Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

There are insufficient data to create the water balance bar figure.



There are insufficient data to create the water balance line figure.

Sibling Summary

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

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the RIVERWASH series and siblings. 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 RIVERWASH 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 .

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.

Competing Series

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

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the RIVERWASH 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 RIVERWASH 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 RIVERWASH, 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 .

This figure is not available.

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. CA-2011-05-27-04 | Mendocino County, Eastern Part, and Trinity County, Southwestern Part - 1991

    Pattern of terraces in Ukiah Valley and adjacent mountains (Soil Survey of Mendocino County, Eastern Part, and Trinity County, Southwestern Part, California; 1991).

  2. IN-2010-09-24-17 | Owen County -

    Typical pattern of soils and parent materials in the Stonelick-Gessie-McAdoo association (Soil Survey of Owen County, Indiana).

  3. NM-2010-09-13-02 | McKinley County -

    Generalized relationship of some soils in the survey area (Soil Survey of McKinley County, New Mexico).

  4. NM-2010-09-13-05 | McKinley County -

    Generalized cross section illustrating soil-geomorphic-geologic relationships of soils on the Chaco slope of the San Juan Basin (Soil Survey of McKinley County, New Mexico).

  5. TX-2010-11-02-01 | Big Bend National Park -

    Altuda, Bissett, Blackgap, Pantera, Riverwash, Stillwell, Strawhouse,

  6. TX-2010-11-02-05 | Big Bend National Park -

    Corazones, Geefour, Ninepoint, Pantera, Riverwash, Solis, Studybutte, Tornillo

  7. TX-2010-11-03-12 | Goliad County - 2010

    Pattern of soils and underlying material in the Papalote-Weesatche general soil map unit (Soil Survey of Goliad County, Texas; 2010).

  8. TX-2010-11-03-76 | Mason County -

  9. TX-2010-11-03-78 | Mason County -

  10. TX-2010-11-03-79 | Mason County -

  11. TX-2012-05-09-02 | Big Bend National Park - 2011

    Relationship of soil mapping units to elevation, geology, and landscape positions. Altuda soils are at elevations around 5,000 feet, and formed from the Santa Elena limestone. Blackgap and Bissett soils formed in residuum and colluvium (Soil Survey of Big Bend National Park, Texas; 2011).

  12. TX-2012-05-09-03 | Big Bend National Park - 2011

    Relationship of soil mapping units, geologic formations, and landscape positions of the Pen Clay, Aguja sandstone, loamy alluvium, and Javelina Formations (Soil Survey of Big Bend National Park, Texas; 2011).

  13. TX-2012-05-09-07 | Guadalupe Mountains National Park - 2010

    Patterns of soils and underlying material from the high country down the east escarpment onto the fan alluvium of the front range (Soil Survey of Guadalupe Mountains National Park, Texas; 2010).

  14. WI-2010-11-08-07 | Pepin County - 2002

    Typical pattern of soils and parent material in the Finchford-Plainfield-Burkhardt and Algansee-Kalmarville-Scotah associations (Soil Survey of Pepin County, Wisconsin; 2002).

  15. WI-2012-03-23-29 | Pepin County - March 1964

    Some of the principal soil series and their underlying material (Soil Survey of Pepin County, WI; 1964).

