Soil Data Explorer - TYPIC CRYORTHENTS

Official Series Description

Lab Data Summary

Aggregate lab data for the TYPIC CRYORTHENTS soil series. This aggregation is based on all pedons with a current taxon name of TYPIC CRYORTHENTS, 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 TYPIC CRYORTHENTS 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 TYPIC CRYORTHENTS 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 TYPIC CRYORTHENTS 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).

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the TYPIC CRYORTHENTS 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the TYPIC CRYORTHENTS 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 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 TYPIC CRYORTHENTS 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).

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the TYPIC CRYORTHENTS 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the TYPIC CRYORTHENTS 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 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 TYPIC CRYORTHENTS, 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).

This figure is not available.

Block Diagrams

No block diagrams are available.

Map Units

Map units containing TYPIC CRYORTHENTS 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
Typic Cryorthents-Urban land complex	185	2119	692935	r81r	ak610	2003	1:25000
Typic Cryorthents, pit spoil	184	1836	692930	r81l	ak610	2003	1:25000
Salchaket-Typic Cryorthents complex	164	1067	692938	r81v	ak610	2003	1:25000
Typic Cryofluvents and Typic Cryorthents soils, 0 to 5 percent slopes	453X	4000	49525	1njl	ak645	1992	1:31680
Urban land-Typic Cryorthents complex, 0 to 2 percent slopes	UC	2008	51103	1q5h	ak650	2006	1:24000
Typic Cryorthents, pit spoil	CL	668	51116	1q5x	ak650	2006	1:24000
Typic Cryorthents, 100 to 150 percent slopes	703	13946	1488138	1lyjg	ak652	2005	1:25000
Dystrocryepts-Typic Cryorthents-Iliamna, cool, complex, 4 to 35 percent slopes	560	2184	1487995	1lycv	ak652	2005	1:25000
Badland, sea cliffs-Typic Cryorthents complex, very steep	504	1403	1487939	1lyb1	ak652	2005	1:25000
Kalifonsky-Typic Cryorthents complex, 4 to 45 percent slopes	591	1097	1488026	1lydv	ak652	2005	1:25000
Typic Cryorthents-Urban land complex	29CR01	978	2025490	25zpd	ak655	2007	1:25000
Lithic Cryofolists-Typic Cryorthents-Typic Histoturbels complex	634	19981	1542128	2z3py	ak683	2005	1:63360
Typic Cryorthents, frequently flooded,-Gushdoiman complex, 0 to 2 percent slopes	D32MCB	2277	3352440	2y248	ak684	2012	1:63360
Crowberry-Typic Cryaquents, frequently flooded, complex, 0 to 2 percent slopes	D31MCA	35240	2922720	2wc6w	ak686	2023	1:63360
Typic Cryorthents, frequently flooded,-Gushdoiman complex, 0 to 2 percent slopes	D32MCB	17793	3089235	2y248	ak686	2023	1:63360
Typic Cryorthents, frequently flooded,-Mine Tailings-Crowberry complex, 0 to 8 percent slopes	D31MCC	6792	3013832	2x94p	ak686	2023	1:63360
Typic Cryaquents-Typic Cryorthents association, flat lowlands, 0 to 5 percent slopes	20PLD	1895	3232636	2tptd	ak692	2021	1:63360
