Soil Data Explorer - MONTALTO

Official Series Description

Lab Data Summary

Aggregate lab data for the MONTALTO soil series. This aggregation is based on all pedons with a current taxon name of MONTALTO, 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 MONTALTO were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
148	87P0186	86MD510004	Montalto	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.3444722,-76.7082611
148	40A0370	S1955PA071007	Montalto	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.1702919,-76.6238251
148	40A0371	S1955PA071010	Montalto	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.1705704,-76.6418762
148	07N0750	S2007MD015002	Montalto	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7154732,-76.1182251

Water Balance

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

Competing Series

Soil series competing with MONTALTO 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 MONTALTO 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 MONTALTO 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 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 MONTALTO, 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. MD-2010-09-03-02 | City of Baltimore - 1998

   Pattern of soils in the Urban land-Legore association (Soil Survey of City of Baltimore, Maryland; 1998).

2. MD-2010-09-10-04 | Cecil County -

   Neshaminy-Montalto-Chrome-Watchung association (Soil Survey of Cecil County, Maryland).

3. MD-2012-02-03-03 | City of Baltimore - 1998

   Pattern of soils in the Urban land-Legore association (Soil Survey of City of Baltimore, Maryland; 1998).

Map Units

Map units containing MONTALTO 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
Talleyville-Montalto-Urban land complex, 0 to 8 percent slopes	TdB	8309	2479901	2p7jt	de003	2009	1:24000
Neshaminy-Montalto silt loams, 25 to 45 percent slopes, very stony	NvE	721	2479877	2p7j1	de003	2009	1:24000
Neshaminy-Montalto silt loams, 15 to 25 percent slopes, very stony	NvD	427	2479876	2p7j0	de003	2009	1:24000
Neshaminy-Montalto silt loams, 8 to 15 percent slopes, very stony	NvC	271	2479875	2p7hz	de003	2009	1:24000
Montalto silt loam, 8 to 15 percent slopes	MxC	213	2479874	2p7hy	de003	2009	1:24000
Montalto silt loam, 3 to 8 percent slopes	MxB	167	2479873	2p7hx	de003	2009	1:24000
Legore-Montalto-Urban land complex, 0 to 8 percent slopes	LgB	5027	2404953	2lqk4	md005	2010	1:12000
Legore-Montalto-Urban land complex, 8 to 15 percent	LgC	1233	2481180	2p8w2	md005	2010	1:12000
Montalto silt loam, 3 to 8 percent slopes	MoB	954	2403987	2lpjz	md005	2010	1:12000
Montalto silt loam, 8 to 15 percent slopes	MoC	243	2403989	2lpk1	md005	2010	1:12000
Montalto silt loam, 3 to 8 percent slopes	MxB	1305	2440734	2mxsc	md015	2009	1:12000
Montalto silt loam, 8 to 15 percent slopes	MxC	1218	2440735	2mxsd	md015	2009	1:12000
Montalto silty clay loam, 15 to 25 percent slopes	MyD	504	2440737	2mxsg	md015	2009	1:12000
Neshaminy-Montalto silt loams, 15 to 25 percent slopes, very stony	NvD	214	2440739	2mxsj	md015	2009	1:12000
Montalto silt loam, 0 to 3 percent slopes	MxA	144	2440733	2mxsb	md015	2009	1:12000
Montalto silty clay loam, 8 to 15 percent slopes	MyC	125	2440736	2mxsf	md015	2009	1:12000
Neshaminy-Montalto silt loams, 25 to 45 percent slopes, very stony	NvE	114	2440740	2mxsk	md015	2009	1:12000
Neshaminy-Montalto silt loams, 8 to 15 percent slopes, very stony	NvC	36	2440738	2mxsh	md015	2009	1:12000
Legore-Montalto gravelly silt loams, 3 to 8 percent slopes, bouldery	LnB	918	535016	kyql	md021	2001	1:12000
Legore-Montalto gravelly silt loams, 15 to 25 percent slopes, bouldery	LnD	644	535018	kyqn	md021	2001	1:12000
Legore-Montalto-Urban land complex, 0 to 8 percent slopes	LoB	1882	793428	vmmg	md027	2004	1:12000
Legore-Montalto silt loams, 3 to 8 percent slopes	LmB	860	793427	vmmf	md027	2004	1:12000
Legore-Montalto-Urban land complex, 8 to 15 percent slopes	LoC	400	793429	vmmh	md027	2004	1:12000
Montalto silt loam, 8 to 15 percent slopes, very stony	24C	441	533609	kx86	md031	1989	1:15840
Montalto silt loam 15 to 25 percent slopes, very stony	24D	149	533610	kx87	md031	1989	1:15840
Montalto silt loam, 3 to 8 percent slopes	26B	147	533613	kx8b	md031	1989	1:15840
Montalto silt loam, 8 to 15 percent slopes	26C	39	533614	kx8c	md031	1989	1:15840
Montalto-Urban land complex, 0 to 8 percent slopes	26UB	1243	533925	kxld	md510	1993	1:12000
Montalto silt loam, 0 to 8 percent slopes	26B	226	533923	kxlb	md510	1993	1:12000
Montalto-Urban land complex, 8 to 15 percent slopes	26UC	127	533926	kxlf	md510	1993	1:12000
Urban land-Montalto complex, 0 to 8 percent slopes	27UB	67	533927	kxlg	md510	1993	1:12000
Montalto silt loam, 8 to 15 percent slopes, very stony	26C	57	533924	kxlc	md510	1993	1:12000
Montalto silt loam, 3 to 8 percent slopes, moderately eroded	MsB2	6545	533438	kx2p	md600	1972	1:15840
Neshaminy and Montalto very stony silt loams 0 to 15 percent slopes	NsC	5201	533443	kx2v	md600	1972	1:15840
Montalto silt loam, 8 to 15 percent slopes, moderately eroded	MsC2	1556	533439	kx2q	md600	1972	1:15840
Neshaminy and Montalto very stony silt loams, 15 to 25 percent slopes	NsD	1473	533444	kx2w	md600	1972	1:15840
Neshaminy and Montalto very stony silt loams, 25 to 45 percent slopes	NsE	606	533445	kx2x	md600	1972	1:15840
Montalto silt loam, 0 to 3 percent slopes	MsA	262	533437	kx2n	md600	1972	1:15840
Neshaminy-Montalto complex, 0 to 8 percent slopes	NmB	1539	984495	30ch8	pa045	1960	1:20000
Montalto silt loam, 8 to 25 percent slopes, very stony	MrD	2	1478525	30cfz	pa045	1960	1:20000
Montalto channery silt loam, 3 to 8 percent slopes	MoB	2	984514	30cfy	pa045	1960	1:20000
Montalto silty clay loam, 7 to 15 percent slopes	42C	692	1726402	1vygd	va047	2006	1:24000
Montalto silty clay loam, 2 to 7 percent slopes	42B	387	1726401	1vygc	va047	2006	1:24000
Montalto silty clay loam, 15 to 25 percent slopes	42D	189	1726403	1vygf	va047	2006	1:24000
Chantilly-Montalto complex, 2 to 7 percent slopes	23B	52	2250299	2fjm9	va059	2007	1:12000
Chantilly-Montalto complex, 7 to 15 percent slopes	23C	36	2250301	2fjmc	va059	2007	1:12000
Montalto and Haymarket soils, 7 to 15 percent slopes	167C	985	1895429	21mbw	va061	2006	1:12000
Montalto loam, 7 to 15 percent slopes	65C	553	1895365	21m8t	va061	2006	1:12000
Montalto silty clay loam, 2 to 7 percent slopes	65B	1479	642091	pk4m	va107	2006	1:12000
Montalto silty clay loam, 2 to 7 percent slopes	40B	941	521196	khbs	va153	1985	1:15840
Montalto silty clay loam, 7 to 15 percent slopes	40C	432	521197	khbt	va153	1985	1:15840
Myersville and Montalto soils, 15 to 25 percent slopes, very stony	32D	8636	518846	kdwz	va187	1980	1:15840
Myersville and Montalto soils, 25 to 65 percent slopes, very stony	32E	8155	518847	kdx0	va187	1980	1:15840
Myersville and Montalto soils, 7 to 15 percent slopes, very stony	32C	2235	518845	kdwy	va187	1980	1:15840
Montalto loam, 7 to 15 percent slopes	29C	1120	518837	kdwp	va187	1980	1:15840

Map of Series Extent

Approximate geographic distribution of the MONTALTO 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).