Official Series Description


Lab Data Summary

Aggregate lab data for the GREYLOCK soil series. This aggregation is based on all pedons with a current taxon name of GREYLOCK, 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 GREYLOCK 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
94B91P013190MI097003Greylock3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.0241623,-84.5360184
94B91P013290MI097004Greylock1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1988907,-85.7905579
94B91P013390MI097005Greylock6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1869431,-85.7977295

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GREYLOCK 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 GREYLOCK 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 GREYLOCK 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 GREYLOCK 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 mountains figure.

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Competing Series

Soil series competing with GREYLOCK 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 GREYLOCK 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 GREYLOCK 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 mountains figure.

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

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Soil series sharing subgroup-level classification with GREYLOCK, 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

No block diagrams are available.

Map Units

Map units containing GREYLOCK 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
Escanaba-Greylock complex, 1 to 6 percent slopes248B441414553901kvg2mi00320071:24000
Greylock-Cookson fine sandy loams, 1 to 6 percent slopes286B238614554251kvh6mi00320071:24000
Greylock fine sandy loam, 1 to 6 percent slopes251B219214553951kvg7mi00320071:24000
Escanaba-Greylock complex, 6 to 15 percent slopes248D218014553911kvg3mi00320071:24000
Greylock fine sandy loam, 6 to 15 percent slopes251D109414553961kvg8mi00320071:24000
Escanaba-Greylock complex, 15 to 35 percent slopes248E33814553921kvg4mi00320071:24000
Greylock fine sandy loam, 1 to 6 percent slopes27B9639416386fz8tmi09719941:20000
Greylock-Adams complex, 0 to 6 percent slopes100B2811416304fz65mi09719941:20000
Greylock fine sandy loam, 6 to 15 percent slopes27D2258416387fz8vmi09719941:20000
Greylock fine sandy loam, 35 to 60 percent slopes27F675416388fz8wmi09719941:20000
Greylock-Adams complex, 6 to 15 percent slopes100D390416305fz66mi09719941:20000
McMillan-Greylock fine sandy loams, 1 to 6 percent slopes62B598614569831kx3gmi15320071:24000
McMillan-Greylock fine sandy loams, 6 to 15 percent slopes62D176914570221kx4qmi15320071:24000
Greylock-McMillan fine sandy loams, 15 to 35 percent slopes62E77314570211kx4pmi15320071:24000
Escanaba-Greylock complex, 1 to 6 percent slopes248B36614569221kx1hmi15320071:24000
Greylock fine sandy loam, 6 to 15 percent slopes531D27914570491kx5lmi15320071:24000
Greylock fine sandy loam, 1 to 6 percent slopes531B22014570501kx5mmi15320071:24000

Map of Series Extent

Approximate geographic distribution of the GREYLOCK 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 .