AndreaBozzo/ceres-open-data-index huggingface dataset:
Conductivity, temperature, and salinity data for the Miami Pockmark and Key Biscayne Pockmark

Conductivity, temperature, and salinity data were collected from two offshore submarine pockmarks, Miami Pockmark and Key Biscayne Pockmark. A series of dives were performed to gather conductivity, temperature, and salinity data using an autonomous underwater vehicle (AUV) with a Conductivity, Temperature and Depth (CDT) instrument. These data were collected between May 5-8, 2016 using a Bluefin B12 AUV equipped with a CDT and an onboard calibrated Kearfott T-24 Inertial Navigation System (INS) aided by a GPS Wide Area Augmentation System (WAAS), 600 kHz RDI Doppler Velocity Log (DVL) and a Valeport sound velocity meter.

Tags: autonomous-underwater-vehicle, auv, conductivity, geoscientificinformation, inertial-navigation-system, ins, key-biscayne-pockmark, marine, miami, miami-pockmark, oceans, pockmark, r-v-weatherbird-ii, subsea-navigation, ultra-short-baseline-sonar, usbl-aided, usgs-5aa19b3ce4b0b1c392e863ef, water-temperature
Organization: Department of the Interior
Lower Brule Reservation Shoreline Erosion, Additional Data Layers, South Dakota, 2018

Additional data layers have been developed to supplement recently published information collected and developed for an investigation of shoreline erosion along the Lower Brule Reservation in Central South Dakota. The additional data layers presented in this data release include georeferenced 1965 single frame aerial photos, digitized shoreline features from the georeferenced 1965 images, digitized shoreline features from 2016 aerial imagery, and real-time kinematic surveys of shoreline features on selected reaches of the Lake Sharpe shoreline in 2018. This effort was completed by the USGS Dakota Water Science Center in cooperation with the Lower Brule Sioux Tribe, Tribal Preservation Office.

Tags: erosion, lake-francis-case, lake-sharpe, long-term-shoreline-erosion, lower-brule, lower-brule-indian-reservation, lyman-county, missouri-river, shoreline, shoreline-erosion, south-dakota, stanley-county, survey, usgs-5aa152abe4b0b1c392e8623b
Organization: Department of the Interior
Habitat and fish field survey data from Wyoming Range streams in 2012 and 2013

Stream habitat characteristics, energy development metrics, and fish catch per unit effort data for 91 sites (100m  stream reach) sampled in the summers of 2012 and 2013.We sampled four streams in the Dry Piney Drainage (Dry Piney, Beaver Dam, Black Canyon,  and North Black Canyon), five in the Fogarty Drainage (North and South Fogarty, North and South Pine Grove, and Sawmill) and four in the South Beaver Drainage (North Beaver, South Beaver, Middle Beaver, and Spring).

Tags: biota, environment, fish, oil-and-natural-gas-development, stream-habitat, upper-green-river, usgs-5aa060eae4b0b1c392e6c0a7, wyoming, wyoming-range
Organization: Department of the Interior
Bathymetric and tidal discharge data for Wilderness Breach, Fire Island National Seashore, Long Island, NY, May 14, 2015 - Bathymetry Contours: U.S. Geological Survey data release

In 2012, Hurricane Sandy created an open breach in the barrier island system along the south shore of Long Island, N.Y.  This breach formed at a location known as Old Inlet and migrated rapidly westward over the winter storm season following Hurricane Sandy. On May 14, 2015, U.S. Geological Survey (USGS) New York Water Science Center (NYWSC) personnel collected data to evaluate channel geometry, water velocity, and discharge of an open breach in the Federal Wilderness area of Fire Island National Seashore, N.Y. The breach resulted from major coastal flooding and overwash created by Hurricane Sandy on October 29, 2012. Data were collected using a Sontek M9 Acoustic Doppler Current Profiler (ADCP) with Real-Time Kinematic (RTK) Global Positioning System (GPS). Data were processed using a Geographic Information System (GIS) for interpolation and display. An initial series of transects was collected starting about 4 hours before ocean low tide on May 14, 2015. Data were collected perpendicular to flow through the breach beginning at 0725 Eastern Standard Time (EST) and ending at 0811 EST. The first set of transects was taken near the bayward side of the breach, with subsequent sets collected progressively closer to the seaward side of the breach. Discharge ranged from 16,400 cfs (cubic feet per second) during the beginning set of transects to 17,400 cfs during the second set of transects. A second series of transects was collected starting about 4 hours before ocean high tide on May 14, 2015. Data collection began at 1335 EST and ended at 1445 EST. The first set of transects was taken perpendicular to the flood tidal channels bayward of the former Great South Bay (GSB) shoreline; subsequent sets were collected progressively closer to the seaward side of the breach. Discharge ranged from 16,500 cfs during the beginning set of transects to 24,900 cfs during the final set of transects. Additional data were collected along the approximate centerline and adjacent to the shores of the channel to map the inundated area of the breach. The overall mapped area includes data collected during discharge measurements of both incoming and outgoing tide conditions.

