Filters: Date Range: {"choice":"week"} (X) > partyWithName: U.S. Geological Survey (X)
Folder: ROOT ( Show direct descendants )
204 results (42ms)
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Panorama with images 1483, 1484, and 1486. Sawtooth Range and Stanley Basin. Custer County, Idaho. No date.
Panorama with image 052. Deer Springs Wash, about one-quarter mile above diversion dam; shows outlier in Nakaibito formation contact seen sloping down toward gully bottom. Mexican Springs Experimental Station. San Juan County, New Mexico. October 1949.
Categories: Image;
Tags: Leopold, L.B. Collection,
Photographers,
San Juan County, New Mexico,
photo print
Two terrace levels along the Arroyo de los Frijoles; the lower terrace, about 18 inches above the channel bed, is in the foreground; at the tree near the channel edge, the upper terrace stance five feet above the present bed and grades smoothly to adjacent hills. Santa Fe County, New Mexico. Circa 1960. Published in U.S. Geological Survey Professional Paper 352-G, Figure 140-B. 1966.
Categories: Image;
Tags: Leopold, L.B. Collection,
Photographers,
Santa Fe County, New Mexico,
photo print
Detail of magnesite prospect on Ash Creek, 30 miles north of Lordsburg. Shows deposit about 9-feet wide broken by several partings. J.E. Conner, prospector. New Mexico. May 6, 1920.
William E. Davies, was born on December 24, 1917 in Cleveland, Ohio. He attended MIT in 1935 and graduated in 1939 with a degree in geology and a minor in geophysics. After graduating MIT, Davies attended a masters program at Michigan State University, recieving an M.S. in 1941. That same year, Davies entered U.S. Army Corps of Engineers as a Secound Lieutenant. In August 1949 Davies joined the USGS as a member of the Military Geology Branch. In 1954, Davies sailed to Antarctica aboard the USS Atka for the purpose of selecting suitable sites for a U.S. research station during the International Geophysical Year. Over Davies career more than 200 titles were added to his bibliography. Davies received the Antarctic...
Categories: Physical Item;
Tags: ndc_collection
This model archive contains the data and software application used to develop a two-dimensional hydrodynamic model of a 1.2 kilometer reach of the North Santiam River in Oregon. The Delft3D-Flexible Mesh modeling system was used to simulate flow conditions at a baseflow discharge of 25 cubic meters per second and thus provide spatially distributed predictions of depth and velocity throughout the reach. This model archive consists of four individual components: (1) information on the hydrodynamic model software application; (2) the topographic data used to construct the model grid and field measurements of water depth used to calibrate the model; (3) complete Delft3D model runs, including both the required inputs...
Categories: Data;
Types: Map Service,
OGC WFS Layer,
OGC WMS Layer,
OGC WMS Service;
Tags: North Santiam River,
Oregon,
depth,
hydrodynamic model,
model archive,
Drilling operations on property of Alphonso Fusco at Elmwood Road Station about three and one-half miles west of Medford. S.J. Taylor, contractor, at left. Different view point. Mount Holly quadrangle. Burlington County, New Jersey. March 13, 1919.
Panorama with image 448. Recent digging at Hoffman's pit about 3 to 4 miles northwest of Birmingham station. W.B. Hicks center. Pemberton quadrangle. Burlington County, New Jersey. January 26, 1919.
Categories: Image;
Tags: Burlington County, New Jersey,
Hoffman's pit,
Mills, Mines, Quarries,
photo print
This dataset includes spreadsheets with statistical data (mean and median absolute error) used in deciding which interpolation method best fit the corresponding dataset. All statistical data were paired with a visual inspection of the interpolation prior to determining the final raster product. All spreadsheets were generated using an automated python script (Jahn, 2020).
This dataset includes "smoothing points" used in the creation of the Cincinnatus hydrogeologic framework. Smoothing points were manually added by the project team and were used to enhance interpolated layers using geologic assumptions and include: valley edge points, centerline bedrock points (and where applicable L1 and L2 points), and upland bedrock SURGO points.
