Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
130B87P0829S1987NC009001Evard6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.3833351,-81.3450012

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

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

Click the image to view it full size.

Select annual climate data summaries for the EVARD series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the EVARD 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Select annual climate data summaries for the EVARD series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the EVARD 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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 EVARD, 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. NC-2010-09-27-05 | Burke County - 2006

    Typical relationship between soils, landform, and parent material in the Evard-Cowee general soil map unit in the Blue Ridge mountains (Soil Survey of Burke County, North Carolina; 2006).

  2. NC-2010-09-27-07 | Burke County - 2006

    Typical relationship between soils, landform, and parent material in the Cliffield-Pigeonroost general soil map unit in the South Mountains (Soil Survey of Burke County, North Carolina; 2006).

  3. NC-2010-09-28-04 | Cleveland County - 2006

    The relationship between soils and parent material in the Pacolet-Bethlehem, Evard-Cowee, and Cliffield-Pigeonroost general soil map units (Soil Survey of Cleveland County, North Carolina; 2006).

  4. NC-2010-09-28-12 | Surry County - 2007

    Relationship of soils, landscape, and geology in the Cowee-Evard general soil map unit and the Chestnut-Peaks general soil map unit (Soil Survey of Surry County, North Carolina; 2007).

  5. NC-2010-09-28-13 | Surry County - 2007

    Relationship of soils, landscape, and geology of Pilot Mountain (Soil Survey of Surry County, North Carolina; 2007).

  6. NC-2012-02-07-05 | Clay County - 1998

    Typical relationship of soils, landscape position, and parent material in the Rosman-Reddies-Arkaqua-French general soil map unit on flood plains and in the Braddock-Tate general soil map unit on low rolling hills (Soil Survey of Clay County, North Carolina; 1998).

  7. NC-2012-02-07-06 | Clay County - 1998

    Typical relationship of soils, aspect, landscape position, and parent material in the Evard-Cowee general soil map unit in the low mountains (Soil Survey of Clay County, North Carolina; 1998).

  8. NC-2012-02-07-18 | Jackson County - June 1997

    Relationship of soils, aspect, parent material, and landscape position in the Evard-Cowee-Saunook-Trimont general soil map unit (Soil Survey of Jackson County, North Carolina; June 1997).

