AndreaBozzo/ceres-open-data-index huggingface dataset:
a) Strontium Isotope Data

The Yellowstone Plateau Volcanic field consists of lavas from the last two million years. The most recent volcanic units are the Central Plateau Member and the older Upper Basin Member rhyolites (Christiansen, 2001). Investigations into the elemental and isotopic composition of these lavas can provide insight into the recent volcanic history of the different eruptive episodes and provide constraints on the hydrothermal fluid compositions that result from water-rock interactions occurring at depth within the hydrothermal system. 
In this Data Release, seventeen samples of Yellowstone rhyolite samples from Upper Basin and Central Plateau Member lava flows were analyzed for strontium isotopic composition. Analyzed samples include recently collected samples along with samples from the rock collection of Robert L. Christiansen (Robinson et al., 2021). This data was collected to constrain models of fluid-rock interaction of Yellowstone’s hydrothermal system. 
Christiansen, R.L., 2001, The Quaternary and Pliocene Yellowstone Plateau Volcanic Field of Wyoming, Idaho, and Montana. U.S. Geological Survey Professional Paper 729-G, 120 p. 
Robinson, J.E., McConville, E.G., Szymanski, M.E., and Christiansen, R.L., 2021, Yellowstone Sample Collection - database: U.S. Geological Survey data release, https://doi.org/10.5066/P94JTACV

Tags: sr-isotopes, usgs-633c75fdd34e900e86cf1a29
Organization: Department of the Interior
CTD (conductivity-temperature-depth) data collected by the U.S. Geological Survey on Stellwagen Bank during three surveys aboard the R/V Auk, September 2020 to August 2021

These data are a part of the effort to map geologic substrates of the Stellwagen Bank National Marine Sanctuary region off Boston, Massachusetts. The overall goal is to develop high-resolution (1:25,000) interpretive maps, based on multibeam sonar data and seabed sampling, showing surficial geology and seabed sediment dynamics. The work was conducted in collaboration with the Stellwagen Bank National Marine Sanctuary, and the data collected will aid research on the ecology of fish and invertebrate species that inhabit the region. The Sanctuary's research vessel, R/V Auk, visited a total of 169 locations on Stellwagen Bank during three separate surveys from September 2020 to August 2021. During these surveys a customized Van Veen grab sampler (SEABOSS) equipped with a video camera and a CTD was deployed in drift mode to collect sediment for grain-size analysis, video imagery of the seabed, and measurements of water column properties including temperature, salinity, density, and fluorescence.

Tags: atlantic-ocean, chemical-oceanography, cmhrp, coastal-and-marine-hazards-and-resources-program, conductivity, ctd, ctd-measurement, depth, environmental-chemistry, fluorescence, geoscientificinformation, marine-chemistry, massachusetts, massachusetts-bay, national-oceanic-and-atmospheric-administration, noaa, north-america, ocean-salinity, ocean-sciences, ocean-temperature, oceanographic-observations, oceans, salinity, sbnms, seabed-observation-and-sampling-system, seaboss, stellwagen-bank, stellwagen-bank-national-marine-sanctuary, temperature, turbidity, u-s-geological-survey, united-states, usgs, usgs-633c8f97d34e900e86cf1a9d, water-density, whcmsc, woods-hole-coastal-and-marine-science-center
Organization: Department of the Interior
Pesticide residues in passive samplers and bee tissue from Conservation Reserve Program fields across an agricultural gradient in eastern Iowa, USA, 2019 (ver 2.0, October 2023)

This data release includes sampling location, pesticide concentrations in passive samplers (silicone bands) and bees foraging in Conservation Reserve Program fields. Sampling took place during July and August of 2019. Fields were located on private land managed for the U.S. Department of Agriculture Conservation Reserve Program in eastern central Iowa, U.S.A.
	  First posted - December 14, 2022(available from author)
		Revised - October 2023 (version 2.0)
	  

Tags: bees, biota, insects, invasion-history, otolith-microchemistry, pesticides, usgs-633c6129d34e900e86cf19e2
Organization: Department of the Interior
Water-Quality, Bed-Sediment, and Invertebrate Tissue Trace-Element Concentrations for Tributaries in the Clark Fork Basin, Montana, October 2019–September 2020

