GeMS validation of BRS_GeMS.gdb

Database path: C:\Users\cconnallon.LANGROUP\Desktop\Blue Ridge Summit Linework\BRS GeMS gdb\BRS_GeMS.gdb
File written by GeMS_ValidateDatabase_AGP2.py, version of 8 July 2021
Wed Sep 29 07:35:04 2021

This file should be accompanied by BRS_GeMS.gdb-ValidationErrors.html, BRS_GeMS.gdb-vFgdcMetadata.txt, and BRS_GeMS.gdb-vFgdcMetadataErrors.txt, all in the same directory.

This database is LEVEL 3 COMPLIANT, pending completion of a peer-reviewed Geologic Names report that includes identification of any suggested modifications to Geolex. The database-level FGDC metadata are formally correct. The metadata record should be examined by a human to verify that it is meaningful.
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Contents

Compliance Criteria
Content not specified in GeMS schema
MapUnits in DescriptionOfMapUnits table, GeologicMap feature dataset, and other feature datasets
Contents of Nonspatial Tables
    DataSources
    DescriptionOfMapUnits
    Glossary
    LabDataTableBRS
Database Inventory

Compliance Criteria

LEVEL 1

Criteria for a LEVEL 1 GeMS database are: Databases with a variety of schema may meet these criteria. This script cannot confirm LEVEL 1 compliance.

LEVEL 2--MINIMALLY COMPLIANT

A LEVEL 2 GeMS database is accompanied by a peer-reviewed Geologic Names report, including identification of suggested modifications to Geolex, and meets the following criteria:

2.1 Has required elements: nonspatial tables DataSources, DescriptionOfMapUnits, GeoMaterialDict; feature dataset GeologicMap with feature classes ContactsAndFaults and MapUnitPolys PASS
2.2 Required fields within required elements are present and correctly defined PASS
2.3 GeologicMap topology: no internal gaps or overlaps in MapUnitPolys, boundaries of MapUnitPolys are covered by ContactsAndFaults PASS
2.4 All map units in MapUnitPolys have entries in DescriptionOfMapUnits table PASS
2.5 No duplicate MapUnit values in DescriptionOfMapUnit table PASS
2.6 Certain field values within required elements have entries in Glossary table PASS
2.7 No duplicate Term values in Glossary table PASS
2.8 All xxxSourceID values in required elements have entries in DataSources table PASS
2.9 No duplicate DataSources_ID values in DataSources table PASS

LEVEL 3--FULLY COMPLIANT

A LEVEL 3 GeMS database meets these additional criteria:
3.1 Table and field definitions conform to GeMS schema PASS
3.2 All map-like feature datasets obey topology rules. No MapUnitPolys gaps or overlaps. No ContactsAndFaults overlaps, self-overlaps, or self-intersections. MapUnitPoly boundaries covered by ContactsAndFaults PASS
3.3 No missing required values PASS
3.4 No missing terms in Glossary PASS
3.5 No unnecessary terms in Glossary PASS
3.6 No missing sources in DataSources PASS
3.7 No unnecessary sources in DataSources PASS
3.8 No map units without entries in DescriptionOfMapUnits PASS
3.9 No unnecessary map units in DescriptionOfMapUnits PASS
3.10 HierarchyKey values in DescriptionOfMapUnits are unique and well formed PASS
3.11 All values of GeoMaterial are defined in GeoMaterialDict. GeoMaterialDict is as specified in the GeMS standard PASS
3.12 No duplicate _ID values PASS
3.13 No zero-length or whitespace-only strings PASS

There are 1 warnings

Content not specified in GeMS schema

Some of the extensions to the GeMS schema identified here may be necessary to capture geologic content and are entirely appropriate. Please document these extensions in metadata for the database, any accompanying README file, and (if applicable) any transmittal letter that accompanies the dataset. Other extensions may be intermediate datasets, fields, or files that should be deleted before distribution of the database.

