[7] N atu re Park Rieserferner-A hrn/Vedrette di Ries

Nature Park Rieserferner-Ahrn/Vedrette di Ries-Aurina
[7]
South Tyrol Nature Parks
Rieserferner-Ahrn/
Vedrette di Ries-Aurina
Nature Park
The boundaries of nature
and the limits of man
© 2015
Nature, Landscape
and Planning Department
Nature Park Office
AUTONOME PROVINZ BOZEN - SÜDTIROL
Abteilung Natur, Landschaft und Raumentwicklung
Cover image
Hochgall
Photo: Leo Unterholzner
The boundaries of nature and the limits of man
Geology and minerals
Going from the Dolomites to the north side of the Puster Valley
entails more than simply crossing over a valley – it involves
crossing over one of the most prominent geological seams in
Europe: the so-called Periadriatic Seam separates the Eastern Alps
from the Southern Alps.
These extremely different rock units were fused together
along this line about 30 million years ago by the Alpide orogeny
­mountain-building event. Thus today the sedimentary rocks
of the Dolomites abut the schists and gneisses of the crystalline
basement. While the Alpide orogeny simply folded and moved
the sedimentary rocks causing little or no mineralogical change,
the rocks of the crystalline basement underwent a profound
transformation (metamorphosis).
The collision of the Southern Alps and the Eastern Alps is a
lengthy process that began some 100 million years ago and
­continues to this day. Roughly speaking, it pushed the Apulian
plate up against the southern edge of the European continent.
The thrust direction has changed several times during the
­process, and short distension periods have also been documented. During one of these distension periods some 30 million
years ago, magma came up out of the earth’s crust along the
Periadriatic Seam and along a fault zone lying a little to the north.
The molten rock crystallized about nine kilometers deep in the
crust and formed the so-called Rieserferner/Vedrette di Ries
Pluton. The rising and erosion of the mountains slowly brought
Fig. 1
A flowering wonder
on the edge of the ice:
the delicate alpine
rock-jasmine is a typical
cushion plant. The form
of these plants protects
them from dying of
dehydration or cold.
The parts of the plant
that die decompose
directly into the
cushion and thus
supply the plant with
nutrients. Nothing is
wasted.
Photo: Leo Unterholzner
Fig. 2
The Tristennöckl above
the Kasseler Hütte/
Rifugio Roma alpine
hut is a “forest above
the tree line”. It is a
Natural Monument.
Rittner Straße 4
39100 Bozen
Ph. +39 0471 417 770
Fax +39 0471 417 789
[email protected]
www.provinz.bz.it/naturparke
PROVINCIA AUTONOMA DI BOLZANO - ALTO ADIGE
Ripartizione Natura, paesaggio e sviluppo del territorio
The lower schistose covering is located on top of the central
gneisses and the old roof. This “shell” consists of various layers of
sediment that originally lay next to each other and, through the
Alpide orogeny events, were stacked and compressed into tight
folds. The original sedimentary rocks have now become an array
of quartzites, mica schists, marbles and powerful calcareous mica
schists.
The upper schistose covering (also known as the Glockner
nappe) consists mostly of deposits from the edge and the
­deep-sea floor of the Pennine Ocean. These powerful calcareous
mica schists with inclusions of quartzites and graphite schists
are also referred to as Bündner slate. There are also thick inter­
layers of green ophiolite, which were formerly the basalts of the
ocean floor. The copper deposits in these rocks were mined in
the Prettau/Predoi mine for centuries up until modern times.
Today, the mine has been turned into a museum and climate
gallery.
The Tauern window is known for the large and well-formed
crystals found in the so-called Alpine chasms. These chasms
formed during the last orogeny uplift phase of the Tauern window: between the plastic and structural deformation, the hard
rocks were particularly under such strain that cracks and wide
fissures formed, into which mineral solutions flowed with enough
space to crystallize. Thus were formed, mainly in the central
gneiss and green ophiolites, beautiful crystals of quartz, smoky
quartz and amethyst, to name just a few.
the plutonic rock tonalite to the earth’s surface. This is how the
Rieserferner/Vedrette di Ries Group was formed.
