Official Series Description


Lab Data Summary

Aggregate lab data for the GLENDALE soil series. This aggregation is based on all pedons with a current taxon name of GLENDALE, 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 GLENDALE 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
3040A3198S1956NV003005GLENDALE5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1805458,-115.0666656
3040A3200S1956NV003006GLENDALE5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1588821,-115.058609
4240A0795S1960NM013015Glendale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4734612,-106.6602936

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GLENDALE 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 GLENDALE 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 GLENDALE 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 GLENDALE 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 GLENDALE 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 GLENDALE 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 GLENDALE 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 hills figure.

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

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Click the image to view it full size.

Soil series sharing subgroup-level classification with GLENDALE, 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. AZ-2011-05-27-03 | Beaver Creek Area - 1967

    Typical section of soils, lower part of Beaver Creek Area. Elevation at Courthouse Butte is approximately 5,000 feet (Soil Survey of Beaver Creek Area, Arizona; 1967).

Map Units

Map units containing GLENDALE 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
Gila-Glendale complex, dry, 1 to 3 percent slopes47412515079101mm38az62720051:24000
Gila-Glendale complex, 1 to 3 percent slopes46119915079091mm37az62720051:24000
Glendale silt loamGt230015453001nw0daz64119651:31680
Glendale gravelly silt loam, 0 to 5 percent slopesGeB1019802854vyfjaz64319671:31680
Glendale gravelly fine sandy loam, 0 to 10 percent slopesGdC73815274451n8ffaz64319671:31680
Glendale-Hantz complex, 0 to 5 percent slopes473822581587mj5waz66120091:24000
Gila and Glendale soils, 0 to 2 percent slopesGgA10610536151ssjaz66219661:20000
Glendale loamGm2080536161sskaz66219661:20000
Glendale silt loam, salineGn1200536171sslaz66219661:20000
Tidwell, Gila, and Glendale soils, saline, 0 to 2 percent slopesTgA1140536421stdaz66219661:20000
Glendale silt loam, saline-alkaliGo1010536181ssmaz66219661:20000
Glendale silty clay loam, salineGp720536191ssnaz66219661:20000
Glendale-Gila complex, 0 to 5 percent slopes, severely eroded1613780544381tn2az66319791:24000
Glendale silty clay loam, 0 to 2 percent slopes**151085544371tn1az66319791:24000
Glendale-Gila complex, eroded2329655536641sv3az66419751:24000
Glendale-Gila association, frequently flooded246491536651sv4az66419751:24000
Glendale-Gila complex222878536631sv2az66419751:24000
Gila-Glendale complex, chihuahuan, 0 to 2 percent slopes403330679607qt5taz66620071:24000
Glendale-Hantz complex, chihuahuan, 0 to 3 percent slopes431100802947vyjjaz66620071:24000
Gila-Glendale complex, sonoran, 0 to 2 percent slopes4160016931741ttwjaz66620071:24000
Glendale-Hantz complex, sonoran, 0 to 3 percent slopes4438016931711ttwfaz66620071:24000
Glendale silty clay loam, 0 to 1 percent slopes421506012320kgaz66620071:24000
Glendale silty clay loamGe1341543641tkpaz66819681:20000
Glendale silty clay loam, severely erodedGe31234543651tkqaz66819681:20000
Glendale loamGd1129543631tknaz66819681:20000