Typic Cryorthents-Typic Cryofluvents association, floodplains, 0 to 5 percent slope	20FPZ	132	3232638	2tpsx	ak692	2021	1:63360
Typic Cryorthents-Typic Haplocryods association, flat lowlands, late seral, 0 to 5 percent slopes	6228A	20754	2805086	2tpt3	ak693	2019	1:63360
Typic Cryorthents-Typic Cryaquents complex, glacial topography, 6 to 35 percent slopes	6366B	12228	2805098	2tpth	ak693	2019	1:63360
Typic Haplocryods-Typic Cryorthents association, uplifted beach ridges and dunes, 0 to 15 percent slopes	7465B	10752	2805112	2tpty	ak693	2019	1:63360
Typic Cryorthents-Oxyaquic Cryofluvents complex, outburst floodplains, mid seral, 0 to 5 percent slopes	6480A	10311	2805104	2tptp	ak693	2019	1:63360
Typic Haplocryods-Typic Cryorthents complex, outburst floodplains, 0 to 5 percent slopes	6428A	7644	2805102	2tptm	ak693	2019	1:63360
Typic Cryaquents-Typic Cryorthents association, flat lowlands, 0 to 5 percent slopes	6298A	6773	2805095	2tptd	ak693	2019	1:63360
Typic Cryorthents-Typic Haplocryods complex, flat lowlands, mid seral, 0 to 5 percent slopes	6265A	5767	2805088	2tpt5	ak693	2019	1:63360
Typic Cryorthents-Oxyaquic Cryofluvents complex, outburst floodplains, late seral, 0 to 5 percent slopes	6483A	3560	2805105	2tptq	ak693	2019	1:63360
Typic Cryorthents-Typic Cryofluvents association, floodplains, 0 to 5 percent slope	5381A	3261	2805080	2tpsx	ak693	2019	1:63360
Typic Cryorthents, flat lowlands, willow phase, 0 to 5 percent slopes	6211A	2337	2805083	2tpt0	ak693	2019	1:63360
Typic Cryorthents, flat lowlands, late seral, 0 to 5 percent slopes	6283A	2131	2805091	2tpt8	ak693	2019	1:63360
Typic Cryorthents, flat lowlands, mid seral, 0 to 5 percent slopes	6280A	1114	2805090	2tpt7	ak693	2019	1:63360
Rubble land-Typic Cryorthents-Rock outcrop-Xeric Dystrocryepts complex, 30 to 80 percent slopes, mountainflanks, metamorphic, mafic, cryic	210yp	916	1670108	hn82	ca731	1981	1:24000
Rock outcrop-Typic Cryorthents-Xeric Dystrocryepts complex, 0 to 35 percent slopes, mountain slopes, joints, cryic	267yp	113	1670123	1ns1c	ca731	1981	1:24000
Rock outcrop, granitic-Canisrocks-Typic Cryorthents, warm complex, 30 to 100 percent slopes	2138	4139	3422873	2r1c4	ca732	1998	1:24000
Rock outcrop, granitic-Typic Cryorthents, warm complex, 30 to 90 percent slopes	2130	2577	3422871	2twpj	ca732	1998	1:24000
Canisrocks-Typic Cryorthents, warm-Rock outcrop, granitic complex, 30 to 100 percent slopes	2137	1614	3422872	2tbf2	ca732	1998	1:24000
Rock outcrop, granitic-Typic Cryorthents-Canisrocks, scree complex, 30 to 100 percent slopes	1137	1279	3422866	2t8zr	ca732	1998	1:24000
Typic Cryorthents, metamorphic, 30 to 90 percent slopes	1151	494	3422867	2w869	ca732	1998	1:24000
Typic Cryorthents, 15 to 50 percent slopes	106H	294	2766843	hnsp	ca732	1998	1:24000
Typic Cryorthents-Xeric Dystrocryepts-Oxyaquic Dystrocryepts complex, 15 to 45 percent slopes, metamorphic, mountain slopes, lateral moraines, cryic	221yp	268	2229327	2dtss	ca732	1998	1:24000
Rubble land-Typic Cryorthents-Rock outcrop-Xeric Dystrocryepts complex, 30 to 80 percent slopes, mountainflanks, metamorphic, mafic, cryic	210yp	94	2229324	2dtsp	ca732	1998	1:24000
