GIS, supplemental data table, and references for focus areas of potential domestic resources of critical minerals and related commodities in the United States and Puerto Rico

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Metadata:

Identification_Information:
Citation:
Citation_Information:
Originator: Connie L. Dicken
Originator: Laurel G. Woodruff
Originator: Jane M. Hammarstrom
Originator: Kelsey E. Crocker
Publication_Date: 20221101
Title:
GIS, supplemental data table, and references for focus areas of potential domestic resources of critical minerals and related commodities in the United States and Puerto Rico
Geospatial_Data_Presentation_Form: Vector Digital Data Set (Polygon)
Publication_Information:
Publication_Place: Denver, CO
Publisher: U.S. Geological Survey
Other_Citation_Details:
Additional information about Originators: Connie L. Dicken, https://orcid.org/0000-0002-1617-8132. Jane M. Hammarstrom, http://orcid.org/0000-0003-2742-3460 Laurel G. Woodruff, http://orcid.org/0000-0002-2514-9923 Kelsey E. Crocker, http://orcid.org/0000-0002-5919-5274
Online_Linkage: https://doi.org/10.5066/P9DIZ9N8
Larger_Work_Citation:
Citation_Information:
Originator: Jane M. Hammarstrom
Originator: Connie L. Dicken
Originator: Laurel G. Woodruff
Originator: Allen K. Andersen
Originator: Sean Brennan
Originator: Warren C. Day
Originator: Benjamin J. Drenth
Originator: Nora K. Foley
Originator: Susan Hall
Originator: Albert H. Hofstra
Originator: Anne E. McCafferty
Originator: Anjana K. Shah
Originator: David A. Ponce
Publication_Date: 2022
Title:
Focus areas for data acquisition for potential domestic resources of 13 critical minerals in the conterminous United States and Puerto Rico — Antimony, barite, beryllium, chromium, fluorspar, hafnium, helium, magnesium, manganese, potash, uranium, vanadium, and zirconium
Geospatial_Data_Presentation_Form: publication
Publication_Information:
Publication_Place: Reston, VA
Publisher: US Geological Survey
Online_Linkage: https://doi.org/10.3133/ofr20191023D
Description:
Abstract:
In response to Executive Order 13817 of December 20, 2017, the U.S. Geological Survey (USGS) coordinated with the Bureau of Land Management (BLM) to identify 36 nonfuel minerals or mineral materials considered critical to the economic and national security of the United States (U.S.) (https://pubs.usgs.gov/of/2018/1021/ofr20181021.pdf). Acquiring information on possible domestic sources of these critical minerals is the rationale for the USGS Earth Mapping Resources Initiative (Earth MRI). The program, which partners the USGS with State Geological Surveys, Federal agencies, and the private sector, aims to collect new geological, geophysical, and topographic (lidar) data in key areas of the U.S. to stimulate mineral exploration and production of critical minerals.

The USGS has identified broad areas within the United States to target acquisition of geologic mapping, geophysical data, and (or) detailed topographic information to aid research, mineral exploration, and evaluation of mineral potential in these areas. Focus areas were defined using existing geologic data including data on known deposits in the United States. The focus areas are provided as geospatial data supported by tables that summarize what is known about the mineral potential and brief descriptions of data gaps that could be addressed by the Earth MRI program. A full discussion of Earth MRI and the rationale and methods used to develop the geospatial data are provided in the following report:

Hammarstrom, J.M., Dicken, C.L., Woodruff, L.G., Andersen, A.K., Brennan, S., Day, W.C., Drenth, B.J., Foley, N.K., Hall, S., Hofstra, A.H., McCafferty, A.E., Shah, A.K., and Ponce, D.A., 2022, Focus areas for data acquisition for potential domestic resources of 13 critical minerals in the conterminous United States and Puerto Rico—Antimony, barite, beryllium, chromium, fluorspar, hafnium, helium, magnesium, manganese, potash, uranium, vanadium, and zirconium, chap. D of U.S. Geological Survey, Focus areas for data acquisition for potential domestic sources of critical minerals: U.S. Geological Survey Open-File Report 2019–1023, 65 p., https://doi.org/10.3133/ofr20191023D.
Purpose:
These geospatial data provide the locations of focus areas to be used for the planning and collection of geophysical, geological, and topographic (lidar) data pertaining to the Earth MRI study of critical mineral resources in the U.S. Focus areas are outlined solely on the basis of geology, regardless of political boundaries. Therefore, areas may include Federal, as well as State, tribal, and private lands, which may or may not be open to exploration and mining activities. These data are shared to meet open data requirements and are suitable for use in Geographic Information Systems (GIS) or other database and geospatial software used to derive maps and perform geospatial analyses.
Supplemental_Information:
The GIS data consist of a polygon layer, or “feature class”, which depicts the locations of focus areas, that might control the distribution of mineral deposits. Individual focus areas may be represented by one or more polygons. When a focus area is defined by more than one polygon, the polygons are grouped to form a “multi-part” feature in the GIS data. For example, the focus area pertaining to the Phosphoria Formation across multiple States consists of 984 polygons. These polygons are grouped and appear as a single record in the GIS attribute table with the UID “RM338”. In all, there are over 59,000 polygons that make up 833 focus areas. Polygons representing different focus areas may overlap. Viewing focus areas as outlines without color fills and with text labels will show where polygons overlap.

Data are provided in ArcGIS 10.8.1 file geodatabase (.gdb) and shapefile formats. The user is also provided a State boundary layer feature class published by Esri (2012) that was modified to include attribute information identifying the four regions used in the study – east, central, west, and Alaska. focusAreas_emri.gdb file geodatabase includes the following:

focusAreas_emri: potential data acquisition areas represented as polygons. states_studyRegions: State boundaries that include study area regions.