Glendale silt loam, 0 to 3 percent slopes3026039538071szqaz66919931:24000
Glendale-Bucklebar complex, 0 to 3 percent slopes294956537991szgaz66919931:24000
Glendale very fine sandy loam, 0 to 2 percent slopes722136549481v5jaz67120001:24000
Anthony and Glendale soils, and riverwash, 0 to 3 percent slopes4668215923611qfzhaz67520091:24000
Glendale-Gila complex, 0 to 3 percent slopes363426592561znhaz67520091:24000
Glendale-Gila complex, saline-sodic, 0 to 3 percent slopes37252114278031jxr5az67520091:24000
Urban land-Agustin-Glendale complex, 1 to 5 percent slopes92132815920791qfpdaz67520091:24000
Glendale clay loam, 0 to 2 percent slopes, flooded2827738545821tsqaz70319931:24000
Glendale silt loam, 1 to 3 percent slopes2915833545851tstaz70319931:24000
Glendale-Pajarito complex, 1 to 3 percent slopes308888545891tsyaz70319931:24000
GLENDALE VARIANT SILT LOAM, SALINE-ALKALI1252300463944hkryca67119781:24000
Mimbres and Glendale silty clay loamsMD33995570311xbqnm02319671:31680
Mimbres and Glendale silty clay loamsMc12475570352sprrnm02319671:31680
Glendale-Arizo complexGD10622570131xb4nm02319671:31680
Mimbres and Glendale silty clay loams, alkaliMe2932570362vsrwnm02319671:31680
Mimbres and Glendale loamsMb1493570342spt9nm02319671:31680
Mimbres and Glendale silty clay loams, strongly alkalMg1221570372sprsnm02319671:31680
Glendale silty clay loamGc535570171xb8nm02319671:31680
Glendale clay loam, 0 to 1 percent slopes MLRA 42.1Gm1960556482tm50nm60019731:24000
Glendale loam MLRA 42Gk1218556472spt5nm60019731:24000
Glendale clay loam, slightly salineGs321556491vx4nm60019731:24000
Glendale clay loam, 0 to 1 percent slopes MLRA 42.1Gs2175558002tm50nm61219701:24000
Glendale soils, slightly salineGt485558011w21nm61219701:24000
Glendale loam, strongly alkaliGr266557991w1znm61219701:24000
Glendale loamGo221557981w1ynm61219701:24000
Glendale-Harkey associationGHA9249375765dm0gnm64419811:24000
Glendale-Pecos-Harkey associationGPA5803375766dm0hnm64419811:24000
Glendale silt loamGbA3614375768dm0knm64419811:24000
Glendale-Gila complex, nearly level3712438565141wt1nm66019811:48000
Glendale clay loam, 0 to 1 percent slopes36729565132t8vxnm66019811:48000
Glendale loam35372565121wsznm66019811:48000
Armijo-Glendale-Bluepoint association, 0 to 3 percent slopes64814135571611xgxnm66419841:24000
Glendale clay loam, 0 to 1 percent slopes224014570891xdlnm66419841:24000
Glendale clay loam, occasionally flooded, 0 to 1 percent slopes2222044570901xdmnm66419841:24000
Glendale sandy loam, 0 to 1 percent slopes122337570821xdcnm66419841:24000
Vinton-Glendale associationVG9419560041w8lnm66619741:24000
Glendale fine sandy loamGe7307559601w75nm66619741:24000
Glendale loamGf5365559611w76nm66619741:24000
Glendale clay loam, 0 to 1 percent slopesGf199966345652t8vxnm6901:24000
Glendale loamGe7821634564p99tnm6901:24000
Glendale clay loam, alkaliGg595634566p99wnm6901:24000
Glendale loam, strongly salineGs5345469378hrf7nv60819671:24000
Glendale loamGr3032469377hrf6nv60819671:24000
Glendale fine sandGo1220469376hrf5nv60819671:24000
Glendale-Bluepoint association19001251478165j1kpnv75419921:24000
Anthony and Glendale soilsAg6443584591ytstx24319711:31680
Glendale soilsGe23514372521dhmttx44319641:31680
Glendale silty clayGs8259696625rcwstx62419671:31680
Glendale silty clay loamGe4689696624rcwrtx62419671:31680
Glendale loamGd935696623rcwqtx62419671:31680
Belen, Glendale and Popotosa soils, 0 to 1 percent slopes, occasionally floodedBGA2360325041892q3cmtx62720121:24000

Map of Series Extent

Approximate geographic distribution of the GLENDALE 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 .