Soil Data Explorer - CANISROCKS

Official Series Description

Lab Data Summary

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

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
22A	97P0129	790035	Canisrocks	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.8588125,-119.6193109

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CANISROCKS 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 CANISROCKS 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 CANISROCKS 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 CANISROCKS 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.

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

Competing Series

Soil series competing with CANISROCKS 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 CANISROCKS 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 CANISROCKS 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 hills 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 CANISROCKS, 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 CANISROCKS 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
Rock outcrop-Canisrocks complex, 30 to 70 percent slopes, mountain slopes, cryic	249yp	415	1670113	1lxty	ca731	1981	1:24000
Canisrocks-Rock outcrop-Glacierpoint complex, 30 to 70 percent slopes, mountain slopes, cryic	248yp	396	1670112	1lxpr	ca731	1981	1:24000
Rock outcrop-Canisrocks-Glacierpoint complex, 30 to 80 percent slopes, mountain slopes, joints, cryic	268yp	229	1670126	1ns1b	ca731	1981	1:24000
Rock outcrop-Canisrocks-Xeric Dystrocryepts complex, 5 to 45 percent slopes, moraines, mountain slopes, cryic	252yp	224	1670114	1nqdy	ca731	1981	1:24000
Canisrocks-Rock outcrop-Rubble land complex, 30 to 80 percent slopes, mountainflanks, cryic	235yp	122	1670110	1lwrp	ca731	1981	1:24000
Rock outcrop-Canisrocks-Xeric Dystrocryepts complex, 0 to 35 percent slopes, mountain slopes, cryic	242yp	122	1670111	1ljwf	ca731	1981	1:24000
Siberian, dry-Canisrocks, dry complex, 15 to 60 percent slopes	2140	5080	3422874	2w86k	ca732	1998	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-Rubble land-Canisrocks association, 0 to 80 percent slopes, cirqued mountainflanks, cryic	219yp	4065	2229326	2dtsr	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
Rock outcrop-Canisrocks-Xeric Dystrocryepts complex, 0 to 35 percent slopes, mountain slopes, cryic	242yp	75	2229330	2dtsw	ca732	1998	1:24000
Xeric Dystrocryepts-Canisrocks-Oxyaquic Dystrocryepts association, 10 to 40 percent slopes, aprons, lateral moraines, cryic	211yp	36	2229325	2dtsq	ca732	1998	1:24000
Rock outcrop, granitic-Typic Cryorthents-Canisrocks, scree complex, 30 to 100 percent slopes	1137	3894	3231058	2t8zr	ca740	1996	1:24000
Rock outcrop-Rubble land-Canisrocks association, 0 to 80 percent slopes, cirqued mountainflanks, cryic	219yp	3212	2230065	2dvkl	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
Siberian, dry-Canisrocks, dry complex, 15 to 60 percent slopes	2140	1100	3422932	2w86k	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
Typic Cryorthents, warm metamorphic-Rock outcrop, metamorphic-Canisrocks complex, 30 to 100 percent slopes	2230	355	3231059	2w86n	ca740	1996	1:24000
Rock outcrop-Rubble land-Canisrocks association, 10 to 65 percent slopes, mountain slopes, cryic	223yp	116	2230068	2dvkp	ca740	1996	1:24000
Canisrocks-Rubble land-Rock outcrop-Crazymule complex, 30 to 75 percent slopes, mountainflanks, colluvial aprons, cryic	222yp	61	2230067	2dvkn	ca740	1996	1:24000
Rock outcrop-Rubble land-Canisrocks association, 0 to 80 percent slopes, cirqued mountainflanks, cryic	219yp	2906	1674981	hn8c	ca750	1983	1:24000
Canisrocks-Xeric Dystrocryepts association, 5 to 30 percent slopes, mountain valleys, moraines, cryic	247yp	1806	1674983	1lxpl	ca750	1983	1:24000
Canisrocks-Glacierpoint-Humic Dystrocryepts complex, 15 to 55 percent slopes, lateral moraines, cryic	253yp	1211	1674985	1nqf7	ca750	1983	1:24000
Canisrocks-Rock outcrop-Glacierpoint complex, 30 to 70 percent slopes, mountain slopes, cryic	248yp	599	1674984	1lxpr	ca750	1983	1:24000
Canisrocks-Rock outcrop-Rubble land-Vitrandic Dystrocryepts association, 2 to 30 percent slopes, glacially scoured mountain valleys, cryic	225yp	269	1674982	hn8k	ca750	1983	1:24000
Siberian, dry-Canisrocks, dry complex, 15 to 60 percent slopes	2140	1431	3231104	2w86k	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
