Soil Data Explorer - CRYAQUOLLS

Official Series Description

Lab Data Summary

Aggregate lab data for the CRYAQUOLLS soil series. This aggregation is based on all pedons with a current taxon name of CRYAQUOLLS, 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 CRYAQUOLLS were used in the calculation. Source: KSSL snapshot (updated 2025-01-21). 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 CRYAQUOLLS 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.

There are insufficient data to create the water balance bar figure.

There are insufficient data to create the water balance line figure.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the CRYAQUOLLS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2025-10-03), parsed OSD records (updated 2025-09-23) and snapshot of SC database (updated 2025-12-01).

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the CRYAQUOLLS 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 2025-10-08).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CRYAQUOLLS 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 2025-10-06).

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.

Competing Series

Soil series competing with CRYAQUOLLS share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2025-09-23) and snapshot of the SC database (updated 2025-12-01).

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the CRYAQUOLLS 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 2025-10-08).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CRYAQUOLLS 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 2025-10-06).

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 CRYAQUOLLS, 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 2025-12-01).

This figure is not available.

Block Diagrams

No block diagrams are available.

Map Units

Map units containing CRYAQUOLLS 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
Cryaquolls, nearly level	21B	415	53938	1t3y	az683	1974	1:24000
Silas family-Cryaquolls association, 0 to 15 percent slopes	114	171	496561	jnq3	co627	1980	1:24000
Cryaquolls and Histosols, flooded	10	3250	498577	jqt4	co630	1975	1:24000
Cryaquolls and Histosols, nearly level	18	1713	498448	jqnz	co633	1981	1:24000
Silas family-Cryaquolls association, 0 to 15 percent slopes	57	482	498429	jqnc	co635	1979	1:24000
Silas family-Cryaquolls association, 0 to 15 percent slopes	101F	5877	509806	k3hc	co636	2011	1:24000
Cryaquolls, cold-Fluvaquentic Haplocryolls association, 0 to 15 percent slopes	100FB	5376	509804	k3h9	co636	2011	1:24000
Cryaquolls-Gateview family complex, 0 to 15 percent slopes	6101A	207	2409404	tqlh	co642	2012	1:24000
Leighcan family, till substratum-Cryaquolls complex, 5 to 40 percent slopes	7202B	44059	766495	tqln	co645		1:24000
Cryaquolls-Gateview family complex, 0 to 15 percent slopes	6101A	28868	766490	tqlh	co645		1:24000
Cryaquolls-Leighcan family, till substratum complex, 0 to 15 percent slopes	7103A	17861	766496	tqlp	co645		1:24000
Leighcan family-Cryaquolls-Moran family complex, 5 to 40 percent slopes	8771B	7973	766492	tqlk	co645		1:24000
Gateview family-Cryaquolls complex, 0 to 15 percent slopes	6102A	7908	766498	tqlr	co645		1:24000
Cryaquepts-Cryaquolls complex, 0 to 15 percent slopes	7102A	5817	766672	tqsc	co645		1:24000
Cryaquolls-Typic Cryohemists complex, 0 to 15 percent slopes	7101A	4473	766497	tqlq	co645		1:24000
Leighcan family, till substratum-Cryaquolls, occasionally flooded complex, 0 to 25 percent slopes	225B	51885	1414885	1jh9g	co654		1:24000
Haplocryolls-Cryaquolls, frequently flooded complex, 0 to 15 percent slopes	104A	34632	1414853	1jh8f	co654		1:24000
Leighcan family, till substratum-Rock outcrop-Cryaquolls complex, 0 to 40 percent slopes	223B	24269	1414884	1jh9f	co654		1:24000
