AndreaBozzo/ceres-open-data-index huggingface dataset:
AA_Q27.TIF - Aleutian Arc U.S. EEZ GLORIA sidescan-sonar data mosaic (27 of 31) (LCC, 50 m, WGS84)

During late July through September 1987 and June and July 1988 the U.S. Geological Survey (USGS) conducted four cruises to cover the U.S. Exclusive Economic Zone (EEZ) region of the Aleutian Arc. As in earlier EEZ reconnaissance surveys, the USGS utilized the GLORIA (Geological LOng-Range Inclined Asdic) sidescan-sonar system to complete the geologic mapping. The collected GLORIA data were processed and digitally mosaicked to produce continuous imagery of the seafloor. A total of 31 digital mosaics of a 3 degree by 3 degree (or smaller) area with a 50-meter pixel resolution were completed for the region.

Tags: acoustic-receivers, acoustic-reflectivity, alaska, aleutian-arc, aleutian-islands-ecoregion, aleutian-trench, amchitka-island, backscatter, bowers-basin, bowers-ridge, cmgp, coastal-and-marine-geology-program, continental-island-slope, distributions, eez, exclusive-economic-zone, exclusive-economic-zone-eez, geological-long-range-inclined-asdic, geoscientificinformation, geotiff-image, gloria, gloria-gt-geological-long-range-inclined-asdic, grey-scale-image, image-mosaics, imagerybasemapsearthcover, infobank-identifier-f-2-87-aa, infobank-identifier-f-3-87-aa, infobank-identifier-f-7-88-aa, infobank-identifier-f-8-88-aa, marine-basin-floor, marine-geology, marine-geophysics, marine-oceanic, ocean-gt-pacific-ocean, ocean-gt-pacific-ocean-gt-north-pacific-ocean, ocean-gt-pacific-ocean-gt-north-pacific-ocean-gt-aleutian-arc, oceans, oceans-gt-ocean-acoustics-gt-acoustic-reflectivity, physical-habitats-and-geomorphology, sea-floor-acoustic-reflectivity, sea-floor-characteristics, seabed, side-scan-sonar, sidescan-sonar, sidescan-sonar-mosaic, stalemate-ridge, tectonic-trench, u-s-geological-survey, usgs, usgs-e4f5be65-b03a-42bd-a28f-1c001bab02d8, wcmg, western-coastal-and-marine-geology, zodiac-fan
Organization: Department of the Interior
Archive of Datasonics SIS-1000 Chirp Subbottom Data Collected During USGS Cruise DIAN 96040 Long Island, NY Inner Shelf -- Fire Island, NY, 4-24 September, 1996

This DVD-ROM contains digital high resolution seismic reflection data
collected during the USGS DIAN 96040 cruise. The coverage is the nearshore
of Long Island, NY in the vicinity of Fire Island. The seismic-reflection
data are stored as SEG-Y standard format that can be read and manipulated
by most seismic-processing software. Much of the information specific to
the data are contained in the headers of the SEG-Y format files. The file
system format is ISO 9660 which can be read with DOS, Unix, and MAC
operating systems with the appropriate DVD-ROM driver software installed.

Tags: atlantic-ocean, chirp, datasonics-sis-1000, distributions, dvd, field-activity-96040, fire-island, geoscientificinformation, long-island-inner-shelf, marine-geophysics, new-york, north-america, ny, oceans, seg-y, seismic-reflection, seismic-reflection-methods, seismic-reflection-profiling, sub-bottom-profiling, substrate, u-s-geological-survey, united-states, usgs, usgs-e4f3b1d5-2349-41c3-bedd-c5afe444e6f4
Organization: Department of the Interior
USGS CoastCam at Isla Verde, Puerto Rico: 2018-2019 Timestack Imagery and Coordinate Data

