Soil Data Explorer - TIVOLI

Official Series Description

Lab Data Summary

Aggregate lab data for the TIVOLI soil series. This aggregation is based on all pedons with a current taxon name of TIVOLI, 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 TIVOLI 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
77C	40A4498	58TX115001	TIVOLI	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.7988892,-102.1633301
77C	40A4654	75TX017008	TIVOLI	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.1528816,-102.9054718
78C	88P0743	88OK059001A	Tivoli	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.6138878,-99.5805588
78C	88P0744	88OK059001B	Tivoli	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.6155548,-99.5805588
79	40A0200	63KS057003	Tivoli	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.6402779,-99.5933304
79	40A1865	63KS057004	Tivoli	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.6630554,-99.5811081
79	40A1809	S1959KS155001	TIVOLI	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.1566658,-98.4349976
79	40A1810	S1959KS155002	TIVOLI	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.1008759,-98.4359131
80A	76-OK-27-25	76-OK053-27-25	Tivoli	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.7711528,-98.109675

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TIVOLI 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 TIVOLI series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the TIVOLI 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 2023-10-09).

Geomorphic description summaries for the TIVOLI 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 2023-10-04).

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

Competing Series

Soil series competing with TIVOLI share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the TIVOLI 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 2023-10-09).

Geomorphic description summaries for the TIVOLI 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 2023-10-04).

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

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

Soil series sharing subgroup-level classification with TIVOLI, 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 2023-10-02).

Block Diagrams

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

1. CO-2011-05-27-16 | Prowers County - 1966

   Main soils and underlying materials in soil association 5 (Soil Survey of Prowers County, Colorado; 1966).

2. CO-2011-05-27-19 | Prowers County - 1966

   Cross sections showing relationships of the soils to the landscape and to the underlying geologic formations in Prowers County. The upper cross section shows relationships in the western part of the county, and the lower shows those in the eastern part of the county (Soil Survey of Prowers County, Colorado; 1966).

3. KS-2012-01-20-26 | Clark County - December 1982

   Typical pattern of soils in the Pratt-Tivoli-Kingsdown association (Soil Survey of Clark County, Kansas; 1982).

4. KS-2012-01-20-49 | Edwards County - September 1973

   Pattern of soils in associations 1, 3, and 7. Association 1 is to the left of Big Coon Creek. Association 7 extends from Big Coon Creek to the Arkansas River. Association 3 is to the right of the Arkansas River (Soil Survey of Edwards County, Kansas; 1973).

5. KS-2012-01-23-02 | Finney County - November 1965

   Typical cross section of the valley of the Arkansas River (Soil Survey of Finney County, Kansas; 1965).

6. KS-2012-01-23-04 | Finney County - November 1965

   Typical cross section of the Manter-Keith association (Soil Survey of Finney County, Kansas; 1965).

7. KS-2012-01-23-05 | Ford County - August 1965

   A geologic cross section west of Dodge City showing the major soil associations in Ford County (Soil Survey of Ford County, Kansas; 1965).

8. KS-2012-01-23-13 | Grant County - December 1969

   Relationships of soils in association 2 (Soil Survey of Grant County, Kansas; 1969).

9. KS-2012-01-23-15 | Grant County - December 1969

   Relationships of soils in association 4 (Soil Survey of Grant County, Kansas; 1969).

10. KS-2012-01-23-16 | Grant County - December 1969

    Relationships of soils in association 5 (Soil Survey of Grant County, Kansas; 1969).

11. KS-2012-01-23-18 | Gray County - January 1968

    Soils of the Mansic-Ulysses soil association are on the right; on the left are soils of the Pratt-Tivoli soil association (Soil Survey of Gray County, Kansas; 1968).

12. KS-2012-01-23-20 | Gray County - January 1968

    Approximate geologic cross section through the central part of Gray County and the general location of soils on the landscape (Soil Survey of Gray County, Kansas; 1968).

13. KS-2012-01-23-25 | Hamilton County - November 1961

    Geologic profile extending in a north-south direction through the central part of Hamilton County (Soil Survey of Hamilton County, Kansas; 1961).

14. KS-2012-01-23-27 | Harvey County - November 1974

    Typical pattern of soils in the Dillwyn-Tivoli association (Soil Survey of Harvey County, Kansas; 1974).

15. KS-2012-01-23-30 | Haskell County - October 1968

    Typical topographic relation of three soil associations in Haskell County. Tivoli-Vona association, the farthest north, blocks drainageways flowing from the Satanta-Manter and the Richfield-Ulysses associations to the south (Soil Survey of Haskell County, Kansas; 1968).