    ContactsAndFaults, field LTYPE
    MapUnitPolys, field PTYPE
    TableView LabDataTableBRS
    FeatureClass ContactsAndFaultsAnno
    FeatureClass MapUnitPolysAnno
    FeatureClass MapUnitOverlayPolysAnno
    FeatureClass ContactsAndFaultsAnno2
    FeatureClass ContactsAndFaultsAnno3
    TextFile 00log.txt
    MapUnitOverlayPolys, field PTYPE
    OrientationPoints, field PTTYPE
    FeatureClass LabDataGenericPoints

MapUnits in DescriptionOfMapUnits table, GeologicMap feature dataset, and other feature datasets

MapUnit  DMU  GeologicMap
QalXX
QcXX
TrgXX
TrgcXX
CfuXX
ChXX
ChmXX
CwoXX
CwmXX
CwmwXX
CwbXX
CZlXX
ZcmXX
ZcrXX
ZcrpXX
ZcmpXX

Contents of Nonspatial Tables

DataSources

OBJECTID Source Notes URL _ID
5 Brezinski, D.K., 2021, Geology of Part of the Blue Ridge Summit Quadrangle, Washington and Frederick County, Maryland. Maryland Geological Survey Geological Map, scale 1:24,000. --- http://www.mgs.md.gov/output/maps/quadgeo/PTOFRGEO2004_1.pdf DS1
3 American Geological Institute, 2012, Glossary of Geology --- --- DS2
4 Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates. --- https://ngmdb.usgs.gov/fgdc_gds/geolsymstd.php FGDC-STD-013-2006