Tags: acoustic-doppler-current-profiler, bathymetry, breach, fire-island-national-seashore, geoscientificinformation, long-island, oceans, suffolk-county, usgs-5aa03f58e4b0b1c392e6abfc, velocity
Organization: Department of the Interior
Bathymetric and tidal discharge data for Wilderness Breach, Fire Island National Seashore, Long Island, NY, May 14, 2015 - Bathymetry Raster Surface: U.S. Geological Survey data release

In 2012, Hurricane Sandy created an open breach in the barrier island system along the south shore of Long Island, N.Y.  This breach formed at a location known as Old Inlet and migrated rapidly westward over the winter storm season following Hurricane Sandy. On May 14, 2015, U.S. Geological Survey (USGS) New York Water Science Center (NYWSC) personnel collected data to evaluate channel geometry, water velocity, and discharge of an open breach in the Federal Wilderness area of Fire Island National Seashore, N.Y. The breach resulted from major coastal flooding and overwash created by Hurricane Sandy on October 29, 2012. Data were collected using a Sontek M9 Acoustic Doppler Current Profiler (ADCP) with Real-Time Kinematic (RTK) Global Positioning System (GPS). Data were processed using a Geographic Information System (GIS) for interpolation and display. An initial series of transects was collected starting about 4 hours before ocean low tide on May 14, 2015. Data were collected perpendicular to flow through the breach beginning at 0725 Eastern Standard Time (EST) and ending at 0811 EST. The first set of transects was taken near the bayward side of the breach, with subsequent sets collected progressively closer to the seaward side of the breach. Discharge ranged from 16,400 cfs (cubic feet per second) during the beginning set of transects to 17,400 cfs during the second set of transects. A second series of transects was collected starting about 4 hours before ocean high tide on May 14, 2015. Data collection began at 1335 EST and ended at 1445 EST. The first set of transects was taken perpendicular to the flood tidal channels bayward of the former Great South Bay (GSB) shoreline; subsequent sets were collected progressively closer to the seaward side of the breach. Discharge ranged from 16,500 cfs during the beginning set of transects to 24,900 cfs during the final set of transects. Additional data were collected along the approximate centerline and adjacent to the shores of the channel to map the inundated area of the breach. The overall mapped area includes data collected during discharge measurements of both incoming and outgoing tide conditions.

Tags: acoustic-doppler-current-profiler, bathymetry, breach, fire-island-national-seashore, geoscientificinformation, long-island, oceans, suffolk-county, usgs-5aa03f31e4b0b1c392e6abf8, velocity
Organization: Department of the Interior
Bathymetric and tidal discharge data for Wilderness Breach, Fire Island National Seashore, Long Island, NY, May 14, 2015 - Ebb Sample Points: U.S. Geological Survey data release

In 2012, Hurricane Sandy created an open breach in the barrier island system along the south shore of Long Island, N.Y.  This breach formed at a location known as Old Inlet and migrated rapidly westward over the winter storm season following Hurricane Sandy. On May 14, 2015, U.S. Geological Survey (USGS) New York Water Science Center (NYWSC) personnel collected data to evaluate channel geometry, water velocity, and discharge of an open breach in the Federal Wilderness area of Fire Island National Seashore, N.Y. The breach resulted from major coastal flooding and overwash created by Hurricane Sandy on October 29, 2012. Data were collected using a Sontek M9 Acoustic Doppler Current Profiler (ADCP) with Real-Time Kinematic (RTK) Global Positioning System (GPS). Data were processed using a Geographic Information System (GIS) for interpolation and display. An initial series of transects was collected starting about 4 hours before ocean low tide on May 14, 2015. Data were collected perpendicular to flow through the breach beginning at 0725 Eastern Standard Time (EST) and ending at 0811 EST. The first set of transects was taken near the bayward side of the breach, with subsequent sets collected progressively closer to the seaward side of the breach. Discharge ranged from 16,400 cfs (cubic feet per second) during the beginning set of transects to 17,400 cfs during the second set of transects. A second series of transects was collected starting about 4 hours before ocean high tide on May 14, 2015. Data collection began at 1335 EST and ended at 1445 EST. The first set of transects was taken perpendicular to the flood tidal channels bayward of the former Great South Bay (GSB) shoreline; subsequent sets were collected progressively closer to the seaward side of the breach. Discharge ranged from 16,500 cfs during the beginning set of transects to 24,900 cfs during the final set of transects. Additional data were collected along the approximate centerline and adjacent to the shores of the channel to map the inundated area of the breach. The overall mapped area includes data collected during discharge measurements of both incoming and outgoing tide conditions.

