OBJECTID|Term|Definition|DefinitionSourceID|Glossary_ID
|1|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|GLO001
2|questionable|Identity of a feature cannot be determined using relevant observations and scientific judgment; therefore, one cannot be reasonably confident in the credibility of this interpretation. For example, IdentityConfidence = questionable is appropriate when a geologist reasons "I can see some kind of planar feature that separates map units in this outcrop, but I cannot be certain if it is a contact or a fault."|FGDC-STD-013-2006|GLO002
3|Anticline- location approximate|A fold, generally convex upward, whose core contains the stratigraphically older rocks. Location approximate.|NeueKKE2005|GLO003
4|Anticline- location concealed|A fold, generally convex upward, whose core contains the stratigraphically older rocks. Location concealed.|NeueKKE2005|GLO004
5|Monocline- location approximate|A local steepening in an otherwise uniform gentle dip. Location approximate.|NeueKKE2005|GLO005
6|Monocline- location inferred|A local steepening in an otherwise uniform gentle dip. Location inferred.|NeueKKE2005|GLO006
7|Monocline- location concealed|A local steepening in an otherwise uniform gentle dip. Location concealed.|NeueKKE2005|GLO007
8|Syncline- location approximate|A fold of which the core contains the stratigraphically younger rocks; it is generally concave upward. Location approximate.|NeueKKE2005|GLO008
9|Syncline- location concealed|A fold of which the core contains the stratigraphically younger rocks; it is generally concave upward. Location concealed.|NeueKKE2005|GLO009
10|DGMI H2|Heading 2 paragraph style. Cambria, Bold, 12pt, left justified|McClJD2024|GLO010
11|DGMI H3|Heading 3 paragraph style. Cambria Bold 11pt left justified|McClJD2024|GLO011
12|DGMI H4|Heading 4 paragraph style. Cambria Bold 10pt left justified|McClJD2024|GLO012
13|DGMI H5|Heading 5 paragraph style. Cambria Bold 9pt left justified|McClJD2024|GLO013
14|DGMI H6|Heading 6 paragraph style. Cambria Bold Italic 9pt left justified|McClJD2024|GLO014
15|DGMI Unit Label|Unit label paragraph style. Cambria Bold 9pt left justified|McClJD2024|GLO015
16|Contact- location accurate|A plane or irregular surface between two types or ages of rock (accuratly located); examples are intrusive borders, bedding planes separating distinct strata, and unconformities.|NeueKKE2005b|GLO016
17|Contact- location approximate|A plane or irregular surface between two types or ages of rock (approximatly located); examples are intrusive borders, bedding planes separating distinct strata, and unconformities.|NeueKKE2005b|GLO017
18|Contact- location inferred|A plane or irregular surface between two types or ages of rock (location inferred); examples are intrusive borders, bedding planes separating distinct strata, and unconformities.|NeueKKE2005b|GLO018
19|Contact- location concealed|A plane or irregular surface between two types or ages of rock (location concealed); examples are intrusive borders, bedding planes separating distinct strata, and unconformities.|NeueKKE2005b|GLO019
20|Internal contact- location accurate|The planar or irregular surface between separately emplaced portions of the same rock type.|NeueKKE2005b|GLO020
21|Fault, unknown offset- location accurate|A discrete surface or zone of discrete surfaces separating two rock masses across which one mass has slid past the other that has generic; vertical, subvertical, or high-angle; or unknown or unspecified orientation or sense of slip. Location accurate.|NeueKKE2005b|GLO021
22|Fault, unknown offset- location approximate|A discrete surface or zone of discrete surfaces separating two rock masses across which one mass has slid past the other that has generic; vertical, subvertical, or high-angle; or unknown or unspecified orientation or sense of slip. Location approximate.|NeueKKE2005b|GLO022
23|Fault, unknown offset- location inferred|A discrete surface or zone of discrete surfaces separating two rock masses across which one mass has slid past the other that has generic; vertical, subvertical, or high-angle; or unknown or unspecified orientation or sense of slip. Location inferred.|NeueKKE2005b|GLO023
24|Fault, unknown offset- location concealed|A discrete surface or zone of discrete surfaces separating two rock masses across which one mass has slid past the other that has generic; vertical, subvertical, or high-angle; or unknown or unspecified orientation or sense of slip. Location concealed.|NeueKKE2005b|GLO024
25|Normal fault- location accurate|A fault in which the hanging wall has moved downward relative to the footwall (location accurate). The angle of the fault is usually 45-90 degrees, and in most cases close to 60 degrees.|NeueKKE2005b|GLO025
26|Normal fault- location approximate|A fault in which the hanging wall has moved downward relative to the footwall (location approximate). The angle of the fault is usually 45-90 degrees, and in most cases close to 60 degrees.|NeueKKE2005b|GLO026
27|Normal fault- location inferred|A fault in which the hanging wall has moved downward relative to the footwall (location inferred). The angle of the fault is usually 45-90 degrees, and in most cases close to 60 degrees.|NeueKKE2005b|GLO027
28|Normal fault- location concealed|A fault in which the hanging wall has moved downward relative to the footwall (location concealed). The angle of the fault is usually 45-90 degrees, and in most cases close to 60 degrees.|NeueKKE2005b|GLO028
29|Thrust fault- location accurate|A fault with a dip of 45 degrees or less over much of its extent, on which the hangingwall has moved upward relative to the footwall. Location accurate.|NeueKKE2005b|GLO029