16. KS-2012-01-23-31 | Haskell County - October 1968

    Soils of the Richfield-Ulysses association in the central part of the county (Soil Survey of Haskell County, Kansas; 1968).

17. KS-2012-01-23-44 | Kearny County - November 1963

    An approximate geologic profile of Kearny County, extending in a north-south direction across the county near Hartland (Soil Survey of Kearny County, Kansas; 1963).

18. KS-2012-01-25-13 | Pratt County - September 1968

    Major soils of associations 1 and 2 and the positions they normally occupy on the landscape (Soil Survey of Pratt County, Kansas; 1968).

19. KS-2012-01-25-27 | Rice County - December 1974

    Distribution of the soils in the Carwile-Farnum-Tabler and Canadian-Kaski-Platte associations (Soil Survey of Rice County, Kansas; 1974).

20. KS-2012-01-26-11 | Stanton County - December 1961

    Diagram of the Manter-Dalhart-Ulysses soil association in the valley of Bear Creek (Soil Survey of Stanton County, Kansas; 1961).

21. KS-2012-01-26-14 | Stevens County - October 1961

    Geological cross section through the central part of Stevens County (Soil Survey of Stevens County, Kansas; 1961).

22. NM-2012-02-14-03 | Harding County - November 1973

    Typical pattern of soils in association 10 in the eastern part of the county (Soil Survey of Harding County, New Mexico; November 1973).

23. NM-2012-02-14-11 | Lea County - January 1974

    Typical pattern of soils, topography, and underlying material in Brownfield-Patricia-Tivoli association (Soil Survey of Lea County, New Mexico; January 1974).

24. NM-2012-02-14-17 | Portales Area - May 1959

    Relative position and underlying material of main soils of Portales Valley: A, B, Mansker (shallow) and Potter (very shallow), underlain by rocky caliche and High Plains marl. C, Church, underlain by strongly calcareous lake sediments. D, Drake, underlain by strongly calcareous sediments from lakebeds. E, F, Arch and Portales, underlain by strongly calcareous valley fill of mixed wind- and water-deposited materials. G, Blackwater, underlain by valley fill and, in turn, by hard caliche at moderate depths. H, Clovis, underlain by mixed water- and wind-deposited sediments from the High Plains upland. I, J, K, Kimbrough, Amarillo, and Arvana, underlain by mixed water- and wind-deposited materials from the High Plains upland; Kimbrough soils underlain by hard caliche at shallow depth, and Arvana soils by hard caliche at moderate depth. L, M, Springer (deep) and Tivoli (very deep), underlain by wind-deposited sands (Soil Survey of Portales Area, New Mexico; May 1959).

25. NM-2012-02-15-01 | Roosevelt County - March 1967

    Generalized diagram of soil patterns that extend southwest to northeast through Roosevelt County (Soil Survey of Roosevelt County, New Mexico; March 1967).

26. OK-2010-09-29-19 | Woods County - 2003

    Typical pattern of soils and underlying material in the Eda-Devol-Lovedale general soil map unit (Soil Survey of Woods County, Oklahoma; 2003).

27. OK-2012-02-16-03 | Beaver County - August 1962

    Parent material and parent rock of most of the soils in Beaver County, and their position on the landscape (Soil Survey of Beaver County, Oklahoma; August 1962).

28. OK-2012-02-16-09 | Cimarron County - June 1960

    Typical landscape in the central and eastern part of Cimarron County: Associations 1, 2, 3, and 5 (Soil Survey of Cimarron County, Oklahoma; June 1960).

29. OK-2012-02-16-21 | Cotton County - December 1963

    Typical pattern of Pratt, Tivoli, and associated soils (Soil Survey of Cotton County, Oklahoma; December 1963).

30. OK-2012-02-16-26 | Dewey County - December 1963

    Typical pattern of the soils in association 4 (Soil Survey of Dewey County, Oklahoma; December 1963).

31. OK-2012-02-16-27 | Dewey County - December 1963

    Typical pattern of most of the soils in association 5 (Soil Survey of Dewey County, Oklahoma; December 1963).

32. OK-2012-02-16-35 | Greer County - March 1967

    Major soils in soil association 1, and their relation to the landscape (Soil Survey of Greer County, Oklahoma; March 1967).

33. OK-2012-02-16-46 | Harper County - June 1960

    A schematic drawing showing a normal pattern of soils formed on alluvial plains and on windblown sands. The typical slope range is given for each soil (Soil Survey of Harper County, Oklahoma; June 1960).