Map Units

Map units containing EVARD 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
Evard-Cowee complex, 15 to 30 percent slopes, stonyEvE697816117811r35yga01520131:12000
Evard-Saluda complex, 30 to 70 percent slopes, stonyExF477816117821r35zga01520131:12000
Cowee-Evard complex, 25 to 45 percent slopesCxF967135317652vx4tga63719901:20000
Clifton-Evard complex, 10 to 25 percent slopesClE811655317612vx4mga63719901:20000
Saunook-Evard complex, 10 to 25 percent slopesSaE25050531784kvcbga63719901:20000
Cowee-Evard complex, 45 to 60 percent slopesCxG203855317662vx4vga63719901:20000
Saunook-Evard complex, 25 to 45 percent slopes, stonySnF19850531785kvccga63719901:20000
Clifton-Evard complex, 6 to 10 percent slopesClC106505317602vx4nga63719901:20000
Cowee-Evard complex, 10 to 25 percent slopesCxE79905317642vx4sga63719901:20000
Urban land-Evard-Clifton complex, 10 to 35 percent slopesUeE560531792kvclga63719901:20000
Evard association, steepEVF15180531392ktypga65119761:20000
Evard-Cowee complex, 25 to 60 percent slopes, stonyEcE150451113522rdx0nc00319881:24000
Evard-Cowee complex, 8 to 25 percent slopes, stonyEcD32301113503qvync00319881:24000
Chester stony loam, 15 to 45 percent slopes (evard)ClF6357545904lb1tnc00519671:15840
Chester clay loam, 15 to 45 percent slopes, eroded (Evard)ChF2475545902lb1rnc00519671:15840
Chester stony loam, 10 to 15 percent slopes (evard)ClD320545903lb1snc00519671:15840
Evard loam, 25 to 45 percent slopesEvF24124545951lb3bnc00919821:24000
Evard loam, 15 to 25 percent slopesEvE17252545950lb39nc00919821:24000
Evard stony loam, 25 to 60 percent slopesEsF13270545949lb38nc00919821:24000
Evard-Cowee complex, 15 to 30 percent slopes, moderately erodedEvD22343216720092v0y7nc02120061:12000
Evard-Cowee complex, basin, 30 to 50 percent slopes, stonyEwE2238116720162vx29nc02120061:12000
Evard-Cowee complex, 30 to 50 percent slopes, moderately erodedEvE21838516720102v0y8nc02120061:12000
Evard-Cowee complex, basin, 15 to 30 percent slopes, stonyEwD1697516720152vx2dnc02120061:12000
Evard-Cowee-Urban land complex, 15 to 30 percent slopesExD330816720181t3w2nc02120061:12000
Evard-Cowee complex, basin, 50 to 95 percent slopes, stonyEwF286616720172ydh7nc02120061:12000
Evard-Cowee complex, basin, 8 to 15 percent slopes, stonyEwC141916720132xpd3nc02120061:12000
Evard-Cowee-Urban land complex, 8 to 15 percent slopesExC99816720201t3w4nc02120061:12000
Evard-Cowee-Urban land complex, 30 to 50 percent slopesExE85316720191t3w3nc02120061:12000
Evard-Cowee complex, 50 to 95 percent slopes, moderately erodedEvF248916720122v0ybnc02120061:12000
Evard-Cowee complex, escarpment, 30 to 50 percent slopes, stonyEvE200301169952vx2bnc02320001:24000
Evard-Cowee complex, escarpment, 15 to 30 percent slopes, stonyEvD90171169942vx2fnc02320001:24000
Evard-Cowee complex, 50 to 85 percent slopes, rockyEuF36671169962tk5qnc02320001:24000
Evard-Cowee complex, escarpment, 8 to 15 percent slopes, stonyEvC13681169932xpd4nc02320001:24000
Evard-Cowee complex, escarpment, 30 to 50 percent slopes, stonyEvE3360526792282vx2bnc02720121:12000
Evard-Cowee complex, escarpment, 15 to 30 percent slopes, stonyEvD980726792252vx2fnc02720121:12000
Evard-Cowee complex, escarpment, 8 to 15 percent slopes, stonyEvC26126792242xpd4nc02720121:12000
Evard-Cowee complex, 30 to 50 percent slopesEvE118905464132vx26nc04319911:12000
