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HomeMy WebLinkAboutSD-321-1I t i f r i i . I I i t t 1 v Q a 0 0 :J M ti - f / l i jam/ � 1 04 At- 1 Soil Analyses & Contours NARRAGANSETT series consists of nearly level to steep, deep, well drained soils on glacial till plains and ground moraine. They formed on silt mantled glacial till. Narragansett soils have friable silt loam or very fine sandy loam surface soil and subsoil that have moderate permeability over friable to loose fine sandy loam to loamy coarse sand substratum at 16 to 36 inches with moderately rapid or rapid permeability. Narragansett soils have a very stony or extremely stony surface, except where stones have been removed. Major limitations are related to slope and stoniness. 9 i Ile i / �f/ / / i ! 0 i Direction of overland flow. Division of existing water,,heds — - - °- Existing swales Drainage Analysis oT�S 1)- EP E ,� G� io Y� AO� E_FVhTIOti{ ON 7HF= Si Z} °jEE DF�It- .- IAl1�t6, �+l- GuLJ�"t"�O7.}� Pp�E t°AtiEt� t3Y M�P�IDIAt -t 1= r- leol�r�Ei=,IHC� /pLt..�r�c�r'�1 "��� , ItiL, 1=�ti�. t�'to4�.E r�ETAiLEt� •� 1� : �- 91 /1 / ♦� / . / , f o Existing Vegetation: `� ®Tbe existing vegetation consists of numerous large oaks and an equal : number of white trine. } ® A secondary tree canopy is developing consisting of cherry, gray birch, Vegetation e.ta Eton Analysis . and black birch. U -b Q 5-10 10 -15 15% and greater.. ti - f / l i jam/ � 1 04 At- 1 Soil Analyses & Contours NARRAGANSETT series consists of nearly level to steep, deep, well drained soils on glacial till plains and ground moraine. They formed on silt mantled glacial till. Narragansett soils have friable silt loam or very fine sandy loam surface soil and subsoil that have moderate permeability over friable to loose fine sandy loam to loamy coarse sand substratum at 16 to 36 inches with moderately rapid or rapid permeability. Narragansett soils have a very stony or extremely stony surface, except where stones have been removed. Major limitations are related to slope and stoniness. 9 i Ile i / �f/ / / i ! 0 i Direction of overland flow. Division of existing water,,heds — - - °- Existing swales Drainage Analysis oT�S 1)- EP E ,� G� io Y� AO� E_FVhTIOti{ ON 7HF= Si Z} °jEE DF�It- .- IAl1�t6, �+l- GuLJ�"t"�O7.}� Pp�E t°AtiEt� t3Y M�P�IDIAt -t 1= r- leol�r�Ei=,IHC� /pLt..�r�c�r'�1 "��� , ItiL, 1=�ti�. t�'to4�.E r�ETAiLEt� •� 1� : �- 91 /1 / ♦� / . / , f o Existing Vegetation: `� ®Tbe existing vegetation consists of numerous large oaks and an equal : number of white trine. } ® A secondary tree canopy is developing consisting of cherry, gray birch, Vegetation e.ta Eton Analysis . and black birch.