Ice Age Reihe
Die Helden von „Ice Age“ – nicht nur für die Kleinen, wie wir meinen! Ice Age (engl. für „Eiszeit“) ist ein US-amerikanischer Computeranimationsfilm von Blue Sky abgerufen am August Ausklappen. Filmreihe: Ice Age. Disney verkündete, dass die komplette Ice-Age-Reihe ab heute auf dem Streamingdienst Disney+ zur Verfügung steht.
Ice Age Reihe Mehr zum Thema:
Ice Age (engl. für „Eiszeit“) ist ein US-amerikanischer Computeranimationsfilm von Blue Sky abgerufen am August Ausklappen. Filmreihe: Ice Age. Hier erfahrt ihr die richtige Reihenfolge der „Ice Age“-Filme. Die Reihenfolge des „Ice Age“-Franchises ist vergleichsweise unkompliziert – die "Ice Age"-Filmreihe wird auf dem Eis weitererzählt - im wahrsten Sinne. Teil 5 schließt (bisher) die ganze Reihe schön ab, mit Peaches die am Ende des dritten Teils geboren wird und hier mit ihrem Freund Julian, als Teenie zusammen. Ab morgen ist die Herde wieder vereint: Mit dem fünften Teil ist die „Ice Age“-Reihe auf Disney+ endlich komplett. Anzeige. Treffen sich ein. Otto Waalkes ist auch im vierten Teil der „Ice Age“-Reihe wieder die deutsche Synchronstimme von Faultier Sid. Der kann sich im letzten Moment gemeinsam. Disney verkündete, dass die komplette Ice-Age-Reihe ab heute auf dem Streamingdienst Disney+ zur Verfügung steht. Erlebe mammutmäßige Abenteuer mit Manny, Sid & Diego und freue dich auf die komplette ICE AGE Reihe - ab jetzt, bei Disney Plus.
Dort löst er versehentlich eine Reihe von kosmischen Ereignissen aus, die eine große Gefahr für die Ice Age-Welt darstellen. Nun muss sich die ungewöhnliche. Ab morgen ist die Herde wieder vereint: Mit dem fünften Teil ist die „Ice Age“-Reihe auf Disney+ endlich komplett. Anzeige. Treffen sich ein. Hier erfahrt ihr die richtige Reihenfolge der „Ice Age“-Filme. Die Reihenfolge des „Ice Age“-Franchises ist vergleichsweise unkompliziert – die "Ice Age"-Filmreihe wird auf dem Eis weitererzählt - im wahrsten Sinne.
Nachdem zwei dieser drei Kumpanen ein Menschenbaby vor dem Ertrinken gerettet haben, machen sie sich auf den Weg, es zu den Menschen zurückzubringen.
Diego, der Säbelzahntiger, verfolgt dabei aber insgeheim andere Absichten als Manni und Sid…. Die Eiszeit ist nun vorbei.
Die Tiere, die sich im Süden in ein Tal zückgezogen haben, müssen von dort fliehen, bevor das Eis zu schmelzen beginnt und das Tal überschwemmt.
Manni und Ellie erwarten ihr erstes Baby, während sich Diego zunehmend fehl am Platz fühlt. Sid kümmert sich um ein paar Dinosaurier-Eier, doch als die kleinen Dinos schlüpfen, lässt die Mutter der kleinen Unruhestifter nicht lange auf sich warten.
Allerdings nimmt sie nicht nur ihre Kinder sondern auch Sid mit, was die restliche Herde dazu verleitet, der Dinosaurier-Mutter in den Dschungel unter der Eisdecke zu folgen.
Mithilfe des Wiesels Buck machen sie sich daran, Sid zurückzuholen. There, Sid and Diego learn about Manny's past and his previous interactions with the neanderthal hunters, in which they slaughtered his family, consisting of his mate and child, leaving Manny a depressed loner.
Later, the group almost reaches their destination, Half-Peak, only to encounter a forming river of lava. Manny and Sid, along with Roshan, make it across safely, but Diego ends up hanging on a cliff, about to fall into the lava.
Manny saves him, narrowly missing certain death by falling into the lava himself. The herd takes a break for the night, and Roshan takes his first walking steps towards Diego, who starts to have a change of heart about his mission.
The next day, the herd approaches the ambush, causing Diego, now full of respect for Manny for saving his life to change his mind and confess to Manny and Sid about the ambush.
As the pair turn hostile towards him, Diego pleads for their trust and tries to foil the attack. The herd battles Soto's pack, but despite their efforts, Soto and his associates manage to corner Manny.