Evard-Cowee complex, 15 to 30 percent slopesEvD96065464122v0ydnc04319911:12000
Evard-Cowee complex, 8 to 15 percent slopesEvC2142546411lbl5nc04319911:12000
Evard-Cowee complex, 50 to 95 percent slopes, stonyEvF11995464142rdwync04319911:12000
Evard-Cowee complex, 2 to 8 percent slopesEvB805464102xpdcnc04319911:12000
Evard-Cowee complex, escarpment, 30 to 50 percent slopes, stonyEvE30071170642vx2bnc04520001:24000
Evard-Cowee complex, escarpment, 15 to 30 percent slopes, stonyEvD10881170632vx2fnc04520001:24000
Evard-Cowee complex, 50 to 85 percent slopes, rockyEwF7381170652tk5qnc04520001:24000
Evard soils, 25 to 45 percent slopesEwF15943546858lc1lnc08919741:20000
Evard soils, 15 to 25 percent slopesEwE11415546857lc1knc08919741:20000
Evard soils, 45 to 70 percent slopesEwG2529546859lc1mnc08919741:20000
Evard fine sandy loam, 7 to 15 percent slopesEvC2510546856lc1jnc08919741:20000
Clifton (evard) stony loam, 15 to 25 percent slopesCfE1113546846lc16nc08919741:20000
Clifton (evard) stony loam, 25 to 45 percent slopesCfF953546847lc17nc08919741:20000
Evard-Cowee complex, 15 to 30 percent slopes, stony (Pisgah National Forest)337D55725092752v0ygnc08919741:20000
Evard-Cowee complex, 30 to 50 percent slopes, stony (Pisgah National Forest)337E29625092762vx25nc08919741:20000
Evard-Cowee complex, high precipitation, 8 to 15 percent slopes, stony337C2625092772xpd5nc08919741:20000
Evard-Cowee complex, 25 to 60 percent slopes, stonyEvF215124249062rdx0nc09720111:12000
Evard-Cowee complex, 8 to 25 percent slopes, stonyEvE105824249052md9rnc09720111:12000
Evard-Cowee complex, 30 to 50 percent slopesEvE251535470722vx26nc09919911:12000
Evard-Cowee complex, 50 to 95 percent slopes, stonyEvF139355470732rdwync09919911:12000
Evard-Cowee complex, 15 to 30 percent slopesEvD112235470712v0ydnc09919911:12000
Evard-Cowee complex, 8 to 15 percent slopesEvC1201547070lc8fnc09919911:12000
Cowee-Evard-Urban land complex, 15 to 30 percent slopesCrD864547051lc7tnc09919911:12000
Evard-Cowee complex, 25 to 60 percent slopesEwE721495471962vx23nc11119891:24000
Hayesville-Evard complex, 15 to 25 percent slopesHeD29397547200lcdmnc11119891:24000
Evard loam, 10 to 25 percent slopesEvD10557547195lcdgnc11119891:24000
Hayesville-Evard-Urban land complex, 15 to 25 percent slopesHrD958547201lcdnnc11119891:24000
Evard-Cowee complex, 30 to 50 percent slopesEvE434065458372vx26nc11319901:12000
Evard-Cowee complex, 15 to 30 percent slopesEvD285065458362v0ydnc11319901:12000
Evard-Cowee complex, 50 to 95 percent slopes, stonyEvF178885458382rdwync11319901:12000
Evard-Cowee complex, 8 to 15 percent slopesEvC5155545835l9zlnc11319901:12000
Evard-Cowee-Urban land complex, 15 to 30 percent slopesExD376545840l9zrnc11319901:12000
Evard-Cowee-Urban land complex, 8 to 15 percent slopesExC274545839l9zqnc11319901:12000
Evard-Cowee complex, 2 to 8 percent slopesEvB795458342xpdcnc11319901:12000
Evard-Cowee complex, 30 to 50 percent slopes, moderately erodedEvE21362816713812v0y8nc11520061:12000
Evard-Cowee complex, 15 to 30 percent slopes, moderately erodedEvD2625316713802v0y7nc11520061:12000
Evard-Cowee complex, basin, 15 to 30 percent slopes, stonyEwD318516713842vx2dnc11520061:12000
Evard-Cowee complex, basin, 30 to 50 percent slopes, stonyEwE318116713852vx29nc11520061:12000