A digital video camera was installed at Isla Verde Beach in San Juan, Puerto Rico (PR) and faced northeast along the beach. Every hour during daylight hours, daily from February 1, 2019, to July 15, 2019, the camera collected raw video and produced snapshots and time-averaged image products. One such product is a "runup timestack". Runup timestacks are images created by sampling a cross-shore array of pixels from an image through time as waves propagate towards and run up a beach. Runup timestacks store the red, green, and blue or monochrome pixel intensity as a function of the cross-shore position as imagery for the sampling period, typically around 10 minutes. The images included in this data release were collected from February 8, 2019, to February 23, 2019. The camera is part of a U.S. Geological Survey (USGS) research project to study the beach and nearshore environment. USGS researchers analyzed the timestack imagery collected from this camera to remotely sense information such as the elevation of wave runup. This camera is part of the USGS CoastCam network, supported by the Total Water Level/Coastal Change Project under the Coastal and Marine Hazards and Resources Program (CMHRP). To learn more about this specific camera visit https://www.usgs.gov/centers/pcmsc/science/using-video-imagery-study-wave-dynamics-isla-verde.

Tags: balneario-isla-verde, cmhrp, coastal-and-marine-hazards-and-resources-program, coastal-processes, coastcam, commonwealth-of-puerto-rico, ecosystem-management, el-alambique-beach, environment, field-methods, geomorphology, geoscientificinformation, image-analysis, image-collections, isla-verde-beach, island-of-puerto-rico, ocean-sciences, optical-methods, pacific-coastal-and-marine-science-center, pcmsc, photography, remote-sensing, runup, total-water-level, u-s-geological-survey, usgs, usgs-e4e2578b-4f2d-4ec7-825b-4070e0060d6c, video-monitoring
Organization: Department of the Interior
COW_Q22.TIF - U.S. Pacific West Coast EEZ GLORIA sidescan-sonar data mosaic (22 of 36) (TM, 50 m, NAD27)

In March 1983, President Ronald Reagan signed a proclamation establishing an Exclusive Economic Zone (EEZ) of the United States extending its territory 200 nautical miles from the coasts of the United States, Puerto Rico, the Northern Mariana Islands, and the U.S. territories and possessions. In 1984, the U.S. Geological Survey (USGS), Office of Marine Geology began a program to map these areas of the EEZ. The U.S. Pacific Coast was the first EEZ region to be mapped and launched GLORIA (Geological LOng-Range Inclined Asdic) mapping program. The area covered by this survey extended from the Mexican to the Canadian borders and from the continental shelf edge, at about the 400-meter bathymetric contour, to 200 nautical miles from the coast. Survey of the U.S. Pacific West Coast EEZ was completed in four consecutive cruises conducted from late April through mid-August 1984. The collected GLORIA data were processed and digitally mosaicked to produce continuous imagery of the seafloor. A total of 36 digital mosaics of an approximate 2 degree by 2 degree (or smaller) area with a 50-meter pixel resolution were completed for the region.

Tags: abyssal-submarine-fan, acoustic-receivers, acoustic-reflectivity, arguello-canyon, arguello-fan, backscatter, baja-seamount-province, blanco-fracture-zone, borderland, california, cascadia-channel, cmgp, coastal-and-marine-geology-program, continental-island-rise, continental-island-slope, coos-bay, delgada-fan, delgado-fan, distributions, eez, escanaba-trough, exclusive-economic-zone, exclusive-economic-zone-eez, farallon-fan, geological-long-range-inclined-asdic, geoscientificinformation, geotiff-image, gloria, gloria-gt-geological-long-range-inclined-asdic, gorda-basin, gorda-escarpment, gorda-plate, gorda-ridge, grey-scale-image, image-mosaics, imagerybasemapsearthcover, infobank-identifier-f-1-84-sc, infobank-identifier-f-2-84-nc, infobank-identifier-f-3-84-nc, infobank-identifier-f-4-84-wo, juan-de-fuca-plate, juan-de-fuca-ridge, marine-basin-floor, marine-geology, marine-geophysics, marine-oceanic, mendocino-canyon, mendocino-channel, mendocino-fracture-zone, monterey-canyon, monterey-fan, murray-fracture-zone, nitinat-fan, northern-california-ecoregion, ocean-gt-pacific-ocean, ocean-gt-pacific-ocean-gt-north-pacific-ocean, oceans, oceans-gt-ocean-acoustics-gt-acoustic-reflectivity, oregon, oregon-washington-vancouver-coast-and-shelf-ecoregion, pacific-plate, physical-habitats-and-geomorphology, point-arena, point-conception, san-diego-trough, san-lucia-escarpment, san-pedro-trough, santa-monica-trough, sea-floor-acoustic-reflectivity, sea-floor-characteristics, seabed, side-scan-sonar, sidescan-sonar, sidescan-sonar-mosaic, southern-california-bight-ecoregion, taney-seamounts, u-s-geological-survey, u-s-pacific-west-coast, usgs, usgs-e4d8ca58-39e9-42e4-9cac-390cfd644a3d, washington, wcmg, western-coastal-and-marine-geology
Organization: Department of the Interior
RES2DINV Format Continuous Resistivity Profiles Collected in the Neuse River, April 20, 2004

