Official Series Description


Lab Data Summary

Aggregate lab data for the GOLDENDALE soil series. This aggregation is based on all pedons with a current taxon name of GOLDENDALE, 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 GOLDENDALE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
640A1005S1958WA039005GOLDENDALE3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.752224,-121.1333313
683P0253S1982WA039001GOLDENDALE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7436104,-121.1691666
683P0255S1982WA039003GOLDENDALE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7591667,-121.1777802
840A0997S1958WA039003GOLDENDALE5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8247223,-120.7194443
840A1004S1958WA039004Goldendale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7808342,-120.8427811

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GOLDENDALE 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.

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Sibling Summary

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

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

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Geomorphic description summaries for the GOLDENDALE 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 .

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

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

Competing Series

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

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

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Geomorphic description summaries for the GOLDENDALE 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 .

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

Soil series sharing subgroup-level classification with GOLDENDALE, 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. WA-2010-11-05-07 | Klickitat County - 2009

    Representative landscape cross section of the Goldendale-Lorena general soil map unit (Soil Survey of Klickitat County, Washington; 2009).

  2. WA-2010-11-05-11 | Klickitat County - 2009

    Representative landscape cross section of the Swalecreek-Niva-Konner general soil map unit (lower part of diagram) (Soil Survey of Klickitat County, Washington; 2009).

  3. WA-2012-05-11-45 | Klickitat County Area - December 2009

    Representative landscape cross-section of general soil map unit 7 (Soil Survey of Klickitat County Area, Washington; December 2009).

  4. WA-2012-05-11-49 | Klickitat County Area - December 2009

    Representative landscape cross-section of general soil map unit 16 (lower part of diagram) (Soil Survey of Klickitat County Area, Washington; December 2009).

Map Units

Map units containing GOLDENDALE 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
Goldendale silt loam, basalt substratum, 5 to 10 percent slopes69A12088764292kjgwa63920031:24000
Goldendale silt loam, basalt substratum, 2 to 5 percent slopes6911243764282kjfwa63920031:24000
Goldendale silt loam, 2 to 5 percent slopes937569765632knswa63920031:24000
Goldendale silt loam, 5 to 10 percent slopes93A5425765662knwwa63920031:24000
Goldendale silt loam, basalt substratum, 10 to 15 percent slopes69B2660764302kjhwa63920031:24000
Goldendale silt loam, 10 to 15 percent slopes93B1471765672knxwa63920031:24000
Goldendale-Lorena-Rockly complex, 30 to 65 percent slopes9911059765962kpvwa63920031:24000
Goldendale silt loam, basalt substratum, 10 to 15 percent slopes969B1036765842kpgwa63920031:24000
Oreoke-Goldendale-Rock outcrop complex, 25 to 50 percent slopes10961014761472k7cwa63920031:24000
Goldendale silt loam, 15 to 30 percent slopes93C967765682knywa63920031:24000
Goldendale silt loam, 10 to 15 percent slopes993B856765982kpxwa63920031:24000
Goldendale silt loam, 15 to 30 percent slopes993C745765992kpywa63920031:24000
Goldendale-Lorena-Rockly complex, 2 to 30 percent slopes990663765952kptwa63920031:24000
Goldendale silt loam, basalt substratum, 15 to 30 percent slopes969C618765852kphwa63920031:24000
Goldendale-Tekison complex, 2 to 15 percent slopes1012548761252k6nwa63920031:24000
Goldendale-Tekison complex, 15 to 30 percent slopes1013528761262k6pwa63920031:24000
Tronsen-Goldendale-Horseflat complex, 15 to 30 percent slopes1017512761302k6twa63920031:24000
Goldendale silt loam, 5 to 10 percent slopes993A389765972kpwwa63920031:24000
Goldendale silt loam, basalt substratum, 5 to 10 percent slopes969A356765832kpfwa63920031:24000
Goldendale silt loam, 30 to 65 percent slopes93D342765692knzwa63920031:24000
Goldendale-Rockly complex, 30 to 65 percent slopes1016319761292k6swa63920031:24000
Goldendale-Lorena complex, 15 to 30 percent slopes1093305761462k7bwa63920031:24000
Goldendale silt loam, 30 to 65 percent slopes993D276766002kpzwa63920031:24000
Tekison-Goldendale complex, 30 to 65 percent slopes1014175761272k6qwa63920031:24000
Goldendale silt loam, 2 to 15 percent slopes79347765182kmbwa63920031:24000
Goldendale silt loam, basalt substratum, 2 to 5 percent slopes96936765822kpdwa63920031:24000
Goldendale silt loam, basalt substratum, 15 to 30 percent slopes69C17764312kjjwa63920031:24000
Goldendale silt loam, 35 to 60 percent slopes5605670867792x9bwa67620141:12000
Goldendale silt loam, 12 to 20 percent slopes563660862922wsmwa67620141:12000
Goldendale silt loam, 20 to 35 percent slopes5604640867492x8cwa67620141:12000

Map of Series Extent

Approximate geographic distribution of the GOLDENDALE 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 .