DescriptionOfMapUnits

OBJECTID MapUnit Name FullName Age Description HierarchyKey ParagraphStyle Label Symbol AreaFillRGB AreaFillPatternDescription DescriptionSourceID GeoMaterial GeoMaterialConfidence _ID
1 Qal Alluvium Alluvium Quaternary Poorly sorted, unconsolidated, tan, reddish brown, to dark-gray mud, silt, sand, and pebbles. These deposits form in stream channels, and on the flood plain adjacent to the streams. Thickness estimated a 3 to 10 feet. 1 header1 Qal --- --- --- DS1 Alluvial sediment High DMU_1
2 Qc Colluvium Colluvium Quaternary Unconsolidated and unsorted cobbles and boulders that accumulate on steep slopes overlying and downslope sandstone and quartzite units. These deposit may move slowly downslope under the influence of frost action and gravity. Two types were recognized in the Blue Ridge Summit Quadrangle. The first type is composed predominately of angular boulders that overlie outcroppings of quartzites of the Weverton Formation on the flanks of Catoctin Mountain. This type of colluvium appears to be the direct result of the mechanical breakdown of the quartzite intervals. The thickness was not determined, but mat be highly variable. The second type of colluvium is composed of highly weathered, reddish brown, rounded pebbles and cobbles of quartzite and vein quartz within a sandy matrix. This type of colluvium is present along the eastern base of Catoctin Mountain and covers outcrops of the Harpers, Frederick, and Gettysburg formations near Thurmont. The thickness of this type of colluvium ranges from a thin veneer less 3 feet to more than 50 feet. 2 header1 Qc --- --- --- DS1 Colluvium and other widespread mass-movement sediment High DMU_2
3 Trg Gettysburg Formation Gettysburg Formation Triassic Cyclically interbedded reddish gray, laminated, very fine-grained, argillaceous sandstone, sandy siltstone and red to reddish brown shale to rooted mudstone. Sandstone and siltstone intervals are commonly laminated to cross-laminated and siltstone intervals are mudcracked. Mudstone intervals are pervasively rooted and show signs of incipient soil development. Along the western margin of the outcrop belt the Gettysburg Formation is composed of a narrow belt of interbedded reddish brown, thin-bedded, fine-grained, argillaceous sandstone and red-brown limestone conglomerate [Trgc]. The thickness of the Gettysburg Formation has been estimated at 8,000 to 22,000 feet (Brezinski, 2004; Root, 1988; Brezinski and Adams,2021). 3 header1 ^rg --- --- --- DS1 Sedimentary rock High DMU_3
18 Trgc Gettysburg conglomerate Gettysburg Formation, conglomerate Triassic Along the western margin of the outcrop belt the Gettysburg Formation is composed of a narrow belt of interbedded reddish brown, thin-bedded, fine-grained, argillaceous sandstone and red-brown limestone conglomerate [Trgc]. 3-1 header2 ^rgc --- --- --- DS1 Sedimentary rock High DMU_18
4 Cfu Frederick Formation Frederick Formation, undivided Cambrian Medium to dark gray, laminated to thin-bedded, pyritic, argillaceous limestone and highly sheared and deformed, laminated limestone. Because of limited exposure no member assignment could be made for the Frederick Formation in the Blue Ridge Summit Quadrangle (see Brezinski, 2004). In this area, the Frederick Formation is interpreted to occur as the foot-wall of the Owens Creek overthrust. Thickness in the Blue Ridge Summit Quadrangle is estimated at 500 to 1000 feet. 4 header1 _fu --- --- --- DS1 Carbonate rock High DMU_4
5 --- Chilhowee Group --- --- --- 5 header3 --- --- --- --- DS1 Metasedimentary rock High DMU_5
6 Ch Harpers Formation Harpers Formation Cambrian Predominately tan-weathering, dark grayish green to dark gray, sheared phyllitic shale and siltstone with lesser amounts of metasandstones that may be quartzitic. Shale and siltstone are gray to greenish gray, dark brown-gray to medium gray in color and commonly containing thin 2- 6 inch, fine-grained sandstone layers. Local areas of intense shearing create phyllitic areas where cleavage obscures bedding. Because of intraformational folding and intense cleavage, determining the thickness of the formation was not possible. Estimates range from 1,500 to 3,000 feet. 6 header1 _h --- --- --- DS1 Metasedimentary rock High DMU_6
