Historic Bayhorse mining district millsite in foreground to thick dolostone cliffs of disputed age--either Lower Ordovician or Neoproterozoic, a difference in interpretations of about 100 million years ago. The Bayhorse Mining district was one of the longest-running silver and lead producers in Idaho.
Karen Lund
Karen Lund is a Research Geologist with the Geology, Geophysics, and Geochemistry Science Center.
Science and Products
Salmon River Mountains Legacy Mining Studies
Northern Rocky Mountains Transect
Petrogenesis and REE Metallogenesis of 1.4 Ga Magmatism in the Conterminous U.S.
Basement Tectonic Framework of the U.S.: Role of Cratonization of Juvenile Crust and Structural Modification in Forming Metallogenic Provinces
Headwaters Province - Idaho and Montana: Earth Science Studies in Support of Public Policy Development and Land Stewardship
SHRIMP U-Pb and LA-ICPMS U-Pb geochronologic data for igneous and metasedimentary rocks in central Idaho mineral province, U.S.A.
Stream Temperature, Conductivity, eDNA, and Streamflow Data from the Big Creek and Monumental Creek Tributaries of the Lower Middle Fork Salmon River, Idaho 2021
Geochemical Data Release for Idaho Primitive Area, including the contiguous Clear Creek-Upper Big Deer Creek Area, the Salmon River Breaks Primitive Area, the Sawtooth Primitive Area, and adjacent areas, central Idaho (ver. 1.2, June 2022)
GIS Data (ver. 2) for Geologic Terranes of the Hailey 1 x 2 Degrees Quadrangle and the Western Part of the Idaho Falls 1 x 2 Degrees Quadrangle, South-Central Idaho
GIS and Data Tables for Focus Areas for Potential Domestic Nonfuel Sources of Rare Earth Elements
Digital Data for the Geologic Map of the Central Beaverhead Mountains, Lemhi County, Idaho, and Beaverhead County, Montana
U-Pb SHRIMP and 40Ar/39Ar geochronologic data and backscatter electron (BSE) and panchromatic cathodoluminescent (CL) imagery of sample materials for study of dikes, country rock, and alteration systems, Butte, U.S.A.
Geochemical Data Release for Gospel-Hump Wilderness Area, Magruder Corridor and Special Mining Management Zone Additions to the Frank Church River of No Return Wilderness Area, and adjacent areas Idaho and Montana
Locatable Mineral Assessment Tracts for the U.S. Geological Survey Sagebrush Mineral Resource Assessment Project
Geologic map of the central Beaverhead Mountains, Lemhi County, Idaho, and Beaverhead County, Montana
Precambrian crystalline basement map of Idaho: An interpretation of aeromagnetic anomalies
Geologic map of the Blackbird Mountain Quadrangle, Lemhi County, Idaho
Geologic map of the Slate Creek-John Day Creek area, Idaho County, Idaho
Historic Bayhorse mining district millsite in foreground to thick dolostone cliffs of disputed age--either Lower Ordovician or Neoproterozoic, a difference in interpretations of about 100 million years ago. The Bayhorse Mining district was one of the longest-running silver and lead producers in Idaho.
Pre-historic Nez Perce trail from the Wallowa Mountains of Oregon to the Great Plains to hunt bison. Ponderosa pine shows scars from the harvesting of cambium as a food source on those trips.
Pre-historic Nez Perce trail from the Wallowa Mountains of Oregon to the Great Plains to hunt bison. Ponderosa pine shows scars from the harvesting of cambium as a food source on those trips.
Exposure of breccia marking trace of normal fault. Clasts of country rock include Eocene granite dike materials and thus provide an age for the fault as Eocene or younger.
Exposure of breccia marking trace of normal fault. Clasts of country rock include Eocene granite dike materials and thus provide an age for the fault as Eocene or younger.
Roles of regional structures and country-rock facies in defining mineral belts in central Idaho mineral province with detail for Yellow Pine and Thunder Mountain mining districts
Temporal relations between the Boulder Batholith and Elkhorn Mountains Volcanics, western Montana: “The Nature of Batholiths” revised
Geology of the Payette National Forest and vicinity, west-central Idaho
Two-event genesis of Butte lode veins: Geologic and geochronologic evidence from ore veins, dikes, and host plutons
Two-event lode-ore deposition at Butte, USA: 40Ar/39Ar and U-Pb documentation of Ag-Au-polymetallic lodes overprinted by younger stockwork Cu-Mo ores and penecontemporaneous Cu lodes
The ore-genesis model for world-class deposits of the Butte mining district, Montana, USA, is deep pre-Main Stage porphyry Cu-Mo and overlying Main Stage Ag-Zn-Cu zoned-lode deposits, both of which formed from hydrothermal fluids driven by minor volumes of rhyolitic magma. The lode-specific model is that hydrothermal processes diminished in intensity outward from district center along lode veins,
Review of the geochemistry and metallogeny of approximately 1.4 Ga granitoid intrusions of the conterminous United States
Geology and mineral resources of the North-Central Idaho Sagebrush Focal Area: Chapter C in Mineral resources of the Sagebrush Focal Areas of Idaho, Montana, Nevada, Oregon, Utah, and Wyoming
Geochemical, modal, and geochronologic data for 1.4 Ga A-type granitoid intrusions of the conterminous United States
SHRIMP U–Pb and REE data pertaining to the origins of xenotime in Belt Supergroup rocks: evidence for ages of deposition, hydrothermal alteration, and metamorphism
Basement domain map of the conterminous United States and Alaska
Hells Canyon to the Bitterroot front: A transect from the accretionary margin eastward across the Idaho batholith
Descriptive and geoenvironmental model for Co-Cu-Au deposits in metasedimentary rocks
Science and Products
Salmon River Mountains Legacy Mining Studies
Northern Rocky Mountains Transect
Petrogenesis and REE Metallogenesis of 1.4 Ga Magmatism in the Conterminous U.S.