Typic Cryorthents-Rock outcrop complex, 0 to 45 percent slopes	114H	26	2766844	hnsy	ca732	1998	1:24000
Xeric Vitricryands-Typic Cryorthents, tephritic complex, 0 to 45 percent slopes	104H	18	2766841	hnsm	ca732	1998	1:24000
Typic Cryorthents, 0 to 35 percent slopes	105H	12	2766842	hnsn	ca732	1998	1:24000
Typic Cryorthents, 30 to 90 percent slopes	1103	8	3422865	2t8z1	ca732	1998	1:24000
Rock outcrop-Typic Cryorthents complex, 40 to 85 percent slopes	148	96387	466892	hnv1	ca740	1996	1:24000
Rock outcrop-Typic Cryorthents complex, 0 to 45 percent slopes	147	68359	466891	hnv0	ca740	1996	1:24000
Typic Cryorthents, 0 to 35 percent slopes	105	33371	466849	hnsn	ca740	1996	1:24000
Typic Cryorthents-Rock outcrop complex, 0 to 45 percent slopes	114	27535	466858	hnsy	ca740	1996	1:24000
Typic Cryorthents-Rock outcrop complex, 40 to 85 percent slopes	115	27136	466859	hnsz	ca740	1996	1:24000
Typic Cryorthents-Rock outcrop-Lithic Cryorthents complex, tephritic, 0 to 30 percest slopes	117	16313	466861	hnt1	ca740	1996	1:24000
Typic Cryumbrepts-Dystric Cryochrepts-Typic Cryorthents complex, 0 to 30 percent slopes	140	16104	466884	hnts	ca740	1996	1:24000
Rock outcrop-Typic Cryorthents-Lithic Cryorthents complex, 0 to 30 percent slopes	149	15630	466893	hnv2	ca740	1996	1:24000
Typic Cryorthents-Dystric Cryochrepts-Rock outcrop complex, 0 to 30 percent slopes	109	15105	466853	hnss	ca740	1996	1:24000
Typic Cryorthents-Typic Cryochrepts-Rock outcrop complex, 0 to 45 percent slopes	111	13722	466855	hnsv	ca740	1996	1:24000
Typic Cryorthents-Entic Cryumbrepts complex, 0 to 45 percent slopes	112	12533	466856	hnsw	ca740	1996	1:24000
Typic Cryorthents-Typic Cryumbrepts-Rock outcrop complex, 0 to 45 percent slopes	113	11237	466857	hnsx	ca740	1996	1:24000
Typic Cryorthents-Dystric Cryochrepts complex, 15 to 60 percent slopes	108	10980	466852	hnsr	ca740	1996	1:24000
Typic Cryumbrepts-Typic Cryorthents-Rock outcrop complex, 0 to 30 percent slopes	139	9941	466883	hntr	ca740	1996	1:24000
Rock outcrop-Typic Cryorthents complex, volcanic, 10 to 45 percent slopes	150	9711	466894	hnv3	ca740	1996	1:24000
Xeric Vitricryands-Typic Cryorthents, tephritic complex, 0 to 45 percent slopes	104	8690	466848	hnsm	ca740	1996	1:24000
Typic Cryorthents-Dystric Cryochrepts-Rock outcrop association, 15 to 45 percent slopes	110	8555	466854	hnst	ca740	1996	1:24000
Typic Cryorthents-Rock outcrop-Lithic Cryorthents complex, 0 to 30 percent slopes	116	8058	466860	hnt0	ca740	1996	1:24000
Dystric Cryochrepts-Typic Cryorthents association, 0 to 30 percent slopes	133	7179	466877	hntk	ca740	1996	1:24000
Typic Cryumbrepts-Dystric Cryochrepts-Typic Cryorthents complex, 15 to 45 percent slopes	141	5999	466885	hntt	ca740	1996	1:24000
Rock outcrop-Typic Cryorthents-Lithic Cryorthents association, volcanic, 0 to 30 percent slopes	151	5986	466895	hnv4	ca740	1996	1:24000
Dystric Cryochrepts-Entic Cryumbrepts-Typic Cryorthents complex, 0 to 45 percent slopes	134	5213	466878	hntl	ca740	1996	1:24000
