{"id":9214,"date":"2025-08-23T18:13:10","date_gmt":"2025-08-23T16:13:10","guid":{"rendered":"https:\/\/test.destination-montagne.ch\/?p=9214"},"modified":"2025-09-20T16:15:33","modified_gmt":"2025-09-20T14:15:33","slug":"aux-simmefall","status":"publish","type":"post","link":"https:\/\/test.destination-montagne.ch\/de\/aux-simmefall\/","title":{"rendered":"Zu den Simmef\u00e4ll"},"content":{"rendered":"\t\t
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Le fond de la haute vall\u00e9e de la Simme pr\u00e9sente la caract\u00e9ristique de beaucoup de vall\u00e9es de montagne\u00a0: un fond plat. Ce fond plat provient du fait que la vall\u00e9e a \u00e9t\u00e9 au cours du temps remplie par des alluvions. Ce n\u2019est que lorsque l\u2019on rejoint le fond du cirque fermant le fond de la vall\u00e9e que le paysage change du tout au tout. On se trouve alors en face d\u2019accident de terrain assez important. C\u2019est par-dessus un de ces ressauts que se trouvent les cascades de la Simme (Simmef\u00e4ll). Les cascades que nous connaissons actuellement sont le r\u00e9sultat d\u2019am\u00e9nagements effectu\u00e9s au 17\u00e8me<\/sup> si\u00e8cle dont le but \u00e9tait de limiter l\u2019importance des crues. C\u2019est durant ces am\u00e9nagements que la roche a \u00e9t\u00e9 taill\u00e9e afin d\u2019offrir au torrent un passage diff\u00e9rent de l\u2019original.<\/p>

Depuis le bout de la vall\u00e9e, deux sentiers sont possibles. Mais il est avantageux de suivre celui qui longe la cascade au plus pr\u00e8s. On subit alors des embruns assez forts par endroits. Plus haut, \u00e0 la Barbarabr\u00fccke, on se fait copieusement asperger. Apr\u00e8s le pont, on retrouve l\u2019autre cheminement, qui suit alors un chemin carrossable assez raide par endroits. Apr\u00e8s avoir rejoint une zone bien plus plate, on ne tarde pas d\u2019atteindre la buvette d\u2019alpage du Rezlisb\u00e4rgli. Il vaut alors la peine d\u2019aller voir les Sibe Br\u00fcnne (les sept fontaines), o\u00f9 l\u2019eau ressort directement de la paroi de rochers.<\/p>

Apr\u00e8s cet endroit, on poursuit encore un moment dans une cuvette relativement plate, avant de monter franchement en direction de Langermatte. Cet endroit, o\u00f9 se trouve \u00e9galement une buvette d\u2019altitude, se trouve sur une croupe domin\u00e9e par le Firstli, une raide ar\u00eate qui \u00e9tait emprunt\u00e9e par une des variantes du Col du Rawyl.<\/p>

Il suffit alors de descendre en direction de l\u2019Iffigbach pour rejoindre l\u2019Iffigenalp. La descente depuis Langermatte est raide par endroit, mais le sentier est bon, et on perd rapidement en hauteur. Iffigenalp se trouve \u00e0 la crois\u00e9e des sentiers menant d\u2019une part au Rawylpass et d\u2019autre part au Schnidejoch, autre alternative pour franchir la cha\u00eene de montagne.<\/p>

Itin\u00e9raire\u00a0: Lenk (gare) \u2013 Simmef\u00e4ll \u2013 Rezlisb\u00e4rgli \u2013 Langermatte \u2013 Iffigenalp
Distance : 13,7Km
D\u00e9nivellation : 920m
Dur\u00e9e : 5h<\/p>

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Der Talboden des oberen Simmetals zeigt die f\u00fcr viele Bergt\u00e4ler typische Eigenschaft: einen flachen Talboden. Dieser entstand dadurch, dass das Tal im Laufe der Zeit mit Schutt aufgef\u00fcllt wurde. Erst wenn man den Talschluss erreicht, \u00e4ndert sich das Landschaftsbild v\u00f6llig. Man steht dann vor einem recht grossen Gel\u00e4ndesprung. \u00dcber einen solchen Sprung befinden sich die […]<\/p>\n","protected":false},"author":1,"featured_media":9221,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_et_pb_use_builder":"","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":"","_wp_rev_ctl_limit":""},"categories":[507,197],"tags":[1087,1086,1083,1084,1085,1082],"class_list":["post-9214","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-alpes-bernoises","category-randonee","tag-iffigenalp","tag-langermatte","tag-lenk","tag-rezlisbarg","tag-sibe-brunnen","tag-simmefall"],"yoast_head":"\nZu den Simmef\u00e4ll - Destination Montagne<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/test.destination-montagne.ch\/de\/aux-simmefall\/\" \/>\n<meta property=\"og:locale\" content=\"de_DE\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Zu den Simmef\u00e4ll - Destination Montagne\" \/>\n<meta property=\"og:description\" content=\"Der Talboden des oberen Simmetals zeigt die f\u00fcr viele Bergt\u00e4ler typische Eigenschaft: einen flachen Talboden. Dieser entstand dadurch, dass das Tal im Laufe der Zeit mit Schutt aufgef\u00fcllt wurde. Erst wenn man den Talschluss erreicht, \u00e4ndert sich das Landschaftsbild v\u00f6llig. 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