Evard-Cowee complex, 50 to 95 percent slopes, moderately erodedEvF280716713822v0ybnc11520061:12000
Evard-Cowee complex, basin, 50 to 95 percent slopes, stonyEwF42416713862ydh7nc11520061:12000
Evard-Cowee complex, central mountain, 30 to 50 percent slopes, stonyEdE47515475662wldcnc12119971:12000
Evard-Cowee complex, central mountain, 15 to 30 percent slopes, stonyEcD35975475652vx2gnc12119971:12000
Evard-Cowee complex, central mountains, 8 to 15 percent slopesEcC12845475642xpd6nc12119971:12000
Evard-Cowee complex, central mountains, 50 to 95 percent slopes, stonyEdF9165475672ydh9nc12119971:12000
Evard-Cowee complex, escarpment, 30 to 50 percent slopes, stonyEvE107031110832vx2bnc14919921:24000
Evard-Cowee complex, escarpment, 15 to 30 percent slopes, stonyEvD32391110822vx2fnc14919921:24000
Evard-Cowee complex, 50 to 85 percent slopes, rockyEvF20301110842tk5qnc14919921:24000
Evard-Cowee complex, escarpment, 30 to 50 percent slopes, stonyEvE298601176162vx2bnc16119971:24000
Evard-Cowee complex, escarpment, 15 to 30 percent slopes, stonyEvD97661176152vx2fnc16119971:24000
Evard-Cowee complex, 50 to 85 percent slopes, rockyEwF93201176192tk5qnc16119971:24000
Evard-Cowee complex, 30 to 50 percent slopes, rockyEwE41251176182vx27nc16119971:24000
Evard-Cowee complex, 15 to 30 percent slopes, rockyEwD11371176172v0yfnc16119971:24000
Evard-Cowee complex, 25 to 45 percent slopes, stonyEcE467614276141jxk2nc17120051:24000
Cowee-Saluda-Evard complex, 45 to 90 percent slopes, rockyCxF260914275961jxjhnc17120051:24000
Evard-Cowee complex, 15 to 25 percent slopes, stonyEcD167814276121jxk0nc17120051:24000
Evard-Cowee complex, 8 to 15 percent slopes, stonyEcC82514276151jxk3nc17120051:24000
Evard loam, 15 to 30 percent slopes, stonyChE1033423903692l7cpnc17519681:15840
Evard loam, 30 to 50 percent slopes, stonyChF558623903702l7cqnc17519681:15840
Evard-Cowee complex, high precipitation, 30 to 50 percent slopes, stonyCrF389823903732vx24nc17519681:15840
Evard-Cowee complex, 15 to 30 percent slopes, stony (Pisgah National Forest)337D367125018522v0ygnc17519681:15840
Evard-Cowee complex, 30 to 50 percent slopes, stony (Pisgah National Forest)337E333225018532vx25nc17519681:15840
Evard loam, 8 to 15 percent slopes, stonyChD215523903712l7crnc17519681:15840
Evard-Cowee complex, high precipitation, 15 to 30 percent slopes, stonyCrE147723903722v0ycnc17519681:15840
Evard-Cowee complex, high precipitation, 8 to 15 percent slopes, stony337C14625018542xpd5nc17519681:15840
Evard-Cowee complex, escarpment, 30 to 50 percent slopes, stonyEvE20365297922vx2bnc18920011:12000
Evard-Cowee complex, escarpment, 15 to 30 percent slopes, stonyEvD12915297912vx2fnc18920011:12000
Evard-Cowee complex, 8 to 15 percent slopes, stonyEvC138529789ks8znc18920011:12000
Evard-Cowee complex, 25 to 60 percent slopes, stonyEsE7409113834462rdx0nc19319931:24000
Evard-Cowee complex, 8 to 25 percent slopes, stonyEsD2597313834441hfl7nc19319931:24000
Evard gravelly sandy loam, 15 to 25 percent slopesErD644713834421hfl5nc19319931:24000
Evard gravelly sandy loam, 6 to 15 percent slopesErC160213834411hfl4nc19319931:24000
Evard-Cowee complex, 25 to 45 percent slopes, stonyEcF232823983622lhpjnc19719601:15840
Evard-Cowee complex, 15 to 25 percent slopes, stonyEcE52923983612lhphnc19719601:15840
Evard-Cowee complex, 10 to 15 percent slopes, stonyEcD27123983592lhpfnc19719601:15840
