Monte Ferra
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Mount Ferra (3094 m) is a
mountain A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher t ...
in the
Cottian Alps The Cottian Alps (; ; ) are a mountain range in the southwestern part of the Alps. They form the border between France (Hautes-Alpes and Savoie) and Italy (Piedmont). The Fréjus Road Tunnel and Fréjus Rail Tunnel between Modane and Susa, Ital ...
, rising in
Italian Italian(s) may refer to: * Anything of, from, or related to the people of Italy over the centuries ** Italians, a Romance ethnic group related to or simply a citizen of the Italian Republic or Italian Kingdom ** Italian language, a Romance languag ...
territory in the upper
Varaita Valley Varaita Valley (in Italian ''Valle Varaita'') is a valley in south-west of Piedmont, in the Province of Cuneo - Italy. Etymology It takes its name from the Varaita, a right-hand tributary of the Po which flows through the valley. Geography Clos ...
, in the
province of Cuneo The province of Cuneo (; ) is a province in the Piedmont region of Italy. To the west, it borders the French region of Provence-Alpes-Côte d'Azur ( departments of Alpes-Maritimes, Alpes-de-Haute-Provence and Hautes-Alpes), to the north the ...
, between the towns of Bellino and
Pontechianale Pontechianale is a ''comune'' (municipality) in the Province of Cuneo in the Italy, Italian region Piedmont, located about southwest of Turin and about northwest of Cuneo, on the border with France. Pontechianale borders the following municipal ...
.


Features

It lies on the ridge separating the Fiutrusa valley to the north from the Bellino Varaita valley to the south. This ridge breaks away from the main alpine watershed at Mt. Salza, and descends in a south-southeast direction to the Fiutrusa Pass (2858 m); from there it ascends in a southeast direction to the Fiutrusa Peak (3068 m). From this point, it makes an arc with the concavity to the southwest, first heading approximately eastward to elevation 3048, then southeast and south-southeast to the summit of Mount Ferra. From there the ridge makes a second, similar arc, which takes it in an east then southeast trend first to elevation 2992, from where it straightens out and proceeds in an east-northeast trend to the Bondormir pass (2651 m) and elevation 2753, where it bends southeast to reach Mount Pietralunga.Cf. cartography Three lateral ridges branch off from this ridge, all with a direction approximately NE-SW. The first is detached from the tip of Fiutrusa, and descends into the Rui valley, separating its upper part from the suspended valley of Vallonetto; the second descends from Mount Ferra toward Mount la Vigna (2935 m) and Mount la Pertia (2820 m), and separates Vallonetto from Cialancia, another suspended valley where Lake Reisassa is located, whose outlet, the Reisassa stream, descends into the upper Bellino valley just downstream from the hamlet of Sant'Anna. The third ridge, called Roccia Ferra, descends from elevation 2992 in a more south-southwesterly direction, separating the Cialancia from the Comba di Rocca Ferra, closed at its summit by the Colle del Bondormir. The two main slopes of the mountain have a very different appearance. The northern slope precipitates over the Fiutrusa valley with steep, precipitous rock faces, clearly visible from
Pontechianale Pontechianale is a ''comune'' (municipality) in the Province of Cuneo in the Italy, Italian region Piedmont, located about southwest of Turin and about northwest of Cuneo, on the border with France. Pontechianale borders the following municipal ...
, while to the south are fairly uniform scree slopes.Giulio Berutto, ''Monviso e le sue valli - Vol. 1 - II edizione'', Istituto Geografico Centrale, Torino, 1997; pagg.109-110 Geologically, the mountain belongs to the
Permo-Carboniferous The Permo-Carboniferous is the time period including the latter parts of the Carboniferous and early part of the Permian period. Permo-Carboniferous rocks are in places not differentiated because of the presence of transitional fossils, and also w ...
of
Sampeyre Sampeyre is a ''comune'' (municipality) in the Province of Cuneo in the Italian region Piedmont, located about southwest of Turin and about northwest of Cuneo. Sampeyre borders the following municipalities: Brossasco, Casteldelfino, Elva, Fra ...
, and is composed essentially of conglomeratic
quartzites Quartzite is a hard, non- foliated metamorphic rock that was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectoni ...
interbedded with mica schists and by sericitic
schists Schist ( ) is a medium-grained metamorphic rock generally derived from fine-grained sedimentary rock, like shale. It shows pronounced ''schistosity'' (named for the rock). This means that the rock is composed of mineral grains easily seen with a ...
, both formations dating back to the
Permian The Permian ( ) is a geologic period and System (stratigraphy), stratigraphic system which spans 47 million years, from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.902 Mya. It is the s ...
. The area is affected by a number of faults with a general north-south trend, with a slightly concave trace to the west; to the east of the easternmost of these faults, toward the Bondormir pass and below the walls of the Fiutrusa valley, the
Jurassic The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately 143.1 Mya. ...
-
Cretaceous The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ...
ophiolitiferous calcareous schists of the Gastaldi greenstone complex emerge.Carta Geologica d'Italia scala 1:100.000 - foglio 78-79 - Argentera-Dronero