The exceptionally bold and rugged peaks of the Rieserferner/
Vedrette di Ries Group (somewhat unusual in the Eastern Alps) are
not due solely to hardness of the tonalite – an igneous rock
similar to granite-, but also to the fact that these rocks, which are
“only” 30-million years old, are some of the youngest geological
formations in South Tyrol.
Eastern Alpine crystalline basement rock units surround, and
often extend over the mass of tonalite. These rocks are more than
500-million years old and have experienced at least two mountain-building events. During these orogeny events the multiple
transformations of schists, gneisses, amphibolites and marbles were
folded by pressure and heat, intensively “kneaded” and recrystallized.
Geologists estimate that the Alps will continue to rise for
another 20 million years. The High Tauern will thus attain a height
of 25,000 meters in theory. Erosion does, however, ensure that the
mountains will not rise much higher. At present, the uplift and
erosion are roughly in balance.
In the glacial regions one finds only scant traces of life and
here man is at his limit. Along with the Hohe Tauern National Park
and the Zillertaler Alps Nature Park, the Rieserferner-Ahrn/­
Vedrette di Ries-Aurina Nature Park has a European dimension.
Photo: Peter Schreiner
The Tauern Window
The Tauern window extends in a narrow strip along the main
ridge of the Alps from Brenner/Brennero to the Katschberg Pass
160 kilometers to the east. It provides a glimpse of those rocks
which lie under the mighty rock strata of the Eastern Alps and
have been brought to the surface here by the ­extreme lifting and
erosion of the mountains. It is estimated that the southern edge
of the European continent formed of the abraded remains of the
Pennine Ocean floor only became visible about ten million years
ago, following massive erosion of the Eastern Alps.
Geologically speaking, the Tauern window forms an elongated
dome, which consists of several shells. Just as with a sliced ​​onion,
the deepest units are at the center, and the youngest in the
outermost shell.
The oldest and deepest geological unit is that of the so-called
old roof (old crystalline basement). It comprises a crystalline
base of transformed (metamorphic) rocks that are more than
550-million years old. The main part consists of various paragneisses and mica schists (formerly sediments) and amphibolites
(formerly basalts). The so-called central gneisses are the product
of molten magma that, sometime between 340 and 250 million
years ago, penetrated into the rocks of the old crystalline basement and solidified.
During the Alpide orogeny the granite and granodiorite
became transformed into the schists and gneisses – known as the
central gneisses due to their presence at the center part of the
dome – that we find today. In the area of the Nature Park they
form the mighty mountain ridge that separates the Ahrn Valley
from the Ziller Valley; the rocks of the old roof, however, are only
found in small quantities.
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1
Habitats, animals and plants
Water and ice have played a large part in shaping the mountains
and valleys. The Rieserferner-Ahrn/Vedrette di Ries-Aurina Nature
Park has the greatest number of glaciers of all South ­Tyrolean nature
parks. The landscape of the central gneisses with their beautiful
ridges, slow rock weathering and soil formation, scree and “stone
mountain” appearance is very different from that of the schist coverings with their wide, rounded ridges and “grassy mountain” look.
Glaciers
Legends had it that they were “glass mountains”, rising inhospitably skywards and inaccessible to all but the “Saligen people” –
the dead. The German word for glacier (from the Latin “glacies”)
is Gletscher, and was in common use in Tyrol only by the 19th
century. Prior to this, the term “Ferner” (from Old High German
“firni” – old snow) was used. In the Ziller Valley, the term “Kees”
(from Rhaetian “Kasa” – ice) was used.
Today, only the northernmost slopes in the Nature Park are
glaciated to a significant degree; this is mostly because the limited
accumulation zones and steep terrain make the glaciers far less
pronounced than those around Großvenediger and Großglockner.
For example, in the upper Gell Valley or at the Kasseler Hütte/
Rifugio Roma alpine hut, the recent retreat of the glaciers provides
an excellent opportunity to observe glacial formation: various
types of moraines, boulders, glacial polish, lakes, rounded-hump
landscapes, and the incipient erosion. Thus, on a small scale,
here we can see the processes that greatly contributed to forming
the landscape at the end of the Ice Age.