Typic Cryorthents-Rock outcrop-Lithic Cryorthents complex, tephritic, 30 to 65 percent slopes	118	5107	466862	hnt2	ca740	1996	1:24000
Typic Cryorthents, moraine-Glaciers complex, 15 to 90 percent slopes	1011	5016	3233141	2t8yx	ca740	1996	1:24000
Typic Cryorthents, 15 to 50 percent slopes	106	4937	466850	hnsp	ca740	1996	1:24000
Rock outcrop, granitic crags-Typic Cryorthents complex, 30 to 100 percent slopes	1101	4830	3231035	2tbfb	ca740	1996	1:24000
Typic Cryorthents-Xeric Vitricryands-Rock outcrop complex, volcanic, 0 to 45 percent slopes	119	4659	466863	hnt3	ca740	1996	1:24000
Typic Cryorthents, 30 to 90 percent slopes	1103	4518	3231048	2t8z1	ca740	1996	1:24000
Rock outcrop, granitic-Typic Cryorthents-Canisrocks, scree complex, 30 to 100 percent slopes	1137	3894	3231058	2t8zr	ca740	1996	1:24000
Rubble land-Typic Cryorthents-Rock outcrop-Xeric Dystrocryepts complex, 30 to 80 percent slopes, mountainflanks, metamorphic, mafic, cryic	210yp	2458	2230063	2dvkj	ca740	1996	1:24000
Rock outcrop-Typic Cryorthents-Typic Cryoborolls complex, volcanic, 25 to 50 percent slopes	152	1909	466896	hnv5	ca740	1996	1:24000
Typic Cryorthents, 50 to 85 percent slopes	107	1357	466851	hnsq	ca740	1996	1:24000
Rock outcrop, granitic-Typic Cryorthents, warm complex, 30 to 90 percent slopes	2130	1318	3422931	2twpj	ca740	1996	1:24000
Canisrocks-Typic Cryorthents, warm-Rock outcrop, granitic complex, 30 to 100 percent slopes	2137	1120	3231046	2tbf2	ca740	1996	1:24000
Typic Cryorthents, metamorphic, 30 to 90 percent slopes	1203	663	3231049	2w869	ca740	1996	1:24000
Rock outcrop, granitic-Canisrocks-Typic Cryorthents, warm complex, 30 to 100 percent slopes	2138	606	3231044	2r1c4	ca740	1996	1:24000
Rock outcrop, metamorphic crags-Typic Cryorthents, metamorphic complex, 30 to 90 percent slopes	1201	568	3292039	2tbfc	ca740	1996	1:24000
Typic Cryorthents, warm metamorphic-Rock outcrop, metamorphic-Canisrocks complex, 30 to 100 percent slopes	2230	355	3231059	2w86n	ca740	1996	1:24000
Rock outcrop, metamorphic-Typic Cryorthents, metamorphic-Benchlake family complex, 10 to 100 percent slopes	1237	260	3231060	2w870	ca740	1996	1:24000
Rock outcrop, metamorphic-Typic Cryorthents, warm metamorphic-Benchlake, warm complex, 15 to 100 percent slopes	2235	139	3231050	2w86c	ca740	1996	1:24000
Rock outcrop, metamorphic-Benchlake family-Typic Cryorthents, metamorphic complex, 10 to 120 percent slopes	1215	127	3292037	2w86m	ca740	1996	1:24000
Typic Cryorthents, warm-Rock outcrop, granitic-McGee complex, 5 to 60 percent slopes	2147	106	3292042	2w86q	ca740	1996	1:24000
Typic Cryorthents-Xeric Dystrocryepts-Oxyaquic Dystrocryepts complex, 15 to 45 percent slopes, metamorphic, mountain slopes, lateral moraines, cryic	221yp	45	2230066	2dvkm	ca740	1996	1:24000
Typic Cryorthents-Rock outcrop-Rubble land complex, 30 to 65 percent slopes, metamorphic, glacially scoured mountain slopes, cryic	215yp	30	2230064	2dvkk	ca740	1996	1:24000
Rubble land-Typic Cryorthents-Rock outcrop-Xeric Dystrocryepts complex, 30 to 80 percent slopes, mountainflanks, metamorphic, mafic, cryic	210yp	162	1674980	hn82	ca750	1983	1:24000