The Neuse River Estuary in North Carolina is a broad, V-shaped water body located on the southwestern end of Pamlico Sound. This estuary suffers from severe eutrophication for which several water quality models have recently been developed to aid in the management of nutrient loading to the estuary. In an effort to help constrain model estimates of the fraction of nutrients delivered by direct ground-water discharge, continuous resistivity profile (CRP) measurements were made during the spring of 2004 and 2005. CRP is used to measure electrical resistivity of sediments, a property that is sensitive to difference in salinity of submarine ground water. The 2004 and 2005 surveys used floating resistivity streamers of 100 m and 50 m respectively. The depth penetration of the streamers is approximately 20% of the streamer length which translates to approximately 20-25 m with the 100 m streamer and 12-14 m with the 50 m streamer. These data were processed using AGI's EarthImager 2D software. CRP data enables the mapping of the extent and depth of the fresher ground water within the estuary.

Tags: cmgp, coastal, coastal-and-marine-geology-program, continuous-resistivity-profiling, crp, ground-water, marine-resistivity, navigational-data, neuse-river, north-america, north-carolina, of-2005-1306, open-file-report, pamlico-sound, submarine-ground-water, u-s-geological-survey, united-states, usgs, usgs-e4aafe04-22d7-43fd-a92b-28bd0c12077d, woods-hole-science-center
Organization: Department of the Interior
Depth-colored hillshade image of bathymetry data collected by the U.S. Geological Survey and the National Oceanic and Atmospheric Administration offshore of Massachusetts between Duxbury and Hull with data gaps (DH_bathyhlshd_wgaps, Depth-colored Hillshade GeoTIFF, UTM Zone 19, WGS84)

These data were collected under a cooperative agreement with the Massachusetts Office of Coastal Zone Management (CZM) and the U.S. Geological Survey (USGS), Coastal and Marine Geology Program, Woods Hole Science Center (WHSC). Initiated in 2003, the primary objective of this program is to develop regional geologic framework information for the management of coastal and marine resources. Accurate data and maps of sea-floor geology are important first steps toward protecting fish habitat, delineating marine resources, and assessing environmental changes due to natural or human impacts. The project is focused on the inshore waters (5-30 m deep) of Massachusetts between the New Hampshire border and Cape Cod Bay. Data collected for the mapping cooperative have been released in a series of USGS Open-File Reports (http://woodshole.er.usgs.gov/project-pages/coastal_mass/html/current_map.html). This spatial dataset is from the study area located between Duxbury and Hull Massachusetts, and consists of high-resolution geophysics (bathymetry, backscatter intensity, and seismic reflection) and ground validation (sediment samples, video tracklines and bottom photographs). The data were collected during four separate surveys conducted between 2003 and 2007 (NOAA survey H10993 in 2003, USGS-WHSC survey 06012 in 2006, and USGS-WHSC surveys 07001 and 07003 in 2007) and cover more than 200 square kilometers of the inner continental shelf.

