Ice Age 5 Filme Collection [5 DVDs]. Mehr Infos: DVD, Sprachen: Deutsch, Englisch, Ab Freigegeben ohne Altersbeschränkung, erschienen am Viele übersetzte Beispielsätze mit "ice age" – Deutsch-Englisch Wörterbuch und Suchmaschine für Millionen von Deutsch-Übersetzungen. Vor Jahren, als die Eiszeit kurz bevorsteht, bevölkern riesige, majestätische Tiere den Erdball - sieht man einmal von einem Quartett gar nicht so edler Vierbeiner ab. Und das sind das verbiesterte wollige Mammut Manny, das ungehobelte.
Englisch-Deutsch Übersetzung für "ice age"Ice Age 5 Filme Collection [5 DVDs]. Mehr Infos: DVD, Sprachen: Deutsch, Englisch, Ab Freigegeben ohne Altersbeschränkung, erschienen am Übersetzung für 'ice age' im kostenlosen Englisch-Deutsch Wörterbuch von LANGENSCHEIDT – mit Beispielen, Synonymen und Aussprache. Ice Age (engl. für „Eiszeit“) ist ein US-amerikanischer Computeranimationsfilm von Blue Sky den Roman zum zweiten Teil Ice Age 2. Er wurde diesmal von Glenn Dakin geschrieben und erschien auf Deutsch im Verlag Dorling Kindersley.
Ice Age Deutsch Navigation menu VideoICE AGE 4 - VOLL VERSCHOBEN - Trailer deutsch german [HD]
The Swedish mining expert Daniel Tilas — was, in , the first person to suggest drifting sea ice in order to explain the presence of erratic boulders in the Scandinavian and Baltic regions.
He regarded glaciation as a regional phenomenon. Only a few years later, the Danish-Norwegian geologist Jens Esmark — argued for a sequence of worldwide ice ages.
In a paper published in , Esmark proposed changes in climate as the cause of those glaciations. He attempted to show that they originated from changes in Earth's orbit.
Andersen In a paper published in , Bernhardi speculated about former polar ice caps reaching as far as the temperate zones of the globe. In , independently of these debates, the Swiss civil engineer Ignaz Venetz — explained the dispersal of erratic boulders in the Alps, the nearby Jura Mountains, and the North German Plain as being due to huge glaciers.
When he read his paper before the Schweizerische Naturforschende Gesellschaft , most scientists remained sceptical.
De Charpentier transformed Venetz's idea into a theory with a glaciation limited to the Alps. His thoughts resembled Wahlenberg's theory.
In fact, both men shared the same volcanistic, or in de Charpentier's case rather plutonistic assumptions, about the Earth's history.
In , de Charpentier presented his paper before the Schweizerische Naturforschende Gesellschaft. He began to wonder where such masses of stone had come from.
During the summer of he made some excursions to the Bavarian Alps. Schimper came to the conclusion that ice must have been the means of transport for the boulders in the alpine upland.
In the winter of to he held some lectures in Munich. Schimper then assumed that there must have been global times of obliteration "Verödungszeiten" with a cold climate and frozen water.
Schimper, de Charpentier and possibly Venetz convinced Agassiz that there had been a time of glaciation. They mainly drew upon the preceding works of Venetz, de Charpentier and on their own fieldwork.
Agassiz appears to have been already familiar with Bernhardi's paper at that time. The audience was very critical and some opposed to the new theory because it contradicted the established opinions on climatic history.
Most contemporary scientists thought that the Earth had been gradually cooling down since its birth as a molten globe.
In order to persuade the skeptics, Agassiz embarked on geological fieldwork. De Charpentier felt that Agassiz should have given him precedence as it was he who had introduced Agassiz to in-depth glacial research.
It took several decades before the ice age theory was fully accepted by scientists. This happened on an international scale in the second half of the s, following the work of James Croll , including the publication of Climate and Time, in Their Geological Relations in , which provided a credible explanation for the causes of ice ages.
Geological evidence for ice ages comes in various forms, including rock scouring and scratching, glacial moraines , drumlins , valley cutting, and the deposition of till or tillites and glacial erratics.
Successive glaciations tend to distort and erase the geological evidence for earlier glaciations, making it difficult to interpret. Furthermore, this evidence was difficult to date exactly; early theories assumed that the glacials were short compared to the long interglacials.
The advent of sediment and ice cores revealed the true situation: glacials are long, interglacials short. It took some time for the current theory to be worked out.
The chemical evidence mainly consists of variations in the ratios of isotopes in fossils present in sediments and sedimentary rocks and ocean sediment cores.
For the most recent glacial periods, ice cores provide climate proxies , both from the ice itself and from atmospheric samples provided by included bubbles of air.
