AndreaBozzo/ceres-open-data-index huggingface dataset:
Data Release for "Reconstructing paleohydrology in the northwest Great Basin since the last deglaciation using Paisley Caves fish remains (Oregon, U.S.A.)"

This dataset includes tables of stratigraphic age-depth information for Paisley Caves 2 and 5, in Oregon U.S.A., along with tables of stable and strontium isotopic data for fish remains and geological samples from the study area surrounding the Paisley Caves.

Tags: chewaucan-river, geochronology, holocene, lake-county, lower-chewaucan-marsh, oregon, pleistocene, summer-lake, upper-chewaucan-marsh, usgs-5fa1af56d34e198cb793ccb1
Organization: Department of the Interior
Debris Flow Video Files for Wide Angle Camera (Station 1), Chalk Cliffs, Colorado, USA, 2015

Chalk Cliffs, located 8 miles southwest of Buena Vista, Colorado, is one of the most active debris-flow areas in the state (U.S. Geological Survey). This "Child item" page includes videos of debris flows captured by one of the high-definition cameras at the monitoring site in Chalk Cliffs, CO. This camera (Wide-angle Camera) is located near Station 1 on the opposite side of the basin with a broad view of the channel. The attached figure "station_and_camera_locations.png" provides an overview figure with the location of the two cameras and three stations along the channel. 
Video recording for all cameras is triggered using a rainfall threshold, derived from rainfall measurements from rain gauges (Michel et al., 2019). The complete videos for all the cameras are downloaded manually during site visits. More detailed information about the cameras and settings used can be found in the metadata file under “Process steps” in “Data quality information.”  
During 2015, several debris flows were captured by the 'Wide-angle Camera'. The videos for all debris flows captured by this camera along with the dates they were captured can be found in the attached zip files. The file names indicate "date_camera_debrisflow." 
The following citations relate to reports that provide background information for this data release:  
Michel, A., Kean, J.W., Smith, J.B., Allstadt, K.E., Coe, J.A. (2019). Taking the pulse of debris flows: Extracting debris-flow dynamics from good vibrations in southern California and central Colorado. Debris-flow hazards mitigation: Mechanics, Monitoring, Modeling, and Assessment. http://dx.doi.org/10.25676/11124/173224   
U.S. Geological Survey Landslide Hazards Program. (2020). Chalk Cliffs, Colorado. U.S Geological Survey, https://www.usgs.gov/natural-hazards/landslide-hazards/science/chalk-cliffs-colorado?qt-science_center_objects=0#qt-science_center_objects 
Kean, J.W., Smith, J.B., and Coe, J.A., 2020, Debris-flow monitoring data, Chalk Cliffs, Colorado, USA, 2014: U.S. Geological Survey data release, https://doi.org/10.5066/P9MUWDFN.

Tags: chalk-cliffs, colorado, debris-flow, flood, geologic-hazards-science-center, geomorphology, hydrology, landslide-hazards-program, landslides, usgs, usgs-5f9c379ed34e198cb78de1a7, video-monitoring, videos
Organization: Department of the Interior
Flood Video Files for Wide Angle Camera (Station 1), Chalk Cliffs, Colorado, USA, 2015

Chalk Cliffs, located 8 miles southwest of Buena Vista, Colorado, is one of the most active debris-flow areas in the state (U.S. Geological Survey). This "Child item" page includes videos of floods captured by one of the high-definition cameras at the monitoring site in Chalk Cliffs, CO. This camera (Wide-angle Camera) is located near Station 1 on the opposite side of the basin with a broad view of the channel. The attached figure "station_and_camera_locations.png" provides an overview figure with the location of the three cameras and three stations along the channel. 
Video recording for all cameras is triggered using a rainfall threshold, derived from rainfall measurements from a rain gauge (Michel et al., 2019). The complete videos for all the cameras are downloaded manually during site visits. More detailed information about the cameras and settings used can be found in the metadata file under “Process steps” in “Data quality information.”  
During 2015, several floods were captured by the 'Wide-angle Camera'. The videos for all floods captured by this camera along with the dates they were captured can be found in the attached zip files. The file names indicate "date_camera_flood." 
The following citations relate to reports that provide background information for this data release:  
Michel, A., Kean, J.W., Smith, J.B., Allstadt, K.E., Coe, J.A. (2019). Taking the pulse of debris flows: Extracting debris-flow dynamics from good vibrations in southern California and central Colorado. Debris-flow hazards mitigation: Mechanics, Monitoring, Modeling, and Assessment. http://dx.doi.org/10.25676/11124/173224 
U.S. Geological Survey Landslide Hazards Program. (2020). Chalk Cliffs, Colorado. U.S Geological Survey, https://www.usgs.gov/natural-hazards/landslide-hazards/science/chalk-cliffs-colorado?qt-science_center_objects=0#qt-science_center_objects 
Kean, J.W., Smith, J.B., and Coe, J.A., 2020, Debris-flow monitoring data, Chalk Cliffs, Colorado, USA, 2014: U.S. Geological Survey data release, https://doi.org/10.5066/P9MUWDFN