Water, bed sediment, and invertebrate tissue were sampled in streams from Butte to near Missoula, Montana, as part of a monitoring program in the Clark Fork Basin. The sampling program was completed by the U.S. Geological Survey, in cooperation with the U.S. Environmental Protection Agency, to characterize aquatic resources in the Clark Fork Basin and monitor trace elements associated with historical mining and smelting activities. Sampling sites were on the Clark Fork River and a subset of its tributaries. Water samples were collected periodically at 22 sites from October 2019 through September 2020. Bed-sediment and tissue samples were collected once at 12 sites during July 2020. 
Water-quality data included concentrations of major ions, dissolved organic carbon, nitrogen (nitrate plus nitrite), trace elements, and suspended sediment. Daily values of turbidity were determined at four sites. Bed-sediment data included trace-element concentrations in the fine-grained (less than 0.063 millimeter) fraction. Biological data included trace-element concentrations in whole-body tissue of selected aquatic benthic invertebrates. Statistical summaries of water-quality, bed-sediment, and invertebrate tissue trace element data for sites in the Clark Fork Basin were provided for the period of record: March 1985–September 2020.

Tags: bed-sediment, biota, clark-fork-basin, montana, trace-elements, usgs-633c59e7d34e900e86cf19bc, water-quality
Organization: Department of the Interior
Elemental and Strontium Isotopic Composition of Select Central Plateau and Upper Basin Member Rhyolites, Yellowstone Plateau Volcanic Field

The Yellowstone Plateau Volcanic field consists of lavas from the last two million years. The most recent volcanic units are the Central Plateau Member and the older Upper Basin Member rhyolites (Christiansen, 2001). Investigations into the elemental and isotopic composition of these lavas can provide insight into the recent volcanic history of the different eruptive episodes and provide constraints on the hydrothermal fluid compositions that result from water-rock interactions occurring at depth within the hydrothermal system.
In this Data Release, twenty-one samples of Yellowstone rhyolite samples from Upper Basin and Central Plateau Member lava flows were analyzed for major and trace element concentrations and strontium isotopic compositions. Analyzed samples include recently collected samples along with samples from the rock collection of Robert L. Christiansen (Robinson and others, 2021). This data was collected to constrain models of fluid-rock interaction of Yellowstone’s hydrothermal system. 
Christiansen, R.L., 2001, The Quaternary and Pliocene Yellowstone Plateau Volcanic Field of Wyoming, Idaho, and Montana. U.S. Geological Survey Professional Paper 729-G, 120 p. 
Robinson, J.E., McConville, E.G., Szymanski, M.E., and Christiansen, R.L., 2021, Yellowstone Sample Collection - database: U.S. Geological Survey data release, https://doi.org/10.5066/P94JTACV.

Tags: major-elements, sr-isotopes, trace-elements, usgs-633c53f3d34e900e86cf19a6, volatile-elements
Organization: Department of the Interior
Selected inputs for examining the complex relations between climate and streamflow in the Mid-Atlantic region of the United States

Streams provide water for human activities and consumption in much of the world. Streamflow is largely controlled by climate forces, therefore it is likely sensitive to climate changes. We analyzed daily air temperature (AT), precipitation (P), and stream discharge (Q) metrics for 124 watersheds in Maryland, Virginia, and North Carolina, United States, from 1981 through 2020. Spatial-raster datasets of daily P in mm were downloaded from Parameter-elevation Regressions on Independent Slopes Model (PRISM; http://prism.oregonstate.edu) on March 30, 2021, and datasets of daily AT in degrees Celsius (°C) were downloaded June 22, 2021, both at a 4-square kilometer (km2) resolution for the contiguous U.S. The final quarter of approved 2020 data for both datasets was downloaded between January 6 and 8, 2022. Daily mean-Q data were downloaded from the USGS’s National Water Information System on January 5, 2022, checked for completeness, and converted to cubic meters per second. The input data sets used to derive trends and PCA results are presented here in the zip file found below. Due to Excel’s maximum row constraints, the files have been subset by decade. Please refer to the linked manuscript below for more information.

