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Layer: madison_012c_salinity_22 (ID: 43)

Name: madison_012c_salinity_22

Display Field: source_organization

Type: Feature Layer

Geometry Type: esriGeometryPolyline

Description: <DIV STYLE="text-align:Left;"><P STYLE="font-size:16ptmargin:7 0 7 0;"><SPAN><SPAN>Water in the area varies significantly in dissolved solids concentration and in temperature, and the density and viscosity vary from area to area. The highest TDS concentrations of about 10,0000 to 300,000 mg/L are on the northeast side of the basin, as shown in the concentration of dissolved solids on the GIS map by Busby (1981, in Downey, 1984, 1986).</SPAN></SPAN></P><DIV><P><SPAN /></P></DIV></DIV>

Service Item Id: 25f1e8d9cbf24685b9d065fbb2559267

Copyright Text: Downey, J. S., 1986, Geohydrology of bedrock aquifers in the northern Great Plains in parts of Montana, North Dakota, South Dakota and Wyoming: U.S. Geological Survey Professional Paper 1402-E, 87 p. * Downey, J. S., 1984, Geohydrology of the Madison and associated aquifers in parts of Montana, North Dakota, South Dakota and Wyoming: U.S. Geological Survey Professional Paper 1273-G, 47 p.

Default Visibility: true

MaxRecordCount: 2000

Supported Query Formats: JSON, geoJSON, PBF

Min Scale: 2000000

Max Scale: 0

Supports Advanced Queries: true

Supports Statistics: true

Has Labels: false

Can Modify Layer: true

Can Scale Symbols: false

Use Standardized Queries: true

Supports Datum Transformation: true

Extent:
Drawing Info: Advanced Query Capabilities:
HasZ: false

HasM: false

Has Attachments: false

HTML Popup Type: esriServerHTMLPopupTypeAsHTMLText

Type ID Field: null

Fields:
Supported Operations:   Query   Query Attachments   Query Analytic   Generate Renderer   Return Updates

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