Soil Data Explorer - CEDARHILL

Official Series Description

Lab Data Summary

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

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

Soil series sharing subgroup-level classification with CEDARHILL, 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 CEDARHILL 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
Cedarhill, high precipitation-Hondoho-Ridgecrest complex, 20 to 50 percent slopes	111	80	82683	2s16	id709	1976	1:24000
Ireland-Cedarhill-Buist complex, 10 to 45 percent slopes, MLRA 13	2200	1808	3238952	2pdcg	id710	1968	1:24000
Buist-Ricrest-Cedarhill complex, 10 to 30 percent slopes	3100	486	3238953	2pt1q	id710	1968	1:24000
Huffman-Ricrest-Cedarhill complex, 10 to 25 percent slopes	RFF	6	3238961	n4cg	id710	1968	1:24000
Cedarhill-Ririe-Watercanyon complex, 30 to 60 percent slopes	30	24209	3163526	2v05z	id711	1983	1:24000
Camelback-Cedarhill, high precipitation-Lanoak complex, 20 to 50 percent slopes	23	12342	3163521	2v063	id711	1983	1:24000
Cedarhill, high precipitation-Hades-Ricrest complex, 20 to 50 percent slopes	33	9963	3163528	2v05x	id711	1983	1:24000
Ririe-Watercanyon-Cedarhill complex, 12 to 30 percent slopes	103	7334	3163558	2szwk	id711	1983	1:24000
Cedarhill-Ireland, extremely stony surface-Rock outcrop complex, 30 to 60 percent slopes	29	6693	3163525	2v060	id711	1983	1:24000
Cedarhill, high precipitation-Hondoho-Ridgecrest, extremely stony surface, complex, 20 to 50 percent slopes	35	5406	3163530	2v06l	id711	1983	1:24000
Cedarhill-Rock outcrop complex, 30 to 60 percent slopes	31	4755	82902	2s88	id711	1983	1:24000
Cedarhill, high precipitation-Camelback-Moonlight complex, 20 to 50 percent slopes	32	4627	3163527	2v05y	id711	1983	1:24000
Cedarhill, high precipitation-Coalbank-Trailcreek complex, 20 to 50 percent slopes	37	4253	3163532	2v05t	id711	1983	1:24000
Cedarhill very cobbly silt loam, 30 to 60 percent slopes	28	2744	3163524	2v061	id711	1983	1:24000
Cedarhill, high precipitation-Hondoho-Arbone complex, 20 to 50 percent slopes	34	2457	3163529	2v05w	id711	1983	1:24000
Coalbank-Lonigan-Trailcreek complex, 20 to 50 percent slopes	40	1424	3163533	2v05s	id711	1983	1:24000
Ireland, extremely stony surface-Hades-Cedarhill complex, 20 to 60 percent slopes	61	1236	3163542	2v05k	id711	1983	1:24000
Cedarhill, high precipitation-Manila complex, 30 to 50 percent slopes	36	1059	3163531	2v05v	id711	1983	1:24000
Cedarhill, high precipitation-Manila complex, 20 to 30 percent slopes	76	655	3163546	2szx0	id711	1983	1:24000
Cedarhill-Ririe-Ricafied complex, 25 to 55 percent slopes	486	357	3173254	2rg0b	id711	1983	1:24000
Cedarhill-Hondoho-Ridgecrest complex, 25 to 55 percent slopes	209	63	3173241	2rfzv	id711	1983	1:24000
Ricafied-Cedarhill complex, 40 to 80 percent slopes	3000	4	3173258	2x01j	id711	1983	1:24000
Cedarhill-Clegg-Drage complex, 5 to 55 percent slopes	47	7293	3163492	2dvl1	id712	2008	1:24000
Dirtyhead-Cedarhill complex, 12 to 45 percent slopes	70	3362	790561	vjmz	id712	2008	1:24000
Cedarhill-Buist complex, 10 to 30 percent slopes	44	2093	642336	pkdj	id712	2008	1:24000
Cedarhill gravelly silt loam, 5 to 25 percent slopes	41	1994	3163491	5bm7	id712	2008	1:24000
Cedarhill-Bearhollow complex, 5 to 20 percent slopes	43	1750	154267	55jc	id712	2008	1:24000
Cedarhill-Pinehollow complex, dry, 5 to 45 percent slopes	48	1454	1586539	1q7xp	id712	2008	1:24000
Cedarhill gravelly silt loam, dry, 10 to 40 percent slopes	42	1073	791546	vknr	id712	2008	1:24000
Cedarhill-Clegg complex, 2 to 20 percent slopes	46	972	1487323	1lxp5	id712	2008	1:24000
Cedarhill-Wursten complex, 5 to 35 percent slopes	49	897	790563	vjn1	id712	2008	1:24000
Cedarhill-Burchert complex, 5 to 50 percent slopes	45	516	632033	p6p5	id712	2008	1:24000
