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NASSFELD - Geopark Karnische Alpen

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Farbprofil: ISO - Coated v2 (basICColor)<br />

Komposit Standardbildschirm<br />

english<br />

100<br />

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<strong>Karnische</strong>r Höhenweg<br />

(Südalpenweg 03)<br />

Gailtaler Höhenweg<br />

DISCOVERING THE GEOPARK<br />

(ADVENTURE GEOPARK)<br />

The 1000 square kilometer Carnic Alps <strong>Geopark</strong><br />

invites you on a journey back in time to discover<br />

the Earth's past. There is no other place where<br />

one can find within such a small and scenic<br />

landscape so many documents of the<br />

Earth's heritage.<br />

<strong>NASSFELD</strong><br />

GEOTRAIL<br />

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GEOTRAIL<br />

<strong>NASSFELD</strong><br />

More than 70 sites between the villages of<br />

Feistritz in the eastern Gail Valley and Maria<br />

Luggau in the Lesach Valley can be visited<br />

to discover the journey through time which lasts<br />

several hundred million years. The hiker will<br />

encounter spectacular waterfalls, mystical<br />

canyons, vertical cliffs, quiet mountain lakes<br />

and fossilized marine and terrestrial faunas<br />

and floras.<br />

In the <strong>Geopark</strong> man plays only a minor role. The<br />

keystone is the elementary power of nature and<br />

geological times which convey an unforgettable<br />

impression to every visitor. The exciting history<br />

starts some 500 million years ago. At that time<br />

the oldest rocks of our mountains were deposited<br />

in an ocean on the other side of the globe. Since<br />

then they have been on a real odyssey from cool<br />

climate during the Ordovician to moderate and<br />

tropic latitudes in the Devonian. At the end of<br />

the Palaeozoic Era, the Permian, the area<br />

experienced a desert climate. In the following<br />

Triassic Period the continental plates crossed the<br />

equator and drifted during the Mesozoic and<br />

Cenozoic Eras centimeter by centimeter towards<br />

present latitudes. Finally, during the Pleistocene<br />

Epoch ice formed the landscape as it is seen<br />

today. Some 20.000 years ago the glaciers<br />

started melting and men invaded the <strong>Geopark</strong> to<br />

settle and cultivate mountains and valleys alike.<br />

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Location of the Naßfeld Geotrail in the <strong>Geopark</strong><br />

Für den Inhalt verantwortlich: Prof. Hans Peter Schönlaub, Kötschach/Mauthen.<br />

Gestaltung: Monika Brüggemann-Ledolter, Geologische Bundesanstalt.<br />

www:geopark-karnische-alpen.at<br />

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Farbprofil: ISO - Coated v2 (basICColor)<br />

Komposit Standardbildschirm<br />

Geological Survey<br />

100 x 210mm 100 x 210mm<br />

97 x 210mm<br />

ADVENTURE GEOLOGY<br />

www.geologie.ac.at<br />

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Left: Fossil debris from mainly brachiopods (Genera Productus and Spirifer) from the<br />

Auernig-Formation. (Naßfeld, west of Krone)<br />

Map<br />

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Below: Thin section with longitudinal and cross sections of fusulinids<br />

(unicellular Foraminifera) from Limestone Bed s of the top of mountain Auernig.<br />

Bottommost: Leaves of the fern Pecopteris sp. from plant locality west of Krone.<br />

Topographie: BEV - 2009, vervielfältigt mit Genehmigung des BEV in Wien, T2009/56516.<br />

Kam<br />

mleiten<br />

Kühweger Alm<br />

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Kühweger Törl<br />

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Gartnerkofel<br />

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Watschiger Alm<br />

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THE <strong>NASSFELD</strong> GEOTRAIL<br />

In geological textbooks about Austria the term<br />

„Naßfeld“ is almost equivalent to Carboniferous and rich<br />

occurrences of all kinds of marine and land-derived<br />

fossils. About half way up to the pass post-Variscan<br />

deposits unconformably overly older strata. These<br />

younger rocks exhibit almost horizontal bedding which<br />

can best be seen on the southern slope of Mount<br />

Auernig at the state border or at the northern cliff of<br />

Mount Gartnerkofel. The latter represents the youngest<br />

strata in this area reflecting dolomites of Middle Triassic<br />

age some 220 million years old.<br />

Access:<br />

Tröpolach - Road to Naßfeld - Parking Watschig Alm.<br />

Route: Watschig Alm (1625 m) - Kühweg Törl<br />

(1914 m) – Mount Kammleiten (1998 m) – Cable road<br />

Station Gartnerkofel (1960 m) – Mount Garnitzen<br />

(1940 m) – Mount Auernig (1863 m) - Watschig Alm.<br />

Length:<br />

Duration:<br />

About 5 km.<br />

4 - 5 hours.<br />

Auernig<br />

1863m<br />

9<br />

I TA L I E N<br />

Garnitzenberg<br />

1951m<br />

Garnitzenalm<br />

/Krone<br />

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Krone<br />

Boards:<br />

1: Scenery of Naßfeld 300 million years ago.<br />

2/1: Muschelkalk Conglomerate, the most colourful<br />

rock in the surrounding.<br />

2/2: Pin pricking the mountain - a drill hole to solve<br />

one of the world's mysteries.<br />

Distant view from the peak Kammleiten.<br />

3: The dominating rock of mountain Gartnerkofel.<br />

4: Lithified lime mud.<br />

Panoramic view from Naßfeld to the Hohe Tauern<br />

region.<br />

5: River gravel transformed to quartz conglomerates.<br />

6: Limestones containing miraculous microfossils.<br />

7: The bed with the brachiopods.<br />

8: Mount Garnitzen representing a Carboniferous<br />

sand pit.<br />

9: Mount Auernig in the Sea, testimony of<br />

marine life.<br />

10: Imprints of fossil plants from Mount Corona<br />

as a memory.<br />

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Exhibitions and Informations: Visitor Center Dellach im Gailtal,<br />

A-9635 Dellach im Gailtal, 65<br />

ABENTEUER ERDGESCHICHTE<br />

Maps: Austrian map 1:50 000, sheet 198 Weißbriach (BEV-Vienna),<br />

Geological map of Austria, sheet 198 Weißbriach (GBA-Vienna)<br />

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Montag, 29. Juni 2009 16:41:03

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