Typic Cryorthents-Rock outcrop complex, 40 to 85 percent slopes	115hs	1556	2370726	2kky1	ca760	1981	1:24000
Typic Cryorthents, warm metamorphic-Rock outcrop, metamorphic-Canisrocks complex, 30 to 100 percent slopes	2230	847	3231106	2w86n	ca760	1981	1:24000
Rock outcrop, granitic crags-Typic Cryorthents complex, 30 to 100 percent slopes	1101	743	3231078	2tbfb	ca760	1981	1:24000
Rock outcrop, granitic-Typic Cryorthents, warm complex, 30 to 90 percent slopes	2130	704	3231080	2twpj	ca760	1981	1:24000
Canisrocks-Typic Cryorthents, warm-Rock outcrop, granitic complex, 30 to 100 percent slopes	2137	512	3231091	2tbf2	ca760	1981	1:24000
Rock outcrop, metamorphic crags-Typic Cryorthents, metamorphic complex, 30 to 90 percent slopes	1201	171	3231079	2tbfc	ca760	1981	1:24000
Rock outcrop, granitic-Typic Cryorthents-Canisrocks, scree complex, 30 to 100 percent slopes	1137	59	3231105	2t8zr	ca760	1981	1:24000
Rock outcrop, metamorphic-Benchlake family-Typic Cryorthents, metamorphic complex, 10 to 120 percent slopes	1215	39	3292033	2w86m	ca760	1981	1:24000
Typic Cryorthents, 30 to 90 percent slopes	1103	34	3231093	2t8z1	ca760	1981	1:24000
Rock outcrop-Typic Cryorthents-Xeric Dystrocryepts complex, 0 to 35 percent slopes, mountain slopes, joints, cryic	267	29722	1542447	1ns1c	ca790	2006	1:24000
Rubble land-Typic Cryorthents-Rock outcrop-Xeric Dystrocryepts complex, 30 to 80 percent slopes, mountainflanks, metamorphic, mafic, cryic	210	13553	466335	hn82	ca790	2006	1:24000
Glacierpoint-Typic Cryorthents complex, 30 to 65 percent slopes, mountain slopes, lateral moraines, aprons, cryic	251	11525	1540354	1npvv	ca790	2006	1:24000
Rock outcrop-Typic Cryorthents-Vitrandic Dystrocryepts complex, 0 to 65 percent slopes, metamorphic, mountain slopes, cryic	270	1786	1542450	1ns1g	ca790	2006	1:24000
Typic Cryorthents-Rock outcrop-Rubble land complex, 30 to 65 percent slopes, metamorphic, glacially scoured mountain slopes, cryic	215	1535	466340	hn87	ca790	2006	1:24000
Typic Cryorthents-Rubble land-Rock outcrop complex, 15 to 40 percent slopes, moraines, cryic	244	1272	1476226	1lk46	ca790	2006	1:24000
Typic Cryorthents-Xeric Dystrocryepts-Oxyaquic Dystrocryepts complex, 15 to 45 percent slopes, metamorphic, mountain slopes, lateral moraines, cryic	221	981	466346	hn8f	ca790	2006	1:24000
Rock outcrop, granitic-Canisrocks-Typic Cryorthents, warm complex, 30 to 100 percent slopes	2138	37672	2777231	2r1c4	ca792	2018	1:24000
Typic Cryorthents, 30 to 90 percent slopes	1103	34469	2777251	2t8z1	ca792	2018	1:24000
Canisrocks-Typic Cryorthents, warm-Rock outcrop, granitic complex, 30 to 100 percent slopes	2137	27624	2777244	2tbf2	ca792	2018	1:24000
Rock outcrop, granitic-Typic Cryorthents-Canisrocks, scree complex, 30 to 100 percent slopes	1137	26076	2924690	2t8zr	ca792	2018	1:24000
Rock outcrop, granitic-Typic Cryorthents, warm complex, 30 to 90 percent slopes	2130	19467	2766855	2twpj	ca792	2018	1:24000
Rock outcrop, granitic crags-Typic Cryorthents complex, 30 to 100 percent slopes	1101	19178	2766852	2tbfb	ca792	2018	1:24000
