BF239E6E} |
| 6 | {5E2AF013-74CF-4277-A893-ACE983B94C7E} | map unit | map unit, generic | 0010 | Qal | Qal | alluvium | alluvium | Quaternary: Holocene | unprovided | Holocene | Holocene | Gravel, sand, silt, and clay along Nevada Creek and its tributaries. Clasts are generally rounded to subrounded, cobble size and smaller, but boulders also present. Thickness generally less than 10 m (33 ft). | 02-01 | dmu, map unit | 255,255,222 | None | {9681AE57-A86A-4E8B-8DD6-6103B1DB9517} | Alluvial sediment, mostly coarse-grained | high | None | 997 | DAS01 | {5E2AF013-74CF-4277-A893-ACE983B94C7E} |
| 13 | {2DA03CF6-204E-4033-AB51-83B55E93794C} | map unit | map unit, generic | AA40 | Qpa | Qpa | paludal deposit | paludal deposit | Quaternary: Holocene | unprovided | Holocene | Holocene | Argillaceous silt, sand, and organic matter deposited in pond or marsh environments associated with floodplain deposits of Nevada and Washington Creeks. Also associated with a landslide deposit south of Buffalo Creek. Thickness probably less than 5 m (15 ft). | 02-02 | dmu, map unit | 235,235,153 | None | {C5A38107-C526-4ED2-814E-6999D10E9CC7} | Peat and muck | high | None | 997 | DAS01 | {2DA03CF6-204E-4033-AB51-83B55E93794C} |
| 5 | {471B50AA-F4E0-42DE-B0DF-6389E4DDD6D6} | map unit | map unit, generic | 0150 | Qaf | Qaf | alluvial fan | alluvial fan | Quaternary: Holocene | unprovided | Holocene | Holocene | Gravel, sand, silt, and clay in fan-shaped deposits along Shingle Mill and Nevada Creeks in the southern part of the map. Large, locally derived clasts are both matrix- and clast-supported. Coarse clast size is dominantly cobbles, but also includes boulders and pebbles. Thickness generally less than 15 m (50 ft). | 02-03 | dmu, map unit | 255,222,128 | None | {9681AE57-A86A-4E8B-8DD6-6103B1DB9517} | Alluvial sediment, mostly coarse-grained | high | None | 997 | DAS01 | {471B50AA-F4E0-42DE-B0DF-6389E4DDD6D6} |
| 4 | {8AA28794-6D1E-4EBD-980D-58D7BD4B5B97} | map unit | map unit, generic | A140 | Qac | Qac | alluvium and colluvium | alluvium and colluvium | Quaternary: Holocene | unprovided | Holocene | Holocene | Silt, sand, granules, and pebbles deposited on slopes by sheetwash alluvium incorporated with locally derived fine-grained colluvium. Deposits support hay fields along lower Washington Creek. Thickness generally less than 8 m (20 ft). | 02-05 | dmu, map unit | 235,222,153 | None | {6C2D6A29-29B2-4583-B4D5-D7B0A66B031F} | Colluvium and other widespread mass-movement sediment | high | None | 997 | DAS01 | {8AA28794-6D1E-4EBD-980D-58D7BD4B5B97} |
| 12 | {4AA60A43-65BC-4588-A2F7-82FCCCAB3628} | map unit | map unit, generic | 1270 | Qm | Qm | mantle | mantle | Quaternary: Holocene and Pleistocene | unprovided | Pleistocene | Holocene | Deposits on pediments that include sheetwash alluvium, fine-grained colluvium, coarse-grained (pebble, cobble, small boulder) lag from older debris-flow deposits, and regolith. Thickness generally less than 6 m (20 ft). | 02-06 | dmu, map unit | 222,204,77 | None | {C4CD626B-0DB5-435A-811F-8D6B2A995DB8} | Residual material | high | None | 997 | DAS01 | {4AA60A43-65BC-4588-A2F7-82FCCCAB3628} |
| 11 | {891143A6-28AE-476F-AD91-448543B32170} | map unit | map unit, generic | A150 | Qls | Qls | landslide deposit | landslide deposit | Quaternary: Holocene or Pleistocene | unprovided | Pleistocene | Holocene | Mass-wasting deposits of rotated or chaotic beds. The bentonitic Climbing Arrow Member of the Renova Formation (Trca) and units that immediately overlie it are particularly prone to developing landslide deposits. Thickness generally less than 60 m (200 ft). | 02-07 | dmu, map unit | 235,222,128 | None | {017338DF-E8E0-4EE7-BAED-C9EBC828F436} | Debris flows, landslides, and other localized mass-movement sediment | high | None | 997 | DAS01 | {891143A6-28AE-476F-AD91-448543B32170} |
| 9 | {53393CD0-293E-4985-9EC0-B3FAA0F48F96} | map unit | map unit, generic | 0160 | Qdf | Qdf | debris-flow deposit | debris-flow deposit | Quaternary: Pleistocene or Holocene | unprovided | Pleistocene | Holocene | Matrix-supported deposits of local, upslope-derived volcanic rock and sparse sedimentary rock. Clasts range from granules to boulders. Thickness generally less than 20 m (75 ft). | 02-08 | dmu, map unit | 255,222,102 | None | {017338DF-E8E0-4EE7-BAED-C9EBC828F436} | Debris flows, landslides, and other localized mass-movement sediment | high | None | 997 | DAS01 | {53393CD0-293E-4985-9EC0-B3FAA0F48F96} |
| 8 | {23CBE90B-57D9-484E-9137-6C621014F1C6} | map unit | map unit, generic | A170 | Qbgr | Qbgr | boulder gravel | boulder gravel | Quaternary: Holocene(?) and Pleistocene | unprovided | Pleistocene | Holocene | Unconsolidated deposits along Nevada Creek of reworked Tbgr. Dominantly weakly stratified rounded pebbles and cobbles in a coarse-grained matrix. Deposits southwest of Dalton Mountain include abundant subangular and angular Belt quartzite boulders as lag on the forest floor, but exposures were not observed. Thickness less than 20 m (70 ft). | 02-09 | dmu, map unit | 235,222,77 | None | {1EA7E66A-155C-44AA-9F48-2FC62780A963} | Sand and gravel of unspecified origin | medium | None | 997 | DAS01 | {23CBE90B-57D9-484E-9137-6C621014F1C6} |