Tags: chalk-cliffs, colorado, debris-flow, flood, geologic-hazards-science-center, geomorphology, hydrology, landslide-hazards-program, landslides, usgs, usgs-5f9c3785d34e198cb78de19f, video-monitoring, videos
Organization: Department of the Interior
Flood Video Files for Bridge Camera (Station 1), Chalk Cliffs, Colorado, USA, 2015

Chalk Cliffs, located 8 miles southwest of Buena Vista, Colorado, is one of the most active debris-flow areas in the state (U.S. Geological Survey). This "Child item" page includes videos of floods captured by one of the high-definition cameras at the monitoring site in Chalk Cliffs, CO. This camera (Bridge Camera) is located at Station 1 which is at the bridge cross section at the channel. The attached figure "station_and_camera_locations.png" provides an overview figure with the location of the two cameras and three stations along the channel. 
Video recording for all cameras is triggered using a rainfall threshold, derived from rainfall measurements from rain gauges (Michel et al., 2019). The complete videos for all the cameras are downloaded manually during site visits. More detailed information about the cameras and settings used can be found in the metadata file under “Process steps” in “Data quality information.”  
During 2015, several floods were captured by the 'Bridge Camera'. The videos for all floods captured by this camera along with the dates they were captured can be found in the attached zip files. The file names indicate "date_camera_flood."  
The following citations relate to reports that provide background information for this data release:  
Michel, A., Kean, J.W., Smith, J.B., Allstadt, K.E., Coe, J.A. (2019). Taking the pulse of debris flows: Extracting debris-flow dynamics from good vibrations in southern California and central Colorado. Debris-flow hazards mitigation: Mechanics, Monitoring, Modeling, and Assessment. http://dx.doi.org/10.25676/11124/173224    
U.S. Geological Survey Landslide Hazards Program. (2020). Chalk Cliffs, Colorado. U.S Geological Survey, https://www.usgs.gov/natural-hazards/landslide-hazards/science/chalk-cliffs-colorado?qt-science_center_objects=0#qt-science_center_objects 
Kean, J.W., Smith, J.B., and Coe, J.A., 2020, Debris-flow monitoring data, Chalk Cliffs, Colorado, USA, 2014: U.S. Geological Survey data release, https://doi.org/10.5066/P9MUWDFN

Tags: chalk-cliffs, colorado, debris-flow, flood, geologic-hazards-science-center, geomorphology, hydrology, landslide-hazards-program, landslides, usgs, usgs-5f9c3768d34e198cb78de197, video-monitoring, videos
Organization: Department of the Interior
Debris Flow Video Files for Bridge Camera (Station 1), Chalk Cliffs, Colorado, USA, 2015

Chalk Cliffs, located 8 miles southwest of Buena Vista, Colorado, is one of the most active debris-flow areas in the state (U.S. Geological Survey). This "Child item" page includes videos of debris flows captured by one of the high-definition cameras at the monitoring site in Chalk Cliffs, CO. This camera (Bridge Camera) is located at Station 1 which is at the bridge cross section at the channel.. The attached figure "station_and_camera_locations.png" provides an overview figure with the location of the two cameras and three stations along the channel. 
Video recording for all cameras is triggered using a rainfall threshold, derived from rainfall measurements from a rain gauge (Michel et al., 2019). The complete videos for all the cameras are downloaded manually during site visits. More detailed information about the cameras and settings used can be found in the metadata file under “Process steps” in “Data quality information.”  
During 2015, several debris flows were captured by the 'Bridge Camera'. The videos for all debris flows captured by this camera along with the dates they were captured can be found in the attached zip files. The file names indicate "date_camera_debrisflow." 
The following citations relate to reports that provide background information for this data release:  
Michel, A., Kean, J.W., Smith, J.B., Allstadt, K.E., Coe, J.A. (2019). Taking the pulse of debris flows: Extracting debris-flow dynamics from good vibrations in southern California and central Colorado. Debris-flow hazards mitigation: Mechanics, Monitoring, Modeling, and Assessment. http://dx.doi.org/10.25676/11124/173224 
U.S. Geological Survey Landslide Hazards Program. (2020). Chalk Cliffs, Colorado. U.S Geological Survey, https://www.usgs.gov/natural-hazards/landslide-hazards/science/chalk-cliffs-colorado?qt-science_center_objects=0#qt-science_center_objects 
Kean, J.W., Smith, J.B., and Coe, J.A., 2020, Debris-flow monitoring data, Chalk Cliffs, Colorado, USA, 2014: U.S. Geological Survey data release, https://doi.org/10.5066/P9MUWDFN.

