Official Series Description


Lab Data Summary

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

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
10199P0455S1999NY043001Honeoye6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8277779,-74.9024963
10106N0435S2005NY069005Honeoye6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8648262,-77.0346909
10106N0439S2005NY069009Honeoye6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8800507,-77.018486
14092P0198S1991NY069001Honeoye6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7666664,-77.3000031

Water Balance

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

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the HONEOYE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the HONEOYE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the HONEOYE 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 .

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There are insufficient data to create the 3D mountains figure.

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

Competing Series

Soil series competing with HONEOYE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the HONEOYE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the HONEOYE 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 .

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 HONEOYE, 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 .

Block Diagrams

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

  1. NY-2010-09-28-20 | Otsego County - 2006

    Typical pattern of soils and underlying material in the Lansing-Conesus-Manheim general soil map unit (Soil Survey of Otsego County, New York; 2006).

  2. NY-2010-09-28-21 | Otsego County - 2006

    Typical pattern of soils and underlying material in the Farmington-Wassaic general soil map unit (Soil Survey of Otsego County, New York; 2006).

  3. NY-2012-02-15-04 | Cayuga County - 1971

    Typical cross section of Honeoye-Lima association (Soil Survey of Cayuga County, New York; 1971).

  4. NY-2012-02-15-19 | Genesee County - March 1969

    A typical cross section of the Cazenovia-Ovid association, the Benson-Honeoye, moderately deep, association, and the Onondaga limestone escarpment (Soil Survey of Genesee County, New York; March 1969).

  5. NY-2012-02-15-27 | Madison County - March 1981

    Typical relationship of soils and underlying material in Palmyra-Phelps, undulating (Soil Survey of Madison County, New York; March 1981).

  6. NY-2012-02-15-41 | Seneca County - April 1972

    Cross section of Honeoye-Lima association (Soil Survey of Seneca County, New York; April 1972).

  7. NY-2012-02-15-47 | Tompkins County - July 1965

    Typical cross section of Lima-Honeoye association and Palmyra association in northwestern Tompkins County (Soil Survey of Tompkins County, New York; July 1965).