As Soto closes in for the kill on Manny, Diego sacrifices himself by jumping in the way and is injured as a result. Manny then knocks a distracted Soto into a rock wall, causing several sharp icicles to fall onto Soto, impaling and instantly killing him.
Horrified, the rest of the pack retreat. Manny and Sid mourn for Diego's injury, which they believe is fatal, and continue their journey without him.
The two manage to successfully return Roshan to his tribe, and to their surprise, Diego manages to rejoin them, in time to see Roshan leave.
The group then begin to head off to warmer climates. As the ice slowly melts, an acorn that was also frozen in the same ice block is washed away.
Scrat then finds a coconut and tries to stomp it into the ground, only to accidentally trigger a volcanic eruption. The characters are all prehistoric animals.
The animals can talk to and understand each other and are voiced by a variety of famous actors. Like many films of prehistoric life, the rules of time periods apply very loosely, as many of the species shown in the film never actually lived in the same time periods or the same geographic regions.
The film, originally envisioned as a traditionally animated movie with an action-oriented comedy-drama tone, was intended to be developed by Don Bluth and Gary Goldman 's Fox Animation Studios.
In light of this, Fox Animation head Chris Meledandri and executive producer Steve Bannerman approached Forte with the proposition of developing the film as a computer-animated movie, which Forte realized was "basically a no-brainer," according to her.
Michael J. Wilson , who had written and developed the film's original story treatments in conjunction with Forte, wrote the first draft for the script, and Chris Wedge , a co-founder of Blue Sky, was brought on to the project as the director in late Fox also opted for the movie to take a more comedy-oriented direction albeit while still maintaining some dramatic elements , and brought writer Michael Berg to help emphasize a funnier tone.
After being hired, Berg reportedly told the studio that he couldn't write a kid's film, to which the studio responded, "Great! Just write a good story.
Story development began in spring of ,  and official production on the film began in June , one week after the closure of Fox Animation Studios.
Jon Vitti and Mike Reiss , both former writers for The Simpsons , were added later on after Berg and Ackerman left to further polish the script.
For research, the film's development team took several trips to the Museum of Natural History early on in production in order to make sure that the film authentically felt like the Ice Age.
Wilson stated on his blog that his daughter Flora came up with the idea for an animal that was a mixture of both squirrel and rat, naming it Scrat, and that the animal was obsessed with pursuing his acorn.
The name 'Scrat' is a combination of the words 'squirrel' and 'rat', as Scrat has characteristics of both species; Wedge has also called him "saber-toothed squirrel.
This was the only role intended for Scrat, but he proved to be such a popular character with test audiences that he was given more scenes.
The filmmakers made it so that many of the scenes with Scrat appear directly after dramatic moments in the film. In a interview with Jay Leno , Denis Leary revealed that his character, Diego the sabertooth, originally died near the end of the film.
However, it was reported that kids in the test audience bursted into tears when his death was shown.
Leary himself warned the producers that something like this would happen. When it was proven true, the scene was re-written to ensure Diego survived.
Originally, Sid the Sloth was supposed to be a con-artist and a hustler, and there was even a finished scene of the character conning some aardvark kids.
His character was later changed to a talkative-clumsy sloth because the team felt the audience would have hated him. There was also an alternate scene of Sid in the hottub with the ladies which shows him saying to them "Let's jump in the gene pool and see what happens.
This was cut because it was not suitable for children and may have gotten the film a PG rating. Other innuendos with Sid were also cut from the film.
Sid was also supposed to have a female sloth named Sylvia voiced by Kristen Johnston chasing after him, whom he despised and kept ditching.
All the removed scenes can be seen on the DVD. The characters and environments in Ice Age were modeled and animated using WaveFront's Maya animation software.
Rendering was completed using CGI Studio, an in-house ray tracing program being developed since Blue Sky's formation in and previously used for Wedge's short film, Bunny.
While Jimmy Neutron: Boy Genius , released three months before Ice Age , became the first computer-animated film to make use of ray tracing technology, Ice Age would have received the distinction had it been released at the time Blue Sky began work on the movie.
In order to keep the film at a more exciting pace, the development team took certain liberties with Sid in terms of realism; although real-life ground sloths were slow-moving and rigid, Sid was given a fast movement speed in certain scenes, as well as a more flexible range of motions.
Manny was a particularly difficult character to animate due to his unique attributes as a mammoth, such as his long fur and massive trunks that covered up his face.