Seitz family-Tellura family, moist-Cryaquolls complex, 0 to 40 percent slopes	382B	24004	1415005	1jhfb	co654		1:24000
Moran family-Rock outcrop-Cryaquolls complex, 0 to 40 percent slopes	908B	22047	1415064	1jhh7	co654		1:24000
Angostura family-Cryaquolls, occasionally flooded complex, 0 to 25 percent slopes	226B	18709	1414887	1jh9j	co654		1:24000
Cryaquolls, frequently flooded-Cryohemists, frequently ponded association, 0 to 5 percent slopes	100A	12297	1414850	1jh8b	co654		1:24000
Moran family-Cryaquolls-Cryohemists, frequently ponded complex, 0 to 25 percent slopes	908A	6442	1415063	1jhh6	co654		1:24000
Haplocryolls-Cryaquolls, occasionally flooded-Cryohemists, frequently ponded complex, 0 to 25 percent slopes	930A	4341	1415065	1jhh8	co654		1:24000
Haplocryolls-Haplocryepts-Cryaquolls complex, 0 to 40 percent slopes	930B	4085	3208636	2zd5w	co654		1:24000
Cryaquolls, frequently flooded-Cryohemists, frequently ponded association, 0 to 5 percent slopes	100A		3176999	1jh8b	co657		1:24000
Pierian family-Cryaquolls, frequently flooded association, 0 to 15 percent slopes	127F		500763	jt2n	co657		1:24000
Haplocryolls-Cryaquolls, frequently flooded complex, 0 to 15 percent slopes	104A		3177000	1jh8f	co657		1:24000
Cryofluvents-Cryaquolls-Histosols complex, 0 to 15 percent slopes, frequently flooded	100F		500737	jt1t	co657		1:24000
Haplocryolls, rarely flooded-Cryaquolls, frequently flooded association, 0 to 15 percent slopes	110F		500759	jt2j	co657		1:24000
Leighcan family, till substratum-Cryaquolls, occasionally flooded complex, 0 to 25 percent slopes	225B	47910	3177006	1jh9g	co657		1:24000
Moran family-Rock outcrop-Cryaquolls, frequently ponded complex, 0 to 40 percent slopes	908C	26903	500843	jt57	co657		1:24000
Leighcan family-Cryaquolls, frequently flooded complex, 0 to 25 percent slopes	625G	23579	500804	jt3z	co657		1:24000
Seitz family-Tellura family, moist-Cryaquolls complex, 0 to 40 percent slopes	382B	22216	3177027	1jhfb	co657		1:24000
Moran family-Rock outcrop-Cryaquolls complex, 0 to 40 percent slopes	908B	20139	3177058	1jhh7	co657		1:24000
Angostura family-Cryaquolls, occasionally flooded complex, 0 to 25 percent slopes	226B	17311	3177007	1jh9j	co657		1:24000
Moran family-Cryaquolls, frequently ponded-Histosols, frequently ponded complex, 0 to 25 percent slopes	950C	7999	500846	jt5b	co657		1:24000
Moran family-Cryaquolls-Cryohemists, frequently ponded complex, 0 to 25 percent slopes	908A	5931	3177057	1jhh6	co657		1:24000
Haplocryolls-Cryaquolls, occasionally flooded-Cryohemists, frequently ponded complex, 0 to 25 percent slopes	930A	4008	3177059	1jhh8	co657		1:24000
Haplocryolls-Cryaquolls, frequently ponded complex, 0 to 25 percent slopes	903C	3526	500842	jt56	co657		1:24000
Frisco family-Cryaquolls, frequently flooded complex, 0 to 25 percent slopes	621G	3523	500802	jt3x	co657		1:24000
Leighcan family-Rock outcrop-Cryaquolls, frequently flooded complex, 0 to 40 percent slopes	623G	2223	500803	jt3y	co657		1:24000
Cryaquolls and Borohemists, 0 to 10 percent slopes	127	12029	509477	k34r	co660	1994	1:24000
Needleton family-Cryaquolls complex, 0 to 40 percent slopes	169	9571	509531	k36h	co660	1994	1:24000
Broad Canyon, warm-Bullbasin-Cryaquolls complex, 0 to 30 percent slopes	110	9385	509455	k341	co660	1994	1:24000
Cryaquolls and histosols	Cs	21741	509733	k3f0	co661	1968	1:31680
Haplocryolls-Cryaquolls, frequently flooded complex, 0 to 15 percent slopes	104A	2023	3176931	1jh8f	co661	1968	1:31680
Haplocryolls-Cryaquolls, occasionally flooded-Cryohemists, frequently ponded complex, 0 to 25 percent slopes	930A	1469	3176938	1jhh8	co661	1968	1:31680
