|Latitude & Longitude (WGS84):||39° 57' 3'' North , 112° 7' 5'' West|
|Latitude & Longitude (decimal):||39.95083,-112.11806|
|Köppen climate type:||Dfb : Warm-summer humid continental climate|
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17 valid minerals.
This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org
|Quaternary - Miocene|
0 - 23.03 Ma
|Cenozoic sedimentary rocks|
Age: Cenozoic (0 - 23.03 Ma)
Lithology: Sedimentary rocks
Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. 
0 - 2.588 Ma
|Alluvium and colluvium|
0 - 0.0117 Ma
Age: Anthropocene (0 - 0.0117 Ma)
Description: Man-made debris, slag heaps, mine dumps, mill tailings, and earthworks constructed from local materials. Some, such as embankments for dams, highway and railroad roadbeds, and engineering structures are engineered fills; others are random accumulations of various materials. Although not shown as the artificial fill unit, much of the Intermountain Power Project site is covered with graded and compacted local and imported earth materials.
Reference: Pampeyan, E.H. Geologic map of the Lynndyl 30′ x 60′ quadrangle, west-central Utah (digitized 2005). Utah Geological Survey Miscellaneous Investigations Series Map I-1830.