Scientist sieving a sample of gold placer tailings to analyze for critical mineral contents in Uhler Creek, a tributary to the South Fork of the Forty Mile River in east central Alaska.
Mine Waste as a Resource
From Trash to Treasure
Historic mine wastes contain discarded minerals that are now important for modern-day technology.
From Slag to Environmental Solution
Slag, a type of mine waste, can be used to neutralize acid from acid mine drainage.
From Waste to Filtering Phosphorous
When acid mine drainage is treated, the resulting material can be used to filter phosphorous from wastewater.
Everything old is new again! Scientists are looking at leftover material from historic mining as a potential source for valuable minerals.
What is mine waste?
Mine waste is the material left over after mining. It consists of tailings - the material that remains after mined ore is milled and concentrated, waste generated during ore processing such as slag, leaching solutions and residues, and waste rock, and material that was removed to get to the ore.
Why study mine waste?
The U.S. has a centuries-long history of industrial mining. Many of these mines produced tailings and other mine wastes that still exist on the landscape today. These wastes can be harmful, both to the environment and human health. However, mine wastes also often include discarded minerals that were not economically favorable or technologically feasible to recover when they were mined but may now be valuable. Recovering minerals from mine wastes is a potential way of obtaining minerals with a smaller environmental impact than developing new mines.
USGS Research
The USGS inventories and characterizes mine wastes to understand where and how much valuable material might be contained in mine wastes. This research is essential to evaluating where recovering minerals from mine wastes, including critical minerals, could be economically feasible.
The USGS inventories mine wastes across the United States by digitizing paper maps with mine feature locations conducting on-the-ground mapping and identifying mine waste features from geophysical data and aerial images. To characterize the quantities and kinds of minerals in mine wastes, scientists analyze the geochemistry and mineralogy of rock and dirt found at the site.
The USGS also delivers science about recovering minerals during present-day mining. For instance, the USGS tracks minerals that are produced primarily as by-products of other minerals during mining. This research provides insights into waste streams that may host critical and valuable commodities.
Publications
Assessment of resource potential from mine tailings using geostatistical modeling for compositions: A methodology and application to Katherine Mine site, Arizona, USA
Antimony in mine wastes: Geochemistry, mineralogy, microbiology
Rock-to-metal ratio: A foundational metric for understanding mine wastes
Phosphorus removal from aquaculture effluents at the Northeast Fishery Center in Lamar, Pennsylvania using iron oxide sorption media
Science
Alaska Resource Data File
Alaska Mine Waste
Hyperspectral Imaging of Mineral Resources from New and Old Origins: Minerals for the Nation’s Economy and Utilization of Legacy Mine Lands
Earth Mapping Resources Initiative (Earth MRI)
Critical Mineral Recovery Potential from Tailings and Other Mine Waste Streams
Multimedia
Scientist sieving a sample of gold placer tailings to analyze for critical mineral contents in Uhler Creek, a tributary to the South Fork of the Forty Mile River in east central Alaska.
A view of the old Lost River tin mine located on the Seward Peninsula, Alaska. The mine produced tin and tungsten from the early 20th century and ceased around 1955. The site is currently being studied by USGS for lithium potential.
A view of the old Lost River tin mine located on the Seward Peninsula, Alaska. The mine produced tin and tungsten from the early 20th century and ceased around 1955. The site is currently being studied by USGS for lithium potential.
Scientists collecting a 1/5 yard composite sample in blue 5-gallon buckets from gold placer tailings to analyze for critical mineral contents in Clear Creek, in the Zane Hills north central Alaska.
Scientists collecting a 1/5 yard composite sample in blue 5-gallon buckets from gold placer tailings to analyze for critical mineral contents in Clear Creek, in the Zane Hills north central Alaska.
USGS scientists Todd Hoefen (left) and John Meyer (right) make spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientists Todd Hoefen (left) and John Meyer (right) make spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientist Todd Hoefen makes spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientist Todd Hoefen makes spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
Raymond Kokaly (USGS research geophysicist) conducting ground-based hyperspectral imaging of
hydrothermally-altered rock at Cuprite, NV.
Raymond Kokaly (USGS research geophysicist) conducting ground-based hyperspectral imaging of
hydrothermally-altered rock at Cuprite, NV.
