Official Series Description


Lab Data Summary

Aggregate lab data for the MOLLY soil series. This aggregation is based on all pedons with a current taxon name of MOLLY, 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 MOLLY 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 MOLLY 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 MOLLY 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 MOLLY 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 MOLLY 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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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 MOLLY 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 MOLLY 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 MOLLY 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 MOLLY, 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 MOLLY 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
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 20 to 40 percent slopes2lg2x3728508042lg2xid60120021:24000
Redraven-Roman-Molly families, complex, glaciated ridges, granitic geology2lg2s2828508032lg2sid60120021:24000
Rock outcrop-Roman family-Molly family, complex, glaciated ridges, granitic geology2lg2p1228508022lg2pid60120021:24000
Roman-Redraven-Molly families, complex, shallow incised glaciated mountain slopes, granitic geology, south aspects2lg32428508052lg32id60120021:24000
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 15 to 45 percent slopes2lg2t4428508482lg2tid60419811:24000
Redraven-Roman-Molly families, complex, steep glaciated mountain slopes, granitic geology2lg2w3728508492lg2wid60419811:24000
Redraven-Roman-Molly families, complex, glaciated ridges, granitic geology2lg2s3328508472lg2sid60419811:24000
Roman-Redraven-Molly families, complex, moderately steep glaciated mountain slopes, granitic geology, south aspects2lg2y2928508512lg2yid60419811:24000
Redraven-Roman-Molly families, complex, steep glaciated mountain slopes, granitic geology, south aspects2lg2z2428508522lg2zid60419811:24000
Roman-Redraven-Molly families, complex, shallow incised glaciated mountain slopes, granitic geology, north aspects2lg301428508532lg30id60419811:24000
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 20 to 40 percent slopes2lg2x1228508502lg2xid60419811:24000
Rock outcrop-Molly family-Redraven family, complex, steep glaciated mountain slopes, granitic geology2lg2r528508462lg2rid60419811:24000
Molly loam, 12 to 30 percent slopesMoC533515412155cnid61819651:24000
Molly loam, 30 to 65 percent slopesMoE297115412255cpid61819651:24000
Molly-Littlesalmon-Rock outcrop complex, 60 to 75 percent slopes1481448811492qfqid65619921:24000
Molly-Littlesalmon complex, 30 to 60 percent slopes147809811482qfpid65619921:24000
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 15 to 45 percent slopes3212106823968212lg2tid6701:24000
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 20 to 40 percent slopes3241875423968242lg2xid6701:24000
Redraven-Roman-Molly families, complex, moderately steep glaciated mountain slopes, granitic geology322741223968222lg2vid6701:24000
Roman-Redraven-Molly families, complex, moderately steep glaciated mountain slopes, granitic geology, south aspects325626023968252lg2yid6701:24000
Roman-Redraven-Molly families, complex, shallow incised glaciated mountain slopes, granitic geology, north aspects331354123968272lg30id6701:24000
Redraven-Roman-Molly families, complex, steep glaciated mountain slopes, granitic geology323324123968232lg2wid6701:24000
Rock outcrop-Roman family-Molly family, complex, glaciated ridges, granitic geology315254123968172lg2pid6701:24000
Roman-Redraven-Molly families, complex, shallow incised glaciated mountain slopes, granitic geology, south aspects333241623968292lg32id6701:24000
Redraven-Roman-Molly families, complex, steep glaciated mountain slopes, granitic geology, south aspects326241023968262lg2zid6701:24000
Redraven-Roman-Molly families, complex, glaciated ridges, granitic geology320217623968202lg2sid6701:24000
Roman-Redraven-Mollly families, complex, moderately to deeply incised draws on glaciated mountain slopes, granitic geology, south aspects334199523968302lg33id6701:24000
Roman-Redraven-Molly families, complex, moderately to deeply incised draws on glaciated mountain slopes, granitic geology, north aspects332136023968282lg31id6701:24000
Rock outcrop-Molly family-Redraven family, complex, steep glaciated mountain slopes, granitic geology317113523968192lg2rid6701:24000
Rock outcrop-Roman family-Molly family, complex, glaciated mountain slopes, granitic geology316101023968182lg2qid6701:24000
Rock outcrop-Roman family-Molly family, complex, glaciated ridges, granitic geology2lg2p9928509472lg2pwa65119811:24000
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 15 to 45 percent slopes2lg2t4428509202lg2twa65119811:24000
Rock outcrop-Roman family-Molly family, complex, glaciated mountain slopes, granitic geology2lg2q1928509252lg2qwa65119811:24000
Redraven-Roman-Molly families, complex, glaciated ridges, granitic geology2lg2s828509542lg2swa65119811:24000
Roman-Redraven-Molly families, complex, moderately to deeply incised draws on glaciated mountain slopes, granitic geology, north aspects2lg31328509522lg31wa65119811:24000
Redraven-Roman-Molly families, complex, moderately steep glaciated mountain slopes, granitic geology2lg2v228509382lg2vwa65119811:24000

Map of Series Extent

Approximate geographic distribution of the MOLLY 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 .