| 7 | {615B0FF8-DA8C-4FD5-9ECC-857F4F6EA812} | map unit | map unit, generic | AA30 | Qalo | Qalo | alluvium, older than Qal | alluvium, older than Qal | Quaternary: Pleistocene | unprovided | Pleistocene | Pleistocene | Fluvial deposits in the Avon Valley in channels wider than those occupied by the present-day underfit streams. Clasts are generally rounded to subrounded cobbles and smaller, but boulders also present. Thickness not known. | 02-10 | dmu, map unit | 235,235,179 | None | {9681AE57-A86A-4E8B-8DD6-6103B1DB9517} | Alluvial sediment, mostly coarse-grained | high | None | 997 | DAS01 | {615B0FF8-DA8C-4FD5-9ECC-857F4F6EA812} |
| 10 | {9298725A-4AAA-4C18-8B27-73102C87B7C0} | map unit | map unit, generic | 0A60 | Qgt | Qgt | glacial deposit | glacial deposit | Quaternary: Pleistocene | unprovided | Pleistocene | Pleistocene | Light brown, brown, and reddish brown granules, pebbles, cobbles, and boulders in a very sandy to silty matrix which locally is clayey and compact. Dominant lithologies are quartzite and argillite. Confined to Willow Creek drainage in northwest corner of map. | 02-11 | dmu, map unit | 255,235,102 | None | {210C2D44-B0B1-4E1C-9C5F-5C578AF3A6EE} | Glacial till, mostly sandy | high | None | 997 | DAS01 | {9298725A-4AAA-4C18-8B27-73102C87B7C0} |
| 14 | {2DE0AF57-9053-476F-B0EF-657BDB5D168F} | map unit | map unit, generic | A270 | QTm | QTm | mantle | mantle | Quaternary and Tertiary | unprovided | Tertiary | Quaternary | Bouldery deposits on slopes near the East Avon Valley Fault on the east side of the Avon Valley. Upslope bedrock on the footwall block is not necessarily the source of the deposits. | 02-12 | dmu, map unit | 235,204,77 | None | {C4CD626B-0DB5-435A-811F-8D6B2A995DB8} | Residual material | high | None | 997 | DAS01 | {2DE0AF57-9053-476F-B0EF-657BDB5D168F} |
| 16 | {ED71F3CD-C3FE-48AA-A0AB-872491B70E58} | map unit | map unit, generic | A3X0 | Tbgr | Tbgr | boulder gravel | boulder gravel | Tertiary | unprovided | Tertiary | Tertiary | Dominantly matrix-supported, but locally clast-supported deposits that primarily occur adjacent to East Avon Valley Fault. Clasts range from pebbles to large boulders in a clay/silt/sand matrix. Clast composition dominantly Belt Supergroup quartzite with subordinate volcanic and plutonic rock. Matrix in many places has incorporated sediment from the Climbing Arrow Member of the Renova Formation (Trca). Deposit has been interpreted as Miocene (Loen, 1990; Schmidt and others, 1994). Contains placer gold (Loen, 1990). May be as thick as 300 m (985 ft). | 02-13 | dmu, map unit | 235,179,0 | None | {1EA7E66A-155C-44AA-9F48-2FC62780A963} | Sand and gravel of unspecified origin | medium | None | 997 | DAS01 | DAS08 | {ED71F3CD-C3FE-48AA-A0AB-872491B70E58} |
| 29 | {3B1C2F5E-32C0-42EB-A17C-B08BA256F8AB} | header | header, generic | None | None | None | TERTIARY SEDIMENTARY ROCKS | TERTIARY SEDIMENTARY ROCKS | Tertiary | unprovided | Tertiary | Tertiary | None | 03 | dmu, header | None | None | None | None | None | None | 997 | DAS01 | {3B1C2F5E-32C0-42EB-A17C-B08BA256F8AB} |
| 20 | {4C170E44-B2DE-42E6-845A-ABFAD6266A42} | map unit | map unit, generic | 0270 | Trcp | Trcp | Renova Formation, Cabbage Patch Member, informal | Cabbage Patch member of Renova Formation of Bozeman Group | Tertiary: Miocene and Oligocene | unprovided | Miocene | Oligocene | Light tan, tuffaceous, micaceous, siltstone and fine-grained sandstone with local lenses of rip-up-clast breccia. Unit has slumped downslope along the west side of Jefferson Creek. It is also present in southwest corner of map and along Cow Creek where it contains numerous fossil root traces. Similar deposits on Antelope Hill in the Gravely Mountain quadrangle to the south were mapped (Mosolf, 2015) as part of the Cabbage Patch member of the Renova Formation (Trcp). Thickness probably less than 45 m (150 ft) in map area. | 03-01 | dmu, map unit | 255,204,77 | None | {2D09A5AE-F0AD-462B-84BC-4092CE922275} | Mostly mudstone | medium | None | 997 | DAS01 | DAS03 | {4C170E44-B2DE-42E6-845A-ABFAD6266A42} |
