Official Series Description


Lab Data Summary

Aggregate lab data for the LAMONT soil series. This aggregation is based on all pedons with a current taxon name of LAMONT, 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 LAMONT 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
104X45-110-1S1965IA089906Lamont2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.34814,-92.09625
104X53-110-1S1985IA105004Lamont2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1455072,-91.3449802
105X191126S1959IA191004Lamont1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3194367,-91.6888738
105X65125-1-1S1962IA065029Lamont1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.055156,-91.8032137
105X65110-1-1S1962IA065030Lamont1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0489327,-91.833859
105X22-110X-2S1975IA043002Lamont2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8551832,-91.0995577
105UMN2081S1975MN055059Lamont3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5121374,-91.2968797
105UMN2066S1976MN055039Lamont3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6097322,-91.3409498
105X49-110C2S1988IA097025Lamont2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.111912,-90.6184981
108A40A2766S1954IL103001Lamont4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5936127,-89.4363861
115C80IL1710601980IL171060Lamont2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5704503,-90.5239379
115C85IL1250491985IL125049Lamont2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.348,-90.0246278
n/aX49-110D-2S1988IA097901Lamont2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LAMONT 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 LAMONT 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 LAMONT 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 LAMONT 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 LAMONT 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 LAMONT 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 LAMONT 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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Click the image to view it full size.

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 LAMONT, 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. IA-2011-05-31-23 | Dubuque County - 1986

    Typical pattern of soils and underlying material in the Chelsea-Sogn-Lamont association (Soil Survey of Dubuque County, Iowa; 1986).