Tags: air-temperature, discharge, nwis, pca, precipitation, prism, season, slr, usgs-633c2a04d34e900e86cf1907
Organization: Department of the Interior
Compilation of Public-Supply Well Construction Depths in California

This data release is a compilation of construction depth information for 12,383 active and inactive public-supply wells (PSWs) in California from various data sources. Construction data from multiple sources were indexed by the California State Water Resources Control Board Division of Drinking Water (DDW) primary station code (PS Code). Five different data sources were compared with the following priority order: 1, Local sources from select municipalities and water purveyors (Local); 2, Local DDW district data (DDW); 3, The United States Geological Survey (USGS) National Water Information System (NWIS); 4, The California State Water Resources Control Board Groundwater Ambient Monitoring and Assessment Groundwater Information System (SWRCB); and 5, USGS attribution of California Department of Water Resources well completion report data (WCR). For all data sources, the uppermost depth to the well's open or perforated interval was attributed as depth to top of perforations (ToP). The composite depth to bottom of well (Composite BOT) field was attributed from available construction data in the following priority order: 1, Depth to bottom of perforations (BoP); 2, Depth of completed well (Well Depth); 3; Borehole depth (Hole Depth). PSW ToPs and Composite BOTs from each of the five data sources were then compared and summary construction depths for both fields were selected for wells with multiple data sources according to the data-source priority order listed above. Case-by-case modifications to the final selected summary construction depths were made after priority order-based selection to ensure internal logical consistency (for example, ToP must not exceed Composite BOT). 
This data release contains eight tab-delimited text files. WellConstructionSourceData_Local.txt contains well construction-depth data, Composite BOT data-source attribution, and local agency data-source attribution for the Local data. WellConstructionSourceData_DDW.txt contains well construction-depth data and Composite BOT data-source attribution for the DDW data. WellConstructionSourceData_NWIS.txt contains well construction-depth data, Composite BOT data-source attribution, and USGS site identifiers for the NWIS data. WellConstructionSourceData_SWRCB.txt contains well construction-depth data and Composite BOT data-source attribution for the SWRCB data. WellConstructionSourceData_WCR.txt contains contains well construction depth data and Composite BOT data-source attribution for the WCR data. WellConstructionCompilation_ToP.txt contains all ToP data listed by data source. WellConstructionCompilation_BOT.txt contains all Composite BOT data listed by data source. WellConstructionCompilation_Summary.txt contains summary ToP and Composite BOT values for each well with data-source attribution for both construction fields. All construction depths are in units of feet below land surface and are reported to the nearest foot.

Tags: environment, geoscientificinformation, groundwater, inlandwaters, usgs-6345a6e9d34e342aee086369, well
Organization: Department of the Interior
Brown trout movement data in Glen and Grand Canyons, Arizona, USA

These data were compiled to test hypotheses regarding drivers of movement of brown trout. Objectives of our study were to test whether the degree of movement varied in response to placement of a weir in Bright Angel Creek, fall timed flooding events, or simply seasonal changes. These data represent summarized capture histories of brown trout in terms of states based on physical locations, data on removal efforts in Bright Angel Creek, and summaries of effort in the mainstem Colorado River. These data were collected at several locations along the Colorado River in Glen and Grand Canyon, including Bright Angel Creek from 2011 to 2018. These data were collected by U.S. Geological Survey, National Park Service, and Arizona Game and Fish. These data can be used to test hypotheses regarding drivers of brown trout movement in the Colorado River in its Grand Canyon segment.

Tags: arizona, biota, bright-angel-creek, brown-trout, capture-histories, coarse-movement-patterns, colorado-river, data-release, electrofishing, field-inventory-and-monitoring, field-sampling, glen-canyon, grand-canyon, inlandwaters, mark-recapture, movement, physical-locations, population-and-community-ecology, probability-of-capture, recapture-rates, removal-efforts, sampling-effort, summaries-of-effort, survival, usgs-633b1532d34e900e86cf13d3, weir
Organization: Department of the Interior
Katahdin Woods and Waters National Monument 4-Band Orthorectified Aerial Images

Katahdin Woods and Waters National Monument was established on August 24, 2016. The monument spans mountains and forest lands in north central Maine.
High-resolution aerial imagery was collected on October 5, 2019 with a Phase One iXU-R 180 RGB camera co-mounted with a Phase One iXU-RS 160 Achromatic camera. Images from the two cameras are merged to create 4-band imagery that can be displayed as either true-color (RGB) or color-infrared (CIR). The imagery has a resolution of approximately 0.15 meter/pixel (6 inches).

