Official Series Description


Lab Data Summary

Aggregate lab data for the FLASHER soil series. This aggregation is based on all pedons with a current taxon name of FLASHER, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to FLASHER were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
5478P01551977ND001010Flasher7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9986111,-102.1669444
5481ND03700181ND037001Flasher3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.4302778,-101.465

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FLASHER soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the FLASHER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the FLASHER series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the FLASHER series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with FLASHER share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the FLASHER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the FLASHER series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with FLASHER, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. ND-2010-09-27-16 | Morton County - 2002

    Typical pattern of soils and underlying materials in the Ekalaka-Lakota-Vebar-Desart association (Soil Survey of Morton County, North Dakota; 2002).

  2. ND-2010-09-27-18 | Morton County - 2002

    Typical pattern of soils and underlying materials in the Vebar-Parshall association (Soil Survey of Morton County, North Dakota; 2002).

  3. ND-2012-02-07-01 | Adams County - September 1987

    Typical pattern of soils and underlying material in the Vebar-Flasher-Parshall association (Soil Survey of Adams County, North Dakota; September 1987).

  4. ND-2012-02-07-03 | Adams County - September 1987

    Typical pattern of soils and underlying material in the Belfield-Daglum-Rhoades association (Soil Survey of Adams County, North Dakota; September 1987).

  5. ND-2012-02-07-41 | Golden Valley County - July 1989

    Typical pattern of soils and parent material in the Absher-Belfield association (Soil Survey of Golden Valley County, North Dakota; July 1989).

  6. ND-2012-02-07-42 | Golden Valley County - July 1989

    Typical pattern of soils and parent material in the Flasher-Vebar-Beisigl association (Soil Survey of Golden Valley County, North Dakota; July 1989).

  7. ND-2012-02-08-06 | Grant County - September 1988

    Typical pattern of soils and parent material in the Vebar-Parshall-Beisigl association (Soil Survey of Grant County, North Dakota; September 1988).

  8. ND-2012-02-08-07 | Grant County - September 1988

    Typical pattern of soils and parent material in the Telfer-Lihen-Seroco association (Soil Survey of Grant County, North Dakota; September 1988).

  9. ND-2012-02-08-09 | Hettinger County - May 1990

    Typical pattern of soils and underlying material in the Vebar-Parshall-Flasher association (Soil Survey of Hettinger County, North Dakota; May 1990).

  10. ND-2012-02-08-30 | Mountrail County - June 1991

    Typical pattern of soils and parent material in the Cabba-Badland association (Soil Survey of Mountrail County, North Dakota; June 1991).

  11. SD-2012-03-15-09 | Corson County - July 1995

    Pattern of soils and parent material in the Flasher-Vebar association (Soil Survey of Corson County, SD; 1995).