The Jamestown study area is located within the counties of Chautauqua and Cattaraugus, New York. The predominant population center is the city of Jamestown. Previous USGS reports here include Open-File Report 82-113 (Stelz and others 1982) and Bulletin 58-1960 (Crain, 1966) The five child pages below break the data up into georeferenced and digitized previous report data, interpreted geologic information, well logs, supplemental point data, and interpolation statistics.
This dataset includes spreadsheets with statistical data (mean and median absolute error) used in deciding which interpolation method best fit the corresponding dataset. All statistical data were paired with a visual inspection of the interpolation prior to determining the final raster product. All spreadsheets were generated using an automated python script (Jahn, 2020).
This dataset includes "smoothing points" used in the creation of the Roundout Neversink hydrogeologic framework. Smoothing points were manually added by the project team and were used to enhance interpolated layers using geologic assumptions and include: valley edge points, centerline bedrock points (and where applicable L1 and L2 points), and upland bedrock SURGO points.
Sketch of wildflowers in Grand Teton National Park, Wyoming drawn in June 1877 by Stephen J. Kubel, Chief Engraver of the U.S. Geological Survey during the Hayden Survey of 1877. Handwritten information on slide holder: S.J. Kubel sketches, June 7 & 9, 1877. Pink flower and blue Columbine. For more information refer to the Grand Teton Nature Notes, Vol. V, No. 1 "An Episode from the Hayden Survey of 1877", by Dr. F.M. Fryxell.
This data release contains the U.S. salient statistics and world production data extracted from the IRON AND STEEL SCRAP data sheet of the USGS Mineral Commodity Summaries 2023.
The U.S. Geological Survey (USGS) maintains shoreline positions for the United States coasts from both older sources, such as aerial photographs or topographic surveys, and contemporary sources, such as lidar-point clouds and digital elevation models. These shorelines are compiled and analyzed in the USGS Digital Shoreline Analysis System (DSAS), version 5.1 software to calculate rates of change. Keeping a record of historical shoreline positions is an effective method to monitor change over time, enabling scientists to identify areas most susceptible to erosion or accretion. These data can help coastal managers understand which areas of the coast are vulnerable to change. This data release, and other associated...
Categories: Data;
Types: Downloadable,
Map Service,
OGC WFS Layer,
OGC WMS Layer,
Shapefile;
Tags: Atlantic Coast,
CMGP,
Caribbean,
Coastal Research and Planning Institute of Puerto Rico,
Coastal and Marine Geology Program,
Erosion pins consisting of 10-inch spike and washer in grid system. Slopewash Tributary (scale is a 6-inch ruler). Santa Fe County, New Mexico. Circa 1960. Published in U. S. Geological Survey Professional Paper 352-G, Figure 162-A. 1966.
Categories: Image;
Tags: Leopold, L.B. Collection,
Photographers,
Santa Fe County, New Mexico,
photo print
Water pouring into open pipe or tunnel leading downward to arroyo channel. The upper opening of this piping hole is at least 15-feet from wall of gully. Rio Pescado near Ramah. McKinley County, New Mexico. August 17, 1946. Published in U. S. Geological Survey Professional Paper 282-A, Figure 5. 1956.
Categories: Image;
Tags: Leopold, L.B. Collection,
McKinley County, New Mexico,
Photographers,
photo print
Montana Earthquake June 27, 1925. Damaged schoolhouse at Manhattan. The separation of partition walls from the outside wall is due to a lack of ties. 1925. Plate 6-A, U.S. Geological Survey Professional paper 147.
Categories: Image;
Tags: Earthquakes,
Montana,
Montana Earthquake June 27, 1925,
Pardee, J.T. Collection,
Photographers,
This dataset includes well logs used in the creation of the Ellicottville hydrogeologic framework. Well logs were used from multiple sources (DEC, DOT, NWIS, ESOGIS, and archived material) and were a crucial component in generating hydrogeologic layer elevations and thicknesses. Well logs are available in their original form on GeoLog Locator (https://webapps.usgs.gov/GeoLogLocator/#!/) and provided here in the digitized form (shapefiles and feature classes), which were used in the generation of the hydrogeologic framework.
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