AndreaBozzo/ceres-open-data-index huggingface dataset:
14BIM01_IFB_xyz: Interferometric Swath Bathymetry XYZ Data Collected in 2014 Near Breton Island, Louisiana

As part of the Barrier Island Monitoring Project, scientists from the U.S. Geological Survey (USGS) St. Petersburg Coastal and Marine Science Center conducted nearshore geophysical surveys off Breton and Gosier Islands, Louisiana, in July and August of 2014. To assist the United States Fish and Wildlife Service (USFWS) with restoration planning efforts, the USGS was tasked with answering fundamental questions about the physical environment of the southern Chandeleur Islands, including the geology, morphology, and oceanography. Baseline data needed to answer these questions was either insufficient or missing in the area.  The USGS conducted a comprehensive geologic investigation in the summer of 2014 by collecting geophysical and sedimentological data.
Breton Island, located at the southern end of the Chandeleur Island chain, Louisiana, was recognized as a natural and globally important nesting sanctuary for several bird species and was established as the Breton National Wildlife Refuge (NWR) in 1904.  The aerial extent of Breton Island has diminished 90% since 1920.  Land loss is attributed to ongoing relative sea-level rise, diminished sediment supply, and storm impacts.  The bird population on Breton Island has also declined over the years, most notably after Hurricane George in 1998 and Hurricane Katrina in 2015, which completely submerged the island.  Despite the decreasing habitable acreage, migratory seabirds continue to return and utilize Breton Island.  To prevent the island from being completely submerged in the future and to protect, stabilize, and provide more nesting and foraging areas for the birding population, the USFWS is proposing a restoration effort to rebuild Breton Island to its pre-Katrina footprint.
This Data Series serves as an archive of processed interferometric-swath, single-beam bathymetry, and side-scan sonar data collected in the nearshore of Breton and Gosier Islands, NWR, Louisiana.  The data were collected during two USGS cruises (USGS Field Activity Numbers 2014-314-FA and 2014-317-FA) in July and August 2014. Geographic Information System data products include a 100 meter-cell-size interpolated bathymetry grid surface, trackline maps, and point data files. Additional files include error analysis maps, Field Activity Collection System logs, and formal Federal Geographic Data Committee (FGDC) metadata.

Tags: 14bim01, 2014-314-fa, barrier-island-evolution-research-project, barrier-island-mapping, bathymetry, breton-island, breton-national-wildlife-refuge, chandeleur-islands, chandeleur-sound, cmgp, coastal-and-marine-geology-program, datum, elevation, geophysical, geoscientificinformation, gosier-islands, gulf-of-mexico, hydrography, ifb, imagerybasemapsearthcover, interferometry, location, louisiana, marine-geology, oceans, sea, shoreline, spcmsc, st-petersburg-coastal-and-marine-science-center, swath, swathplus-h, systems-engineering-and-assessment, u-s-geological-survey, usgs, usgs-c27a90ae-05a2-482a-8574-01256e9e5d87, water
Organization: Department of the Interior
Hydrologic Data Sites for Wayne County, Utah

This map shows the USGS (United States Geologic Survey), NWIS (National
Water Inventory System) Hydrologic Data Sites for Wayne 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: altitude, environment, estuary, geoscientificinformation, hole-depth, hydrologic-data-site, inlandwaters, lake, reservoir, spring, state-of-utah, stream, usgs-c94d8f9f-dead-4049-bd85-cd3a352b295a, utah, water-use, wayne, wayne-county, well, well-depth
Organization: Department of the Interior
Aerial photo mosaic of the Bridge Reach, Middle Fork Coquille River, Oregon in 1939