Tags: 2003, 2006, 2007, atlantic-ocean, bathymetry, boston-south-shore, brant-rock, cape-cod-bay, cmgp, coastal-and-marine-geology-program, computational-methods, duxbury-bay, duxbury-beach, geoscientificinformation, geospatial-datasets, geotiff, hull-bay, imagerybasemapsearthcover, interferometric-sonar, interferometry, marine-geology, marine-geophysics, marshfield, massachusetts, massachusetts-bay, multibeam-bathymetry, multibeam-sonar, nantasket-beach, noaa-hydrographic-survey-registry-number-h10993, noaa-launch-1005, noaa-launch-1014, noaa-ship-thomas-jefferson, north-america, oceans, r-v-megan-t-miller, r-v-rafael, reson-8101, reson-8125, scituate, sea-floor-characteristics, sea-submetrix, sea-swathplus, seafloor, swath-bathymetry, u-s-geological-survey, united-states, usgs, usgs-e7c83112-e332-4805-b862-9981f4a99f6f, whsc, whsc-field-activity-serial-number-06012, whsc-field-activity-serial-number-07001, woods-hole-science-center
Organization: Department of the Interior
High Plains aquifer (SUPERCEDED)

This data set represents the extent of the High Plains aquifer in the states of South Dakota, Wyoming, 
Nebraska, Colorado, Kansas, New Mexico, Oklahoma, and Texas. This aquifer extent has been 
superceded by DS543 https://water.usgs.gov/GIS/metadata/usgswrd/XML/ds543.xml

Tags: aquifer, aquifer-extent, colorado, environment, geoscientificinformation, groundwater, inlandwaters, kansas, nebraska, new-mexico, oklahoma, south-dakota, texas, usgs-e459c09f-0779-4b90-9357-5915499c36c5, wyoming
Organization: Department of the Interior
Specific Water Quality Sites for Sanjuan County, Utah

This map shows specific water-quality items and hydrologic data site
information which come from QWDATA (Water Quality) and GWSI (Ground
Water Information System). Both QWDATA and GWSI are subsystems of
NWIS (National Water Inventory System)of the USGS (United States
Geologic Survey).
		
This map is for San Juan County, Utah.
		
The scope and purpose of NWIS is defined on the web site:
		
http://water.usgs.gov/public/pubs/FS/FS-027-98/

Tags: alkalinity, ammonia, ammonia-unionize, dissolved-solids, environment, flow-rate, geoscientificinformation, hardness, hardness-total, inlandwaters, nitrogen, nitrogen-nitrate, ph, quality, san-juan, san-juan-county, specific-conductance, state-of-utah, usgs-e42c6861-24d1-4f07-af35-fb5589d4c609, utah, water, water-level, water-quality, water-quality-site, water-temperature
Organization: Department of the Interior
Specific Water Quality Sites for Summit County, Utah

This map shows specific water-quality items and hydrologic data site
information which come from QWDATA (Water Quality) and GWSI (Ground
Water Information System). Both QWDATA and GWSI are subsystems of
NWIS (National Water Inventory System)of the USGS (United States
Geologic Survey).
		
This map is for Summit County, Utah.
		
The scope and purpose of NWIS is defined on the web site:
		
http://water.usgs.gov/public/pubs/FS/FS-027-98/

Tags: alkalinity, ammonia, ammonia-unionize, dissolved-solids, environment, flow-rate, geoscientificinformation, hardness, hardness-total, inlandwaters, nitrogen, nitrogen-nitrate, ph, quality, specific-conductance, state-of-utah, summit, summit-county, usgs-e42778f6-9dcd-4d89-a01d-d93cd9ecb960, utah, water, water-level, water-quality, water-quality-site, water-temperature
Organization: Department of the Interior
Archive of Boomer Seismic Reflection Data Collected on USGS Cruise 99LCA01, Crescent Beach Spring, Florida, 26 April - 27 April, 1999.

This report consists of two-dimensional marine seismic reflection profile data from Crescent Beach Spring, Florida.
These data were acquired in April of 1999 with the Research Vessel G.K. Gilbert. The data are available in a variety of formats, including binary, ASCII, HTML, and GIF images. Binary data are in Society of Exploration Geophysicists (SEG) SEG-Y format and may be downloaded for further processing or display. Trackline maps and GIF images of the profiles may be viewed with your WWW browser.
For more information on the seismic surveys see http://walrus.wr.usgs.gov/infobank/g/g199fl/html/g-1-99-fl.meta.html
These data are also available via GeoMapApp (http://www.geomapapp.org/) and Virtual Ocean ( http://www.virtualocean.org/) earth science exploration and visualization applications.