| 19 | {135F23B0-072A-431E-9CD1-8DE6ADC02499} | map unit | map unit, generic | A2X0 | Trca | Trca | Renova Formation, Climbing Arrow Member | Climbing Arrow Member of Renova Formation of Bozeman Group | Tertiary: Eocene | unprovided | Eocene | Eocene | Pale olive, light olive gray, moderate olive brown, and medium light gray bentonitic mudstone, yellowish gray siltstone, and subordinate brownish gray sandstone and gravel/conglomerate lenses. Sandstone dominantly medium- to coarse-grained, with quartz, feldspar, biotite, and rhyolite grains. Gravel/conglomerate consists of clast-supported lenses of rounded granules, pebbles, and cobbles of rhyolite porphyry. A coalbed approximately 0.3 m (1 ft) thick occurs a short distance above the mouth of Jefferson Creek (Pardee and Schrader, 1933) and may be the same as a coalbed near Finn mined for domestic use (Glenna Stuckey, oral commun., 2012). West of Finn and east of Jefferson Creek, fish scales occur in platy siltstone and paper shale beds in a road cut along Highway 141. Bentonitic mudstone typically displays “popcorn” weathering, large desiccation cracks, and is prone to landslide development. Springs in NW¼ sec. 9, and NW¼ sec. 22, T. 12 N., R. 9 W. are concealed by thin crusts of Climbing Arrow Member. Unit referred to as “Blackfoot City beds” by Loen (1990). Base of unit not exposed. Exposed thickness approximately 180 m (600 ft). | 03-02 | dmu, map unit | 235,204,0 | None | {2D09A5AE-F0AD-462B-84BC-4092CE922275} | Mostly mudstone | medium | None | 997 | DAS01 | DAS04 | {135F23B0-072A-431E-9CD1-8DE6ADC02499} |
| 30 | {5A8B7599-C419-440A-A610-08DA53CC8F69} | header | header, generic | None | None | None | TERTIARY VOLCANIC ROCKS | TERTIARY VOLCANIC ROCKS | Tertiary | unprovided | Tertiary | Tertiary | None | 04 | dmu, header | None | None | None | None | None | None | 997 | DAS01 | {5A8B7599-C419-440A-A610-08DA53CC8F69} |
| 15 | {E0A69B14-4CB1-4561-97BD-319DD4A774CB} | map unit | map unit, generic | 2430 | Tba | Tba | basalt | basalt | Tertiary: Eocene | unprovided | Eocene | Eocene | Black, fine-grained, massive basalt flows with scattered olivine and pyroxene phenocrysts. Locally vesicular. Weathers to light brown, angular to sub-rounded blocks. Perhaps age equivalent to basaltic-andesite flows in the Gravely Mountain quadrangle to the south that yielded a U-Pb zircon age of 30.00 ± 0.19 Ma (Mosolf, 2015) and basalt in the Nevada Mountain quadrangle (McDonald and others, 2016) with a K-Ar (whole rock) age of 32.3 Ma (Mitchell Reynolds, written commun., 2014). | 04-01 | dmu, map unit | 204,153,179 | None | {374338FC-22B1-4121-A922-CC4048B88B2A} | Mafic-composition lava flows | high | None | 997 | DAS01 | DAS03 | DAS05 | {E0A69B14-4CB1-4561-97BD-319DD4A774CB} |
| 17 | {F2C53477-10C0-49D2-AEFE-7D851026A2E0} | map unit | map unit, generic | A310 | Tda | Tda | dacite | dacite | Tertiary: Eocene | unprovided | Eocene | Eocene | Gray and dark gray weathering, aphanitic to slightly porphyritic dacite to trachydacite lava flow with autobrecciated flow bottoms overlain by massive coherent flow interiors; zones of vesiculation are rarely preserved. Individual flows commonly exhibit distinctive flow banding and form flaggy, angular talus, often with red iron staining on parting surfaces. Aphanitic lavas exhibit a strong trachytic texture consisting mainly of plagioclase microlites, but also pyroxene, magnetite, and volcanic glass. Slightly porphyritic flows exhibit a similar trachytic texture and groundmass mineralogy, but contain subhedral to euhedral phenocrysts of plagioclase, hornblende, and some biotite. | 04-02 | dmu, map unit | 235,179,222 | None | {30BDD0D8-7FED-4AFE-B710-D3BE417CE43B} | Intermediate-composition lava flows | high | None | 997 | DAS01 | {F2C53477-10C0-49D2-AEFE-7D851026A2E0} |
| 18 | {CF551CF2-55AD-4F7E-9F10-2A9A67682CEA} | map unit | map unit, generic | 3540 | Tdap | Tdap | dacite, porphyry | dacite, porphyry | Tertiary: Eocene | unprovided | Eocene | Eocene | Gray, green, and red weathering dacite to trachydacite lava flows with a distinct coarse, porphyritic texture. Lava flows contain subhedral to euhedral phenocrysts of plagioclase (up to ~5 mm) and minor amounts of amphibole, biotite, and quartz. The aphanitic groundmass commonly has a trachytic texture and consists mainly of aligned microlites of plagioclase, but also includes amphibole, biotite, and magnetite. Carapaces of autobreccia several meters thick commonly encompass coherent interiors of individual lava flows. This unit weathers into blocks or plates, with some outcrops forming hoodoos and spires. A sample from the NE¼ sec. 4, T. 12 N., R. 9. W., yielded a U-Pb zircon age of 47.55 ± 0.16 Ma. | 04-03 | dmu, map unit | 179,128,153 | None | {30BDD0D8-7FED-4AFE-B710-D3BE417CE43B} | Intermediate-composition lava flows | high | None | 997 | DAS01 | {CF551CF2-55AD-4F7E-9F10-2A9A67682CEA} |
| 31 | {80D95336-70A2-4D34-AE1D-152DA5E3F603} | header | header, generic | None | None | None | CRETACEOUS INTRUSIVE ROCKS | CRETACEOUS INTRUSIVE ROCKS | Cretaceous | unprovided | Cretaceous | Cretaceous | None | 05 | dmu, header | None | None | None | None | None | None | 997 | DAS01 | {80D95336-70A2-4D34-AE1D-152DA5E3F603} |