Because water containing lighter isotopes has a lower heat of evaporation , its proportion decreases with warmer conditions.
This evidence can be confounded, however, by other factors recorded by isotope ratios. The paleontological evidence consists of changes in the geographical distribution of fossils.
During a glacial period, cold-adapted organisms spread into lower latitudes, and organisms that prefer warmer conditions become extinct or retreat into lower latitudes.
This evidence is also difficult to interpret because it requires 1 sequences of sediments covering a long period of time, over a wide range of latitudes and which are easily correlated; 2 ancient organisms which survive for several million years without change and whose temperature preferences are easily diagnosed; and 3 the finding of the relevant fossils.
Despite the difficulties, analysis of ice core and ocean sediment cores  has provided a credible record of glacials and interglacials over the past few million years.
These also confirm the linkage between ice ages and continental crust phenomena such as glacial moraines, drumlins, and glacial erratics.
Hence the continental crust phenomena are accepted as good evidence of earlier ice ages when they are found in layers created much earlier than the time range for which ice cores and ocean sediment cores are available.
There have been at least five major ice ages in the Earth's history the Huronian , Cryogenian , Andean-Saharan , late Paleozoic , and the latest Quaternary Ice Age.
Outside these ages, the Earth seems to have been ice free even in high latitudes;   such periods are known as greenhouse periods.
Rocks from the earliest well-established ice age, called the Huronian , have been dated to around 2.
Several hundreds of kilometers of the Huronian Supergroup are exposed 10 to kilometers 6. Marie to Sudbury, northeast of Lake Huron, with giant layers of now-lithified till beds, dropstones , varves , outwash , and scoured basement rocks.
Correlative Huronian deposits have been found near Marquette, Michigan , and correlation has been made with Paleoproterozoic glacial deposits from Western Australia.
The Huronian ice age was caused by the elimination of atmospheric methane , a greenhouse gas , during the Great Oxygenation Event.
The next well-documented ice age, and probably the most severe of the last billion years, occurred from to million years ago the Cryogenian period and may have produced a Snowball Earth in which glacial ice sheets reached the equator,  possibly being ended by the accumulation of greenhouse gases such as CO 2 produced by volcanoes.
The Andean-Saharan occurred from to million years ago, during the Late Ordovician and the Silurian period. The evolution of land plants at the onset of the Devonian period caused a long term increase in planetary oxygen levels and reduction of CO 2 levels, which resulted in the late Paleozoic icehouse.
Its former name, the Karoo glaciation, was named after the glacial tills found in the Karoo region of South Africa.
There were extensive polar ice caps at intervals from to million years ago in South Africa during the Carboniferous and early Permian Periods.
Correlatives are known from Argentina, also in the center of the ancient supercontinent Gondwanaland. Since then, the world has seen cycles of glaciation with ice sheets advancing and retreating on 40, and ,year time scales called glacial periods , glacials or glacial advances, and interglacial periods, interglacials or glacial retreats.
The earth is currently in an interglacial, and the last glacial period ended about 10, years ago. All that remains of the continental ice sheets are the Greenland and Antarctic ice sheets and smaller glaciers such as on Baffin Island.
The definition of the Quaternary as beginning 2. The Antarctic ice sheet began to form earlier, at about 34 Ma, in the mid- Cenozoic Eocene-Oligocene Boundary.
The term Late Cenozoic Ice Age is used to include this early phase. Ice ages can be further divided by location and time; for example, the names Riss ,—, years bp and Würm 70,—10, years bp refer specifically to glaciation in the Alpine region.
The maximum extent of the ice is not maintained for the full interval. The scouring action of each glaciation tends to remove most of the evidence of prior ice sheets almost completely, except in regions where the later sheet does not achieve full coverage.
Within the current glaciation, more temperate and more severe periods have occurred. The colder periods are called glacial periods , the warmer periods interglacials , such as the Eemian Stage.
The glacial cycles of the late Paleozoic ice house are likely responsible for the deposition of cyclothems. Glacials are characterized by cooler and drier climates over most of the earth and large land and sea ice masses extending outward from the poles.
Mountain glaciers in otherwise unglaciated areas extend to lower elevations due to a lower snow line. Sea levels drop due to the removal of large volumes of water above sea level in the icecaps.
There is evidence that ocean circulation patterns are disrupted by glaciations. The glacials and interglacials coincide with changes in orbital forcing of climate due to Milankovitch cycles , which are periodic changes in the Earth's orbit and the tilt of the Earth's rotational axis.
The earth has been in an interglacial period known as the Holocene for around 11, years,  and an article in Nature in argues that it might be most analogous to a previous interglacial that lasted 28, years.
Moreover, anthropogenic forcing from increased greenhouse gases is estimated to potentially outweigh the orbital forcing of the Milankovitch cycles for hundreds of thousand of years.
