Last glacial period led to the appearance of the woolly mammoth and a huge increase in the area of ​​​​glaciers. But it was only one of many that have cooled the Earth throughout its 4.5 billion years of history.

So, how often does the planet go through ice ages, and when should we expect the next one?

The main periods of glaciation in the history of the planet

The answer to the first question depends on whether you mean the big glaciations or the small ones that occur during these long periods. Throughout history, the Earth has experienced five long periods glaciations, some of which lasted for hundreds of millions of years. In fact, even now, the Earth is going through a large period of glaciation, and this explains why it has polar ice.

The five main ice ages are the Huronian (2.4-2.1 billion years ago), the Cryogenian glaciation (720-635 million years ago), the Andean-Saharan (450-420 million years ago), the late Paleozoic glaciation (335-260 million years ago) and Quaternary (2.7 million years ago to present).

These major periods of glaciation may alternate between smaller ice ages and warm periods (interglacials). At first Quaternary glaciation(2.7-1 million years ago) these cold ice ages occurred every 41 thousand years. However, in the last 800,000 years, significant ice ages have occurred less frequently, about every 100,000 years.

How does the 100,000 year cycle work?

Ice sheets grow for about 90,000 years and then begin to melt during the 10,000 year warm period. Then the process is repeated.

Given that the last ice age ended about 11,700 years ago, perhaps it's time for another one to begin?

Scientists believe that we should be experiencing another ice age right now. However, there are two factors associated with the Earth's orbit that influence the formation of warm and cold periods. Considering how much carbon dioxide we emit into the atmosphere, the next ice age won't start for at least another 100,000 years.

What causes an ice age?

The hypothesis put forward by the Serbian astronomer Milyutin Milanković explains why there are cycles of ice and interglacial periods on Earth.

As a planet revolves around the Sun, the amount of light it receives from it is affected by three factors: its tilt (which ranges from 24.5 to 22.1 degrees in a 41,000-year cycle), its eccentricity (changing the shape of its orbit around of the Sun, which fluctuates from a near circle to an oval shape) and its wobble (one complete wobble occurs every 19-23 thousand years).

In 1976, a landmark paper in the journal Science presented evidence that these three orbital parameters explained the planet's glacial cycles.

Milankovitch's theory is that orbital cycles are predictable and very consistent in a planet's history. If the Earth is going through an ice age, then it will be covered in more or less ice, depending on these orbital cycles. But if the Earth is too warm, no change will occur, at least in regards to the growing amount of ice.

What can affect the warming of the planet?

The first gas that comes to mind is carbon dioxide. Over the past 800,000 years, carbon dioxide levels have fluctuated between 170 and 280 parts per million (meaning that out of 1 million air molecules, 280 are carbon dioxide molecules). A seemingly insignificant difference of 100 parts per million leads to the appearance of glacial and interglacial periods. But carbon dioxide levels are much higher today than they were in past fluctuations. In May 2016, carbon dioxide levels over Antarctica reached 400 parts per million.

The earth has warmed up so much before. For example, during the time of the dinosaurs, the air temperature was even higher than now. But the problem is that in modern world it is growing at a record pace because we have released too much carbon dioxide into the atmosphere in such a short time. In addition, given that emission rates are not declining to date, it can be concluded that the situation is unlikely to change in the near future.

The consequences of warming

The warming caused by the presence of this carbon dioxide will have big consequences, because even a small increase in the average temperature of the Earth can lead to drastic changes. For example, the Earth was on average only 5 degrees Celsius colder during the last ice age than it is today, but this has led to a significant change in regional temperature, the disappearance of a huge part of the flora and fauna, and the appearance of new species.

If global warming causes all of the ice sheets in Greenland and Antarctica to melt, ocean levels will rise by 60 meters compared to today.

What causes great ice ages?

The factors that caused long periods of glaciation, such as the Quaternary, are not as well understood by scientists. But one idea is that a massive drop in carbon dioxide levels could lead to cooler temperatures.

So, for example, according to the uplift and weathering hypothesis, when plate tectonics leads to the growth of mountain ranges, new unprotected rock appears on the surface. It is easily weathered and disintegrates when it enters the oceans. Marine organisms use these rocks to create their shells. Over time, stones and shells take carbon dioxide from the atmosphere and its level drops significantly, which leads to a period of glaciation.