Tags: 99lca01, anastasia-island, boomer, crescent-beach, crescent-beach-spring, distributions, florida, iso-9660-cd-rom, marine-geophysics, marine-seismic-reflection, seg-y, seismic-reflection, seismic-reflection-methods, sub-bottom-profiling, substrate, usgs-e4277494-d38c-44f0-8045-7403b9583b9f
Organization: Department of the Interior
Archive of Chirp Subbottom Profile Data Collected in 2018 from the Northern Chandeleur Islands, Louisiana

From August 16 to 21, 2018, the U.S. Geological Survey (USGS) conducted a geophysical survey to investigate the geologic controls on barrier island evolution and medium-term and interannual sediment transport along the sand berm constructed in 2011 (offshore, at the northern end of the Chandeleur Islands, Louisiana) as mitigation of the Deepwater Horizon oil spill. This investigation is part of a broader USGS project, which seeks to better understand barrier island evolution over medium time scales (months to years). This publication serves as an archive of unprocessed, digital chirp subbottom data, survey trackline map, navigation files, geographic information system (GIS) data, and formal Federal Geographic Data Committee (FGDC) metadata. Processed subbottom profile images are also provided. The archived trace data are in standard Society of Exploration Geophysicists (SEG) SEG Y revision 0 format (Barry and others, 1975) and may be downloaded and processed with commercial or public domain software such as Seismic Unix (SU).
These data are available for viewing using GeoMapApp (http://www.geomapapp.org/) and Virtual Ocean (http://www.virtualocean.org/) multi-platform open source software. In addition, the SEG Y files can be downloaded from the USGS Coastal and Marine Geoscience Data System (CMGDS, https://cmgds.marine.usgs.gov).

Tags: 2018-350-fa, barrier-island-mapping, chandeleur-islands, chirp, coastal-processes, distributions, geology, geoscientificinformation, gulf-of-mexico, louisiana, marine-geology, oceans, physical-habitats-and-geomorphology, seg-y, seismic-reflection, seismic-reflection-profiling, society-of-exploration-geophysicists, sub-bottom-profiling, united-states, usgs-e421d0d8-c5ca-46de-bcc4-4b6a12f1371c
Organization: Department of the Interior
Wetted channel and bar features for the Tillamook, Trask, Wilson, Kilchis, and Miami Rivers, Oregon in 1967

The Tillamook Bay subbasins and Nehalem River basins encompass 1,369 and 2,207 respective 
square kilometers of northwestern Oregon and drain to the Pacific Ocean. The Tillamook, Trask, 
Wilson, Kilchis, and Miami Rivers flow into Tillamook Bay near the towns of Tillamook and Garibaldi. 
The Wilson and Trask River basins cover the largest areas (500 and 451 square kilometers, 
respectively) whereas the Tillamook and Kilchis Rivers encompass similar sized areas (156 and 
169 square kilometers, respectively) and the Miami River the smallest area (94 square kilometers). 
In cooperation with the U.S. Army Corps of Engineers, the U.S. Geological Survey completed a 
reconnaissance-level assessment of channel condition and bed-material transport relevant to the 
permitting of in-stream gravel extraction along the the major alluvial portions of six river systems, 
including the lowermost 14.1 km of the Tillamook River, 16.3 km of the Trask River, 15.2 km of 
the Wilson River, 7.8 km of the Kilchis River, 11.6 km of the Miami River, and 31.4 km of the 
Nehalem River. To support these analyses, digital channel maps were produced to depict channel 
and floodplain conditions in the Tillamook Bay sub-basins and Nehalem River basin from different 
time periods. GIS layers defining the wetted channel and bar features and channel centerline in 
the study area were developed for four time periods: 1939, 1967, 2005, and 2009. For this project, 
the active channel was defined as area typically inundated during annual high flows, and includes 
the low-flow channel as well as side channels, islands, and channel-flanking gravel bars. The wetted 
channel and bar feature datasets were developed by digitizing from aerial photographs. Aerial 
photographs from 1939 and 1967 were scanned, rectified, and mosaicked for this project (See 
metadata for each photograph set for more information on the rectification process and resolution 
of each dataset). Digital orthophotographs from 2005 and 2009 are publicly available.