Map Units

Map units containing RIVERWASH 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
Riverwash and Niklavar soils, 0 to 2 percent slopes18210543503121pbzak60019961:24000
Riverwash and Niklavar soils, 0 to 2 percent slopes444286605140n9pnak60520011:25000
Riverwash162847692934r81qak61020031:25000
Riverwash-Nizina complex, 0 to 2 percent slopes4618185516741qrxak61219911:24000
Riverwash221849493351nbgak61519951:24000
Riverwash22931332494081ndtak63119861:31680
Stratify and Riverwash, 0 to 3 percent slopes3036492494281nfgak64019861:24000
Riverwash3226128494471ng2ak64019861:24000
Salchaket-Riverwash association, 0 to 3 percent slopes3235304494481ng3ak64019861:24000
Riverwash1243554517131qt5ak64119851:31680
Riverwash127983517631qvsak64219901:24000
Riverwash24243517991qwyak64319981:24000
RiverwashRW1394498351nvlak64419941:31680
Riverwash774307495731nl4ak64519921:31680
Cryofluvents-Riverwash association, 0 to 5 percent slopes53I20367501241p4xak64619921:31680
Riverwash, 0 to 5 percent slopes53R10214501261p4zak64619921:31680
RiverwashRv17511021q5gak65020061:24000
Riverwash64935314880841lygqak65220051:25000
RiverwashBA303314833591lsk9ak65620051:24000
Swedna-Riverwash-Dackey complexFPA110714833641lskgak65620051:24000
Dackey-Tangoe-Riverwash, high elevation, complexFPC85114833671lskkak65620051:24000
Dackey-Tangoe-Riverwash complexFPB85114833661lskjak65620051:24000
Schleyer-Broxson-Riverwash complexAFL52714833551lsk5ak65620051:24000
Nizina-Sinona-Riverwash complex, 0 to 12 percent slopesAFA51614833511lsk1ak65620051:24000
Kluna-Nizina-Maclaren complex, 0 to 20 percent slopes7FP0455543340608631d3bak65920241:63360
RiverwashRW3315730294502xfykak65920241:63360
Schleyer-Broxson-Riverwash complexAFL23133844781lsk5ak65920241:63360
Riverwash-Nizina complex, 0 to 2 percent slopes46122433546821qrxak65920241:63360
Riverwash6473199615421411nrqhak68320051:63360
Teedrinjik-Riverwash-Hodzana association, 0 to 3 percent slopesD32FP69343827370392snhtak68520201:63360
Typic Cryaquents, frequently flooded-Theodore-Riverwash association, 0 to 3 percent slopesD32FP11717627370332snhmak68520201:63360
RiverwashRW2062329058372w4s4ak69220211:63360
Riverwash-Oxyaquic Cryorthents complex, 0 to 5 percent slopes20RW2519232326332tpsrak69220211:63360
Riverwash-Oxyaquic Cryorthents complex, 0 to 5 percent slopes5300878528050752tpsrak69320191:63360
RiverwashRW634232332w4s4ak69320191:63360
Typic Cryaquents, frequently flooded-Theodore-Riverwash association, 0 to 3 percent slopesD32FP11533755562snhmak7391:250000
RiverwashRW833547662xfykak7661:250000
Kluna-Nizina-Maclaren complex, 0 to 20 percent slopes7FP042600335481131d3bak7691:250000
RiverwashRW3315733548902xfykak7751:250000
Kluna-Nizina-Maclaren complex, 0 to 20 percent slopes7FP049547335485931d3bak7751:250000
RiverwashRe167328196c0hzal00319611:20000
RiverwashRw129330489c2wyal08719971:24000
Riverwash, sandy, frequently flooded22225579297mft0ar00119951:24000
Alluvial land, frequently floodedMu286885652752rv6bar01719641:20000
RiverwashRIV27324953752pwx9ar07719741:20000
Riverwash-Ceda complex, 0 to 3 percent slopes, frequently flooded44B3795775252t5yvar09719971:24000