The Coquille River system is an unregulated system that encompasses 2,745 square kilometers of southwestern 
Oregon and flows into the Pacific Ocean near the town of Bandon, Oregon. Beginning in the Rogue River-Siskiyou National Forest, 
the South Fork Coquille River gains the Middle Fork Coquille River (drainage area 798 square kilometers) and shortly thereafter the 
North Fork Coquille River (749 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 South Fork Coquille River from river kilometer (RKM) 115.4 near its confluence with Upper Land Creek 
to RKM 58.5 at its confluence with the North Fork Coquille River, the mainstem Coquille River from RKM 58.5 at the confluence of the 
South and North Forks of the Coquille River to its mouth, the Middle Fork Coquille River from RKM 15.4 to its confluence with the 
South Fork Coquille River, and the North Fork Coquille River from RKM 14.6 to its confluence with the South Fork Coquille River. To 
support these analyses, digital channel maps were produced to depict channel and floodplain conditions in the Coquille River basin 
from different time periods. GIS layers defining the wetted channel and bar features and channel centerline of Hunter Creek 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: aerial-photograph, channel-stability, coos-county, coquille-river, curry-county, environment, fluvial-geomorphology, geoscientificinformation, historical-channel-change, inlandwaters, middle-fork-coquille-river, north-fork-coquille-river, oregon-coast-range, sediment-transport, south-fork-coquille-river, usgs-c9045936-bc98-48de-b5f8-e19454f21ee3
Organization: Department of the Interior
JI_250M_LCC_WGS84.TIF - Johnston Atoll U.S. EEZ GLORIA sidescan-sonar composite mosaic (LCC, 250 m, WGS84)

In 1984, the U.S. Geological Survey (USGS), Office of Marine Geology, launched a program using the Geological LOng-Range Inclined Asdic (GLORIA) sidescan-sonar system to study the entire U.S. Exclusive Economic Zone (EEZ). From December 1990 through February 1991, the USGS and IOS (Institute of Oceanographic Sciences, U.K.) scientists conducted three surveys within the Johnston Atoll U.S. EEZ surrounding Johnston Island. The surveys during that time period, and conducted in succession from 6 December 1990 to 21 February 1991, focused on the U.S. Exclusive Economic Zone surrounding the Johnston Atoll. The results of these surveys were 16 digital mosaics of approximately a 2 degree by 2 degree area with a 50-meter pixel resolution.

Tags: acoustic-receivers, acoustic-reflectivity, akau-island, backscatter, central-pacific-ocean, cmgp, coastal-and-marine-geology-program, distributions, eez, exclusive-economic-zone, exclusive-economic-zone-eez, field-activity-number-f-1-91-cp, field-activity-number-f-13-90-cp, field-activity-number-f-2-91-cp, geological-long-range-inclined-asdic, geoscientificinformation, geotiff-image, gloria, gloria-gt-geological-long-range-inclined-asdic, grey-scale-image, hawaii-ecoregion, hikina-island, image-mosaics, imagerybasemapsearthcover, johnston-atoll-eez, johnston-atoll-exclusive-economic-zone, johnston-island, marine-basin-floor, marine-geology, marine-geophysics, marine-oceanic, ocean-gt-pacific-ocean, ocean-gt-pacific-ocean-gt-central-pacific-ocean, oceans, oceans-gt-ocean-acoustics-gt-acoustic-reflectivity, physical-habitats-and-geomorphology, sand-island, sea-floor-acoustic-reflectivity, sea-floor-characteristics, seabed, side-scan-sonar, sidescan-sonar, sidescan-sonar-mosaic, u-s-geological-survey, usgs, usgs-c9010756-a57a-40f3-9ea1-53fa3554600b, wcmg, western-coastal-and-marine-geology
Organization: Department of the Interior
Chirp Seismic Shotpoint Navigation every 100 shots in Geographic Coordinates - Lake Mead Survey 2001

