Name: repetto_006_continuity_sandbod_22

Display Field: continuity

Type: Feature Layer

Geometry Type: esriGeometryPolygon

Description: <DIV STYLE="text-align:Left;"><P STYLE="text-align:Justify;font-size:16ptmargin:7 0 7 0;"><SPAN><SPAN>The sandy deposits of the Repetto Formation, consisting of channel-fill deposits in suprafan facies, are distributed in the central structural trough north and east of the Palos Verdes Hills (Redin, 1991). These sandstones were sourced from the northeast, from conglomeratic mid- to upper-channelized fan deposits. Repetto sandstones grade southward from the suprafan facies into distal submarine-fan facies into offshore areas.</SPAN></SPAN></P><DIV><P><SPAN /></P></DIV></DIV>

Service Item Id: 0572a2b5252546049de16823db197076

Copyright Text: Conrey, B. L., 1967, Early Pliocene sedimentary history of the Los Angeles Basin, California: California Division of Mines and Geology Special Report 93, 63 p.

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Supported Query Formats: JSON, geoJSON, PBF

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Use Standardized Queries: true

Supports Datum Transformation: true

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YMin: 3960058.280100003
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Spatial Reference: 102100  (3857)

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Type ID Field: null

Fields:

• objectid ( type: esriFieldTypeOID, alias: OBJECTID )
• edx_sp_csod.sde.repetto_006_continuity_sandbody.area ( type: esriFieldTypeDouble, alias: edx_sp_csod.sde.repetto_006_continuity_sandbody.area )
• perimeter ( type: esriFieldTypeDouble, alias: PERIMETER )
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• st_perimeter(shape) ( type: esriFieldTypeDouble, alias: st_perimeter(shape) )

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

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