Map Units

Map units containing HONEOYE 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
Honeoye silt loam, 3 to 8 percent slopesHnB437312894132w3p2ny01119681:15840
Honeoye silt loam, 8 to 15 percent slopesHnC92822894142w3p6ny01119681:15840
Ontario, Honeoye, and Lansing soils, 20 to 35 percent slopesOtE81372894702w3mxny01119681:15840
Honeoye and Lansing soils, 14 to 20 percent slopesHsD31092894172w3nhny01119681:15840
Ontario, Honeoye, and Lansing soils, 35 to 50 percent slopesOtF19832894712w3mqny01119681:15840
Honeoye loam, 3 to 8 percent slopesHoB14912908212w3npny02919791:15840
Honeoye loam, 0 to 3 percent slopesHoA3772908202w3nnny02919791:15840
Honeoye silt loam, 3 to 8 percent slopesHoB1237325183332w3p2ny04320181:24000
Honeoye silt loam, 8 to 15 percent slopesHoC939825183342w3p6ny04320181:24000
Honeoye and Lansing soils, 25 to 35 percent slopesHrE895225183362w3mmny04320181:24000
Honeoye silt loam, 15 to 25 percent slopesHoD613325183352w3p8ny04320181:24000
Honeoye and Mohawk very stony silt loams, 0 to 25 percent slopesHsD184825183379sx6ny04320181:24000
Honeoye loam, 8 to 15 percent slopes58C78631003862w3nrny05120191:24000
Honeoye silt loam, 3 to 8 percent slopesHnB193822925652w3p2ny05319751:15840
Honeoye silt loam, 8 to 15 percent slopesHnC131322925662w3p6ny05319751:15840
Honeoye silt loam, 15 to 25 percent slopesHnD44892925672w3p8ny05319751:15840
Honeoye silt loam, 25 to 50 percent slopesHnE23412925682w3pdny05319751:15840
Honeoye-Farmington complex, 25 to 65 percent slopes, rockyHOE19732925692w3pcny05319751:15840
Honeoye silt loam, 3 to 8 percent slopesHnB39802927102w3p2ny05519671:15840
Honeoye silt loam, 3 to 8 percent slopes, bedrock substratumHoB27652927132w3nyny05519671:15840
Honeoye silt loam, 0 to 3 percent slopes, bedrock substratumHoA9212927122w3nxny05519671:15840
Honeoye silt loam, 8 to 15 percent slopesHnC4662927112w3p6ny05519671:15840
Honeoye silt loam, 3 to 8 percent slopes102B107272932932w3p2ny06519931:24000
Honeoye silt loam, 8 to 15 percent slopes102C75322932942w3p6ny06519931:24000
Honeoye and Cazenovia soils, 25 to 45 percent slopes104E35292932972w3pbny06519931:24000
Honeoye silt loam, 15 to 25 percent slopes102D34832932952w3p8ny06519931:24000
Honeoye-Urban land complex, 2 to 8 percent slopes103B25722932962w3p0ny06519931:24000
Honeoye silt loam, 3 to 8 percent slopesHnB298762935742w3p2ny06719731:20000
Honeoye silt loam, 8 to 15 percent slopesHnC217722935752w3p6ny06719731:20000
Honeoye and Lansing soils, 15 to 25 percent slopesHoD161762935772w3mzny06719731:20000
Honeoye, Lansing, and Ontario soils, 25 to 35 percent slopesHTE90792935662w3mtny06719731:20000
Honeoye, Lansing, and Ontario soils, 35 to 50 percent slopesHTF53952935672w3mrny06719731:20000
Honeoye very stony soils, slopingHSC13372935659vgvny06719731:20000
Honeoye loam, 3 to 8 percent slopes101B976316110552w3npny06920121:12000
Honeoye loam, 3 to 8 percent slopes, lower clay surface104B763916110592w3pjny06920121:12000
Honeoye loam, 8 to 15 percent slopes101C541716110562w3nrny06920121:12000
Honeoye loam, 0 to 3 percent slopes, lower clay surface104A344516110582w3pgny06920121:12000
Honeoye loam, 15 to 25 percent slopes101D253316110572w3ntny06920121:12000
Honeoye loam, 8 to 15 percent slopes, lower clay surface104C195716110602w3pkny06920121:12000
Ontario, Honeoye, and Lansing soils, 35 to 55 percent slopes118F186617276162w3mpny06920121:12000
Honeoye loam, 0 to 3 percent slopes101A175316110542w3nnny06920121:12000
Honeoye loam, 25 to 35 percent slopes101E44525124172w3nvny06920121:12000
Honeoye and Lansing soils, 25 to 50 percent slopesHoE23142942212w3msny07719931:24000
Honeoye silt loam, 8 to 15 percent slopesHnC23042942192w3p6ny07719931:24000
Honeoye silt loam, 3 to 8 percent slopesHnB14382942182w3p2ny07719931:24000
Honeoye silt loam, 15 to 25 percent slopesHnD8612942202w3p8ny07719931:24000
Mohawk and Honeoye soils, 10 to 20 percent slopesMhC166422945102w3p5ny09519651:15840
Honeoye-Farmington complex, 2 to 10 percent slopesHfB107082944812w3nzny09519651:15840
Mohawk and Honeoye soils, 20 to 30 percent slopesMhD66092945122w3p9ny09519651:15840
Mohawk and Honeoye soils, 30 to 50 percent slopesMhF26712945132w3pfny09519651:15840
Honeoye-Farmington complex, 10 to 20 percent slopesHfC6442944822w3p4ny09519651:15840
Honeoye silt loam, 3 to 8 percent slopesHnB85782947252w3p2ny09919661:15840
Honeoye silt loam, 8 to 15 percent slopesHnC18282947262w3p6ny09919661:15840
Honeoye, Ontario, and Lansing soils, 25 to 40 percent slopesHoE9752947282w3mvny09919661:15840
Honeoye silt loam, 15 to 25 percent slopesHnD2462947272w3p8ny09919661:15840
Honeoye gravelly silt loam, 2 to 8 percent slopesHmB24352956152w3p1ny10919631:20000
Honeoye gravelly silt loam, 8 to 15 percent slopesHmC5242956162w3p3ny10919631:20000
Honeoye loam, 3 to 8 percent slopes101B914332504122w3npny12319481:12000
Honeoye loam, 3 to 8 percent slopes, lower clay surface104B599332503802w3pjny12319481:12000
Honeoye loam, 8 to 15 percent slopes101C245932503772w3nrny12319481:12000
Ontario, Honeoye, and Lansing soils, 35 to 55 percent slopes118F210532503722w3mpny12319481:12000
Honeoye loam, 8 to 15 percent slopes, lower clay surface104C64932503812w3pkny12319481:12000
Honeoye loam, 15 to 25 percent slopes101D53232503782w3ntny12319481:12000
Honeoye loam, 0 to 3 percent slopes, lower clay surface104A29614077862w3pgny12319481:12000
Honeoye loam, 0 to 3 percent slopes101A27114077902w3nnny12319481:12000
Honeoye loam, 25 to 35 percent slopes101E7832503792w3nvny12319481:12000

Map of Series Extent

Approximate geographic distribution of the HONEOYE 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 .