Milky white water gurgles forth from the mouth of the glacier,
rushing over the smooth, flat rocks to flow over waterfalls into the
valley. The Reinbachfälle/Cascate di Riva waterfalls in the Tobel/
Tobl gorge at the entrance to the Rein/Valle di Riva valley vividly
convey a sense of the force of the glacier landscape that issues
forth from the Rieserferner/Vedrette di Ries Group. There is almost
nothing comparable to it in South Tyrol, and the water is the true
wealth of the Nature Park.
Algae, crustaceans and mosses are soon visible upon the stones
and sandy pebbles, followed by the first pioneer plants (plant
species which are the first to colonize adverse habitats and adapt
well to extreme conditions, and the lack of water and nutrients).
Late spring blooms in the snow beds (small valleys and hollows
where the snow often remains for up to eight or ten months per
year), as late as early August. Here we can find specially adapted
plants, such as the alpine snowbell, the two-flowered sandwort,
the alpine daisy or dwarf cudweed. Many of the plant species
found in the snow beds begin to bud while they are still buried by
the snow. There is such little time that every ray of sunshine must
be used before the weather changes and the long winter sets in.
In some extreme places the loss of a single leaf may be decisive for
the survival of the plant.
3
Several pioneer plant species are evergreens and thus save a
lot of energy and time by not having to constantly reproduce their
foliage.
Lakes
The third largest lake in South Tyrol lies nestled amid the mixed
pine forest of the Antholz/Anterselva Valley. Antholz/Anterselva lake
is a summer attraction for thousands of tourists who are drawn to
its refreshing, cool mountain setting. A nature trail around the lake
provides information about the flora, fauna, cultural background
and characteristics of the area. Several smaller but extremely
attractive lakes are found above the tree line. High above the
Bachertal/Val del Rio valley are the Kofler lakes, in which the glacier
mountains of the Rieserferner/Vedrette di Ries Group are mirrored.
The Klammlsee/Lago di Gola lake is located southwest of the
Klammljoch pass at the end of the Knuttental/Valle dei Dossi valley,
and the three Maler lakes lie below the Schneebigen Nock/Monte
Nevoso. Lesser known lakes include the Pojen Valley lakes (Schreinsee, Schlossbergsee and Schwarzsee/Lago Nero) in the foothills of
the southwestern Durreck Group, nestled in the barren landscape
of the upper Pojen Valley between the Ahrn/Aurina and Rein/Riva
Valleys.
Bogs
Especially in the northern side valleys of the Ahrn/Aurina Valley,
but also in other parts of the Natural Park, one can find numerous
precious wetland habitats. The largest is 22 hectares in size and
the best preserved bog is the habitat protected Pürschtal bog at
over 2,000 meters above St. Peter/S. Pietro between the Pürschtal
meadow and Katzenkofel/Cima del Gatto. There are beautiful
4
5
6
7
Fig. 3
The Lahner pasture
with the Dreiherrenspitz/Picco dei Tre
Signori in the background. The high
mountain pastures
are centuries-old
testaments to man’s
presence and
­endeavors in the Park.
wet meadows where orchids bloom in early summer situated in
Großklausen, southeast of Steinhaus/Cadipietra. The Rötmoos
is superbly set against the scenic backdrop of the Rötspitze/Pizzo
Rosso, and also worth mentioning are the lower bogs on the
valley floor in the further stretches of the Wielen Valley, the Pojen
bog or the bog near the Oberen Kofler pasture in Rein/Riva. Plants
such as the round-leaved sundew or the alpine butterwort and
animals, such as the grass frog are frequently found in these areas.
Fig. 6
The wood grouse is a
typical forest dweller.
This grouse species
prefers solitary woods
with dense undergrowth, and is
particularly sensitive to
any disturbance of its
habitat.
Photo: Luis Steger
Forests
On the Tristennöckl above the Kasseler Hütte/Rifugio Roma
alpine hut at an elevation of 2,465 meters is one of the highest
Swiss pines in the Eastern Alps. The roots of the tree penetrate
deep into the rocks between the schists. The north-facing slope
provides just the right shade for this record-setting elevation.
