Laserfiche WebLink
Fai;o - .s- <br />Preliminary Soil, fli und Wetland Evaluation <br />Painters Creek Estate in City of Orono <br />I« <br />b <br />1- <br />!t <br />•, ■ <br />5. <br />V ^K <br />11 <br />* ^ <br />Medium <br />Blue <br />Medium <br />Blue <br />Medium <br />Green <br />Light <br />Red <br />/ <br />2. Glencoesilty clay loam: <br />The map symbol for this soil is Gc and the map color is medium blue. <br />This soil is deep and ver>' poorly drained, 'fhe soil was formed in <br />loamy colluvium over calcareous loamy till, llie soil is nearly level <br />occupying depressions and sluggish drainageways. <br />Site development characteristics are generally unfavorable. The water <br />table is above or near the surface the entire year and the soil <br />has low soil strength. <br />5. Hamel loam: <br />The map symbol for this soil is 11a and the map color is medium blue. <br />This is a deep, well-drained loam soil that occurs in short, narrow <br />drainageways on foot slopes and in long winding drainageways between <br />knolls and hills. During wet periods of the year there is a perched <br />watertable within 1 foot of the surface. These soils often wet <br />for a good portion of the year. They are also subject to ponding <br />and the upper horizons are high in organic matter content giving than <br />low bearing values. There is also a high potential for frost action <br />to roads or parking lots constructed on these soils. <br />4. Hayden loam: <br />This is a deep, well-drained loam soil that occurs on gently sloping <br />to very steep slopes, on knolls and hillsides. The soil was strongly <br />influenced by a forest environment in its development. Shale and <br />limestone fragments as well as granitic cobbles and boulders are com­ <br />mon throughout. Several slope phases are mapped. Each slope phase <br />is discussed separately. <br />a). Hayden loam - 2 to 6 percent slope: <br />The map symbol for this soil is HbB and the map color is medium <br />green. TTiis is a gently undulating soil occupying areas on knolls <br />and hillsides. This soil is well-drained and therefore never <br />saturated although sidehill seepage is not uncommon around base­ <br />ment walls during rainy seasons or spring thaws. The rolling <br />slopes offer attractive building sites. <br />5. Lerdal loam: <br />The map symbol for this soil is LmB and the map color is light red. <br />This is a deep, somewhat poorly drained soil that formed in a cal­ <br />careous loamy mantle of till 3 to 20 feet thick. The soil is nearly <br />level occupying areas low knolls and on the tops of large hills. There <br />is a seasonal groundwater table at a 3-5 foot depth during wet periods <br />and usually persists near these levels over winter after a wet fall. <br />Soil strength is adequate. The infiltration rate of this soil is very <br />slow. Shrink-swell potential is moderate. <br />P <br />« <br />r.' <br />. f <br />> ! <br />: 1