Tags: imagerybasemapsearthcover, katahdin-woods-and-waters-national-monument, maine, usgs-633b0f03d34e900e86cf1389
Organization: Department of the Interior
Model Archive: Simulations of Sediment Transport, Middle Channel of St. Clair River Delta, Michigan

This archive contains results of flow and sediment transport simulations of a reach of the Middle Channel of the St. Clair River delta, Michigan using the iRIC modeling system and the Flow and Sediment Transport with Morphologic Evolution of Channels (FASTMECH) solver.
Two hydraulic model simulations were used to determine lateral eddy viscosity and roughness settings. One simulation contains results of the Wilcox-Kenworthy (WK) two-fraction sediment transport model. The WK model was used to simulate the movement of fine grained sediment into coarser immobile substrate. The coarse rock rubble substrate (reefs) constructed in the Middle Channel in 2012 began filling with sand within a year. However, detailed field data to verify the spatial and temporal process of colmation in the Middle Channel reefs are not available. Thus, the sediment transport predictions cannot be explicitly validated but can be compared with field measurements of bedform translation. The archive is split into child-items to help distinguish the individual components of the archive and make downloading of large files more manageable in terms of data size.

Tags: habitat, inlandwaters, lake-sturgeon, michigan, modeling, rivers, sediment-transport, st-clair-river, usgs-633aeb6ad34e900e86cf1309
Organization: Department of the Interior
Geochemistry of fine sediment from San Francisco Bay shoals (2012) and tributaries (2010, 2012, 2013)

Elemental chemistry and weight percent of the less than 0.063 mm fine sediment fraction are reported for surface sediments from shoals, the ebb tide delta, local tributaries, and inland rivers that carry sediment to San Francisco Bay, California.

Tags: alameda-creek, cmhrp, coastal-and-marine-hazards-and-resources-program, corte-madera-creek, environment, fort-funston, geochemistry, geoscientificinformation, grab-sampling, guadelupe-river, mass-spectroscopy, napa-river, pacific-coastal-and-marine-science-center, pcmsc, petaluma-river, rare-earth-elements, sacramento-river, san-francisco-bay, san-francisquito-creek, san-joaquin-river, san-pablo-bay, sediment-geochemistry, sonoma-creek, south-bay, substrate, suisun-bay, u-s-geological-survey, usgs, usgs-63387bfcd34e900e86cdd8c8, wildcat-creek
Organization: Department of the Interior
Meteorological data at a Sunset Crater cinder field: March 2021 to May 2022: U.S. Geological Survey data release

A meteorological station equipped with a rain gauge, atmospheric pressure sensor, temperature and relative humidity sensor, soil moisture sensor, and an anemometer (measuring wind speed, gust speed, and direction) was deployed at a cinder field in Sunset Crater National Monument, Arizona. This dataset has been collecting data every 15 minutes with the goal to provide atmospheric context for a subsurface temperature profiler buried nearby.

Tags: air-temperature, arizona, climate-data, climatologymeteorologyatmosphere, geoscientificinformation, meteorological-data, relative-humidity, sunset-crater-national-monument, usgs-6337bd79d34e900e86cc6037, wind
Organization: Department of the Interior
Cinder field subsurface temperature and relative humidity profiles at Sunset Crater National Monument, Arizona, March 09, 2021 to May 26, 2022: U.S. Geological Survey data release

The vadose zone (unsaturated zone) in a soil is of particular interest because it is broadly applicable to desert soils, which are seldom saturated and usually dry. In the absence of strong geothermal heating, the near-surface soil temperature profile is expected to exhibit maximum variation (for a given diurnal period) at the surface, with the diurnal variations becoming successively damped with depth. The temperature at a given depth is the result of diffusive heat transport vertically within the soil column. Water vapor also is expected to be transported via diffusion through the soil column [1].
We have selected a small cinder field in Sunset Crater National Monument, Arizona (SUCR) and deployed temperature and relative humidity sensors at 5 different depths (1, 6, 12, 24, and 48 cm) to capture diurnal temperature and humidity variations. 
[1] Hillel, D., (1980) Fundamentals of Soil Physics Data presented here span from March 09, 2021 to August 10, 2022.