Tags: chalk-cliffs, colorado, debris-flow, flood, geologic-hazards-science-center, geomorphology, hydrology, landslide-hazards-program, landslides, usgs, usgs-5f9c374cd34e198cb78de191, video-monitoring, videos
Organization: Department of the Interior
The distribution and structure of mangroves (Avicennia germinans and Rhizophora mangle) near a rapidly changing range limit in the northeastern Gulf of Mexico

In coastal wetlands, one of the most striking examples of climate change is the poleward range expansion of mangrove forests in response to warming winters. In North America, the Cedar Key region has often been considered the range limit for mangroves along the western coast of Florida (USA). However, within the past several decades, robust stands of Avicennia germinans and Rhizophora mangle have been observed in the Apalachicola Bay region, which is 200 km northwest of Cedar Key. This dataset characterizes the distribution and structure of the mangroves in the Apalachicola Bay area of Florida identified via extensive ground surveys and photointerpretation of aerial imagery from 2018 to 2019.

Tags: apalachicola-bay, dog-island, ecology, ecosystem-monitoring, effects-of-climate-change, saint-george-island, saint-joseph-bay, saint-vincent-island, usgs-5f9c3dced34e198cb78de1e6
Organization: Department of the Interior
Chirp sub-bottom data of USGS field activity 2017-612-FA collected in Puget Sound and Lake Washington, Washington in February of 2017

High-resolution chirp sub-bottom data were collected by the U.S. Geological Survey and the University of Washington in February of 2017 west of Seattle in Puget Sound and in Lake Washington, Washington. Data were collected aboard the University of Washington’s R/V Clifford A. Barnes during USGS field activity 2017-612-FA using an Edgetech SB-512i sub-bottom profiler. Sub-bottom acoustic penetration spans several tens of meters and is variable by location.

Tags: acoustic-methods, baby-island, bainbridge-island, ballard, bellevue, blake-island, camano-island, clinton, cmhrp, coastal-and-marine-hazards-and-resources-program, colby, distributions, edmonds, freeland, gedney-island, geophysics, geoscientificinformation, geospatial-datasets, greenbank, harbor-island, lake-washington, manchester, mapping, marine-geophysics, mercer-island, mukilteo, oceans, ohlers-island, pacific-coastal-and-marine-science-center, pcmsc, puget-sound, seabed, seismic-reflection-profiling, state-of-washington, sub-bottom-profiling, substrate, u-s-geological-survey, usgs, usgs-5f9aed21d34e198cb78b8880, vashon-island, west-seattle, whidbey-island
Organization: Department of the Interior
Multichannel boomer data of USGS field activity 2017-612-FA collected in Lake Washington, Washington in February of 2017

High-resolution multichannel boomer seismic-reflection data were collected by the U.S. Geological Survey and the University of Washington in February of 2017 east of Seattle in Lake Washington, Washington. Data were collected aboard University of Washington’s R/V Clifford A. Barnes during USGS field activity 2017-612-FA using an Applied Acoustics triple plate S-Boom sound source and recorded on a 24 channel Geometrics digital hydrophone streamer. Sub-bottom acoustic penetration spans several hundreds of meters and is variable by location.

Tags: acoustic-methods, bellevue, cmhrp, coastal-and-marine-hazards-and-resources-program, distributions, edmonds, geophysics, geoscientificinformation, geospatial-datasets, lake-washington, mapping, marine-geophysics, mercer-island, oceans, ohlers-island, pacific-coastal-and-marine-science-center, pcmsc, seabed, seattle, seismic-reflection-profiling, state-of-washington, sub-bottom-profiling, substrate, u-s-geological-survey, usgs, usgs-5f9aecf0d34e198cb78b8879
Organization: Department of the Interior
Multichannel minisparker data of USGS field activity 2017-612-FA collected in Puget Sound, Washington in February of 2017

High-resolution multichannel minisparker seismic-reflection data were collected by the U.S. Geological Survey and the University of Washington in February of 2017 west of Seattle in Puget Sound and in Lake Washington, Washington. Data were collected aboard University of Washington’s R/V Clifford A. Barnes during USGS field activity 2017-612-FA using a 500 Joule SIG 2-mille minisparker sound source and recorded on a 48 channel Geometrics digital hydrophone streamer. Sub-bottom acoustic penetration spans several hundreds of meters and is variable by location.