Evard-Cowee complex, 6 to 10 percent slopes, stonyEcC21123983582lhpdnc19719601:15840
Evard-Cowee complex, central mountain, 30 to 50 percent slopes, stonyEcE96235478412wldcnc19919971:12000
Evard-Cowee complex, central mountain, 15 to 30 percent slopes, stonyEcD47475478402vx2gnc19919971:12000
Evard-Cowee complex, 8 to 15 percent slopes, moderately erodedEaC27075478392xpd2nc19919971:12000
Evard-Cowee complex, 30 to 50 percent slopes, stonyEvE63895562842vx28nc60520071:12000
Evard-Cowee complex, 15 to 30 percent slopes, stonyEvD24425562832vx2cnc60520071:12000
Evard-Cowee complex, 50 to 95 percent slopes, stonyEvF18885562852rdwync60520071:12000
Evard-Cowee-Urban land complex, 15 to 30 percent slopesExD660556292lnvxnc60520071:12000
Evard-Cowee-Urban land complex, 30 to 50 percent slopesExE6321910255223s4nc60520071:12000
Evard-Cowee complex, 8 to 15 percent slopesEvC43556282lnvlnc60520071:12000
Evard-Cowee-Urban land complex, 2 to 15 percent slopesExC34556290lnvvnc60520071:12000
Evard-Cowee complex, 30 to 50 percent slopesEvE208135467702vx26nc60619911:12000
Evard-Cowee complex, 15 to 30 percent slopesEvD104345467692v0ydnc60619911:12000
Evard-Cowee complex, 50 to 95 percent slopes, stonyEwF36175467712rdwync60619911:12000
Evard-Cowee-Urban land complex, 15 to 30 percent slopesExD1058546772lbytnc60619911:12000
Evard-Brevard association, steepEVF208131324804fvksc04519721:20000
Brevard-Evard complex, 15 to 25 percent slopesBvE169421324634fv0sc04519721:20000
Grover fine sandy loam, 40 to 80 percent slopesGrG53151310354dbysc07719671:20000
Grover fine sandy loam, 25 to 40 percent slopesGrF40811310344dbxsc07719671:20000
Hayesville fine sandy loam, 40 to 80 percent slopesHeG23941310394dc2sc07719671:20000
Grover fine sandy loam, 6 to 15 percent slopes, erodedGrD218591310324dbvsc07719671:20000
Grover fine sandy loam, 15 to 25 percent slopesGrE15071310334dbwsc07719671:20000
Hayesville fine sandy loam, 15 to 40 percent slopesHeF12331310384dc1sc07719671:20000
Clifton fine sandy loam, 15 to 35 percent slopesCtF5101310274dbpsc07719671:20000
Porters loam, 15 to 40 percent slopesPoF4581310614dcssc07719671:20000
Ashe sandy loam, 10 to 25 percent slopesAsE2311310134db7sc07719671:20000
Madison fine sandy loam, high, 25 to 40 percent slopesMfF44511309914d9jsc60219601:20000
Madison fine sandy loam, high, 15 to 25 percent slopesMfE17951309894d9gsc60219601:20000
Madison fine sandy loam, high, 10 to 15 percent slopes, erodedMfD211601309884d9fsc60219601:20000
Madison fine sandy loam, high, 15 to 25 percent slopes, erodedMfE211591309904d9hsc60219601:20000
Madison fine sandy loam, high, 6 to 10 percent slopes, erodedMfC210111309864d9csc60219601:20000
Lloyd loam, moderately shallow, 25 to 40 percent slopesLmF6731309794d94sc60219601:20000
Madison fine sandy loam, high, 10 to 15 percent slopesMfD4981309874d9dsc60219601:20000
Lloyd loam, moderately shallow, 15 to 25 percent slopes, erodedLmE23891309784d93sc60219601:20000
Madison loam, high, 15 to 25 percent slopes, severely erodedMhE33221309924d9ksc60219601:20000
Madison fine sandy loam, high, 6 to 10 percent slopesMfC2981309854d9bsc60219601:20000
Evard fine sandy loam, 25 to 50 percent slopes6E297911307454d1lsc60419821:24000
Evard fine sandy loam, 50 to 80 percent slopes6F142601307464d1msc60419821:24000
Evard fine sandy loam, 15 to 25 percent slopes6D89161307444d1ksc60419821:24000
