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04-24-2000 Council Packet
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04-24-2000 Council Packet
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Physical Features <br />Big Island encompasses approximately 250 acres in area, of which approximately 50 <br />acres is wetland. A navigable channel actually separates Big Island into two distinct <br />islands. The shoreland ranges from flat, low wetland areas near the lake level to <br />steep and often eroded bluffs extending as much as 30-40' above lake level. The <br />topography is hilly. The highest point on the island is 988', nearly 60' above lake <br />level, located near the south end of Morse Island Park. <br />Soils on Big Island are mapped as Hayden loam and clay loam, typical of soils <br />located in central and northern Orono. Beach sand soils occur in a number of flat, low <br />areas near the shoreline. Except for scattered clearings to accommodate individual <br />cabins or recreation areas, the island remains heavily vegetated with hardwood <br />species typical of the "Big Woods". <br />Services <br />Big Island is provided with only a minimal degree of municipal services. There is <br />no municipal sewer or water on the island, hence the use of individual septic systems <br />and wells is common. The island is provided with telephone service and electric <br />power via lines from the mainland. Police protection is minimally provided by the <br />City of Orono and the Hennepin County Sheriff. Fire protection is provided by the <br />Long Lake Fire Department although response time is understandably poor due to the <br />lack of roads or bridges connecting the island to the mainland, and access to the <br />island makes firefighting extremely difficult. Other services such as street repair, <br />snow removal, inspections, and rev'ar garbage remr val are difficult, uneconomical <br />and in some instances virtually ii, .possible to provide to residential property located <br />on the island. <br />Access <br />There are no improved roads on Big Island. A limited system of roadways and alleys <br />was platted more than a century ago in the Morse Island Park and Pleasantview <br />subdivisions, which primarily created narrow lakeshore lots but also resulted in a <br />small number of inland lots not abutting the lakeshore and needing access to the lake. <br />These platted corridors exist today as walking trails which on occasion are used for <br />vehicular access. Since most lots do abut the shoreline, use of the interior roadwav <br />system has been primarily by the owners of interior lots, and by ovviiers of lakeshore <br />lots with shoreline slopes that prohibit direct lake access. <br />Vehicular access is necessary for nearly all island properties on occasion, hence the <br />interior roadways are an important transp-mation element for Big Island. Overuse <br />of the road system by residents or the general public is of concern, since the roads are <br />not improved. Erosion and trespass are two main issues, because the roadways ere <br />not marked and they often traverse steep slopes, especially where lanes extend to the <br />lakeshore. <br />CMP3B-40
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