Soil Data Explorer - AGASSIZ

Official Series Description

Lab Data Summary

Aggregate lab data for the AGASSIZ soil series. This aggregation is based on all pedons with a current taxon name of AGASSIZ, 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 AGASSIZ were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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 AGASSIZ 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 AGASSIZ 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 AGASSIZ 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 AGASSIZ 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).

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

Competing Series

Soil series competing with AGASSIZ 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 AGASSIZ 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 AGASSIZ 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 terrace figure.

Soil series sharing subgroup-level classification with AGASSIZ, 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 AGASSIZ 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
Rodie-Shalcleav-Agassiz association	420	4275	475030	hy9k	nv765	1986	1:24000
Agassiz-Croesus-Rubble land association	1010	3945	474862	hy44	nv765	1986	1:24000
Amene-Ekim-Agassiz assocation	561	2620	475056	hybd	nv765	1986	1:24000
Agassiz-Skutum-Lizzant complex, 25 to 70 percent slopes	DRG	19795	2810262	2trdn	ut013		1:24000
Senchert-Calfhollow-Agassiz complex, 5 to 35 percent slopes	QuC	5495	2503735	2pw0c	ut013		1:24000
Starvation-Isbell-Agassiz complex, 15 to 60 percent slopes, very stony	SNF	2788	1428095	1jy1l	ut013		1:24000
Agassiz-Rock outcrop-Sheep Creek association, 25 to 75 percent slopes, extremely stony	SRG	687	1426064	1jvy2	ut013		1:24000
Agassiz-Picayune association, very steep	AGG	4887	481316	j4vb	ut602	1969	1:20000
Elzinga-Agassiz association, steep	EMF	855	481345	j4w8	ut602	1969	1:20000
AGASSIZ-DATEMAN ASSOCIATION, ERODED	ADG2	14318	482657	j67l	ut603	1968	1:20000
AGASSIZ-BRADSHAW ASSOCIATION, ERODED	ABG2	9508	482656	j67k	ut603	1968	1:20000
BICKMORE-SHEEP CREEK ASSOCIATION, ERODED	BLG2	8423	482675	j685	ut603	1968	1:20000
SHEEP CREEK-AGASSIZ ASSOCIATION, ERODED	SOG2	6259	482826	j6f1	ut603	1968	1:20000
BRADSHAW-AGASSIZ ASSOCIATION, ERODED	BSG2	5012	482676	j686	ut603	1968	1:20000
MULT-AGASSIZ ASSOCIATION	MNE	3717	482772	j6c9	ut603	1968	1:20000
AGASSIZ VERY COBBLY SILT LOAM, 6 TO 30 PERCENT SLOPES	AAE	2927	482654	j67h	ut603	1968	1:20000
AGASSIZ-ELWOOD ASSOCIATION, ERODED	AEG2	2717	482658	j67m	ut603	1968	1:20000
PICAYUNE-AGASSIZ ASSOCIATION, ERODED	POG2	2554	482794	j6d0	ut603	1968	1:20000
AGASSIZ VERY COBBLY SILT LOAM, 30 TO 70 PERCENT SLOPES,ERODED	AAG2	1817	482655	j67j	ut603	1968	1:20000
POLELINE-AGASSIZ ASSOCIATION, ERODED	PSG2	1671	482796	j6d2	ut603	1968	1:20000
AGASSIZ-GORING ASSOCIATION	AGE	1548	482659	j67n	ut603	1968	1:20000
HOSKIN-ELZINGA ASSOCIATION, ERODED	HMG2	1510	482731	j69z	ut603	1968	1:20000
AGASSIZ-GORING ASSOCIATION, ERODED	AGG2	1444	482660	j67p	ut603	1968	1:20000
BICKMORE-AGASSIZ ASSOCIATION, ERODED	BKG2	1338	482674	j684	ut603	1968	1:20000
LUCKY STAR-RED SPUR COMPLEX, 6 TO 30 PERCENT SLOPES	LWE	1123	482764	j6c1	ut603	1968	1:20000
MULT-AGASSIZ ASSOCIATION, ERODED	MNG2	1081	482773	j6cb	ut603	1968	1:20000
ELWOOD-AGASSIZ ASSOCIATION	EGE	999	482712	j69c	ut603	1968	1:20000
MULT-LUCKY STAR ASSOCIATION	MSE	668	482774	j6cc	ut603	1968	1:20000