Each glacial period is subject to positive feedback which makes it more severe, and negative feedback which mitigates and in all cases so far eventually ends it.
An important form of feedback is provided by the Earth's albedo , which is how much of the sun's energy is reflected rather than absorbed by the Earth.
Ice and snow increase Earth's albedo, while forests reduce its albedo. When the air temperature decreases, ice and snow fields grow, and they reduce forest cover.
This continues until competition with a negative feedback mechanism forces the system to an equilibrium. In , Ewing and Donn  hypothesized that an ice-free Arctic Ocean leads to increased snowfall at high latitudes.
When low-temperature ice covers the Arctic Ocean there is little evaporation or sublimation and the polar regions are quite dry in terms of precipitation, comparable to the amount found in mid-latitude deserts.
This low precipitation allows high-latitude snowfalls to melt during the summer. An ice-free Arctic Ocean absorbs solar radiation during the long summer days, and evaporates more water into the Arctic atmosphere.
With higher precipitation, portions of this snow may not melt during the summer and so glacial ice can form at lower altitudes and more southerly latitudes, reducing the temperatures over land by increased albedo as noted above.
Furthermore, under this hypothesis the lack of oceanic pack ice allows increased exchange of waters between the Arctic and the North Atlantic Oceans, warming the Arctic and cooling the North Atlantic.
Current projected consequences of global warming include a largely ice-free Arctic Ocean within 5—20 years. Diego, one of the tigers that attacked the humans, comes also claiming the baby, and the trio form an uneasy alliance during their journey to the humans.
Manny, Sid, and Diego are currently living in a large valley surrounded by an enormously high ice wall on all sides.
However, the trio discovers that the ice wall is actually a wall that is barely holding a massive body of water that could flood the valley to nearly a mile underwater.
A vulture tells them that there is a boat at the other end of the valley that may save them all, but they only have three days to reach it or die.
Manny is also having trouble fearing the fact that he may be the last mammoth left. Along the way, they meet Ellie, a mammoth who thinks she is a possum, and her possum brothers Crash and Eddie.
As they begin to travel together, Manny learns, with help from Diego and Sid, that he must move on from his past.
During their journey, Scrat the sabre-toothed squirrel has his own adventure. Manny and Ellie are expecting their first child, Peaches.
Scrat falls in love with fellow squirrel Scratte. Diego is anxious about settling down for a domestic life with Manny's new family.
Sid begins to wish for a family of his own, and steals some dinosaur eggs which leads to Sid ending up in an underground world where his herd must rescue him.
The herd also meets Buck, an insane one-eyed weasel who aids them on their quest. Taking place several years after the events of the third film, with Peaches now a teenager, Scrat's pursuit of acorns has world-changing consequences, separating Manny, Sid and Diego from the rest of their group.
As they try to return home, they come into conflict with a pirate gang led by sadistic Captain Gutt. Scrat's pursuit of his elusive acorn catapults him outside of Earth aboard a UFO, where he accidentally sets off a series of cosmic events that transform and threaten the planet.
To save themselves from peril, Manny, Sid, Diego, and the rest of the herd leave their home and reunite with Buck, who leads them on a journey to find a way to save the planet.
On the possibility of a potential sixth film, in June , Galen T. Chu, co-director of the film, stated that there were some ideas for the next installment.
The film is set to release in early Gone Nutty is a animated short film, directed by Carlos Saldanha , and originally released on the Ice Age DVD.
The film was nominated for the Academy Award for Animated Short Film. No Time for Nuts is a animated short film, directed by Chris Renaud and Mike Thurmeier , and it was originally released on the Ice Age: The Meltdown DVD.
No Time for Nuts was nominated for the Academy Award for Best Animated Short Film. Surviving Sid is a animated short film, directed by Galen Tan Chu and Karen Disher.
It was originally released on the Horton Hears a Who! DVD and Blu-ray. Scrat's Continental Crack-Up is the first of a two-part animated short.
It was released in theaters and home media alongside Gulliver's Travels. Scrat's Continental Crack-Up: Part 2 is the second of a two-part animated short.
It was released in theaters and home media alongside Alvin and the Chipmunks: Chipwrecked. Cosmic Scrat-tastrophe is a animated short film.
The short once again follows Scrat, who discovers a flying saucer frozen in a block of ice and accidentally powers it on and ends up creating the Solar System through a series of mishaps.
Scrat: Spaced Out is a animated short film. The short once again follows Scrat, trying to get back to Earth after the events in Cosmic Scrat-tastrophe.
In the middle of decorating for the holiday season, Sid accidentally destroys Manny's favourite decorations.
