OBJECTID|Term|Definition|DefinitionSourceID|Glossary_ID|created_user|created_date|last_edited_user|last_edited_date
|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|GLO0001|||ROMPA|2022-04-22 13:50:03
3|Ice-contact face|Ice-contact slope: The steep slope of sediment that was deposited against a wall of glacier ice, marking the position of the ice margin (glacial boundary); an irregular scarp against which glacier ice once rested.|AGI_2005|GLO0003|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-10 09:05:53
4|contact|A plane or irregular surface between two types or ages of rock; examples are faults, intrusive borders, bedding planes separating distinct strata, and unconformities.|AGI_2005|GLO0004|ROMPA|2022-04-21 13:30:11|ROMPA|2022-04-22 13:50:03
5|stream cutbank|A local term in the Western U.S. for a steep bare slope formed by lateral erosion of a stream.|AGI_2005|GLO0005|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-02 09:32:50
6|shoreline|The intersection of a specified plane of water with the shore or beach; it migrates with changes of the tide or of the water level.|AGI_2005|GLO0006|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-02 09:32:50
7|map boundary|Neat line: The line that surrounds a map, separating the map from the margin.|AGI_2005|GLO0007|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-02 09:46:12
8|drumlin|A low, smoothly rounded, elongate oval hill, mound, or ridge of compact glacial till or, less commonly, other kinds of drift (sandy till, varved clay), built under the margin of ice and shaped by its flow, or carved out of an older moraine by readvancing ice; its longer axis is parallel to the direction of movement of the ice. It usually has a blunt nose pointing in the direction from which the ice approached, and a gentler slope tapering in the other direction.|AGI_2005|GLO0008|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-02 09:32:50
9|esker|A long, narrow, sinuous, steep-sided ridge composed of irregularly stratified sand and gravel that was deposited by a subglacial or englacial stream flowing between ice walls or in an ice tunnel of a stagnant or retreating glacier.|AGI_2005|GLO0009|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-02 09:32:50
10|ice-margin position|Glacial boundary: The position occupied, in a given region or during a given glacial stage, by the outer or lower margin of an ice sheet; this may extend beyond the terminal moraine.|AGI_2005|GLO0010|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-02 09:32:50
11|sand dune|An accumulation of loose sand heaped up by the wind, commonly found along low-lying seashores above high-tide level, more rarely on the border of large lakes of river valleys, as well as in various desert regions, where abundant dry surface sand is present during some part of the year.|AGI_2005|GLO0011|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-02 09:32:50
12|meltwater channel|Meltwater: water derived from the melting of snow or ice, esp. the stream flowing in, under, or from melting glacier ice|AGI_2005|GLO0012|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-02 09:04:30.000001
13|steep slope|The inclined surface of any part of the Earth’s surface as a hillslope|AGI_2005|GLO0013|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-02 09:04:30.000001
14|moraine crest|Moraine: a mound, ridge, or other distinct accumulation of unsorted, unstratified glacial drift, prodominately till, deposited chiefly by direct action of glacier ice, in a variety of topographic landforms that are independent of the surface on which the drift lies.|AGI_2005|GLO0014|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-02 09:32:50
16|Heading2|Cambria, 16 pt, teal|FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|GLO0016|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-13 14:22:35
17|Heading3|Cambria, 15 pt, tan|FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|GLO0017|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-13 14:22:35
18|standaloneunit|Segoe UI, 10 pt|FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|GLO0018|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-13 14:22:35
19|superunit|Segoe UI, 10 pt|FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|GLO0019|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-13 14:22:35
20|subunit|Segoe UI, 10 pt|FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|GLO0020|ROMPA|2022-04-21 13:30:11|ROMPA|2022-05-13 14:22:35
21|high|The selected term in the GeoMaterial field (and its definition) adequately characterizes1 the overall lithologic nature of rocks and (or) sediments in the map unit.|GeMS_2020|GLO0023|ROMPA|2022-05-02 09:17:59|ROMPA|2022-05-10 09:22:55
22|medium|The selected term in the GeoMaterial field (and its definition) generally characterizes the overall lithologic nature of rocks and (or) sediments in the map unit, but one or more significant but minor lithologies are not adequately described by the selected term.|GeMS_2020|GLO0022|ROMPA|2022-05-02 09:17:59|ROMPA|2022-05-10 09:22:55
23|low|Either (1) the overall lithologic nature of rocks and (or) sediments in this map unit is not adequately classifiable using the available list of GeoMaterial terms (and their definitions), but the selected term is the best available, or (2) this map unit is not sufficiently known enough to confidently assign a GeoMaterial term.|GeMS_2020|GLO0021|ROMPA|2022-05-02 09:17:59|ROMPA|2022-05-10 09:22:55
