Soil Data Explorer - FINN

Official Series Description

Lab Data Summary

Aggregate lab data for the FINN soil series. This aggregation is based on all pedons with a current taxon name of FINN, 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 FINN were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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 FINN 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.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the FINN series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the FINN series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the FINN 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 (updated 2024-10-23).

Competing Series

Soil series competing with FINN share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the FINN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the FINN 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 (updated 2024-10-23).

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

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with FINN, 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 (updated 2024-10-23).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing FINN 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
Finn and Tepete families, 0 to 15 percent slopes	101A	34570	509255	k2xl	co647		1:24000
Frisco family, very stony-Finn family, very stony-Water complex, 0 to 20 percent slopes	666A	26650	509375	k31g	co647		1:24000
Frisco family, very stony-Finn family, very stony-Water complex, 0 to 20 percent slopes	666A	7910	3176977	k31g	co650		1:24000
Leighcan, very stony-Finn families, complex, 1 to 60% slopes	607C	4554	507547	k14h	co650		1:24000
Finn and Tepete families, 0 to 15 percent slopes	101A	3399	3176972	k2xl	co650		1:24000
Finn, occasionally ponded-Histic Cryaquepts, frequently ponded, complex, 0 to 2 percent slopes	12102	624	3173428	2yy56	id703		1:24000
Foolhen, rarely flooded-Bearmouth-Finn, frequently flooded families, complex, valley bottoms	644G	6384	148848	4zwk	mt605	2007	1:24000
Libeg-Finn, frequently flooded-Sebud families, complex, alluvial-colluvial deposits	617G	5447	149131	505p	mt605	2007	1:24000
Rooset-Woodhurst-Tiban families, complex, gentle mountain slopes	523E	4864	149210	5087	mt605	2007	1:24000
Finn, frequently flooded-Wander-Foolhen, rarely flooded families, complex, valley bottoms	647G	4640	149133	505r	mt605	2007	1:24000
Wetopa-Finn, frequently flooded-Wichup, rarely flooded families, complex, valley bottoms	642G	1286	149011	501t	mt605	2007	1:24000
Libeg-Finn, frequently flooded-Sebud families, complex, ice-margin slopes	467G	1074	149121	505c	mt605	2007	1:24000
Wetopa-Finn, frequently flooded-Wichup, rarely flooded families, complex, alluvial-colluvial deposits	612G	1009	148721	4zrg	mt605	2007	1:24000
Wetopa-Philipsburg-Prudy families, complex, gentle mountain slopes	523C	355	149229	508v	mt605	2007	1:24000
Bearmouth-Mooseflat-Finn complex, 0 to 4 percent slopes	9B	188	1859513	20dz9	mt605	2007	1:24000
Finn-Water complex, 0 to 4 percent slopes	776B	53	1859588	20f1q	mt605	2007	1:24000
Finn loam, 0 to 4 percent slopes	676B	39	1859583	20f1k	mt605	2007	1:24000
Foolhen-Finn complex, 0 to 4 percent slopes, frequently flooded	72B	8	2403831	2lpcy	mt605	2007	1:24000
Finn-Slagamelt-Hairpin, stony complex, 0 to 8 percent slopes	243C	5	2403837	2lpd4	mt605	2007	1:24000
Bearmouth-Mooseflat-Finn complex, 0 to 4 percent slopes	9B	3507	806446	w25d	mt610	2005	1:24000
Libeg-Finn-Sebud families, complex, alluvial-colluvial deposits	617G	524	1531233	1ndcm	mt610	2005	1:24000
Finn-Wander-Foolhen families, complex, valley bottoms	647G	118	1531245	1ndd0	mt610	2005	1:24000
Foolhen-Finn complex, 0 to 4 percent slopes, frequently flooded	72B	1848	1868613	20qfv	mt612	2011	1:24000
Finn-Slagamelt-Hairpin, stony complex, 0 to 8 percent slopes	243C	1617	1860657	20g56	mt612	2011	1:24000
Tibson-Finn complex, 2 to 25 percent slopes	94E	657	2383943	2l0pd	mt612	2011	1:24000
Copperbasin, rarely flooded-Finn-Mooseflat, occasionally flooded complex, 1 to 4 percent slopes	280B	273	2515392	2ppjl	mt612	2011	1:24000
