Name: potomac_006_cont_sandbody
Display Field: source_organization
Type: Feature Layer
Geometry Type: esriGeometryPolyline
Description: Number of studies present cross sections that include geophysical logs (gamma ray, spontaneous potential, resistivity) that can be used to evaluate sand-body continuity within the lower Potomac aquifer (Hansen, 1968; Brown and others, 1972; Cushing and others, 1973; Trapp and others, 1984). These cross sections indicate that a number of thicker sands are continuous. Cushing and others (1973, their plate 2) generated a map showing the thickness distribution of a major sand unit in the Potomac aquifer. This map, which is digitized, demonstrates that the major sand bodies are continuous, and for this particular interval, are more than 50 ft thick across the entire Delmarva Peninsula.
Service Item Id: 546b9dc4ddd6458fa7fed23b017c5174
Copyright Text: Cushing, E. M., Kantrowitz, I. H., and Taylor, K. R., 1973, Water resources of the Delmarva Peninsula: U.S. Geological Survey, Professional Paper 822, 58 p
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Supported Query Formats: JSON, geoJSON, PBF
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Supports Advanced Queries: true
Supports Statistics: true
Has Labels: false
Can Modify Layer: true
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Use Standardized Queries: true
Supports Datum Transformation: true
Extent:
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YMin: 4574823.052000001
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Spatial Reference: 102100
(3857)
LatestVCSWkid(0)
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HasZ: false
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Type ID Field: null
Fields:
-
objectid
(
type: esriFieldTypeOID, alias: OBJECTID
)
-
seg_id
(
type: esriFieldTypeInteger, alias: SEG_ID
)
-
thickn_ft_
(
type: esriFieldTypeDouble, alias: THICKN_FT_
)
-
thickn_m_
(
type: esriFieldTypeDouble, alias: THICKN_M_
)
-
shape_leng
(
type: esriFieldTypeDouble, alias: Shape_Leng
)
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source_organization
(
type: esriFieldTypeString, alias: Source Organization, length: 255
)
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hyperlink
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type: esriFieldTypeString, alias: Link, length: 255
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