eis – -Translation – Keybot Dictionary

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Show textShow cached sourceOpen source URL	Eis ausserhalb Gletscher
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Show textShow cached sourceOpen source URL	Innerhalb von vier Tagen hat sich das Wasser deutlich tiefer ins Eis erodiert und tritt deshalb weiter unten aus. Weiter oben ist ein älterer, verlassener Kanal erkennbar (14.7.2008).
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Within four days the water has eroded noticable into the ice, and the waterfall emrges at a lower level. An older, abandoned channel appears further up (July 14th, 2008).

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Show textShow cached sourceOpen source URL	Phantom Lake und Phantom Peak von Port Hendrigan, 13.7.2008. Das Eis, das von Thomspon Glacier von links her hereinfliesst, schwimmt mehrheitlich und löst sich langsam in einzelne Eisberge auf.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Phantom Lake and Phantom Peak from Port Hendrigan, July 13th, 2008. The ice from Thomspon Glacier, flowing in from the left, is mostly floating and disintegrates into icebergs in the background.

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Show textShow cached sourceOpen source URL	Der südlichste aktive Vulkan der Welt ist Mount Erebus (3795m), der Dampf ausstösst. Er ist fast vollständig von Eis bedeckt. MH
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	The southernmost active volcano in the world is Mount Erebus (3795 m) giving off occasional puffs of steam. The volcano, seen here from New Zealand’s Scott Base, is almost completely ice-covered. MH

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Show textShow cached sourceOpen source URL	Der Iceberg Glacier auf der Axel Heiberg Island ist ein Surge-Gletscher, erkennbar an den geschwungenen Moränen und an der löchrigen Oberfläche (entstanden durch Schmelzwasserströme in stagnierendem Eis).
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Iceberg Glacier on Axel Heiberg Island is a surge-type glacier, here in its quiescent state (1977), recognizable by the contorted moraines and pitted surface resulting from streams in stagnant ice.

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Show textShow cached sourceOpen source URL	Falten im Eis kann man besonders gut an einer senkrechten Gletscherstirn beobachten. Thompson Glacier, Axel Heiberg Island, kanadische Arktis. MH
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Folding of ice is well seen in ice cliffs, especially if debris from the base is entrained as well. This S-shaped fold is in the vertical cliff of Thompson Glacier on Axel Heiberg Island in the Canadian Arctic. MH

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Show textShow cached sourceOpen source URL	Alfabet Nunatakker am Rande des Eisschilds in Ostgrönland von Tillit Nunatak aus gesehen. Diese Nunataks sind die Gipfel von 2000 bis 3000 Meter hohen Bergen, die fast vollständig vom Eis bedeckt sind.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Isolated peaks known as Alfabet Nunatakker at the edge of the Greenland Ice Sheet in East Greenland, viewed from Tillit Nunatak. These nunataks represent the summits of 2000 to 3000 m-high peaks that are almost buried by ice.

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Show textShow cached sourceOpen source URL	Vier Geologen untersuchen einen von Eis abgeschliffenen Gesteinsaufschluss des Ossian Sarsfjellets im Nordwesten von Spitzbergen, während kleine Brocken Eis von kalbenden Gletschern vorbeitreiben.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Four geologists examining an ice-worn rock outcrop on Ossian Sarsfjellet, northwest Spitsbergen, as small lumps of ice from calving glaciers drift by.