7 Chm Mont Alto Member Harpers Formation, Mont Alto member Cambrian Within the lower Harpers Formation there is a mappable metagraywacke that can be traced along the flank of Catoctin Mountain. This interval is light- to medium gray, medium-bedded, coarse-grained to conglomeratic, quartzitic, and contains Skolithos-burrowed. This interval is considered equivalent to the Mont Alto Member of the Harpers Formation in Pennsylvania (Brezinski, 1992). The Mont Alto Member is between 30 to 50 feet thick in the Blue Ridge Summit Quadrangle, but thickens northward into southern Pennsylvania. 6-1 header2 _hm --- --- --- DS1 Metasedimentary rock High DMU_7
8 --- Weverton Formation Weverton Formation Cambrian Light- to medium-gray quartzite, conglomerate, medium to dark gray metagraywacke with intervals of dark-gray to black metasiltstone and phyllite. Three members are recognized (Brezinski, 1992). 7 header1 --- --- --- --- DS1 Metasedimentary rock High DMU_8
9 Cwo Owens Creek Member Weverton Formation, Owens Creek member Cambrian Medium to dark gray, very coarse grained to conglomeratic, cross-bedded, medium- to thick-bedded metagraywacke. The coarse-grained character of this member makes recognition of cross-bedding difficult. Conglomeratic intervals contain large, (1 to 3 cm) white and pink quartz pebbles. The type section of this member is along MD 550 along Owens Creek. Thickness ranges from 200 to 300 feet. 7-1 header2 _wo --- --- --- DS1 Metasedimentary rock High DMU_9
10 Cwm Maryland Heights Member Weverton Formation, Maryland Heights member Cambrian Interbedded, thin (less than 30 feet), white quartzite and medium gray metagraywacke and very dark gray, highly cleaved, volcaniclastic siltstone and phyllitic shale. Shales and siltstones are very poorly exposed and individual quartzites and graywackes are only locally traceable. Near the middle of this member there is a light gray, massive, coarse-grained quartzite. Herein termed the Wolf Rock Quartzite Bed [Cwmw] (=middle quartzite of Whitaker, 1955 and ledge-maker quartzite of Fauth, 1977). This unit is up to 30 feet thick in the Blue Ridge Summit Quadrangle. Thickness of the Maryland Heights Member ranges from 200 to 400 feet. 7-2 header2 _wm --- --- --- DS1 Metasedimentary rock High DMU_10
17 Cwmw Wolf Rock Quartzite Bed Weverton Formation, Maryland Heights member, Wolf Rock quartzite bed Cambrian Near the middle of the Weverton Formation, Maryland Heights member there is a light gray, massive, coarse-grained quartzite. Herein termed the Wolf Rock Quartzite Bed [Cwmw] (=middle quartzite of Whitaker, 1955 and ledge-maker quartzite of Fauth, 1977). This unit is up to 30 feet thick in the Blue Ridge Summit Quadrangle. 7-2-1 header2 _wmw --- --- --- DS1 Quartzite High DMU_17
11 Cwb Buzzard Knob Member Weverton Formation, Buzzard Knob member Cambrian The lowest member of the Weverton Formation consists of two ledge-forming quartzites, which are often difficult to discern between. The lower ledge consists of light- to medium-gray to light greenish gray, medium-bedded quartzite with dark-gray argillaceous layers up to 4 cm thick, separating the quartzite beds. Cross-bedding within individual quartzite strata is pervasive and is commonly accentuated by purplish or yellow-gold bands demarcating the individual cross-bed foresets. The upper ledge-forming quartzite is composed of medium- to thick-bedded, very light gray, quartzite. Cross-bedding is abundant, but less obvious than in the lower ledge. This member is the main ridge-forming unit of the Maryland Blue Ridge. Thickness ranges from 175 to 350 feet. 7-3 header2 _wb --- --- --- DS1 Quartzite High DMU_11
12 CZl Loudoun Formation Loudoun Formation Cambrian-Late Proterozoic Interbedded, medium-gray, medium-to thin-bedded, tuffaceous sandstone, granule to pebble conglomerate, and dark gray, tuffaceous phyllite. Massive, cross-bedded, quartzite, and thin, quartz-pebble conglomerate and pebbly polymictic lenses of conglomerate are interbedded within phyllite as are layers of flattened phyllite pebbles. The width of the outcrop belt widens dramatically in the Blue Ridge Summit and Emmitsburg quadrangles indicating a localized thickening of the formation. In the Blue Ridge Summit Quadrangle, the Loudoun Formation is graphically determined to be from 800 to 1,500 feet in thickness. 8 header1 _Zl --- --- --- DS1 Lower-grade metamorphic rock, of unspecified origin High DMU_12