Lake Mead is a large interstate reservoir located in the Mojave Desert of southeastern Nevada and northwestern Arizona.  It was impounded in 1935 by the construction of Hoover Dam and is one of a series of multi-purpose reservoirs on the Colorado River.  The lake extends 183 km from the mouth of the Grand Canyon to Black Canyon, the site of Hoover Dam, and provides water for residential, commercial, industrial, recreational, and other non-agricultural users in communities across the southwestern United States.  Extensive research has been conducted on Lake Mead, but a majority of the studies have involved determining levels of anthropogenic contaminants such as synthetic organic compounds, heavy metals and dissolved ions, furans/dioxins, and nutrient loading in lake water, sediment, and biota (Preissler, et al., 1998; Bevans et al, 1996; Bevans et al., 1998; Covay and Leiker, 1998; LaBounty and Horn, 1997; Paulson, 1981).  By contrast, little work has focused on the sediments in the lake and the processes of deposition (Gould, 1951).  To address these questions, sidescan-sonar imagery and high-resolution seismic-reflection profiles were collected throughout Lake Mead by the USGS in cooperation with researchers from University of Nevada Las Vegas (UNLV).  These data allow a detailed mapping of the surficial geology and the distribution and thickness of sediment that has accumulated in the lake since the completion of Hoover Dam.  Results indicate that the accumulation of post-impoundment sediment is primarily restricted to former river and stream beds that are now submerged below the lake while the margins of the lake appear to be devoid of post-impoundment sediment.  The sediment cover along the original Colorado River bed is continuous and is typically greater than 10 m thick through much of its length.  Sediment thickness in some areas exceeds 35 m while the smaller tributary valleys typically are filled with less than 4 m of sediment.  Away from the river beds that are now covered with post-impoundment sediment, pre-impoundment alluvial deposits and rock outcrops are still exposed on the lake floor.

Tags: boulder-basin, chirp, cmgp, coastal-and-marine-geology-program, cruise-serial-number-01007, geophysics, geospatial-datasets, gregg-basin, hoover-dam, inlandwaters, lake-mead, location, mojave-desert, navigation, navigational-data, nevada, north-america, ofr03-320, open-file-report, overton-arm, seismic, seismic-reflection, shotpoint, sis-1000, subbottom, u-s-geological-survey, united-states, usgs, usgs-c8f0b556-3bca-47ab-8415-729f37453c8b, virgin-basin, woods-hole-field-center
Organization: Department of the Interior
Single-Beam Bathymetry Sounding Data of Cape Canaveral, Florida, (2014) gridded in ESRI ASCII GRID format

The Cape Canaveral Coastal System (CCCS) is a prominent feature along the Southeast U.S. coastline and is the only large cape south of Cape Fear, North Carolina. Most of the CCCS lies within the Merritt Island National Wildlife Refuge and included in its boundaries are the Cape Canaveral Air Force Station (CCAFS), NASA’s Kennedy Space Center (KSC), and a large portion of Canaveral National Seashore. The actual promontory of the modern cape falls within the jurisdictional boundaries of the CCAFS. These various agencies have ongoing concerns related to erosion hazards and vulnerability of the system including critical infrastructure, habitats, and recreational and cultural resources.
The USGS conducted a bathymetric mapping survey August 18-20, 2014, in the Atlantic Ocean offshore of Cape Canaveral, Florida (USGS Field Activity Number 2014-324-FA). The study area covered an area extending south from Port Canaveral, Florida, to the northern end of the KSC property and from the shoreline to about 2.5 km offshore. Bathymetric data were collected with single-beam sonar- and lidar-based systems. Two jet skis and a 17-ft outboard motor boat equipped with the USGS SANDS hydrographic system collected precision sonar data. The sonar operations were conducted in three missions, one on each day, with the boat and jet skis operating concurrently. The USGS airborne EAARL-B mapping system flown in a twin engine plane was used to collect lidar data. The lidar operations were conducted in three missions, one in the afternoon of August 19, 2015, and two more in the morning and afternoon of August 20, 2014. The missions were synchronized such that there was some temporal and spatial overlap between the sonar and lidar operations. Additional data were collected to evaluate the actual water clarity corresponding to lidar's ability to receive bathymetric returns.
This dataset serves as an archive of processed single-beam and lidar bathymetry data collected at Cape Canaveral, Florida, in 2014 (in XYZ comma delimited, ASCII and shapefile format). Also included in this archive are Geographic Information System (GIS) data products: gridded map data (in ESRI binary and ASCII grid format), and a color-coded bathymetry map (in PDF format).

