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T.II I ION T. 9 N T. /N. T. 7 N. NEBRASKA 103'30' I 103'20' 103'10' KI \i 8.11.1 rnt'NT %' l'�L r•nrvr/n Vr rnr'N'PV 1 SECTIONALIZED TdWNSHIP Su1e 1:316./00 7) O41 s S 4 1312 1 I N sa rc N. se W, 7 / 9 10 11 12 0,' 16 IS utter rI Opoorly i�W�ii� ZI ?2 v 21 Eorh areo viti..d en Mir map ronrlrlr of 30 29 H Z7 ZS 25 r Mon one kmd or wit. The mop h lhur X011 37 - I I A 36 Nr general Planning rolher Man o boor 71 77 94 ON THE UPLANDS b• deri,i— oa Ph, — 0 .",di, 1nxN. Deep, undulating to hilly, excessively drained soils forming in noncalcar. f OValenta eous eolian sandy materials on uplands Dailey- lulesburg: Deep, nearly level to moderately sloping, somewhat excessively _ — Q drained and well drained soils forming In noncalcareous eolian sandy materials on uplands QMaxtun- Julesourg: Deep, nearly level to moderately sloping, well drained soils forming In noncaicareous eolian sandy loam materials on uplands Manler- A scat on -Vona: Deep, nearly level to moderately sloping, well drained Oj soils forming In calcareous eolian and alluvial sandy and sandy loam materials on uplands SANDY LOAM TO CLAY LOAM SOILS FORMING ON UNCONSOLIDATED MATE. 10.40' RIALS ON THE UPLANDS Planner -Ft ago- RosaWd: Dap and moderately deep, nearly level to moderately Osloping, well drained sells forming in loamy alluvisl and eollan materials on uplands Weld- Platner- As "alon: Deep, nearly level to moderately sloping, well drained O9 soils forming In loamy alluvial and eollan materials on uplands Norka- Ulysses- Colby: Deep, gently sloping to strongly sloping, well drained 10 soils forming In calcareous loamy eollan materials on uplands Wages- Satanta�Norka: Deep, nearly level to strongly sloping, well drained soils 11 forming In calcareous, loamy alluvial and eolian materials on upland flats, in valleys, and on ridges DEEP, MODERATELY DEEP AND SHALLOW SOILS UNDERLAIN BY CONSOL. IDATED SEDIMENTS ON THE UPLANDS 12 a►�: �Rrk7.ri. 0.30' Uslic Tortiorlhents-Badlan& Shallow, steep, well drained loamy soils, underlain 13 by slltstone and calcareous sandstone, and Badland; on uplands ® Mitchell Keola: Deep and moderalely deep, neatly level to moderately sloping, ■■S> well drained soils formed in loamy materials derived from slltsione; on uplands Stoneham - Cushman - Shingle: Deep to shallow, gently sloping to strongly sloping, 15 N ■� uplands f ■ ■ ■r�1I11■i. Dix. Eckley- Chappell: Deep, gently sloping.to moderately steep, well drained 16 and somewhat excessively drained soils forming In gravelly alluvium; on upland ■I� ridges and alluvial tans ■� ■i ■■imp ■�.�ra�i� ■m��.0 ' ■ � ■ MEN ■ ;� ■ �■■NO��..r�l� I�111I ■■ ■�.i!� ■ ■_ ■ice ■ ■ ■OOm ■�!i��w��- i ■► ■ ■■►J %ice` ` �ir1', ■1111 ► ■I ._ ■ ■ ■! %SOON 14 1 7W a its �■iiliiiiii \■Iii ■ \':In. 11 a Ma141 �� �iiii ■■ '= `° .... WIF 1 101.2.61141 I M 0 0101 t 1� ■��. ■ ■'�IS• �� �rrJ. WIF ERIC, ■� 1J ��i`-■ ■■�� - ..■ ■ iiie�i� �� � Q ■ ■1 ��► - I ■ ■■ NMI ■ 0111iri� ■ ■■ - \�1lrl O� r ®1�1l, r ■ ■►'\ ■/111 ■ ■ ■1\ 'il> 1/I .. ■ ■■■■ ■ '.,� ■ ■PIAW I ■ ■ ►.fi r± ■r© ��,�e1 ■ ■ ■�.� . �� ►�� ■�� n`M��,'�'��' ■0��.��1!/� i�.!:'� !� ■a �■■ H�� X3..0 ��._.