This data release provides descriptions of more than 60 mineral regions, mines, and mineral deposits within the United States and its territories that are reported to contain enrichments of cobalt (Co). To focus the scope of this data release, we report only mined deposits and exploration prospects with past production, or resource and reserve estimates of 1,000 metric tons or more of cobalt. Cobalt has diverse uses because of its properties, which include ferromagnetism, hardness, wear-resistance, low conductivity, and high melting point. The primary uses for cobalt are in rechargeable battery electrodes, and in superalloys used to make gas turbine engines. In 2017, the United States had a net import reliance as a percentage of apparent consumption of 72 percent for cobalt, and cobalt is considered a critical mineral. Cobalt mineralogy is diverse; it occurs in a variety of sulfide, arsenide, sulfarsenide, and oxyhydroxide minerals. In the United States, cobalt could be derived as a byproduct from mineral deposits that primarily produce other metals, including nickel, copper, zinc, and lead. The inclusion of a particular mineral deposit or prospect in this database is not meant to imply that it has economic potential. Rather, these entries were included to capture the characteristics of the deposits and prospects in the United States and its territories that have the largest cobalt resources. These deposits and prospects occur in Alaska, California, Idaho, Maine, Michigan, Minnesota, Missouri, Montana, North Carolina, New Mexico, Oregon, Pennsylvania, Puerto Rico and Tennessee. Several deposits and prospects were not included in this database, because they contain less than 1,000 metric tons of cobalt. A prime example is the Bunkerville project in Nevada (Ludington and others, 2006). The Stillwater deposit in Montana produced cobalt, but this was a byproduct, and to our knowledge, there are no published records of the amount of cobalt produced, or the amount of cobalt contained within the deposit. Analyses of rock chips from 47 outcrops of the Katahdin deposit in Maine indicates that the deposit locally contains approximately 0.1 percent cobalt (Miller, 1945), but a thorough analysis of the deposit is lacking. Mine La Motte in Missouri and the Stone Corral project in California were not included because of a lack of ore reserve information in publicly available references. However, we are aware that cobalt is present in the area and we welcome further information on these sites. The entries and descriptions in the database were derived from published papers, reports, data, and internet documents, published from 1908 to 2018, representing a variety of sources, including geologic and exploration studies described in State, Federal, and industry reports. Although an attempt was made to capture as many examples as possible, this dataset is a progress report that is part of an ongoing effort. The authors welcome additional published information in order to continually update and refine this dataset.

Sediment hosted gold deposits in Nevada were first mined in the 1960s from open pit mines with large tonnage and low grade resources. Since that time, continuing exploration and discovery have identified extraordinary resources, and together these deposits now form the second-largest gold endowment on Earth, surpassed only by the Witwatersrand Gold Fields of South Africa. The data herein are part of a larger U.S. Geological Survey (USGS) project to develop an updated geospatial database of mines, mineral deposits and mineral regions in the United States. The point and polygon layers within this database represent locations of mines, mineral occurrences (which includes deposits and prospects), and mining districts in an approximately 200-square mile area northwest of Carlin, Nevada. Tables contain additional information such as commodity, geology, deposit types, activity status, deposit resources, and mine production. The extent of surface workings, when visible on imagery, is also captured and shows the relative size of mining operations. All data were compiled from publicly available sources published from 1910 - 2017. Where possible, data were compiled from primary source reports rather than from syntheses of past reports. Although the selected area does not include the entire Carlin Trend, the area, which covers nine 7.5-minute quadrangles, does contain a wide range of deposit types described through a variety of public data and information. These data are being compiled by the USGS Mineral Deposit Database project with support from the Bureau of Land Management.

