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
3|Anticline- location approximate|A fold, generally convex upward, whose core contains the stratigraphically older rocks. Location approximate.|NeueKKE2005|GLO003
4|Syncline- location approximate|A fold of which the core contains the stratigraphically younger rocks; it is generally concave upward. Location approximate.|NeueKKE2005|GLO004
5|DGMI H2|Heading 2 paragraph style. Cambria, Bold, 12pt, left justified|McClJD2024|GLO005
6|DGMI H3|Heading 3 paragraph style. Cambria Bold 11pt left justified|McClJD2024|GLO006
7|DGMI H4|Heading 4 paragraph style. Cambria Bold 10pt left justified|McClJD2024|GLO007
8|DGMI H5|Heading 5 paragraph style. Cambria Bold 9pt left justified|McClJD2024|GLO008
9|DGMI H6|Heading 6 paragraph style. Cambria Bold Italic 9pt left justified|McClJD2024|GLO009
10|DGMI Unit Label|Unit label paragraph style. Cambria Bold 9pt left justified|McClJD2024|GLO010
11|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|GLO011
12|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|GLO012
13|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|GLO013
14|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. Location approximate.|NeueKKE2005|GLO014
15|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. Location concealed.|NeueKKE2005|GLO015
16|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|GLO016
17|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|GLO017
18|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|GLO018
19|Reverse fault- location concealed|A fault on which the hanging wall appears to have moved upward relative to the footwall (location concealed). 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|GLO019
20|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|GLO020
21|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|GLO021
22|Strike-slip fault, left-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 left. Location approximate.|NeueKKE2005|GLO022
23|Strike-slip fault, left-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 left. Location inferred.|NeueKKE2005|GLO023
24|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|GLO024
25|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.|NeueKKE2005b|GLO025
26|Horizontal bedding|An inclusive term for bedding parallel to the principal surface of deposition.|NeueKKE2005b|GLO026
27|Inclined bedding|An inclusive term for bedding inclined to the principal surface of deposition.|NeueKKE2005|GLO027
28|Horizontal bedding, as determined remotely or from aerial photographs|A term for bedding parallel to the principal surface of deposition. As determined remotely from a digital elevation model or from aerial photographs.|NeueKKE2005b|GLO028
29|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|GLO029
30|Moderately inclined bedding, as determined remotely or from aerial photographs- Showing approximate strike and direction of dip|An inclusive 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|GLO030
31|Water well, type unspecified|Water well, type unspecified|FGDC-STD-013-2006|GLO031
32|Well used for domestic-water supply|Well used for domestic-water supply|FGDC-STD-013-2006|GLO032
33|Well used for irrigation-water supply|Well used for irrigation-water supply|FGDC-STD-013-2006|GLO033
34|Well used for public-water supply|Well used for public-water supply|FGDC-STD-013-2006|GLO034
35|Cross-section line|Vector lines that have no real-world physical existence and do not participate in map-unit topology.|McClJD2024|GLO035
36|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|GLO036
37|Ma|Mega-annum, one million (10^6) years. Informal SI notation, where annum is age in years before present, with "present" fixed as 1950. Ths term has lagely replaced the various abbrevations for "millions of years before present" in geologcal literature. It is not equivalent to the elapsed time interval or duration in "millions of years" (myr).|NeueKKE2005|GLO037
38|K-Ar|Potassium-argon age method. Determination of the age of a mineral or rock in years, based on measurement of the ratio of radiogenic argon-40 to potassium-40 and the known radioactive decay rate of potassium-40 to argon-40.|NeueKKE2005|GLO038
39|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|GLO039
40|High|Qualifier for GeneralLithology: The term and definition adequately characterize the overall lithology of the map unit.|USGS-GeMS-2020|GLO040
41|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|GLO041
42|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|GLO042
43|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|GLO043
44|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