Riverwash, frequently flooded491369566032m003ar10119841:20000
RiverwashRIV66924953762pwx9ar10719711:20000
Riverwash-Ceda complex, 0 to 3 percent slopes, frequently flooded6928615429142t5yvar10920051:20000
Riverwash, frequently flooded722110566494m0h0ar12919871:20000
Riverwash-Torrifluvents complex, 1 to 3 percent slopes644026524111rjpaz62319941:24000
Riverwash5179525571rpdaz62519921:24000
Arizo-Franconia-Riverwash complex, dry, 1 to 3 percent slopes101867015078731mm22az62720051:24000
Carrizo-Riverwash complex, 3 to 8 percent slopes MLRA 30211514015078842ss19az62720051:24000
Dudleyville-Vinton-Riverwash complex, dry, 1 to 3 percent slopes701206715079331mm40az62720051:24000
Arizo-Franconia-Riverwash complex, 1 to 3 percent slopes91021215078721mm21az62720051:24000
Dudleyville-Vinton-Riverwash complex, 1 to 3 percent slopes69598215079321mm3zaz62720051:24000
Carrizo-Riverwash complex, 1 to 3 percent slopes22593915078851mm2gaz62720051:24000
Carrizo family-Riverwash complex, 1 to 3 percent slopes20514215078831mm2daz62720051:24000
Riverwash-Fluvaquents association, 0 to 3 percent slopes10224015079651mm51az62720051:24000
Jocity-Joraibi-Navajo-Riverwash complex, 0 to 2 percent slopes221210130510392v1cmaz63119801:24000
Ives-Riverwash complex, 1 to 5 percent slopes, rarely flooded107120225068812v1bgaz63119801:24000
Riverwash36190526691rt0az63119801:24000
Riverwash-Typic Torrifluvents complex, 0 to 5 percent slopes5017200542251tf6az63319941:24000
Riverwash-Ustic Torrifluvents complex, 0 to 5 percent slopes51820542261tf7az63319941:24000
RiverwashRH421017185281vp8daz63519681:31680
RiverwashRw315515454651nw5qaz64119651:31680
Riverwash5526667534761sn1az65319851:24000
RiverwashRv171535301spsaz65519691:20000
Carrizo family-Riverbend family-Riverwash complex, dry, 0 to 3 percent slopes39018084824402942mxb5az6571:24000
Brios-Riverwash complex, 0 to 1 percent slopes2102031924205482m7s6az6571:24000
Brios- Riverwash complex, dry, 0 to 3 percent slopes3801189131096302ybrxaz6571:24000
Queencreek-Riverwash complex, 0 to 3 percent slopes690216531934302z8vgaz6571:24000
Queencreek soils and riverwash, 0 to 5 percent slopes7830075581585mj5taz66120091:24000
Bodecker-Riverwash complex, 0 to 5 percent slopes61468014788402tdt7az66120091:24000
Hayhook-Riverwash complex, 1 to 5 percent slopes521183816127771r472az66120091:24000
Carrizo family-Brios-Riverwash complex, 0 to 5 percent slopes1190526010320jtaz66120091:24000
Cascabel soils, wetrock soils, and riverwash, 0 to 5 percent slopes132558610861nhn6az66120091:24000
Oxyaquic Torrifluvents-Riverwash complex, 0 to 5 percent slopes72118716520322svvnaz66120091:24000
RiverwashRh1330536371st7az66219661:20000
Torrifluvents-Riverwash complex, 1 to 5 percent slopes*4212355544671tp0az66319791:24000
Bodecker-Riverwash complex, 0 to 5 percent slopes76800601292tdt7az66620071:24000
Queencreek-Riverwash complex, chihuahuan, 0 to 5 percent slopes6534006010820jzaz66620071:24000
Rafter-Riverwash complex, 0 to 5 percent slopes671300189684321nthaz66620071:24000
Cascabel, quiburi soils, and riverwash, chihuahuan, 0 to 5 percent slopes171280802945vyjgaz66620071:24000