Tags: acoustic-methods, baby-island, bainbridge-island, ballard, bellevue, blake-island, camano-island, clinton, cmhrp, coastal-and-marine-hazards-and-resources-program, colby, distributions, edmonds, freeland, gedney-island, geophysics, geoscientificinformation, geospatial-datasets, greenbank, harbor-island, lake-washington, manchester, mapping, marine-geophysics, mercer-island, mukilteo, oceans, ohlers-island, pacific-coastal-and-marine-science-center, pcmsc, puget-sound, seabed, seismic-reflection-profiling, state-of-washington, sub-bottom-profiling, substrate, u-s-geological-survey, usgs, usgs-5f9aecc6d34e198cb78b8871, vashon-island, west-seattle, whidbey-island
Organization: Department of the Interior
R Scripts and Results of Estimated Water Use Associated with Continuous Oil and Gas Development, Permian Basin, United States, 2010–2019 (ver. 2.0, April 2022)

For more than 100 years, the Permian Basin has been an important source of oil and gas produced from conventional reservoirs; directional drilling combined with hydraulic fracturing has greatly increased production in the past 10 years to the extent that the Permian Basin is becoming one of the world’s largest continuous oil and gas (COG) producing fields (U.S. Energy Information Administration, 2020). These recent techniques extract oil and gas by directionally drilling and hydraulically fracturing the surrounding reservoir rock. The extraction of COG by using these techniques requires large volumes of water and estimates of the total water volume used in COG require a comprehensive assessment to determine the amount of water needed to extract reservoir resources. This data release contains the R scripts used to process input data (Ball and others, 2020) and the results (output data) produced by those scripts. Linear and quantile regression models of water use in relation to the number of oil and gas wells developed were fitted to the direct, indirect, and ancillary water-use categories for the Permian Basin. Confidence intervals for each parameter estimate (regression model coefficient) obtained from the linear regression models were computed as a measure of uncertainty. Together, these scripts and output data can be used to model water use associated with COG development in the Permian Basin, with estimates by individual well and by county.
In March, 2022, U.S. Geological Survey staff noticed an incorrect version of a file that was not part of the Bureau approved data release was included within this data release by mistake. The data release has been updated by replacing the incorrect version of the file with the original Bureau approved version of the file. The file in question is located within the top-level "Model.zip" directory and is the "mungeDataRelease.R" script. The incorrect file had the same name as the correct file. First release: August 2021; revised April 2022 (version 2.0). The previous version can be obtained by contacting the USGS Oklahoma-Texas Water Science Center using the "Point of Contact" link on the landing page on ScienceBase.

Tags: computational-methods, environment, new-mexico, permian-basin, regression-analysis, statistical-analysis, texas, usgs-5f9aea9ed34e198cb78b8868, visualization-methods, water-use
Organization: Department of the Interior
Digital Shoreline Analysis System version 4.1 Transects with Long-Term Rate Calculations for the Delmarva North region from Cape Henlopen, Delaware to the southern end of Assateague Island, Virginia (DelmarvaN_LT.shp)

Sandy ocean beaches are a popular recreational destination, often surrounded by communities containing valuable real estate.  Development is on the rise despite the fact that coastal infrastructure is subjected to flooding and erosion.  As a result, there is an increased demand for accurate information regarding past and present shoreline changes.  To meet these national needs, the Coastal and Marine Geology Program of the U.S. Geological Survey (USGS) is compiling existing reliable historical shoreline data along open-ocean sandy shores of the conterminous United States and parts of Alaska and Hawaii under the National Assessment of Shoreline Change project.
There is no widely accepted standard for analyzing shoreline change.  Existing shoreline data measurements and rate calculation methods vary from study to study and prevent combining results into state-wide or regional assessments.  The impetus behind the National Assessment project was to develop a standardized method of measuring changes in shoreline position that is consistent from coast to coast.  The goal was to facilitate the process of periodically and systematically updating the results in an internally consistent manner.