Map Units

Map units containing LAMONT 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
Chelsea-Fayette-Lamont complex, 9 to 18 percent slopes293D34404028692tgqzia01119771:15840
Chelsea-Fayette-Lamont complex, 5 to 9 percent slopes293C18774028682tgqtia01119771:15840
Chelsea-Fayette-Lamont complex, 18 to 25 percent slopes293F16184028702tgr3ia01119771:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B9354028092thk0ia01119771:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C5484028102thk2ia01119771:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B16634032022thk0ia01919781:15840
Lamont fine sandy loam, 0 to 2 percent slopes1102814032012thjzia01919781:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B5504033392thk0ia02319781:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C3064033402thk2ia02319781:15840
Lamont fine sandy loam, 9 to 18 percent slopes110E41913970522thk3ia03120081:12000
Lamont fine sandy loam, 2 to 9 percent slopes110C39913970512thk1ia03120081:12000
Lamont fine sandy loam, 5 to 9 percent slopes110C2134041972thk2ia04319791:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B1644041962thk0ia04319791:15840
Lamont fine sandy loam, 0 to 2 percent slopes1101144041952thjzia04319791:15840
Chelsea-Fayette-Lamont complex, 9 to 18 percent slopes293E7014044012tgqzia04519781:15840
Lamont fine sandy loam, 2 to 9 percent slopes110C6744043302thk1ia04519781:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B14904049732thk0ia05519841:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C13204049742thk2ia05519841:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C11034053692thk2ia06119831:15840
Lamont fine sandy loam, 9 to 14 percent slopes110D4394053702thk4ia06119831:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B3604053682thk0ia06119831:15840
Urban land-Lamont complex, 2 to 7 percent slopes4110B358405424flw6ia06119831:15840
Lamont fine sandy loam, 5 to 14 percent slopes110C3854056922thk5ia06519751:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B3584056912thk0ia06519751:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B6124058352thk0ia06719891:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C2934058362thk2ia06719891:15840
Chelsea-Fayette-Lamont complex, 5 to 9 percent slopes293C9064068472tgqtia08719821:15840
Chelsea-Fayette-Lamont complex, 9 to 18 percent slopes293E8044068482tgqzia08719821:15840
Chelsea-Fayette-Lamont complex, 18 to 25 percent slopes293F7924068492tgr3ia08719821:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B5894067922thk0ia08719821:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C5724067932thk2ia08719821:15840
Chelsea-Fayette-Lamont complex, 2 to 5 percent slopes293B4154068462tgqria08719821:15840
Ainsworth-Lamont complex, 9 to 18 percent slopes154E374406815fnb2ia08719821:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B3094070082thk0ia08919691:15840
Lamont fine sandy loam, 0 to 2 percent slopes110A2254070072thjzia08919691:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C1464070092thk2ia08919691:15840
Fayette-Lamont-Chelsea complex, 9 to 14 percent slopes, moderately eroded293D22101407489fp0tia09719881:15840
Fayette-Lamont-Chelsea complex, 18 to 25 percent slopes, moderately eroded293F21006407492fp0xia09719881:15840
Fayette-Lamont-Chelsea complex, 5 to 9 percent slopes, moderately eroded293C2997407487fp0ria09719881:15840
Fayette-Lamont-Chelsea complex, 18 to 25 percent slopes293F928407491fp0wia09719881:15840
Fayette-Lamont-Chelsea complex, 14 to 18 percent slopes, moderately eroded293E2756407490fp0via09719881:15840
Fayette-Lamont-Chelsea complex, 25 to 40 percent slopes293G508407493fp0yia09719881:15840
Fayette-Lamont-Chelsea complex, 9 to 14 percent slopes293D505407488fp0sia09719881:15840
Lamont sandy loam, 5 to 9 percent slopes, moderately eroded110C2252407437fnz4ia09719881:15840
Chelsea-Fayette-Lamont complex, 25 to 40 percent slopes293G5394076552tgr5ia09919751:15840
Chelsea-Fayette-Lamont complex, 18 to 25 percent slopes293F3444077872tgr3ia10119921:15840
Chelsea-Fayette-Lamont complex, 5 to 9 percent slopes293C2564077842tgqtia10119921:15840
Chelsea-Fayette-Lamont complex, 5 to 9 percent slopes, eroded293C243524079942tgqvia10319791:15840
Chelsea-Fayette-Lamont complex, 9 to 14 percent slopes, eroded293D234334079962tgqyia10319791:15840
Chelsea-Fayette-Lamont complex, 18 to 25 percent slopes293F24364079992tgr3ia10319791:15840
Chelsea-Fayette-Lamont complex, 14 to 18 percent slopes, eroded293E220654079982tgr1ia10319791:15840
Chelsea-Fayette-Lamont complex, 25 to 40 percent slopes293G19634080002tgr5ia10319791:15840
Chelsea-Fayette-Lamont complex, 5 to 9 percent slopes293C10394079932tgqtia10319791:15840
Chelsea-Fayette-Lamont complex, 14 to 18 percent slopes293E6884079972tgr0ia10319791:15840
Chelsea-Fayette-Lamont complex, 9 to 14 percent slopes293D6344079952tgqwia10319791:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C6124079232thk2ia10319791:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B4674079222thk0ia10319791:15840
