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  • 100 Jahre Bergsturz Sandling

    100 Jahre Bergsturz Sandling 100 years of the Sandling landslide 100 years ago, in September 1920, a massive landslide occurred in the West Face of Sandling. The so-called "Pulverhörndl", around 200 m high, which split off from the West Face of Sandling in a landslide in 1765, collapsed in September 1920. In May 1907 the summit was first climbed. Namely by the Ischl mountain guides Mathias Röchenbauer and Alois Wazinger. A cairn visible from afar at the summit testified to your first ascent. In the years that followed, the summit was climbed more often and the summit stone man soon gathered cards from the best Upper Austrian climbers. Der Sandlingturm, aufgenommen von Franz Maier, 1915. The west side of the Sandling summit with the Pulverhörndl in front of the landslide and the old scree heaps. In anticipation of the catastrophe, the builder, Weinzierl, had the pictured house of the alpine grass garden relocated to the foot of the Raschberg to the west of the stream. The western face of Sandling Peak after the landslide. On the far left, the seating area separates parts of the old scree heap from the new giant screed. About the geology: The Sandling has always been a troubled mountain . Namely, there is a high limestone on plastic Haselgebirge. And 1920 was a very wet, rainy year. This precipitation penetrated through the fissured and waterlogged limestone and marl and softened the underlying clayey layers. In addition, in the Ausseer salt mine in 1920 there were several "heavenly collapses", which destabilized the base of the rock masses of the "Pulverhörndl" just above. Beginning in the spring of 1920, salvos of rock pelted through the West Face of Sandling. Throughout the summer, much more frequently than usual, mighty boulders broke from the weathered rock and thundered down into the valley. Sandling rock stratification, Otto Lehmann 1926 The catastrophe: The sodden layers became this rainy summer literally squeezed out by the solid limestone marls and the limestone resting on them on the west wall. Then, on September 12, 1920, the unheard of happened . 20 people were still on the Vordersandlingalm. In the morning there was increasingly heavy rockfall from the west face, which was increasing constant noise. A climber who approached the summit from Altausse at 1 p.m. thought he heard train traffic, which surprised him because the railway lines were interrupted due to the heavy rain. The view down was already blocked by billowing clouds of dust. At about 4:30 p.m., even more violent boulder falls occurred, notably from the large rock pillars and pinnacles that towered between the Pulverhörndl and the face of the mountain. This was probably the time when the tower moved away from the wall, exposing the rocks wedged behind it. Cracks and faults became visible to the right of the tower, and the forest below slowly sank to the depths. At 5:30 p.m., a dairymaid noticed with horror that the Almboden was beginning to burst. Towards evening the mountain calmed down to some extent after most of the rocks between the Pulverhörndl and the wall had fallen down. Rock masses were no longer pressing on the back of the tower. But on the front, the pressure from the fallen rocks has increased considerably. The Pulverhörndl was now a bit shifted and isolated from the mountain up. But nobody took that as an opportunity to leave the Alm, only sleeping was out of the question. Around 11:00 p.m., a terrible roar began again, and a commotion was already felt in the ground. It was new moon and therefore pitch black, dust covered the pasture, lanterns could not illuminate anything. Now the fear was great: Valuables were hastily buried at the foot of the "Diebskögel" and the decision was made to leave the pasture and the cattle quickly. And not via the usual Almweg south along the Michelhallbach, but via the Raschberg to the Hütteneckalm. No one was harmed by this prudence! The Powder Tower collapsed on the night of September 13 with deafening thunder. Approx. 