| 2 | {170A86EE-246F-404B-B180-A72721FC10D5} | map unit | map unit, generic | 1770 | Kgd | Kgd | granodiorite | granodiorite | Late Cretaceous | unprovided | Late Cretaceous | Late Cretaceous | Medium to dark gray, equigranular to porphyritic granodiorite composed of plagioclase, potassium feldspar, quartz, biotite and hornblende; forms main body of the Dalton Mountain Stock and associated smaller intrusions. Schmidt and others (1994) report a K-Ar age on biotite of 77.9 ± 2.8 Ma. | 05-01 | dmu, map unit | 222,77,77 | None | {24E7A633-6C4C-41F2-8335-2A639C8E3639} | Coarse-grained, intermediate-composition intrusive igneous rock | high | None | 997 | DAS01 | DAS02 | {170A86EE-246F-404B-B180-A72721FC10D5} |
| 1 | {026E0B9C-5C12-4D1B-B800-59483C8191D1} | map unit | map unit, generic | A670 | Kgb | Kgb | gabbro | gabbro | Late Cretaceous | unprovided | Late Cretaceous | Late Cretaceous | Dark gray to greenish black, equigranular to porphyritic, medium- to coarse-grained quartz gabbro composed primarily of pyroxene and plagioclase with minor biotite and magnetite. Occurs as two small bodies along the Washington Creek drainage. | 05-02 | dmu, map unit | 235,102,77 | None | {9B41DDE4-2FCC-4898-9CEE-307D9CA9E730} | Coarse-grained, mafic-composition intrusive igneous rock | high | None | 997 | DAS01 | {026E0B9C-5C12-4D1B-B800-59483C8191D1} |
| 32 | {359624ED-DCDF-432E-91DE-2A67878146A8} | header | header, generic | None | None | None | MESOPROTEROZOIC BELT SUPERGROUP | MESOPROTEROZOIC BELT SUPERGROUP | Mesoproterozoic | unprovided | Mesoproterozoic | Mesoproterozoic | None | 06 | dmu, header | None | None | None | None | None | None | 997 | DAS01 | {359624ED-DCDF-432E-91DE-2A67878146A8} |
| 33 | {26E26467-1473-4269-AA4A-EEA3CF932015} | header | header, generic | None | None | None | MISSOULA GROUP | MISSOULA GROUP | None | unprovided | None | None | None | 06-01 | dmu, header | None | None | None | None | None | None | 997 | DAS01 | {26E26467-1473-4269-AA4A-EEA3CF932015} |
| 21 | {EB40BEB3-AEC0-4C8E-9F00-4F100995229C} | map unit | map unit, generic | 2350 | Ybo | Ybo | Bonner Formation | Bonner Formation of Missoula Group of Belt Supergroup | Mesoproterozoic | unprovided | Mesoproterozoic | Mesoproterozoic | Pink to red, medium- to coarse-grained, poorly sorted, feldspathic quartzite. Abundant trough and planar crossbeds in beds typically 0.5–1.0 m thick. Quartzite beds often separated by thin (0.1–1.0 cm), red to maroon argillite beds. Contains sparse subangular granules and small pebbles. A slabbed and stained sample contained 55 percent quartz, 35 percent potassium feldspar, and 10 percent plagioclase. Upper contact not exposed but is about 550 m (1,800 ft) thick in the west-adjacent Nevada Lake quadrangle (McDonald and others, 2016). | 06-01-01 | dmu, map unit | 204,179,128 | None | {BA96A3AA-660F-4C81-87EB-463C01EB9F06} | Sandstone | high | None | 997 | DAS01 | DAS05 | {EB40BEB3-AEC0-4C8E-9F00-4F100995229C} |
| 23 | {0C8AECB8-1E32-4B83-A9E9-F661F49D336B} | map unit | map unit, generic | 3350 | Yms3 | Yms3 | Mount Shields Formation, member 3 | Mount Shields Formation, member 3, of Missoula Group of Belt Supergroup | Mesoproterozoic | unprovided | Mesoproterozoic | Mesoproterozoic | Grayish red to blackish red, fine-grained quartzite to argillite couples and couplets with abundant desiccation cracks, mudchips, and diagnostic cubic salt casts. Includes green interbeds and some red microlaminae. Thickness about 275 m (900 ft). | 06-01-02 | dmu, map unit | 179,179,128 | None | {FDA3C54D-61D0-4798-ACC3-21A2F1270733} | Mostly sandstone | medium | None | 997 | DAS01 | {0C8AECB8-1E32-4B83-A9E9-F661F49D336B} |
| 22 | {310B1130-7C43-4073-B811-5745D2AD1F69} | map unit | map unit, generic | 5570 | Yms2 | Yms2 | Mount Shields Formation, member 2 | Mount Shields Formation, member 2, of Missoula Group of Belt Supergroup | Mesoproterozoic | unprovided | Mesoproterozoic | Mesoproterozoic | Pink to red, poorly sorted, medium- to coarse-grained, feldspathic quartzite. Abundant planar and trough crossbeds. Contains sparse subangular granules. Lower part is thinner bedded, consisting of couples of white to pink, medium-grained quartzite and thin red argillite. Bases of quartzite beds contain abundant red mudchips. The lower part was included in the top part of the Mount Shields Formation, member 1 of Schmidt and others (1994). Two slabbed and stained samples from the Ophir Creek 7.5' quadrangle east of the Avon Valley contained 65–75 percent quartz, 5–15 percent potassium feldspar, and 20 percent plagioclase (Lonn and Vuke, 2015). Thickness about 520 m (1,700 ft). | 06-01-03 | dmu, map unit | 128,128,77 | None | {BA96A3AA-660F-4C81-87EB-463C01EB9F06} | Sandstone | high | None | 997 | DAS01 | DAS02 | DAS06 | {310B1130-7C43-4073-B811-5745D2AD1F69} |
