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 24-120mm f/4 S @ 24 mm
Aperture used
f/8.0
Exposure used
1/100 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.
Foto Info
B_Z9-0165a.jpg
1667*2500
(1898 KB)
626x bezocht
Description
Titel
Cirque du Fer-à-Cheval with 2nd from the right the mountain peak Corne du Chamois (Chamois Horns)
Beschrijving
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 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 with horse riders in the foreground
Gebeurtenis
Holiday 2025 - Le Mont (Sixt-Fer-à-Cheval, France)
Kernwoorden
00 OTHER
10 FAMILIE
_FRANKRIJK 2025
Auvergne-Rhône-Alpes
Cirque du Fer-à-Cheval
Corne du Chamois
EN: Chamois Horns
EN: Giffre valley
EN: Horseshoe Circus
Equus caballus
France
GEZIN
Haute-Savoie
hiker
hiking
horse
horseriding
livestock
mountain
mountain peak
pine tree
system-favorite
tree
unknown people
Vallée du Giffre
Wilma Kruse
Capture info
(IPTC Instructions)
(IPTC Instructions)
-
Location
Locatie
- - - -
Altitude
947 meter
Properties
Originele bestandsnaam
Z9-0165a.NEF
Gefotografeerd op
9-Aug-2025 11:39:38
Digitale bron
Digital camera
Posted first on
22-Feb-2026 23:46:32
Update posted on
22-Feb-2026 23:46:38
Rating/label
Adobe Lightroom
Adobe Lightroom
Label and rating as set in Adobe Lightroom
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Copyright © 2025 Jan-Willem Kruse (www.fotokruse.eu)
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Fotograaf
Jan-Willem Kruse
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