Layers:
- Punktobjekt
- Linjeobjekt
- Jordart, tunt eller osammanhängande ytlager
- Jordart, djuplager (okomplett & osäkert)
- Jordart, grundlager
Layer: Jordartskartan, Sveriges geologiska undersökning (95)
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Geometry Type: null
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Copyright Text:
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Supports Query Analytic: false
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Label: Berg
Description: N/A
Symbol:
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Label: Dödisgrop
Description: N/A
Symbol:
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Value: Jätteblock
Label: Jätteblock
Description: N/A
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Value: Källa
Label: Källa
Description: N/A
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- SHAPE ( type: esriFieldTypeGeometry, alias: SHAPE )
Layer: Punktobjekt (96)
Parent Layer: Jordartskartan, Sveriges geologiska undersökningName: Punktobjekt
Display Field: SP_TX
Type: Feature Layer
Geometry Type: esriGeometryPoint
Description: Punktobjekt innehåller geologiska företeelser såsom mindre berghällar och landformer.
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Copyright Text:
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Supports Having Clause: true
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Supports Time Relation: true
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Supports Query Analytic: true
Supports Query With Current User: true
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Symbol:-
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Label: Fornstrand
Description: N/A
Symbol:-
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Label: Högsta kustlinjen
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Symbol:-
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Label: Krön på isälvsavlagring
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Symbol:-
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Description: N/A
Symbol:-
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Label: Isälvsränna, bredd <50 m
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Symbol:-
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Symbol:-
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Label: Övergiven fluvial fåra
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Layer: Linjeobjekt (97)
Parent Layer: Jordartskartan, Sveriges geologiska undersökningName: Linjeobjekt
Display Field: SL_TX
Type: Feature Layer
Geometry Type: esriGeometryPolyline
Description: Linjeobjekt innehåller geologiska företeelser såsom smalare bergblottningar och landformer.
Service Item Id: 1ff6144fb54c4c9c8302821ba94bb800
Copyright Text:
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Field 2: N/A
Field 3: N/A
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Supports OrderBy: true
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Label: Lera--silt
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Layer: Jordart, tunt eller osammanhängande ytlager (98)
Parent Layer: Jordartskartan, Sveriges geologiska undersökningName: Jordart, tunt eller osammanhängande ytlager
Display Field: JY1_TX
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: På många ställen förekommer tunna eller osammanhängande ytliga jordlager med en sammansättning som avviker från grundlagrets (JG2). Tunna eller osammanhängande ytlager av torv är särskilt vanliga, liksom ytlager av morän (eller oklassificerad jord) på berg. Ytlager JY1 avser sådana ytliga jordlager med en mäktighet mindre än ca 0,5 m eller osammanhängande ytliga jordlager med en bedömd medelmäktighet av ca 0,5-1 m. JY1 överlagrar i förekommande fall grundlager, JG2.
Service Item Id: 1ff6144fb54c4c9c8302821ba94bb800
Copyright Text:
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MaxRecordCount: 2000
Supported Query Formats: JSON, geoJSON, PBF
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Max Scale: 0.0
Supports Advanced Queries: true
Supports Statistics: true
Has Labels: false
Can Modify Layer: true
Can Scale Symbols: true
Use Standardized Queries: true
Supports Datum Transformation: true
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Supports OrderBy: true
Supports Distinct: true
Supports Pagination: true
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Supports Returning Query Extent: true
Supports Query With Distance: true
Supports Sql Expression: true
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Supports Query With LOD Spatial Reference: false
Supports Percentile Statistics: true
Supports Having Clause: true
Supports Count Distinct: true
Supports Time Relation: true
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Supports Query Analytic: true
Supports Query With Current User: true
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HasM: false
Has Attachments: false
HTML Popup Type: esriServerHTMLPopupTypeAsHTMLText
Type ID Field: null
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Label: Isälvssediment
Description: N/A
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Label: Morän
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Layer: Jordart, djuplager (okomplett & osäkert) (99)
Parent Layer: Jordartskartan, Sveriges geologiska undersökningName: Jordart, djuplager (okomplett & osäkert)
Display Field: JD3_TX
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: Underliggande lager JD3 avser jordlager som underlagrar det jordlager som representeras i grundlagret JG2. Sådana underliggande jordlager har kartlagts endast då de bedömts vara av stor praktisk betydelse, såsom t ex sand- och gruslager under lera och lera under sand- och gruslager. Kartläggningen är långt ifrån heltäckande och frånvaron av ett underliggande lager i data kan inte tas som intäkt för att ett sådant jordlager inte existerar. Det underliggande lagrets avgränsning bygger ofta på borrningar och är mycket osäker. Underliggande lager är inte knutet till något visst djupintervall. JD3 underlagrar i förekommande fall JG2.