| 25 | {99EFE0E1-9CBB-42E6-9261-36EE86B923E0} | map unit | map unit, generic | 3330 | Ysh | Ysh | Shepard Formation | Shepard Formation of Missoula Group of Belt Supergroup | Mesoproterozoic | unprovided | Mesoproterozoic | Mesoproterozoic | Dolomitic and non-dolomitic, dark green siltite and light green argillite in microlaminae. Couplets of non-dolomitic red quartzite to argillite. Poorly exposed, but weathers to thin plates that, when dolomitic, have a characteristic orange-brown weathering rind. Ripples and load casts are common; mudcracks are rare. The upper half of the formation contains intervals of pink to gray, fine-grained feldspathic quartzite originally included in Mount Shields Formation, member 1 by Schmidt and others (1994). However, we place the formation’s upper contact at the top of a 50-m (160-ft) thick interval of distinctive rose-colored, dolomitic siltite–argillite couplets as was done in areas to the west (Lonn and others, 2010). The lower contact is placed at the bottom of the lowest dolomite-bearing beds. A stromatolite bed is often found near the base. Metamorphosed to pale green, striped hornfels near the contact with the Dalton Mountain Stock. Thickness about 610 m (2,000 ft). | 06-01-04 | dmu, map unit | 179,179,179 | None | {31CBE54B-0B07-457B-8AC5-A73AB365E34C} | Mostly carbonate rock | medium | None | 997 | DAS01 | DAS02 | DAS07 | {99EFE0E1-9CBB-42E6-9261-36EE86B923E0} |
| 26 | {954767B4-598E-4E73-8FC6-0AD2DDFC2F81} | map unit | map unit, generic | 4560 | Ysn | Ysn | Snowslip Formation | Snowslip Formation of Missoula Group of Belt Supergroup | Mesoproterozoic | unprovided | Mesoproterozoic | Mesoproterozoic | Interbedded intervals of quartzite to red argillite couplets, dark green siltite to light green argillite couplets, and microlaminated argillite. Desiccation cracks and mud rip-up clasts are common. Argillite beds often contain irregular “bumps” thought to be ill-defined salt casts or related to microbial mats. Contains beds and lenses of distinctive white, coarse-grained, well-sorted, feldspar-poor quartzite containing some well-rounded, frosted quartz grains. Lower 50 m (160 ft) dominated by microlaminated green dolomitic siltite and argillite. Upper 50–75 m (160–245 ft) is red, flat laminated, medium-grained quartzite in beds 0.5–1.0 m thick. Thickness approximately 1,430 m (4,700 ft). | 06-01-05 | dmu, map unit | 153,128,102 | None | {2D09A5AE-F0AD-462B-84BC-4092CE922275} | Mostly mudstone | medium | None | 997 | DAS01 | {954767B4-598E-4E73-8FC6-0AD2DDFC2F81} |
| 34 | {3150CC0B-03E5-4255-8876-F001EDB06E8F} | header | header, generic | None | None | None | PIEGAN GROUP | PIEGAN GROUP | None | unprovided | None | None | None | 06-02 | dmu, header | None | None | None | None | None | None | 997 | DAS01 | {3150CC0B-03E5-4255-8876-F001EDB06E8F} |
| 24 | {3761F534-F8DB-46B7-879A-3177E1DE6DA9} | map unit | map unit, generic | 5670 | Ypg | Ypg | Piegan Group | Piegan Group of Belt Supergroup | Mesoproterozoic | unprovided | Mesoproterozoic | Mesoproterozoic | Adjacent to the Dalton Mountain Stock, carbonates of the Piegan Group are contact metamorphosed to pale to dark green hornfels with diopside and/or tremolite. Thickness not determined. | 06-02-01 | dmu, map unit | 128,102,77 | None | {8E6EA7F0-74BB-43B3-899F-D7E3ACE54552} | Meta-carbonate rock | medium | None | 997 | DAS01 | {3761F534-F8DB-46B7-879A-3177E1DE6DA9} |
| OBJECTID | Glossary_ID | Term | Definition | DefinitionSourceID | GlobalID |
|---|---|---|---|---|---|
| 2 | {1B8731B8-5390-47EB-B981-FD0FDB4EC2C9} | 2 sigma | 2 sigma error of measure. Standard deviation multiplied by 2. | DAS10 | {1B8731B8-5390-47EB-B981-FD0FDB4EC2C9} |
| 3 | {B5BF0602-C559-46D5-B2F5-E98C4DA7EF7F} | Ma | Age expressed as millions of years ago. | DAS10 | {B5BF0602-C559-46D5-B2F5-E98C4DA7EF7F} |
| 4 | {C73BE7D5-C877-4A8A-81DF-0CC150BEF268} | accurate | 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. | DAS10 | {C73BE7D5-C877-4A8A-81DF-0CC150BEF268} |
| 5 | {1D3C46F2-0A62-4EA5-AC76-37C3859F4A10} | approximate | 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 LocationConfidenceLooku table. | DAS10 | {1D3C46F2-0A62-4EA5-AC76-37C3859F4A10} |
| 8 | {97A7ECF6-358A-4C35-B23D-1D84D26D0BDF} | bedding, generic | As defined in the AGI Glossary of Geology, see term "bed [stratig]". | DAS09 | {97A7ECF6-358A-4C35-B23D-1D84D26D0BDF} |
| 10 | {4F03E2D2-4418-40B3-8163-DD34C6DC1C00} | boundary, map | A linear feature indicating where one map unit ends at the map boundary. | DAS10 | {4F03E2D2-4418-40B3-8163-DD34C6DC1C00} |
| 11 | {4DFF2899-DF18-4CA6-B92E-A55313F266B5} | certain | Indicates that the author is reasonably confident in the scientific credibility of the existence of the feature. | DAS10 | {4DFF2899-DF18-4CA6-B92E-A55313F266B5} |
| 13 | {5F805BA3-FBCE-4244-88C8-78B74F337C71} | cleavage, generic | As defined in the AGI Glossary of Geology, see term "cleavage [struc geol]". | DAS09 | {5F805BA3-FBCE-4244-88C8-78B74F337C71} |
| 15 | {E3F0ACE2-A8DD-4A25-A5DF-DEBB2B85F673} | contact, generic | A linear feature indicating where two map units meet. As defined in the AGI Glossary of Geology, see term "contact". | DAS09 | DAS10 | {E3F0ACE2-A8DD-4A25-A5DF-DEBB2B85F673} |