200,000 m3 of rock poured towards Michelhallbach. A large part of the overlying rock of the Sandlingalm was then torn down, creating a 400 m wide and 100 m deep shell-shaped crack. Incidentally, the entire Sandling was shaken, the entire western wall was speckled with light from stones that had broken out, and the trail through the western wall was then in a desolate condition. The Alm after the disaster: The four huts that were lifted and moved when the Almgrund was devastated. From the fourth by H. Joh. Reisenauer you can only see the ruins on the right in front. The "Diebskögerl" and the pressed and advanced Almgrund, which filled the meadow valley of the stream and leveled it. The objects (clothes and tools) buried at the foot of the "Diebskögerl" on September 12 were completely buried and have remained lost. The Mure: A huge debris flow moved down the valley. Only the southern part of the moraine mass, which had started to move, lost its connection and ended up as a mudflow. The upper, northern part was only loosened and sunk about 40 m deep into the trough created by the outflow of the Haselgebirge. On September 14th, a forest ranger from Bad Goisern, Paul Elsenwenger, was watching the debris flow from the foot of the Raschbergwand when the surrounding forest suddenly began to sway, the ground crunched, roots broke. He was only just able to save himself on the rocky valley wall! The Mure now filled the creek bed of the Michelhallbach and the large Zlambach for about 3.7 km and has dammed the spring streams that flow in on the east side to form two small lakes. 50 m / hour was the initial speed of the Murkopf and covered 2 km in the first 6 days. In the next 10 days he advanced another 1.2 km and in the next 15 days he came to a halt after a total of 3.7 km. View towards the southern part of the eastern tear-out niche. A shattered mound of lias marl covered with tree corpses. The rounded rock tower behind heralds the appearance of the Hallstatt limestone on the eastern slope. Tree corpses covered the debris flow. Reservoir at the mouth of a side stream. Just before it flows into the Zlambach, the Mure divided and an island was formed on which the handsome and spacious Leisling wooden room stood. This was dismantled in days of hard work and salvaged by hand. Witnesses of historical rockfall catastrophes can be found at the foot of the rock tower "Uh-sinnig Kira" (popular expression for "mad scream") at the Michelhallbach. Judging from archaeological excavations, there was already a rockfall accident there during Roman times (approx. in the 5th century AD) . There is historically reliable information about another catastrophe in the spring of 1546 , in which the surface facility of the small Michlhallbach salt mine was buried by a rock avalanche and claimed victims among the miners. The rock flow of 1920 also revealed evidence of this salt mine, namely a weak brine spring. It had been dyed red and exposed in several places. Literature: Company newspaper of the Austrian saltworks April 1928, Bergrat Ing. Hans Reinl The devastation in the Sandlin group, Otto Lehmann, 1926 Geological Map of the Republic of Austria Sheet 96 Bad Ischl, 2012 Mass movements in the hard-to-soft system and their anthropogenic influence, Weidinger JT, Spitzbart I. 2005 Vordersandlingalm 2020 Sandling West Face February 25, 2020 from a helicopter perspective by Raich Markus:

  • Blog | glueckauf

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  • Via Salis 2 | glueckauf

    Tour Reinfalz Tour Hinterrad Dark moments: Art objects salvage 1944/45 Moors, water, salt 100 years of the Sandling landslide Hutneck rack railway 450 years of salt pans 12 Johannesstollen 11 b main channel 11 a High water tunnel 11 Lipplesgraben - tunnel 13 Emperor Matthias – tunnels + iron ore 14 Neuberg-Stollen 15 Mitterberg-Stollen 18 Rabenbrunn tunnel 16 Old Steinberg tunnels 17 New Steinberg tunnels 19 Steinberg saw 10 Frauenholz – Stollen 8th Empress Amalia – Stollen 9 mountain church 7 Empress Elisabeth – Stollen 6 Empress Ludovika- Stollen 5 Emperor Joseph – Stollen 4 Empress Maria Theresa – Stollen 3a Rosa's waterfalls 3 Emperor Leopold – tunnels 2a strand 2 Emperor Franzens - Stollen 1 village square 20 Emperor Franz Josef – Erbstollen 25 pit locomotive 23 Perneck gypsum mining 24 strand 22 Antonius Dicklberger Strasse 21 Moosberg - Tunnel Village shop Perneck VIA SALIS Ways of salt A journey through time in the footsteps of the miners ​ More than 450 years ago, miners dug deep tunnels into the mountains in Bad Ischl. An adventurous journey for the whole family, for school classes and any other type of group excursion leads to where the men once fetched the salt from the mountain. Join us on a journey into the past! ​ Along the themed trail you will visit historical sites that were once used for the Salzkammergut were of great importance. Hinterradrunde Tour Hinterrad A 5.9 km loop trail passes the above stations and ends back at the starting point. ​ There can be total get to know ten tunnels. As retaining the mountain church, old miners' houses, the former Schaffer sawmill and other buildings and ruins. ​ Plan about 3 hours for the route. Good footwear is recommended. ​ station descriptions difficulty ​ Route ​ duration ​ rise ​ descent ​ accessible by bus easy ​ 5.9 km ​ 3 hours ​ 360 m ​ 360 m ​ ​ elevation profile Reinfalzrunde Tour Reinfalz A 10.2 km loop trail passes the above stations and ends back at the starting point. ​ 16 tunnel systems of the Pernecker and Lauffner salt storage can be visited. As retaining the mountain church, old miners' houses, the former Schaffer saw, rock carvings and other buildings and ruins. Even older traces of mining can be found near the Matthias tunnel, namely the so-called Eisenarz, where iron ore and vitriol were extracted until 1563. ​ Plan about 4.5 hours for the route. Good footwear is recommended. ​ station descriptions medium ​ 10.2 km ​ 4.5 hrs ​ 660 m ​ 660 m ​ ​ difficulty ​ Route ​ duration ​ rise ​ descent ​ accessible by bus elevation profile Ways to us: Are you interested in a guided tour? Registration by phone or email ​ 067761168967 Horst Feichtinger horst.feichtinger@gmx.at

  • viasalis Bad Ischl

    experience history Via Salis ways of salt Salt has been mined in Bad Ischl since 1563. Historical tunnel entrances, the mountain church, miners' houses, the former Schaffersag and other localities can on Via Salis be visited.... Continue reading Bad Ischl and the salt The blessing of the coveted mineral salt lay over the entire Salzkammergut. Hence the name, which is made up of the words Kammergut and Salz... Continue reading IGM Interest group Mitterbergstollen Between 2013 and 2018, the "Interessengemeinschaft Mitterbergstollen" ( IGM ) restored a total of 12 tunnel portals at considerable expense... Continue reading NEWS Project: Saving the historic saw at the Maria Theresia tunnel No posts published in this language yet Once posts are published, you’ll see them here.

  • Forum | glueckauf

    To see this working, head to your live site. Categories All Posts My Posts Login / Sign up Create New Post Neuigkeiten, Bilder,... Follow Views Posts 39 Führungen Follow Views Posts 6 Bilder, Kommentare, Wünsche, Kritik,.... New Posts Franz Kranabitl May 31 Arbeiten bei der alten Bergsäge: Neuigkeiten, Bilder,... Sogar Kranabitl Rudolf Sen. hilft tatkräftig mit: Like 0 comments 0 Franz Kranabitl May 24 Kulturehrenurkunde für IGM Neuigkeiten, Bilder,... Like 0 comments 0 Franz Kranabitl Apr 09 Schächte Neuigkeiten, Bilder,... Schächte sind von der Erdoberfläche (vom Tage) oder auch von anderen Grubenbauen seiger oder fast seiger (senkrecht oder stark geneigt) ausgehende bergmännische Einbaue, die ins Innere des Gebirges niedergehen und eine Lagerstätte von ober Tage aus erschließen oder zwei oder mehre Sohlen miteinander verbinden. Schächte wurden im alpinen Salzbergbau seit jeher für verschiedene Zwecke, wie zur Fahrung (Begehung), Förderung, Wetterführung oder der Wasser Zu‐ und Ableitung, errichtet. Details zu Schächte Like 0 comments 0 Forum - Frameless

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