giftsight.blogg.se - Geology abandoned meander

Meandering is a natural operation of streams of all sizes flowing across fine-grained sediments. The house suffered flooding in 1997 and was razed shortly thereafter. As the slope progressively failed, the house began to incline toward the river. Terrace Street in Fargo bordered on a shallow meander loop of the Red River. The backward tilt of this small house on N.

The actions of man (removing stabilizing vegetation, adding load on top of the slope, introducing water on and into the affected areas, etc.).

Water levels in the Red River (higher water levels tend to induce a positive pressure against the river bank, slowing the movement of earth materials channelward).

Soil moisture conditions (rates have increased dramatically since 1993, when the "late 1980's" drought ended).

Aside from the rate of erosional processes induced by the river, they are also tied to: Rates of slope retreat are difficult to predict. Yet residential development in the Fargo-Moorhead region continues on these vulnerable land surfaces. Lands bordering the outside margins of meander loops are inheritantly unstable. Note proximity of some housing to vulnerable slopes on outsides of meanders. New housing along Red River in south Fargo. Many of the parklands of eastern Fargo (Mickelson Field, "Elephant" Park, Trollwood Park, El Zagal Golf Course, Lindenwood Park, etc.) are developed on abandoned meander loops of the Red River: evidence of this river's past dynamic history of an ever-shifting channel. As erosion progresses, cutbank slopes become unstable under gravity and susceptible to mass wasting. The river channel shifts over time in a direction toward the outside of the meander loop. The erosional cliff (cutbank) retreats by erosion and mass wasting, shifting the channel in a direction toward the outside of the meander. With the river ever cutting toward the outside edges of its meanders, the channel over time shifts in position. After witnessing decades of futile projects involving channel straightening, most geologists and engineers appreciate that a river has a need to meander. The development of meanders is a natural operation of such rivers.

Along such areas, the emplacement of any weight (house, dike, walls, or even the simple watering of a lawn) only tends to exacerbate the rate of slope failure. While these areas may present desirable views onto the river, they are also prone to failure and mass wasting. Thus, the outside of a meander generally represents a region of active erosion, where cliffs or cutbanks develop. The zone of highest velocity (red dot on cross-section) is diverted toward the outside of the meander. Map and cross-sectional views of a typical meander loop on the Red River. With this diversion of velocity is a diversion of the higher stream energy: the outside edges of meander loops typically represent regions of active stream erosion. The higher velocity of river waters passing through a meander tends to be diverted toward the "outside" of the meander loop. Due to its extensive meander belt, the Red River's path northward from Wahpeton to Pembina is about twice as long as a straight-lined path. Such is the case, of course, with the Red River of the North.

Rivers that flow across unconsolidated, fine-grained sediments tend to meander. Where these weak sediments are exposed "on edge" (for example, in a highway cut or along the channel of the Red River or its tributaries), they are susceptible to failure. The Red River Valley is underlain by a thick wedge of fine-grained sediments, whose engineering strengths are exceptionally low. But they represent precarious locations for development. Note the cutbank on the outside of the meander. Meander loop on Red River in north Fargo. Mass Wasting in the Fargo, North Dakota, Region: Problem Overview NORTH DAKOTA STATE UNIVERSITY