34. OK-2012-02-16-52 | Jackson County - June 1961

    Typical pattern of Miles, Enterprise, Tivoli, and associated soil (Soil Survey of Jackson County, Oklahoma; June 1961).

35. OK-2012-02-17-12 | Major County - October 1968

    Soil associations in the central part of the county (Soil Survey of Major County, Oklahoma; October 1968).

36. OK-2012-02-17-13 | Major County - October 1968

    Cross section along a line extending across the middle of the county from the western to the eastern boundary (Soil Survey of Major County, Oklahoma; October 1968).

37. OK-2012-02-17-54 | Texas County - July 1961

    Typical pattern of the soils in association 4, Texas County, Okla (Soil Survey of Texas County, Oklahoma; July 1961).

38. OK-2012-02-17-59 | Woodward County - November 1963

    Typical pattern of soils of the Pratt association (Soil Survey of Woodward County, Oklahoma; November 1963).

39. OK-2012-02-17-61 | Woodward County - November 1963

    Typical pattern of soils of the Lincoln-Las Animas association (Soil Survey of Woodward County, Oklahoma; November 1963).

40. TX-2010-11-02-22 | Carson County -

    General relationship of the soils in Carson County (Soil Survey of Carson County, Texas).

41. TX-2012-03-20-02 | Bailey County - April 1963

    Typical patterns of soils in the Tivoli-Brownfield association and the Amarillo loamy fine sand association (Soil Survey of Bailey County, TX; 1963).

42. TX-2012-03-20-10 | Carson County - July 1962

    General relationship of the soils in Carson County (Soil Survey of Carson County, TX; 1962).

43. TX-2012-03-20-15 | Carson County - July 1962

    Soil toposequence of the escarpment separating the High Plains from the Rolling Plains (Soil Survey of Carson County, TX; 1962).

44. TX-2012-03-20-20 | Childress County - July 1963

    Soils developed in eolian materials (Soil Survey of Childress County, TX; 1963).

45. TX-2012-03-20-35 | Dawson County - August 1960

    Soils on high plains developed from sandy parent material (Soil Survey of Dawson County, TX; 1960).

46. TX-2012-03-21-21 | Lamb County - March 1962

    Some soils of general soil area 3 (Soil Survey of Lamb County, TX; 1962).

47. TX-2012-03-21-36 | Lipscomb County - December 1975

    Pattern of soils and underlying material in association 3 (Soil Survey of Lipscomb County, TX; 1975).

48. TX-2012-03-21-92 | Terry County - February 1962

    Soils developed from sandy parent material (Soil Survey of Terry County, TX; 1962).

49. TX-2012-03-22-04 | Wheeler County - October 1975

    Relationship of soils in the Devol-Tivoli association to parent material and relief (Soil Survey of Wheeler County, TX; 1975).

50. TX-2012-03-22-08 | Wilbarger County - September 1962

    Block diagram showing the geographical association of the soils in association 2. Here, the soils formed in a mantle of windblown sand, which lies over sandy outwash material (Soil Survey of Wilbarger County, TX; 1962).

