Soil Data Explorer - MANILA

Official Series Description

Lab Data Summary

Aggregate lab data for the MANILA soil series. This aggregation is based on all pedons with a current taxon name of MANILA, 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 MANILA 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
25	78P0425	78ID031007	Manila	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.0522232,-113.7783356
25	78P0426	78ID031008	Manila	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.1199989,-113.7719421

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MANILA 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 MANILA 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 MANILA 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 MANILA 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 MANILA 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 MANILA 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 MANILA 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 flats position figure.

Soil series sharing subgroup-level classification with MANILA, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. ID-2010-08-30-03 | Franklin County Area - 2008

   Typical pattern of soils and underlying material in general soil map units 1 (Lando-Battle-Creek-Trenton) and 10 (Manilla-Lanoak-Broadhead) (Soil Survey of Franklin County Area, Idaho; 2008).

2. ID-2010-08-30-08 | Franklin County Area - 2008

   Typical pattern of soils and underlying material in general soil map units 8 (Yeates Hollow-Vitale-Northwater) and 9 (Yeates Hollow-Manila-Softback) (Soil Survey of Franklin County Area, Idaho; 2008).

3. ID-2010-08-30-09 | Franklin County Area - 2008

   Typical pattern of soils and underlying material in general soil map unit 11 (Wormcreek-Lonigan-Manila) (Soil Survey of Franklin County Area, Idaho; 2008).

Map Units

Map units containing MANILA 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
Manila-Merlin-Mascamp families association, 10 to 35 percent slopes.	212	6871	470527	hsm9	ca703	1983	1:24000
Manila-Merlin-Mascamp families association, 35 to 60 percent slopes.	213	4350	470528	hsmb	ca703	1983	1:24000
Aninto-Manila complex, 8 to 20 percent slopes	5	4725	82522	2rw0	id708	1987	1:24000
Manila-Hades complex, 8 to 20 percent slopes	96	1109	82573	2rxn	id708	1987	1:24000
Manila-Dranyon association, hilly	34	1552	82609	2ryt	id709	1976	1:24000
Yago, very bouldery surface-Manila, extremely stony surface, complex, 10 to 35 percent slopes, MLRA 13	308	91	3163622	2pwvl	id709	1976	1:24000
Manila-Bancroft complex, 6 to 15 percent slopes	75	2253	82950	2s9t	id711	1983	1:24000
Bancroft-Manila complex, 15 to 30 percent slopes	11	1789	82862	2s6z	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
Manila-Lonigan complex, 6 to 40 percent slopes	76-O	485	3173263	2v073	id711	1983	1:24000
Copenhagen-Lonigan-Manila association, 12 to 50 percent slopes	24-O	273	3173261	2v06s	id711	1983	1:24000
Manila-Tahquats family-Faim complex, 12 to 25 percent slopes	462	245	3173250	2rg02	id711	1983	1:24000
Yago, very bouldery surface-Manila, extremely stony surface, complex, 10 to 35 percent slopes, MLRA 13	308	90	3173244	2pwvl	id711	1983	1:24000
Yago, very stony surface-Manila-Faim complex, 20 to 50 percent slopes	549	13	3173256	2rg07	id711	1983	1:24000
Manila-Broadhead complex, 12 to 30 percent slopes, MLRA 47	7547	236	3173320	2x027	id712	2008	1:24000
Yago, very bouldery surface-Manila, extremely stony surface, complex, 20 to 45 percent slopes, MLRA 43B	30843	54	3173315	2x01x	id712	2008	1:24000
Yeates Hollow, extremely stony surface-Manila-Softback complex, 12 to 40 percent slopes	162	6642	2917058	2sltq	id713		1:24000
Yago, very stony surface-Manila-Faim complex, 20 to 50 percent slopes	549	4139	2619875	2rg07	id713		1:24000
Manila-Tahquats family-Faim complex, 12 to 25 percent slopes	462	2837	2619870	2rg02	id713		1:24000
Manila-Broadhead complex, 12 to 30 percent slopes, MLRA 13	75	2799	2619851	2v072	id713		1:24000
Copenhagen-Lonigan-Manila association, 12 to 50 percent slopes	24	2705	2619844	2v06s	id713		1:24000
Manila-Lonigan complex, 6 to 40 percent slopes	76	2068	2619882	2v073	id713		1:24000
Manila-Broadhead complex, 12 to 30 percent slopes, MLRA 47	7547	1809	2980914	2x027	id713		1:24000
Yeates Hollow family, extremely stony surface-Manila family, very stony surface, perched water table-Booneville complex, 5 to 35 percent slopes	1088	948	2980916	2x029	id713		1:24000
Yago, very bouldery surface-Manila, extremely stony surface, complex, 10 to 35 percent slopes, MLRA 13	308	724	2497414	2pwvl	id713		1:24000
Yago-Manila-Hades complex, 20 to 40 percent slopes	133	447	2619842	2v07n	id713		1:24000
Manila-Broadhead complex, 4 to 12 percent slopes	74	284	2619850	2v071	id713		1:24000
Yago, very bouldery surface-Manila, extremely stony surface, complex, 20 to 45 percent slopes, MLRA 43B	30843	236	2980904	2x01x	id713		1:24000
Cedarhill, high precipitation-Manila complex, 30 to 50 percent slopes	36-B	145	2619916	2v05v	id713		1:24000
Manila-Obnot complex, 4 to 12 percent slopes	77	112	2619907	2v074	id713		1:24000
Cedarhill, high precipitation-Manila complex, 20 to 30 percent slopes	76-B	21	2619899	2szx0	id713		1:24000
Manila silt loam, 4 to 12 percent slopes	88-F	17	2619896	2v07x	id713		1:24000
Yeates Hollow, extremely stony surface-Manila-Softback complex, 12 to 40 percent slopes	162	22297	3163582	2sltq	id714	1997	1:24000
Manila-Broadhead complex, 12 to 30 percent slopes	92	9303	485343	j917	id714	1997	1:24000
Manila-Broadhead complex, 4 to 12 percent slopes	91	6365	485341	j915	id714	1997	1:24000
Manila-Yeates Hollow complex, 6 to 20 percent slopes	94	1862	485345	j919	id714	1997	1:24000
Copenhagen-Lonigan-Manila association, 12 to 50 percent slopes	40	1789	485285	j8zc	id714	1997	1:24000
Manila silt loam, 12 to 30 percent slopes	89	1336	485338	j912	id714	1997	1:24000
Manila silt loam, 4 to 12 percent slopes	88	714	3163573	2v07x	id714	1997	1:24000
Manila-Lonigan complex, 6 to 40 percent slopes	93	555	485344	j918	id714	1997	1:24000
