Ice age

An ice age is a period of time in which the Earth's temperature is too low for the winter ice to melt back fully during summer. Ice ages, of which there have been many, are characterised by massive glaciers covering the subpolar and mountainous parts of the world, and by a lowering of sea levels. Evidence of ice ages was first discovered by Swiss geologists in the 17th century, after they realised that scratched rocks, u-shaped valleys and boulder depositions in the lowlands of the country were similar to glacial effects further up.Quaternary Ice Ages and Dating Techniques These glaciation remains have since been found in many parts of the world, and have been dated to several geological periods.
A very extreme ice age could lead to complete coverage of Earth in an ice sheet. This is often referred to as a "snowball Earth". However, whether this has actually happened in the past (or if it is even possible) is still a hotly debated topic in palaeogeography.
==Ice age vs glaciation==
By the usual geological definition of the term, an ice age occurs whenever there are fairly extensive ice sheets at the poles, which are the coldest parts of the surface, not taking into account high mountains which are possibly colder because of altitude effects. By this definition, we are still living in an ice age as Antarctica and the counter-intuitively named Greenland are both extensively covered by ice. In the more popular definition used, the term refers to extreme levels of ice coverage, where polar ice extends much closer to the equator than at present.
This latter definition is much closer to that of a glaciation. The present ice age has been made up of numerous glacial and interglacial periods, where the Earth has been cold and lukewarmLike it is now. respectively. Together, they make up an ice age. However, it is also possible for an ice age to be made up of only a single glacial event — it depends on the underlying cause of the age.
==Known ice ages==
Our knowledge of this aspect of Earth's temperature record is likely to be incomplete, as glaciations tend to obliterate evidence of their predecessors. However, we know of a number of ice ages that have occurred over the course of Earth's history. For further information on these events, see .
===Huronian glaciation===
The Huronian glaciation is the earliest known ice age, caused by the . The build-up of oxygen in the Earth's atmosphere oxidised atmospheric methane, weakening the greenhouse effect and causing global temperatures to drop drastically. This ice age began around 2.4 billion years ago, and lasted 300 million years.Context It was one of the most severe of all the ice ages.
===Cryogenian===
The Cryogenian was a geologic period from 850 to 635 million years ago.Context This period included both the Sturtian and Marinoan glaciations, the greatest glaciations known.Though not all of the period was glaciation. It is these glaciations that are the basis of the concept of the "snowball Earth," however there is much controversy as to whether they entailed a global glacier, or whether the term should instead be "slushball Earth." It is argued that photosynthesising life could not have survived in a world covered completely by ice — breaks in the coating must have existed throughout..
A third, earlier glaciation may also have occurred during this period — the Kaigas. However, this is debated. Also taking place in the Cryogenian was the breakup of the supercontinent and the formation of the supercontinent — tt is not impossible that this had something to do with the glaciations.
===Andean-Saharan ice age===
We have evidence of glaciation between 460 and 430 million years agoContext in the Andes mountains, Arabia, the central Sahara, the lower Amazon, and Western Africa (in no particular order).Major glaciations in Earth history At this time these areas were part of the continent of Gondwana, which was located where Antarctica is now.
===Karoo ice age===
The Karoo ice age was between 360 and 260 million years ago.Context It was caused by the formation of the supercontinent of and the associated closure of the Rheic and Iapetus Oceans. We know of two glaciations in this ice age, centred in different locations — in the first, from 359.2 to 318.1 mya, glaciers expanded from what is now Africa and South America; in the second, 318.1–299 mya, they were centred in Australia and India.
===Quaternary glaciation===
The Quaternary glaciation began 2.58 million years ago and continues to the present,Context and is thus the current ice age. This ice age is the most well known, for obvious reasons, and has so far included dozens of glacial and interglacial periods.
====Past====
The precise cause of the last ice age is unknown. It probably had something to do with astronomical cycles, the composition of the atmosphere, plate tectonics and/or ocean currents. Whatever the cause, the Earth's temperature has been cycling between the present temperature and bloody freezing for the last two and a half million years. During the height of the glacial periods, ice sheets covered much of Northern Europe and North America; in interglacials this reduced to merely Greenland and Antarctica. The majority of the variability in ice cover, therefore, has been in the Northern Hemisphere — this is in contrast to many of the previous ice ages which have been Southern Hemisphere-based.
The glaciations of the last hundred thousand years or so have repeated in a 40,000 year cycle related to the changes in the Earth's orbit around the Sun, with the Earth coming out of glaciation when the time of Perihelion (when earth is closest to the Sun) aligns with the summer solstice of the Southern Hemisphere. Deglaciations tend to be fairly rapid, while the descent back into cooler weather happens much slower.
====Present====
The last glacial maximum was around 18,000 years ago, and we entered the present interglacial 10,000 years ago — but we are by no means out of the ice age as a whole. Since then the climate has fluctuated around the average temperature of 15°C (59°F). Due to the nature of the return to glaciation in this particular ice age it is possible that the cooling period known as the "little ice age" was, in fact, the first sign of this - certainly, there was much fear around the 1960's that we were slipping back into one. In 1971, Gordon Rattray Taylor's scaremongering non-fiction The Doomsday Book predicted that temperatures would fall by 4° F (2.2° C) by 1975 with a new ice age due by 1980.State of Emergency, Dominic Sandbrook, Penguin, p 181
====Future====
However, by the 1970s evidence mounted that – within only a few years – warming caused by emissions of CO2 would overwhelm any natural cooling trend. The average temperature of Earth's troposphere has been steadily increasing since the 1980s, and there is no indication that glaciers will make it to the borders of London any time soon.
The consequences of this warming over the longer term in the context of the still-ongoing quaternary ice age remain debatable. Various mixes of the following are up for consideration:
*Runaway global warming, with the methane trapped in the permafrost being released etc, turns the Earth into a clone of Venus.The planet, not the Goddess. The oceans boil, water splits into its component hydrogen and oxygen, lead melts... that kind of thing.
*Runaway global warming is sufficient to permanently break us out of this ice age, but the Venus thing doesn't happen.
*We fuck the climate up to such an extent that it reverts to glaciation in protest.Or rather, the Gulf Stream ceases to reach Europe, causing a freeze there that increases the albedo of the Earth as a whole, cooling the planet.
*Things get toasty for a few hundred or thousand years, but in 20,000 years we're covered in glaciers nonetheless.
*Global warming is a hoax perpetrated by liberals, and any temperature increase in the short term is just part of a natural cycle: we freeze anyway.
*Ice ages are also a hoax, temperatures aren't going anywhere, and we're all going to get raptured shortly anyway.And if you believe that one you can go back to CreationWiki
At this stage we can probably rule out the last two, but the rest remain contenders.
==See also==
*Global warming
==Notes==
==References==
Category:Geology
Category:