Map Units

Map units containing FLASHER as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D32129921711vzssmt02519911:24000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F1843422461vzsvmt02519911:24000
Tally-Flasher complex, 4 to 25 percent slopes21610495342453chbwmt02719791:24000
Tally-Flasher-Rock outcrop complex, 25 to 45 percent slopes1039428342328ch6vmt02719791:24000
Tally-Flasher complex, 25 to 45 percent slopes2176277342454chbxmt02719791:24000
Flasher fine sandy loam, 4 to 20 percent slopesFf4768345419clfkmt10319611:20000
Flasher loamy fine sandFm2840345421clfmmt10319611:20000
Flasher fine sandy loam, 20 to 35 percent slopesFh2777345420clflmt10319611:20000
Bainville-Flasher complex, 15 to 40 percent slopesBh15941345611clmrmt10919561:31680
Rockland-Flasher complex, 15 to 50 percent slopesRk8141345655clp5mt10919561:31680
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F68133456291vzsvmt10919561:31680
Flasher loamy fine sand, 10 to 14 percent slopesFd6411345628cln9mt10919561:31680
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D56843456621vzssmt10919561:31680
Flasher loamy fine sand, 4 to 9 percent slopesFc4013345627cln8mt10919561:31680
Bainville-Flasher complex, 6 to 14 percent slopesBg1170345610clmqmt10919561:31680
Beisigl-Flasher-Telfer loamy fine sands, 6 to 15 percent slopesE1403D5265825257341vzstnd00119831:20000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F1289725257361vzswnd00119831:20000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F348725257351vzsvnd00119831:20000
Flasher-Beisigl, very stony-Parshall complex, 6 to 70 percent slopesE1431F57927556442rdb5nd00119831:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D39627556431vzssnd00119831:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D1411017151761vzssnd00719981:24000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F610726990511vzsvnd00719981:24000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F31426990521vzswnd00719981:24000
Beisigl-Flasher-Telfer loamy fine sands, 6 to 15 percent slopesE1403D1901525635251vzstnd01119691:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D343325636271vzssnd01119691:20000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F211125635531vzsvnd01119691:20000
Flasher-Beisigl, very stony-Parshall complex, 6 to 70 percent slopesE1431F61525635522rdb5nd01119691:20000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F26525635541vzswnd01119691:20000
Flasher-Vebar complex, 9 to 15 percent slopesFhD21599282212b3jnd01119691:20000
Flasher and Vebar very stony soils, 3 to 25 percent slopesFm8299282312b3knd01119691:20000
Vebar-Flasher fine sandy loams, 6 to 9 percent slopesVfC2799291812b6mnd01119691:20000
Vebar-Flasher fine sandy loams, 9 to 15 percent slopesVfD1399291912b6nnd01119691:20000
Flasher-Vebar complex, 9 to 15 percent slopesC952D968425641842q76knd01519671:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D721026616931vzssnd01519671:20000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F639726616941vzswnd01519671:20000
Flasher-Vebar-Rock outcrop complex, 15 to 70 percent slopesC955F431725641762q6m3nd01519671:20000
Livona-Lihen-Flasher complex, 9 to 35 percent slopesC369F107225641872q778nd01519671:20000
Flasher-Telfer loamy fine sands, 15 to 35 percent slopesC950F3425956622q76jnd01519671:20000
Flasher-Vebar-Parshall complex, 15 to 50 percent slopesC953F2025956562q1p3nd01519671:20000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F5563817146271vzsvnd02519811:20000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F1225317146281vzswnd02519811:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D33217146261vzssnd02519811:20000
Vebar-Arikara-Flasher complex, 9 to 50 percent slopesE1661F12127584731vzt0nd02519811:20000
Beisigl-Flasher-Telfer loamy fine sands, 6 to 15 percent slopesE1403D3527584721vzstnd02519811:20000
Flasher-Vebar complex, 15 to 70 percent slopesE1425F102252661749cdl4nd02919791:20000
Linton-Sutley-Flasher complex, 9 to 25 percent slopesE3807E14112661762d1xmnd02919791:20000
Vebar-Flasher complex, 9 to 15 percent slopesC978D85425954622q834nd02919791:20000
Flasher-Telfer loamy fine sands, 15 to 35 percent slopesC950F60025968382q76jnd02919791:20000
Flasher-Vebar-Parshall complex, 15 to 50 percent slopesC953F24725954562q1p3nd02919791:20000
Telfer-Flasher loamy fine sands, 6 to 15 percent slopesC335D14225643562pwffnd02919791:20000
Beisigl-Flasher-Telfer loamy fine sands, 6 to 15 percent slopesE1403D1887527072801vzstnd03319851:24000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F319127072811vzsvnd03319851:24000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D32827585471vzssnd03319851:24000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F6244025258701vzsvnd03719851:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D5376225258681vzssnd03719851:20000
Beisigl-Flasher-Telfer loamy fine sands, 6 to 15 percent slopesE1403D1921625258691vzstnd03719851:20000
Flasher-Beisigl, very stony-Parshall complex, 6 to 70 percent slopesE1431F615125258712rdb5nd03719851:20000
Vebar-Flasher complex, 6 to 15 percent slopes, very stonyE1655D371125258752rdb4nd03719851:20000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F36727596401vzswnd03719851:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D2221017185921vzssnd04119861:20000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F629725257931vzsvnd04119861:20000
