Field Trip a CARNIC ALPS by Hans P. SCHÖNLAUB with Contributions
Field Trip A CARNIC ALPS By Hans P. SCHÖNLAUB with contributions from H. JAEGER, M. R. HOUSE, J. D. PRJCE, B. GÖDDERTZ, H. PRIEWALDER, O. H. WALLISER, J. KRIZ, W. HAAS & G. B. VAI 29 figures and plates 1—10 A contribution to Project „Ecostratigraphy" Authors addresses: Doz. Dr. Hans P. Schönlaub, Dr. H. Priewalder, Geologische Bundesanstalt, P. O. Box 154, Rasumofskygasse 23, A-1031 Wien/Austria; Doz. Dr. H. Jaeger, Museum für Naturkunde, Humboldt Universität Berlin, Invalidenstraße 43, DDR-104 Berlin; Prof. Dr. M. R. House, Dr. J. D. Price, Department of Geology, The University of Hull, Cottingham Road, Hull, HU6 7RX, England; Prof. Dr. W. Haas, B. Göddertz, Institut für Paläontologie, Universität, Nußallee 8, D-53 Bonn; Prof. Dr. O. H. Walliser, Geologisch-Paläontologisches Institut, Universität, Goldschmied-Str. 3, D-3400 Göttingen; Dr. J. Kriz, Ustredni Ustav Geologicky, Malostranske nam. 19, Praha 1; Prof. Dr. G. B. Vai, Istituto di Geologia e Paleontologia dell'Universita, Via Zamboni 63—67,1-40127 Italia. Introduction The Carnic Alps are an east-west directed 100 km long and 10—20 km broad mountain chain in Sou thern Austria and Northern Italy. Towards the east they continue to the Karawanken Alps forming the border between Austria and Yugoslavia. The highest peak is Hohe Warte (Mt. Coglians) in the Central Carnic Alps with an altitude of almost 2800 m; most peaks, however, range between 2000 to 2500 m. The mountains are separated by deep valleys and thus form a spectacular landscape, the scenery of which is strongly influenced by repeated alternations from shale dominated areas to rocky limestone regions.
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