Typic Cryorthents, warm metamorphic-Rock outcrop, metamorphic-Canisrocks complex, 30 to 100 percent slopes	2230	6854	2924694	2w86n	ca792	2018	1:24000
Rock outcrop, metamorphic-Typic Cryorthents, warm metamorphic-Benchlake, warm complex, 15 to 100 percent slopes	2235	6588	2924633	2w86c	ca792	2018	1:24000
Typic Cryorthents, warm-Rock outcrop, granitic-McGee complex, 5 to 60 percent slopes	2147	5858	2924692	2w86q	ca792	2018	1:24000
Typic Cryorthents, moraine-Glaciers complex, 15 to 90 percent slopes	1011	5090	2777246	2t8yx	ca792	2018	1:24000
Rock outcrop, metamorphic crags-Typic Cryorthents, metamorphic complex, 30 to 90 percent slopes	1201	4961	2766853	2tbfc	ca792	2018	1:24000
Typic Cryorthents, metamorphic, 30 to 90 percent slopes	1203	3751	2924631	2w869	ca792	2018	1:24000
Rock outcrop, metamorphic-Benchlake family-Typic Cryorthents, metamorphic complex, 10 to 120 percent slopes	1215	3401	2924691	2w86m	ca792	2018	1:24000
Rock outcrop, metamorphic-Typic Cryorthents, metamorphic-Benchlake family complex, 10 to 100 percent slopes	1237	2106	2924864	2w870	ca792	2018	1:24000
Typic Cryorthents-Lithic Haplocryolls association, 40 to 80 percent slopes	201S	1188	500946	jt8k	co634		1:24000
Cryorthents-Rubble land complex, 30 to 75 percent slopes	254	6311	507119	k0pp	co672	2003	1:24000
Typic Haplocryepts family, extremely stony surface-Typic Cryorthents family, very bouldery surface-Typic Haplocryalfs family complex, 25 to 70 percent slopes	43B7AR		3402846	31cfl	id701		1:24000
Typic Haplocryepts family, stony surface-Typic Haplocryepts family-Typic Cryorthents family complex, 10 to 55 percent slopes	43B7AS		3402849	31cfp	id701		1:24000
Typic Haplocryepts-Typic Cryorthents families complex, 15 to 60 percent slopes	43B7AM		3402850	31cfq	id701		1:24000
Typic Cryorthents, Furniss, rarely flooded, and Mined land soils, 0 to 12 percent slopes	6099	178	3175633	2z43s	id716		1:24000
Typic Cryorthents, extremely bouldery	46	5571	779464	v530	mt631	1988	1:24000
Typic Cryorthents, reclaimed area-Beeftrail, severely impacted complex, 4 to 30 percent slopes	402E	630	843608	x9v5	mt670	2007	1:24000
Typic Cryorthents, 15 to 50 percent slopes	6010	37	477001	j0c4	nv774	1985	1:24000
Lithic Cryorthents-Mollic Haplocryalfs-Typic Cryorthents complex, 10 to 50 percent slopes	575T	273	157769	595b	wy656	2008	1:24000
Typic Cryochrepts-Typic Cryorthents association, 40 to 70 percent slopes	488T	102	157767	5958	wy656	2008	1:24000
Glacial Trough Sideslopes, Subalpine Fir Complex	5741	17556	151890	531p	wy662	1998	1:24000
Glacial Trough Sideslopes, Forested Scree-Subalpine Fir Complex	5701	4072	151888	531m	wy662	1998	1:24000
Typic Cryorthents-Haycamp family, complex, 40 to 90 percent slopes	366	6273	152021	535x	wy663	2012	1:24000
Hanks family-Como, family, moderately deep-Typic Cryorthents, shallow, complex	8335	170370	3056548	2xttb	wy665	1996	1:62500
Kangas family-Typic Cryorthents-Perfa family, complex	8167	11385	3056551	2xtt8	wy665	1996	1:62500

Map of Series Extent

Approximate geographic distribution of the TYPIC CRYORTHENTS 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).