(black curve) with the modelled duration of yearly snow cover (blue curve) and the instrumental data (red curve) represented by the mean value of the snow cover duration records for the stations within a distance of 50 km and an elevation of ±250 m from the study site (n = ...
Total distance covered: 120 km.Scenery: Stunning views of the Pacific Ocean. 08:00 a.m. – Departure from Tokyo.09:00 a.m. – Kamakura. Known as an "oasis of peace," Kamakura served as Japan’s capital for two centuries and is home to a wealth of shrines, temples, and gardens. ...
5 and 6 to be the distance between the edge of the European margin (where the slab ruptured at c. 35–40 Ma) and the present Alpine thrust front at the base of the Subalpine Molasse, as discussed in the next section. Plate and crustal motions in the central Mediterranean area since 84...
However, in a 2–3 km distance from the Ivrea-Verbano Zone, the Strona-Ceneri Zone was overprinted during Permian magmatism along the Cossato-Mergozzo-Brissago Line. Zurbriggen (1996, p. 119) defined between Cannobio and Brissago the Nuova Pace Line, north of which the Strona-Ceneri ...
The average travel time to get from Jeju Alps Hotel to the airport is 15 minutes, but please take into account that the travel time may fluctuate based on traffic, weather conditions, and time of day. What points of interest are close by Jeju Alps Hotel that are in walking distance?
Ocean-derived series occupy most of the Queyras area while margin-derived series domi- nate along the western limit of the Piedmont zone, close to the Briançonnais zone (e.g. Rochebrune nappe: Dumont et al. 1984b). A major pinched klippe of this type of nappe is pre- served within ...
We caution to infer hiatuses on a section based only on the spacing of the biohorizons of a single group because of the risk of diachroneities in the stressed early Danian environment. By comparing the "distance" of the key biohorizons (i.e. the First Occurrence (FO) of Cruciplacolithus...
2. The early stages of ocean opening have been recog- nized to yield characteristic structures in the distal part of passive margins (ocean–continent transition), such as small-scale blocks of continental crust (i.e. exten- sional allochthons) tectonically emplaced on top of serpentinized ...
This block was limited by the Penninic Ocean (= Alpine Tethys) to the north and the Vardar Ocean to the south-east (Scotese, 2001, Stampfli et al., 2002). The Puez Formation includes three members from bottom to top: Puez Limestone, Puez Redbed and Puez Marl (Lukeneder, 2010). The...
The European Alps formed during two orogenic cycles that took place in the Cretaceous and Cenozoic (e.g., Trümpy1960; Frisch1978; Froitzheim et al.1994; Schmid et al.1996). The first phase of mountain building was related to the closure of the Meliata ocean between the Late Jurassic and...