13 --- Catoctin Formation Catoctin Formation Late Proterozoic The Catoctin Formation is a suite of volcanigenic rocks that consists principally of metabasalt, metarhyolite, and tuffaceaous phyllites. 9 header1 --- --- --- --- DS1 Meta-volcaniclastic rock High DMU_13
14 Zcm Metabasalt Catoctin Formation, metabasalt Late Proterozoic Medium to dark greenish gray, medium-grained, massive, metabasalt. Textures vary greatly between exposures, but commonly consists of massive to highly cleaved aphanitic, greenish gray metabasalt exhibiting a range of primary textures including amygdaloidal, porphyoblastic, banded, vesicular, and flow-top brecciation. Areas of tectonic deformation are suggested by schistose chlorite- and actinolite-bearing metabasalt that are epidote-rich. Porphyroblasts most commonly epidote, plagioclase feldspar, or chlorite that are flattened and elongated and composed of chlorite, actinolite, or epidote, ranging between 10 and 25 mm (0.4 to 1 inch) in length (Fauth, 1977). Vesicles are oval-shaped voids or may be filled amygdules that contain epidote, feldspar, and quartz. Primary layering is present in many exposures along the eastern margin of the Blue Ridge Anticlinorium. Prominent veins and nodular masses of epidote and quartz are widely distributed throughout the unit. Thickness of the entire metabasalt unit is estimated at greater than 2,000 feet. 9-1 header2 Zcm --- --- --- DS1 Meta-volcaniclastic rock High DMU_14
15 Zcr Metarhyolite Catoctin Formation, metarhyolite Late Proterozoic Medium gray to medium dark bluish gray, dense, metarhyolite. A variety of variations are noted on the map, not delineated separately. The most common is aphanitic bluish gray metarhyolite that is massive and dense, and exhibits a conchoidal fracture. Rare phenocrysts, are present, but comprise less than 1 percent of the rock. Weathers light gray to light medium gray. Several textural subunits have been noted but noted mapped. Medium bluish gray, flow-banded metarhyolite containing planar to convoluted flow bands 0.12 to 0.4 inch (3 to 10 mm) thick. Banding is discontinuous and most prominent on weathered surfaces. Phenocrysts typically constitute less than 5 percent of the rock. Medium to dark bluish gray, porphyritic, aphanitic metarhyolite contain very light gray to very pale orange or pinkish gray feldspar laths. Phenocrysts are up to 0.2 inches (6mm) long, rectangular, and make up more than 5 percent of the rock. Minimum aggregate thickness is estimated at 500 to 800 feet (Fauth, 1977). 9-2 header2 Zcr --- --- --- DS1 Meta-volcaniclastic rock High DMU_15
16 Zcrp Interbanded Metabasalt, Metarhyolite and Tuffaceous Phyllite Catoctin Formation, Interbanded Metabasalt, Metarhyolite and Tuffaceous Phyllite Late Proterozoic Interlayered greenish gray granular phyllite, pale purplish gray, to very light gray, tuffaceous phyllite, greenish gray metabasalt, and dark gray metarhyolite. Medium greenish gray phyllite contains small elongate felspathic laths and is commonly interbedded with thin bands (4-10 cm) of gray metarhyolite or metabasalt. Gray phyllites typically are tuffaceous and volcanoclastic. Especially well-developed in the Harbaugh Valley. Estimated thickness 1000 to 1,500 feet. 9-3 header2 Zcrp --- --- --- DS1 Meta-volcaniclastic rock High DMU_16
19 Zcmp Porphyritic metabasalt Catoctin Formation, porphyritic metabasalt Late Proterozoic Medium to dark greenish gray, medium-grained, massive, metabasalt. Textures vary greatly between exposures, but commonly consists of massive to highly cleaved aphanitic, greenish gray metabasalt exhibiting a range of primary textures including amygdaloidal, porphyoblastic, banded, vesicular, and flow-top brecciation. Areas of tectonic deformation are suggested by schistose chlorite- and actinolite-bearing metabasalt that are epidote-rich. Porphyroblasts most commonly epidote, plagioclase feldspar, or chlorite that are flattened and elongated and composed of chlorite, actinolite, or epidote, ranging between 10 and 25 mm (0.4 to 1 inch) in length (Fauth, 1977). Vesicles are oval-shaped voids or may be filled amygdules that contain epidote, feldspar, and quartz. Primary layering is present in many exposures along the eastern margin of the Blue Ridge Anticlinorium. Prominent veins and nodular masses of epidote and quartz are widely distributed throughout the unit. Thickness of the entire metabasalt unit is estimated at greater than 2,000 feet. 9-4 header2 Zcmp --- --- --- DS1 Meta-volcaniclastic rock High DMU_19

