Official Series Description


Lab Data Summary

Aggregate lab data for the MOREHOUSE soil series. This aggregation is based on all pedons with a current taxon name of MOREHOUSE, 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 MOREHOUSE 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
2379P042979OR037005Morehouse6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.2465037,-121.0302666
2395P005894OR037002Morehouse6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3045606,-120.8391511

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MOREHOUSE 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 MOREHOUSE 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 MOREHOUSE 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 MOREHOUSE 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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Competing Series

Soil series competing with MOREHOUSE 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 MOREHOUSE series and competing. 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 MOREHOUSE 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 .

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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.

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Soil series sharing subgroup-level classification with MOREHOUSE, 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

No block diagrams are available.

Map Units

Map units containing MOREHOUSE 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
Morehouse ashy loamy fine sand, 0 to 2 percent slopes4704289816899721tqk7or63520061:24000
Morehouse ashy loamy fine sand, 2 to 20 percent slopes4721355916899741tqk9or63520061:24000
Fort Rock-Morehouse complex, 1 to 5 percent slopes3231276816898321tqdqor63520061:24000
Lostforest-Sandrock-Morehouse complex, 0 to 10 percent slopes420549116899251tqhqor63520061:24000
Morehouse ashy loamy fine sand, 1 to 15 percent slopes471263816899731tqk8or63520061:24000
Fort Rock-Morehouse complex, moist, 0 to 8 percent slopes324260916898331tqdror63520061:24000
Overallflat-Morehouse complex, 0 to 5 percent slopes501187216900031tql7or63520061:24000
Fort Rock-Morehouse complex, 0 to 2 percent slopes322165916898311tqdpor63520061:24000
Goodtack-Morehouse complex, 1 to 15 percent slopes342141716898501tqf9or63520061:24000
Morehouse complex, 1 to 20 percent slopes474102716899761tqkcor63520061:24000
Thornlake-Morehouse complex, 0 to 15 percent slopes63195416901311tqqcor63520061:24000
Dune land-Morehouse complex, 1 to 10 percent slopes27692116897851tqc6or63520061:24000
Morehouse-Playas complex, 0 to 2 percent slopes47577516899771tqkdor63520061:24000
Puzzlebark-Morehouse-Morehouse, gently sloping complex, 2 to 25 percent slopes52671716900261tqlzor63520061:24000
Borobey-Morehouse complex, 0 to 20 percent slopes22757616897381tq9por63520061:24000
Morehouse ashy loamy fine sand, high precipitation, 15 to 35 percent slopes47347216899751tqkbor63520061:24000
Bonnick-Morehouse complex, 0 to 10 percent slopes22146416897321tq9hor63520061:24000
Wegert-Morehouse complex, 2 to 10 percent slopes66920416901681tqrkor63520061:24000

Map of Series Extent

Approximate geographic distribution of the MOREHOUSE 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 .