Beisigl-Flasher-Telfer loamy fine sands, 6 to 15 percent slopesE1403D20127556771vzstnd04119861:20000
Flasher-Beisigl, very stony-Parshall complex, 6 to 70 percent slopesE1431F15025257942rdb5nd04119861:20000
Vebar-Flasher complex, 9 to 15 percent slopesC978D32825665422q834nd04719921:20000
Flasher-Vebar complex, 15 to 70 percent slopesE1425F3142661845cdl4nd04719921:20000
Flasher-Vebar-Parshall complex, 15 to 50 percent slopesC953F26025665232q1p3nd04719921:20000
Vebar-Flasher complex, 9 to 15 percent slopesC978D53325666282q834nd05119921:24000
Flasher-Vebar-Parshall complex, 15 to 50 percent slopesC953F6225666122q1p3nd05119921:24000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F3835427150561vzsvnd05320031:24000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D2032127150541vzssnd05320031:24000
Beisigl-Flasher-Telfer loamy fine sands, 6 to 15 percent slopesE1403D1330127150551vzstnd05320031:24000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F517727150581vzswnd05320031:24000
Vebar-Arikara-Flasher complex, 9 to 50 percent slopesE1661F309127150611vzt0nd05320031:24000
Flasher-Vebar complex, 9 to 15 percent slopesC952D33125667212q76knd05519741:20000
Vebar-Flasher-Zahl complex, 6 to 25 percent slopesC959E8525671582q836nd05519741:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D5326624531vzssnd05519741:20000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F498726992561vzswnd05719761:20000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F51417151001vzsvnd05719761:20000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F6292317183451vzsvnd05919981:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D3803417183431vzssnd05919981:20000
Beisigl-Flasher-Telfer loamy fine sands, 6 to 15 percent slopesE1403D1518017183441vzstnd05919981:20000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F820126991661vzswnd05919981:20000
Vebar-Arikara-Flasher complex, 9 to 50 percent slopesE1661F240717183471vzt0nd05919981:20000
Vebar-Flasher complex, 6 to 15 percent slopes, very stonyE1655D327596712rdb4nd05919981:20000
Vebar-Flasher-Zahl complex, 6 to 25 percent slopesC959E334425667792q836nd06119881:24000
Flasher-Vebar complex, 15 to 70 percent slopesE1425F18952662499cdl4nd06119881:24000
Flasher-Vebar-Parshall complex, 15 to 50 percent slopesC953F34925955672q1p3nd06119881:24000
Flasher-Vebar complex, 9 to 15 percent slopesC952D125671072q76knd06119881:24000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F188525259221vzswnd06519711:20000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F4139626990901vzsvnd08519921:24000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D3124426991331vzssnd08519921:24000
Flasher-Vebar complex, 15 to 70 percent slopesE1425F74352699089cdl4nd08519921:24000
Badland-Flasher complex, 9 to 40 percent slopesE1499F43782699068d1w7nd08519921:24000
Linton-Sutley-Flasher complex, 9 to 25 percent slopesE3807E38492699102d1xmnd08519921:24000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F265026990881vzswnd08519921:24000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopes23101155337813cbj6nd08519921:24000
Flasher-Vebar complex, 35 to 70 percent slopes23081121337811cbj4nd08519921:24000
Linton-Sutley-Flasher complex, 9 to 25 percent slopes231780337820cbjfnd08519921:24000
Beisigl-Flasher-Telfer loamy fine sands, 6 to 15 percent slopesE1403D713427073981vzstnd08719741:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D475727073971vzssnd08719741:20000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F250017167791vzsvnd08719741:20000
Flasher-Badland complex, 6 to 70 percent slopesE1495F85627074002qz6vnd08719741:20000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F4327073991vzswnd08719741:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesE1355D2505617134981vzssnd08919651:20000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesE1423F971617135001vzsvnd08919651:20000
Beisigl-Flasher-Telfer loamy fine sands, 6 to 15 percent slopesE1403D666717134991vzstnd08919651:20000
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopesE1475F606517135011vzswnd08919651:20000
Vebar-Arikara-Flasher complex, 9 to 50 percent slopesE1661F330317135051vzt0nd08919651:20000
Vebar-Flasher-Zahl complex, 9 to 25 percent slopes23591392339070cctrnd10519931:24000
Vebar-Flasher-Zahl complex, 6 to 25 percent slopesC959E133225670472q836nd10519931:24000
Vebar-Flasher-Tally fine sandy loams, 3 to 9 percent slopes2360338339071cctsnd10519931:24000
Flasher loamy fine sand, 25 to 50 percent slopes32F637354704cx32sd02119781:20000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesCvD6049328378701vzsssd03119861:24000
Flasher-Vebar-Parshall complex, 9 to 35 percent slopesFtF545573561621vzsvsd03119861:24000
Flasher-Rock outcrop complex, 30 to 60 percent slopesFrF1871356161cym2sd03119861:24000
Vebar-Flasher complex, 2 to 9 percent slopesVfB15991354250cwmfsd04119721:24000
Flasher-Vebar complex, 6 to 15 percent slopesFvD8991354193cwklsd04119721:24000
Flasher-Vebar complex, 15 to 25 percent slopesFvE3421354194cwkmsd04119721:24000
Flasher loamy fine sand, 25 to 40 percent slopesFbF727354192cwkksd04119721:24000
Vebar-Flasher-Tally complex, 9 to 15 percent slopesVaD630193546681vzsssd10519771:24000

Map of Series Extent

Approximate geographic distribution of the FLASHER soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .