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Ellie comes with some excess baggage in the form of her two possum "brothers"-- Crash and Eddie, a couple of daredevil pranksters and cocky, loud-mouthed troublemakers.

Manny, Sid and Diego quickly learn that the warming climate has one major drawback: A huge glacial dam holding off oceans of water is about to break, threatening the entire valley.

The only chance of survival lies at the other end of the valley. So our three heroes, along with Ellie, Crash and Eddie, form the most unlikely Written by gavin gunmasterM hotmail.

Similar to the first Ice Age, the promotional material for the sequel was out in the theatres way in advance, and courtesy of the Scrat character too, up to its usual antics of getting to that elusive acorn.

Here, Scrat opens the movie, and emulating the style of the first, he provides most of the laughs, also as an intermission from the actual scenes from the main cast.

We learn that Sid has gone into the early childhood business, educating the young minds of pre-historic brats. However, I felt that this movie was somehow darker in tone than the original.

While the original was one which dealt with hope, this one had its setting in extinction, disaster and death.

The valley which they live in is threatened by the melting ice, no thanks to global warming. So all the animals embark on a journey to salvation, to that rumored ark which will save them from the massive floods to come.

Along the way, our trio meets up with another trio of characters, who were added to expand the cast, featuring 2 Possums Crash Seann William Scott and Eddie Josh Peck , and another, but female, mammoth Queen Latifah.

Pretty wide scope, but they manage to fit in place nicely. The villains in this sequel are pretty nasty, besides the looming natural disaster, we have two sea creatures with nasty teeth and attitude, as well as menacing vultures ever ready to pounce on the flesh of animals who have fallen.

And that makes this sequel, as enjoyable as, if not better, than the original. Recommended stuff this week!

Plus, we hear why more than one celeb wants to be snowed in with Idris Elba. See our favorite Sundance moments.

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Keep track of everything you watch; tell your friends. Full Cast and Crew. Manny, Sid, and Diego discover that the ice age is coming to an end, and join everybody for a journey to higher ground.

On the trip, they discover that Manny, in fact, is not the last of the woolly mammoths. Share this Rating Title: The Meltdown 6. Use the HTML below.

You must be a registered user to use the IMDb rating plugin. User Polls What age would you like to live in?

Best Animated Second Installment To be continued Learn more More Like This. Dawn of the Dinosaurs Escape 2 Africa Kung Fu Panda Shrek the Third Kung Fu Panda 2 Despicable Me 2 Edit Cast Cast overview, first billed only: There are three main contributors from the layout of the continents that obstruct the movement of warm water to the poles: Another important contribution to ancient climate regimes is the variation of ocean currents , which are modified by continent position, sea levels and salinity, as well as other factors.

They have the ability to cool e. The closing of the Isthmus of Panama about 3 million years ago may have ushered in the present period of strong glaciation over North America by ending the exchange of water between the tropical Atlantic and Pacific Oceans.

Analyses suggest that ocean current fluctuations can adequately account for recent glacial oscillations. This realigned the thermohaline circulation in the Atlantic, increasing heat transport into the Arctic, which melted the polar ice accumulation and reduced other continental ice sheets.

The release of water raised sea levels again, restoring the ingress of colder water from the Pacific with an accompanying shift to northern hemisphere ice accumulation.

According to Kuhle, the plate-tectonic uplift of Tibet past the snow-line has led to a surface of c. The reflection of energy into space resulted in a global cooling, triggering the Pleistocene Ice Age.

This comparatively insignificant warming, when combined with the lowering of the Nordic inland ice areas and Tibet due to the weight of the superimposed ice-load, has led to the repeated complete thawing of the inland ice areas.

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.

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.

Yet this is by far the weakest of the three frequencies predicted by Milankovitch. During the period 3. 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. Muller , Gordon J.

MacDonald , [61] [62] [63] 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 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.

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.

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. Human timeline and Nature timeline. History of climate change science. 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.

Please help improve this section by adding citations to reliable sources. Unsourced material may be challenged and removed. January Learn how and when to remove this template message.

Glacial history of Minnesota. Retrieved 7 January No More Ice Ages". Comptes Rendus Geoscience in French. The annals of Mont Blanc.

Discovering the Ice Ages. The Earth in Decay. A History of British Geomorphology — Regulator of Global Climates?: A climate disaster triggered by the evolution of oxygenic photosynthesis" PDF.

Retrieved 8 August Life through deep time. Archived from the original on 15 June Archived from the original PDF on June 27, Ice Sheets and Landforms.

Retrieved 10 August Archived from the original PDF on Newswise, Retrieved on December 17, Development in Quaternary Science: Extent and Chronology Vol.

Encyclopedia of Snow, Ice and Glaciers. Retrieved 25 April Global Warming, Naturally Weather Underground". Archived from the original on Moscariello, , Global chronostratigraphical correlation table for the last 2.

Development in Quaternary Science. Quaternary Glaciations — Extent and Chronology: The Ice Age World: Earthquakes at North-Atlantic passive margins: Neotectonics and postglacial rebound.

Earth and Planetary Science Letters. Antarctica Greenland Last glacial period 1st: Antarctic 34 to 2. Karoo Mya to Mya.

Andean-Saharan Mya to Mya. Sturtian to Mya ; Marinoan to Mya. Greenhouse and Icehouse Earth. Geology portal Paleontology portal.

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