Queencreek-Riverwash complex, sonoran, 0 to 5 percent slopes66127516931641ttw6az66620071:24000
Cascabel, quiburi soils, and riverwash, sonoran, 0 to 5 percent slopes1838016931751ttwkaz66620071:24000
Keysto-Riverwash complex, 1 to 5 percent slopes522156012720klaz66620071:24000
RiverwashRu2171543941tlnaz66819681:20000
Arizo-Riverwash complex, 0 to 3 percent slopes533156538441t0xaz66919931:24000
Bodecker-Riverwash complex, 0 to 5 percent slopes1276800549432tdt7az67120001:24000
Keysto-Riverwash complex, 1 to 5 percent slopes945185550211v7waz67120001:24000
Hayhollow-Rafter-Riverwash complex, 0 to 5 percent slopes884330550471v8qaz67120001:24000
Brookline-Fluvaquents-Riverwash complex, 0 to 3 percent slopes173528550191v7taz67120001:24000
Arizo family-Riverwash complex, 0 to 3 percent slopes31706550271v82az67120001:24000
Quiburi-Fluvaquents-Riverwash complex, 0 to 5 percent slopes123815550291v84az67120001:24000
Riverwash, 1 to 10 percent slopes126772550551v8zaz67120001:24000
Rafter and Stanford soils and riverwash, 0 to 5 percent slopes35420825135812pzpjaz6731:24000
Bodecker-Altar-Riverwash complex, 1 to 10 percent slopes7404425135962pzq0az6731:24000
Bodecker-Riverwash complex, 0 to 5 percent slopes5357024985642tdt7az6731:24000
Queencreek soils and riverwash, 0 to 5 percent slopes3486825009522q0lraz6731:24000
Bodecker-Altar-Riverwash complex, 0 to 5 percent slopes665125135862pzppaz6731:24000
Oxyaquic Torrifluvents-Riverwash complex, 0 to 5 percent slopes302424985682svvnaz6731:24000
Queencreek-Brazito-Riverwash complex, 0 to 8 percent slopes6020759592601znmaz67520091:24000
Anthony and Glendale soils, and riverwash, 0 to 3 percent slopes4668215923611qfzhaz67520091:24000
Frazwell family-Riverwash complex, 0 to 2 percent slopes33487015971081qlxmaz67520091:24000
Rafter-Riverwash complex, 1 to 5 percent slopes61338914151511jhl1az67520091:24000
Bodecker soils and Riverwash, 0 to 5 percent slopes12324824200862vymkaz67520091:24000
Riverwash-Ubik-Oxyaquic Torrifluvents complex, 0 to 5 percent slopes653131592521zncaz67520091:24000
Ustifluvents soils, riverwash, rock outcrop, and water, 0 to 2 percent slopes94127724225132m9tlaz67520091:24000
Riverwash-Amuzet complex, 0 to 3 percent slopes6344924086102lvc3az67520091:24000
Paymaster family and Typic Fluvaquents soils and riverwash, 0 to 3 percent slopes5630324084362lv5haz67520091:24000
Queencreek soils and riverwash, 0 to 5 percent slopes5924223847892l1kpaz67520091:24000
Riverwash-Brazito-Oxyaquic Torrifluvents complex, 2 to 5 percent slopes64174592511znbaz67520091:24000
Bodecker soils and Riverwash, 0 to 5 percent slopes655119924328472vymkaz6871:24000
Oxyaquic Torrifluvents and Typic Fluvaquents soils and Riverwash, 0 to 5 percent slopes60031724554612nf3faz6871:24000
Oxyaquic Ustifluvents-Frazwell family-Riverwash complex, 0 to 3 percent slopes80029624842122pd0waz6871:24000
Courtland family-Riverwash complex, 0 to 15 percent slopes63512124416832myrzaz6871:24000
Oxyaquic Ustifluvents soils and Riverwash, 0 to 3 percent slopes80110224842532pd26az6871:24000
Oxyaquic Torrifluvents-Riverwash-Water complex, 0 to 5 percent slopes5475024342212mq08az6871:24000