Horrocks-Cedarhill complex, 12 to 50 percent slopes	102	341	1487324	1lxp6	id712	2008	1:24000
Cedarhill, high precipitation-Hades-Ricrest complex, 20 to 50 percent slopes	33-B	65	3173265	2v05x	id712	2008	1:24000
Cedarhill-Ireland, extremely stony surface-Rock outcrop complex, 30 to 60 percent slopes	29-B	57	3173264	2v060	id712	2008	1:24000
Geemore family-Cedarhill-Laschance complex, 30 to 65 percent slopes	2022	52	3173314	2x01g	id712	2008	1:24000
Cedarhill-Ririe-Ricafied complex, 25 to 55 percent slopes	486	5637	2619902	2rg0b	id713		1:24000
Cedarhill, high precipitation-Hades-Ricrest complex, 20 to 50 percent slopes	33	3366	2514578	2v05x	id713		1:24000
Ricafied-Cedarhill complex, 40 to 80 percent slopes	3000	3148	2980885	2x01j	id713		1:24000
Geemore family-Cedarhill-Laschance complex, 30 to 65 percent slopes	2022	1320	2980883	2x01g	id713		1:24000
Cedarhill-Ricafied-Dranburn complex, 15 to 55 percent slopes	2440	1158	2917054	2pt1f	id713		1:24000
Camelback-Cedarhill, high precipitation-Lanoak complex, 20 to 50 percent slopes	23	882	2514572	2v063	id713		1:24000
Cedarhill-Ireland, extremely stony surface-Rock outcrop complex, 30 to 60 percent slopes	29	826	2514576	2v060	id713		1:24000
Cedarhill-Ririe-Watercanyon complex, 30 to 60 percent slopes	30	578	2514600	2v05z	id713		1:24000
Cedarhill-Hondoho-Ridgecrest complex, 25 to 55 percent slopes	209	483	2619859	2rfzv	id713		1:24000
Arbone-Hondoho-Cedarhill complex, 12 to 30 percent slopes	6	325	2619849	2v06p	id713		1:24000
Ireland, extremely stony surface-Hades-Cedarhill complex, 20 to 60 percent slopes	61	265	2619898	2v05k	id713		1:24000
Ririe-Watercanyon-Cedarhill complex, 12 to 30 percent slopes	103	236	2520211	2szwk	id713		1:24000
Cedarhill, high precipitation-Camelback-Moonlight complex, 20 to 50 percent slopes	32	190	2514577	2v05y	id713		1:24000
Cedarhill, high precipitation-Hondoho-Arbone complex, 20 to 50 percent slopes	34	188	2514579	2v05w	id713		1:24000
Arbone-Hondoho-Cedarhill complex, 4 to 12 percent slopes	5	182	2619848	2v06n	id713		1:24000
Cedarhill-Hondoho-Ridgecrest complex, 20 to 60 percent slopes	BHG	166	2965723	n4b8	id713		1:24000
Cedarhill gravelly silt loam, 15 to 40 percent slopes, very stony surface	170JJ	164	2520245	20fvh	id713		1:24000
Cedarhill, high precipitation-Hondoho-Ridgecrest, extremely stony surface, complex, 20 to 50 percent slopes	35	146	2520215	2v06l	id713		1:24000
Cedarhill, high precipitation-Manila complex, 30 to 50 percent slopes	36-B	145	2619916	2v05v	id713		1:24000
Cedarhill-Clegg-Drage complex, 5 to 55 percent slopes	47-BL	76	2965718	2dvl1	id713		1:24000
Cedarhill, high precipitation-Coalbank-Trailcreek complex, 20 to 50 percent slopes	37	65	2619857	2v05t	id713		1:24000
Coalbank-Lonigan-Trailcreek complex, 20 to 50 percent slopes	40	52	2619917	2v05s	id713		1:24000
Cedarhill, high precipitation-Manila complex, 20 to 30 percent slopes	76-B	21	2619899	2szx0	id713		1:24000
Cedarhill very cobbly silt loam, 30 to 60 percent slopes	28	13	2514575	2v061	id713		1:24000
Cedarhill gravelly silt loam, 5 to 25 percent slopes	41-BL	1	3093902	5bm7	id713		1:24000
Cedarhill very gravelly silt loam, 12 to 20 percent slopes	34	1501	485278	j8z4	id714	1997	1:24000
Cedarhill-Hondoho, stony surface-Ridgecrest, extremely stony surface complex, 20 to 50 percent slopes	36	514	485280	j8z6	id714	1997	1:24000
Ricafied-Cedarhill complex, 40 to 80 percent slopes	3000	514	3173353	2x01j	id714	1997	1:24000
Cedarhill-Hades-Ricrest complex, 20 to 50 percent slopes	35	47	485279	j8z5	id714	1997	1:24000
Ireland, extremely stony surface-Hades-Cedarhill complex, 20 to 60 percent slopes	61-B	26	3173322	2v05k	id714	1997	1:24000
Cedarhill-Ricafied-Dranburn complex, 15 to 55 percent slopes	2440	9	3173333	2pt1f	id714	1997	1:24000