Map Units

Map units containing TIVOLI 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
Tivoli sand	Tn	14752	94215	3516	co009	1966	1:20000
Tivoli-Dune land complex	To	10978	94213	3514	co009	1966	1:20000
Eda-Tivoli sands, 1 to 12 percent slopes	5447	4630	3156049	2yd7j	ks007	1973	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	3582	1382514	1hdm7	ks007	1973	1:24000
Tivoli fine sand, 5 to 30 percent slopes	5972	1371	1382525	2sg3b	ks007	1973	1:24000
Goltry-Tivoli fine sands, 5 to 12 percent slopes	6201	18	3221133	2y2rz	ks007	1973	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	4656	1440496	2ww14	ks009	1979	1:24000
Eda-Tivoli sands, 1 to 12 percent slopes	5447	26175	3156050	2yd7j	ks025	1980	1:24000
Tivoli fine sand, 5 to 30 percent slopes	5972	13616	1381746	2sg3b	ks025	1980	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	1043	1381738	1hct6	ks025	1980	1:24000
Eda-Tivoli sands, 1 to 12 percent slopes	5447	15852	3156051	2yd7j	ks033	1987	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	5663	1381284	1hcbk	ks033	1987	1:24000
Tivoli fine sand, 5 to 30 percent slopes	5972	3993	1381294	2sg3b	ks033	1987	1:24000
Lincoln-Tivoli complex, 0 to 10 percent slopes	6063	4577	1382942	30yql	ks035	1977	1:24000
Attica-Tivoli loamy fine sands, 3 to 15 percent slopes	5866	1287	1382921	2wtxk	ks035	1977	1:24000
Tivoli fine sand, 10 to 30 percent slopes	5972	90	1382971	2ww15	ks035	1977	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	28356	1380389	2ww14	ks047	1967	1:24000
Tivoli fine sand, 10 to 30 percent slopes	5972	12539	1380396	2ww15	ks047	1967	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	19595	1380461	2ww14	ks057	1962	1:24000
Tivoli fine sand, 10 to 30 percent slopes	5972	7555	1473192	2ww15	ks057	1962	1:24000
Las Animas-Tivoli complex, 0 to 6 percent slopes, occasionally flooded	1189	1194	1380438	1hbg8	ks057	1962	1:24000
Tivoli fine sand, 4 to 20 percent slopes, eroded	2810	207	1380472	1hbhc	ks057	1962	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	24352	1468906	2ww14	ks069	1965	1:24000
Tivoli fine sand, 10 to 30 percent slopes	5972	1228	1382746	2ww15	ks077	1965	1:24000
Goltry-Tivoli fine sands, 5 to 12 percent slopes	6201	869	3221136	2y2rz	ks077	1965	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	24	1382725	1hdv1	ks077	1965	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	3386	1155458	2ww14	ks079	1970	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	4469	1444802	2ww14	ks095	1977	1:24000
Tivoli fine sand, 10 to 30 percent slopes	5972	1247	1651572	2ww15	ks095	1977	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	34828	1380539	2ww14	ks097	1983	1:24000
Tivoli fine sand, 10 to 30 percent slopes	5972	9149	1380548	2ww15	ks097	1983	1:24000
Tivoli fine sand, 10 to 30 percent slopes	5972	2	1455147	1kv67	ks119	1973	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	8128	1380144	2ww14	ks145	1976	1:24000
Tivoli fine sand, 10 to 30 percent slopes	5972	1425	1380149	2ww15	ks145	1976	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	1733	1445161	2ww14	ks151	1965	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	1674	1433298	2ww14	ks159	1971	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	2374	1443985	2ww14	ks173	1976	1:24000
Pratt-Tivoli loamy fine sands, 5 to 15 percent slopes	5941	24146	1443669	2ww14	ks185	1975	1:24000
Tivoli fine sand, 10 to 30 percent slopes	5972	2427	1444625	2ww15	ks191	1974	1:24000
Lincoln-Tivoli complex, 0 to 10 percent slopes	6063	881	1444632	30yql	ks191	1974	1:24000
Tivoli fine sand	TF	46886	376381	dmnb	nm021	1968	1:31680
Tivoli-Springer complex	TG	14899	376382	dmnc	nm021	1968	1:31680
Tivoli fine sand	TF	38607	376198	dmgf	nm676	1969	1:31680
Goltry-Tivoli fine sands, 5 to 12 percent slopes	GoTE	11827	3041113	2y2rz	ok003	1971	1:24000
Aline-Tivoli complex, 5 to 12 percent slopes	AlTE	1712	381409	2y2s0	ok003	1971	1:24000