�■ ■ - s �rm�i �■ It No o � � � ■■■■ I `■o► MOSOMEMM 10011I.W10 Ems VIE ■ CAI ■N ■l�911� ■��A ■- MORGAN Jr�c■►Liq ■_■■ ■ ■ ■■to ■■■■■■■ ■ r®■■■■■ f fff�� 1� l�� low �■ MEN SECTIONALIZED TdWNSHIP Su1e 1:316./00 7) O41 s S 4 1312 1 I N sa rc N. se W, 7 / 9 10 11 12 Is 17 16 IS 14 17 rI Opoorly 19 M ZI ?2 v 21 Eorh areo viti..d en Mir map ronrlrlr of 30 29 H Z7 ZS 25 r Mon one kmd or wit. The mop h lhur X011 37 - I I A 36 Nr general Planning rolher Man o boor 71 77 94 ON THE UPLANDS b• deri,i— oa Ph, — 0 .",di, 1nxN. .WASHINGTON COUNTY , ;YUMA COUNTY! R, 52 W. R. 51 W. R. 50 W. R. 49 W. I R. 48 W. N U. S. DEPARTMENT OF AGRICULTURE SOIL CONSERVATION SERVICE COLORADO AGRICULTURAL EXPERIMENT STATION -,;- GENERAL SOIL MAP LOGAN COUNTY, CO1,011AI)0 Su1e 1:316./00 1 0 1 2 3 4 5 Meer I�Lr1...L. -.__ .... __J z us SOIL LEGEND SOILS FORMING IN UNCONSOLIDATED ALLUVIUM ON STREAM TERRACES, FLOOD PLAINS AND BOTTOMLANDS rI Opoorly Aida- Loveland- FluvaOUents: Deep, nearly level, somewhat poorly drained and drained soils forming mostly in loamy alluvium underlain by sand and gravel, on bottomlands and low terraces Nunn- Sananta- Haverson: Deep, nearly level, well drained and moderately well - 40'50' drained soils forming in loamy alluvium or. terraces and 11.1 plains t =3 Mosher- Lehsack: Deep, nearly level, somewhat poorly drained, saline and alkali - I I affected soils forming In clayey alluvium on bottomlands and terraces SAND TO FINE SANDY LOAM SOILS FORMING ON UNCONSOLIDATED MATERIALS x ON THE UPLANDS Deep, undulating to hilly, excessively drained soils forming in noncalcar. f OValenta eous eolian sandy materials on uplands Dailey- lulesburg: Deep, nearly level to moderately sloping, somewhat excessively _ — Q drained and well drained soils forming In noncalcareous eolian sandy materials on uplands QMaxtun- Julesourg: Deep, nearly level to moderately sloping, well drained soils forming In noncaicareous eolian sandy loam materials on uplands Manler- A scat on -Vona: Deep, nearly level to moderately sloping, well drained Oj soils forming In calcareous eolian and alluvial sandy and sandy loam materials on uplands SANDY LOAM TO CLAY LOAM SOILS FORMING ON UNCONSOLIDATED MATE. 10.40' RIALS ON THE UPLANDS Planner -Ft ago- RosaWd: Dap and moderately deep, nearly level to moderately Osloping, well drained sells forming in loamy alluvisl and eollan materials on uplands Weld- Platner- As "alon: Deep, nearly level to moderately sloping, well drained O9 soils forming In loamy alluvial and eollan materials on uplands Norka- Ulysses- Colby: Deep, gently sloping to strongly sloping, well drained 10 soils forming In calcareous loamy eollan materials on uplands Wages- Satanta�Norka: Deep, nearly level to strongly sloping, well drained soils 11 forming In calcareous, loamy alluvial and eolian materials on upland flats, in valleys, and on ridges DEEP, MODERATELY DEEP AND SHALLOW SOILS UNDERLAIN BY CONSOL. IDATED SEDIMENTS ON THE UPLANDS 12 Rosebud- Escabosa-Canyon: Moderately deep and shallow, gently eloping to mod erately slap, well drained loamy soils underlain by calcareous sandstone; on up- lands 0.30' Uslic Tortiorlhents-Badlan& Shallow, steep, well drained loamy soils, underlain 13 by slltstone and calcareous sandstone, and Badland; on uplands Mitchell Keola: Deep and moderalely deep, neatly level to moderately sloping, 14 well drained soils formed in loamy materials derived from slltsione; on uplands Stoneham - Cushman - Shingle: Deep to shallow, gently sloping to strongly sloping, 15 well drained soils formed in calcareous loamy materials underlain by shale; on uplands DEEP SOILS FORMING IN UNCONSOLIDATED GRAVELLY MATERIALS ON UPLAND RIDGE$ AND FANS Dix. Eckley- Chappell: Deep, gently sloping.to moderately steep, well drained 16 and somewhat excessively drained soils forming In gravelly alluvium; on upland ridges and alluvial tans Compiled 1976