Sediment hosted gold deposits in Nevada were first mined in the 1960s from open pit mines with large tonnage and low grade resources. Since that time, continuing exploration and discovery have identified extraordinary resources, and together these deposits now form the second-largest gold endowment on Earth, surpassed only by the Witwatersrand Gold Fields of South Africa. The data herein are part of a larger U.S. Geological Survey (USGS) project to develop an updated geospatial database of mines, mineral deposits and mineral regions in the United States. The point and polygon layers within this database represent locations of mines, mineral occurrences (which includes deposits and prospects), and mining districts in an approximately 200-square mile area northwest of Carlin, Nevada. Tables contain additional information such as commodity, geology, deposit types, activity status, deposit resources, and mine production. The extent of surface workings, when visible on imagery, is also captured and shows the relative size of mining operations. All data were compiled from publicly available sources published from 1910 - 2017. Where possible, data were compiled from primary source reports rather than from syntheses of past reports. Although the selected area does not include the entire Carlin Trend, the area, which covers nine 7.5-minute quadrangles, does contain a wide range of deposit types described through a variety of public data and information. These data are being compiled by the USGS Mineral Deposit Database project with support from the Bureau of Land Management.

DGGS Digital Data Series 18, Alaska Minerals Database, is a working, internal database that supports multiple data products developed by the Alaska Division of Geological & Geophysical Surveys (DGGS), including the Alaska Mineral Industry Report series (https://dggs.alaska.gov/pubs/minerals) and a web service of significant mineral industry occurrences and industry activity in 2020. DGGS anticipates developing additional products from the database in the future. This abstract and data dictionary will be updated as more of the database becomes publicly available over time. The full, unpublished database contains information about significant mineral occurrences in Alaska, including industry activity by year, mineral resource estimates, mine production statistics by year, and an interpreted mineral system type using the classification scheme of Hofstra and Kreiner (2020). The database also associates records in Alaska Resource Data File (ARDF; U.S. Geological Survey, 1996) with significant mineral occurrences, as interpreted by DGGS. DGGS annually compiles mineral industry information from past-year statements issued by companies, including press releases and corporate annual and financial reports, as well as phone interviews, replies to questionnaires, and news media articles. Only publicly available data compiled by DGGS are visible; confidential data are incorporated into statewide figures. The database is actively updated as new mineral activity data become available each year. Property information and previous years' data will be updated to resolve errors, reflect new geologic interpretations, and display newly available data. Consequently, products developed from the database may change over time as information and figures are updated. DGGS encourages members of the public to contact DGGS' Mineral Resources Section staff to discuss potential changes to the data or errors to be resolved in our derivative products. The data are available from the DGGS website: http://doi.org/10.14509/30873.

This data release provides descriptions of more than 120 mineral regions, mines, and mineral deposits within the United States that are reported to contain enrichments of tin (Sn). This data release only includes sites with publicly available records of past production of tin, or a defined resource of tin, or both. The inclusion of a particular mineral deposit in this database is not meant to imply that it has economic potential; it may be produced only as a byproduct at some sites. Rather, these deposits were included to capture the distribution of characteristics of the known, reported tin deposits in the United States. This logic also applies to the other commodities listed with tin in some occurrences. The primary uses for tin within the United States are for alloys, chemicals, and solder, amongst others. Tin has not been produced in the United States since 1993, and with the United States not having any active tin reserves the commodity has been deemed a critical strategic metal (Kamilli and others, 2017). As of 2017, the United States maintains a net import reliance as a percentage of apparent consumption of approximately 75 percent for tin, where 25 percent of the apparent consumption is attributed to the recycling of tin (U.S. Geological Survey, 2018). In the United States, tin most commonly occurs in the mineral cassiterite. The majority of tin occurrences are located in the state of Alaska, but tin is known to occur in many other locations in the contiguous United States. The cassiterite ore originates from various lode deposit types, including greisens, pegmatites, skarns, and veins, as well as from placers sourced from these systems. The entries and descriptions in the database were derived from published papers, reports, data, and internet documents representing a variety of sources, including geologic and exploration studies described in State, Federal, and industry reports. Although an attempt was made to capture as many examples as possible, this dataset is a progress report that is part of an ongoing effort. The authors welcome additional published information in order to continually update and refine this dataset.