The southern slopes of the Rieserferner/Vedrette di Ries, on the
other hand, are much warmer and the intense sunlight in the
spring would deplete the pine needles of their water reserves at
a time when there is no replenishment source from the frozen
ground: the tree would thus get “dried out”.
The spread of the pine trees and their occurrence in particular
locations such as on large boulders are the result of the tireless
work of the nutcracker. This relative of the crow feeds almost
exclu­sively on the seeds of the Swiss pine, the pine nuts, and is
thus by far the greatest propagator of this tree species. The nutcracker eagerly gathers the seeds in autumn to store up as food
for the winter and buries them in different locations. Those nuts
that it fails to recover then germinate and grow into new trees.
Hooved animals are also widespread in the Nature Park. Red
Deer and roe deer – the males of which bear antlers, which they
Fig. 7
The creeping avens is
sometimes found just
a few meters away
from patches of ice.
This pioneer plant is
characterized by
yellow flowers, fuzzy
fruit and long stolons
similar to the straw­
berry plant.
Fig. 4
In order to soar up to
the heights from which
to seek its prey, the
golden eagle requires
strong updrafts.
Despite this, he is
known as the “Lord of
the Skies”.
Photo: Nature Park Archives Office
Fig. 5
Steep terrain and an
abundance of water
produce scenic
landscapes with
spectacular waterfalls.
The Reinsbach Falls are
a good example of
this natural sight and
sound experience.
Photo: Ghedina
Photo: Josef Hackhofer
Photo: Josef Hackhofer
grow each year after losing the old ones – are fond wood dwellers. The entire Nature Park is home to the chamois, whereas the
alpine ibex found in the Durreck and Venediger Groups tend to
live far above the tree line.
The coniferous forests differ greatly from the valley up to the
tree line. The spruce is dominant in the lower part, and is the tree
most common to the Nature Park. As one goes higher in elevation, it is slowly replaced by larch and Swiss pine; each of these
trees, either jointly or alone, depending on the location, form the
upper timberline. The southern part of the Nature Park, especially
in particularly dry locations, is extensively covered by a forest of
Scots pine. These trees are especially beautiful in the spring when
the spring heather comes into bloom. The crested tit is a bird
species common to this habitat.
The mountain pine is found in great numbers in the Knutten
Valley, but also in the Pojener pastures and throughout the Ahrn/
Aurina Valley. A bird typically found among the mountain pines is
the redpoll.
The woods also contain particular specimens of various
deciduous trees, such as the rowan, birch, aspen, willow or the
gray alder, which cover great swaths of the Antholz/Anterselva
Valley; the green alder may also be found in some moist gullies.
These gullies are frequented by the hazel grouse, or the
smaller grouse. Black grouse and wood grouse, two more representatives of this genus, however, prefer the upper edge of the
forest and the dwarf shrub heaths or among the mountain forests
with lots of undergrowth of blueberries and cranberries and
anthills, which provide an important source of protein for feeding
their chicks. The anthill larvae are also favorites of the wood­
peckers, of which five different types exist in the Park. Also worthy
of mention here is the three-toed woodpecker, which lives a
secretive life among the natural mountain forests, but whose
presence is easily noted by the ringed imprints he leaves on trees.
The Human Factor
Humans play an important role in the Rieserferner-Ahrn/
Vedrette di Ries-Aurina Nature Park. In many areas, with the
exception of those dominated by high-mountain wilderness, the
natural habitats have benefited from human management.
Mountain meadows and pastures, of which there are over a
hundred in the Nature Park, have been shaped for centuries
through agriculture. The natural tree line has in fact been lowered
by grazing and mowing in many areas. The abundance of flowers
present, which visitors so greatly admire, is only possible because
the mountain meadows have been regularly mowed and not
over-fertilized, and the pastures have been evenly grazed. Only a
proper balance ensures the survival of certain plant and animal
species. On the one hand, the hemming in of pastures with roads
creates less time-consuming management, on the other hand,
many plants cannot tolerate fertilizer or to be grazed too
­frequently. Increased mechanization of agricultural processes
requires uniform, easy-to-work surfaces, which destroy many
valuable micro-habitats. The conservation of traditional farming
methods takes on even greater value, and the protected area
has greater importance for the conservation of habitats. The
scientific research undertaken, including that across the border
in cooperation with the Hohe Tauern National Park, is a valuable
aid in preserving bio-diversity and gaining new knowledge.