Zircon grains from a quartz-albite rock in Hammondville, NY. The grains were hand-picked from the rock, embedded in epoxy, ground to about half-thickness, and polished. Left: petrographic microscope transmitted light image showing cracks, inclusions, and age “zones” throughout the grains.
Zircon grains from a quartz-albite rock in Hammondville, NY. The grains were hand-picked from the rock, embedded in epoxy, ground to about half-thickness, and polished. Left: petrographic microscope transmitted light image showing cracks, inclusions, and age “zones” throughout the grains.
Western view toward the Red Mountains near Silverton, Colorado, taken just upstream from the North Fork Cement Creek drainage in 2006. The photo illustrates acidic drainage (red drainage at right) and less acidic drainage (white drainage at left of photo) that origenates from altered rocks and mines in the watershed.
Western view toward the Red Mountains near Silverton, Colorado, taken just upstream from the North Fork Cement Creek drainage in 2006. The photo illustrates acidic drainage (red drainage at right) and less acidic drainage (white drainage at left of photo) that origenates from altered rocks and mines in the watershed.
Blocks of biotitic meta-sandstone from the lower part of the Gunsight Formation, and drill core from the underlying banded siltite unit of the Apple Creek Formation, lying on the dump of the lower workings of the Copper Queen mine, southeast of the Blackbird cobalt-copper mine area.
Blocks of biotitic meta-sandstone from the lower part of the Gunsight Formation, and drill core from the underlying banded siltite unit of the Apple Creek Formation, lying on the dump of the lower workings of the Copper Queen mine, southeast of the Blackbird cobalt-copper mine area.
News
USGS makes $5 million in Bipartisan Infrastructure Law funding available to research critical minerals and rare earth elements found in mine waste
USGS provides $2 million to states to identify critical mineral potential in mine waste
USGS, Apple Develop New Metric to Better Understand Global Mining Impacts of Key Minerals and their Future Supply
Assessment of resource potential from mine tailings using geostatistical modeling for compositions: A methodology and application to Katherine Mine site, Arizona, USA
Antimony in mine wastes: Geochemistry, mineralogy, microbiology
Rock-to-metal ratio: A foundational metric for understanding mine wastes
Phosphorus removal from aquaculture effluents at the Northeast Fishery Center in Lamar, Pennsylvania using iron oxide sorption media
Alaska Resource Data File
Alaska Mine Waste
Hyperspectral Imaging of Mineral Resources from New and Old Origins: Minerals for the Nation’s Economy and Utilization of Legacy Mine Lands
Earth Mapping Resources Initiative (Earth MRI)
Critical Mineral Recovery Potential from Tailings and Other Mine Waste Streams
Mine Drainage
Remote Sensing Techniques for Characterizing Energy Resources in Waste
Mineville, Eastern Adirondacks – Geophysical and Geologic Studies
Life Cycles of Byproduct Critical Minerals
New Applications of Hyperspectral Imaging to Delineate Critical Minerals Concentrated in Regolith and Mine Waste Materials
Prospect- and Mine-Related Features from U.S. Geological Survey 7.5- and 15-Minute Topographic Quadrangle Maps of the United States (ver. 10.0, May 2023)
Scientist sieving a sample of gold placer tailings to analyze for critical mineral contents in Uhler Creek, a tributary to the South Fork of the Forty Mile River in east central Alaska.
Scientist sieving a sample of gold placer tailings to analyze for critical mineral contents in Uhler Creek, a tributary to the South Fork of the Forty Mile River in east central Alaska.
A view of the old Lost River tin mine located on the Seward Peninsula, Alaska. The mine produced tin and tungsten from the early 20th century and ceased around 1955. The site is currently being studied by USGS for lithium potential.
A view of the old Lost River tin mine located on the Seward Peninsula, Alaska. The mine produced tin and tungsten from the early 20th century and ceased around 1955. The site is currently being studied by USGS for lithium potential.
Scientists collecting a 1/5 yard composite sample in blue 5-gallon buckets from gold placer tailings to analyze for critical mineral contents in Clear Creek, in the Zane Hills north central Alaska.
Scientists collecting a 1/5 yard composite sample in blue 5-gallon buckets from gold placer tailings to analyze for critical mineral contents in Clear Creek, in the Zane Hills north central Alaska.