Tags: channel-stability, environment, fluvial-geomorphology, geoscientificinformation, historical-channel-change, inlandwaters, kilchis-river, miami-river, nehalem-bay, nehalem-river, oregon-coast-range, sediment-transport, tillamook-bay, tillamook-county, tillamook-river, trask-river, usgs-e412a289-35cb-40f4-8200-b0ca5c9b9575, wilson-river
Organization: Department of the Interior
Raw Continuous Resistivity Profiles from Cape Cod National Seashore, Feb. 28, 2006

Continuous resistivity profiling (CRP) surveys were conducted at Cape Cod National Seashore in 2004 and 2006 in order to test hypotheses about groundwater flow under and into estuaries and the Atlantic Ocean. Coastal resource managers here and elsewhere are concerned about nutrients that are entering coastal waters via submarine groundwater discharge, which are contributing to eutrophication and harmful algal blooms. CRP is used to measure electrical resistivity of sediments, a property that is sensitive to differences in salinity of submarine ground water. The 2004 and 2006 surveys used floating resistivity streamers of 100 m and 50 m respectively. The depth penetration of the streamers is approximately 20% of the streamer length which translates to approximately 20-25 m with the 100 m streamer and 12-14 m with the 50 m streamer. These data were processed using AGI's EarthImager 2D software.

Tags: atlantic-ocean, cape-cod, cmgp, coastal-and-marine-geology-program, continuous-resistivity-profiling, crp, geoscientificinformation, ground-water, inlandwaters, location, massachusetts, nauset-marsh, navigational-data, north-america, oceans, of-2006-1169, open-file-report, salt-pond, submarine-ground-water, u-s-geological-survey, united-states, usgs, usgs-e3d8efd6-dfc0-4dd5-a387-8fc593472a31, whsc-field-activity-serial-number-06007, woods-hole-science-center
Organization: Department of the Interior
Digital data sets that describe aquifer characteristics of the Central Oklahoma aquifer in central Oklahoma

This data set consists of digitized polygons of a constant
hydraulic conductivity value for the Central Oklahoma aquifer
in central Oklahoma. This area encompasses all or part of
Cleveland, Lincoln, Logan, Oklahoma, Payne, and Pottawatomie
Counties. The Central Oklahoma aquifer includes the alluvial
and terrace deposits along major streams, the Garber
Sandstone and Wellington Formations, and the Chase, Council
Grove, and Admire Groups. The Quaternary-age alluvial and
terrace deposits consist of unconsolidated clay, silt, sand,
and gravel.
The hydraulic conductivity data set was created from digital
data sets developed to produce a map for a previously
published report. The hydraulic conductivity of the alluvial
and terrace deposits are not included in this data set. This
data set represents the hydraulic conductivities of only the
sandstone units in the Garber Sandstone and Wellington
Formations and the Chase, Council Grove, and Admire Groups.
The median hydraulic conductivity of the sandstones in the
Garber Sandstone and Wellington Formations and the Chase,
Council Grove, and Admire Groups, calculated from specific
capacity data, is 4.5 feet per day The contact between the
Wellington Formation and the Chase, Council Grove, and Admire
Groups was included in this data set because the median
percentage of sandstone in the Chase, Council Grove, and
Admire Groups is 43 percent of the median sandstone
percentage of the Garber Sandstone and Wellington
Formations. The hydraulic conductivity values for the other
rock units, such as the siltstone, mudstone, shale, and
limestone, in the Garber Sandstone and Wellington Formations
and the Chase, Council Grove, and Admire Groups were not
reported.

Tags: admire-group, aquifers, central-oklahoma-aquifer, chase-group, council-grove-group, environment, garber-sandstone, geoscientificinformation, ground-water, ground-water-vulnerability, groundwater, groundwater-vulnerability, hydraulic-conductivity, inlandwaters, usgs-e3cd0a9a-ddbf-42a7-aee2-d1cebe03fdb7, wellington-formation
Organization: Department of the Interior