Natural settings that are ecologically intact are a basic need for
people seeking recreation.
Rieserferner-Ahrn/Vedrette di Ries-Aurina Nature Park (7)
Area: 31,320 hectares, established in 1988, expanded in 1994
DREIHERRENSPITZE
PICCO DEI TRE SIGNORI
3499
VENEDIGERGRUPPE
N AT I O N A L PA R K H O H E TA U E R N
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RÖTSPITZE
PIZZO ROSSO
3495
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TRIANGOLO DI RIVA
3031
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ANTERSELVA DI MEZZO
1241
10b
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6
WINDSCHAR
CIMA DEL VENTO
3041 m
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MÜHLBACH
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1462
TESSELBERG
MONTASSILONE
1478
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CAMINATA IN TURES
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2
AMATEN
AMETO
UTTENHEIM
VILLA OTTONE
837
MÜHLEN
MOLINI DI TURES
DIETENHEIM
TEODONE
GAIS
836
TAU F
LUTTACH
LUTAGO
962
Key
OLANG
VALDAORA
PERCHA
PERCA
973
3b
SAND IN TAUFERS
CAMPO TURES
865
in Kasern/Casere; Prettau/Predoi
Open: in summer from early June
to mid-October 10:00 am – 5:00 pm,
closed on Sundays; from mid-July to
mid-September daily 9:00 am – 6:00 pm;
in winter from Christmas to Easter daily
9:00 am – 4:00 pm. Admission free!
Ph. +39 0474 654188
[email protected]
www.provinz.bz.it/naturparke
NIEDERRASEN
RASUN DI SOTTO
LA
Gönneralm
BLOSSBERG
2619
10a
Kasern/Casere Nature Park
Information Center
va
4
LE
3a
33
sel
7a
LB
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Pojenalm
AHORNACH
ACERETO
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OBERRASEN
RASUN DI SOPRA
1030
1
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P.TA DELLA CASCATA
2652
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MONTE NALLE
2231
6
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nb
33
ST. JOHANN
S. GIOVANNI
1018
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10c
RAMMELSTEIN
MONTONE
2463
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ANTHOLZ-NIEDERTAL
ANTERSELVA DI SOTTO
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10a
LUTTERKOPF
M. LUTTA
2145
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1A
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OBERPOJEN
POIA DI SOPRA
1579
in Sand in Taufers/Campo Tures
Open: from early May to late October,
late December to late March, Tuesday
to Saturday, 9:30 am – 12:30 pm and
2:30 pm – 6:00 pm. Also open on Sundays
in July, August and September. Admission
free!