Glossary

OBJECTID Term Definition DefinitionSourceID _ID
5 banding A banded sctructure of metamorphic rocks consisting of nearly parallel bands having different textures or minerals or both. It may be produced by incomplete segregation of constituents during recrystallization or may be inherited from bedding in sediments or from layering in igneous rocks. DS2 GLID_5
15 bedding The arrangement of sedimentary rocks in beds or layers of varying thickness and character; the general physical structural character or pattern of the beds and their contacts within a rock mass, such as cross-bedding and graded bedding; a collective term denoting the existence of beds. Also, the structure so produced. The term may be applied to the layered arrangement and structure of an igneous or metamorphic rock. DS2 GLID_15
14 certain Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation. FGDC-STD-013-2006 GLID_14
16 cleavage A locally planar fabric in an unmetamorphosed or weakly metamorphosed, fine-grained rock defined by either the tendency of a rock to split in a particular direction, a preferred orientation of crystal planes in mineral grains, or a preferred orientation of inequant grain shapes; it is a produce of deformation or metamorphism. DS2 GLID_16
3 contact A planar surface that bounds a geologic unit. FGDC-STD-013-2006 GLID_3
18 fault A discrete surface or zone of discrete surfaces separating two rock masses across which one mass has slid past the other. DS2 GLID_18
31 foliation A general term for a planar arrangement of textural or structural features in any type of rock, esp. the locally planar fabric in a rock defined by a fissility, a preferred orientation of crystal planes in mineral grains, a preferred orientation of inequant grain shapes, or from compositional banding. In igneous rocks, planar parallelism of flaky or tabular minerals and mineral aggregates, slabby xenoliths, or flattened vesicles as well as compositional layering. In metamorphic rocks, planar parallelism of flaky minerals and compositional layering. DS2 GLID_31
11 header1 Formation header, bolded text, no indent. This format is used for Formations, Quaternary deposits, and basement complex. DS1 GLID_11
12 header2 Member header, bolded text, indented. This format is used for named members (e.g. Benevola Member, under Tomstown Formation) and for sub-units without proper names (e.g. Quartzite, under Swift Run Formation). DS1 GLID_12
13 header3 Group header, bolded text, capitalized, no indent. DS1 GLID_13
10 High High level of confidence that GeoMaterial term accurately and appropriately describes the map unit. FGDC-STD-013-2006 GLID_10
32 joint A planar fracture, crack, or parting in a rock, without shear displacement; the surface is usually decorated with a plumose structure. Often occurs with parallel joints to form part of a joint set. DS2 GLID_32
29 joints A planar fracture, crack, or parting in a rock, without shear displacement; the surface is usually decorated with a plumose structure. Often occurs with parallel joints to form part of a joint set. DS2 GLID_29
30 Sample A subset of a population that, if properly selected, may be used to estimate the parameters of the population. DS2 GLID_30