Carrizo-Riverwash complex, 3 to 8 percent slopes MLRA 3017267087983652ss19az69720051:24000
Arizo-Franconia-Riverwash complex, 1 to 3 percent slopes626681798389vsshaz69720051:24000
Arizo-Riverwash complex, dry, 0 to 1 percent slopes912824798397vssraz69720051:24000
Carrizo-Riverwash complex, 0 to 1 percent slopes169446798364vsrpaz69720051:24000
Arizo-Riverwash complex, 1 to 4 percent slopes85251798355vsrdaz69720051:24000
Arizo-Riverwash complex, 0 to 1 percent slopes74831798394vssnaz69720051:24000
Arizo-Riverwash complex, moist, 1 to 3 percent slopes104387798375vss1az69720051:24000
Cordes-Manikan-Riverwash complex, 1 to 6 percent slopes22130113982741hy0maz69720051:24000
Mathis family-Riverwash complex, 1 to 4 percent slopes82606798481vswgaz69720051:24000
Arizo-Riverwash complex, 1 to 3 percent slopes35230544781tpcaz69919931:24000
Arizo-Riverwash complex, 0 to 3 percent slopes410522546101ttmaz70319931:24000
Keysto-Riverwash complex, 0 to 5 percent slopes382799546071ttjaz70319931:24000
Jocity-Joraibi-Navajo-Riverwash complex , 0 to 2 percent slopes2189711590572rqpsaz70720111:24000
Ives-Riverwash association, 0 to 2 percent slopes1814155590522rqpqaz70720111:24000
Ives-Riverwash complex, 1 to 5 percent slopes, rarely flooded10727730510502v1bgaz70720111:24000
Mido-Radnik-Riverwash complex, 1 to 8 percent slopes281584116022522rqs1az71120081:24000
Pinepoint-Aridic Ustorthents-Riverwash complex, 1 to 5 percent slopes36243316132032sdvjaz71120081:24000
Riverwash-Sheppard complex, 0 to 24 percent slopes4099122476532sdwsaz71120081:24000
Riverwash-Bebeevar complex, 0 to 3 percent slopes16186251566721by8az7121:24000
Tsosie-Councelor-Riverwash complex, 0 to 4 percent slopes554177124233502sdxfaz71320111:24000
Aridic Ustorthents-Lindrith-Riverwash complex, 0 to 6 percent slopes73415124233692sdxgaz71320111:24000
Ustifluventic Haplocambids-Ustic Haplocambids, rocky-Riverwash association, 1 to 70 percent slopes641597124867382sdy7az71320111:24000
Trail-Ives-Riverwash complex, 0 to 2 percent slopes51617924954082sdydaz71320111:24000
Oxyaquic Haplustolls-Riverwash complex, 1 to 4 percent slopes36196824954142sdykaz71320111:24000
Riverwash-Bebeevar complex, 0 to 3 percent slopes422825068612sdz2az71320111:24000
Trail-Riverwash association, 0 to 1 percent slopes12214292580262qsynaz71520071:24000
Notal-Trail-Riverwash association, 0 to 1 percent slopes731010580242qsylaz71520071:24000
Riverwash-Typic Torrifluvents complex, 0 to 5 percent slopes989316506532sflyaz71520071:24000
Riverwash-Bebeevar association, 0 to 1 percent slopes9763581122sflgaz71520071:24000
Riverwash1851636461584hh9tca01119991:24000
Arand-Riverwash complex, 0 to 2 percent slopes, frequently flooded524577461640hhcmca01119991:24000
RiverwashRh6999458819hdfmca02119611:20000
Columbia soils, channeled, 0 to 10 percent slopesCrB278458615hd71ca02119611:20000
Riverwash134tw42216125831r40tca03119801:24000
Xerofluvents-Riverwash complex2494799459652hf9hca03319851:24000
Riverwash1991814459602hf7wca03319851:24000
Riverwash1741000458998hdmdca05519741:24000
Riverwash203360461947hhpjca06719891:24000