Table data are provided as a single excel work sheet with tabs, listed below (as well as comma separated values (.csv) files.) Abbreviations - list of abbreviations used in the data set. Explanations - describes each attribute in the EMRI focus area tab as well as related GIS field name. For example, 'Critical mineral commodities' is the column name in the table and it is called 'CritMin' in the focusAreas_emri GIS table. Additional explanations are below for descriptions of fields in the References tab. EMRI focus areas - full table of attributes for the focus areas. References - table that lists the short reference, full citation, and links where available. * status defined in Explanations tab. Mineral Systems - table 1 modified from Hofstra and Kreiner (2020) that relates critical minerals and commodities to deposit types and mineral systems.

Esri, 2012, USA States: Esri Data & Maps for ArcGIS, 2012 – World, Europe, and United States, Redlands, CA.

These data are published as a Science Base Data Release, however the Hammarstrom and others (2022) Open-File Report 2019–1023 contains the discussion of Earth MRI and the rationale and methods used to develop these geospatial data (https://doi.org/10.3133/ofr20191023D).
Time_Period_of_Content:
Time_Period_Information:
Single_Date/Time:
Calendar_Date: 2022
Currentness_Reference: publication date
Status:
Progress: Complete
Maintenance_and_Update_Frequency: As needed
Spatial_Domain:
Bounding_Coordinates:
West_Bounding_Coordinate: -173.0000
East_Bounding_Coordinate: -66.0000
North_Bounding_Coordinate: 72.0000
South_Bounding_Coordinate: 18.0000
Keywords:
Theme:
Theme_Keyword_Thesaurus: ISO 19115 Topic Category
Theme_Keyword: geoscientificInformation
Theme:
Theme_Keyword_Thesaurus: USGS Thesaurus
Theme_Keyword: mineral deposits
Theme_Keyword: economic geology
Theme_Keyword: geospatial datasets
Theme_Keyword: critical minerals
Theme_Keyword: aluminum
Theme_Keyword: antimony
Theme_Keyword: arsenic
Theme_Keyword: barite
Theme_Keyword: beryllium
Theme_Keyword: bismuth
Theme_Keyword: cesium
Theme_Keyword: chromium
Theme_Keyword: cobalt
Theme_Keyword: fluorspar
Theme_Keyword: gallium
Theme_Keyword: germanium
Theme_Keyword: graphite
Theme_Keyword: hafnium
Theme_Keyword: indium
Theme_Keyword: lithium
Theme_Keyword: magnesium
Theme_Keyword: manganese
Theme_Keyword: nickel
Theme_Keyword: niobium
Theme_Keyword: platinum group elements (PGE)
Theme_Keyword: potash
Theme_Keyword: rare earth elements (REE)
Theme_Keyword: rhenium
Theme_Keyword: rubidium
Theme_Keyword: scandium
Theme_Keyword: strontium
Theme_Keyword: tantalum
Theme_Keyword: tellurium
Theme_Keyword: tin
Theme_Keyword: titanium
Theme_Keyword: tungsten
Theme_Keyword: uranium
Theme_Keyword: vanadium
Theme_Keyword: zinc
Theme_Keyword: zirconium
Theme:
Theme_Keyword_Thesaurus: USGS Metadata Identifier
Theme_Keyword: USGS:610438e7d34ef8d7055fbcae
Place:
Place_Keyword_Thesaurus: Common geographic areas
Place_Keyword: United States
Place_Keyword: Alabama
Place_Keyword: Alaska
Place_Keyword: Arizona
Place_Keyword: Arkansas
Place_Keyword: California
Place_Keyword: Colorado
Place_Keyword: Connecticut
Place_Keyword: Delaware
Place_Keyword: District of Columbia
Place_Keyword: Florida
Place_Keyword: Georgia
Place_Keyword: Hawaii
Place_Keyword: Idaho
Place_Keyword: Illinois
Place_Keyword: Indiana
Place_Keyword: Iowa
Place_Keyword: Kansas
Place_Keyword: Kentucky
Place_Keyword: Louisiana
Place_Keyword: Maine
Place_Keyword: Maryland
Place_Keyword: Massachusetts
Place_Keyword: Michigan
Place_Keyword: Minnesota
Place_Keyword: Mississippi
Place_Keyword: Missouri
Place_Keyword: Montana
Place_Keyword: Nebraska
Place_Keyword: Nevada
Place_Keyword: New Hampshire
Place_Keyword: New Jersey
Place_Keyword: New Mexico
Place_Keyword: New York
Place_Keyword: North Carolina
Place_Keyword: North Dakota
Place_Keyword: Ohio
Place_Keyword: Oklahoma
Place_Keyword: Oregon
Place_Keyword: Pennsylvania
Place_Keyword: Puerto Rico
Place_Keyword: Rhode Island
Place_Keyword: South Carolina
Place_Keyword: South Dakota
Place_Keyword: Tennessee
Place_Keyword: Texas
Place_Keyword: Utah
Place_Keyword: Vermont
Place_Keyword: Virginia
Place_Keyword: Washington
Place_Keyword: West Virginia
Place_Keyword: Wisconsin
Place_Keyword: Wyoming
Access_Constraints: None. Please see 'Distribution Info' for details.
Use_Constraints:
There is no guarantee concerning the accuracy of the data. Data have been checked to ensure the accuracy. If any errors are detected, please notify the originating office. The U.S. Geological Survey recommends users read all metadata prior to using data. Acknowledgment of the U.S. Geological Survey would be appreciated in products derived from these data. User specifically agrees not to misrepresent the data, nor to imply that changes made were approved or endorsed by the U.S. Geological Survey.
Point_of_Contact:
Contact_Information:
Contact_Person_Primary:
Contact_Person: Connie Dicken
Contact_Organization: U.S. Geological Survey, NORTHEAST REGION
Contact_Position: Geologist
Contact_Address:
Address_Type: mailing address
Address: Mail Stop 954, 12201 Sunrise Valley Dr
City: Reston
State_or_Province: VA
Postal_Code: 20192
Country: US
Contact_Voice_Telephone: 703-648-6482
Contact_Facsimile_Telephone: 703-648-6252
Contact_Electronic_Mail_Address: cdicken@usgs.gov
Data_Set_Credit:
Development of the dataset was funded by the U.S. Geological Survey Mineral Resources Program. The spatial data set and supporting tables were developed by 4 regional teams: Geology, Energy & Minerals Science Center (Reston, VA); Geology, Geophysics, and Geochemistry Science Center (Denver, CO); Geology, Minerals, Energy, and Geophysics Science Center (Spokane, WA and Tucson, AZ); and Alaska Science Center - Geology Office (Anchorage, AK). Database reviews and contributions were made by USGS personnel Heather Parks, Ryan Taylor, Carlin Green, Dan Hayba, Damon Bickerstaff, and Patricia Loferski.