Tags: acoustic-doppler-current-profiler, breach, fire-island-national-seashore, geoscientificinformation, long-island, oceans, suffolk-county, usgs-5aa03f15e4b0b1c392e6abf5, velocity
Organization: Department of the Interior
Bathymetric and tidal discharge data for Wilderness Breach, Fire Island National Seashore, Long Island, NY, May 14, 2015 - Flood Sample Points: U.S. Geological Survey data release

In 2012, Hurricane Sandy created an open breach in the barrier island system along the south shore of Long Island, N.Y.  This breach formed at a location known as Old Inlet and migrated rapidly westward over the winter storm season following Hurricane Sandy. On May 14, 2015, U.S. Geological Survey (USGS) New York Water Science Center (NYWSC) personnel collected data to evaluate channel geometry, water velocity, and discharge of an open breach in the Federal Wilderness area of Fire Island National Seashore, N.Y. The breach resulted from major coastal flooding and overwash created by Hurricane Sandy on October 29, 2012. Data were collected using a Sontek M9 Acoustic Doppler Current Profiler (ADCP) with Real-Time Kinematic (RTK) Global Positioning System (GPS). Data were processed using a Geographic Information System (GIS) for interpolation and display. An initial series of transects was collected starting about 4 hours before ocean low tide on May 14, 2015. Data were collected perpendicular to flow through the breach beginning at 0725 Eastern Standard Time (EST) and ending at 0811 EST. The first set of transects was taken near the bayward side of the breach, with subsequent sets collected progressively closer to the seaward side of the breach. Discharge ranged from 16,400 cfs (cubic feet per second) during the beginning set of transects to 17,400 cfs during the second set of transects. A second series of transects was collected starting about 4 hours before ocean high tide on May 14, 2015. Data collection began at 1335 EST and ended at 1445 EST. The first set of transects was taken perpendicular to the flood tidal channels bayward of the former Great South Bay (GSB) shoreline; subsequent sets were collected progressively closer to the seaward side of the breach. Discharge ranged from 16,500 cfs during the beginning set of transects to 24,900 cfs during the final set of transects. Additional data were collected along the approximate centerline and adjacent to the shores of the channel to map the inundated area of the breach. The overall mapped area includes data collected during discharge measurements of both incoming and outgoing tide conditions.

Tags: acoustic-doppler-current-profiler, bathymetry, breach, fire-island-national-seashore, geoscientificinformation, long-island, oceans, suffolk-county, usgs-5aa03ef9e4b0b1c392e6abf2, velocity
Organization: Department of the Interior
West Nile virus susceptibility of American singer canaries: Data

Three datasets are included: 1) survival of domesticated canaries and American crows following sub-cutaneous challenges ranging from 101 – 105 plaque forming units of West Nile virus. 2) Arbitrary units of WNV detected by RT-PCR or plaque forming units of WNV cultured in vero cells in 4 separate studies. Culture results are indicated for each day post WNV challenge. 3) Weight (mass) changes in grams in canaries and crows each day following WNV challenge. Day 0 (inoculation) set to 0 gms, then each subsequent day is change in gms from previous day.

Tags: american-crow, american-singer-canary, animal-model, biota, disease, health, usgs-5aa0279be4b0b1c392e6a16d, west-nile-virus
Organization: Department of the Interior
Geochemical and geophysical data for wells in the Rosedale Ranch oil and gas field