Finn, frequently flooded-Wander-Foolhen, rarely flooded families, complex, valley bottoms	647G	135	2597762	505r	mt612	2011	1:24000
Foolhen, rarely flooded-Bearmouth-Finn, frequently flooded families, complex, valley bottoms	644G	106	2597748	4zwk	mt612	2011	1:24000
Libeg-Finn, frequently flooded-Sebud families, complex, alluvial-colluvial deposits	617G	64	2597761	505p	mt612	2011	1:24000
Wetopa-Finn, frequently flooded-Wichup, rarely flooded families, complex, valley bottoms	642G	1	2511827	501t	mt612	2011	1:24000
Tibson-Finn complex, 2 to 25 percent slopes	94E	395	2517423	2l0pd	mt614	2012	1:24000
Finn-Slagamelt-Hairpin, stony complex, 0 to 8 percent slopes	243C	61	2520838	20g56	mt614	2012	1:24000
Foolhen-Finn complex, 0 to 4 percent slopes, frequently flooded	72B	37	2520742	20qfv	mt614	2012	1:24000
Finn loam, 0 to 4 percent slopes	676B	1577	154982	568f	mt616	2003	1:24000
Finn-Water complex, 0 to 4 percent slopes	776B	816	155056	56bt	mt616	2003	1:24000
Worock-Finn-Cujob complex, 1 to 25 percent slopes, moderately impacted	5012E	499	154849	5644	mt616	2003	1:24000
Finn gravelly loam, dry, 0 to 4 percent slopes	576B	384	154939	5671	mt616	2003	1:24000
Loberg-Finn complex, 8 to 25 percent slopes	5014E	106	154851	5646	mt616	2003	1:24000
Finn loam, 0 to 4 percent slopes	676B	383	144547	4vdt	mt621	1997	1:24000
Finn-Water complex, 0 to 4 percent slopes	776B	174	144573	4vfn	mt621	1997	1:24000
Cryofluvents-Finn family-Water complex, rolling stream terraces and flood plains	64GJ1	8705	149468	50jk	mt635	2006	1:24000
Finn-Lowder-Dunkleber families, complex, stream terraces and flood plains	64UJ1	4404	149475	50js	mt635	2006	1:24000
Finn-Lowder families, complex, moderately steep young moraines	21UJ1	3701	149409	50gn	mt635	2006	1:24000
Libeg-Marcetta-Finn families, complex, moderately steep young moraines	21UH2	3487	149407	50gl	mt635	2006	1:24000
Libeg-Sebud-Finn families, complex, rolling stream terraces and flood plains	64UH2	1457	149473	50jq	mt635	2006	1:24000
Worock-Cowood-Finn families, complex, steep glaciated mountain slopes and ridges	15VEE	1386	149394	50g5	mt635	2006	1:24000
Elve-Finn families-Water complex, rolling stream terraces and flood plains	64UF2	1261	149472	50jp	mt635	2006	1:24000
Finn-Lowder families, complex, moderately steep trough bottoms	37UJ1	743	149438	50hl	mt635	2006	1:24000
Finn-Elvick families-Water complex, moderately steep young moraines	21GJ2	590	149397	50g8	mt635	2006	1:24000
Redchief-Libeg-Finn families, complex, moderately steep old moraines	22UH2	576	149414	50gt	mt635	2006	1:24000
Braziel-Shawmut-Finn families, complex, moderately steep young moraines	21UHF	298	149408	50gm	mt635	2006	1:24000
Finn loam, 0 to 4 percent slopes	676B	128	1703004	1v53m	mt635	2006	1:24000
Finn-Lowder-Dunkleber families, complex, stream terraces and flood plains	260	76	1703440	1v5kp	mt636	1983	1:24000
Libeg-Marcetta-Finn families, complex, moderately steep young moraines	317	30	1703433	1v5kg	mt636	1983	1:24000
Wetopa-Finn-Wichup families, complex, valley bottoms	302	11	1710159	1vdkf	mt636	1983	1:24000
Elve-Finn families-Water complex, rolling stream terraces and flood plains	64UF2	5	1704490	1v6nk	mt644	1995	1:24000
Moslander-Finn-Philipsburg complex, 0 to 4 percent slopes	1208	971	1697518	1tzdn	wy635		1:24000
Southeast Mountains Sideslopes, Subalpine Fir-Aspen-Meadow Complex	7645	545	2554714	5330	wy635		1:24000
Mountain Front Floodplains, Meadow-Willow-Silver Sagebrush Complex	4111	8	2554698	531f	wy635		1:24000
Southeast Mountains Sideslopes, Subalpine Fir-Aspen-Meadow Complex	7645	5003	151931	5330	wy662	1998	1:24000
Mountain Front Bottoms, Meadow-Willow Complex	4511	677	151920	532n	wy662	1998	1:24000
Mountain Front Floodplains, Meadow-Willow-Silver Sagebrush Complex	4111	670	151882	531f	wy662	1998	1:24000
Foolhen, stony-Finn, occasionally flooded-Adel families, complex, 0 to 6 percent slopes	13	1288	2980435	2wqqk	wy667		1:24000

Map of Series Extent

Approximate geographic distribution of the FINN 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 (updated 2024-10-30).