We are at the mercy of autumn and it's getting colder. Are we moving towards an ice age, one of the readers wonders.

The fleeting Danish summer is behind us. The leaves are falling from the trees, the birds are flying south, it's getting darker and, of course, colder too.

Our reader Lars Petersen from Copenhagen has begun to prepare for the cold days. And he wants to know how seriously he needs to prepare.

“When does the next ice age start? I learned that glacial and interglacial periods alternate regularly. Since we live in an interglacial period, it is logical to assume that the next ice age is ahead of us, right? he writes in a letter to the Ask Science section (Spørg Videnskaben).

We in the editorial office shudder at the thought of cold winter, which lies in wait for us at that end of autumn. We, too, would love to know if we are on the verge of an ice age.

The next ice age is still far away

Therefore, we addressed the teacher of the Center fundamental research ice and climate at the University of Copenhagen to Sune Olander Rasmussen.

Sune Rasmussen studies the cold and gets information about past weather, storms, Greenland glaciers and icebergs. In addition, he can use his knowledge in order to fulfill the role of "foreteller of ice ages."

“In order for an ice age to occur, several conditions must coincide. We cannot accurately predict when the ice age will begin, but even if humanity did not further influence the climate, our forecast is that the conditions for it will develop in the best case in 40-50 thousand years,” Sune Rasmussen reassures us.

Since we are still talking to the "ice age predictor", we can get some more information about what these "conditions" are. in question to understand a little more about what the ice age actually is.

What is an ice age

Sune Rasmussen says that during the last ice age average temperature on the ground was a few degrees lower than today, and that the climate at higher latitudes was colder.

Much of the northern hemisphere was covered in massive ice sheets. For example, Scandinavia, Canada and some other parts North America were covered with a three-kilometer ice shell.

The enormous weight of the ice sheet pressed the earth's crust one kilometer inside the earth.

Ice ages are longer than interglacials

However, 19 thousand years ago, changes in the climate began to occur.

This meant that the Earth gradually became warmer, and over the next 7,000 years, freed itself from the cold grip of the Ice Age. After that, the interglacial period began, in which we are now.

Context

New ice age? Not soon

glacial period

This means that 11,715 years have passed since the last ice age, and this is completely normal length interglacial.

“It's funny that we usually think of the Ice Age as an 'event', when in fact it's just the opposite. The middle ice age lasts 100 thousand years, while the interglacial lasts from 10 to 30 thousand years. That is, the Earth is more often in an ice age than vice versa.

“The last couple of interglacials lasted only about 10,000 years each, which explains the widely held but erroneous belief that our current interglacial period is nearing its end,” says Sune Rasmussen.

Three Factors Influence the Possibility of an Ice Age

The fact that the Earth will plunge into a new ice age in 40-50 thousand years depends on the fact that there are small variations in the orbit of the Earth around the Sun. Variations determine how much sunlight hits which latitudes, and thereby affects how warm or cold it is.

This discovery was made by the Serbian geophysicist Milutin Milanković almost 100 years ago and is therefore known as the Milanković cycle.

Milankovitch cycles are:

1. The orbit of the Earth around the Sun, which changes cyclically about once every 100,000 years. The orbit changes from nearly circular to more elliptical, and then back again. Because of this, the distance to the Sun changes. The farther the Earth is from the Sun, the less solar radiation our planet receives. In addition, when the shape of the orbit changes, so does the length of the seasons.

2. The tilt of the earth's axis, which fluctuates between 22 and 24.5 degrees relative to the orbit of rotation around the Sun. This cycle spans approximately 41,000 years. 22 or 24.5 degrees - it seems not such a significant difference, but the tilt of the axis greatly affects the severity of the different seasons. How more Earth tilted, the greater the difference between winter and summer. The Earth's axial tilt is currently at 23.5 and is decreasing, which means that differences between winter and summer will decrease over the next thousand years.

3. The direction of the earth's axis relative to space. The direction changes cyclically with a period of 26 thousand years.

“The combination of these three factors determines whether there are prerequisites for the beginning of the ice age. It is almost impossible to imagine how these three factors interact, but with the help of mathematical models we can calculate how much solar radiation is received by certain latitudes at certain times of the year, as well as received in the past and will receive in the future,” says Sune Rasmussen.

Snow in summer leads to ice age

Especially important role in this context play temperatures in summer.

Milankovitch realized that for the ice age to start, summers in the northern hemisphere would have to be cold.

If winters are snowy and most of the northern hemisphere is covered with snow, then temperatures and amounts sundial in the summer determine whether the snow will be allowed to stay for the whole summer.

“If the snow does not melt in the summer, then little sunlight penetrates the Earth. The rest is reflected back into space in a snow-white veil. This exacerbates the cooling that began due to a change in the orbit of the Earth around the Sun,” says Sune Rasmussen.

“Further cooling brings even more snow, which further reduces the amount of absorbed heat, and so on, until the ice age begins,” he continues.

Similarly, a period of hot summers leads to the end of the Ice Age. Then the hot sun melts the ice enough to sunlight again could fall on dark surfaces, like soil or the sea, which absorb it and heat the Earth.

Humans are delaying the next ice age

Another factor that is relevant to the possibility of an ice age is the amount of carbon dioxide in the atmosphere.

Just as snow that reflects light increases the formation of ice or accelerates its melting, the increase in carbon dioxide in the atmosphere from 180 ppm to 280 ppm (parts per million) helped bring the Earth out of the last ice age.

However, ever since industrialization began, people have been pushing the CO2 share further all the time, so it's almost 400 ppm now.

“It took nature 7,000 years to raise the share of carbon dioxide by 100 ppm after the end of the ice age. Humans have managed to do the same in just 150 years. It has great importance whether the Earth can enter a new ice age. This is a very significant influence, which means not only that an ice age cannot begin at the moment,” says Sune Rasmussen.

We thank Lars Petersen for the good question and send the winter gray T-shirt to Copenhagen. We also thank Sune Rasmussen for the good answer.

We also encourage our readers to submit more scientific questions to [email protected]

Did you know?

Scientists always talk about the ice age only in the northern hemisphere of the planet. The reason is that there is too little land in the southern hemisphere on which a massive layer of snow and ice can lie.

With the exception of Antarctica, the entire southern part of the southern hemisphere is covered with water, which does not provide good conditions for the formation of a thick ice shell.

The materials of InoSMI contain only assessments of foreign media and do not reflect the position of the editors of InoSMI.

Scientists note that the ice age is part of the ice age, when the earth covers ice on long millions years. But many people call the ice age a segment of the history of the Earth, which ended about twelve thousand years ago.

It is worth noting that ice age history had a huge number of unique features that have not reached our time. For example, unique animals that were able to adapt to existence in this difficult climate - mammoths, rhinos, saber-toothed tigers, cave bears and others. They were covered with thick fur and quite large in size. Herbivores adapted to get food from under the icy surface. Let's take rhinos, they raked ice with their horns and ate plants. Surprisingly, the vegetation was varied. Of course, many plant species disappeared, but herbivores had free access to food.

Despite the fact that the ancient people were not large in size and did not have a cover of wool, they also managed to survive during the Ice Age. Their life was incredibly dangerous and difficult. They built small dwellings for themselves and insulated them with the skins of dead animals, and ate the meat. People came up with various traps to lure large animals there.

Rice. 1 - Ice Age

For the first time, the history of the Ice Age was discussed in the eighteenth century. Then geology began to form as a scientific branch, and scientists began to find out what origin the boulders in Switzerland have. Most researchers agreed in a single point of view that they have a glacial beginning. In the nineteenth century, it was suggested that the planet's climate was subject to severe cooling. A little later, the term itself was announced "glacial period". It was introduced by Louis Agassiz, whose ideas were not at first recognized by the general public, but then it was proved that many of his works really have a basis.

In addition to the fact that geologists were able to establish the fact that the ice age took place, they also tried to find out why it arose on the planet. The most common opinion is that the movement of lithospheric plates can block warm currents in the ocean. This gradually causes the formation of an ice mass. If large-scale ice sheets have already formed on the surface of the Earth, then they will cause a sharp cooling by reflecting sunlight, and therefore heat. Another reason for the formation of glaciers could be a change in the level of greenhouse effects. The presence of large Arctic massifs and the rapid spread of plants eliminates the greenhouse effect by replacing carbon dioxide with oxygen. Whatever the reason for the formation of glaciers, this is a very long process that can also enhance the influence of solar activity on the Earth. Changes in our planet's orbit around the Sun make it extremely susceptible. The remoteness of the planet from the "main" star also has an effect. Scientists suggest that even during the largest ice ages, the Earth was covered with ice only one third of the entire area. There are suggestions that ice ages also took place, when the entire surface of our planet was covered with ice. But this fact is still controversial in the world of geological research.

To date, the most significant glacial massif is the Antarctic. The thickness of the ice in some places reaches more than four kilometers. Glaciers move at an average speed of five hundred meters per year. Another impressive ice sheet is found in Greenland. Approximately seventy percent of this island is occupied by glaciers, and this is one tenth of the ice of our entire planet. On this moment time, scientists believe that the ice age will not be able to start for at least another thousand years. The thing is that in the modern world there is a colossal release of carbon dioxide into the atmosphere. And as we found out earlier, the formation of glaciers is possible only at a low level of its content. However, this poses another problem for mankind - global warming, which can be no less massive than the beginning of the ice age.

The last ice age ended 12,000 years ago. In the most severe period, glaciation threatened man with extinction. However, after the glacier melted, he not only survived, but also created a civilization.

Glaciers in the history of the Earth

Last ice age in the history of the Earth - Cenozoic. It began 65 million years ago and continues to this day. Modern man is lucky: he lives in the interglacial, in one of the warmest periods of the planet's life. Far behind is the most severe ice age - the Late Proterozoic.

Despite global warming, scientists are predicting a new ice age. And if the real one comes only after millennia, then the Little Ice Age, which will reduce by 2-3 degrees annual temperatures, could come pretty soon.

The glacier became a real test for man, forcing him to invent means for his survival.

last ice age

The Würm or Vistula glaciation began about 110,000 years ago and ended in the tenth millennium BC. The peak of cold weather fell on the period of 26-20 thousand years ago, the final stage of the Stone Age, when the glacier was the largest.

Little Ice Ages

Even after the glaciers melted, history has known periods of noticeable cooling and warming. Or, in other words, climate pessimism And optima. Pessima are sometimes referred to as Little Ice Ages. In the XIV-XIX centuries, for example, the Little Ice Age began, and the time of the Great Migration of Peoples was the time of the early medieval pessimum.

Hunting and meat food

There is an opinion according to which the human ancestor was rather a scavenger, since he could not spontaneously occupy a higher ecological niche. And all known tools were used to butcher the remains of animals that were taken from predators. However, the question of when and why a person began to hunt is still debatable.

In any case, thanks to hunting and eating meat, the ancient man received a large supply of energy, which allowed him to better endure the cold. The skins of slaughtered animals were used as clothing, shoes and walls of the dwelling, which increased the chances of surviving in a harsh climate.

bipedalism

Bipedalism appeared millions of years ago, and its role was much more important than in the life of a modern office worker. Having freed his hands, a person could engage in intensive construction of a dwelling, the production of clothing, the processing of tools, the extraction and preservation of fire. Upright ancestors moved freely in open area, and their life no longer depended on the collection of fruits of tropical trees. Already millions of years ago, they freely moved over long distances and obtained food in river flows.

Walking upright played an insidious role, but it became more of an advantage. Yes, man himself came to cold regions and adapted to life in them, but at the same time he could find both artificial and natural shelters from the glacier.

Fire

fire in life ancient man was initially an unpleasant surprise, not a boon. Despite this, the ancestor of man first learned to “extinguish” it, and only later to use it for his own purposes. Traces of the use of fire are found in sites that are 1.5 million years old. This made it possible to improve nutrition through the preparation of protein foods, as well as to remain active at night. This further increased the time to create conditions for survival.

Climate

The Cenozoic Ice Age was not a continuous glaciation. Every 40 thousand years, the ancestors of people had the right to a “respite” - temporary thaws. At this time, the glacier receded, and the climate became milder. During periods of harsh climate, natural shelters were caves or regions rich in flora and fauna. For example, the south of France and the Iberian Peninsula were home to many early cultures.

The Persian Gulf 20,000 years ago was rich in forests and grassy vegetation of the river valley, a truly "antediluvian" landscape. flowed here wide rivers, exceeding in size the Tigris and Euphrates one and a half times. Sahara in some periods became a wet savanna. Last time this happened 9000 years ago. This can be confirmed by the rock paintings, which depict the abundance of animals.