| 17 | {F34EE059-8875-4380-B977-15193A65703F} | dmu, header | Description of Map Unit generic paragraph format for headings. | DAS10 | {F34EE059-8875-4380-B977-15193A65703F} |
| 18 | {E11CD18C-7CCF-40DB-989B-393035152F57} | dmu, map unit | Description of Map Unit generic paragraph format for map units. | DAS10 | {E11CD18C-7CCF-40DB-989B-393035152F57} |
| 20 | {A38AF8A7-DC33-42F0-A31E-9CA4DE113557} | fault, generic | As defined in the AGI Glossary of Geology, see term "fault [struc geol]". | DAS09 | {A38AF8A7-DC33-42F0-A31E-9CA4DE113557} |
| 21 | {D6A0CC42-2BC6-4BE6-998D-1422D35935FB} | fault, normal | As defined in the AGI Glossary of Geology, see term "normal fault". | DAS09 | {D6A0CC42-2BC6-4BE6-998D-1422D35935FB} |
| 22 | {AFBC6B65-7FC4-409E-B239-0FE24EDE4DC2} | fault, thrust | As defined in the AGI Glossary of Geology, see term "thrust fault". | DAS09 | {AFBC6B65-7FC4-409E-B239-0FE24EDE4DC2} |
| 24 | {2740707A-BBD7-4B63-AB18-1BDC44FC0BF7} | fold, syncline | As defined in the AGI Glossary of Geology, see term "syncline". | DAS09 | {2740707A-BBD7-4B63-AB18-1BDC44FC0BF7} |
| 26 | {73B592F2-430D-4AAE-A091-52264C9806FA} | foliation, igneous, generic | As defined in the AGI Glossary of Geology, see term "primary foliation" formed in "igneous" rocks. See notes field for details. | DAS09 | {73B592F2-430D-4AAE-A091-52264C9806FA} |
| 27 | {A0C1830E-7DDD-4B19-8A5B-78C3AFBD290C} | generalized | 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. | DAS10 | {A0C1830E-7DDD-4B19-8A5B-78C3AFBD290C} |
| 28 | {E053723A-8D44-4527-99CA-571193137B91} | generic document | A generic document, such as a standards manual or guide. | DAS10 | {E053723A-8D44-4527-99CA-571193137B91} |
| 30 | {1CA13CD2-15AD-43CB-BF21-E2CF7E7DE57C} | geochem, whole-rock | As defined in the AGI Glossary of Geology, see term "whole-rock". | DAS09 | {1CA13CD2-15AD-43CB-BF21-E2CF7E7DE57C} |
| 32 | {24F6A5E0-BC11-4B00-8F66-154EFD31D8C9} | geochron, U-Pb | As defined in the AGI Glossary of Geology, see term "uranium-lead age method". | DAS09 | {24F6A5E0-BC11-4B00-8F66-154EFD31D8C9} |
| 33 | {4257AA1A-F598-4339-9BB4-626A9ED444F3} | geologic mapping | A geologic map. | DAS10 | {4257AA1A-F598-4339-9BB4-626A9ED444F3} |
| 34 | {47BC064F-21BC-4C01-AD61-3C5439F3128A} | geologic report | A written geologic report. | DAS10 | {47BC064F-21BC-4C01-AD61-3C5439F3128A} |
| 37 | {3C4DC51C-1AAD-4A5C-AE7F-8582104A2726} | graphic, cross section line | A graphic line on the map indicating where a cross-section is generated. | DAS10 | {3C4DC51C-1AAD-4A5C-AE7F-8582104A2726} |
| 39 | {8D9942B5-38CB-4ADA-8DCB-3EF2F0569299} | header, generic | A generic header item in a description of map units. No specific map unit attributes are provided. | DAS10 | {8D9942B5-38CB-4ADA-8DCB-3EF2F0569299} |
| 40 | {F3CEE89F-3072-406E-B241-1ED84535D9EA} | high | Indicates that the author has a high confidence in this value. | DAS10 | {F3CEE89F-3072-406E-B241-1ED84535D9EA} |
| 41 | {7E065BC8-FF10-4EB6-BBCF-AC0AA48F4B2F} | inferred | 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. | DAS10 | {7E065BC8-FF10-4EB6-BBCF-AC0AA48F4B2F} |
| 43 | {05BF463F-C93D-4BF3-AC1A-2098BCE197FF} | joint, minor, inclined | 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. | DAS09 | {05BF463F-C93D-4BF3-AC1A-2098BCE197FF} |
| 45 | {8C81BBBB-4F10-4BA7-B681-6149734AA98F} | lineation, at intersection | As defined in the AGI Glossary of Geology, see term "intersection lineation". | DAS09 | {8C81BBBB-4F10-4BA7-B681-6149734AA98F} |
| 47 | {CD01A36A-C70E-4A64-856D-0F8FD654448C} | map unit, generic | As defined in the AGI Glossary of Geology, see term "lithostratigraphic unit". | DAS09 | {CD01A36A-C70E-4A64-856D-0F8FD654448C} |
| 48 | {1D9DC125-F79D-45D9-9CC9-3EE608F346A3} | medium | Indicates that the author is somewhat confident in this value. | DAS10 | {1D9DC125-F79D-45D9-9CC9-3EE608F346A3} |
| 51 | {3A87FDC6-C7AB-40FF-A602-49283B94E946} | unprovided | No specific knowledge available to provide a valid entry. Normally primarily in data conversion projects. | DAS10 | {3A87FDC6-C7AB-40FF-A602-49283B94E946} |
| OBJECTID | GlossaryFull_ID | Term | Definition | DefinitionSourceID | GlobalID |
|---|---|---|---|---|---|
| 1 | {5A7A65E8-F112-498D-A12B-EC6DC4555AD0} | 2 sigma | 2 sigma error of measure. Standard deviation multiplied by 2. | DAS10 | {5A7A65E8-F112-498D-A12B-EC6DC4555AD0} |
| 2 | {FAAA8E88-C28C-459A-BB86-05BEE3E9B1C1} | Ma | Age expressed as millions of years ago. | DAS10 | {FAAA8E88-C28C-459A-BB86-05BEE3E9B1C1} |
| 3 | {3BCAE349-18D6-4ED5-9138-3C125F2A7613} | accurate | 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. | DAS10 | {3BCAE349-18D6-4ED5-9138-3C125F2A7613} |
| 4 | {3FD50115-7C71-4CED-88FA-D224BD41D625} | approximate | 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 LocationConfidenceLooku table. | DAS10 | {3FD50115-7C71-4CED-88FA-D224BD41D625} |