The U.S. Geological Survey (USGS) in cooperation with the California State Water Resources Control Board compiled and analyzed data for the purpose of mapping groundwater salinity in selected oil and gas fields in California. The data for the Rosedale Ranch oil field include well construction data, digitized borehole geophysical data, geochemical analyses of water samples from oil and gas wells and groundwater wells, geological formation depths, and the groundwater total dissolved solids (TDS) calculations used in the accompanying manuscript. These data have been compiled from many sources and span several decades. The well construction data includes attributes such as the date drilling began (spud date), well depth, the depth of top producing perforation, and borehole orientation. These data have been in archived scanned pages in raster format on the Division of Oil, Gas, and Geothermal Resources (DOGGR) website. Similarly, the borehole geophysical data, measured by oil companies, have been archived in raster format. This project has converted the borehole geophysical data from selected oil and gas wells into a computer readable numerical format. The geochemical analyses have also been archived in scanned formats, but are now compiled and verified for analysis. All of the data collected are part of the California State Water Resources Control Board's Program of Regional Monitoring of Water Quality in Areas of Oil and Gas Production and the USGS California Oil, Gas, and Groundwater (COGG) program.

Tags: borehole-geophysics, california, central-valley, geochemistry, geological-formation, groundwater-salinity, inland-waters, oil-and-gas, produced-waters, rosedale-ranch, usgs-5a9f2acae4b0b1c392e502f5
Organization: Department of the Interior
Regional scale magnetotelluric data from the Rio Grande Rift and southern Rocky Mountains, Station rgr017

This dataset consists of 102 magnetotelluric (MT) stations collected in 2012-2014 in the Rio Grande Rift and southern Rocky Mountains. The U.S. Geological Survey acquired these data to improve regional conductivity models of the western United States. This work is in support of studies of the effect of lithospheric modification on electrical resistivity structure and tectonic evolution of the western United States.

Tags: apparent-resistivity, colorado, electromagnetic-surveying, geology-geophysics-and-geochemistry-science-center, geophysics, geoscientificinformation, gggsc, impedance, magnetic-field-earth, magnetotelluric, mineral-resources-program, mrp, mt, phase, regional-conductivity-models, rio-grande-rift, rocky-mountains, time-series, tipper, usgs-5ad9176be4b0e2c2dd27a90c
Organization: Department of the Interior
Elk GPS collar data from National Elk Refuge 2006-2015

17 adult female elk were captured on or around the National Elk Refuge and monitored with GPS collars from 2006 to 2015. Each of these elk were monitored for 1 to 2 years and migrated from the National Elk Refuge to Yellowstone National Park during the spring. Here we provide the unique identifier for each individual elk, the date/time stamp of each GPS location, the GPS location of the elk in UTMs and Lat-Long, the month of each GPS location, the year of each GPS location, and the date of each GPS location in numeric form.

Tags: biota, cervus-canadensis, connectivity, ecology, elk, gps-data, grand-teton-national-park, location, movement, national-elk-refuge, park, resource-selection, teton, ungulate, usgs-5a9f2782e4b0b1c392e502ea, wyoming, yellowstone-national-park
Organization: Department of the Interior
Airborne Magnetic Surveys over Oklahoma, 2017

Airborne magnetic surveys were conducted in Oklahoma from August 11th, 2017-October 28th, 2017, by Goldak Airborne Surveys. Here we present downloadable flight line data from those surveys in comma-separated values (csv format). Three areas were flown along a draped surface with a nominal survey height above ground of 120 meters. The flight line spacing for these areas was 200 to 400 m for Area 123, in southwestern Oklahoma; 1000 m for Area 4, in northwestern Oklahoma, and 800 m for Area 5, in north-central Oklahoma. For each area control lines were flown at ten times the traverse line spacing. The surveys were flown to map subsurface geologic variations including ancient magmatic bodies, faults, and other geologic contacts by measuring subtle changes in Earth's magnetic field that reflect different types of buried rock.

Tags: aeromagnetic-surveying, airborne-geophysics, earthquake-hazards, geologic-framework-studies, geology-geophysics-and-geochemistry-science-center, geophysics, geoscientificinformation, gggsc, induced-seismicity, layered-mafic-intrusions, magnetic-data, magnetic-field-earth, mineral-resources, mineral-resources-program, mrp, oklahoma-geological-survey, usgs-5a9f0b3ce4b0b1c392e50241, usgs-earthquake-hazards-program
Organization: Department of the Interior
Land Use Land Cover, 1998 - 2013, Clarksburg (Montgomery County, MD)

This dataset contains digitized land use/land cover (LULC) polygons for years between 1998 and 2013 for six watersheds within and near the Clarksburg Special Protection Area located in Montgomery County, Maryland, USA. Each polygon is representative of the LULC for a specific year within 500-foot buffered watersheds. Watershed boundaries for Cabin Branch (CB), Crystal Rock (CR), Soper Branch (SB), Tributary 104 (T104), and Tributary 109 (T109) were derived using USGS topographic maps while Ten Mile Creek (TMC) was derived using Montgomery County, Maryland LiDAR data. The Habitat Digitizer Extension add-in from NOAA for ArcMap was used to customize a hierarchical classification scheme to attribute polygons delineated by visually interpreting aerial imagery and orthoimagery taken during tree leaf-off season.