Fauna

Huge glacial mammals such as bison, woolly rhinoceros and mammoth became an important and unique source of food for ancient people. Hunting such large animals required a lot of coordination and brought people together noticeably. The effectiveness of "collective work" has shown itself more than once in the construction of parking lots and the manufacture of clothing. Deer and wild horses among ancient people enjoyed no less "honor".

Language and communication

Language was, perhaps, the main life hack of an ancient person. It was thanks to speech that they were preserved and passed down from generation to generation. important technologies processing tools, mining and maintaining fire, as well as various human adaptations for everyday survival. Perhaps in the Paleolithic language, the details of the hunt for large animals and the direction of migration were discussed.

Allerd warming

Until now, scientists are arguing whether the extinction of mammoths and other glacial animals was the work of man or caused by natural causes - the Allerd warming and the disappearance of forage plants. As a result of the extermination a large number species of animals, a person in harsh conditions was threatened with death from lack of food. There are known cases of the death of entire cultures simultaneously with the extinction of mammoths (for example, the Clovis culture in North America). However, warming has become an important factor migration of people to regions whose climate became suitable for the emergence of agriculture.

In the history of the Earth, there were long periods when the entire planet was warm - from the equator to the poles. But there were also times so cold that glaciations reached those regions that currently belong to temperate zones. Most likely, the change of these periods was cyclical. During warmer times, there could be relatively little ice, and it was only in the polar regions or on the tops of mountains. Important feature ice ages is that they change the nature earth's surface: each glaciation affects appearance Earth. By themselves, these changes may be small and insignificant, but they are permanent.

History of Ice Ages

We do not know exactly how many ice ages there have been throughout the history of the Earth. We know of at least five, possibly seven, ice ages, starting with the Precambrian, in particular: 700 million years ago, 450 million years ago (Ordovician), 300 million years ago - Permo-Carboniferous glaciation, one of the largest ice ages, affecting the southern continents. The southern continents refer to the so-called Gondwana, an ancient supercontinent that included Antarctica, Australia, South America, India and Africa.

The most recent glaciation refers to the period in which we live. Quaternary period cenozoic era began about 2.5 million years ago, when the glaciers of the Northern Hemisphere reached the sea. But the first signs of this glaciation date back 50 million years ago in Antarctica.

The structure of each ice age is periodic: there are relatively short warm epochs, and there are longer periods of icing. Naturally, cold periods are not the result of glaciation alone. Glaciation is the most obvious consequence of cold periods. However, there are quite long intervals that are very cold, despite the absence of glaciations. Today, examples of such regions are Alaska or Siberia, where it is very cold in winter, but there is no glaciation, because there is not enough rainfall to provide enough water for the formation of glaciers.

Discovery of ice ages

The fact that there are ice ages on Earth has been known to us since the middle of the 19th century. Among the many names associated with the discovery of this phenomenon, the first is usually the name of Louis Agassiz, a Swiss geologist who lived in the middle of the 19th century. He studied the glaciers of the Alps and realized that they were once much more extensive than they are today. It wasn't just him who noticed. In particular, Jean de Charpentier, another Swiss, also noted this fact.

It is not surprising that these discoveries were made mainly in Switzerland, since there are still glaciers in the Alps, although they are melting quite quickly. It is easy to see that once the glaciers were much larger - just look at the Swiss landscape, the troughs (glacial valleys) and so on. However, it was Agassiz who first put forward this theory in 1840, publishing it in the book "Étude sur les glaciers", and later, in 1844, he developed this idea in the book "Système glaciare". Despite initial skepticism, over time, people began to realize that this was indeed true.

With the advent of geological mapping, especially in Northern Europe, it became clear that before the glaciers had a huge scale. Then there were extensive discussions about how this information relates to the Flood, because there was a conflict between geological evidence and biblical teachings. Initially, glacial deposits were called deluvial because they were considered evidence Flood. Only later it became known that such an explanation is not suitable: these deposits were evidence of a cold climate and extensive glaciation. By the beginning of the 20th century, it became clear that there were many glaciations, and not just one, and from that moment this area of ​​​​science began to develop.

