Titlebook: Quantitative Parameterization and 3D‐run‐out Modelling of Rockfalls at Steep Limestone Cliffs in the; Bettina Sellmeier Book 2015 Springer

Heart-Attack

Book 2015ain objective was to cover not only low-magnitude, high-frequency rockfalls (<10 m.3.) but also Mid-Magnitude events, which involve rock volumes of between 10 and 100 m.3. (boulder falls) and between 100 and 10,000 m.3. (block falls). As Mid-Magnitude events have been insufficiently covered in terms

scrutiny

Nostalgia

Glossy

Methodology,ed consideration of the degree of fragmentation of the block itself and of the surrounding rock mass. Due to the subsequent stability analysis of the whole block the joint persistence was recorded in detail from the out- and inside. Based on the field data a 3D-visualization of the block was develop

小畫像

Results,rock failure at the Wachterl-Horn (Sect. 5.1). Section?5.2 illustrates the results of discontinuity analysis and the quantitative magnitude assessment and the third part will refer to the implementation of the magnitude information into 3D-rockfall simulations (Sect.?5.3).

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BLA

Trochlea

Study Site, project site extends at the east (right) valley side. The terrain can be characterized as a steep and densely forested limestone slope with two extensive cliffs in two altitude levels in the middle and upper slope, providing the majority of the rockfall material. The cliff faces dip with an angle of 50°–90° in west direction.

Genteel

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