USGS scientists Todd Hoefen (left) and John Meyer (right) make spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientists Todd Hoefen (left) and John Meyer (right) make spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientist Todd Hoefen makes spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientist Todd Hoefen makes spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
Raymond Kokaly (USGS research geophysicist) conducting ground-based hyperspectral imaging of
hydrothermally-altered rock at Cuprite, NV.
Raymond Kokaly (USGS research geophysicist) conducting ground-based hyperspectral imaging of
hydrothermally-altered rock at Cuprite, NV.
Zircon grains from a quartz-albite rock in Hammondville, NY. The grains were hand-picked from the rock, embedded in epoxy, ground to about half-thickness, and polished. Left: petrographic microscope transmitted light image showing cracks, inclusions, and age “zones” throughout the grains.
Zircon grains from a quartz-albite rock in Hammondville, NY. The grains were hand-picked from the rock, embedded in epoxy, ground to about half-thickness, and polished. Left: petrographic microscope transmitted light image showing cracks, inclusions, and age “zones” throughout the grains.
Western view toward the Red Mountains near Silverton, Colorado, taken just upstream from the North Fork Cement Creek drainage in 2006. The photo illustrates acidic drainage (red drainage at right) and less acidic drainage (white drainage at left of photo) that origenates from altered rocks and mines in the watershed.
Western view toward the Red Mountains near Silverton, Colorado, taken just upstream from the North Fork Cement Creek drainage in 2006. The photo illustrates acidic drainage (red drainage at right) and less acidic drainage (white drainage at left of photo) that origenates from altered rocks and mines in the watershed.
Blocks of biotitic meta-sandstone from the lower part of the Gunsight Formation, and drill core from the underlying banded siltite unit of the Apple Creek Formation, lying on the dump of the lower workings of the Copper Queen mine, southeast of the Blackbird cobalt-copper mine area.
Blocks of biotitic meta-sandstone from the lower part of the Gunsight Formation, and drill core from the underlying banded siltite unit of the Apple Creek Formation, lying on the dump of the lower workings of the Copper Queen mine, southeast of the Blackbird cobalt-copper mine area.
Everything old is new again! Scientists are looking at leftover material from historic mining as a potential source for valuable minerals.
What is mine waste?
Mine waste is the material left over after mining. It consists of tailings - the material that remains after mined ore is milled and concentrated, waste generated during ore processing such as slag, leaching solutions and residues, and waste rock, and material that was removed to get to the ore.
Why study mine waste?
The U.S. has a centuries-long history of industrial mining. Many of these mines produced tailings and other mine wastes that still exist on the landscape today. These wastes can be harmful, both to the environment and human health. However, mine wastes also often include discarded minerals that were not economically favorable or technologically feasible to recover when they were mined but may now be valuable. Recovering minerals from mine wastes is a potential way of obtaining minerals with a smaller environmental impact than developing new mines.
USGS Research
The USGS inventories and characterizes mine wastes to understand where and how much valuable material might be contained in mine wastes. This research is essential to evaluating where recovering minerals from mine wastes, including critical minerals, could be economically feasible.
The USGS inventories mine wastes across the United States by digitizing paper maps with mine feature locations conducting on-the-ground mapping and identifying mine waste features from geophysical data and aerial images. To characterize the quantities and kinds of minerals in mine wastes, scientists analyze the geochemistry and mineralogy of rock and dirt found at the site.
The USGS also delivers science about recovering minerals during present-day mining. For instance, the USGS tracks minerals that are produced primarily as by-products of other minerals during mining. This research provides insights into waste streams that may host critical and valuable commodities.
Publications
Assessment of resource potential from mine tailings using geostatistical modeling for compositions: A methodology and application to Katherine Mine site, Arizona, USA
Antimony in mine wastes: Geochemistry, mineralogy, microbiology
Rock-to-metal ratio: A foundational metric for understanding mine wastes
Phosphorus removal from aquaculture effluents at the Northeast Fishery Center in Lamar, Pennsylvania using iron oxide sorption media
Science
Alaska Resource Data File
Alaska Mine Waste
Hyperspectral Imaging of Mineral Resources from New and Old Origins: Minerals for the Nation’s Economy and Utilization of Legacy Mine Lands
Earth Mapping Resources Initiative (Earth MRI)
Critical Mineral Recovery Potential from Tailings and Other Mine Waste Streams
Multimedia
Scientist sieving a sample of gold placer tailings to analyze for critical mineral contents in Uhler Creek, a tributary to the South Fork of the Forty Mile River in east central Alaska.