LabDataTableBRS

OBJECTID PointID Lab_No Field_No Description Depth_Inches Depth_FT type ICP60_Al ICP60_Ca ICP60_Fe ICP60_K ICP60_Mg ICP60_P ICP60_S ICP60_Si ICP60_Ti ICP60_AgPPM ICP60_AsPPM ICP60_BPPM ICP60_BaPPM ICP60_BePPM ICP60_BiPPM ICP60_CdPPM ICP60_CePPM ICP60_CoPPM ICP60_CrPPM ICP60_CsPPM ICP60_CuPPM ICP60_DyPPM ICP60_ErPPM ICP60_EuPPM ICP60_GaPPM ICP60_GdPPM ICP60_GePPM ICP60_HfPPM ICP60_HoPPM ICP60_InPPM ICP60_LaPPM ICP60_LiPPM ICP60_LuPPM ICP60_MnPPM ICP60_MoPPM ICP60_NbPPM ICP60_NdPPM ICP60_NiPPM ICP60_PbPPM ICP60_PrPPM ICP60_RbPPM ICP60_RePPM ICP60_SbPPM ICP60_ScPPM ICP60_SePPM ICP60_SmPPM ICP60_SnPPM ICP60_SrPPM ICP60_TaPPM ICP60_TbPPM ICP60_TePPM ICP60_ThPPM ICP60_TlPPM ICP60_TmPPM ICP60_UPPM ICP60_VPPM ICP60_WPPM ICP60_YPPM ICP60_YbPPM ICP60_ZnPPM ICP60_ZrPPM XRFmjr_Al2O3 XRFmjr_BaO XRFmjr_CaO XRFmjr_Cr2O3 XRFmjr_Fe2O3 XRFmjr_K2O XRFmjr_LOI XRFmjr_MgO XRFmjr_MnO XRFmjr_Na2O XRFmjr_P2O5 XRFmjr_SiO2 XRFmjr_SrO XRFmjr_TiO2 XRFmjr_V2O5 _ID
1 BLUE-H1 C-510964 BLUE-H1-10 soil B horizon 10.0 --- pit, hand dug 9.28 1.21 11.7 1.31 1.1 0.09 -999.0 23.1 1.63 -999.0 8.0 -999.0 368.0 -999.0 0.1 -999.0 94.6 53.0 126.0 1.5 121.0 9.08 5.49 2.09 30.8 9.65 3.0 14.0 1.72 -999.0 35.2 24.0 0.93 1560.0 -999.0 42.6 41.2 53.0 14.0 10.0 67.4 -999.0 0.4 36.0 -999.0 8.9 4.0 101.0 3.3 1.41 -999.0 8.9 0.6 0.84 2.32 325.0 1.0 42.2 5.9 174.0 508.0 17.2 0.05 1.68 0.02 16.0 1.56 10.2 1.84 0.21 0.59 0.23 46.9 -999.0 2.78 0.06 Lab_1
2 BLUE-H1 C-510966 BLUE-H1-17 soil B horizon 17.0 --- pit, hand dug 8.7 0.88 11.1 1.34 1.04 0.1 -999.0 21.0 1.54 2.0 8.0 -999.0 304.0 -999.0 0.1 -999.0 136.0 47.5 103.0 1.0 121.0 18.7 9.18 4.29 31.0 22.2 3.0 14.0 3.4 -999.0 88.5 22.0 1.15 1690.0 -999.0 44.1 99.2 45.0 16.0 24.3 59.7 -999.0 0.4 36.0 -999.0 20.9 5.0 71.1 2.6 3.22 -999.0 7.4 -999.0 1.26 2.06 297.0 1.0 79.2 7.8 190.0 529.0 17.8 0.05 1.32 0.02 16.5 1.76 9.67 1.88 0.23 0.48 0.27 46.7 -999.0 2.87 0.06 Lab_2
3 BLUE-H1 C-510967 BLUE-H1-32 soil C horizon 32.0 --- pit, hand dug 9.69 0.25 10.5 1.53 1.04 0.1 -999.0 22.6 1.39 1.0 7.0 -999.0 363.0 -999.0 -999.0 0.2 181.0 46.9 82.0 0.8 124.0 32.2 16.0 5.73 35.8 36.3 4.0 17.0 5.97 -999.0 118.0 43.0 1.67 2310.0 -999.0 53.3 144.0 60.0 14.0 33.2 59.6 -999.0 0.3 35.0 -999.0 30.3 6.0 17.5 3.1 5.48 -999.0 8.1 0.5 2.05 2.25 283.0 2.0 154.0 11.9 285.0 644.0 18.9 0.06 0.35 0.01 15.0 1.92 10.0 1.78 0.3 0.2 0.27 48.3 -999.0 2.45 0.05 Lab_3
4 BLUE-H1 C-510963 BLUE-H1-5 soil A horizon 5.0 --- pit, hand dug 7.86 1.29 8.44 1.21 0.87 0.14 -999.0 24.8 1.48 -999.0 6.0 -999.0 447.0 -999.0 0.2 0.7 161.0 46.0 97.0 1.6 82.0 28.2 13.3 5.3 27.2 31.0 2.0 14.0 5.12 -999.0 111.0 20.0 1.25 3340.0 -999.0 47.3 126.0 46.0 36.0 30.4 76.5 -999.0 0.6 27.0 6.0 26.5 7.0 106.0 4.8 4.85 -999.0 11.3 0.8 1.63 2.74 243.0 1.0 134.0 9.4 265.0 471.0 14.9 0.07 1.85 0.01 12.5 1.49 11.6 1.54 0.43 0.66 0.35 51.7 -999.0 2.56 0.05 Lab_4
5 BLUE-H1 C-510954 BLUE-H1-R weathered rock from augur hole --- --- pit, hand dug 7.21 0.39 11.0 2.39 1.25 0.24 -999.0 25.0 2.24 -999.0 14.0 -999.0 386.0 6.0 -999.0 0.4 219.0 48.2 -999.0 0.8 77.0 81.1 31.6 17.8 32.1 90.3 6.0 12.0 13.4 -999.0 300.0 28.0 2.38 2930.0 -999.0 29.4 385.0 41.0 12.0 92.1 86.5 -999.0 0.2 35.0 -999.0 88.2 4.0 17.1 2.0 14.6 -999.0 3.5 0.9 3.78 1.58 263.0 2.0 313.0 20.7 648.0 455.0 13.5 0.06 0.54 -999.0 16.3 2.93 5.62 2.14 0.37 0.05 0.55 54.0 -999.0 3.92 0.05 Lab_5