RiverwashRw6437456269h9scca06919651:20000
Xerofluvents-Riverwash association, 0 to 2 percent slopes23246325626402q3fkca06919651:20000
Toags-Oxyaquic Haploxerolls-Riverwash complex, 0 to 2 percent slopes132134186198720hk3ca06919651:20000
Psammentic Haploxerolls-Mollic Fluvaquents-Riverwash complex, 0 to 8 percent slopes81116729249532x4d2ca07719901:24000
Riverwash165326455941h9fsca08719761:24000
RiverwashRw707456110h9m7ca09519691:24000
Xerofluvents-Riverwash complex, 0 to 2 percent slopes218em16076311qyw2ca09719681:20000
RiverwashRnA6225459861hfj7ca09719681:20000
Riverwash178pl11459392hf13ca10119841:24000
RiverwashRh4354459262hdwxca11319681:20000
Riverwash2123540459121hdrcca60219781:24000
Riverwash3002038487189jbysca60419941:24000
XEROFLUVENTS-RIVERWASH COMPLEX, 0 TO 5 PERCENT SLOPES2172747466120hn14ca60619901:24000
RiverwashRw4228460112hfsbca60719671:20000
Molinos complex, channeledMztte3112766092hgkdca60719671:20000
Riverwash300im9023757822kr64ca60719671:20000
Fluvents-Riverwash complex, 0 to 1 percent slopes2031649487485jc8bca60820001:24000
RiverwashRh2925456617hb4lca60919631:20000
Riverwash14186456694hb72ca61019751:24000
Riverwash, 0 to 2 percent slopes frequently flooded990382461204hgxkca61220051:24000
Riverwash, 1 to 25 percent slopesRw6263233152307g7ca61419671:24000
Mixed alluvial landMdB41832330942zmrkca61419671:24000
Riverwash, 1 to 45 percent slopesR63233151307g6ca61419671:24000
RIVERWASH2131180460520hg6hca61819911:24000
Riverwash178340640132ph3fca61919701:24000
Riverwash1782400460342hg0rca62019751:24000
Placer diggings and RiverwashPw5278462433hj66ca62819631:20000
Mine tailings and RiverwashMn3314462408hj5dca62819631:20000
Cumulic Humixerepts-Riverwash complex, 0 to 8 percent slopes8110778523997802lk58ca63020181:24000
Psammentic Haploxerolls-Mollic Fluvaquents-Riverwash complex, 0 to 8 percent slopes811192929249552x4d2ca63020181:24000
Mine dredge tailings-Riverwash complex, 0 to 5 percent slopes15120714034421j3dbca63220061:24000
Psammentic Haploxerolls-Mollic Fluvaquents-Riverwash complex, 0 to 8 percent slopes81111729249662x4d2ca63220061:24000
RiverwashRm2109332959282zwskca63819671:24000
Riverwash191114049731j4zqca63819671:24000
RiverwashRr1499462696hjgpca64419591:24000
Psammentic Haploxerolls-Mollic Fluvaquents-Riverwash complex, 0 to 8 percent slopes811134729249802x4d2ca64419591:24000
RiverwashRr15374460918hgmbca64519611:20000
Molinos complex, channeledMzt4798460858hgkdca64519611:20000
RiverwashRg5244457044hblcca64619671:24000
RiverwashRf2649463137hjxxca64819591:20000
Tujunga gravelly sand, channeled, 0 to 8 percent slopesTsA649463188hjzkca64819591:20000
Tujunga sand, channeled, 0 to 8 percent slopesTwA502463191hjznca64819591:20000
Honcut silty clay loam, channeled, 0 to 8 percent slopesHzA269463059hjvdca64819591:20000
Temple clay loam, slightly saline, channeled, 0 to 3 percent slopesTdA255463177hjz6ca64819591:20000
Piper soils, strongly saline-alkali, channeled, 0 to 3 percent slopesPuA243463120hjxcca64819591:20000
Riverwash and tailingsRb3208463292hk2xca64919671:24000
RiverwashRh3758329587130r99ca65119591:20000
Columbia soils, channeled, 0 to 8 percent slopesCrB154463369hk5dca65119591:20000