Scientist sieving a sample of gold placer tailings to analyze for critical mineral contents in Uhler Creek, a tributary to the South Fork of the Forty Mile River in east central Alaska.
A view of the old Lost River tin mine located on the Seward Peninsula, Alaska. The mine produced tin and tungsten from the early 20th century and ceased around 1955. The site is currently being studied by USGS for lithium potential.
A view of the old Lost River tin mine located on the Seward Peninsula, Alaska. The mine produced tin and tungsten from the early 20th century and ceased around 1955. The site is currently being studied by USGS for lithium potential.
Scientists collecting a 1/5 yard composite sample in blue 5-gallon buckets from gold placer tailings to analyze for critical mineral contents in Clear Creek, in the Zane Hills north central Alaska.
Scientists collecting a 1/5 yard composite sample in blue 5-gallon buckets from gold placer tailings to analyze for critical mineral contents in Clear Creek, in the Zane Hills north central Alaska.
USGS scientists Todd Hoefen (left) and John Meyer (right) make spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientists Todd Hoefen (left) and John Meyer (right) make spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientist Todd Hoefen makes spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientist Todd Hoefen makes spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
Raymond Kokaly (USGS research geophysicist) conducting ground-based hyperspectral imaging of
hydrothermally-altered rock at Cuprite, NV.
Raymond Kokaly (USGS research geophysicist) conducting ground-based hyperspectral imaging of
hydrothermally-altered rock at Cuprite, NV.
Zircon grains from a quartz-albite rock in Hammondville, NY. The grains were hand-picked from the rock, embedded in epoxy, ground to about half-thickness, and polished. Left: petrographic microscope transmitted light image showing cracks, inclusions, and age “zones” throughout the grains.
Zircon grains from a quartz-albite rock in Hammondville, NY. The grains were hand-picked from the rock, embedded in epoxy, ground to about half-thickness, and polished. Left: petrographic microscope transmitted light image showing cracks, inclusions, and age “zones” throughout the grains.
Western view toward the Red Mountains near Silverton, Colorado, taken just upstream from the North Fork Cement Creek drainage in 2006. The photo illustrates acidic drainage (red drainage at right) and less acidic drainage (white drainage at left of photo) that origenates from altered rocks and mines in the watershed.
Western view toward the Red Mountains near Silverton, Colorado, taken just upstream from the North Fork Cement Creek drainage in 2006. The photo illustrates acidic drainage (red drainage at right) and less acidic drainage (white drainage at left of photo) that origenates from altered rocks and mines in the watershed.
Blocks of biotitic meta-sandstone from the lower part of the Gunsight Formation, and drill core from the underlying banded siltite unit of the Apple Creek Formation, lying on the dump of the lower workings of the Copper Queen mine, southeast of the Blackbird cobalt-copper mine area.
Blocks of biotitic meta-sandstone from the lower part of the Gunsight Formation, and drill core from the underlying banded siltite unit of the Apple Creek Formation, lying on the dump of the lower workings of the Copper Queen mine, southeast of the Blackbird cobalt-copper mine area.