Alaska Division of Geological and Geophysical Surveys – Werdon, M.B. Arizona Geological Survey - Richardson, C.A. Arkansas Geological Survey - Cannon, C., Chandler, A., and Hanson, W.D. California Geological Survey - Bohlen, S., Callen, B., Gius, F.W., Goodwin, J., Higgins, C., Key, E.L., Marquis, G., Mills, S., Tuzzolino, A., and Wesoloski, C. Colorado Geological Survey - Morgan, M.L., and O'Keeffe, M.K. Connecticut Geological Survey - Thomas, M. Delaware Geological Survey - KunleDare, M., and Tomlinson, J. Florida Geological Survey - Means, H. Geological Survey of Alabama - VanDervoort, D.S., and Whitmore, J.P. Idaho Geological Survey - Berti, C., Gillerman, V.S., and Lewis, R.S. Illinois State Geological Survey - Denny, F.B., Freiburg, J., Scott, E., and Whittaker, S. Indiana Geological and Water Survey - Mastalerz, M., McLaughlin, P.I., and Motz, G. Iowa Geological Survey - Clark, R.J., Kerr, P., and Tassier-Surine, S. Kansas Geological Survey - Husiuk, F., Oborny, S., and Smith, J. Kentucky Geological Survey - Andrews, W.M., Harris, D., Hickman J., and Lukoczki, G. Maine Geological Survey - Beck, F.M., Bradley, D., Marvinney, R., Slack, J., and Whittaker, A.H. Maine Mineral and Gem Museum - Felch, M. Maryland Geological Survey - Kavage Adams, R.H., Brezinski, D.K., Junkin, W., and Ortt, R. Michigan Geological Survey - Yellich, J. Minnesota Department of Natural Resources - Arends, H., Dahl, D.A., and Saari, S. Minnesota Natural Resources Research Institute - Hudak, G.J. Minnesota Geological Survey - Block, A. Missouri Geological Survey - Ellis, T., Lori, L., Pierce, L., Seeger, C.M., and Steele, A. Montana Bureau of Mines and Geology - Gunderson, J., Korzeb, S.L., and Scarberry, K.C. Nevada Bureau of Mines and Geology - Faulds, J., and Muntean, J.L. New Mexico Bureau of Geology and Mineral Resources - Gysi, A., Kelley, S.A., and McLemore, V.T. North Carolina Geological Survey - Chapman, J.S., Farrell, K.M., Taylor, K.B., Thornton, E., and Veach, D. North Dakota Geological Survey - Kruger, N. Ohio Geological Survey - McDonald, J., and Stucker, J. Pennsylvania Geological Survey - Hand, K., and Shank, S.G. South Carolina Geological Survey - Howard, C.S., and Morrow, R.H. South Dakota Geological Survey - Cowman, T., Luczak, J.N., and Myman, T.J. Tennessee Geological Survey - Lemiszki, P. Texas Bureau of Economic Geology - Paine, J. Utah Geological Survey - Boden, T., Mills, S.E., and Rupke, A. Virginia Division of Geology and Mineral Resources - Coiner, L.V., and Lassetter, W.L. Washington Geological Survey - Eungard, D.W., and Skov, R. West Virginia Geological and Economic Survey - Brown, S.R., Dinterman, P., and Moore, J.P. Western Michigan University - Thakurta, J., Harrison, W., and Voice, P. Wisconsin Geological and Natural History Survey - Ames, C., Gotschalk, B., Lodge, R., Stewart, E.K., and Stewart, E. Wyoming State Geological Survey - Gregory, R.W., Lynds, R.M., Mosser, K., Toner, R., and Webber, P.