Tags: arizona, climatologymeteorologyatmosphere, deserts, geoscientificinformation, relative-humidity, soil-temperature, subsurface-profiler, sunset-crater-national-monument, usgs-6337af3fd34e900e86cc602c
Organization: Department of the Interior
Context images at a Sunset Crater cinder field: U.S. Geological Survey data release: March 09, 2021 to August 10, 2022

A BlazeVideo camera has been set up next to a meteorological station at a small cinder field in Sunset Crater National Monument, Arizona. Images are taken every hour. Data presented here span from  March 09, 2021 to August 10, 2022.

Tags: arizona, climatologymeteorologyatmosphere, deserts, environment, ripples, sunset-crater-national-monument, usgs-63378879d34e900e86cc2632
Organization: Department of the Interior
Katahdin Woods and Waters National Monument Seboeis Unit Vegetation Mapping Project: Project Geodatabase

The Katahdin Woods and Waters National Monument Seboeis Unit Vegetation Mapping Project was initiated in the fall of 2019 by a grant through the USGS Natural Resource Preservation Program to classify and map vegetation types of the Seboeis Unit thereby providing resource managers and biological researchers with useful baseline vegetation information. This layer provides the vegetation map for the Seboeis Unit. Information for this layer was collected in 2019 and 2020. After completion of the accuracy assessment process, 33 map classes represent the Seboeis Unit of the monument. Of the 33 map classes that represent the Seboeis Unit, 28 represent natural (including ruderal) vegetation types, consisting of 50 U.S. National Vegetation Classification (USNVC) association types. For the remaining 5 of the overall 33 map classes, 2 represent USNVC cultural types for barren areas and developed areas and 3 represent non-USNVC types for non-vegetated open water. Of the 28 map classes representing natural (including ruderal) vegetation types, 15 represent a single vegetation type (when it exists above the minimum mapping unit [MMU]), 7 represent 2 vegetation types mapped together, 5 represent 3 vegetation types mapped together, and 1 represents 6 vegetation types mapped together. Polygon units were mapped to either a 0.5 ha or 0.25 ha minimum mapping unit, depending on vegetation type. 
The information in this layer is explained in depth in the report titled Vegetation Map for the Seboeis Unit of Katahdin Woods and Waters National Monument.

Tags: accuracy-assessment, aerial-imagery, biota, data-collection, environment, image-interpretation, imagerybasemapsearthcover, katahdin-woods-and-waters-national-monument, maine, map, national-park-service, national-vegetation-classification-standard, natural-resources-preservation-program, nvcs, plot, project-boundary, u-s-national-vegetation-classification, united-states, usgs-6335f4cad34e900e86c8bf79, usgs-nrpp, usnvc, vegetation
Organization: Department of the Interior
One-second USGS Tucson (TUC) magnetic observatory data collected before 2013

The USGS Geomagnetism Program operates a network of magnetic observatories that collect vector and scalar magnetometer data for use in Earth main-field modeling, geophysics research, space physics research, and space weather hazard assessment and mitigation. Until mid-2011, only 1-minute time resolution magnetic field measurements were archived with the INTERMAGNET consortium following international magnetic observatory standards. 1-second time resolution magnetic field measurements, which had already been collected by all the USGS observatories for up to almost a decade prior, started being archived with INTERMAGNET on June 13, 2011, or July 27, 2012 in the case of the more recently constructed Deadhorse (DED) magnetic observatory. This data release contains 1-second time resolution magnetic field measurements collected up through the end of 2012, after which time 1-second data from USGS magnetic observatories may be obtained from INTERMAGNET. There is some overlap between data in this release and those data archived with INTERMAGNET. Any discrepancies that may exist between these two data sources should resolve in favor of INTERMAGNET.
TUC-specific notes:
- some filenames originally possessing a ".sec" extension were renamed to ".raw"

Tags: geologic-hazards-science-center, geomagnetism-program, geoscientificinformation, magnetic-observatory, magnetic-scalar-field, magnetic-variometer, magnetic-vector-field, magnetometer, north-america, tucson-arizona, united-states, usgs, usgs-6334f263d34e900e86c71761
Organization: Department of the Interior