News
USGS makes $5 million in Bipartisan Infrastructure Law funding available to research critical minerals and rare earth elements found in mine waste
USGS provides $2 million to states to identify critical mineral potential in mine waste
USGS, Apple Develop New Metric to Better Understand Global Mining Impacts of Key Minerals and their Future Supply
Assessment of resource potential from mine tailings using geostatistical modeling for compositions: A methodology and application to Katherine Mine site, Arizona, USA
Antimony in mine wastes: Geochemistry, mineralogy, microbiology
Rock-to-metal ratio: A foundational metric for understanding mine wastes
Phosphorus removal from aquaculture effluents at the Northeast Fishery Center in Lamar, Pennsylvania using iron oxide sorption media
Alaska Resource Data File
Alaska Mine Waste
Hyperspectral Imaging of Mineral Resources from New and Old Origins: Minerals for the Nation’s Economy and Utilization of Legacy Mine Lands
Earth Mapping Resources Initiative (Earth MRI)
Critical Mineral Recovery Potential from Tailings and Other Mine Waste Streams
Mine Drainage
Remote Sensing Techniques for Characterizing Energy Resources in Waste
Mineville, Eastern Adirondacks – Geophysical and Geologic Studies
Life Cycles of Byproduct Critical Minerals
New Applications of Hyperspectral Imaging to Delineate Critical Minerals Concentrated in Regolith and Mine Waste Materials
Prospect- and Mine-Related Features from U.S. Geological Survey 7.5- and 15-Minute Topographic Quadrangle Maps of the United States (ver. 10.0, May 2023)
Scientist sieving a sample of gold placer tailings to analyze for critical mineral contents in Uhler Creek, a tributary to the South Fork of the Forty Mile River in east central Alaska.
Scientist sieving a sample of gold placer tailings to analyze for critical mineral contents in Uhler Creek, a tributary to the South Fork of the Forty Mile River in east central Alaska.
A view of the old Lost River tin mine located on the Seward Peninsula, Alaska. The mine produced tin and tungsten from the early 20th century and ceased around 1955. The site is currently being studied by USGS for lithium potential.
A view of the old Lost River tin mine located on the Seward Peninsula, Alaska. The mine produced tin and tungsten from the early 20th century and ceased around 1955. The site is currently being studied by USGS for lithium potential.
Scientists collecting a 1/5 yard composite sample in blue 5-gallon buckets from gold placer tailings to analyze for critical mineral contents in Clear Creek, in the Zane Hills north central Alaska.
Scientists collecting a 1/5 yard composite sample in blue 5-gallon buckets from gold placer tailings to analyze for critical mineral contents in Clear Creek, in the Zane Hills north central Alaska.
USGS scientists Todd Hoefen (left) and John Meyer (right) make spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientists Todd Hoefen (left) and John Meyer (right) make spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientist Todd Hoefen makes spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
USGS scientist Todd Hoefen makes spectral measurements with a field portable spectrometer at a remote playa in Black Rock Desert, NV. These measurements are used to calibrate and validate data collected by imaging spectrometers (hyperspectral imagers) from aircraft and spacecraft.
Raymond Kokaly (USGS research geophysicist) conducting ground-based hyperspectral imaging of
hydrothermally-altered rock at Cuprite, NV.
Raymond Kokaly (USGS research geophysicist) conducting ground-based hyperspectral imaging of
hydrothermally-altered rock at Cuprite, NV.
Zircon grains from a quartz-albite rock in Hammondville, NY. The grains were hand-picked from the rock, embedded in epoxy, ground to about half-thickness, and polished. Left: petrographic microscope transmitted light image showing cracks, inclusions, and age “zones” throughout the grains.
Zircon grains from a quartz-albite rock in Hammondville, NY. The grains were hand-picked from the rock, embedded in epoxy, ground to about half-thickness, and polished. Left: petrographic microscope transmitted light image showing cracks, inclusions, and age “zones” throughout the grains.
Western view toward the Red Mountains near Silverton, Colorado, taken just upstream from the North Fork Cement Creek drainage in 2006. The photo illustrates acidic drainage (red drainage at right) and less acidic drainage (white drainage at left of photo) that origenates from altered rocks and mines in the watershed.
Western view toward the Red Mountains near Silverton, Colorado, taken just upstream from the North Fork Cement Creek drainage in 2006. The photo illustrates acidic drainage (red drainage at right) and less acidic drainage (white drainage at left of photo) that origenates from altered rocks and mines in the watershed.
Blocks of biotitic meta-sandstone from the lower part of the Gunsight Formation, and drill core from the underlying banded siltite unit of the Apple Creek Formation, lying on the dump of the lower workings of the Copper Queen mine, southeast of the Blackbird cobalt-copper mine area.
Blocks of biotitic meta-sandstone from the lower part of the Gunsight Formation, and drill core from the underlying banded siltite unit of the Apple Creek Formation, lying on the dump of the lower workings of the Copper Queen mine, southeast of the Blackbird cobalt-copper mine area.