Lamont fine sandy loam, 9 to 18 percent slopes110E4354079242thk3ia10319791:15840
Chelsea-Fayette-Lamont complex, 2 to 9 percent slopes293C31494081352tgqsia10519881:15840
Chelsea-Fayette-Lamont complex, 9 to 14 percent slopes293D28854081362tgqwia10519881:15840
Chelsea-Fayette-Lamont complex, 14 to 25 percent slopes293F19294081372tgr2ia10519881:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C3164080772thk2ia10519881:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B2204080762thk0ia10519881:15840
Lamont fine sandy loam, 9 to 18 percent slopes110E1684080782thk3ia10519881:15840
Chelsea-Fayette-Lamont complex, 9 to 14 percent slopes293D10044470772tgqwia10719981:12000
Chelsea-Fayette-Lamont complex, 14 to 18 percent slopes293E5714470792tgr0ia10719981:12000
Chelsea-Fayette-Lamont complex, 5 to 9 percent slopes293C5214470752tgqtia10719981:12000
Chelsea-Fayette-Lamont complex, 18 to 25 percent slopes293F4034470812tgr3ia10719981:12000
Chelsea-Fayette-Lamont complex, 9 to 18 percent slopes, moderately eroded293D2418840860430qwfia11319701:15840
Chelsea-Fayette-Lamont complex, 18 to 25 percent slopes293F27044086052tgr3ia11319701:15840
Chelsea-Fayette-Lamont complex, 9 to 18 percent slopes293D12664086032tgqzia11319701:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B12414085292thk0ia11319701:15840
Chelsea-Fayette-Lamont complex, 18 to 25 percent slopes, eroded293F212194086062tgr4ia11319701:15840
Chelsea-Fayette-Lamont complex, 5 to 9 percent slopes, eroded293C210174086022tgqvia11319701:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C7304085302thk2ia11319701:15840
Chelsea-Fayette-Lamont complex, 5 to 9 percent slopes293C5124086012tgqtia11319701:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B3314087052thk0ia11519841:15840
Chelsea-Fayette-Lamont complex, 5 to 9 percent slopes293C2824087592tgqtia11519841:15840
Chelsea-Fayette-Lamont complex, 9 to 18 percent slopes293E2184087602tgqzia11519841:15840
Lamont fine sandy loam, 2 to 5 percent slopes110B6354096152thk0ia13119711:15840
Lamont fine sandy loam, 0 to 2 percent slopes1104964096142thjzia13119711:15840
Lamont-Renova complex, 2 to 5 percent slopes610B354409688fr9ria13119711:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C2124096162thk2ia13119711:15840
Chelsea-Fayette-Lamont complex, 25 to 40 percent slopes293G3854099632tgr5ia13919861:15840
Chelsea-Fayette-Lamont complex, 18 to 25 percent slopes293F5074109562tgr3ia16319891:15840
Chelsea-Fayette-Lamont complex, 9 to 18 percent slopes293E5064109552tgqzia16319891:15840
Chelsea-Fayette-Lamont complex, 5 to 9 percent slopes293C3514109542tgqtia16319891:15840
Downs-Lamont complex, 9 to 14 percent slopes, moderately eroded429D2962411485ft5qia17119891:15840
Chelsea-Fayette-Lamont complex, 9 to 14 percent slopes293D9504114442tgqwia17119891:15840
Chelsea-Fayette-Lamont complex, 14 to 18 percent slopes, eroded293E29454114472tgr1ia17119891:15840
Chelsea-Fayette-Lamont complex, 25 to 40 percent slopes293G8054114512tgr5ia17119891:15840
Chelsea-Fayette-Lamont complex, 18 to 25 percent slopes293F7674114492tgr3ia17119891:15840
Chelsea-Fayette-Lamont complex, 9 to 14 percent slopes, eroded293D26564114452tgqyia17119891:15840
Downs-Lamont complex, 14 to 18 percent slopes, moderately eroded429E2596411486ft5ria17119891:15840
Chelsea-Fayette-Lamont complex, 14 to 18 percent slopes293E5184114462tgr0ia17119891:15840
Downs-Lamont complex, 18 to 25 percent slopes, moderately eroded429F2344411488ft5tia17119891:15840
Chelsea-Fayette-Lamont complex, 18 to 25 percent slopes, eroded293F22894114502tgr4ia17119891:15840
Lamont fine sandy loam, 5 to 9 percent slopes110C2534113522thk2ia17119891:15840
Downs-Lamont complex, 14 to 18 percent slopes, severely eroded429E3237411487ft5sia17119891:15840
Clinton-Lamont-Chelsea complex, 9 to 14 percent slopes, eroded295D28024120452thljia18319831:15840
Fayette-Lamont-Chelsea complex, 14 to 25 percent slopes, eroded293E27424120412tgr6ia18319831:15840
Clinton-Lamont-Chelsea complex, 5 to 9 percent slopes, eroded295C24634120442thlhia18319831:15840
Clinton-Lamont-Chelsea complex, 9 to 14 percent slopes, severely eroded295D33404120462thlkia18319831:15840
Lamont sandy loam, 18 to 35 percent slopes175F81423785892kv3pil00119971:12000
Lamont sandy loam, 35 to 60 percent slopes175G57423785902kv3qil00119971:12000
Lamont fine sandy loam, 2 to 7 percent slopes, occasionally flooded8175B442609543ng8pil00320021:12000
Lamont fine sandy loam, 2 to 5 percent slopes175B348602838n79dil00320021:12000
Lamont fine sandy loam, 0 to 2 percent slopes175A193602837n79cil00320021:12000
Lamont fine sandy loam, 5 to 10 percent slopes175C23602839n79fil00320021:12000
Lamont sandy loam, 35 to 60 percent slopes175G7101729565sz7il00919841:12000
Lamont sandy loam, 18 to 35 percent slopes175F5761729555sz6il00919841:12000
Lamont fine sandy loam, 2 to 5 percent slopes175B754186270620j99il01120071:12000
