AndreaBozzo/ceres-open-data-index huggingface dataset:
Brookfield City Lake near Brookfield, Missouri, 2021

Water supply lakes are the primary source of water for many communities in northern and western Missouri.  Therefore, accurate and up-to-date estimates of lake capacity are important for managing and predicting adequate water supply. Many of the water supply lakes in Missouri were previously surveyed by the U.S. Geological Survey in the early 2000s (Richards, 2013) and in 2013 (Huizinga, 2014); however, years of potential sedimentation may have resulted in reduced water storage capacity. Periodic bathymetric surveys are useful to update the area/capacity table and to determine changes in the bathymetric surface.
Brookfield City Lake is a water supply lake used by the city of Brookfield in north-central Missouri. The surface area of Brookfield City Lake is about 112 acres at the full pool level of the primary spillway (799.3 feet above the North American Vertical Datum of 1988).  A previous bathymetric survey was completed in 2000 with a single-beam echosounder.  In March 2021, the U.S. Geological Survey, in cooperation with the Missouri Department of Natural Resources and in collaboration with the City of Brookfield, completed a bathymetric survey of Brookfield City Lake using a multibeam echosounder.  The water-surface elevation during the survey was about 799.3 feet. The echosounder data can be combined with light detection and ranging (lidar) data to prepare a bathymetric map and a surface area and capacity table for the lake.
The gridded bathymetric point data (Brookfield2021_bathy_pts.zip) were computed on a 1.64-foot (0.50-meter) grid using the Combined Uncertainty and Bathymetry Estimator (CUBE) method, which is used as the source of points to create the bathymetric surface.
Bathymetric quality-assurance data (Brookfield2021_QA_raw.zip) were collected to evaluate the vertical accuracy of the gridded bathymetric point data.
Each of these two zip files contains a shapefile with an attribute table. Attribute/column labels of each table are described in the "Entity and attribute" section of the metadata file.
References Cited:
Huizinga, R.J., 2014, Bathymetric surveys and area/capacity tables of water-supply reservoirs for the city of Cameron, Missouri, July 2013: U.S. Geological Survey Open-File Report 2014–1005, 15 p., http://dx.doi.org/10.3133/ofr20141005.
Richards, J.M., 2013, Bathymetric surveys of selected lakes in Missouri—2000–2008: U.S. Geological Survey Open-File Report 2013–1101, 9 p. with appendix, http://pubs.usgs.gov/of/2013/1101.

Tags: bathymetry, bathymetry-and-elevation, brookfield, brookfield-city-lake, linn-county, missouri, multibeam, multibeam-sonar, u-s-geological-survey, usgs, usgs-62e1952fd34e10763b59913f
Organization: Department of the Interior
New Marceline City Lake near Marceline, Missouri, 2021

Water supply lakes are the primary source of water for many communities in northern and western Missouri. Therefore, accurate and up-to-date estimates of lake capacity are important for managing and predicting adequate water supply. Many of the water supply lakes in Missouri were previously surveyed by the U.S. Geological Survey in the early 2000s (Richards, 2013) and in 2013 (Huizinga, 2014); however, years of potential sedimentation may have resulted in reduced water storage capacity. Periodic bathymetric surveys are useful to update the area/capacity table and to determine changes in the bathymetric surface.
New Marceline City Lake is a water supply lake used by the city of Marceline in north-central Missouri. The surface area of New Marceline City Lake is about 209 acres at the full pool level of the primary spillway (761.6 feet above the North American Vertical Datum of 1988). A previous bathymetric survey was completed in 2003 with a single-beam echosounder. In March 2021, the U.S. Geological Survey, in cooperation with the Missouri Department of Natural Resources and in collaboration with the City of Marceline, completed a bathymetric survey of New Marceline City Lake using a multibeam echosounder. The water-surface elevation during the survey was about 757.2 feet. The echosounder data can be combined with light detection and ranging (lidar) data to prepare a bathymetric map and a surface area and capacity table for the lake.
The gridded bathymetric point data (MarcelineNew2021_bathy_pts.zip) were computed on a 1.64-foot (0.50-meter) grid using the Combined Uncertainty and Bathymetry Estimator (CUBE) method, which is used as the source of points to create the bathymetric surface.
Bathymetric quality-assurance data (MarcelineNew2021_QA_raw.zip) were collected to evaluate the vertical accuracy of the gridded bathymetric point data.
Each of these two zip files contains a shapefile with an attribute table. Attribute/column labels of each table are described in the "Entity and attribute" section of the metadata file.
References Cited:
Huizinga, R.J., 2014, Bathymetric surveys and area/capacity tables of water-supply reservoirs for the city of Cameron, Missouri, July 2013: U.S. Geological Survey Open-File Report 2014–1005, 15 p., http://dx.doi.org/10.3133/ofr20141005.
Richards, J.M., 2013, Bathymetric surveys of selected lakes in Missouri—2000–2008: U.S. Geological Survey Open-File Report 2013–1101, 9 p. with appendix, http://pubs.usgs.gov/of/2013/1101.