RiverwashRh2077464435hl8sca65419661:24000
Riverwash1343370467206hp55ca65919991:24000
Riverwash1512261463616hkfcca66019771:24000
Riverwash19438457166hbq9ca66419771:24000
Xerofluvents, occasionally flooded-Riverwash complex, 0 to 5 percent slopes306ne16523271sgcwca66619831:24000
Riverwash2292280463774hklgca66619831:24000
Xerofluvents-Riverwash association, 0 to 2 percent slopes9053775458521hd40ca66720031:24000
Aquents-Aquolls-Riverwash complex, 0 to 5 percent slopes, flooded2203410467334hp99ca66820071:24000
Xerofluvents, occasionally flooded-Riverwash complex, 0 to 5 percent slopes3062306467394hpc7ca66820071:24000
Inyo-Riverwash complex, 0 to 5 percent slopes, frequently flooded2161690467332hp97ca66820071:24000
Whitewolf-Riverwash complex, 0 to 5 percent slopes, frequently flooded2171065467333hp98ca66820071:24000
Goodale-Riverwash complex, 0 to 5 percent slopes352578467402hpchca66820071:24000
Riverwash139233467283hp7nca66820071:24000
Inyo-Riverwash complex, 0 to 5 percent slopes, frequently flooded216ne12922180912dg3bca67019771:24000
RIVERWASH15711600463976hkszca67119781:24000
RiverwashRs145457476hc19ca67219661:20000
RiverwashRA138457634hc6dca67319741:24000
RiverwashRw8311457760hcbgca67419681:24000
RiverwashRg6866457894hcgsca67519681:24000
Riverwash1916165458092hcp5ca67819741:24000
RiverwashRsC9095458354hcymca67919671:15840
RiverwashRA4375464049hkwbca68019741:24000
RiverwashRw38513987621hyjcca68119681:24000
Inyo-Riverwash complex, 0 to 5 percent slopes, frequently flooded443681186030320fssca68220071:24000
Fluvaquents-Riverwash complex, 2 to 8 percent slopes399544488685jdj1ca68520061:24000
Riverwash-Water complex99038716095831r0x1ca68620101:24000
Riverwash99120316092621r0kpca68620101:24000
Xerofluvents-Riverwash complex, 0 to 2 percent slopes2185217461103hgt9ca68719851:24000
Riverwash307mnf325048802q42kca68719851:24000
Typic Xerofluvents-Riverwash complex, 0 to 8 percent slopes1905821020156137k8ca68820081:24000
Xerofluvents-Haploxerepts-Riverwash complex, 0 to 15 percent slopes3891570466587hnj6ca69120081:24000
Riverwash2901243466406hnbcca69120081:24000
Fluvaquents-Riverwash complex, 0 to 5 percent slopes202290469931hs02ca69220011:24000
Riverwash191oc32911742hcp5ca69620161:24000
Typic Xerofluvents-Riverwash association, 2 to 10 percent slopes10014503470206hs8yca70119841:24000
Clallam family, very deep-Riverwash association, 0 to 15 percent slopes.1157214470336hsf4ca70219841:24000
Riverwash1745146470395hsh1ca70219841:24000
Typic Xerofluvents-Riverwash association, 2 to 10 percent slopes.100sr10190577721z3pca70219841:24000
Riverwash212sc9190595821z9jca70219841:24000
Fluvaquents-Riverwash complex, 2 to 8 percent slopes399sv8189816021q5zca70319831:24000
Xerofluvents-Riverwash association, 0 to 20 percent slopes.35115509470949ht1xca70719831:24000
Xerofluvents-Riverwash complex, 0 to 5 percent slopes217tw131186885420qpmca70719831:24000
Riverwash212sc34186768820ph0ca70719831:24000
RiverwashRwsh22186845020q8lca70719831:24000

Map of Series Extent

Approximate geographic distribution of the RIVERWASH 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 .