Tags: clarksburg, land-use-and-land-cover, land-use-change, maryland, montgomery-county, stormwater-runoff, usgs-5a9f011ae4b0b1c392e501cc
Organization: Department of the Interior
Lake Michigan 2010-11 selected common loon telemetry observations

Implantable satellite transmitters (e.g., Model PTT-100, Microwave Telemetry, Inc) were incorporated into the study to provide fine-resolution location data for a sample of the adult male common loons fitted with geolocator tags in 2010 and 2011.  Transmitters were implanted in the abdominal cavity following procedures developed by Korschgen et al. (1996).  The satellite transmitters were programmed to transmit on a variable schedule based on the anticipated stage of migration during the loon’s annual cycle - 8 hours on:72 hours off during the breeding season, 8 hours on:24 hours off while migrating, 6 to 8 hours on:96 hours off on the wintering grounds, and 8 hours on:24 hours off during spring migration, and 8 hours on:96 hours off for the remaining life of the transmitter.  Transmitter data, received by equipment on polar-orbiting National Oceanic and Atmospheric Administration Tiros-N weather satellites, were transmitted to the Service Argos data processing center in Landover, Maryland, where loon locations were estimated from the Doppler shift in the transmitter's carrier frequency.  Location estimates were acquired using Argos Standard Service Processing (Argos Location Classes [LC] 3, 2, 1, and 0) and Auxiliary Location Processing (LC A, B, and Z).  One standard deviation of nominal accuracy for location estimates with LC 3, 2, 1, and 0 are &lt;250, 250 to 500, 500 to 1,500, and &gt;1,500 m, respectively (Service Argos 2008).  We utilized the most accurate locations per 8-hour transmission period for each individual to describe the daily location of that adult loon.  Spot measurements of water depth and distance to shore were determined for each radiomarked loon location.  Only location estimates for LC qualities 1-3 were used in the analyses.

Tags: common-loon, distribution, location-estimate, platform-terminal-transmitter, satellite-transmitter-implant, usgs-5a9ebcb2e4b0699060731523
Organization: Department of the Interior
Geospatial datasets of AUV observations including bottom dissolved oxygen in Great South Bay, Long Island, New York, August 2016

This data set provides locations and values of water quality parameters from a survey  conducted on August 26, 2016 using an Autonomous Underwater Vehicle (AUV) in Patchogue Bay, NY.  During the August 26 survey, 16,487 observations of water quality parameters were made.  Parameters collected include dissolved oxygen, pH, water temperature, specific conductance, and salinity. Data was collected in approximately east-west transects by the AUV, with the northern-most transects made first.  Data was collected between the hours of 1 am and 5 am to obtain minimum DO values in the daily cycle.

Tags: autonomous-underwater-vehicle, brown-creek, connetquot-river, estuarine-processes, great-south-bay, hydrology, long-island, nicoll-bay, oxygen-content-water, patchogue-bay, salinity, south-shore-estuary-reserve, usgs-5a9e9fc6e4b069906073147f, water-ph, water-quality, water-resource-management, water-temperature
Organization: Department of the Interior
Geospatial datasets of AUV observations including bottom dissolved oxygen in Great South Bay, Long Island, New York, August 2016

This data set provides locations and values of water quality parameters from a survey  conducted on August 25, 2016 using an Autonomous Underwater Vehicle (AUV) in Nicoll Bay, NY.  During the August 25 survey, 12,275 observations of water quality parameters were made.  Parameters collected include dissolved oxygen, pH, water temperature, specific conductance, and salinity. Data was collected in approximately east-west transects by the AUV, with the northern-most transects made first.  Data was collected between the hours of 1 am and 5 am to obtain minimum DO values in the daily cycle.

Tags: autonomous-underwater-vehicle, brown-creek, connetquot-river, estuarine-processes, great-south-bay, hydrology, long-island, nicoll-bay, oxygen-content-water, patchogue-bay, salinity, south-shore-estuary-reserve, usgs-5a9e9fb8e4b069906073147d, water-ph, water-quality, water-resource-management, water-temperature
Organization: Department of the Interior