Tags: bathymetry, bathymetry-and-elevation, chariton-county, marceline, missouri, multibeam, multibeam-sonar, new-marceline-city-lake, u-s-geological-survey, usgs, usgs-62e1984bd34e10763b599146
Organization: Department of the Interior
Marceline Old Reservoir near Marceline, Missouri, 2021

Water supply lakes are the primary source of water for many communities in northern and western Missouri. Therefore, accurate and up-to-date estimates of lake capacity are important for managing and predicting adequate water supply. Many of the water supply lakes in Missouri were previously surveyed by the U.S. Geological Survey in the early 2000s (Richards, 2013) and in 2013 (Huizinga, 2014); however, years of potential sedimentation may have resulted in reduced water storage capacity. Periodic bathymetric surveys are useful to update the area/capacity table and to determine changes in the bathymetric surface.
Marceline Old Reservoir is a water supply lake used by the city of Marceline in north-central Missouri. The surface area of Marceline Old Reservoir is about 65.4 acres at the full pool level of the primary spillway (817.7 feet above the North American Vertical Datum of 1988). No previous bathymetric survey has been completed at this reservoir. In March 2021, the U.S. Geological Survey, in cooperation with the Missouri Department of Natural Resources and in collaboration with the City of Marceline, completed a bathymetric survey of Marceline Old Reservoir using a multibeam echosounder. The water-surface elevation during the survey was about 817.7 feet. The echosounder data can be combined with light detection and ranging (lidar) data to prepare a bathymetric map and a surface area and capacity table for the lake.
The gridded bathymetric point data (MarcelineOld2021_bathy_pts.zip) were computed on a 0.82-foot (0.25-meter) grid using the Combined Uncertainty and Bathymetry Estimator (CUBE) method, which is used as the source of points to create the bathymetric surface.
Bathymetric quality-assurance data (MarcelineOld2021_QA_raw.zip) were collected to evaluate the vertical accuracy of the gridded bathymetric point data.
Each of these two zip files contains a shapefile with an attribute table. Attribute/column labels of each table are described in the "Entity and attribute" section of the metadata file.
References Cited:
Huizinga, R.J., 2014, Bathymetric surveys and area/capacity tables of water-supply reservoirs for the city of Cameron, Missouri, July 2013: U.S. Geological Survey Open-File Report 2014–1005, 15 p., http://dx.doi.org/10.3133/ofr20141005.
Richards, J.M., 2013, Bathymetric surveys of selected lakes in Missouri—2000–2008: U.S. Geological Survey Open-File Report 2013–1101, 9 p. with appendix, http://pubs.usgs.gov/of/2013/1101.

Tags: bathymetry, bathymetry-and-elevation, linn-county, marceline, marceline-old-reservoir, missouri, multibeam, multibeam-sonar, u-s-geological-survey, usgs, usgs-62e19a1dd34e10763b599148
Organization: Department of the Interior
Shelbina Lake near Shelbina, Missouri, 2021