U.S. Geological Survey - Anderson, A.K., Bickerstaff, D., Bern, C.R., Brady, S., Brezinski, C., Brock, J., Bultman, M.W., Carter, M.W., Cossette, P.M., Crafford, T., Crocker, K.E., Day, W.C., Dicken, C.L., Drenth, B.J., Emsbo, P., Foley, N.K., Frost, T.P., Gettings, M.E., Grauch, V.J.S., Hall, S.M., Hammarstrom, J.M., Hayes, T.S., Hofstra, A.H., Horton, J.D., Horton, J.W., Hubbard, B.E., Hudson, M., John, D.A., Johnson, M.R., Jones, J.V. III, Kreiner, D.C., Mauk, J.L., McCafferty, A.E., McPhee, D., Merchat, A.J., Nicholson, S.W., Ponce, D.A., Roberts-Ashby, T., Rosera, J., San Juan, C.A., Shah, A.K., Scheirer, D., Siler, D.L., Soller, D.R., Stillings, L.L., Swezey, C.S., Taylor, R.D., Thompson, R., Van Gosen, B.S., Verplanck, P., Vikre, P.G., Walsh, G.J., Woodruff, L.G., and Zurcher, L.
Native_Data_Set_Environment:
Microsoft Windows 10 Version 1909; Esri ArcGIS 10.8.1 Version 10.8.1.14362
Data_Quality_Information:
Attribute_Accuracy:
Attribute_Accuracy_Report:
The data are intended to be used at regional scales for planning purposes. Unique values in attribute fields were acquired through frequency analyses. The unique values in each attribute field were reviewed and checked for spelling, consistency of terms, accuracy, adherence to established vocabularies, and completeness.
Logical_Consistency_Report:
A single focus area may be represented by numerous, dispersed polygons. Where this occurs, the polygons are grouped to form a “multi-part” feature which has a single record in the GIS attribute table. There are over 59,000 polygons that make up 833 multi-part focus areas. Consequently, polygons representing different focus areas may overlap.
Completeness_Report:
Focus areas are based on existing data and reports published 1889–2022. Focus areas are based solely on geologic information and rationale. Focus areas intentionally include areas of incomplete information that could be better understood by the collection of new or additional data.
Positional_Accuracy:
Horizontal_Positional_Accuracy:
Horizontal_Positional_Accuracy_Report:
The quality of focus areas is highly variable and generally reflects the accuracy of source reports and data. The data are intended to show the general distribution of known mineral deposits and regions as well as areas that potentially contain resources for critical minerals. The data can be queried to identify commodities. The data are intended to be used at regional scales for planning purposes.
Lineage:
Source_Information:
Source_Citation:
Citation_Information:
Originator: Albert H. Hofstra
Originator: Douglas C. Kreiner
Publication_Date: 20200525
Title:
Systems-Deposits-Commodities-Critical Minerals Table for Earth Mapping Resources Initiative (ver. 1.1, May 2021)
Edition: 1.1
Geospatial_Data_Presentation_Form: publication
Series_Information:
Series_Name: Open-File Report
Issue_Identification: 2020-1042
Online_Linkage: https://doi.org/10.3133/ofr20201042
Type_of_Source_Media: Digital and/or Hardcopy
Source_Time_Period_of_Content:
Time_Period_Information:
Single_Date/Time:
Calendar_Date: 2021
Source_Currentness_Reference: publication date
Source_Citation_Abbreviation: Hofstra and Kreiner (2020)
Source_Contribution: Mineral systems, deposit types and commodities for Earth MRI.
Source_Information:
Source_Citation:
Citation_Information:
Originator: Esri
Publication_Date: 2012
Title: USA States: Esri Data & Maps for ArcGIS
Geospatial_Data_Presentation_Form: vector digital data
Online_Linkage:
Source_Scale_Denominator: 3000000
Type_of_Source_Media: Digital and/or Hardcopy
Source_Time_Period_of_Content:
Time_Period_Information:
Single_Date/Time:
Calendar_Date: 2012
Source_Currentness_Reference: publication date
Source_Citation_Abbreviation: Esri (2012)
Source_Contribution:
Used for State boundaries and added USGS EMRI regions to the attributes for general use.
Process_Step:
Process_Description:
To define focus areas, project teams first evaluated existing data on critical mineral occurrences (deposits, prospects, and showings), past exploration, resources and production, geochemical and geophysical data, and the status of geologic mapping for the eastern, central, and western conterminous U.S. and Alaska. Resulting focus areas ranged from areas with identified resources and past production to areas with geologic characteristics permissive for undiscovered deposits with no known deposits. Specific data needs that could be addressed by the Earth MRI program to better evaluate each focus area for critical mineral potential were summarized.

The evaluation of existing data formed the rationale for developing polygon features in a GIS. The geospatial delineation of focus areas involved a variety of data sources and approaches. Focus areas for potential 36 critical minerals were developed by querying digital State geologic map data for permissive host rocks based on lithology and age. Other focus areas were derived using generalized outlines of mining districts or mineral belts, distributions of observed occurrences, and in some cases, geochemical and (or) geophysical anomalies associated with deposits.