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Show textShow cached sourceOpen source URL	Viele Gletscher in polaren Regionen enthalten auch Eis, welches kälter als der Druck-Schmelzpunkt ist, und zwar vor allem am Rand und nahe der Oberfläche. Man nennt sie polythermale Gletscher. JA
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Many glaciers of polar regions contain at least some ice which is colder than the pressure melting point, particularly near the surface and along the rim. They are then called polythermal. Glaciers whose ice is entirely “cold”, i.e. temperatures below the melting point throughout, are common only in Antarctica. JA

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Show textShow cached sourceOpen source URL	Schmelzwasserkanäle waschen feineres Material aus Moränen. Anderswo wird es wieder abgelagert und schützt das Eis vor Ablation, wodurch sich Sandkegel bilden. Glacier de Tsijiore Nouve, Schweiz. MH
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Supraglacial streams often wash out the finer material (sand and pebbles) from the moraine cover. Pockets of debris protect the ice from ablation, and dirt cones may form, as here on Glacier de Tsijiore Nouve, below Pigne d’Arolla (3796 m), Switzerland. MH

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Show textShow cached sourceOpen source URL	Die vom Eis abgeschürfte Oberfläche im Vordergrund besteht aus altem kristallinen Gneis (von starker Hitze und hohem Druck metamorphosiertes Gestein) in Gåseland, Inner Vestfjorden (Scoresby Sund), Ostgrönland.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	The ice-scoured surface in the foreground comprises ancient crystalline gneisses (rocks metamorphosed by strong heat and high pressure) of the Laurentian shield in Gåseland, inner Vestfjorden (Scoresby Sund), East Greenland.

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Show textShow cached sourceOpen source URL	Kleiner eisgestauter See auf dem White Glacier, unterhalb des Yellowhead Mountain. Beachte wie das aus dem letzten Winter stammende Eis auf dem See gestaucht und verfaltet wird. Wolf Mountain ist rechts im Hintergrund sichtbar.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Small ice-dammed lake on White Glacier, below Yellowhead Mountain. Note how lake ice from the previous winter is compressed and folded by the two converging glaciers. Wolf Mountain is in the right background.

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Show textShow cached sourceOpen source URL	Das Bild zeigt eine Eislawine von der Gletscherstirn des Festigletscher, Kanton Wallis, Schweiz, in 1981. Etwa 2000 Kubikmeter Eis brachen ab. Sehr viel grössere Eislawinen bedrohten das Dorf Randa im Tal darunter.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Ice avalanche from the snout of Festigletscher, Canton Valais, Switzerland in 1981. An estimated 2000 cubic metres of ice were involved. Considerably larger events of this nature have been known to threaten the village of Randa in the valley below. JA

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Show textShow cached sourceOpen source URL	Wo das Eis langsamer wird verbinden sich Moränen miteinander, können aber durch ihre unterschiedliche Färbung immer noch unterscheiden werden. Hubbard Glacier, Alaska. MH
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Where the ice slows down and becomes crevassed, medial moraines merge into one another, as on Hubbard Glacier, Alaska. Despite now merging into a continuous cover of debris, the individual moraines may be distinguished on the basis of the different-coloured rock types. MH

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Show textShow cached sourceOpen source URL	Die inneren Fjorde Ostgrönlands zeigen vom Eis erodierte Bergwände aus altem kristallinen Gestein. Dieser Aufschluss aus präkambrischem Gestein im Nordvestfjord, Ostgrönland, zeigt grosse Anteile von rosarotem, magmatischen und Gestein, das mit stark metamorphosiertem grauem Gestein verfältet ist.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	The inner fjords of East Greenland reveal ice-carved rock faces with structure of ancient crystalline rocks. This exposure of Precambrian rock in Nordvestfjord, East Greenland, shows large bodies of pink igneous and partially melted material folded in with strongly metamorphosed grey rock.

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Show textShow cached sourceOpen source URL	Ausschnittsvergrösserung aus dem vorangehenden Bild: In der Kalbungsfront ist links eine schöne Bogenstruktur erkennbar. Der Abfluss von den Wasserfällen verschwindet hinter dem regenerierten Gletscher und gelangt unter dem Eis hindurch in den See (Foto Marco Zanoli, 2005).
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Enlarged section of previous image. In the left part of the cliff a nice arch structure can be sen. The water from the falls disappears behind the remnant glacier on the right, reaching the lake through a subglacial channel (photo Marco Zanoli, 2005).