Water supply lakes are the primary source of water for many communities in northern and western Missouri. Therefore, accurate and up-to-date estimates of lake capacity are important for managing and predicting adequate water supply. Many of the water supply lakes in Missouri were previously surveyed by the U.S. Geological Survey in the early 2000s (Richards, 2013) and in 2013 (Huizinga, 2014); however, years of potential sedimentation may have resulted in reduced water storage capacity. Periodic bathymetric surveys are useful to update the area/capacity table and to determine changes in the bathymetric surface.
Shelbina Lake is a water supply lake used by the city of Shelbina in north-central Missouri. The surface area of Shelbina Lake is about 46.6 acres at the full pool level of the primary spillway (715.1 feet above the North American Vertical Datum of 1988). A previous bathymetric survey was completed in 2001 with a single-beam echosounder. In March 2021, the U.S. Geological Survey, in cooperation with the Missouri Department of Natural Resources and in collaboration with the City of Shelbina, completed a bathymetric survey of Shelbina Lake using a multibeam echosounder. The water-surface elevation during the survey was about 715.1 feet. The echosounder data can be combined with light detection and ranging (lidar) data to prepare a bathymetric map and a surface area and capacity table for the lake.
The gridded bathymetric point data (Shelbina2021_bathy_pts.zip) were computed on a 0.82-foot (0.25-meter) grid using the Combined Uncertainty and Bathymetry Estimator (CUBE) method, which is used as the source of points to create the bathymetric surface.
Bathymetric quality-assurance data (Shelbina2021_QA_raw.zip) were collected to evaluate the vertical accuracy of the gridded bathymetric point data.
Each of these two zip files contains a shapefile with an attribute table. Attribute/column labels of each table are described in the "Entity and attribute" section of the metadata file.
References Cited:
Huizinga, R.J., 2014, Bathymetric surveys and area/capacity tables of water-supply reservoirs for the city of Cameron, Missouri, July 2013: U.S. Geological Survey Open-File Report 2014–1005, 15 p., http://dx.doi.org/10.3133/ofr20141005.
Richards, J.M., 2013, Bathymetric surveys of selected lakes in Missouri—2000–2008: U.S. Geological Survey Open-File Report 2013–1101, 9 p. with appendix, http://pubs.usgs.gov/of/2013/1101.

Tags: bathymetry, bathymetry-and-elevation, missouri, multibeam, multibeam-sonar, shelbina, shelbina-lake, shelby-county, u-s-geological-survey, usgs, usgs-62e19a3bd34e10763b59914a
Organization: Department of the Interior
Memphis Lake (Lake Showme) near Memphis, Missouri, 2021

Water supply lakes are the primary source of water for many communities in northern and western Missouri. Therefore, accurate and up-to-date estimates of lake capacity are important for managing and predicting adequate water supply. Many of the water supply lakes in Missouri were previously surveyed by the U.S. Geological Survey in the early 2000s (Richards, 2013) and in 2013 (Huizinga, 2014); however, years of potential sedimentation may have resulted in reduced water storage capacity. Periodic bathymetric surveys are useful to update the area/capacity table and to determine changes in the bathymetric surface.
Memphis Lake (locally known as Lake Showme) is a water supply lake used by the city of Memphis in northeastern Missouri. The surface area of  Memphis Lake is about 294 acres at the full pool level of the primary spillway (773.8 feet above the North American Vertical Datum of 1988). A previous bathymetric survey was completed in 2002 with a single-beam echosounder. In April 2021, the U.S. Geological Survey, in cooperation with the Missouri Department of Natural Resources and in collaboration with the City of Memphis, completed a bathymetric survey of  Memphis Lake using a multibeam echosounder. The water-surface elevation during the survey was about 769.8 feet. The echosounder data can be combined with light detection and ranging (lidar) data to prepare a bathymetric map and a surface area and capacity table for the lake.
The gridded bathymetric point data (LakeShowme2021_bathy_pts.zip) were computed on a 1.64-foot (0.50-meter) grid using the Combined Uncertainty and Bathymetry Estimator (CUBE) method, which is used as the source of points to create the bathymetric surface.
Bathymetric quality-assurance data (LakeShowme2021_QA_raw.zip) were collected to evaluate the vertical accuracy of the gridded bathymetric point data.
Each of these two zip files contains a shapefile with an attribute table. Attribute/column labels of each table are described in the "Entity and attribute" section of the metadata file.
References Cited:
Huizinga, R.J., 2014, Bathymetric surveys and area/capacity tables of water-supply reservoirs for the city of Cameron, Missouri, July 2013: U.S. Geological Survey Open-File Report 2014–1005, 15 p., http://dx.doi.org/10.3133/ofr20141005.
Richards, J.M., 2013, Bathymetric surveys of selected lakes in Missouri—2000–2008: U.S. Geological Survey Open-File Report 2013–1101, 9 p. with appendix, http://pubs.usgs.gov/of/2013/1101.