Ascension to the summit

The
normal route A normal route or normal way (; ) is the most frequently used climbing route for ascending and descending a given mountain peak; it is usually the easiest and often the most straightforward route. Other generic names include the ''Tourism, tourist ...
is spread over the southern slope, where the homogeneous hillside allows relatively easy access. The typical route runs from the valley of the Reisassa stream and the Cialancia; starting from Sant'Anna di Bellino, one follows first trail U65, then an unnumbered path that leads to Reisassa Lake, at the foot of the peak. One climbs the scree slope with a free path, encountering at one point a trail that leads up to the summit. The route is a
hiking trail A hike is a long, vigorous walk, usually on trails or footpaths in the countryside. Walking for pleasure developed in Europe during the eighteenth century. Long hikes as part of a religious pilgrimage have existed for a much longer time. " ...
, with difficulty rated as EE.gulliver.it - via normale al monte Ferra
The same route can be done in winter with
snowshoes Snowshoes are specialized outdoor gear for walking over snow. Their large footprint spreads the user's weight out and allows them to travel largely on top of rather than through snow. Adjustable bindings attach them to appropriate winter footw ...
or
skis Skis are runners, attached to the user's feet, designed to glide over snow. Typically employed in pairs, skis are attached to ski boots with ski bindings, with either a free, lockable, or partially secured heel. For climbing slopes, ski skins can ...
.gulliver.it - ascensione invernale con gli sci
G. Berutto, ''op. cit.'', pag.274


Mountaineering routes

Mount Ferra has some interesting
mountaineering Mountaineering, mountain climbing, or alpinism is a set of outdoor activities that involves ascending mountains. Mountaineering-related activities include traditional outdoor climbing, skiing, and traversing via ferratas that have become mounta ...
routes, particularly in winter, when ice climbing is possible. One of these routes is the Y-shaped
couloir A couloir (, "passage" or "corridor") is a narrow gully with a steep gradient in a mountainous terrain.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, p. 121. . Geology A couloir may be a seam, scar, or fissure, o ...
on the NE buttress, which can be reached by ascending the Fiutrusa valley from
Pontechianale Pontechianale is a ''comune'' (municipality) in the Province of Cuneo in the Italy, Italian region Piedmont, located about southwest of Turin and about northwest of Cuneo, on the border with France. Pontechianale borders the following municipal ...
; it is a classic ice climb, with a difficulty rating of D. A real icefall, on the other hand, is the Grassi-Tessera
gully A gully is a landform A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). Landforms together make up a given ter ...
, which can be reached by ascending from Sant'Anna di Bellino to the Bondormir pass. It is a 6-rope length icefall, with long 80° sections and a vertical section in the first pitch, first climbed by Gian Carlo Grassi.


See also

*
Varaita Valley Varaita Valley (in Italian ''Valle Varaita'') is a valley in south-west of Piedmont, in the Province of Cuneo - Italy. Etymology It takes its name from the Varaita, a right-hand tributary of the Po which flows through the valley. Geography Clos ...


References


Bibliography

;Cartography * Official Italian cartography of the
Istituto Geografico Militare The ''Istituto Geografico Militare'' (IGM), or Military Geographic Institute, is an Italian public organization, dependent on the Italian Army general staff (''Stato Maggiore dell'Esercito''). It is the national mapping agency for Italy.
(IGM) at a scale of 1:25,000 and 1:100,000
available online

Sistema Informativo Territoriale della provincia di Cuneo
on a 1:10,000 cartographic base * Istituto Geografico Centrale - Trail map 1:50,000 no. 6 "''Monviso''" and no. 106 "''Monviso-Sampeyre-Bobbio Pellice''" {{DEFAULTSORT:Ferra Three-thousanders of Italy Mountains of Italy Mountains of Piedmont Province of Cuneo