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Show textShow cached sourceOpen source URL	Segregationseis entsteht in Lockersedimenten durch wiederholtes Gefrieren und Schmelzen. Das gebildete Eis dehnt sich aus und hebt das darüber liegende Material an; es bilden sich kleine Hügel, die man von dieser Art vor allem in Flussebenen sieht.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Segregation of ice from sediment by repeated freezing and thawing is a common process on river plains, raising the overlying material into a mound. In this example from Engelskbukta, northwest Spitsbergen, the mound is collapsing as the ice core, now exposed, melts.

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Show textShow cached sourceOpen source URL	Vier Geologen untersuchen einen von Eis abgeschliffenen Gesteinsaufschluss des Ossian Sarsfjellets im Nordwesten von Spitzbergen, während kleine Brocken Eis von kalbenden Gletschern vorbeitreiben.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Four geologists examining an ice-worn rock outcrop on Ossian Sarsfjellet, northwest Spitsbergen, as small lumps of ice from calving glaciers drift by.

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Show textShow cached sourceOpen source URL	Innerhalb des Gletschers verformt sich das Eis plastisch. Bestehende Schichten können gefaltet werden. Griesgletscher in den Schweizer Alpen. MH
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	At depth within the glacier, ice deforms rather like a plastic material such as plasticene. Existing layers can become folded as at the surface of Griesgletscher in the Swiss Alps. MH

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Show textShow cached sourceOpen source URL	Strukturen im Eis
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Structures in the ice

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Show textShow cached sourceOpen source URL	Der stärkste Zoom zeigt intensiv verfaltetes Eis beim orographisch linken Gletscherrand.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	The strongest zoom shows intensively folded ice near the true left margin of the glacier.

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Show textShow cached sourceOpen source URL	Eis und Wasser
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Show textShow cached sourceOpen source URL	Auch das Eis unterhalb dieses kleinen Eisfalls wird in Längsrichtung gestaucht und verfaltet.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Ice of a tributary glacier descending via a small icefall is strongly compressed in the longitudinal direction, also causing folding.

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Show textShow cached sourceOpen source URL	Ein Kontinent unter Eis [mehr]
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	The icy continent [more]

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Show textShow cached sourceOpen source URL	In einem tief eingeschnittenen Schmelzwasserkanal erkennt man Foliationsstrukturen im Eis.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	A deeply incised meltwater channel exposes foliation structures in the ice.

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Show textShow cached sourceOpen source URL	Vom höchsten Gipfel der Erde, dem Mount Everest (8848 m, links), fliesst das Eis des Khumbugletschers über einen gewaltigen Eisfall (ganz links) und nachher unterhalb der Nuptse- Westflanke vorbei, im Bild nach rechts unten.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	The world’s highest peak, Mount Everest (8848 m) on the left, feeds the Khumbu Icefall and then the Khumbu Glacier which flows beneath Nuptse 7861 m) towards the right. MH

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Show textShow cached sourceOpen source URL	Über einen riesigen Eisfall gelangt das Eis des Ewigschneefäld zum Konkordiaplatz.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Icefall below Ewigschneefäld, near Konkordiaplatz.

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Show textShow cached sourceOpen source URL	Eis in Bewegung
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Living ice

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Show textShow cached sourceOpen source URL	Fotos und 3 Videoclips von Eis, Schnee und Dampfringen von Jürg Alean und Marco Fulle [mehr]
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Photos and 3 video clips of ice, snow and steam rings by Jürg Alean and Marco Fulle [more]

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Show textShow cached sourceOpen source URL	Cathedral Rocks (2663m) jenseits des Gipfelplateaus. Infolge des Rückgangs der Gletscher bleibt hier nur noch wenige Eis das ganze Jahr liegen.
Compare text pagesCompare HTM pagesOpen source URLOpen target URLDefine swisseduc.ch as primary domain	Cathedral Rocks (2663m) sul lato opposto del Plateau Sommitale. Un ghiacciaio molto piccolo è ciò che qui rimane in seguito al ritiro glaciale.