Tags: bathymetry, bathymetry-and-elevation, lake-showme, memphis, memphis-lake, missouri, multibeam, multibeam-sonar, scotland-county, u-s-geological-survey, usgs, usgs-62e19a6fd34e10763b59914e
Organization: Department of the Interior
Memphis Reservoir near Memphis, Missouri, 2021

Water supply lakes are the primary source of water for many communities in northern and western Missouri. Therefore, accurate and up-to-date estimates of lake capacity are important for managing and predicting adequate water supply. Many of the water supply lakes in Missouri were previously surveyed by the U.S. Geological Survey in the early 2000s (Richards, 2013) and in 2013 (Huizinga, 2014); however, years of potential sedimentation may have resulted in reduced water storage capacity. Periodic bathymetric surveys are useful to update the area/capacity table and to determine changes in the bathymetric surface.
Memphis Reservoir is a water supply lake used by the city of Memphis in northeastern Missouri. The surface area of Memphis Reservoir is about 39.8 acres at the full pool level of the primary spillway (718.1 feet above the North American Vertical Datum of 1988). A previous bathymetric survey was completed in 2001 with a single-beam echosounder. In April 2021, the U.S. Geological Survey, in cooperation with the Missouri Department of Natural Resources and in collaboration with the City of Memphis, completed a bathymetric survey of Memphis Reservoir using a multibeam echosounder. The water-surface elevation during the survey was about 718.2 feet. The echosounder data can be combined with light detection and ranging (lidar) data to prepare a bathymetric map and a surface area and capacity table for the lake.
The gridded bathymetric point data (Memphis2021_bathy_pts.zip) were computed on a 0.82-foot (0.25-meter) grid using the Combined Uncertainty and Bathymetry Estimator (CUBE) method, which is used as the source of points to create the bathymetric surface.
Bathymetric quality-assurance data (Memphis2021_QA_raw.zip) were collected to evaluate the vertical accuracy of the gridded bathymetric point data.
Each of these two zip files contains a shapefile with an attribute table. Attribute/column labels of each table are described in the "Entity and attribute" section of the metadata file.
References Cited:
Huizinga, R.J., 2014, Bathymetric surveys and area/capacity tables of water-supply reservoirs for the city of Cameron, Missouri, July 2013: U.S. Geological Survey Open-File Report 2014–1005, 15 p., http://dx.doi.org/10.3133/ofr20141005.
Richards, J.M., 2013, Bathymetric surveys of selected lakes in Missouri—2000–2008: U.S. Geological Survey Open-File Report 2013–1101, 9 p. with appendix, http://pubs.usgs.gov/of/2013/1101.

Tags: bathymetry, bathymetry-and-elevation, memphis, memphis-reservoir, missouri, multibeam, multibeam-sonar, scotland-county, u-s-geological-survey, usgs, usgs-62e19a90d34e10763b599150
Organization: Department of the Interior
Bowling Green Reservoir (Jack Floyd Memorial Lake) near Bowling Green, Missouri, 2021