Tags: atlantic-ocean, bathymetry, cape-canaveral, cape-canaveral-air-force-station, cape-canaveral-coastal-system, circulation-model, cmgp, coastal-and-marine-geology-program, earrl-b, echosounder, elevation, environment, erosion, fl, florida, geoscientificinformation, hydrography, hydrology, imagerybasemapsearthcover, inlandwaters, kennedy-space-center, lidar, mapping, merritt-island-national-wildlife-refuge, oceans, port-canaveral, sands, second-generation-experimental-advanced-airborne-research-lidar, sediment-dynamics, single-beam, soundings, spcmsc, st-petersburg-coastal-and-marine-science-center, system-for-accurate-nearshore-depth-surveying, transect-viewer, u-s-geological-survey, united-states, us, usgs, usgs-c8ed933e-305f-40e8-9627-df37867801a7, water-depth
Organization: Department of the Interior
Video transects of the sea floor on Stellwagen Bank during U.S. Geological Survey field activity 2015-074-FA, aboard the R/V Auk, December 1, 2015

This field activity is 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. This cruise 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 21 locations on Stellwagen Bank at which 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.

Tags: atlantic-ocean, cmhrp, coastal-and-marine-hazards-and-resources-program, location, marine-geology, massachusetts, massachusetts-bay, national-oceanic-and-atmospheric-administration, navigation, navigational-data, noaa, north-america, oceans, polyline-shapefile, sbnms, seabed-observation-and-sampling-system, seaboss, stations, stellwagen-bank, stellwagen-bank-national-marine-sanctuary, trackline, u-s-geological-survey, united-states, usgs, usgs-c91ea6df-2008-4ba1-844b-a2d71e057a78, video, video-observation, videography, videos, whcmsc, woods-hole-coastal-and-marine-science-center
Organization: Department of the Interior
Crocker Reef, Florida, 2016-2017 Seafloor Elevation Stability Models, Maps, and Tables

The U.S. Geological Survey (USGS) St. Petersburg Coastal and Marine Science Center (SPCMSC) conducted research to identify areas of seafloor elevation stability and instability based on elevation changes between the years of 2016 and 2017 at Crocker Reef near Islamorada, Florida (FL), within a 33.62 square-kilometer area. USGS SPCMSC staff used seafloor elevation-change data from Yates and others (2019) derived from an elevation-change analysis between two elevation datasets acquired in 2016 and 2017 using the methods of Yates and others (2017). A seafloor stability threshold was determined for the 2016-2017 Crocker Reef elevation-change dataset based on the vertical uncertainty of the 2016 and 2017 digital elevation models (DEMs). Five stability categories (which include, Stable: 0.0 meters (m) to ±0.24 m or 0.0 m to ±0.49 m; Moderately stable: ±0.25 m to ±0.49 m; Moderately unstable: ±0.50 m to ±0.74 m; Mostly unstable: ±0.75 m to ±0.99 m; and Unstable: ±1.00 m to Max/Min elevation change) were created and used to define levels of stability and instability for each elevation-change value (8,402,223 data points at 2-m horizontal resolution) based on the amount of erosion and accretion during the 2016 to 2017 time period. Seafloor-stability point and triangulated irregular network (TIN) surface models were created at five different elevation-change data resolutions (1st order through 5th order) with each resolution becoming increasingly more detailed. The stability point models were used to determine the level of seafloor stability at nine habitat types found at Crocker Reef. This data release includes ArcGIS map packages containing the binned and color-coded stability point and surface (TIN) models and habitat files; maps of each stability model; and data tables containing stability and elevation-change data for the habitat types. Data were collected under Florida Keys National Marine Sanctuary permit FKNMS-2016-068.

Tags: altimetry, coelenterates, crocker-reef, doi-usgs-cmg-gt-coastal-and-marine-geology-u-s-geological-survey-u-s-department-of-interior, elevation, elevation-change, florida, florida-keys, florida-keys-national-marine-sanctuary, florida-reef-tract, geoscientificinformation, lidar-gt-light-detection-and-ranging, marine-geology, mbes-gt-multibeam-mapping-system, ocean-gt-bathymetry-seafloor-topography-gt-water-depth, ocean-gt-coastal-processes-gt-coastal-elevation, ocean-gt-coastal-processes-gt-coral-reefs, ocean-gt-coastal-processes-gt-erosion, oceans, reef-ecosystems, sea-floor-characteristics, seafloor, seafloor-accretion, seafloor-elevation, seafloor-erosion, seafloor-stability, submerged, submerged-topography, usgs-c8d76205-133c-45ef-8ee4-68e256b836eb
Organization: Department of the Interior
JPEG images of photographs of vibracores collected by the U.S. Geological Survey within Apalachicola Bay, Florida, 2007

