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• <br />Anoka County Multi- Jurisdictional <br />All Hazards Mitigation Plan <br />Slumps usually damage utilities within or below the slide mass, but seldom cause a threat to life. <br />Flows, in addition to the above hazards can flow around well -built structures, preserving them <br />but causing damage from water and mud. <br />Translational slides can be the most catastrophic. <br />In addition to presenting a hazard to structures <br />and utilities, they can cause damage and death <br />both far from and only slightly below the source. <br />The hazards associated with landslides are as <br />diverse as the types of failure. Falls may damage <br />roads or buildings at the base of a steep slope, <br />injure climbers, or remain on a road as a hazard <br />to transportation. <br />In addition to the direct hazards of a landslide <br />moving out from under or onto structures or <br />utilities, there is a major indirect hazard. Large <br />slides generally do not stop moving until they <br />reach the bottom of a valley where they block streams, <br />to the system ecology (e.g. sediment). <br />• 4.2.1.4 Land Subsidence <br />Subsidence is the formation of depressions, <br />cracks, and sinkholes in the earth's surface, <br />which normally occurs over many days to a few <br />years. <br />• <br />Karst topography develops when beds of <br />relatively soft limestone and dolomite are present. <br />The diluted organic acids present in water <br />percolates downward and dissolves these <br />formations. In such places, rock is honeycombed <br />with cracks, fissures and potentially sizable <br />caverns, which can collapse. <br />In some areas natural drainage occurs primarily <br />below ground rather than surface streams. These underground passages are commonly <br />connected to the surface by funnel- shaped depressions called sinkholes. The formation of these <br />sinkholes often leads to ground subsidence or collapse. This results from the settlement of <br />collapse of overlying materials into solution openings beneath the surface, such as caves or <br />enlarged joints. Sinkhole development is usually a slow process, however, they may occur <br />suddenly, without warning. <br />usually resulting in flooding and damage <br />Abandoned mines, mine shafts, and tunnels sometimes give way. Incidence of subsidence is <br />always a danger to property, dams, factories, and utility lines, but when sudden failures occur, <br />they can also threaten lives. <br />77 <br />