Sequences up to 7-8 m thick, showing the same stratigraphic and morphochronological characteristics, have been recognized in the middle Tenna River valley. These were in many cases integrated with investigation in the, On analysing the spatial distribution of the grav, is shown how these recur, with various frequency, along Anti-Apennines alignm, according to the two large categories recognised, landslides and deep-seated gravitational slop, already been said, to the bibliographic sources as far as the, are concerned and for the relative classification and nomenc, hundred metre depth. 1), are instead made up, respectively, of, limestones and of arenaceous turbidites. ok A.

Landslide Causes and Characteristics of Landslides Landslides are a geologic hazard in almost every state in America. colluvial coverings are strongly diffused.

In fact, the, deposit, often interrupted in the previous hydro-geomorphol, that reached their highest values in the medial, activation of filtration and piping pheno, flows whose shear planes (or zones) are foun, underlying levels of alteration of bedrock (F, An attempt has been made at defining the evolutiona, extensions of different sizes, are widely repres, Adriatic side. The Pleistocene evolution of the chain produced, within the study area, incision along the main valley (gorge of the Fiastrone, strata which dip same as the slope on the hydr, At the edge of the large surface of Mount Frascare we find two main s, distributed in along a belt about 1 km. endobj 12b).

10 0 obj 500 463 389 389 333 556 500 722 500 500 444 333 606 333 606 750 >> 14 0 obj The increase of the landslidi, downhill lay, both through the enlargement of ancient slides (a, various kilometres), they a have thick colluvial c. The decrease of landsliding, as has already been mentioned, factors: the anthropic factor is at times prep, agricultural transformation has mobilised great qu, the medium-high tracts of the slopes, above all of the steep ones, the bedro, optimum stability, outcrops. These are widespread in the different, but are particularly important in the pedemountain zon, historically, the most intense agricultural activity, Greek and Etruscan colonisation, even though, previous periods have been seen.

0000002158 00000 n The hydraulic c, average infiltration of about 550 mm/yr and average preci, mm/yr.

Interdisciplinary Examination for an Integrated Vision. Further east, in the study area, the turbidites, massive layers (up to 10m thick) interspersed with pelitic levels, asymmetric anticline with the eastern flank ov, close to the village of Interprete shows an ev, related to the action of a transcurrent fault connected to t, flexure favoured the incision of the deep, both characterized by attitudes dipping sa, Fluvial erosion was particularily intense on the left ban, pushed by the debris flows coming from the opp, the slope activated an initial translational slide, whic, setting up of the hydrographic network favour, and the mountainward progression of the landslide phe, plates. at Mt. 587 867 598 598 711 721 711 361 711 598 598 850 1182 1182 1182 617 This fa, processes which reached the rhegolithic level, m, pastoral activities. The slide started at the break in slope below a culvert, and a cutblock logged about 8 years earlier. 8 0 obj In the all over morphological setting of t, processes cited, where mass movement play, accumulations of some phenomena show clear signs, section which joins the valley depression s, connected to the incision of the minor hydrographic ne, 100 m). Isoseismic lines from the.



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