Lamont fine sandy loam, 5 to 10 percent slopes, eroded175C2378186270720j9bil01120071:12000
Lamont fine sandy loam, 10 to 18 percent slopes175D319186270820j9cil01120071:12000
Lamont fine sandy loam, 18 to 35 percent slopes, eroded175F21050796107vqdwil01520051:12000
Tell-Lamont complex, 18 to 35 percent slopes, eroded952F2948905338zd2gil01520051:12000
Tell-Lamont complex, 10 to 18 percent slopes, eroded952D2583902724z9c4il01520051:12000
Tell-Lamont complex, 5 to 10 percent slopes, eroded952C2527902719z9bzil01520051:12000
Lamont fine sandy loam, 5 to 10 percent slopes, eroded175C2420796102vqdqil01520051:12000
Lamont fine sandy loam, 10 to 18 percent slopes, eroded175D2372796075vqcvil01520051:12000
Tell-Lamont complex, 10 to 18 percent slopes, severely eroded952D3304902727z9c7il01520051:12000
Lamont fine sandy loam, 2 to 5 percent slopes175B153796101vqdpil01520051:12000
Lamont fine sandy loam, 10 to 18 percent slopes, severely eroded175D3142796103vqdril01520051:12000
Lamont fine sandy loam, 2 to 5 percent slopes, rarely flooded7175B55316074521qyp9il02320061:12000
Lamont fine sandy loam, 10 to 18 percent slopes, eroded175D228816074532zxdbil02320061:12000
Lamont fine sandy loam, 1 to 4 percent slopes175B7472116117365il05919661:20000
Lamont fine sandy loam, 4 to 7 percent slopes175C6132116122zxd3il05919661:20000
Lamont fine sandy loam, 7 to 12 percent slopes, eroded175D23212116132zxd9il05919661:20000
Lamont fine sandy loam, 2 to 5 percent slopes175B33713884ryvjil06920031:12000
Lamont fine sandy loam, 10 to 18 percent slopes, eroded175D2657210893428sj4il08519901:12000
Lamont fine sandy loam, 2 to 5 percent slopes175B482194963123frbil08519901:12000
Lamont fine sandy loam, 0 to 2 percent slopes175A37821516wkvjil08720051:12000
Lamont fine sandy loam, 5 to 10 percent slopes, eroded175C223821514wkvgil08720051:12000
Lamont fine sandy loam, 2 to 5 percent slopes175B21821512wkvdil08720051:12000
Lamont fine sandy loam, 2 to 4 percent slopes175B12161766822zxd4il10119521:42240
Lamont fine sandy loam, 0 to 2 percent slopes175A3951766812zxd2il10119521:42240
Lamont fine sandy loam, 4 to 7 percent slopes175C2901766832zxd3il10119521:42240
Lamont fine sandy loam, 4 to 7 percent slopes, eroded175C21181766842zxd6il10119521:42240
Lamont fine sandy loam, 7 to 12 percent slopes, eroded175D2721766852zxd9il10119521:42240
Lamont fine sandy loam, 10 to 18 percent slopes, eroded175D248807983w3rzil12720041:12000
Lamont fine sandy loam, 2 to 5 percent slopes175B46807980w3rwil12720041:12000
Lamont fine sandy loam, 5 to 10 percent slopes, eroded175C226807982w3ryil12720041:12000
Lamont sandy loam, 2 to 5 percent slopes175B89313989091hyp3il14120051:12000
Lamont sandy loam, 5 to 10 percent slopes175C52713989111hyp5il14120051:12000
Lamont sandy loam, 18 to 35 percent slopes175F12762011326r94il14920011:12000
Lamont sandy loam, 35 to 60 percent slopes175G7992011346r96il14920011:12000
Lamont fine sandy loam, 2 to 5 percent slopes175B207607171nct5il15120031:12000
Lamont fine sandy loam, 5 to 10 percent slopes, eroded175C271607173nct7il15120031:12000
Lamont fine sandy loam, 5 to 10 percent slopes175C7607172nct6il15120031:12000
Lamont fine sandy loam, 2 to 5 percent slopes175B64748898t490il15320041:12000
Lamont fine sandy loam, 18 to 35 percent slopes175F2975793041vm6zil19520031:12000
Lamont fine sandy loam, 10 to 18 percent slopes, eroded175D22844793040vm6yil19520031:12000
Lamont fine sandy loam, 2 to 5 percent slopes, eroded175B21858793039vm6xil19520031:12000
Lamont fine sandy loam, 2 to 6 percent slopes216B805397823fbz0mn04719771:15840
Lamont fine sandy loam, 6 to 12 percent slopes216C419397824fbz1mn04719771:15840
Timula-Lamont complex, 20 to 40 percent slopes, moderately eroded1858F30563982372wtrmmn05519811:15840
Lamont fine sandy loam, 1 to 6 percent slopes216B386398250fcdsmn05519811:15840
Lamont-Racine complex, 2 to 6 percent slopes1811B1553400719ffzfmn10919771:15840
Lamont sandy loam, 2 to 6 percent slopes216B1081400728ffzqmn10919771:15840
Lamont sandy loam, 2 to 6 percent slopesLcB464428253gcmmmn14719671:20000
Lamont sandy loam, 6 to 12 percent slopesLcC228428254gcmnmn14719671:20000
Lamont sandy loam, 12 to 18 percent slopesLcD97428255gcmpmn14719671:20000
Lamont fine sandy loam, driftless, 20 to 45 percent slopes, moderately erodedLaE25674242882wtr9wi04319591:20000
Lamont fine sandy loam, driftless, 12 to 20 percent slopes, moderately erodedLaD21754242852wtr8wi04319591:20000
Lamont fine sandy loam, driftless, 6 to 12 percent slopes, moderately erodedLaB2704242842wtr7wi04319591:20000
Lamont fine sandy loam, 2 to 6 percent slopes, moderately eroded503B248516975071tzd9wi09320061:12000
Lamont fine sandy loam, 6 to 12 percent slopes, moderately eroded503C239616975081tzdbwi09320061:12000
Lamont fine sandy loam, 12 to 20 percent slopes, moderately eroded503D26116975061tzd8wi09320061:12000

Map of Series Extent

Approximate geographic distribution of the LAMONT 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 .