In 2007, the U.S. Geological Survey collected 24 vibracores within Apalachicola Bay, Florida. The vibracores were collected using a Rossfelder electric percussive (P-3) vibracore system during a cruise on the R/V Gilbert. Selection of the core sites was based on a geophysical survey that was conducted during 2005 and 2006 in collaboration with the National Oceanic and Atmospheric Administration's (NOAA) Coastal Services Center (CSC) and the Apalachicola Bay National Estuarine Research Reserve. Available data include the vibracore data logs and photographs, select seismic-reflection profiles (from the geophysical survey), and core-derived data including: grain size analyses, radiocarbon ages, microfossil counts, and sedimentological interpretations. The long-term goal of this study is to provide maps, data, and assistance to the Apalachicola Bay National Estuarine Research Reserve in their effort to monitor and understand the geology and ecology of Apalachicola Bay Estuary. These data will inform coastal managers charged with resource preservation.

Tags: apalachicola, apalachicola-bay, cmgp, coastal-and-marine-geology-program, core-photographs, core-photos, cores, cruise-id-app-07, dog-island, east-bay, east-pass, florida, geoscientificinformation, gulf-of-mexico, image-collections, imagerybasemapsearthcover, indian-pass, lithology, little-saint-george-island, oceans, r-v-gilbert, saint-george-island, saint-george-sound, saint-vincent-island, saint-vincent-sound, sedimentary-structure, u-s-geological-survey, united-states, usgs, usgs-c8d51e9f-f5ec-4cdc-9b55-009439007d50, vibracores, vibracoring, west-pass, whsc, whsc-field-activity-07008, woods-hole-science-center
Organization: Department of the Interior
LANDFIRE Remap Scott and Burgan Fire Behavior Fuel Model (FBFM40) Marshall Islands

LANDFIRE’s (LF) 2016 Remap (Remap) Scott and Burgan Fire Behavior Fuel Model 40 (FBFM40) product represents distinct distributions of fuel loadings found among surface fuel components (live and dead), size classes, and fuel types (Scott &amp; Burgan 2005). The fuel models are described by the most common fire carrying fuel type (grass, brush, timber, or slash), loading and surface area-to-volume ratio by size class and component, fuel bed depth, and moisture of extinction. FBFM40 contains more fuel models for every fuel type than Anderson Fire Behavior Fuel Model 13 (FBFM13), and the number of fuel models representing relatively High dead fuel moisture content is increased. In FBFM40 fuel models with an herbaceous component are dynamic, to simulate curing, rather than remaining constant. 
LF Remap used vegetation products and 10-years of disturbance data to create Fuel Vegetation Type (FVT), Fuel Vegetation Cover (FVC), and Fuel Vegetation Height (FVH) for disturbed areas to represent pre-disturbance scenarios in FBFM40. A combination of pre-disturbance and non-disturbance Existing Vegetation Type (EVT) are used to assign surface fuel models. FBFM40 was developed using the most recent 10 years of Annual Disturbance products and is a capable fuels product that calculates Time Since Disturbance (TSD) assignments for disturbed areas using an "effective year." For example, year 2020 fuels may be calculated for the year 2020. the new process considers all the existing disturbances included in LF Remap and adjusts the TSD for these to the effective year (2020 in the example), making the products "2020 capable fuels." More information about capable fuels can be found at https://www.landfire.gov/lf_remap.php.

Tags: biota, fbfm, fbfm40, fire-behavior-fuel-model-40, fires, geographic-information-systems, geospatial-datasets, hazard-preparedness, ia, image-collections, imagerybasemapsearthcover, insular-areas, landfire-2016-remap, lf-2016-remap, marshall-islands, oconus, raster-digital-data, remote-sensing, scott-and-burgan-fire-behavior-fuel-model, u-s-forest-service-usfs, u-s-geological-survey-usgs, united-states, us, usgs-c8a8492e-2965-4f6c-8990-d0d7d1c7fad5
Organization: Department of the Interior