Identification_Information: Citation: Citation_Information: Originator: V.E. Langenheim, Shawn Biehler, D.K. McPhee, C.A. McCabe, J.T. Watt, M. Anderson, B.A. Chuchel, and P. Stoffer Publication_Date: 2007 Title: Preliminary isostatic gravity map of Joshua Tree National Park and vicinity, southern California, California Edition: rev 1.0 Publication_Information: Publication_Place: U.S. Geological Survey, Menlo Park, CA Publisher: U.S. Geological Survey Online_Linkage: http://pubs.usgs.gov/of/2007/1218/ Description: Abstract: Gravity data were compiled, collected, and edited to produce an isostatic gravity map of Joshua Tree National Park and vicinity, California. Purpose: To provide basic geophysical information to regional mapping and hydrologic studies Point_of_Contact: Contact_Information: Contact_Person_Primary: Contact_Person: Victoria Langenheim Contact_Organization: U.S. Geological Survey Contact_Address: Address: 345 Middlefield Rd. MS 989 City: Menlo Park State_or_Province: CA Postal_Code: 94025 Country: USA Address_Type: mailing and physical address Contact_Voice_Telephone: 650-329-5313 Spatial_Domain: Bounding_Coordinates: West_Bounding_Coordinate: -116.5 East_Bounding_Coordinate: -115.083 North_Bounding_Coordinate: 33.53 South_Bounding_Coordinate: 34.25 Native_Data_Set_Environment: data was stored and analysed on a SUN Ultra4000 UNIX platform Status: Progress: Preliminary report Maintenance_and_Update_Frequency: none planned Keywords: Place: Place_Keyword: California, Joshua Tree National Park Theme: Theme_Keyword: gravity, density, isostatic anomaly Access_Constraints: none Use_Constraints: none Data_Quality_Information: Positional_Accuracy: Horizontal_Positional_Accuracy: Horizontal_Positional_Accuracy_Report: Accuracy of the point data is roughly 40m, as well as the data can be located on a 1:24,000-scale topographic map Vertical_Positional_Accuracy: Vertical_Positional_Accuracy_Report: Accuracy of the point data vary; most of the elevations are accurate to 10 feet or less. In some of the more mountainous areas, the accuracy may fall to 20 to 40 feet. Attribute_Accuracy: Attribute_Accuracy_Report: Observed gravity data are accurate to 0.05 mGal; reduced anomalies are accurate to 1-2 mGal. Data are more accurate in the valleys than in the mountains because of uncertainties in elevation and in the terrain correction. Logical_Consistency_Report: see open-file report Completeness_Report: Dataset based on geophysical analysis. see open-file report. Lineage: Source_Information: Source_Citation: Citation_Information: Originator: Roberts, C.W., Jachens, R.C., and Oliver, H.W. Publication_Date: 1990 Title: Isostatic gravity map of California and offshore southern California Series_Information: Series_Name: California Division of Mines and Geology Geologic Data Map NO. 7 Edition: first edition Spatial_Reference_Information: Horizontal_Coordinate_System_Definition: Geodetic_Model: Horizontal_Datum_Name: Geographic NAD27 Ellipsoid_Name: CLARKE 1866 Entity_and_Attribute_Information: Detailed_Description: Entity_Type: Entity_Type_Definition: Point_Type Overview_Description: Entity_and_Attribute_Overview: The data file is in ASCII format. The data define point data with information as follows: STATION NAME (a8) .............An alphanumeric combination of up to 8 characters used for station identification; LAT (f3.0,f4.2)................Latitude in degrees and minutes, to 0.01 minute; LON (f4.0,f4.2)................Longitude in degrees and minutes, to 0.01 minute; ELEV (f6.1)....................Elevation, to 0.1 ft; OG (f7.2)......................Observed gravity, to 0.01 mGal; FAA (f6.2) ....................Free-air anomaly to 0.01 mGal; SBA (f6.2).....................Simple Bouguer anomaly to 0.01 mGal; ITC (f5.2).....................Inner terrain correction for a density of 2.67 g/cc, to 0.01 mGal, followed by a letter denoting the extent of the correction. "Z" indicates computer terrain correction from the station out to 166.7 km with inner terrain correction out to D zone; TC (f5.2)......................Total terrain correction from the station to 166.7 km for a density of 2.67 g/cc, to 0.01 mGal; TC CODE (a1)................Letter denoting the extent of the correction, according to the Hayford-Bowie template (e.g. 'D' means 590 meters); CBA (f6.2)...................Complete Bouguer anomaly reduced for a density of 2.67 g/cc, to 0.01 mGal; ISO (f6.2)..................Isostatic residual anomaly values assuming an Airy model for isostatic compensation of topographic loads. This model assumes a a crustal thickness of 25 km, a topographic load density of 2.67 g/cc, and a density contrast across the base of the model crust of 0.4 g/cc. Overview_Description: Entity_and_Attribute_Overview: point data representing gravity data Metadata_Reference_Information: Metadata_Date: 20070918 Metadata_Standard_Name: FGDC Content Standards for Digital Geospatial Metadata