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Cirque du Fer-à-Cheval with 2nd from the right the mountain peak Corne du Chamois (Chamois Horns)
Camera brand and type used to take photo
NIKON Z 9
Lens used
NIKKOR Z 14-24mm f/2.8 S @ 14 mm
NIKON Z 9
Lens used
NIKKOR Z 14-24mm f/2.8 S @ 14 mm
Aperture used
f/11.0
Exposure used
1/80 s
Exposure compensation applied
0.0 EV
ISO used
64
f/11.0
Exposure used
1/80 s
Exposure compensation applied
0.0 EV
ISO used
64
Copyright © 2025 Jan-Willem Kruse (www.fotokruse.eu).
All rights reserved. For consideration only, no reproduction without prior permission.
All rights reserved. For consideration only, no reproduction without prior permission.
Photo Info
FGK-Z9-0156a-.jpg
8256*5504
(50860 KB)
1462x visited
Description
Headline
Cirque du Fer-à-Cheval with 2nd from the right the mountain peak Corne du Chamois (Chamois Horns)
Caption
From left to right; Chalet d'Accueil du Fer à Cheval providing tourist information, Le Chalet de Laura for food and 2nd from the right the mountain peak Corne du Chamois (Chamois Horns, 2523m) rising above the Giffre valley at Cirque du Fer à Cheval.
The Cirque du Fer-à-Cheval is a large cirque in the Giffre Massif in the French Prealps near the village of Sixt-Fer-à-Chevalat. This natural cirque lies at the end of the Giffre River valley (Vallée du Giffre) and has cliffs ranging from 500 to 700 meters in height. The cirque is surrounded by peaks reaching almost 3000 meters.
The Cirque du Fer-à-Cheval takes its name from the shape of its cliffs, which form a semicircle. Its impressive height (2000 m). The site comprises two parts: the Cirque du Fer-à-Cheval and the Fond de la Combe. The two are separated by the protrusion of the Pic de Tenneverge (2836 m) and its extension, the Cornes du Chamois (2523 m).
The rocks forming this Horseshoe Massif are limestones formed during the Jurassic period (199 to 145 million years ago). During the uplift of the Alps, from 50 MA, these rock masses were pushed towards the west and were strongly folded (some rocks multiple times).
In the cirque, around thirty waterfalls tumble from the cliffs in the spring when the snow melts. During the summer, eleven waterfalls remain. At the bottom of the valley, the Bout du Monde also has a good ten waterfalls.
The Cirque du Fer-à-Cheval is a large cirque in the Giffre Massif in the French Prealps near the village of Sixt-Fer-à-Chevalat. This natural cirque lies at the end of the Giffre River valley (Vallée du Giffre) and has cliffs ranging from 500 to 700 meters in height. The cirque is surrounded by peaks reaching almost 3000 meters.
The Cirque du Fer-à-Cheval takes its name from the shape of its cliffs, which form a semicircle. Its impressive height (2000 m). The site comprises two parts: the Cirque du Fer-à-Cheval and the Fond de la Combe. The two are separated by the protrusion of the Pic de Tenneverge (2836 m) and its extension, the Cornes du Chamois (2523 m).
The rocks forming this Horseshoe Massif are limestones formed during the Jurassic period (199 to 145 million years ago). During the uplift of the Alps, from 50 MA, these rock masses were pushed towards the west and were strongly folded (some rocks multiple times).
In the cirque, around thirty waterfalls tumble from the cliffs in the spring when the snow melts. During the summer, eleven waterfalls remain. At the bottom of the valley, the Bout du Monde also has a good ten waterfalls.
Image Alt text
Mountain peak Corne du Chamois (Chamois Horns) rising high from the green meadow at Cirque du Fer à Cheval
Event
Holiday 2025 - Le Mont (Sixt-Fer-à-Cheval, France)
Keywords
Capture info
(IPTC Instructions)
(IPTC Instructions)
-
Location
Location
- - - -
Altitude
985 meter
Properties
Original filename
Z9-0156a.NEF
Taken on
9-Aug-2025 11:22:34
Digital Source
Digital camera
Posted first on
27-Dec-2025 22:10:00
Update posted on
19-Feb-2026 22:33:19
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Adobe Lightroom
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Copyright
Credit line
Copyright © 2025 Jan-Willem Kruse (www.fotokruse.eu)
Copyright
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Copyright Notice
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Photographer
Jan-Willem Kruse
Other Info
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