Canisrocks-Typic Cryorthents, warm-Rock outcrop, granitic complex, 30 to 100 percent slopes	2137	512	3231091	2tbf2	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-Canisrocks complex, 30 to 70 percent slopes, mountain slopes, cryic	249	43070	1487471	1lxty	ca790	2006	1:24000
Rock outcrop-Canisrocks-Xeric Dystrocryepts complex, 0 to 35 percent slopes, mountain slopes, cryic	242	38187	1475985	1ljwf	ca790	2006	1:24000
Rock outcrop-Rubble land-Canisrocks association, 0 to 80 percent slopes, cirqued mountainflanks, cryic	219	34176	466344	hn8c	ca790	2006	1:24000
Rock outcrop-Canisrocks-Xeric Dystrocryepts complex, 5 to 45 percent slopes, moraines, mountain slopes, cryic	252	32810	1540884	1nqdy	ca790	2006	1:24000
Canisrocks-Rock outcrop-Rubble land complex, 30 to 80 percent slopes, mountainflanks, cryic	235	31553	1486440	1lwrp	ca790	2006	1:24000
Rock outcrop-Canisrocks-Glacierpoint complex, 30 to 80 percent slopes, mountain slopes, joints, cryic	268	28419	1542446	1ns1b	ca790	2006	1:24000
Canisrocks-Rock outcrop-Glacierpoint complex, 30 to 70 percent slopes, mountain slopes, cryic	248	27386	1487341	1lxpr	ca790	2006	1:24000
Canisrocks-Rock outcrop-Rubble land-Vitrandic Dystrocryepts association, 2 to 30 percent slopes, glacially scoured mountain valleys, cryic	225	19118	466350	hn8k	ca790	2006	1:24000
Canisrocks-Xeric Dystrocryepts association, 5 to 30 percent slopes, mountain valleys, moraines, cryic	247	16712	1487336	1lxpl	ca790	2006	1:24000
Canisrocks-Glacierpoint-Humic Dystrocryepts complex, 15 to 55 percent slopes, lateral moraines, cryic	253	16133	1540893	1nqf7	ca790	2006	1:24000
Canisrocks-Xeric Dystrocryepts complex, 15 to 45 percent slopes, mountain slopes, moraines, cryic	279	15413	1542320	1nrx8	ca790	2006	1:24000
Canisrocks-Rock outcrop-Glacierpoint complex, 0 to 35 percent slopes, mountain slopes, moraines, joints, cryic	269	14457	1542308	1nrww	ca790	2006	1:24000
Canisrocks-Crazymule complex, 15 to 45 percent slopes, mountain slopes, lateral moraines, cryic	227	11559	466352	hn8m	ca790	2006	1:24000
Canisrocks-Glacierpoint complex, 0 to 25 percent slopes, lateral moraines, cryic	232	11311	466357	hn8s	ca790	2006	1:24000
Canisrocks-Rubble land-Rock outcrop-Crazymule complex, 30 to 75 percent slopes, mountainflanks, colluvial aprons, cryic	222	10030	466347	hn8g	ca790	2006	1:24000
Rock outcrop-Canisrocks-Xeric Dystrocryepts association, 0 to 35 percent slopes, mountain valleys, scoured, filled, cryic	245	9953	1476716	1lkn0	ca790	2006	1:24000
Canisrocks-Glacierpoint-Vitrandic Cryorthents complex, bouldery, 5 to 20 percent slopes, ground moraines, cryic	237	6704	1486461	1lwsc	ca790	2006	1:24000
Crazymule-Canisrocks complex, 0 to 20 percent slopes, ground moraines, cryic	239	6215	1487331	1lxpf	ca790	2006	1:24000
Canisrocks-Glacierpoint-Vitrandic Dystrocryepts complex, bouldery, 20 to 45 percent slopes, medial moraines, cryic	213	6143	466338	hn85	ca790	2006	1:24000
Rock outcrop-Rubble land-Canisrocks association, 10 to 65 percent slopes, mountain slopes, cryic	223	5840	466348	hn8h	ca790	2006	1:24000
Canisrocks, 5 to 35 percent slopes, mountain valleys, cryic	241	3311	1475655	1ljjs	ca790	2006	1:24000
Crazymule-Canisrocks association, 0 to 20 percent slopes, lateral moraines, wet/dry meadows, cryic	264	2639	1542443	1ns17	ca790	2006	1:24000
Oxyaquic Cryorthents-Canisrocks complex, 0 to 15 percent slopes, ground moraines, wet/dry, cryic	238	1755	1487078	1lxf8	ca790	2006	1:24000
Xeric Dystrocryepts-Canisrocks-Oxyaquic Dystrocryepts association, 10 to 40 percent slopes, aprons, lateral moraines, cryic	211	1587	466336	hn83	ca790	2006	1:24000
Canisrocks-Xeric Dystrocryepts association, 5 to 40 percent slopes, mountain valleys, moraines, avalanches, cryic	250	1013	1539918	1npds	ca790	2006	1:24000
Canisrocks-Typic Cryaquents complex, 5 to 30 percent slopes, lateral moraines, aprons, wet/dry, cryic	231	460	466356	hn8r	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
Canisrocks-Typic Cryorthents, warm-Rock outcrop, granitic complex, 30 to 100 percent slopes	2137	27624	2777244	2tbf2	ca792	2018	1:24000
Siberian, dry-Canisrocks, dry complex, 15 to 60 percent slopes	2140	27606	2924687	2w86k	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
Typic Cryorthents, warm metamorphic-Rock outcrop, metamorphic-Canisrocks complex, 30 to 100 percent slopes	2230	6854	2924694	2w86n	ca792	2018	1:24000

Map of Series Extent

Approximate geographic distribution of the CANISROCKS 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).