Ph. +39 0474 677546
[email protected]
www.provinz.bz.it/naturparke
TH
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Grentealm
RAUCHKOFEL
M. FUMO
6a
Rieserferner-Ahrn/Vedrette
di Ries-Aurina Nature Park
­Visitor’s Center
3
SCHWARZE WAND
CRODA NERA
3105
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10b
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M. NOVALE DI FUORI
2493
SCHNEEBIGER NOCK
M. NEVOSO
3358
6a
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GR. LÖFFLER
M. LOVELLO
3376
11
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TRISTENNÖCKL
Kasseler Hütte
Rif. Roma
DURRECKSPITZ
CIMA DURA
3130
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SCHWARZENSTEIN
SASSO NERO
3368
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MAGERSTEIN
MONTE MAGRO
3273
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RIVA DI TURES
1595
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Lago di Chiusetta
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ST. JAKOB
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1194
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1052
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2687
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Lago di Anterselva
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Sand in Taufers/Campo Tures: 5,293 inhabitants, Area 16,447 hectares, of which 12,016
hectares are part of the Nature Park; Tourist office: Ph. +39 0474 678076, www.taufers.com
Gais: 3,186 inhabitants, Area 6,034 hectares, of which 2,912 hectares are part of the Nature
Park; Tourist office: Ph. +39 0474 504220, www.gais-uttenheim.com
Percha/Perca: 1,474 inhabitants, Area 3,028 hectares, of which 2,048 hectares are part of
the Nature Park; Bruneck tourist office: Ph. +39 0474 555722, www.bruneck.com
Rasen/Rasun-Antholz/Anterselva: 2,885 inhabitants, Area 12.092 hectares, of which
4,584 hectares are part of the Nature Park; Rasen/Rasun-Antholz/Anterselva Valley
tourist office: Ph. +39 0474 496269, www.rasen.it; Antholz/Anterselva Valley tourist
office: Ph. +39 0474 492116, www.antholz.com
Ahrntal/Valle Aurina: 5,920 inhabitants, Area 18.728 hectares, of which 3,467 hectares are
part of the Nature Park; Tourist office: Ph. +39 0474 671136, www.ahrntal.it
Prettau/Predoi: 604 inhabitants, Area 8,649 hectares, of which 6,293 hectares are part of
the Nature Park; Tourist office: Ph. +39 0474 652198, www.ahrntal.org
8a
Koflerseen
Knuttenalm
da
Nature Park communities
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The heart of the Nature Park is the Rieserferner/Vedrette di Ries
Group between Antholz/Anterselva and Rein in Taufers/Riva di
Tures, of which the Hochgall/Collalto (3,436 m) is the most
recognizable landmark. The Durreck Group lies between Rein/Riva
and Ahrntal/Valle Aurina, in which the Durreckspitze (3,135 m) is
the highest peak. Further eastwards, the Venediger Group has the
two highest peaks of the Nature Park, Rötspitz/Pizzo Rosso
(3,495 m) and the Dreiherrenspitze/Picco dei Tre Signori (3,499 m).
The Rieserferner-Ahrn/Vedrette di Ries-Aurina Nature Park is the
second largest nature park in South Tyrol and seamlessly abuts
the Austrian Hohe Tauern National Park and the Zillertal Alps High
Mountain Nature Park at the border.
Together these three protected areas contain more than
2,500 sq. km of the largest connected nature reserve in Central
Europe. The village of Kematen in Sand in Taufers/Camminata di
Tures at 900 meters is the lowest point in the Park, right next to
the mighty Rein/Riva waterfalls that offer spectacular natural
scenery and are a tourist attraction. The village Rein in Taufes/Riva
di Tures is like an island within the Nature Park and is the jumping-off point for wonderful hiking and mountain tours. Other
major accesses are the valley entrances of Prettau/Predoi and
Antholz/Anterselva lake. Peaceful valleys lying to the south
include those of Mühlbach/Rio Molino, Tesselberg/Montassilone
and, Wielen/Vila. Near Platten/Plata above Percha/Perca are the
famous earth pyramids, which are easily accessible to everyone.
Overall, the nature reserve offers an amazing amount of
diversity unlike anything else in the more southerly Dolomites
and are a welcome alternative destination. The Visitor’s center in
Sand in Taufers/Campo Tures and Information center in Kasern/
Casere house modern permanent exhibitions that offer visitors to
the Nature Park a good place to start.
1
eg
er W
a
Fuld
2
-T
.A
ur
ino
WOLLBACHSPITZE
CIMA DI VALLE
3210
A Brief Overview of the Nature Park
D
RE
l
Fu
H
TA
LE
EP
PE
UP
KGR
REC
DUR
NAPFSPITZ
CIMA CADINI
3143
hr
A
16b
EN
AS
AL
L-V
AL
EN
PRETTAU
PREDOI
1467
L
EL
RIO
Waldnersee
WILDGALL
COLLASPRO
3272
8c
9A
WEISSE
WAND
VA
ROTE WAND
CRODA ROSSA
2817
39
Bärenluegscharte
9
1b
KASERN
CASERE
1595
16b
HOCHGALL
COLLALTO
3435
PURG
LL
13
L
ST. MARTIN
S. MARTINO
Staller Sattel
Passo Stalle
2052
Barmer Hütte
8
Hl. Geist
S. Spirito
3
Hundskehljoch
Passo del Cane
Klammljoch
Passo di Gola
2298
POJ
RAUCHKOFEL
MONTE FUMO
3252
South Tyrol Nature Parks
Nature parks are of particular importance for the preservation
of nature and landscapes, education and research, and providing
an opportunity to experience nature. The concept is based on a
few clear principles:
1. South Tyrol Nature Parks protect and preserve the diversity of
the mountains with their habitats, plants and animals.