Evard fine sandy loam, 7 to 15 percent slopes6C16741307434d1jsc60419821:24000
Evard-Hayesville complex, 15 to 30 percent slopesErD14832523750kl05tn13919971:24000
Evard-Hayesville complex, 5 to 15 percent slopesErC8485523749kl04tn13919971:24000
Gullied land-Evard complex, 15 to 30 percent slopesGeD4966523754kl09tn13919971:24000
Gullied land-Evard complex, 5 to 15 percent slopesGeC2477523753kl08tn13919971:24000
Evard-Hayesville complex, 15 to 30 percent slopes, gulliedEvD2209523752kl07tn13919971:24000
Evard-Hayesville complex, 5 to 15 percent slopes, gulliedEvC1478523751kl06tn13919971:24000
Evard loam, 15 to 30 percent slopesEdD1159523748kl03tn13919971:24000
Evard loam, 5 to 15 percent slopesEdC488523747kl02tn13919971:24000
Evard loam, 20 to 40 percent slopesEvE881528412kqvktn17119801:24000
Evard loam, 10 to 20 percent slopesEvD422528411kqvjtn17119801:24000
Evard-Cowee complex, 50 to 95 percent slopes, stonyEvF2315553550ll0gtn64020071:24000
Evard-Cowee complex, 30 to 50 percent slopes, stonyEvE454557250lpvttn64020071:24000
Evard-Cowee complex, 15 to 30 percent slopes, stonyEvD271557262lpw6tn64020071:24000
Evard-Cowee complex, 30 to 50 percent slopes, stony, windsweptEpE5613381nl8htn64020071:24000
Cowee-Cliffield-Evard complex, 25 to 45 percent slopes, very rocky12E79581966mjl3va06720041:24000
Cowee-Cliffield-Evard complex, 15 to 25 percent slopes, very rocky12D9581964mjl1va06720041:24000
Cowee-Cliffield-Evard complex, 8 to 15 percent slopes, very rocky12C3581962mjkzva06720041:24000
Evard-Cowee complex, 15 to 25 percent slopes, stony27D9516852kbtnva07720061:24000
Cliffield-Evard complex, 25 to 45 percent slopes, very rocky7E328632027580261vtva14120081:24000
Cliffield-Evard complex, 15 to 25 percent slopes, very rocky7D54012027579261vsva14120081:24000
Cliffield-Evard complex, 45 to 90 percent slopes, very rocky7F47172027581261vvva14120081:24000
Evard-Cowee complex, 8 to 15 percent slopes17C235814740721lgwqva14120081:24000
Cliffield-Evard complex, 8 to 15 percent slopes, very rocky7C19232027578261vrva14120081:24000
Evard-Cowee complex, 15 to 25 percent slopes17D163714740731lgwrva14120081:24000
Evard-Cowee complex, 25 to 45 percent slopes17E137314740741lgwsva14120081:24000
Evard-Cowee complex, 2 to 8 percent slopes17B28514740711lgwpva14120081:24000
Evard-Cowee complex, 25 to 45 percent slopes, very stony18E28414741931lh0mva14120081:24000
Evard-Cowee complex, 15 to 25 percent slopes, very stony18D26614741921lh0lva14120081:24000
Evard-Cowee complex, 8 to 15 percent slopes, very stony18C9914741911lh0kva14120081:24000
Evard-Cowee complex, 2 to 8 percent slopes, very stony18B614741901lh0jva14120081:24000
Evard fine sandy loam, 25 to 55 percent slopes17E3467520230kgbmva16119901:24000
Evard fine sandy loam, 15 to 25 percent slopes17D1960520229kgblva16119901:24000
Evard fine sandy loam, 7 to 15 percent slopes17C1188520228kgbkva16119901:24000
Evard sandy loam, 35 to 60 percent slopes52E848625252542qm1nva6061:24000
Evard sandy loam, 15 to 35 percent slopes52D291525252532qm1mva6061:24000
Evard sandy loam, 3 to 15 percent slopes52C17925252522qm1lva6061:24000
Evard sandy loam, 60 to 80 percent slopes52F12225252552qm1pva6061:24000

Map of Series Extent

Approximate geographic distribution of the EVARD 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 .