Official Series Description


Lab Data Summary

Aggregate lab data for the LOS GATOS soil series. This aggregation is based on all pedons with a current taxon name of LOS GATOS, 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 LOS GATOS 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
15UCD541101854-CA-11-018LOS GATOS1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7162552,-122.6012192
15UCD585203058-CA-52-030LOS GATOS2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1472092,-122.6937332

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LOS GATOS 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 LOS GATOS 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 LOS GATOS 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 LOS GATOS 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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Competing Series

Soil series competing with LOS GATOS 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 LOS GATOS 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 LOS GATOS 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 LOS GATOS, 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 LOS GATOS 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
Los Gatos loam, 30 to 50 percent slopesLeF18695455816h99rca01319731:24000
Los Gatos loam, 50 to 75 percent slopesLeG4840455817h99sca01319731:24000
Los Osos-Los Gatos complexLk4145455821h99xca01319731:24000
Los Gatos loam, 15 to 30 percent slopesLeE715455815h99qca01319731:24000
Maymen-Los Gatos gravelly loams, 30 to 65 percent slopesMdoE6645458710hdb3ca02119611:20000
Los Gatos gravelly loam, schist bedrock, 30 to 50 percent slopeLvE1420458688hd9dca02119611:20000
Los Gatos gravelly loam, 30 to 50 percent slopes, MLRA 15LuE12734586852wv93ca02119611:20000
Los Gatos gravelly loam, schist bedrock, 50 to 65 percent slopeLvF1253458689hd9fca02119611:20000
Los Gatos-Parrish gravelly loams, 30 to 50 percent slopesLyE584458691hd9hca02119611:20000
Los Gatos-Josephine gravelly loams, 30 to 50 percent slopesLxE532458690hd9gca02119611:20000
Maymen-Los Gatos gravelly loams, 10 to 30 percent slopesMdoD501458709hdb2ca02119611:20000
Los Gatos gravelly loam, 50 to 65 percent slopes, MLRA 15LuF2534586862wv95ca02119611:20000
Los Gatos gravelly loam, schist bedrock, 10 to 30 percent slopeLvD114458687hd9cca02119611:20000
Los Gatos gravelly loam, 50 to 75 percent slopesLkG5930455647h949ca05319721:24000
Los Gatos gravelly loam, 30 to 50 percent slopes, thermic, high precipitation, MLRA 15LkF18804556462wv92ca05319721:24000
Maymen-Los Gatos complex, 50 to 75 percent slopes1629155458986hdm0ca05519741:24000
Los Gatos loam, 30 to 50 percent slopes1591995458983hdlxca05519741:24000
Los Gatos loam, 50 to 75 percent slopes1601660458984hdlyca05519741:24000
Los Gatos loam, 5 to 30 percent slopes158425458982hdlwca05519741:24000
Maymen-Los Gatos complex, 30 to 75 percent slopes, MLRA 15MlGsn548165162wv8tca05519741:24000
Los Gatos clay loam, 30 to 50 percent slopes, eroded, thermic, MLRA 15LvF227184562282wv8rca06919651:20000
Los Gatos clay loam, 15 to 30 percent slopesLvE2624456227h9r0ca06919651:20000
Los Gatos rocky clay loam, 15 to 50 percent slopes, ero dedLwF2517456229h9r2ca06919651:20000
Los Gatos clay loam, 30 to 50 percent slopes20221525150352mxvdca06919651:20000
Maymen-Los Gatos loams, 15 to 75 percent slopes, severe ly erodedMeG312624456093h9lpca09519691:24000
Los Gatos loam, 30 to 75 percent slopes, MLRA 15LkG2337127477322tb6yca09719681:20000
Los Gatos gravelly loam, 30 to 75 percent slopesLmG8720459816hfgsca09719681:20000
Los Gatos-Josephine complex, 30 to 75 percent slopesLnG1974459817hfgtca09719681:20000
Hugo-Los Gatos complex, 50 to 75 percent slopesHrG989459775hffgca09719681:20000
