Name: mor_008_cto

Display Field: CONTINUITY

Type: Feature Layer

Geometry Type: esriGeometryPolygon

Description: The continuity of the Morrison aquifer can be estimated from the sandstone isolith map of Galloway (1980), in addition to the outcrop patterns and faults on the edge of the basin. These fluvial sandstones are highly heterogeneous.

Service Item Id: 853af3d39e054a74a87568c3c610f53e

Copyright Text: Galloway, W. E., 1980, Deposition and early hydrologic evolution of the Westwater Canyon and other fluvial fan systems, in Rautman, C. A., compiler, Geology and mineral technology of the Grants uranium region: New Mexico Bureau of Mines and Mineral Resources Memoir 38, p. 59–69.

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Extent:

XMin: -1.21501887639E7
YMin: 4194127.4614000022
XMax: -1.19917614866E7
YMax: 4446568.406300001
Spatial Reference: 102100  (3857)

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Fields:

• objectid ( type: esriFieldTypeOID, alias: OBJECTID )
• seg_id ( type: esriFieldTypeInteger, alias: SEG_ID )
• continuity ( type: esriFieldTypeString, alias: CONTINUITY, length: 11 )
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