Basement Tectonic Framework of the U.S.: Role of Cratonization of Juvenile Crust and Structural Modification in Forming Metallogenic Provinces
Headwaters Province - Idaho and Montana: Earth Science Studies in Support of Public Policy Development and Land Stewardship
SHRIMP U-Pb and LA-ICPMS U-Pb geochronologic data for igneous and metasedimentary rocks in central Idaho mineral province, U.S.A.
Stream Temperature, Conductivity, eDNA, and Streamflow Data from the Big Creek and Monumental Creek Tributaries of the Lower Middle Fork Salmon River, Idaho 2021
Geochemical Data Release for Idaho Primitive Area, including the contiguous Clear Creek-Upper Big Deer Creek Area, the Salmon River Breaks Primitive Area, the Sawtooth Primitive Area, and adjacent areas, central Idaho (ver. 1.2, June 2022)
GIS Data (ver. 2) for Geologic Terranes of the Hailey 1 x 2 Degrees Quadrangle and the Western Part of the Idaho Falls 1 x 2 Degrees Quadrangle, South-Central Idaho
GIS and Data Tables for Focus Areas for Potential Domestic Nonfuel Sources of Rare Earth Elements
Digital Data for the Geologic Map of the Central Beaverhead Mountains, Lemhi County, Idaho, and Beaverhead County, Montana
U-Pb SHRIMP and 40Ar/39Ar geochronologic data and backscatter electron (BSE) and panchromatic cathodoluminescent (CL) imagery of sample materials for study of dikes, country rock, and alteration systems, Butte, U.S.A.
Geochemical Data Release for Gospel-Hump Wilderness Area, Magruder Corridor and Special Mining Management Zone Additions to the Frank Church River of No Return Wilderness Area, and adjacent areas Idaho and Montana
Locatable Mineral Assessment Tracts for the U.S. Geological Survey Sagebrush Mineral Resource Assessment Project
Geologic map of the central Beaverhead Mountains, Lemhi County, Idaho, and Beaverhead County, Montana
Precambrian crystalline basement map of Idaho: An interpretation of aeromagnetic anomalies
Geologic map of the Blackbird Mountain Quadrangle, Lemhi County, Idaho
Geologic map of the Slate Creek-John Day Creek area, Idaho County, Idaho
Historic Bayhorse mining district millsite in foreground to thick dolostone cliffs of disputed age--either Lower Ordovician or Neoproterozoic, a difference in interpretations of about 100 million years ago. The Bayhorse Mining district was one of the longest-running silver and lead producers in Idaho.
Historic Bayhorse mining district millsite in foreground to thick dolostone cliffs of disputed age--either Lower Ordovician or Neoproterozoic, a difference in interpretations of about 100 million years ago. The Bayhorse Mining district was one of the longest-running silver and lead producers in Idaho.
Pre-historic Nez Perce trail from the Wallowa Mountains of Oregon to the Great Plains to hunt bison. Ponderosa pine shows scars from the harvesting of cambium as a food source on those trips.
Pre-historic Nez Perce trail from the Wallowa Mountains of Oregon to the Great Plains to hunt bison. Ponderosa pine shows scars from the harvesting of cambium as a food source on those trips.
Exposure of breccia marking trace of normal fault. Clasts of country rock include Eocene granite dike materials and thus provide an age for the fault as Eocene or younger.
Exposure of breccia marking trace of normal fault. Clasts of country rock include Eocene granite dike materials and thus provide an age for the fault as Eocene or younger.
Roles of regional structures and country-rock facies in defining mineral belts in central Idaho mineral province with detail for Yellow Pine and Thunder Mountain mining districts
Temporal relations between the Boulder Batholith and Elkhorn Mountains Volcanics, western Montana: “The Nature of Batholiths” revised
Geology of the Payette National Forest and vicinity, west-central Idaho
Two-event genesis of Butte lode veins: Geologic and geochronologic evidence from ore veins, dikes, and host plutons
Two-event lode-ore deposition at Butte, USA: 40Ar/39Ar and U-Pb documentation of Ag-Au-polymetallic lodes overprinted by younger stockwork Cu-Mo ores and penecontemporaneous Cu lodes
The ore-genesis model for world-class deposits of the Butte mining district, Montana, USA, is deep pre-Main Stage porphyry Cu-Mo and overlying Main Stage Ag-Zn-Cu zoned-lode deposits, both of which formed from hydrothermal fluids driven by minor volumes of rhyolitic magma. The lode-specific model is that hydrothermal processes diminished in intensity outward from district center along lode veins,