This data release provides descriptions of more than 120 mineral regions, mines, and mineral deposits within the United States that are reported to contain enrichments of tin (Sn). This data release only includes sites with publicly available records of past production of tin, or a defined resource of tin, or both. The inclusion of a particular mineral deposit in this database is not meant to imply that it has economic potential; it may be produced only as a byproduct at some sites. Rather, these deposits were included to capture the distribution of characteristics of the known, reported tin deposits in the United States. This logic also applies to the other commodities listed with tin in some occurrences. The primary uses for tin within the United States are for alloys, chemicals, and solder, amongst others. Tin has not been produced in the United States since 1993, and with the United States not having any active tin reserves the commodity has been deemed a critical strategic metal (Kamilli and others, 2017). As of 2017, the United States maintains a net import reliance as a percentage of apparent consumption of approximately 75 percent for tin, where 25 percent of the apparent consumption is attributed to the recycling of tin (U.S. Geological Survey, 2018). In the United States, tin most commonly occurs in the mineral cassiterite. The majority of tin occurrences are located in the state of Alaska, but tin is known to occur in many other locations in the contiguous United States. The cassiterite ore originates from various lode deposit types, including greisens, pegmatites, skarns, and veins, as well as from placers sourced from these systems. The entries and descriptions in the database were derived from published papers, reports, data, and internet documents representing a variety of sources, including geologic and exploration studies described in State, Federal, and industry reports. Although an attempt was made to capture as many examples as possible, this dataset is a progress report that is part of an ongoing effort. The authors welcome additional published information in order to continually update and refine this dataset.

This data release provides data for the single site in the United States (U.S.) that has public record of germanium (Ge) production. Germanium, which is currently classified as a critical mineral in the U.S., is also extracted as a byproduct from deposits in Alaska, Washington, and Tennessee. However, there is no public information that documents germanium production from these deposits. Current annual production of refined germanium is led by China at 85,000 tons, while estimates place U.S. reserves near 2,500 tons. Reported production of germanium in the U.S. is limited to one site, the Apex mine in Washington County, Utah. The Apex mine produced gallium (Ga) and germanium as primary products during the mid-1980s. Since its closure, germanium recovery has been restricted to refining processes of ore concentrates and recycling of waste scrap both in and outside the U.S. (U.S. Geological Survey, 2020). As a part of the process set forth by Executive Order 13817, the USGS National Minerals Information Center (NMIC) identified germanium as a critical mineral (Department of the Interior, 2018) due to the import reliance and importance in the sectors of defense, manufacturing, and telecommunications (Fortier and others, 2018). Germanium is used for strategic, consumer, and commercial applications due to its high refractive index, transparency to infrared light, and properties as a semiconductor. Most notably, germanium is a major component in infrared devices, fiber optic cables, and PET plastics (Melcher and Buchholz, 2014). As of 2019, the U.S. maintains greater than 50% reliance on imported germanium from countries such as Belgium and China who were the main U.S. suppliers between 2015–2018. Germanium is imported to the U.S. as germanium metal and dioxide for consumption (U.S. Geological Survey, 2020). Some germanium is recovered from recycling of scrap during the manufacturing process, such as the manufacture of fiber-optic cables (Mercer, 2015). The element germanium largely occurs as a geochemical substitute in various sulfide minerals, primarily in the mineral sphalerite (ZnS), with minor inclusion in silicate minerals. The greatest germanium concentrations occur in Kipushi-type deposits, principally in oxidation zones of sulfide ore (Höll and others, 2007). The largest past producers of germanium from Kipushi-type deposits occurred in Kipushi, Democratic Republic of the Congo, and Tsumeb, Namibia. These deposits host 60 million tonnes (t) at 100–200 parts per million (ppm) Ge and 28 million t at 50–150 ppm Ge, respectively. Currently, germanium is produced as a byproduct of zinc-bearing ore deposits. Acid mine drainage may have elevated signatures of germanium because of germanium’s strong association to sulfide minerals (Shanks and others, 2017). Germanium is also recovered from lignite and coal deposits worldwide (Melcher and Buchholz, 2014). The entries and descriptions in the database were derived from published papers, reports, data, and internet documents representing a variety of sources, including geologic and exploration studies described in State, Federal, and industry reports. Production and resource information extracted from older sources might not be compliant with current rules and guidelines in minerals industry standards such as National Instrument 43-101 (NI 43-101). The presence of a germanium mineral deposit in this database is not meant to imply that the deposit is currently economic. Inclusion of material in the database is for descriptive purposes only and does not imply endorsement by the U.S. Government. The authors welcome additional published information in order to continually update and refine this dataset. Department of the Interior, 2018, Final list of critical minerals 2018: Federal Register Notice 83 FR 23295, no. 97, p. 23295–23296, https://www.federalregister.gov/d/2018-10667. Fortier, S.M., Nassar, N.T., Lederer, G.W., Brainard, J., Gambogi, J., and McCullough, E.A., 2018, Draft critical