Water supply lakes are the primary source of water for many communities in northern and western Missouri. Therefore, accurate and up-to-date estimates of lake capacity are important for managing and predicting adequate water supply. Many of the water supply lakes in Missouri were previously surveyed by the U.S. Geological Survey in the early 2000s (Richards, 2013) and in 2013 (Huizinga, 2014); however, years of potential sedimentation may have resulted in reduced water storage capacity. Periodic bathymetric surveys are useful to update the area/capacity table and to determine changes in the bathymetric surface.
Bowling Green Reservoir (locally known as Jack Floyd Memorial Lake) is a water supply lake used by the city of Bowling Green in northeastern Missouri. The surface area of Bowling Green Reservoir is about 44.4 acres at the full pool level of the primary spillway (795.0 feet above the North American Vertical Datum of 1988). A previous bathymetric survey was completed in 2005 with a single-beam echosounder. In April 2021, the U.S. Geological Survey, in cooperation with the Missouri Department of Natural Resources and in collaboration with the City of Bowling Green, completed a bathymetric survey of Bowling Green Reservoir using a multibeam echosounder. The water-surface elevation during the survey was about 794.8 feet. The echosounder data can be combined with light detection and ranging (lidar) data to prepare a bathymetric map and a surface area and capacity table for the lake.
The gridded bathymetric point data (JackFloyd2021_bathy_pts.zip) were computed on a 0.82-foot (0.25-meter) grid using the Combined Uncertainty and Bathymetry Estimator (CUBE) method, which is used as the source of points to create the bathymetric surface.
Bathymetric quality-assurance data (JackFloyd2021_QA_raw.zip) were collected to evaluate the vertical accuracy of the gridded bathymetric point data.
Each of these two zip files contains a shapefile with an attribute table. Attribute/column labels of each table are described in the "Entity and attribute" section of the metadata file.
References Cited:
Huizinga, R.J., 2014, Bathymetric surveys and area/capacity tables of water-supply reservoirs for the city of Cameron, Missouri, July 2013: U.S. Geological Survey Open-File Report 2014–1005, 15 p., http://dx.doi.org/10.3133/ofr20141005.
Richards, J.M., 2013, Bathymetric surveys of selected lakes in Missouri—2000–2008: U.S. Geological Survey Open-File Report 2013–1101, 9 p. with appendix, http://pubs.usgs.gov/of/2013/1101.

Tags: bathymetry, bathymetry-and-elevation, bowling-green, bowling-green-reservoir, jack-floyd-memorial-lake, missouri, multibeam, multibeam-sonar, pike-county, u-s-geological-survey, usgs, usgs-62e19aa9d34e10763b599152
Organization: Department of the Interior
Old Lake (Bowling Green West) near Bowling Green, Missouri, 2021

Water supply lakes are the primary source of water for many communities in northern and western Missouri. Therefore, accurate and up-to-date estimates of lake capacity are important for managing and predicting adequate water supply. Many of the water supply lakes in Missouri were previously surveyed by the U.S. Geological Survey in the early 2000s (Richards, 2013) and in 2013 (Huizinga, 2014); however, years of potential sedimentation may have resulted in reduced water storage capacity. Periodic bathymetric surveys are useful to update the area/capacity table and to determine changes in the bathymetric surface.
Old Lake (locally known as Bowling Green West) is a water supply lake used by the city of Bowling Green in northeastern Missouri. The surface area of Old Lake is about 33.6 acres at the full pool level of the primary spillway (779.6 feet above the North American Vertical Datum of 1988). A previous bathymetric survey was completed in 2005 with a single-beam echosounder. In April 2021, the U.S. Geological Survey, in cooperation with the Missouri Department of Natural Resources and in collaboration with the City of Bowling Green, completed a bathymetric survey of Old Lake using a multibeam echosounder. The water-surface elevation during the survey was about 773.9 feet. The echosounder data can be combined with light detection and ranging (lidar) data to prepare a bathymetric map and a surface area and capacity table for the lake.
The gridded bathymetric point data (BowlingGreenWest2021_bathy_pts.zip) were computed on a 0.82-foot (0.25-meter) grid using the Combined Uncertainty and Bathymetry Estimator (CUBE) method, which is used as the source of points to create the bathymetric surface.
Bathymetric quality-assurance data (BowlingGreenWest2021_QA_raw.zip) were collected to evaluate the vertical accuracy of the gridded bathymetric point data.
Each of these two zip files contains a shapefile with an attribute table. Attribute/column labels of each table are described in the "Entity and attribute" section of the metadata file.
References Cited:
Huizinga, R.J., 2014, Bathymetric surveys and area/capacity tables of water-supply reservoirs for the city of Cameron, Missouri, July 2013: U.S. Geological Survey Open-File Report 2014–1005, 15 p., http://dx.doi.org/10.3133/ofr20141005.
Richards, J.M., 2013, Bathymetric surveys of selected lakes in Missouri—2000–2008: U.S. Geological Survey Open-File Report 2013–1101, 9 p. with appendix, http://pubs.usgs.gov/of/2013/1101.

Tags: bathymetry, bathymetry-and-elevation, bowling-green, bowling-green-west, missouri, multibeam, multibeam-sonar, old-lake, pike-county, u-s-geological-survey, usgs, usgs-62e19abfd34e10763b599154
Organization: Department of the Interior