Official Series Description


Lab Data Summary

Aggregate lab data for the TOMBSTONE soil series. This aggregation is based on all pedons with a current taxon name of TOMBSTONE, 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 TOMBSTONE 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
4186P083585AZ003091Tombstone7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.7477779,-109.9541702
4169C0207S1969AZ003001Tombstone7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.7316666,-110.0180588

Water Balance

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

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

Soil series sharing subgroup-level classification with TOMBSTONE, 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 TOMBSTONE 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
Tombstone-Caralampi-Eloma complex, 10 to 50 percent slopes1181485915079811mm5kaz62720051:24000
Tombstone soils, Luckyhills soils and Urban land, 2 to 10 percent slopes4382179582561ym7az63920121:24000
Tuzigoot soils, Tombstone soils and Urban land, 1 to 15 percent slopes4331624582531ym4az63920121:24000
Penthouse-Tombstone complex, 2 to 30 percent slopes441850582591ymbaz63920121:24000
Penthouse-Tombstone complex, 2 to 25 percent slopes54111582661ymkaz63920121:24000
Tombstone-Luckyhills complex, 2 to 10 percent slopes5388582221yl4az63920121:24000
Selevin-Tombstone-Saddlebrook complex, 3 to 45 percent slopes915820314788431lmvmaz66120091:24000
Pedregosa-Tombstone complex, 5 to 45 percent slopes642480017273231vzf3az66620071:24000
Tombstone-Stronghold complex, 5 to 30 percent slopes832350016774121t9h2az66620071:24000
Nolam-Tombstone complex, 8 to 30 percent slopes5138275538461t0zaz66919931:24000
Bernardino-Tombstone association, 5 to 16 percent slopes631920538641t1kaz66919931:24000
Tombstone very gravelly loam, 15 to 50 percent slopes7928559538921t2gaz66919931:24000
Pedregosa-Tombstone complex, 3 to 20 percent slopes1198432550601v94az67120001:24000
Tombstone very gravelly fine sandy loam, 8 to 15 percent slopes1427570549461v5gaz67120001:24000
Eloma-Tombstone-White House complex, 3 to 50 percent slopes213612525135852pzpnaz6731:24000
Pedregosa-Tombstone complex, 5 to 45 percent slopes3319924985612pznwaz6731:24000
Tombstone-Eloma-Pedregosa complex, 5 to 65 percent slopes mlra 38834600315915622rv8laz67520091:24000
Bigtoe-Ryallen-Tombstone complex, 3 to 30 percent slopes1044091592531zndaz67520091:24000
Tombstone-Torriorthents complex, 5 to 70 percent slopes849826592571znjaz67520091:24000
Tombstone-Eloma-Pedregosa complex, 5 to 65 percent slopes mlra 38595376524328462rv8laz6871:24000
Tombstone-Ustic Torriorthents complex, 5 to 70 percent slopes55166624328442mnkvaz6871:24000
Tombstone-Caralampi-Nolam families complex, 2 to 30 percent slopes14322064755705tcclaz69720051:24000
Pedregosa-Tombstone families complex, 1 to 15 percent slopes1108124755718tcd0az69720051:24000

Map of Series Extent

Approximate geographic distribution of the TOMBSTONE 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 .