| 5 | {77C34DD5-3FA1-4D82-BCB7-5C58C5E19662} | basalt | As defined in the AGI Glossary of Geology, see term "basalt". | DAS09 | {77C34DD5-3FA1-4D82-BCB7-5C58C5E19662} |
| 6 | {E6A92302-FC6A-4252-A72C-F920038D43E7} | bedding | As defined in the AGI Glossary of Geology, see term "bed [stratig]". | DAS09 | {E6A92302-FC6A-4252-A72C-F920038D43E7} |
| 7 | {5704CB95-8328-4655-B9A2-E1C97FFA9DE6} | bedding, generic | As defined in the AGI Glossary of Geology, see term "bed [stratig]". | DAS09 | {5704CB95-8328-4655-B9A2-E1C97FFA9DE6} |
| 8 | {07B26769-E97D-4345-B823-4EFD50C245D3} | boundary | A linear feature indicating where one map unit ends without an adjacent map unit. | DAS10 | {07B26769-E97D-4345-B823-4EFD50C245D3} |
| 9 | {1B8AC123-70CD-4340-BEF1-186422233CCE} | boundary, map | A linear feature indicating where one map unit ends at the map boundary. | DAS10 | {1B8AC123-70CD-4340-BEF1-186422233CCE} |
| 10 | {FCF479FB-E5F4-4FD2-ABAF-F74C1ACB9C01} | certain | Indicates that the author is reasonably confident in the scientific credibility of the existence of the feature. | DAS10 | {FCF479FB-E5F4-4FD2-ABAF-F74C1ACB9C01} |
| 11 | {09A0321B-6A32-4575-B414-978DC3337518} | cleavage | As defined in the AGI Glossary of Geology, see term "cleavage [struc geol]". | DAS09 | {09A0321B-6A32-4575-B414-978DC3337518} |
| 12 | {C5AF325C-AECA-453F-B555-44FB16FEF311} | cleavage, generic | As defined in the AGI Glossary of Geology, see term "cleavage [struc geol]". | DAS09 | {C5AF325C-AECA-453F-B555-44FB16FEF311} |
| 13 | {30DC98D3-42CD-4736-8C02-7A16754CBE62} | contact | A linear feature indicating where two map units meet. As defined in the AGI Glossary of Geology, see term "contact". | DAS09 | DAS10 | {30DC98D3-42CD-4736-8C02-7A16754CBE62} |
| 14 | {BA503D66-DE44-46AE-A0AC-507E778C22B2} | contact, generic | A linear feature indicating where two map units meet. As defined in the AGI Glossary of Geology, see term "contact". | DAS09 | DAS10 | {BA503D66-DE44-46AE-A0AC-507E778C22B2} |
| 15 | {84828345-2441-4F1F-BA23-D5BB619610C6} | dacite | As defined in the AGI Glossary of Geology, see term "dacite". | DAS09 | {84828345-2441-4F1F-BA23-D5BB619610C6} |
| 16 | {1E235DDC-99E2-4868-BAFB-8AD494956AF9} | dmu, header | Description of Map Unit generic paragraph format for headings. | DAS10 | {1E235DDC-99E2-4868-BAFB-8AD494956AF9} |
| 17 | {CC0D045E-2D92-4916-8CC2-B4DDE5E7488F} | dmu, map unit | Description of Map Unit generic paragraph format for map units. | DAS10 | {CC0D045E-2D92-4916-8CC2-B4DDE5E7488F} |
| 18 | {7F7A467D-DBC2-44EA-B22A-E2D42BFF13D5} | fault | As defined in the AGI Glossary of Geology, see term "fault [struc geol]". | DAS09 | {7F7A467D-DBC2-44EA-B22A-E2D42BFF13D5} |
| 19 | {EBDBB3C4-63C3-4BA0-B803-921A8C0407CB} | fault, generic | As defined in the AGI Glossary of Geology, see term "fault [struc geol]". | DAS09 | {EBDBB3C4-63C3-4BA0-B803-921A8C0407CB} |
| 20 | {61278D91-EEEF-4722-BC03-D6A345E1C189} | fault, normal | As defined in the AGI Glossary of Geology, see term "normal fault". | DAS09 | {61278D91-EEEF-4722-BC03-D6A345E1C189} |
| 21 | {9B0F1925-D146-44F3-B414-3F94C96B12C0} | fault, thrust | As defined in the AGI Glossary of Geology, see term "thrust fault". | DAS09 | {9B0F1925-D146-44F3-B414-3F94C96B12C0} |
| 22 | {A874D6BA-395D-4822-85CB-AD3E0595E3CB} | fold | As defined in the AGI Glossary of Geology, see term "fold [struc geol]". | DAS09 | {A874D6BA-395D-4822-85CB-AD3E0595E3CB} |
| 23 | {C5175D33-48D5-4814-8800-E897C0017754} | fold, syncline | As defined in the AGI Glossary of Geology, see term "syncline". | DAS09 | {C5175D33-48D5-4814-8800-E897C0017754} |
| 24 | {309EB4A7-0703-43BC-A3B6-109485F2F33C} | foliation | As defined in the AGI Glossary of Geology, see term "foliation [struc geol]". | DAS09 | {309EB4A7-0703-43BC-A3B6-109485F2F33C} |
| 25 | {4F31E1A4-0445-4079-A1C5-53829289EB98} | foliation, igneous, generic | As defined in the AGI Glossary of Geology, see term "primary foliation" formed in "igneous" rocks. See notes field for details. | DAS09 | {4F31E1A4-0445-4079-A1C5-53829289EB98} |
| 26 | {5ADDE782-AA88-4578-BBC8-89950D877A86} | generalized | 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. | DAS10 | {5ADDE782-AA88-4578-BBC8-89950D877A86} |
| 27 | {FC03401F-DF68-48CB-8CCF-DFD65CD627EE} | generic document | A generic document, such as a standards manual or guide. | DAS10 | {FC03401F-DF68-48CB-8CCF-DFD65CD627EE} |
| 28 | {C3889E59-6B61-4004-ABE1-338077BBA52D} | geochem | As defined in the AGI Glossary of Geology, see term "geochemistry". | DAS09 | {C3889E59-6B61-4004-ABE1-338077BBA52D} |
| 29 | {643C17A2-1672-4271-A302-ABE499D2BB2C} | geochem, whole-rock | As defined in the AGI Glossary of Geology, see term "whole-rock". | DAS09 | {643C17A2-1672-4271-A302-ABE499D2BB2C} |
| 30 | {89778B8F-D42E-4724-9FAD-4B0941676E2B} | geochron | As defined in the AGI Glossary of Geology, see term "geochronology". | DAS09 | {89778B8F-D42E-4724-9FAD-4B0941676E2B} |
| 31 | {F0007F07-5F87-4C7E-ADBC-A0923FD1AC90} | geochron, U-Pb | As defined in the AGI Glossary of Geology, see term "uranium-lead age method". | DAS09 | {F0007F07-5F87-4C7E-ADBC-A0923FD1AC90} |
| 32 | {520EE0C9-1279-4956-9437-2761EE554A31} | geologic mapping | A geologic map. | DAS10 | {520EE0C9-1279-4956-9437-2761EE554A31} |
| 33 | {1DD0C03E-8662-4365-BCC4-A5DFDA735913} | geologic report | A written geologic report. | DAS10 | {1DD0C03E-8662-4365-BCC4-A5DFDA735913} |
| 34 | {2FEB77C4-3CAC-405F-B15D-4FA32F35BA1D} | geospatial | 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. | DAS01 | {2FEB77C4-3CAC-405F-B15D-4FA32F35BA1D} |
| 35 | {F7888BD9-7197-4BC7-A00A-345FA8E8EB88} | graphic | A visual object used on the map with no intent to correctly model and/or attribute a real-world physical feature. | DAS10 | {F7888BD9-7197-4BC7-A00A-345FA8E8EB88} |
| 36 | {7CA06810-1E63-43CC-B659-6688C8B17DF3} | graphic, cross section line | A graphic line on the map indicating where a cross-section is generated. | DAS10 | {7CA06810-1E63-43CC-B659-6688C8B17DF3} |
| 37 | {13D6A586-9813-4D67-8E6B-D62AB2AF62BF} | header | A header item in a description of map units. No specific map unit attributes are provided. | DAS10 | {13D6A586-9813-4D67-8E6B-D62AB2AF62BF} |
| 38 | {37BAE996-06B3-4472-9E1A-D826F1F7C25D} | header, generic | A generic header item in a description of map units. No specific map unit attributes are provided. | DAS10 | {37BAE996-06B3-4472-9E1A-D826F1F7C25D} |
| 39 | {C89E58D3-06A6-4367-9BA8-06F97A0D78E0} | high | Indicates that the author has a high confidence in this value. | DAS10 | {C89E58D3-06A6-4367-9BA8-06F97A0D78E0} |
| 40 | {6E4E66B2-A7BF-4146-BC08-986ECB132227} | inferred | 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. | DAS10 | {6E4E66B2-A7BF-4146-BC08-986ECB132227} |
| 41 | {F0E97CAA-8A1E-46E1-9B71-8E17205A44DC} | joint | As defined in the AGI Glossary of Geology, see term "joint [struc geol]". | DAS09 | {F0E97CAA-8A1E-46E1-9B71-8E17205A44DC} |
| 42 | {5BC3B3CC-F2C0-43E4-8E73-F4B94B9BE89B} | joint, minor, inclined | 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. | DAS09 | {5BC3B3CC-F2C0-43E4-8E73-F4B94B9BE89B} |
| 43 | {C19E57CD-16F9-443C-BB2E-4F041C82D234} | lineation | As defined in the AGI Glossary of Geology, see term "lineation [struc]". | DAS09 | {C19E57CD-16F9-443C-BB2E-4F041C82D234} |
| 44 | {60260810-3939-44BC-8ED0-9EEB2271BC51} | lineation, at intersection | As defined in the AGI Glossary of Geology, see term "intersection lineation". | DAS09 | {60260810-3939-44BC-8ED0-9EEB2271BC51} |
| 45 | {9B6219D5-BE82-4FEC-95A0-8AAE929CE721} | map unit | As defined in the AGI Glossary of Geology, see term "lithostratigraphic unit". | DAS09 | {9B6219D5-BE82-4FEC-95A0-8AAE929CE721} |
| 46 | {CC4AE2FF-AA47-4496-9CDB-C826B8F5FA2F} | map unit, generic | As defined in the AGI Glossary of Geology, see term "lithostratigraphic unit". | DAS09 | {CC4AE2FF-AA47-4496-9CDB-C826B8F5FA2F} |
| 47 | {8940F5DF-F3B4-46F2-BB5A-2C463EA63AA0} | medium | Indicates that the author is somewhat confident in this value. | DAS10 | {8940F5DF-F3B4-46F2-BB5A-2C463EA63AA0} |
| 48 | {28713443-093C-41EF-BACC-37AEB9CB6B9D} | non-geospatial | Data source does not have a defined geospatial area. | DAS10 | {28713443-093C-41EF-BACC-37AEB9CB6B9D} |
| 49 | {FD8B678E-FEC2-46EC-B066-5B3CF5F4617E} | trachydacite | As defined in the AGI Glossary of Geology, see term "trachydacite". | DAS09 | {FD8B678E-FEC2-46EC-B066-5B3CF5F4617E} |
| 50 | {5E17ED8A-6A6F-4952-90AC-59F8F9B57B70} | unprovided | No specific knowledge available to provide a valid entry. Normally primarily in data conversion projects. | DAS10 | {5E17ED8A-6A6F-4952-90AC-59F8F9B57B70} |
| OBJECTID | LocationConfidenceLookup_ID | ScaleDenom | AccurateMin | AccurateDefault | AccurateMax | ApproximateMin | ApproximateDefault | ApproximateMax | InferredMin | InferredDefault | InferredMax | GlobalID | UnprovidedLocationConfidence |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 1 | {5D0350C3-5346-4B93-BD45-5AE4BFFDE530} | 24000 | 0 | 25 | 25 | 26 | 50 | 50 | 51 | 120 | None | {5D0350C3-5346-4B93-BD45-5AE4BFFDE530} | 997 |
| 2 | {F9136468-6CA9-47E1-896C-F140693E6A51} | 50000 | 0 | 50 | 50 | 51 | 100 | 100 | 101 | 250 | None | {F9136468-6CA9-47E1-896C-F140693E6A51} | 997 |
| 3 | {12390D62-CE9B-43AD-8AC4-8440C9E7C2EB} | 100000 | 0 | 100 | 100 | 101 | 200 | 200 | 201 | 500 | None | {12390D62-CE9B-43AD-8AC4-8440C9E7C2EB} | 997 |
| 4 | {DF807FC9-7905-4A5A-94F5-E5BEC19FB303} | 500000 | 0 | 254 | 254 | 255 | 508 | 508 | 509 | 800 | None | {DF807FC9-7905-4A5A-94F5-E5BEC19FB303} | 997 |
| OBJECTID | OrientationConfidenceLookup_ID | HighMin | HighDefault | HighMax | MediumMin | MediumDefault | MediumMax | LowMin | LowDefault | LowMax | GlobalID |
|---|---|---|---|---|---|---|---|---|---|---|---|
| 1 | {D1D1CFF0-7CB8-4847-B2A4-13E8BF043FCF} | 5 | 5 | 5 | 6 | 10 | 20 | 21 | 20 | None | {D1D1CFF0-7CB8-4847-B2A4-13E8BF043FCF} |