Deutsch: Rückzugsschotter Français: Gravier de retrait Italiano: Ghiaie di ritiro glaciale English: Gravel of a glacial retreat
DE: Rückzugsschotter wird während eines Gletscherrückzugs im Gletschervorfeld abgelagert wurde (Schotter wird von Moräne unterlagert).
FR: Les graviers de retrait sont des graviers fluvioglaciaires déposés à l’avant du glacier lors du retrait du glacier (les graviers recouvrent par conséquent la moraine).
The Mesozoic is the middle geochronologic era of the Phanerozoic eon, starting with the Induan age (at the transition from the Paleozoic era) and ending with the Maastrichtian age (at the transition to the Cenozoic period). It is subdivided in three periods (Triassic, Jurassic and Cretaceous).
Mesozoik, Ère secondaire, Erdmittelalter, Mittelalter, Secondario, ère des Reptiles, ère des Dinosaures, Zeitalter der Reptilien, Zeitalter der Dinosaurier, Zeit der Tethys
The Pleistocene is the first geochronologic epoch of the Quaternary, starting with the Gelasian age (at the transition from the Pliocene epoch) and ending with an unnamed age at the transition to the Holocene epoch. It is subdivided in three subepochs (Early, Middle and Late Pleistocene).
The Infra-Niesen Mélange, forming the base of the Niesen Nappe, is composed of slivers of pre-flysch series within a mainly gypsum-anhydrite and rarely “wildflysch” matrix. These slivers consist of rare gneiss, Triassic to Late Jurassic sedimentary rocks as well as Niesen Flysch.
Subniesenzone (Zingg 1983 und 1984), zone infra-Niesen = mélange infra-Niesen (Escher et al. 1987), Infra-Niesen-Formation, Formation de l'Infra-Nisen, mélange infr-Niesen = Sub-Niesen mélanges (Jeanbourquin 1991), série détritique anté-flysch = écailles Infra-Niesen (Ackermann et al. 1991)
Deutsch: Umbrail–Terza-Schuppenkomplex Français: Complexe d'écailles de l'Umbrail–Terza Italiano: Complesso di scaglie Umbrail–Terza English: Umbrail–Terza Slice Complex
The Umbrail-Terza Slice Complex consists of two geographically separated parts: the smaller Terza Slice (a klippe overlying the westernmost part of the Quattervals Nappe) and the larger Umbrail-Chavalatsch Slices further to the east (a very complicated zone of imbrication underneath the Ötztal Nappe Complex).
A proposito Lessico Litostratigrafico della Svizzera Questo lessico online è stato concepito come uno strumento di riferimento pratico per i geologi che lavorano nella ricerca accademica (soprattutto