Hofstra and Kreiner (2020) table 1 was used to define and categorize focus areas based on a hierarchical data structure of mineral systems and deposit types.
Source_Used_Citation_Abbreviation: Hofstra and Kreiner (2020)
Source_Used_Citation_Abbreviation: Esri (2012)
Process_Date: 20210330
Process_Contact:
Contact_Information:
Contact_Person_Primary:
Contact_Person: Connie Dicken
Contact_Organization: U.S. Geological Survey, NORTHEAST REGION
Contact_Position: Geologist
Contact_Address:
Address_Type: mailing address
Address: Mail Stop 954, 12201 Sunrise Valley Dr
City: Reston
State_or_Province: VA
Postal_Code: 20192
Country: US
Contact_Voice_Telephone: 703-648-6482
Contact_Facsimile_Telephone: 703-648-6252
Contact_Electronic_Mail_Address: cdicken@usgs.gov
Spatial_Data_Organization_Information:
Direct_Spatial_Reference_Method: Vector
Point_and_Vector_Object_Information:
SDTS_Terms_Description:
SDTS_Point_and_Vector_Object_Type: G-polygon
Point_and_Vector_Object_Count: 833
Spatial_Reference_Information:
Horizontal_Coordinate_System_Definition:
Planar:
Map_Projection:
Map_Projection_Name: Albers Conical Equal Area
Albers_Conical_Equal_Area:
Standard_Parallel: 29.5
Standard_Parallel: 45.5
Longitude_of_Central_Meridian: -96.0
Latitude_of_Projection_Origin: 37.5
False_Easting: 0.0
False_Northing: 0.0
Planar_Coordinate_Information:
Planar_Coordinate_Encoding_Method: coordinate pair
Coordinate_Representation:
Abscissa_Resolution: 0.6096
Ordinate_Resolution: 0.6096
Planar_Distance_Units: meters
Geodetic_Model:
Horizontal_Datum_Name: North_American_Datum_1983
Ellipsoid_Name: GRS_1980
Semi-major_Axis: 6378137.0
Denominator_of_Flattening_Ratio: 298.257222101
Entity_and_Attribute_Information:
Detailed_Description:
Entity_Type:
Entity_Type_Label: focusAreas_emri Attribute Table
Entity_Type_Definition:
Table containing attribute information associated with the data set.
Entity_Type_Definition_Source: Producer defined
Attribute:
Attribute_Label: UID
Attribute_Definition:
A unique identifier for each focus area based on subregion and a 4 digit number.
Attribute_Definition_Source: USGS authors
Attribute_Domain_Values:
Unrepresentable_Domain:
An alphanumeric identifier formatted as XX#### where XX represents the subregion and the #### is a number. The value of subregion can be Alaska (AK), Hawaii (HI), North Central (NC), Northeast (NE), Northwest (NW), Rocky Mountains (RM), South Central (SC), Southeast (SE), or Southwest (SW). Some focus areas may be two or more polygons grouped together, or a “multi-part”. A focus area may also be part of more than one subregion, but only one is listed.
Attribute:
Attribute_Label: AuthorID
Attribute_Definition:
An identifier created by the focus area primary author that captured subregion or State. Useful to retain link to original author's records.
Attribute_Definition_Source: USGS authors
Attribute_Domain_Values:
Unrepresentable_Domain: Author id to retain link with original records.
Attribute:
Attribute_Label: Region
Attribute_Definition: Study region within the United States.
Attribute_Definition_Source: USGS authors
Attribute_Domain_Values:
Unrepresentable_Domain:
Regions include Alaska, East, Central, and West. States (including District of Columbia and Puerto Rico) were grouped into regions for purposes of the study as follows: Alaska (AK); East (AL, CT, DC, DE, FL, GA, KY, MA, MD, ME, MS, NC, NH, NJ, NY, OH, PA, PR, RI, SC, TN, VA, VT, WV); Central (AR, IL, IN, IA, KS, LA, MI, MN, MO, NE, ND, OK, SD, WI); and West (AZ, CA, CO, HI, ID, MT, NM, NV, OR, TX, UT, WA, WY).
Attribute:
Attribute_Label: SubRegion
Attribute_Definition: 9 study subregions within the United States.
Attribute_Definition_Source: USGS authors
Attribute_Domain_Values:
Unrepresentable_Domain:
Alaska (AK), Hawaii (HI), Northwest (NW), Southwest (SW), Rocky Mountains (RM), North Central (NC), South Central (SC), Northeast (NE), and Southeast (SE). Note that Puerto Rico is included with the Southeast subregion.
Attribute:
Attribute_Label: States
Attribute_Definition: States included in the focus area listed in alphabetical order.
Attribute_Definition_Source: USGS authors
Attribute_Domain_Values:
Unrepresentable_Domain:
District of Columbia, Puerto Rico, Alabama, Alaska, Arizona, Arkansas, California, Colorado, Connecticut, Delaware, Florida, Georgia, Idaho, Illinois, Indiana, Iowa, Kansas, Kentucky, Louisiana, Maine, Maryland, Massachusetts, Michigan, Minnesota, Mississippi, Missouri, Montana, Nebraska, Nevada, New Hampshire, New Jersey, New Mexico, New York, North Carolina, North Dakota, Ohio, Oklahoma, Oregon, Pennsylvania, Rhode Island, South Carolina, South Dakota, Tennessee, Texas, Utah, Vermont, Virginia, Washington, West Virginia, Wisconsin, and Wyoming.
Attribute:
Attribute_Label: FocusArea
Attribute_Definition:
A descriptive name for the focus area. May be a geographic area, a mining district, a mineral belt, or an age/lithologic term.
Attribute_Definition_Source: USGS authors
Attribute_Domain_Values:
Unrepresentable_Domain: Informal names assigned by the USGS to distinguish focus areas.
Attribute:
Attribute_Label: MinSystem
Attribute_Definition: Type of mineral system.
Attribute_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Alkalic Porphyry
Enumerated_Domain_Value_Definition:
Alkalic porphyry systems form in oceanic and continental magmatic arcs and in continental rifts by similar processes from fluids exsolved from more fractionated alkalic plutons and stocks. Resulting ore deposits tend to be more enriched in Au, Te, Bi, and V.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Arsenide
Enumerated_Domain_Value_Definition:
Arsenide systems form in continental rifts where deep-seated, oxidized, metal-rich, metamorphic basement brines ascend to shallow levels. Native elements (Ag, Bi, As), Ni-, Co- and Fe-mono-, di- and sulf-arsenides precipitate by reduction as hydrocarbons, graphite, or sulfide minerals are oxidized to form carbonates and barite.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Basin Brine Path
Enumerated_Domain_Value_Definition:
Basin brine path systems emanate from marine evaporite basins and extend downward and laterally through permeable strata to discharge points in the ocean. Limestone is replaced by reflux dolomite at low temperatures and hydrothermal dolomite at high temperatures. Basin brines evolve to become ore fluids by scavenging metals from various rock types along gravity-driven flow paths. The mineralogy of the aquifers controls the redox and sulfidation state of the brine and the suite of elements that can be scavenged. Copper and Pb-Zn sulfide deposits form where oxidized brines encounter reduced S. Unconformity U deposits form where oxidized brines are reduced. Barium and Sr deposits form where reduced brines encounter marine sulfate or carbonate.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Carlin-type
Enumerated_Domain_Value_Definition:
Carlin-type systems occur in continental magmatic arcs, but are remote from subjacent stocks and plutons. Consequently, ore fluids consist largely of meteoric water containing volatiles discharged from deep intrusions. Ore fluids scavenge elements from carbonaceous pyritic sedimentary rocks as they convect through them. Gold ore containing disseminated pyrite forms where acidic reduced fluids dissolve carbonate and sulfidize Fe-bearing minerals in host rocks. Arsenic, Hg, and Tl minerals precipitate by cooling. Stibnite precipitates with quartz by cooling from Au-, As-, Hg-, Tl-depleted fluids.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Chemical weathering
Enumerated_Domain_Value_Definition:
Chemical weathering systems operate in stable areas of low to moderate relief with sufficient rainfall to chemically dissolve and concentrate elements present in various rock types and mineral occurrences by the downward percolation of surface water in the unsaturated zone. Chemical gradients cause different elements to be concentrated at different positions in the weathering profile and at the water table. Bauxite, Ni-laterite, and carbonatite laterite are restricted to tropical climatic zones; others form in temperate and arid climates. Dissolved U is reduced on carbonaceous material in lakes and swamps. Dissolved Mn precipitates at redox interface in lakes.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Climax-type
Enumerated_Domain_Value_Definition:
Climax-type systems occur in continental rifts with hydrous bimodal magmatism. Aqueous supercritical fluids exsolved from A-type topaz rhyolite plutons and the apices of subvolcanic stocks form a variety of deposit types as they move upward and outward, split into liquid and vapor, react with country rocks, and mix with ground water. The broad spectrum of deposit types results from the large thermal and chemical gradients in these systems. At deep levels, NYF pegmatites emanate from plutons.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Coeur d-Alene-type
Enumerated_Domain_Value_Definition:
Metamorphic dewatering of moderately oxidized siliciclastic sequences during exhumation with fluid flow along dilatant structures. Metasedimentary host rocks may contain basin brine path Pb-Zn and Cu ± Co deposits.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Hybrid magmatic REE / basin brine path
Enumerated_Domain_Value_Definition:
This hybrid system operates where CO2- and HF-bearing magmatic volatiles condense into basinal brines that replace carbonate with fluorspar ± barite, REE, Ti, Nb, and Be, as in the Illinois-Kentucky Fluorspar District and Hicks Dome.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: IOA-IOCG
Enumerated_Domain_Value_Definition:
IOA-IOCG systems form in both subduction- and rift-related magmatic provinces. IOA deposits form as hot brine discharged from subvolcanic mafic to intermediate composition intrusions reacts with cool country rocks. Albitite U deposits form at deeper levels where brines albitize country rocks. IOCG deposits form on the roof or periphery of IOA mineralization at lower temperatures, often with involvement of external fluids. Polymetallic skarn, replacement and vein deposits occur outboard from IOCG deposits. Manganese replacement and lacustrine Fe deposits form near or at the paleosurface.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Lacustrine evaporite
Enumerated_Domain_Value_Definition:
Lacustrine evaporite systems operate in closed drainage basins in arid to hyper-arid climatic zones. Elements present in meteoric surface, ground, and geothermal recharge water are concentrated by evaporation. As salinity increases, evaporite minerals typically precipitate in the following sequence: gypsum or anhydrite, halite, sylvite, carnallite, borate. Nitrates are concentrated in basins that accumulate sea spray. Residual brines enriched in Li and other elements often accumulate in aquifers below dry lake beds. Lithium-clay and Li-B-zeolite deposits form where residual brine reacts with lake sediment, ash layers, or volcanic rocks.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Mafic magmatic
Enumerated_Domain_Value_Definition:
Mafic magmatic systems generally form in large igneous provinces (LIP) related to mantle plumes or meteorite impacts. Nickel-Cu sulfide ores with PGEs result from settling and accumulation of immiscible sulfide liquids in mafic layered intrusions and ultramafic magma conduits. In layered intrusions, Fe-Ti oxides, chromite and PGE minerals crystalize from evolving parental magmas and are concentrated by physical processes in cumulate layers. In anorthosites, Fe-Ti oxides ± apatite crystalize from residual magmas entrained in plagioclase-melt diapirs. In convergent settings, Alaskan-type intrusions with Fe-Ti oxides and PGE form from mantle melts.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Magmatic REE
Enumerated_Domain_Value_Definition:
Magmatic REE systems typically occur in continental rifts or along translithospheric structures. REE and other elements in mantle-derived ultrabasic, alkaline, and peralkaline (agpaitic) intrusions are enriched by fractionation and separation of immiscible carbonatite melts ± saline hydrothermal liquids. Exsolved magmatic fluids or heated external fluids may deposit REE and other elements in adjacent country rocks.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Marine chemocline
Enumerated_Domain_Value_Definition:
Marine chemocline systems operate where basin brines discharge into the ocean, resulting in increases in bioproductiviy that can produce metalliferous black shales. Changes in ocean chemistry (for example, oceanic anoxic events) and development of chemoclines result in chemical sedimentation of phosphate and Mn and Fe carbonates and oxides.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Marine evaporite
Enumerated_Domain_Value_Definition:
Marine evaporite systems operate in shallow restricted epicontinental basins in arid to hyper-arid climatic zones. Sabka dolomite and sedimentary magnesite form in coastal salt flats and lagoons. Elements present in seawater are concentrated by evaporation. As salinity increases, evaporite minerals typically precipitate in the following sequence: gypsum or anhydrite, halite, sylvite. Residual basin brines are enriched in conserved elements, such as Mg and Li. Incursion of fresh water or seawater can produce halite dissolution brines.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Metamorphic
Enumerated_Domain_Value_Definition:
Metamorphic systems recrystallize rocks containing organic carbon or REE phosphate minerals or U minerals. Crystalline magnesite forms by carbonation of peridotite.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Meteoric convection
Enumerated_Domain_Value_Definition:
Low-sulfidation Au-Ag deposits associated with mantle plume volcanic rocks form under relatively low oxygen and sulfur fugacities, have low base metal contents, and high Au/Ag ratios and Se contents. Low-sulfidation deposits along extensional fault zones that are not associated with proximal, coeval magmatic activity may be underlain by rift-related dikes and sills.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Meteoric recharge
Enumerated_Domain_Value_Definition:
Meteoric recharge systems operate where oxidized meteoric groundwater displaces reduced connate water in sandstone aquifers that often contain volcanic ash or in granitic intrusions or where such groundwater evaporates at the surface. As oxidized water descends through sandstone aquifers it scavenges U and other elements from detrital minerals and/or volcanic glass. Uranium and other elements precipitate at a redox front with reduced connate water, on carbonaceous material in the aquifers, or ferrous Fe minerals in granite, or at the surface in calcrete by evaporation. In ultramafic rocks, dissolved CO2 in meteoric ground water reacts with Mg-silicates to form magnesite, which may also precipitate in permeable sediment or rocks nearby.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Orogenic
Enumerated_Domain_Value_Definition:
Metamorphic dewatering of sulfidic volcanic and/or sulfidic carbonaceous and/or calcareous siliciclastic sequences during exhumation with fluid flow along dilatant structures. Iron minerals in host rocks are often sulfidized. Metavolcanic host rocks often contain volcanogenic seafloor sulfide deposits.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Petroleum
Enumerated_Domain_Value_Definition:
Nickel and V in porphyry complexes are the most abundant metals in plant and animal remains in source rocks and in derived petroleum. Helium is produced by radioactive decay of U and Th in felsic igneous rocks and siliciclastic rocks derived from them. It is released by magmatic heat and/or fracturing and accumulates in gas reservoirs below an impermeable seal.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Placer
Enumerated_Domain_Value_Definition:
Placer systems operate in drainage basins and along shorelines where there is either topographic relief and gravity driven turbulent flow of surface water or tidal- and wind-driven wave action. Placer systems concentrate insoluble resistate minerals liberated from various rock types and mineral occurrences by the chemical breakdown and winnowing away of enclosing minerals by the movement of water. The distribution of insoluble resistate minerals is controlled by their size, density and the turbulence of fluid flow.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Porphyry Cu-Mo-Au
Enumerated_Domain_Value_Definition:
Porphyry Cu-Mo-Au systems operate in oceanic and continental magmatic arcs with calc-alkaline compositions. Aqueous supercritical fluids exsolved from felsic plutons and the apices of subvolcanic stocks form a variety of deposit types as they move upward and outward, split into liquid and vapor, react with country rocks, and mix with ground water. The broad spectrum of deposit types results from the large thermal and chemical gradients in these systems.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Porphyry Sn (granite-related)
Enumerated_Domain_Value_Definition:
Granite-related porphyry Sn systems form in back arc or hinterland settings by similar processes from fluids exsolved from more crustally contaminated S-type peraluminous plutons and stocks. At deep levels, LCT pegmatites emanate from plutons. Resulting ore deposits tend to be poor in Cu and Mo and enriched in Li, Cs, Ta, Nb, Sn, W, Ag, Sb and In.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Reduced Intrusion-related
Enumerated_Domain_Value_Definition:
Reduced intrusion-related systems form in continental magmatic arcs by similar processes from fluids exsolved from calc-alkaline plutons and stocks that assimilated carbonaceous pyritic country rocks. Resulting ore deposits tend to be poor in Cu, Mo, Sn and enriched in W, Au, Ag, Te, Bi, Sb and As.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Volcanogenic Seafloor
Enumerated_Domain_Value_Definition:
Volcanogenic seafloor systems are driven by igneous activity along spreading centers, back arc basins and magmatic arcs. In spreading centers and back arc basins, seawater evolves to become an ore fluid by convection through hot volcanic rocks. In magmatic arcs, ore fluids exsolved from subvolcanic intrusions may mix with convecting seawater. Ore deposits form where hot reduced ore fluids vent into cool oxygenated seawater. Sulfides and sulfates precipitate in or near vents. Manganese and Fe precipitate at chemoclines over wide areas in basins with seafloor hydrothermal activity.
Enumerated_Domain_Value_Definition_Source: Hofstra and Kreiner (2020)
Attribute:
Attribute_Label: DepType
Attribute_Definition:
Type of mineral deposit; if more than one deposit type, they are listed in alphabetical order.
Attribute_Definition_Source: Hofstra and Kreiner (2020)
Attribute_Domain_Values:
Unrepresentable_Domain:
Mineral deposit type (a) Deposits sharing a relatively wide variety and large number of attributes (Cox and Singer, 1986). (b) A “class representing all the recognized mineral deposits that are defined by physical and genetic factors that can be consistently differentiated from those of other classes or deposit types” (Barton and others, 1995, p. 80).