6 BLUE-H2 C-510970 BLUE-H2-17 soil B horizon 17.0 --- pit, hand dug 7.25 0.17 4.17 2.65 0.29 0.04 -999.0 31.7 0.48 2.0 -999.0 -999.0 203.0 -999.0 -999.0 -999.0 225.0 13.7 29.0 1.6 27.0 16.5 10.9 1.06 31.8 15.3 2.0 23.0 3.42 -999.0 72.0 12.0 1.6 491.0 -999.0 93.8 65.6 18.0 15.0 16.9 81.6 -999.0 0.3 7.0 -999.0 13.4 10.0 24.1 6.9 2.48 -999.0 13.6 0.6 1.57 3.04 90.0 1.0 93.0 10.4 140.0 924.0 14.1 0.04 0.22 -999.0 6.22 3.3 6.38 0.5 0.07 0.14 0.09 67.2 -999.0 0.84 0.02 Lab_6
7 BLUE-H2 C-510971 BLUE-H2-36 soil B horizon 36.0 --- pit, hand dug 7.49 0.13 3.56 3.0 0.24 0.02 -999.0 32.5 0.4 2.0 9.0 -999.0 146.0 -999.0 -999.0 -999.0 263.0 9.2 20.0 1.1 24.0 27.5 15.3 1.72 33.6 28.7 2.0 27.0 5.42 -999.0 138.0 -999.0 2.0 246.0 -999.0 105.0 128.0 17.0 12.0 33.0 71.8 -999.0 0.2 7.0 -999.0 25.1 12.0 17.2 7.4 4.45 -999.0 15.1 -999.0 2.15 3.22 68.0 1.0 147.0 13.4 141.0 1040.0 14.5 0.04 0.16 -999.0 5.27 3.74 5.47 0.41 0.03 0.12 0.05 68.8 -999.0 0.68 0.01 Lab_7
8 BLUE-H2 C-510972 BLUE-H2-60 soil C horizon 60.0 --- pit, hand dug 6.56 0.07 4.15 3.03 0.69 0.02 -999.0 33.0 0.45 2.0 -999.0 -999.0 173.0 -999.0 -999.0 0.2 252.0 17.1 25.0 0.7 29.0 38.7 19.4 2.76 40.4 42.5 3.0 24.0 6.96 -999.0 176.0 11.0 2.05 829.0 -999.0 93.5 186.0 15.0 9.0 47.1 136.0 -999.0 0.2 8.0 -999.0 38.3 8.0 6.2 6.2 6.67 -999.0 11.9 -999.0 2.55 2.38 106.0 2.0 199.0 14.5 140.0 940.0 12.8 0.05 0.07 -999.0 6.03 3.82 4.1 1.15 0.1 0.05 0.06 70.5 -999.0 0.78 0.02 Lab_8
9 BLUE-H2 C-510968 BLUE-H2-7 soil A horizon 7.0 --- pit, hand dug 6.38 0.28 4.69 2.2 0.36 0.07 -999.0 31.4 0.65 2.0 14.0 -999.0 277.0 -999.0 0.1 -999.0 246.0 53.4 34.0 1.6 39.0 47.7 20.6 3.89 29.8 50.8 3.0 17.0 8.31 -999.0 198.0 12.0 1.73 2290.0 -999.0 84.1 196.0 25.0 27.0 49.8 95.5 -999.0 0.5 10.0 -999.0 41.7 8.0 30.1 5.7 8.19 -999.0 10.1 0.5 2.42 3.0 115.0 1.0 236.0 13.1 159.0 691.0 12.4 0.05 0.39 -999.0 6.89 2.75 8.27 0.62 0.3 0.21 0.18 66.9 -999.0 1.13 0.02 Lab_9
10 BLUE-H2 C-510955 BLUE-H2-R rock from augur hole and float rock from field site --- --- pit, hand dug 6.47 0.07 2.59 4.82 0.19 -999.0 -999.0 34.5 0.18 1.0 -999.0 -999.0 130.0 -999.0 -999.0 -999.0 118.0 4.0 -999.0 0.2 7.0 19.2 12.2 1.11 27.9 17.9 2.0 27.0 3.83 0.2 85.5 -999.0 1.84 354.0 -999.0 85.0 95.2 21.0 7.0 26.2 93.0 -999.0 -999.0 -999.0 -999.0 19.6 9.0 19.7 5.9 3.1 -999.0 11.5 0.6 1.88 2.32 29.0 -999.0 98.6 12.4 50.0 1010.0 12.0 0.02 0.11 -999.0 3.79 5.94 2.33 0.35 0.04 0.51 0.02 74.3 -999.0 0.31 -999.0 Lab_10

Database Inventory

This summary of database content is provided as a convenience to GIS analysts, reviewers, and others. It is not part of the GeMS compliance criteria.

DataSources, nonspatial table, 3 rows
DescriptionOfMapUnits, nonspatial table, 19 rows
GeoMaterialDict, nonspatial table, 101 rows
Glossary, nonspatial table, 14 rows
LabDataTableBRS, nonspatial table, 10 rows
GeologicMap, feature dataset
    ContactsAndFaults, polyline feature class, 371 rows
    LabDataGenericPoints, point feature class, 2 rows
    MapUnitOverlayPolys, polygon feature class, 33 rows
    MapUnitPolys, polygon feature class, 57 rows
    OrientationPoints, point feature class, 335 rows