Manila silt loam, 0 to 4 percent slopes	87	386	485336	j910	id714	1997	1:24000
Manila-Lonigan complex, 6 to 40 percent slopes	76-O	171	3173329	2v073	id714	1997	1:24000
Yago, very stony surface-Manila-Faim complex, 20 to 50 percent slopes	549	87	3173348	2rg07	id714	1997	1:24000
Manila-Broadhead complex, 4 to 12 percent slopes	74-O	72	3173328	2v071	id714	1997	1:24000
Manila-Bancroft complex, 6 to 15 percent slopes	90	25	485340	j914	id714	1997	1:24000
Yeates Hollow family, extremely stony surface-Manila family, very stony surface, perched water table-Booneville complex, 5 to 35 percent slopes	1088	8	3173403	2x029	id714	1997	1:24000
Copenhagen-Lonigan-Manila association, 12 to 50 percent slopes	24	9871	3163589	2v06s	id715	1994	1:24000
Manila-Broadhead complex, 12 to 30 percent slopes, MLRA 13	75	8091	3163598	2v072	id715	1994	1:24000
Manila-Broadhead complex, 4 to 12 percent slopes	74	7361	3163597	2v071	id715	1994	1:24000
Yago-Manila-Hades complex, 20 to 40 percent slopes	133	6150	3163617	2v07n	id715	1994	1:24000
Manila-Yago complex, 4 to 12 percent slopes	78	3395	485675	j9cy	id715	1994	1:24000
Manila-Lonigan complex, 6 to 40 percent slopes	76	3008	3163599	2v073	id715	1994	1:24000
Manila-Obnot complex, 4 to 12 percent slopes	77	1860	3163600	2v074	id715	1994	1:24000
Manila-Yago complex, 12 to 30 percent slopes	79	1770	485676	j9cz	id715	1994	1:24000
Manila silt loam, 4 to 12 percent slopes	73	374	485670	j9cs	id715	1994	1:24000
Manila-Tahquats family-Faim complex, 12 to 25 percent slopes	462	226	3173374	2rg02	id715	1994	1:24000
Yago, very stony surface-Manila-Faim complex, 20 to 50 percent slopes	549	65	3173379	2rg07	id715	1994	1:24000
Hades-Manila-Taylow complex, 4 to 30 percent slopes	6095	836	3074033	2xxdg	id716		1:24000
Yeates Hollow, extremely stony surface-Manila-Softback complex, 12 to 40 percent slopes	162	233	2984401	2sltq	id716		1:24000
Curtis Creek, very stony-Senchert-Manila, extremely stony complex, 10 to 50 percent slopes	QuR	7858	2503728	2pw04	ut013		1:24000
Manila-Yeates Hollow complex, 4 to 40 percent slopes, very stony	TVD	1014	1484057	1lt8t	ut013		1:24000
Manila-Clegg association, 2 to 20 percent slopes	UVB	775	749221	t4mf	ut013		1:24000
Broad-Manila association, steep	BTG	7555	481328	j4vq	ut602	1969	1:20000
Manila loam, 10 to 25 percent slopes	MbE	2538	481423	j4ys	ut602	1969	1:20000
Manila-Smarts association, steep	MDG	2091	481415	j4yj	ut602	1969	1:20000
Manila loam, 25 to 60 percent slopes	MCG	791	481414	j4yh	ut602	1969	1:20000
Manila loam, 6 to 10 percent slopes	MbC	686	481422	j4yr	ut602	1969	1:20000
Manila loam, 4 to 8 percent slopes	MeC	1585	482551	j645	ut608	1981	1:24000
Manila loam, 8 to 15 percent slopes	MeD	1305	482552	j646	ut608	1981	1:24000
Manila loam, 25 to 40 percent slopes	MbE	6775	506583	k04d	ut609	1974	1:24000
Manila loam, 10 to 25 percent slopes	MbD	3510	506582	k04c	ut609	1974	1:24000
Manila loam, 6 to 10 percent slopes	MbC	2295	506581	k04b	ut609	1974	1:24000
Manila-Yeates Hollow complex, 10 to 25 percent slopes	McD	1875	506584	k04f	ut609	1974	1:24000
Manila-Yeates Hollow complex, 25 to 70 percent slopes	McG	1520	506585	k04g	ut609	1974	1:24000
Manila loam, 3 to 6 percent slopes	MbB	760	506580	k049	ut609	1974	1:24000
Manila loam, 0 to 3 percent slopes	MbA	540	506579	k048	ut609	1974	1:24000
Manila-Harter complex, 2 to 8 percent slopes	156	4022	508201	k1tl	ut613	1999	1:24000
Manila-Ant Flat loams, 2 to 8 percent slopes	154	3995	508200	k1tk	ut613	1999	1:24000
Manila-Henefer complex, 8 to 15 percent slopes	157	1909	508198	k1th	ut613	1999	1:24000
Manila-Ant Flat loams, 8 to 15 percent slopes	155	1789	508199	k1tj	ut613	1999	1:24000
Manila silt loam, 10 to 30 percent slopes	MAF	1293	483333	j6yd	ut621	1966	1:20000
Manila silt loam, 10 to 20 percent slopes	MaD	513	504284	jxr7	ut622	1967	1:24000
Manila silt loam, 3 to 6 percent slopes	MaB	485	504282	jxr5	ut622	1967	1:24000
Manila silt loam, 6 to 10 percent slopes	MaC	394	504283	jxr6	ut622	1967	1:24000
Manila loam, 3 to 10 percent slopes	MbC	5085	482295	j5vx	ut627	1971	1:24000

Map of Series Extent

Approximate geographic distribution of the MANILA 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).