Name: stpeter_003_formation_thick_22
Display Field: source_organization
Type: Feature Layer
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Description: <DIV STYLE="text-align:Left;"><P STYLE="font-size:16ptmargin:7 0 7 0;"><SPAN><SPAN>We chose to use the map of Collinson and others (1988) because it shows thickness at 50 (rather than 100) ft intervals. Kreutzfeld (1982) pointed out that the thickness of the St. Peter Sandstone is much more variable than the formation-thickness map indicates. The variation in thickness is due to postdepositional erosion and its highly irregular lower boundary. The base of the St. Peter Sandstone is a major regional unconformity (Collinson and others, 1988; Young, 1992b). </SPAN></SPAN></P><DIV><P><SPAN /></P></DIV></DIV>
Service Item Id: 024af67a5da446658e6637444901948e
Copyright Text: Collinson, C., Sargent, M. L., and Jennings, J. R., 1988, Chapter 14: Illinois Basin region, in Sloss, L. L., ed., The Geology of North America, v. D-2, Sedimentary Cover—North American Craton: U.S.: Decade of North American Geology: Geological Society of America, p. 383–426.
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Supported Query Formats: JSON, geoJSON, PBF
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Extent:
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YMin: 4395853.491099998
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Spatial Reference: 102100
(3857)
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Type ID Field: null
Fields:
-
objectid
(
type: esriFieldTypeOID, alias: OBJECTID
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seg_id
(
type: esriFieldTypeInteger, alias: SEG_ID
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thickn_ft_
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type: esriFieldTypeDouble, alias: THICKN_FT_
)
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thickn_m_
(
type: esriFieldTypeDouble, alias: THICKN_M_
)
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shape_leng
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type: esriFieldTypeDouble, alias: Shape_Leng
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source_organization
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type: esriFieldTypeString, alias: Source Organization, length: 255
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