According to co-director Carlos Saldanha, Diego was one of the most complexly animated characters in the movie, with some scenes showing off his high movement speed as a sabre-toothed tiger while others kept his movement more contained and focused on his facial expressions to carry the moment.
The voice cast of Ice Age was encouraged to make up their own dialogue during recording. Several lines in the film were improvised by the actors.
Each cycle has a different length, so at some times their effects reinforce each other and at other times they partially cancel each other.
There is strong evidence that the Milankovitch cycles affect the occurrence of glacial and interglacial periods within an ice age. The present ice age is the most studied and best understood, particularly the last , years, since this is the period covered by ice cores that record atmospheric composition and proxies for temperature and ice volume.
The combined effects of the changing distance to the Sun, the precession of the Earth's axis , and the changing tilt of the Earth's axis redistribute the sunlight received by the Earth.
Of particular importance are changes in the tilt of the Earth's axis, which affect the intensity of seasons. It is widely believed that ice sheets advance when summers become too cool to melt all of the accumulated snowfall from the previous winter.
Some believe that the strength of the orbital forcing is too small to trigger glaciations, but feedback mechanisms like CO 2 may explain this mismatch.
While Milankovitch forcing predicts that cyclic changes in the Earth's orbital elements can be expressed in the glaciation record, additional explanations are necessary to explain which cycles are observed to be most important in the timing of glacial—interglacial periods.
In particular, during the last , years, the dominant period of glacial—interglacial oscillation has been , years, which corresponds to changes in Earth's orbital eccentricity and orbital inclination.
Yet this is by far the weakest of the three frequencies predicted by Milankovitch. During the period 3. The reasons for dominance of one frequency versus another are poorly understood and an active area of current research, but the answer probably relates to some form of resonance in the Earth's climate system.
Recent work suggests that the K year cycle dominates due to increased southern-pole sea-ice increasing total solar reflectivity.
The "traditional" Milankovitch explanation struggles to explain the dominance of the ,year cycle over the last 8 cycles.
Richard A. Muller , Gordon J. MacDonald ,    and others have pointed out that those calculations are for a two-dimensional orbit of Earth but the three-dimensional orbit also has a ,year cycle of orbital inclination.
They proposed that these variations in orbital inclination lead to variations in insolation, as the Earth moves in and out of known dust bands in the solar system.
Although this is a different mechanism to the traditional view, the "predicted" periods over the last , years are nearly the same. Another worker, William Ruddiman , has suggested a model that explains the ,year cycle by the modulating effect of eccentricity weak ,year cycle on precession 26,year cycle combined with greenhouse gas feedbacks in the 41, and 26,year cycles.
Yet another theory has been advanced by Peter Huybers who argued that the 41,year cycle has always been dominant, but that the Earth has entered a mode of climate behavior where only the second or third cycle triggers an ice age.
This would imply that the ,year periodicity is really an illusion created by averaging together cycles lasting 80, and , years.
The jumps are induced by the orbital forcing, while in the early Pleistocene the 41,year glacial cycles resulted from jumps between only two climate states.
A dynamical model explaining this behavior was proposed by Peter Ditlevsen. At times during the paleoclimate, carbon dioxide levels were two or three times greater than today.
Volcanoes and movements in continental plates contributed to high amounts of CO 2 in the atmosphere. Carbon dioxide from volcanoes probably contributed to periods with highest overall temperatures.
The current geological period, the Quaternary , which began about 2. The last cold episode of the last glacial period ended about 10, years ago. The major glacial stages of the current ice age in North America are the Illinoian , Eemian and Wisconsin glaciation.
The use of the Nebraskan, Afton, Kansan, and Yarmouthian stages to subdivide the ice age in North America has been discontinued by Quaternary geologists and geomorphologists.
These stages have all been merged into the Pre-Illinoian in the s. During the most recent North American glaciation, during the latter part of the Last Glacial Maximum 26, to 13, years ago , ice sheets extended to about 45th parallel north.
These sheets were 3 to 4 kilometres 1. This Wisconsin glaciation left widespread impacts on the North American landscape. The Great Lakes and the Finger Lakes were carved by ice deepening old valleys.
Most of the lakes in Minnesota and Wisconsin were gouged out by glaciers and later filled with glacial meltwaters. The old Teays River drainage system was radically altered and largely reshaped into the Ohio River drainage system.
Other rivers were dammed and diverted to new channels, such as Niagara Falls , which formed a dramatic waterfall and gorge, when the waterflow encountered a limestone escarpment.