Maymen-Los Gatos complex, 30 to 75 percent slopes, MLRA 15MlG9404598302wv8tca09719681:20000
Los Gatos-Los Osos complex, 30 to 75 percent slopes, eroded, MLRA 15LpF227477312tb6zca60919631:20000
Gaviota-Los Gatos complex, 30 to 50 percent slopes, MLRA 15GmFes27477252stj3ca60919631:20000
Los Gatos loam, 50 to 75 percent slopesLeGcc115045017m49ca60919631:20000
Los Gatos gravelly loam, 30 to 50 percent slopes, thermic, low precipitation, MLRA 15LfFes7004542wv91ca60919631:20000
Los Gatos-Gaviota complex, 50 to 75 percent slopesLhGes700455rhwbca60919631:20000
Los Gatos loam, 30 to 50 percent slopesLeFcc801718vx7wca60919631:20000
Los Osos-Los Gatos complexLkcc801721vx7zca60919631:20000
Los Gatos-Los Osos complex, 30 to 45 percent slopes, eroded, thermic, MLRA 15LpE211934565932wv8sca60919631:20000
Maymen-Los Gatos complex, 30 to 75 percent slopes, low precipitation, MLRA 1512719444566802wv8vca61019751:24000
Los Gatos-Los Osos complex, 50 to 75 percent slopes119483456672hb6cca61019751:24000
Los Gatos loam, very steepLzF57456459h9zhca63719581:15000
Los Gatos clay loam, steep, erodedLyE224456458h9zgca63719581:15000
Los Gatos clay loam, sloping, erodedLyC218456457h9zfca63719581:15000
Gaviota-Los Gatos complex, 30 to 50 percent slopes, MLRA 15405168027477262stj3ca64120091:24000
Los Gatos-Gaviota complex, 50 to 75 percent slopes40780424354742mr9pca64120091:24000
Los Gatos gravelly loam, 50 to 75 percent slopes4061924354732mr9nca64120091:24000
Los Gatos-Maymen gravelly loams, 30 to 65 percent slopesLhE6522460808hghsca64519611:20000
Los Gatos gravelly loam, loamy-skeletal, 30 to 50 percent slopes, MLRA 15LgE63644608062wv94ca64519611:20000
Parrish-Los Gatos gravelly loams, 30 to 50 percent slopesPgE3382460900hglrca64519611:20000
Los Gatos gravelly loam, loamy-skeletal, 50 to 65 percent slopes, MLRA 15LgF22594608072wv8xca64519611:20000
Los Gatos-Gaviota complex, 50 to 75 percent slopesLhG62301457017hbkhca64619671:24000
Los Gatos gravelly loam, 50 to 75 percent slopesLfG8941457016hbkgca64619671:24000
Los Gatos gravelly loam, 30 to 50 percent slopes, thermic, low precipitation, MLRA 15LfF19754570152wv91ca64619671:24000
Los Gatos gravelly loam, 15 to 30 percent slopes, erodedLfE2322457014hbkdca64619671:24000
Los Gatos-Los Osos complex, 45 to 75 percent slopes, erodedLpF2aa159699384rgrsca64619671:24000
Los Gatos-Los Osos complex, 30 to 45 percent slopes, eroded, thermic, MLRA 15LpE2626993882wv8sca64619671:24000
Los Gatos clay loam, 30 to 50 percent slopes, eroded, thermic, MLRA 15LvF2sb36996822wv8rca64619671:24000
Gaviota-Los Gatos complex, 30 to 50 percent slopes, MLRA 15GmF127477272stj3ca64619671:24000
Los Gatos loam, 30 to 75 percent slopes, MLRA 15115569627477332tb6yca68919851:24000
Xerolls, loamy-skeletal-Los Gatos complex, 30 to 75 percent slopes7002055466574hnhsca69120081:24000
Pass Canyon-Los Gatos families complex, 1 to 20 percent slopes.228mf213190621221zkqca70219841:24000
Pass Canyon-Los Gatos families complex, 1 to 20 percent slopes.22831770470543hsmtca70319831:24000
Stukel-Los Gatos pas canyon families complex, 1 to 10 percent slopes.26710183470580hsp0ca70319831:24000
Ridd-Los Gatos-Grin families association, 5 to 35 percent slopes.2379272470551hsn2ca70319831:24000
Los Gatos family-Lithic Haploxeralfs association, 0 to 15 percent slopes.61la43643059826ht4nca70719831:24000
Los Gatos family-Lithic Haploxeralfs association, 0 to 15 percent slopes.61547471034ht4nca70819841:24000
Los Gatos-Kilburn-Panamint families association, 30 to 60 percent slopes2141788465287hm58ca77219811:24000
Los Gatos-Kilburn-Panamint families association, 10 to 30 percent slopes2019884465286hm57ca77219811:24000

Map of Series Extent

Approximate geographic distribution of the LOS GATOS 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 .