Agassiz-Rock outcrop complex, 25 to 60 percent slopes	ACF	8030	503800	jx7m	ut604	1980	1:24000
Mult-Agassiz complex, 10 to 25 percent slopes	MCD	2340	503876	jxb2	ut604	1980	1:24000
Agassiz-Mult complex, 10 to 25 percent slopes	AAD	2030	503797	jx7j	ut604	1980	1:24000
Agassiz-Richville complex, 10 to 60 percent slopes	ABF	1250	503799	jx7l	ut604	1980	1:24000
Agassiz-Mult complex, 25 to 60 percent slopes	AAF	1230	503798	jx7k	ut604	1980	1:24000
Richens-Agassiz complex, 25 to 60 percent slopes	RGF	550	503895	jxbp	ut604	1980	1:24000
Agassiz-Rock outcrop complex, 30 to 70 percent slopes	AbF	19575	482445	j60r	ut608	1981	1:24000
Agassiz very stony loam, 30 to 70 percent slopes	AaF	2057	482444	j60q	ut608	1981	1:24000
Calpac-Agassiz complex, 30 to 70 percent slopes	CbF	1886	482476	j61r	ut608	1981	1:24000
Agassiz-Rock outcrop complex, 40 to 70 percent slopes	AaG	12030	506504	k01v	ut609	1974	1:24000
Geertsen-Agassiz complex, 30 to 70 percent slopes	GcG	5005	506549	k039	ut609	1974	1:24000
Agassiz-Rock outcrop complex, shallow, 40 to 70 percent slopes	AbG	2320	506505	k01w	ut609	1974	1:24000
Agassiz-Geertsen-Rock outcrop association, very steep	AGG	1555	506503	k01t	ut609	1974	1:24000
Bradshaw-Agassiz association, steep	BEG	9795	482868	j6gd	ut612	1967	1:20000
Agassiz association, very steep	AGG	2573	482865	j6g9	ut612	1967	1:20000
Horrocks-Agassiz very cobbly loams, 30 to 70 percent slopes	143	16114	508187	k1t4	ut613	1999	1:24000
Hades-Agassiz-Rock outcrop complex, 30 to 70 percent slopes	136	11611	508180	k1sx	ut613	1999	1:24000
Agassiz-Rock outcrop complex, 30 to 70 percent slopes	101	6240	508227	k1vf	ut613	1999	1:24000
Agassiz-Wallsburg association, very steep	AWF	608	504175	jxmq	ut622	1967	1:24000
Burgi-Agassiz association, very steep	BXF	576	504202	jxnl	ut622	1967	1:24000
Agassiz very cobbly loam, 25 to 60 percent slopes	AGF	446	504174	jxmp	ut622	1967	1:24000
Agassiz channery silt loam, 10 to 40 percent slopes	75	2266	756857	tdkr	ut647		1:24000
Agassiz-Bezzant family, very stony-Rock outcrop complex, 30 to 70 percent slopes	103	2049	757982	tfr1	ut647		1:24000
Agassiz channery silt loam, 40 to 70 percent slopes	78	1957	757481	tf6w	ut647		1:24000
Agassiz-Abes-Rock outcrop complex, 15 to 70 percent slopes	104	1733	757981	tfr0	ut647		1:24000
Agassiz, extremely stony-Onkeyo, rubbly-Bradshaw families association, 30 to 70 percent slopes	R35	562	623909	ny73	ut647		1:24000
Bezzant family, very stony-Agassiz association, 30 to 70 percent slopes	40-78	265	757990	tfr9	ut647		1:24000
Agassiz-Abes association, 15 to 70 percent slopes	70-78	146	757482	tf6x	ut647		1:24000
Agassiz-Hourglass families-Rock outcrop complex, 30 to 70 percent slopes	103		625182	nzk5	ut649		1:24000
Agassiz family-Rock outcrop complex, 15 to 50 percent slopes	104		581646	mj7s	ut649		1:24000
Forsey-Forsey, moderately deep-Agassiz families, association, 30 to 70 percent slopes	155		581651	mj7y	ut649		1:24000
Pernty family-Agassiz family-Rock outcrop complex, 40 to 75 percent slopes	182		581653	mj80	ut649		1:24000
Pernty family-Agassiz family-Rock outcrop complex, 5 to 40 percent slopes	181		581655	mj82	ut649		1:24000
Agassiz-Forsey families-Rock outcrop complex, 30 to 70 percent slopes	102		625183	nzk6	ut649		1:24000
Jebo family, extremely stony-Agassiz family, rubbly complex, 25 to 60 percent slopes	63	4581	812397	w8cc	ut651		1:24000

Map of Series Extent

Approximate geographic distribution of the AGASSIZ 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).