Tags: accretion, assateague-island, atlantic-coast, baseline, bethany-beach, chincoteague-island, cmgp, coastal-and-marine-geology-program, coastal-processes, continental-island-shore-complex, delaware, delmarva, digital-shoreline-analysis-system, dsas, effects-of-coastal-change, endpoint-rate, environment, erosion, geoscientificinformation, historic-shoreline, linear-regression-rate, maryland, mid-atlantic, national-assessment-of-shoreline-change-project, ocean-city, oceans, rehoboth-beach, shoreline, shoreline-accretion, shoreline-change-rate, shoreline-erosion, transect, u-s-geological-survey, united-states, usgs, usgs-5f99fdc2-7b96-4275-927e-b85cabd2dbd8, virginia, virginian-ecoregion, whcmsc, woods-hole-coastal-and-marine-science-center
Organization: Department of the Interior
Target-chemical concentrations, exposure activity ratios, and bioassay results for assessment of mixed-organic/inorganic chemical exposures in northeast Iowa private-well tapwater, 2018

In the United States and globally, contaminant exposure in unregulated private-well point-of-use (POU) tapwater (TW) is a recognized public health data gap and an obstacle to both risk management and homeowner decision making. To help address the lack of data on broad contaminant exposures in private-well TW from hydrologically vulnerable (alluvial or karst) aquifers in agriculturally intensive landscapes, samples were collected in 2018-2019 from 47 northeast Iowa farms and analyzed for 437 unique organic compounds, 32 inorganic constituents, 5 in vitro bioassays, and 11 microbial assays.

Tags: biota, environmental-health, groundwater, inorganic-constituents, karst-topography, microbial-constituents, organic-constituents, private-well, tap-water, tapwater, usgs-5fad56aad34eb413d5df459c
Organization: Department of the Interior
Debris-flow and Flood Video Files, Chalk Cliffs, Colorado, USA, 2015

Chalk Cliffs, located 8 miles southwest of Buena Vista, Colorado, is one of the most active debris-flow areas in the state (U.S. Geological Survey). Three stations were set up at Chalk Cliffs which are located sequentially along a channel draining the 0.3 km^2 study area. These stations are equipped with rain gauges, laser distance meters, and data loggers to record rainfall and stage data (Kean, et al., 2020). This data release includes videos of debris-flows and floods captured by high-definition cameras placed at two different locations, associated with the monitoring stations, along the study area at Chalk Cliffs during 2015.  Both cameras are located near the Upper Station (Station 1). One is located at the bridge cross section at the channel (Bridge Camera) and another on the opposite side of the basin with a broad view of the channel (Wide-angle Camera). The attached figure "station_and_camera_locations.png" provides an overview figure with the location of the two cameras and three stations along the channel. The videos and their audio are used to record information on flow type and velocity of debris flows. They can also be used to interpret how the flow characteristics, such as sediment concentration, vary with time to compare to seismic observations.
Video recording for all cameras is triggered using a rainfall threshold, derived from rainfall measurements using the rain gauges (Michel et al., 2019). The complete videos for all the cameras are downloaded manually during site visits. More detailed information about the cameras and settings used can be found in the metadata file under “Process steps” in “Data quality information.” 
During 2015, several debris flows and floods were captured by the two cameras. The videos can currently be viewed in the individual ‘Child item’ pages accessible below. The ‘Child item’ pages contain either flood or debris flow video files for each camera described above. 
The following citations relate to reports that provide background information for this data release: 
Michel, A., Kean, J.W., Smith, J.B., Allstadt, K.E., Coe, J.A. (2019). Taking the pulse of debris flows: Extracting debris-flow dynamics from good vibrations in southern California and central Colorado. Debris-flow hazards mitigation: Mechanics, Monitoring, Modeling, and Assessment. http://dx.doi.org/10.25676/11124/173224   
U.S. Geological Survey Landslide Hazards Program. (2020). Chalk Cliffs, Colorado. U.S Geological Survey, https://www.usgs.gov/natural-hazards/landslide-hazards/science/chalk-cliffs-colorado?qt-science_center_objects=0#qt-science_center_objects
Kean, J.W., Smith, J.B., and Coe, J.A., 2020, Debris-flow monitoring data, Chalk Cliffs, Colorado, USA, 2014: U.S. Geological Survey data release, https://doi.org/10.5066/P9MUWDFN.

Tags: chalk-cliffs, colorado, debris-flow, flood, geologic-hazards-science-center, geomorphology, hydrology, landslide-hazards-program, landslides, usgs, usgs-5f9c36f9d34e198cb78de18b, video-monitoring, videos
Organization: Department of the Interior