ABSTRACT

A detailed geomorphological map of the Mt. Babia Góra Massif (1725 m a.s.l.), at a scale 1:10,000 is presented. A slope, glacial, periglacial and fluvial features were mapped on the base of the coupled field studies and LiDAR DEM analyses. This study underlines the complexity of rock slope failures (RSFs), in shaping the morphology of compact and isolated upland, exhibiting one of the highest incidences of RSFs yet recorded in Europe (29% for a whole massif, and 45% for the north face). A total of 212 RSFs were mapped of which 18 failures are large landslides (>0.25 km²), among them is one of the largest known (2.6 km² and 150 × 106 m³) in the Polish Flysch Carpathians. The mapping and Schmidt-hammer results shed light on the problem of glacial relief of the massif, documenting the remnants of glacial deposits beyond the tongues of landslides in the Szumiąca Woda valley.

摘要

山的详细地貌图。呈现了比例为1：10,000的BabiaGóraMassif（1725 m asl）。在耦合野外研究和LiDAR DEM分析的基础上，绘制了斜坡，冰川，周缘和河流特征。这项研究强调了岩石边坡破坏（RSF）的复杂性，在塑造紧凑而孤立的高地形态时，显示出欧洲有史以来RSF发生率最高的事件之一（整个断层发生率为29％，北壁为45％） ）。总共绘制了212个RSF，其中18个是大型滑坡（> 0.25 km ²），其中是最大的滑坡之一（2.6 km ²和150×106 m ^3）。）在波兰的Flysch喀尔巴阡山脉。测绘结果和施密特-哈默（Schmidt-hammer）结果揭示了断层的冰川融化问题，记录了SzumiącaWoda山谷滑坡舌头以外的冰川沉积物残留。