2. Information, environmental education and a special nature
experience offer visitors a new understanding of nature and
promote good governance.
3. The Nature Parks comprise mountains, pastures and forests;
permanent settlements are not part of the area.
4. Forest and alpine farming and transhumance are maintained
using sustainable methods.
5. No construction is permitted (except for the forest and alpine
farming and transhumance). No overhead lines, mines, gravel
mines or use of water for hydroelectric or industrial purposes
is allowed.
R
13
L
TA
ÖT
GABELSPITZ
3071
TT
Schlern-Rosengarten/Sciliar-Catinaccio Nature Park
Texelgruppe/Gruppo di Tessa Nature Park
Puez-Geisler/Puez-Odle Nature Park
Fanes-Sennes-Prags/Fanes-Senes-Braies Nature Park
Trudner Horn/Monte Corno Nature Park
Drei Zinnen/Tre Cime Nature Park
Rieserferner-Ahrn/Vedrette di Ries-Aurina Nature Park
Stilfser Joch/Stelvio National Park
-
VA
TA
KNU
1
2
3
4
5
6
7
N
Hl.-Geist-Jöchl
F.lla di Campo
2658
ER
Obersee
RO
TRINKSTEIN
FONTE ALLA ROCCIA
IES
TER
12
IN
5
GR. OHRENSPITZE
GRANDE ORECCHIO
ERE
R TA L
Nature park boundary
VAL
LE
DI T
URES
Marked hiking trail
Access road
Difficult path
Waters
Via ferrata
Waterfall
Lift
Parking lot
Pass/gap
Closed Road
Earth pyramids
Tavern/Rest station
National border
Alpine hut
Visitor’s center
Ahr
- T. A
ur
ino
1
BRUNECK
BRUNICO
835
PU
DT
AL
14
GS
VA L P
US
Krimmler Tauern
Passo dei Tauri
2633
ST. MAGDALENA
S. MADDALENA
LENKSTEIN
SASSO LUNGO
3238
r-H
14
GGEN TA L
RE
FE
DE
TA L
RT
STE
TO
Z AC H
EN
WAR
DE
1
SCH
Lenkjöchlhütte
Rif. Giogo Lungo
LE
Bozen
13
WAL
3
N
DE
LÖFFELSPITZE
PIZZO CUCCHIAIO
us
La
F E R E G G E N TA
Birnlückenhütte
Rif. Tridentina
13
Ar t u
eg
erw
itz
Franziskusweg
Meran
KLOCKERKARKOPF
VETTA D’ITALIA
2913
-V
AL
Schlanders
Bruneck
Brixen
LE D
EL
2
BIRNLÜCKE
FORCELLA DEL PICCO
2667
ST. GEORGEN
S. GIORGIO
822
Alpine emergency signals
• Within 1 minute emit 6 audio/visual
signals (at 10 second intervals)
• Pause for 1 minute
• Repeat the signal (until a response is
received)
• Response: 3 signals within 1 minute
Emergency number for
mountain accidents
Provincial emergency call center 118
Park regulations
• No motor vehicles, use public transport
to access the Park.
• Stay on the trails.
• Avoid making noise.
• Do not throw anything away, do not
take anything (mushrooms, plants,
minerals).
• Tents? Camping? No. Please have con­
sideration for the facilities of the Park.
• Fire hazard! No campfires, no grills.
Cigarettes?
• Take your time, and enjoy the experience.