Moran family-Rock outcrop-Cryaquolls complex, 0 to 40 percent slopes	908B	1311	3176937	1jhh7	co661	1968	1:31680
Angostura family-Cryaquolls, occasionally flooded complex, 0 to 25 percent slopes	226B	878	3176948	1jh9j	co661	1968	1:31680
Haplocryolls-Haplocryepts-Cryaquolls complex, 0 to 40 percent slopes	930B	678	3176993	2zd5w	co661	1968	1:31680
Cryaquolls	Cr	582	509732	k3dz	co661	1968	1:31680
Moran family-Cryaquolls-Cryohemists, frequently ponded complex, 0 to 25 percent slopes	908A	260	3176940	1jhh6	co661	1968	1:31680
Leighcan family, till substratum-Rock outcrop-Cryaquolls complex, 0 to 40 percent slopes	223B	82	3176933	1jh9f	co661	1968	1:31680
Leighcan family, till substratum-Cryaquolls, occasionally flooded complex, 0 to 25 percent slopes	225B	48	3176926	1jh9g	co661	1968	1:31680
Cryaquolls, frequently flooded-Cryohemists, frequently ponded association, 0 to 5 percent slopes	100A	35	3176958	1jh8b	co661	1968	1:31680
Cryolls-Cryaquolls association, 0 to 15 percent slopes	108	10980	505012	jyhq	co663	2000	1:24000
Cryaquolls-Cryohemists complex, 0 to 5 percent slopes	106	4576	505010	jyhn	co663	2000	1:24000
Cryaquolls-Cryoborolls association, 0 to 20 percent slopes	124	52147	2453669	2nc7m	co664	1987	1:24000
Cryohemists-Cryaquolls association, 0 to 12 percent slopes	128	20224	2453673	2nc7r	co664	1987	1:24000
Quander-Cryaquolls-Cryohemists association, 1 to 30 percent slopes	161	9197	2453698	2nc8k	co664	1987	1:24000
Conejos-Youga-Cryaquolls complex, 0 to 30 percent slopes	H3-D	1373	780326	v5zt	co668	2018	1:24000
Cryohemists-Cryaquolls association, 0 to 8 percent slopes	128	278	783664	v9gh	co668	2018	1:24000
Cryaquolls-Argicryolls association, 0 to 20 percent slopes	124	65	782514	v88d	co668	2018	1:24000
Typic Cryaquents-Cryaquolls-Cryofibrists complex, 0 to 5 percent slopes	56	6090	737691	srmh	co672	2003	1:24000
Cryaquolls-Typic Cryaquents complex, 1 to 5 percent slopes	53	4162	737689	srmf	co672	2003	1:24000
Quazar-Cryaquolls-Cryohemists association, 1 to 30 percent slopes	967	37	507312	k0wx	co672	2003	1:24000
Cryaquolls, 0 to 3 percent slopes	905	26	507287	k0w3	co672	2003	1:24000
Cryaquolls-Borohemists complex, 0 to 5 percent slopes	109	5603	505157	jynd	co674	1998	1:24000
Cryoborolls-Cryaquolls association, 0 to 15 percent slopes	111	2614	505160	jynh	co674	1998	1:24000
Cryaquolls, 0 to 3 percent slopes	108	12	505156	jync	co674	1998	1:24000
Cryaquolls, 0 to 3 percent slopes	37	1010	502045	jvf0	co675	1986	1:24000
Cryaquolls, nearly level	20	300	496760	jnxj	co683	1977	1:24000
Cryaquolls, 2 to 8 percent slopes	2609	189	2493279	51kk	id650	2011	1:24000
Cryaquolls and Cryaquolls, very poorly drained, 0 to 6 percent slopes	2606	10329	150458	51kh	id758	1998	1:24000
Cryaquolls, 2 to 8 percent slopes	2609	2751	150460	51kk	id758	1998	1:24000
Cryaquolls, 0 to 2 percent slopes	2000	2277	150454	51kc	id758	1998	1:24000
Bootjack and Cryaquolls, 0 to 2 percent slopes	2608	53	150459	51kj	id758	1998	1:24000
Graminoid Cryaquolls, 0 to 2 percent slopes	157	614	83726	2t3v	id762	1988	1:24000
Salix/Graminoid Cryaquolls and Salix/Graminoid Cryaquolls, poorly drained, 0 to 6 percent slopes	159	513	83728	2t3x	id762	1988	1:24000
Cryaquolls and Cryaquents, flood plains	66-1A	11262	157206	58l5	mt623	1988	1:24000
Typic Cryochrepts-Rock outcrop-Cryaquolls complex, glaciated moutain ridges	22-3C	7526	157160	58jp	mt623	1988	1:24000
Bridger-Cryaquolls complex, 2 to 25 percent slopes	25	1150	146447	4xd3	mt636	1983	1:24000
Presa-Cryaquolls association, steep	PYF	8627	507865	k1gr	nm670	1976	1:24000
Cryoborolls-Cryaquolls complex, 0 to 8 percent slopes	CTC	3562	507804	k1ds	nm670	1976	1:24000
Quander-Cryaquolls, occasionally flooded-Cryohemists, frequently flooded, association, 1 to 30 percent slopes, stony	QcE	42	2770162	2tl92	nm672		1:24000