Jester and Tivoli soils, 1 to 30 percent slopes	57	6520	381696	dt5s	ok009	1978	1:24000
Eda-Tivoli sands, 1 to 12 percent slopes	EdsF	3	381681	2yd7j	ok009	1978	1:24000
Tivoli fine sand, 5 to 30 percent slopes	TrD	485	381778	2sg3b	ok011	1965	1:24000
Eda and Tivoli soils, 3 to 12 percent slopes	PvC	5046	382245	dtrh	ok033	1961	1:24000
Eda-Tivoli complex, 5 to 12 percent slopes	PtE	3134	382337	2sg3c	ok039	1973	1:24000
Eda-Tivoli sands, 1 to 12 percent slopes	Pt	7501	382390	2yd7j	ok043	1961	1:24000
Tivoli fine sand, 5 to 30 percent slopes	Tv	5455	382403	2sg3b	ok043	1961	1:24000
Tivoli fine sand, 5 to 30 percent slopes	Tv	3621	382473	2sg3b	ok045	1963	1:24000
Tivoli fine sand, 5 to 12 percent slopes	TvlE	20603	383040	dvl4	ok059	1998	1:24000
Tivoli fine sand, 12 to 45 percent slopes	TvlG	10410	383043	dvl7	ok059	1998	1:24000
Tivoli fine sand, 1 to 5 percent slopes	TvlC	1869	383038	dvl2	ok059	1998	1:24000
Tivoli fine sand, 5 to 30 percent slopes	TrD	5887	383869	2sg3b	ok093	1965	1:24000
Eda-Tivoli sands, 1 to 12 percent slopes	PtD	5799	383851	2yd7j	ok093	1965	1:24000
Tivoli fine sand, 5 to 30 percent slopes	TivG	36775	385241	2sg3b	ok151	1995	1:24000
Tivoli loamy fine sand, 5 to 12 percent slopes	TviE	18070	385242	dxw5	ok151	1995	1:24000
Dune land-Tivoli complex, 3 to 60 percent slopes	DuTH	4507	385174	dxsz	ok151	1995	1:24000
Eda-Tivoli sands, 1 to 12 percent slopes	Pt	61612	385294	2yd7j	ok153	1961	1:24000
Tivoli fine sand, 5 to 30 percent slopes	Tv	23650	385304	2sg3b	ok153	1961	1:24000
Tivoli fine sand, 5 to 30 percent slopes	TfF	3805	363301	2sg3b	tx045	1972	1:20000
Tivoli-Springer association, 1 to 8 percent slopes	TSD	1204	393895	f6w9	tx065	2000	1:24000
Tivoli fine sand	51	676	363906	d6nx	tx077	1977	1:24000
Tivoli fine sand, 5 to 30 percent slopes	Tv	9829	364129	2sg3b	tx087	1965	1:20000
Devol and Tivoli soils, hummocky	StD	1608	364619	d7dx	tx101	1969	1:20000
Tivoli fine sand, dry, 5 to 30 percent slopes	Tv	465	364745	2t3rk	tx107	1964	1:20000
Tivoli fine sand, 5 to 30 percent slopes	Tf	8266	365209	2sg3b	tx129	1975	1:24000
Tivoli fine sand, dry, 5 to 30 percent slopes	Ts	4447	365813	2t3rk	tx151	1964	1:24000
Tivoli fine sand, dry, 5 to 30 percent slopes	Tv	2011	378359	2t3rk	tx169	1965	1:24000
Heatly-Tivoli complex, 0 to 8 percent slopes	Tw	420	378360	2vt8f	tx169	1965	1:24000
Tivoli fine sand, 5 to 30 percent slopes	Tf	20543	391956	2sg3b	tx179	1965	1:20000
Tivoli fine sand, 5 to 30 percent slopes	Tv	20837	366969	2sg3b	tx191	1965	1:20000
Tivoli fine sand, 5 to 30 percent slopes	Tv	10726	367169	2sg3b	tx197	1965	1:20000
Tivoli-Nobscot complex, 5 to 15 percent slopes	TvND	694	2713444	2r5rz	tx207	1960	1:20000
Heatly-Tivoli complex, 0 to 8 percent slopes	BtB	3523	368474	2vt8f	tx263	1968	1:31680
Tivoli fine sand, dry, 5 to 30 percent slopes	Tv	3181	368507	2t3rk	tx263	1968	1:31680
Nobscot and Tivoli soils, undulating	NtB	418	368492	dcfv	tx263	1968	1:31680
Tivoli fine sand, dry, 5 to 30 percent slopes	Tf	12093	370745	2t3rk	tx335	1965	1:20000
Tivoli fine sand, dry, 5 to 30 percent slopes	Tf	8265	370897	2t3rk	tx345	1972	1:24000
Devol and Tivoli soils, 1 to 8 percent slopes	DtD	1495	370858	dfx5	tx345	1972	1:24000
Tivoli fine sand	Tf	7917	3124171	dg6f	tx359	1978	1:24000
Tivoli-Springer association, undulating	TSD	2320	3124236	dgfk	tx375	1974	1:24000
Tivoli fine sand, dry, 5 to 30 percent slopes	Tv	2969	372036	2t3rk	tx415	1966	1:24000
Tivoli fine sand, 5 to 30 percent slopes	Tv	29255	373329	2sg3b	tx483	1970	1:24000
Blown-out land-Tivoli complex	Bt	906	373282	djfc	tx483	1970	1:24000
Tivoli fine sand	Tv	1035	373391	djjw	tx485	1972	1:20000
Tivoli fine sand, 5 to 30 percent slopes	Tv	12104	373450	2sg3b	tx487	1960	1:20000

Map of Series Extent

Approximate geographic distribution of the TIVOLI 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 2023-10-04).