Deposit types in this study include: 5 element veins; Albitite uranium; Antimony; Arsenic-thallium-mercury; Barite; Barite (replacement and bedded); Basin brine; Black shale; Calcrete uranium; Carbonate uranium; Carbonatite; Cassiterite; Chromite; Clay; Coal uranium; Copper (sed-hosted and replacement); Copper-zinc sulfide; Cryptocrystalline magnesite; Distal disseminated silver-gold; Fluorspar; Garnet; Gneiss uranium; Gold; Graphite (coal or carbonaceous sed); Greisen; Greisen-S-R beryllium; High sulfidation; High sulfidation gold-silver; Ilmenite/rutile/leucoxene; Iron oxide apatite; Iron oxide copper gold; Iron-manganese; Iron-titanium oxide; Lacustrine manganese ; Lamproite; Lithocap alunite; Lithocap kaolinite; Low sulfidation; Low sulfidation epithermal Au-Ag; Magnesite; Manganese oxide (layers, crusts, nodules); Monazite/xenotime; Natural gas, He; Nickel-cobalt laterite; Nickel-copper-PGE sulfide; Oil and natural gas; Pegmatite LCT; Pegmatite NYF; Peralkaline syenite/granite/rhyolite/alaskite/pegmatites; PGE; PGE (low sulfide); Phosphate; Polymetallic sulfide; Polymetallic sulfide S-R-V; Polymetallic sulfide S-R-V-IS; Porphyry molybdenum; Porphyry/skarn; Porphyry/skarn copper; Porphyry/skarn molybdenum; Potash; Reflux and hydrothermal dolomite; Regolith (Ion adsorption) REE; Replacement manganese; Residual brine; Sabka dolomite; Salt; Sandstone uranium; Sedimentary magnesite; Skarn copper-molybdenum-tungsten; Skarn magnesite; Skarn molybdenum; S-R-V tungsten; Strontium (replacement and bedded); Supergene manganese; Uraninite, autunite-group minerals; Uranium (unconformity and breccia pipe); Volcanogenic beryllium; Volcanogenic uranium; Wolframite/scheelite; Zinc-copper sulfide; Zinc-lead (MVT and sedex); Zircon.
Attribute:
Attribute_Label: CritMin
Attribute_Definition:
List of known or potential critical mineral commodities associated with the focus area.
Attribute_Definition_Source: USGS authors
Attribute_Domain_Values:
Unrepresentable_Domain:
Critical minerals are those listed in the Federal Register as of May 18, 2018 https://www.federalregister.gov/documents/2018/05/18/2018-10667/final-list-of-critical-minerals-2018. Helium was removed from the list and nickel and zinc added.
Attribute:
Attribute_Label: OtherComm
Attribute_Definition:
Other commodities associated with the focus area (not on the critical minerals list). Includes primary and minor commodities reported. Commodity names are spelled out, except for REE (rare earth elements) and PGE (platinum group elements).
Attribute_Definition_Source: USGS authors
Attribute_Domain_Values:
Unrepresentable_Domain:
Includes primary and minor commodities reported. Commodity names are spelled out, except for REE (rare earth elements) and PGE (platinum group elements).
Attribute:
Attribute_Label: KnownCrit
Attribute_Definition:
List of critical minerals definitely known in the focus area (active or past production, resources).
Attribute_Definition_Source: USGS authors
Attribute_Domain_Values:
Unrepresentable_Domain:
Commodity names are spelled out, except for REE (rare earth elements) and PGE (platinum group elements).
Overview_Description:
Entity_and_Attribute_Overview:
The entity and attribute information provided here describes the EMRI focus areas tabular data associated with the data set. Please review the detailed descriptions that are provided (the individual attribute descriptions) for information on the values that appear as fields/table entries of the data set.
Entity_and_Attribute_Detail_Citation:
The entity and attribute information were generated by the individual and/or agency identified as the originator of the data set. Please review the rest of the metadata record for additional details and information.
Distribution_Information:
Distributor:
Contact_Information:
Contact_Person_Primary:
Contact_Person: ScienceBase
Contact_Organization: U.S. Geological Survey
Contact_Address:
Address_Type: mailing and physical
Address: Building 810, Mail Stop 302, Denver Federal Center
City: Denver
State_or_Province: CO
Postal_Code: 80225
Country: USA
Contact_Voice_Telephone: 1-888-275-8747
Contact_Electronic_Mail_Address: sciencebase@usgs.gov
Distribution_Liability:
Unless otherwise stated, all data, metadata and related materials are considered to satisfy the quality standards relative to the purpose for which the data were collected. Although these data and associated metadata have been reviewed for accuracy and completeness and approved for release by the U.S. Geological Survey (USGS), no warranty expressed or implied is made regarding the display or utility of the data for other purposes, nor on all computer systems, nor shall the act of distribution constitute any such warranty.
Standard_Order_Process:
Digital_Form:
Digital_Transfer_Information:
Format_Name: Vector Digital Data Set (Polygon)
Digital_Transfer_Option:
Online_Option:
Computer_Contact_Information:
Network_Address:
Network_Resource_Name: https://doi.org/10.5066/P9DIZ9N8
Fees: None. No fees are applicable for obtaining the data set.
Metadata_Reference_Information:
Metadata_Date: 20221101
Metadata_Contact:
Contact_Information:
Contact_Person_Primary:
Contact_Person: Connie Dicken
Contact_Organization: U.S. Geological Survey, NORTHEAST REGION
Contact_Position: Geologist
Contact_Address:
Address_Type: mailing address
Address: Mail Stop 954, 12201 Sunrise Valley Dr
City: Reston
State_or_Province: VA
Postal_Code: 20192
Country: US
Contact_Voice_Telephone: 703-648-6482
Contact_Facsimile_Telephone: 703-648-6252
Contact_Electronic_Mail_Address: cdicken@usgs.gov
Metadata_Standard_Name: FGDC Content Standard for Digital Geospatial Metadata
Metadata_Standard_Version: FGDC-STD-001-1998

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