Arbone-Hondoho-Cedarhill complex, 12 to 30 percent slopes	6	17809	3163587	2v06p	id715	1994	1:24000
Arbone-Hondoho-Cedarhill complex, 4 to 12 percent slopes	5	15698	3163586	2v06n	id715	1994	1:24000
Cedarhill gravelly silt loam, 4 to 12 percent slopes	18	1507	485609	j99t	id715	1994	1:24000
Ririe-Cedarhill complex, 4 to 12 percent slopes	111	1262	485579	j98v	id715	1994	1:24000
Cedarhill-Lostine complex, 12 to 30 percent slopes	21	1222	485613	j99y	id715	1994	1:24000
Cedarhill-Hymas association, 20 to 55 percent slopes	20	1163	485612	j99x	id715	1994	1:24000
Cedarhill gravelly silt loam, 12 to 30 percent slopes	19	1139	485610	j99v	id715	1994	1:24000
Ririe-Cedarhill complex, 12 to 20 percent slopes	112	1082	485580	j98w	id715	1994	1:24000
Ricafied-Cedarhill complex, 40 to 80 percent slopes	3000	269	3173381	2x01j	id715	1994	1:24000
Cedarhill, high precipitation-Hades-Ricrest complex, 20 to 50 percent slopes	33-B	74	3173359	2v05x	id715	1994	1:24000
Cedarhill-Ireland, extremely stony surface-Rock outcrop complex, 30 to 60 percent slopes	29-B	20	3173358	2v060	id715	1994	1:24000
Ireland-Cedarhill-Buist complex, 10 to 45 percent slopes, MLRA 13	2200	18963	2484540	2pdcg	id716		1:24000
Ricafied-Ireland-Cedarhill complex, 20 to 50 percent slopes	2530	10867	2495468	2pt1l	id716		1:24000
Buist-Ricrest-Cedarhill complex, 10 to 30 percent slopes	3100	7751	2495472	2pt1q	id716		1:24000
Cedarhill-Ricrest complex, 15 to 45 percent slopes	3150	6583	2495473	2pt1r	id716		1:24000
Cedarhill-Ricafied-Dranburn complex, 15 to 55 percent slopes	2440	3365	2495462	2pt1f	id716		1:24000
Cedarhill, extremely stony surfface-Rubble land-Kackley, extremely stony surface, complex, 5 to 30 percent slopes	145A	2981	599838	n45m	id716		1:24000
Ricrest-Cedarhill complex, 10 to 50 percent slopes	7065	2842	3074039	2xxdn	id716		1:24000
Dranburn-Calpac-Cedarhill complex, 15 to 50 percent slopes	3250	1945	2495475	2pt1t	id716		1:24000
Cedarhill-Clegg-Drage complex, 5 to 55 percent slopes	47	1570	2230079	2dvl1	id716		1:24000
Ireland-Cedarhill-Buist complex, 20 to 70 percent slopes, MLRA 43B	7200	1101	3136434	2ypjs	id716		1:24000
Cedarhill-Hondoho-Ridgecrest complex, 20 to 60 percent slopes	BHG	975	599982	n4b8	id716		1:24000
Cedarhill gravelly silt loam, 15 to 40 percent slopes, very stony surface	170JJ	777	1860356	20fvh	id716		1:24000
Huffman-Ricrest-Cedarhill complex, 10 to 25 percent slopes	RFF	576	600019	n4cg	id716		1:24000
Cedarhill gravelly silt loam, 5 to 25 percent slopes	170H	575	159161	5bm7	id716		1:24000
Vicking-Cedarhill complex, 10 to 35 percent slopes	KCG	570	600002	n4bx	id716		1:24000
Cedarhill-Clegg complex, 2 to 20 percent slopes	170KK	569	2230098	2dvln	id716		1:24000
Hades-Camelback, very deep-Cedarhill complex, 10 to 55 percent slopes	2210	442	2484543	2pdck	id716		1:24000
Cedarhill-Chausse-Jebo complex, 10 to 40 percent slopes	CT	420	599990	n4bj	id716		1:24000
Cedarhill-Bearhollow complex, 5 to 35 percent slopes	170G	337	159160	5bm6	id716		1:24000
Cedarhill-Wursten complex, 12 to 30 percent slopes	170DD	268	1859995	20fgv	id716		1:24000
Cedarhill, high precipitation-Camelback, deep-Moonlight complex, 20 to 50 percent slopes	BBF	224	599978	n4b4	id716		1:24000
Camelback-Cedarhill, high precipitation-Lanoak complex, 20 to 50 percent slopes	23	53	3136435	2v063	id716		1:24000
Horrocks-Cedarhill complex, 12 to 50 percent slopes	118AA	14	2230097	2dvlm	id716		1:24000
Ireland-Cedarhill-Buist complex, 10 to 45 percent slopes, MLRA 13	2200	477	3238990	2pdcg	id770	1968	1:24000
Cedarhill-Clegg-Drage complex, 5 to 55 percent slopes	47	16	2396249	2lfhc	ut604	1980	1:24000

Map of Series Extent

Approximate geographic distribution of the CEDARHILL 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).