Cryaquolls, frequently flooded-Argicryolls association, 0 to 20 percent slopes	CqD	24	2770156	2tl8w	nm672		1:24000
Aquic Vitricryands-Cryaquolls-Histic Cryaquands complex, rarely flooded, 0 to 5 percent slopes	1601	4165	3462435	31xz4	or605		1:24000
Steiger-Silverdollar-Cryaquolls, rarely flooded, complex, 0 to 5 percent slopes	1337	2141	3462389	31vb8	or605		1:24000
Cryaquolls, rarely flooded, 0 to 3 percent slopes	1603	671	3462437	31xz6	or605		1:24000
Cryaquolls, 0 to 3 percent slopes	29A	8118	63591	245b	or620	1992	1:24000
Haploxerolls-Endoaquolls-Cryaquolls association, 0 to 3 percent slopes	s6505	1631	3439624	30xwy	or626	2018	1:24000
Becks family-Cryaquolls-Silas family complex, 0 to 5 percent slopes, flooded	42		3312879	30gws	ut645		1:24000
Haploxerandic Haplocryepts-Cryaquolls complex, 0 to 35 percent slopes	285	270	1899819	21rxh	wa649	2008	1:24000
Vitrixerandic Haplocryepts-Cryaquolls, 0 to 5 percent slopes	541	150	1900735	21sw1	wa649	2008	1:24000
Naxing-Darland-Cryaquolls complex, 0 to 50 percent slopes	75	551	75631	2jpq	wa680	2003	1:24000
Andic Eutrocryepts-Cryaquolls complex, 0 to 35 percent slopes	105	1843	75728	2jsv	wa749	2005	1:24000
Vitrandic Eutrocryepts-Cryaquolls complex, 0 to 5 percent slopes	386	1172	75743	2jtb	wa749	2005	1:24000
Cryaquolls, 0 to 5 percent	87	11	152136	539m	wy043	1976	1:24000
Cryaquolls, 1 to 9 percent slopes	143	4706	501680	jv17	wy601	1991	1:24000
Cryaquolls and Cryaquepts	CR	5695	152693	53wl	wy623	1971	1:20000
Cryaquepts, Cryaquolls, and Cryofluvents soils, 0 to 3 percent slopes, volcanic alluvium, frequently flooded	102	839	3302899	596v	wy629		1:24000
Cryofluvents, extremely stony Cryaquolls, extremely stony and Cryaquepts soils, 0 to 15 percent slopes, frequently flooded	402	12	3250495	598x	wy629		1:24000
Cryaquolls, 1 to 9 percent slopes -- draft	1143	1499	2573050	2x8p6	wy630		1:24000
Cryaquepts, Cryaquolls, and Cryofluvents soils, 0 to 15 percent slopes, granite alluvium	607	212	1857226	20blj	wy647		1:24000
Cryaquepts, Cryaquolls, and Cryofluvents soils, 0 to 3 percent slopes, volcanic alluvium	613	10	1862622	20j6l	wy647		1:24000
Cryaquolls, 0 to 5 percent slopes	16	14328	158027	59fn	wy650	1982	1:24000
Cryaquepts, Cryaquolls, and Cryofluvents soils, 0 to 3 percent slopes, volcanic alluvium, frequently flooded	102	43057	157816	596v	wy656	2008	1:24000
Cryaquepts, Cryaquolls, and Cryofluvents soils, 0 to 15 percent slopes, granite alluvium	302	10305	157898	599h	wy656	2008	1:24000
Typic Cryochrepts-Rock outcrop-Cryaquolls complex, glaciated mountain ridges	22-3C	6186	157965	59cn	wy656	2008	1:24000
Cryofluvents-Cryaquolls-McCort family complex, 0 to 30 percent slopes	412	4039	157888	5995	wy656	2008	1:24000
Cryaquolls-Cryaquepts-Eutrocryepts complex, 0 to 55 percent slopes	190	2717	157862	598b	wy656	2008	1:24000
Cryaquepts-Cryaquolls-Cryofibrists complex, 0 to 15 percent slopes	318	2207	157913	599z	wy656	2008	1:24000
Cryaquepts, Cryaquolls, and Cryofluvents soils, 0 to 35 percent slopes, sedimentary alluvium	201	1428	157778	595m	wy656	2008	1:24000
Cryaquolls, Cryofluvents, and Riverwash, 0 to 15 percent slopes	301	1361	157897	599g	wy656	2008	1:24000
Cryofluvents, Cryaquepts, and Cryaquolls soils, 0 to 35 percent slopes	202	1254	157779	595n	wy656	2008	1:24000
Cryofluvents, extremely stony Cryaquolls, extremely stony and Cryaquepts soils, 0 to 15 percent slopes, frequently flooded	402	763	157880	598x	wy656	2008	1:24000
Cryaquolls-Cryofibrists complex *	12	14014	153259	54gv	wy666	1978	1:24000
Cryaquolls, 0 to 5 percent slopes	981	1204	1528046	1n91t	wy719	2013	1:24000

Map of Series Extent

Approximate geographic distribution of the CRYAQUOLLS 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 2025-10-04).