Copyright Text:
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MaxRecordCount: 2000
Supported Query Formats: JSON, geoJSON, PBF
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Supports Statistics: true
Has Labels: false
Can Modify Layer: true
Can Scale Symbols: false
Use Standardized Queries: true
Supports Datum Transformation: true
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Supports Query Analytic: true
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Symbol:-
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Outline:-
N/A
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Outline:-
N/A
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Symbol:-
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Outline:-
N/A
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Outline:-
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Outline:-
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Label: Isälvssediment, sand
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Symbol:-
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Outline:-
N/A
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Label: Moränlera eller lerig morän
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Symbol:-
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Outline:-
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Layer: Jordart, grundlager (100)
Parent Layer: Jordartskartan, Sveriges geologiska undersökningName: Jordart, grundlager
Display Field: JG2_TX
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: Grundlagret ger en heltäckande bild av jordarternas utbredning i eller nära markytan. Lagret avser den jordartstyp som normalt kan förväntas på karteringsdjup, dvs. ca 0,5 m under markytan, och som bedöms ha en mäktighet väl överstigande 0,5 meter. Dessutom redovisas i detta lager områden där berggrunden går i dagen eller endast täcks av tunna eller osammanhängande jordlager.
Service Item Id: 1ff6144fb54c4c9c8302821ba94bb800
Copyright Text:
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MaxRecordCount: 2000
Supported Query Formats: JSON, geoJSON, PBF
Min Scale: 0.0
Max Scale: 0.0
Supports Advanced Queries: true
Supports Statistics: true
Has Labels: false
Can Modify Layer: true
Can Scale Symbols: true
Use Standardized Queries: true
Supports Datum Transformation: true
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Supports Percentile Statistics: true
Supports Having Clause: true
Supports Count Distinct: true
Supports Time Relation: true
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Description: Jorddjupsmodel beräknad 2014-02-04. Kartans syfte är att ge en generell bild av jordtäckets mäktighet. Kartan grundas på analys av jorddjupsinformation från brunnsborrningar, undersökningsborrningar, schakter och seismiska undersökningar. För att identifiera områden där jordtäcket är mycket tunt eller saknas helt har information om berg från SGUs jordartskartor använts. Jorddjupet har beräknats genom att interpolera kända jorddjupsdata. Eftersom vissa jordarter uppvisar betydligt större jorddjup än andra har jordartskartan använts som stöd vid denna interpolering. Information om sprickzoner i berggrunden har använts för att ta fram områden med speciellt stora jorddjup. Osäkerheten i beräkningarna ökar med avståndet till punkter med uppmätta jorddjup. Om avståndet exempelvis är flera hundra meter till närmaste observation är osäkerheten i det beräknade jorddjupet betydande. Ny information om jorddjup tillkommer hela tiden vilket gör att kartan successivt kan förbättras. Kartan kommer därför att uppdateras ungefär en gång per år. Vi tar hjälp av jordarter för att beräkna jorddjup. Datakällor: • Jorddjup: SGUDW.JORDDJUP • BARK-Brunnsarkivet ,HALL-Hällpunkter berggrundskartering, JRAF-Isräfflor,JSTR-Jordlagerföljder, PETR-Petrofysikdatabas • Hällpunkterjordartskartering: GDWJORD.JKAR_(A,BCDEG)_HALL_P_VY • Hällytor JBAS = 10,11(Berg,tunt jordtäcke)GDWJORD.JKAR_(A,BCDEG,N,M,R)_JBAS_VY • Jordarter: GDWJORD.JKAR_(A,BCDEG,N,M,R)_JBAS_VY • Deformationszoner: • SGUDW.(BELA,BELO)_STRL_LEV_LINE . Deformationszon, ospecificerad,Spröd deformationszon (förkastning, spricka, sprickzon) • Höjd: DEM \sgudb\sgudw\geofysik\strand_dw\DEM\demlake50 • 50x50m höjdraster ifrån Lantmäteriet, kompleterat med djup i hav samt stora sjöar. • Modell: • JORDKLASSER JBAS : • Lera,silt[2,3]; • Morän,moränlera[8,9]; • Isälvssediment,sand-block[7] • Sand[4]; • Grus[5]; • (Organisk jordart-torv[1], tar medelvärde ifrån alla punkter vid interpolering) • (;Berg,tunt jordtäcke[10,11] = 0, jorddjup = 0)
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