This data release provides data for the single site in the United States (U.S.) that has public record of germanium (Ge) production. Germanium, which is currently classified as a critical mineral in the U.S., is also extracted as a byproduct from deposits in Alaska, Washington, and Tennessee. However, there is no public information that documents germanium production from these deposits. Current annual production of refined germanium is led by China at 85,000 tons, while estimates place U.S. reserves near 2,500 tons. Reported production of germanium in the U.S. is limited to one site, the Apex mine in Washington County, Utah. The Apex mine produced gallium (Ga) and germanium as primary products during the mid-1980s. Since its closure, germanium recovery has been restricted to refining processes of ore concentrates and recycling of waste scrap both in and outside the U.S. (U.S. Geological Survey, 2020). As a part of the process set forth by Executive Order 13817, the USGS National Minerals Information Center (NMIC) identified germanium as a critical mineral (Department of the Interior, 2018) due to the import reliance and importance in the sectors of defense, manufacturing, and telecommunications (Fortier and others, 2018). Germanium is used for strategic, consumer, and commercial applications due to its high refractive index, transparency to infrared light, and properties as a semiconductor. Most notably, germanium is a major component in infrared devices, fiber optic cables, and PET plastics (Melcher and Buchholz, 2014). As of 2019, the U.S. maintains greater than 50% reliance on imported germanium from countries such as Belgium and China who were the main U.S. suppliers between 2015–2018. Germanium is imported to the U.S. as germanium metal and dioxide for consumption (U.S. Geological Survey, 2020). Some germanium is recovered from recycling of scrap during the manufacturing process, such as the manufacture of fiber-optic cables (Mercer, 2015). The element germanium largely occurs as a geochemical substitute in various sulfide minerals, primarily in the mineral sphalerite (ZnS), with minor inclusion in silicate minerals. The greatest germanium concentrations occur in Kipushi-type deposits, principally in oxidation zones of sulfide ore (Höll and others, 2007). The largest past producers of germanium from Kipushi-type deposits occurred in Kipushi, Democratic Republic of the Congo, and Tsumeb, Namibia. These deposits host 60 million tonnes (t) at 100–200 parts per million (ppm) Ge and 28 million t at 50–150 ppm Ge, respectively. Currently, germanium is produced as a byproduct of zinc-bearing ore deposits. Acid mine drainage may have elevated signatures of germanium because of germanium’s strong association to sulfide minerals (Shanks and others, 2017). Germanium is also recovered from lignite and coal deposits worldwide (Melcher and Buchholz, 2014). The entries and descriptions in the database were derived from published papers, reports, data, and internet documents representing a variety of sources, including geologic and exploration studies described in State, Federal, and industry reports. Production and resource information extracted from older sources might not be compliant with current rules and guidelines in minerals industry standards such as National Instrument 43-101 (NI 43-101). The presence of a germanium mineral deposit in this database is not meant to imply that the deposit is currently economic. Inclusion of material in the database is for descriptive purposes only and does not imply endorsement by the U.S. Government. The authors welcome additional published information in order to continually update and refine this dataset. Department of the Interior, 2018, Final list of critical minerals 2018: Federal Register Notice 83 FR 23295, no. 97, p. 23295–23296, https://www.federalregister.gov/d/2018-10667. Fortier, S.M., Nassar, N.T., Lederer, G.W., Brainard, J., Gambogi, J., and McCullough, E.A., 2018, Draft critical

The Alaska Resource Data File (ARDF) is a database of mines, prospects, and mineral occurrences in Alaska. It contains information compiled from published and unpublished sources from industry, U.S. Bureau of Mines (BOM), U.S. Geological Survey (USGS), and other government and private sources. ARDF is not a mining claims database.

The Alaska Resource Data File (ARDF) is a database of mines, prospects, and mineral occurrences in Alaska. It contains information compiled from published and unpublished sources from industry, U.S. Bureau of Mines (BOM), U.S. Geological Survey (USGS), and other government and private sources. ARDF is not a mining claims database.