Ice Age Research

Known geological evidence of ice ages. The main evidence for glaciations comes from the characteristic deposits formed by glaciers. They are preserved in the geological section in the form of thick ordered layers of special deposits (sediments) - diamicton. These are simply glacial accumulations, but they include not only deposits of a glacier, but also deposits of melt water formed by its flows, glacial lakes or glaciers moving into the sea.

There are several forms of glacial lakes. Their main difference is that they are a water body enclosed by ice. For example, if we have a glacier that rises into a river valley, then it blocks the valley like a cork in a bottle. Naturally, when ice blocks a valley, the river will still flow and the water level will rise until it overflows. Thus, a glacial lake is formed through direct contact with ice. There are certain deposits that are contained in such lakes that we can identify.

Due to the way glaciers melt, which depends on seasonal changes in temperature, there is an annual melting of ice. This leads to an annual increase in minor sediments falling from under the ice into the lake. If we then look into the lake, we see stratification (rhythmic layered sediments) there, which is also known by the Swedish name "varves" (varve), which means "annual accumulations". So we can actually see annual layering in glacial lakes. We can even count these varves and find out how long this lake has existed. In general, with the help of this material, we can get a lot of information.

In Antarctica, we can see huge ice shelves that come off the land into the sea. And of course, ice is buoyant, so it floats on water. As it swims, it carries pebbles and minor sediments with it. Due to the thermal action of the water, the ice melts and sheds this material. This leads to the formation of the process of the so-called rafting of rocks that go into the ocean. When we see fossil deposits from this period, we can find out where the glacier was, how far it extended, and so on.

Causes of glaciation

Researchers believe that ice ages occur because the Earth's climate depends on the uneven heating of its surface by the Sun. So, for example, the equatorial regions, where the Sun is almost vertically overhead, are the warmest zones, and the polar regions, where it is at a large angle to the surface, are the coldest. This means that the difference in heating of different parts of the Earth's surface controls the ocean-atmospheric machine, which is constantly trying to transfer heat from the equatorial regions to the poles.

If the Earth were an ordinary sphere, this transfer would be very efficient, and the contrast between the equator and the poles would be very small. So it was in the past. But since there are now continents, they get in the way of this circulation, and the structure of its flows becomes very complex. Simple currents are restrained and altered, in large part by mountains, leading to the circulation patterns we see today that drive the trade winds and ocean currents. For example, one of the theories about why the ice age began 2.5 million years ago links this phenomenon with the emergence of the Himalayan mountains. The Himalayas are still growing very fast and it turns out that the existence of these mountains in a very warm part of the Earth governs things like the monsoon system. The start of the Quaternary Ice Age is also associated with the closing of the Isthmus of Panama, which connects the north and south of America, which prevented the transfer of heat from equatorial zone Pacific Ocean to the Atlantic.

If the position of the continents relative to each other and relative to the equator allowed the circulation to work efficiently, then it would be warm at the poles, and relatively warm conditions would persist throughout the earth's surface. The amount of heat received by the Earth would be constant and vary only slightly. But since our continents create serious barriers to circulation between north and south, we have pronounced climatic zones. This means that the poles are relatively cold while the equatorial regions are warm. When everything is happening as it is now, the Earth can change under the influence of variations in the number of solar heat which she receives.

These variations are almost completely constant. The reason for this is that over time the earth's axis changes, as does the earth's orbit. Given such a complex climatic zoning orbital change could contribute to long-term changes in climate, resulting in climate wobble. Because of this, we have not continuous icing, but periods of icing, interrupted by warm periods. This happens under the influence of orbital changes. The latest orbital changes are seen as three separate phenomena: one 20,000 years long, the second 40,000 years long, and the third 100,000 years long.

This led to deviations in the pattern of cyclic climate change during the Ice Age. The icing most likely occurred during this cyclic period of 100,000 years. The last interglacial epoch, which was as warm as the current one, lasted about 125,000 years, and then came a long ice epoch, which took about 100,000 years. We are now living in another interglacial era. This period will not last forever, so another ice age awaits us in the future.

Why do ice ages end?