Sid, convinced by Manny that he is now on Santa's naughty list, takes off with Crash, Eddie and Peaches for the North Pole to get back on the Santa's good side.
When on the North Pole, Sid and his crew accidentally destroy Santa's Workshop. When Manny, Ellie and Diego, worried over Peaches's safety, arrive at the North Pole, they must come together and save Christmas.
The special centers on a harried prehistoric bird mom who entrusts her precious, soon-to-hatch egg to Sid. When she recommends him to her neighbors—a condor mother, Cholly Bear and Gladys Glypto—business booms at his new egg-sitting service.
However, dastardly pirate bunny Squint, who is seeking revenge on the herd, steals, camouflages and hides all the eggs.
While the first film received generally positive reviews, the series has received some criticism for making no attempt to be scientifically accurate    and has suffered a steadily declining critical reception with each succeeding film.
Ice Age Live! A Mammoth Adventure is a live arena ice show that combines ice skating, aerial arts, puppetry and film, and tells a new story based on the first three Ice Age films.
Her father Manny sets off to rescue Peaches, accompanied by Sid and Diego. Their mission is successful, but on the way home they encounter avalanches and rockfalls, diverting them into a fantasy underground kingdom.
It is being produced by Stage Entertainment Touring Productions, and directed by Guy Caron and Michael Curry. A Mammoth Adventure concluded its world tour and was replaced in North America by Ice Age On Ice.
Ice Age inspired rides and attractions will be featured at the first 20th Century Fox theme park, called 20th Century Fox World ,  to open in as part of Malaysia-based Resorts World Genting.
From Wikipedia, the free encyclopedia. American multimedia franchise based on five animated films. Main article: Ice Age film. Main article: Ice Age: The Meltdown.
Main article: Ice Age: Dawn of the Dinosaurs. Main article: Ice Age: Continental Drift. NEU: PODCAST:. Die besten Streaming-Tipps gibt's im Moviepilot-Podcast Streamgestöber.
Ice Age ist ein Computeranimationsfilm aus dem Jahr von Chris Wedge und Carlos Saldanha mit Ray Romano , John Leguizamo und Denis Leary.
Komplette Handlung und Informationen zu Ice Age Ice Age: Die Welt vor Deine Bewertung. Vormerken Ignorieren Zur Liste Kommentieren.
Schaue jetzt Ice Age. Mehr Infos: SD Deutsch. Mehr Infos: HD Deutsch. Ray Romano. John Leguizamo. Denis Leary. Goran Visnjic. Jack Black.
Cedric the Entertainer. Stephen Root. Diedrich Bader. Arne Elsholtz. Otto Waalkes. Thomas Fritsch.
Ice age , also called glacial age , any geologic period during which thick ice sheets cover vast areas of land. Such periods of large-scale glaciation may last several million years and drastically reshape surface features of entire continents.
A number of major ice ages have occurred throughout Earth history. The earliest known took place during Precambrian time dating back more than million years.
The most recent periods of widespread glaciation occurred during the Pleistocene Epoch 2. A lesser, recent glacial stage called the Little Ice Age began in the 16th century and advanced and receded intermittently over three centuries in Europe and many other regions.
Its maximum development was reached about , at which time glaciers were more widespread on Earth than at any time since the last major ice age ended about 11, years ago.
Ice age Article Media Additional Info. Print Cite verified Cite.Vor Jahren, als die Eiszeit kurz bevorsteht, bevölkern riesige, majestätische Tiere den Erdball - sieht man einmal von einem Quartett gar nicht so edler Vierbeiner ab. Und das sind das verbiesterte wollige Mammut Manny, das ungehobelte. Ice Age (engl. für „Eiszeit“) ist ein US-amerikanischer Computeranimationsfilm von Blue Sky den Roman zum zweiten Teil Ice Age 2. Er wurde diesmal von Glenn Dakin geschrieben und erschien auf Deutsch im Verlag Dorling Kindersley. Viele übersetzte Beispielsätze mit "ice age" – Deutsch-Englisch Wörterbuch und Suchmaschine für Millionen von Deutsch-Übersetzungen. Ice age 4 download deutsch kostenlos. 14th June by dn_admin 0 0. Im Film war “Chasing the Sun”, gespielt von The Wanted dem ersten Titelsong des. The Bronze Age marked the first time humans started to work with metal. According to Kuhle, the plate-tectonic uplift of Tibet past the snow-line has led to a surface of c. Furthermore, under this hypothesis König Artus Film lack of oceanic pack ice allows increased exchange of waters between the Arctic and the North Atlantic Alle Menschen Werden Brüder, warming 4g Geschwindigkeit Arctic and cooling the North Atlantic. The weight of the redistributed surface mass loaded the lithospherecaused it to flex and also induced stress within the Earth.