Parent Layer: Heber City 7.5 M-295DM

Name: Geologic Units

Display Field: UnitName

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Description: The Heber City quadrangle includes the northern half of Heber Valley and much of Jordanelle Reservoir. Parts of the Park City mining district and Deer Valley Resort, and much of Wasatch Mountain State Park, occupy the northwestern part of the quadrangle. The area’s geology is dominated by Paleozoic- and Mesozoic-age shallow-marine and continental strata in the Wasatch Range, which host late Eocene- to early Oligocene-age shallow intrusions collectively called the Park City porphyries, the source of mineralization in what was once one of the West’s most important silver-lead-zinc mining districts. Volcanic rocks derived from these and other nearby shallow intrusions dominate the eastern half of the map area. The town of Midway, at the western edge of the valley, is well known for its hot springs and calcareous tufa deposits. Numerous hiking, mountain biking, and Nordic ski trails make this a popular year-round recreational area.

Copyright Text: Program Manager: Stefan M. Kirby (UGS) Project Manager: Robert F. Biek (UGS) GIS and Cartography: Basia Matyjasik and Jessica S. Pierson (UGS) Geology review: Zachary W. Anderson, Stefan M. Kirby, Stephanie M. Carney, and Michael D. Hylland (UGS) GIS and Cartography review: Rosemary Fasselin (UGS) Funding: U.S. Geological Survey, STATEMAP award number G18AC00202, 2018–2019

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Spatial Reference: 102100  (3857)

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• Value: 13;Qgmp1;Glacial till of Pinedale age
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• Value: 15;Qgmb;Older glacial till of likely Bull Lake age
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• Value: 16;Qmsh;Landslide deposits
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• Value: 19;Qmt;Talus
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• Value: 20;Qac;Alluvium and colluvium
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• Value: 25;Qst;Calcareous spring tufa deposits
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• Value: 26;Qaf2/Qst;Middle fan alluvium over calcareous spring tufa deposits
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• Value: 28;Qafo/PIPw;Old fan alluvium over Weber sandstone
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• Value: 30;QTa;Old alluvial deposits
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• Value: 31;Tkcf;Lava flows of Coyote Canyon
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• Value: 32;Tkcc;Volcanic mudflow breccia of Coyote Canyon
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• Value: 33;Tkcc(w);Brecciated Weber Sandstone block in volcanic mudflow breccia of Coyote Canyon
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• Value: 35;Tkf;Lava flows associated with Park Premier porphyry stocks
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• Value: 36;Tksh;Lava flows and volcanic mudflow breccia of Sage Hen Hollow
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• Value: 38;Tpp;Park Premier porphyry stock
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• Value: 39;Tppb;Park Premier porphyry, intrusive breccia phase
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• Value: 40;Tf;Flagstaff Mountain porphyry
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• Value: 41;Tfb;Flagstaff Mountain porphyry, intrusive breccia phase
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• Value: 42;To;Ontario porphyry
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• Value: 43;Tpc;Pine Creek porphyry
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• Value: 44;Tv;Valeo porphyry
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• Value: 45;Tg;Glencoe porphyry
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• Value: 46;Tm;Mayflower porphyry
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• Value: 47;Tjb;Jordanelle porphyry, breccia phase
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• Value: 48;Tj;Jordanelle porphyry
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• Value: 53;Jtr?;Twin Creek Limestone, Rich Member
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• Value: 54;Jts;Twin Creek Limestone, Sliderock Member
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• Value: 58;TRt;Thaynes Formation, undivided
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• Value: 59;TRtu;Thaynes Formation, upper unit
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• Value: 61;TRtl;Thaynes Formation, lower unit
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• Value: 62;TRw;Woodside Formation
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• Value: 63;Ppc;Park City and Phosphoria Formations, undivided
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• Value: 68;IPrv;Round Valley Limestone
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• Value: 69;IPrv?;Round Valley Limestone
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• Value: 70;Mdo;Doughnut Formation
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• Value: 71;Mh;Humbug Formation
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• Value: 72;Md;Deseret Limestone
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• Value: 74;Co;Ophir Formation
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• Value: 75;Ct;Tintic Quartzite
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