Orbital changes change the climate, and it turns out that ice ages are characterized by alternating cold periods, which can last up to 100,000 years, and warm periods. We call them the glacial (glacial) and interglacial (interglacial) epochs. The interglacial era is usually characterized by approximately the same conditions that we observe today: high level seas, limited areas of icing and so on. Naturally, even now there are glaciations in Antarctica, Greenland and other similar places. But in general climatic conditions relatively warm. This is the essence of interglacial: high sea level, warm temperature conditions and, in general, a fairly even climate.

But during the Ice Age mean annual temperature changes significantly, the vegetative belts are forced to shift north or south, depending on the hemisphere. Regions like Moscow or Cambridge become uninhabited, at least in winter. Although they may be habitable in summer due to the strong contrast between seasons. But what is actually happening is that the cold zones are expanding substantially, the average annual temperature is dropping, and the overall climate is getting very cold. While the largest glacial events are relatively limited in time (perhaps around 10,000 years), the entire long cold period can last 100 thousand years or even more. This is what the glacial-interglacial cycle looks like.

Due to the length of each period, it is difficult to say when we will exit the current era. This is due to plate tectonics, the location of the continents on the surface of the Earth. Currently North Pole and the South Pole are isolated: Antarctica is at the South Pole and the North Arctic Ocean in the north. Because of this, there is a problem with heat circulation. As long as the location of the continents does not change, this ice age will continue. In line with long-term tectonic changes, it can be assumed that it will take another 50 million years in the future until significant changes occur that allow the Earth to emerge from the ice age.

Geological implications

This frees up huge sections of the continental shelf that are flooded today. This will mean, for example, that one day it will be possible to walk from Britain to France, from New Guinea to South East Asia. One of the most critical places is the Bering Strait, which connects Alaska with Eastern Siberia. It is quite small, about 40 meters, so if the sea level drops to a hundred meters, then this area will become land. This is also important because plants and animals will be able to migrate through these places and get into regions where they cannot go today. Thus, the colonization of North America depends on the so-called Beringia.

Animals and the Ice Age

It is important to remember that we ourselves are the "products" of the ice age: we evolved during it, so we can survive it. However, it is not a matter of individual individuals - it is a matter of the entire population. The problem today is that there are too many of us and our activities have significantly changed the natural conditions. Under natural conditions, many of the animals and plants that we see today have a long history and survive the Ice Age well, although there are some that evolved slightly. They migrate and adapt. There are zones in which animals and plants survived the Ice Age. These so-called refugiums were located further north or south from their present distribution.

But as a result human activity some of the species died or became extinct. This has happened on every continent, with the possible exception of Africa. A huge number of large vertebrates, namely mammals, as well as marsupials in Australia, were exterminated by man. This was caused either directly by our activities, such as hunting, or indirectly by the destruction of their habitat. Animals living in northern latitudes today, in the past lived in the Mediterranean. We have destroyed this region so much that it will most likely be very difficult for these animals and plants to colonize it again.

Consequences of global warming

IN normal conditions by geological standards, we would soon enough be back in the Ice Age. But because of global warming, which is a consequence of human activity, we are postponing it. We will not be able to completely prevent it, since the causes that caused it in the past still exist today. Human activity, an unforeseen element of nature, affects atmospheric warming, which may have already caused a delay in the next glacial.

Today, climate change is a very relevant and exciting issue. If the Greenland Ice Sheet melts, sea levels will rise by six meters. In the past, during the previous interglacial epoch, which was about 125,000 years ago, the Greenland Ice Sheet melted profusely, and sea levels were 4–6 meters higher than today. It's certainly not the end of the world, but it's not time complexity either. After all, the Earth has recovered from catastrophes before, it will be able to survive this one.

The long-term outlook for the planet is not bad, but for humans, that's a different matter. The more research we do, the better we understand how the Earth is changing and where it leads, the better we understand the planet we live on. This is important because people are finally starting to think about changing sea levels, global warming and the impact of all these things on agriculture and the population. Much of this has to do with the study of ice ages. Through these studies, we will learn the mechanisms of glaciation, and we can use this knowledge proactively in an attempt to mitigate some of the changes that we ourselves are causing. This is one of the main results and one of the goals of research on ice ages.
Of course, the main consequence of the Ice Age is huge ice sheets. Where does water come from? Of course, from the oceans. What happens during ice ages? Glaciers form as a result of precipitation on land. Due to the fact that the water does not return to the ocean, the sea level falls. During the most severe glaciations, sea levels can drop by more than a hundred meters.