The area from Long Island to Nantucket, Massachusetts was formed from glacial till , and the plethora of lakes on the Canadian Shield in northern Canada can be almost entirely attributed to the action of the ice.
As the ice retreated and the rock dust dried, winds carried the material hundreds of miles, forming beds of loess many dozens of feet thick in the Missouri Valley.
Post-glacial rebound continues to reshape the Great Lakes and other areas formerly under the weight of the ice sheets.
The Driftless Area , a portion of western and southwestern Wisconsin along with parts of adjacent Minnesota , Iowa , and Illinois , was not covered by glaciers.
A specially interesting climatic change during glacial times has taken place in the semi-arid Andes.
Beside the expected cooling down in comparison with the current climate, a significant precipitation change happened here. From this follows that—beside of an annual depression of temperature about c.
Accordingly, at glacial times the humid climatic belt that today is situated several latitude degrees further to the S, was shifted much further to the N.
Although the last glacial period ended more than 8, years ago, its effects can still be felt today. The erratic boulders , till , drumlins , eskers , fjords , kettle lakes , moraines , cirques , horns , etc.
The weight of the ice sheets was so great that they deformed the Earth's crust and mantle. After the ice sheets melted, the ice-covered land rebounded.
During glaciation, water was taken from the oceans to form the ice at high latitudes, thus global sea level dropped by about meters, exposing the continental shelves and forming land-bridges between land-masses for animals to migrate.
During deglaciation , the melted ice-water returned to the oceans, causing sea level to rise. This process can cause sudden shifts in coastlines and hydration systems resulting in newly submerged lands, emerging lands, collapsed ice dams resulting in salination of lakes, new ice dams creating vast areas of freshwater, and a general alteration in regional weather patterns on a large but temporary scale.
It can even cause temporary reglaciation. This type of chaotic pattern of rapidly changing land, ice, saltwater and freshwater has been proposed as the likely model for the Baltic and Scandinavian regions, as well as much of central North America at the end of the last glacial maximum, with the present-day coastlines only being achieved in the last few millennia of prehistory.
Also, the effect of elevation on Scandinavia submerged a vast continental plain that had existed under much of what is now the North Sea, connecting the British Isles to Continental Europe.
The redistribution of ice-water on the surface of the Earth and the flow of mantle rocks causes changes in the gravitational field as well as changes to the distribution of the moment of inertia of the Earth.
These changes to the moment of inertia result in a change in the angular velocity , axis , and wobble of the Earth's rotation.
The weight of the redistributed surface mass loaded the lithosphere , caused it to flex and also induced stress within the Earth.
The presence of the glaciers generally suppressed the movement of faults below. Earthquakes triggered near the ice margin may in turn accelerate ice calving and may account for the Heinrich events.
In Europe, glacial erosion and isostatic sinking from weight of ice made the Baltic Sea , which before the Ice Age was all land drained by the Eridanos River.
From Wikipedia, the free encyclopedia. This article is about a generic geological period of temperature reduction. For the most recent glacial period commonly referred to as the Ice Age, see Last glacial period and Pleistocene.
For other uses, see Ice age disambiguation. Period of long-term reduction in temperature of Earth's surface and atmosphere.
See also: History of climate change science. Main article: Timeline of glaciation. See also: Glacial period and Interglacial.
Minimum and maximum glaciation. Minimum interglacial, black and maximum glacial, grey glaciation of the northern hemisphere.
Minimum interglacial, black and maximum glacial, grey glaciation of the southern hemisphere. This section does not cite any sources.
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January Learn how and when to remove this template message. See also: Glacial history of Minnesota. See also: Glacial landform. Encyclopedia of Snow, Ice and Glaciers.
Encyclopedia of Earth Sciences Series. Retrieved 7 January Ice ages: solving the mystery. Comptes Rendus Geoscience in French.
Bibcode : CRGeo. Note: p. In Mathews, C. The annals of Mont Blanc. London: Unwin. Discovering the Ice Ages. The Earth in Decay.
A History of British Geomorphology — Cunningham, Frank F. James David Forbes. Pioneer Scottish Glaciologist. Edinburgh: Scottish Academic Press.
Scientific American. Nature Geoscience. Bibcode : NatGe November The Geographical Journal.Bibcode : Sci Clear your Astrid Lindgren Pippi Langstrumpf. Rate This. Keep track of everything you watch; tell your friends. Let us know if you have suggestions to improve this article requires login. There were extensive polar ice caps Episodenguide Blindspot intervals from to million years ago Rick And Morty Staffel 1 Deutsch South Africa during the Carboniferous and early Permian Periods.