30|Reverse fault- location approximate|A fault on which the hanging wall appears to have moved upward relative to the footwall (location approximate). The dip of the fault is usually greater than 45 degrees. There is dip separation but there may or may not be dip slip.|NeueKKE2005|GLO030
33|Strike-slip fault, right-lateral offset- location accurate|A fault on which the movement is parallel to the fault's strike and on which the side opposite the observer has been displaced to the right. Location accurate.|NeueKKE2005b|GLO033
34|Strike-slip fault, right-lateral offset- location approximate|A fault on which the movement is parallel to the fault's strike and on which the side opposite the observer has been displaced to the right. Location approximate.|NeueKKE2005b|GLO034
35|Strike-slip fault, right-lateral offset- location inferred|A fault on which the movement is parallel to the fault's strike and on which the side opposite the observer has been displaced to the right. Location inferred.|NeueKKE2005b|GLO035
36|Strike-slip fault, right-lateral offset- location concealed|A fault on which the movement is parallel to the fault's strike and on which the side opposite the observer has been displaced to the right. Location concealed.|NeueKKE2005b|GLO036
37|Oblique-slip fault, right-lateral- location accurate|A fault on which the net slip has dip slip and strike slip components on which the side opposite the observer has been displaced to the right. Location accurate.|NeueKKE2005|GLO037
38|Oblique-slip fault, right-lateral- location approximate|A fault on which the net slip has dip slip and strike slip components on which the side opposite the observer has been displaced to the right. Location approximate.|NeueKKE2005|GLO038
39|Oblique-slip fault, right-lateral- location inferred|A fault on which the net slip has dip slip and strike slip components on which the side opposite the observer has been displaced to the right. Location inferred.|NeueKKE2005|GLO039
40|Oblique-slip fault, right-lateral- location concealed|A fault on which the net slip has dip slip and strike slip components on which the side opposite the observer has been displaced to the right. Location concealed.|NeueKKE2005|GLO040
41|Oblique-slip fault, left-lateral- location accurate|A fault on which the net slip has dip slip and strike slip components on which the side opposite the observer has been displaced to the left. Location accurate.|NeueKKE2005b|GLO041
42|Oblique-slip fault, left-lateral- location approximate|A fault on which the net slip has dip slip and strike slip components on which the side opposite the observer has been displaced to the left. Location approximate.|NeueKKE2005b|GLO042
44|Oblique-slip fault, left-lateral- location concealed|A fault on which the net slip has dip slip and strike slip components on which the side opposite the observer has been displaced to the left. Location concealed.|NeueKKE2005b|GLO044
45|Thrust fault- location approximate|A fault with a dip of 45 degrees or less over much of its extent, on which the hangingwall has moved upward relative to the footwall. Location approximate.|NeueKKE2005b|GLO045
46|Thrust fault- location inferred|A fault with a dip of 45 degrees or less over much of its extent, on which the hangingwall has moved upward relative to the footwall. Location inferred.|NeueKKE2005b|GLO046
47|Thrust fault- location concealed|A fault with a dip of 45 degrees or less over much of its extent, on which the hangingwall has moved upward relative to the footwall. Location concealed.|NeueKKE2005b|GLO047
48|Inclined bedding|An inclusive term for bedding inclined to the principal surface of deposition.|NeueKKE2005|GLO048
49|Gently inclined bedding, as determined remotely or from aerial photographs- Showing approximate strike and direction of dip|A term for bedding inclined (between 0° and 30°) to the principal surface of deposition. As determined remotely from a digital elevation model or from aerial photographs.|NeueKKE2005b|GLO049
50|Moderately inclined bedding, as determined remotely or from aerial photographs- Showing approximate strike and direction of dip|A term for bedding inclined (between 30° and 60°) to the principal surface of deposition. As determined remotely from a digital elevation model or from aerial photographs.|NeueKKE2005b|GLO050
51|Steeply inclined bedding, as determined remotely or from aerial photographs- Showing approximate strike and direction of dip|A term for bedding inclined (between 60° and 90°) to the principal surface of deposition. As determined remotely from a digital elevation model or from aerial photographs.|NeueKKE2005b|GLO051
52|Water well, type unspecified|Water well, type unspecified|FGDC-STD-013-2006|GLO052
53|Well used for domestic-water supply|Well used for domestic-water supply|FGDC-STD-013-2006|GLO053
54|cross-section line|Vector lines that have no real-world physical existence and do not participate in map-unit topology.|McClJD2024|GLO054
55|Portable Fluxgate Magnetometer|A portable electrical instrument that measures the change in magnetic field along the axis of its sensor with  sensitivity of one gamma or more. Readings are displayed digitally.|NeueKKE2005b|GLO055
58|XRF|X-ray fluorescence spectroscopy: A type of X-ray emission spectroscopy in which the characteristic X-ray spectrum of a substance is produced by using X-rays of short wavelength to induce the substance to emit X-rays of a longer wavelength.|NeueKKE2005|GLO058
59|High|Qualifier for GeneralLithology: The term and definition adequately characterize the overall lithology of the map unit.|USGS-GeMS-2020|GLO059
60|Medium|Qualifier for GeneralLithology: The term and definition generally characterize the overall lithology of the map unit, but there are one or more significant minor lithologies that are not described by the selected term.|USGS-GeMS-2020|GLO060
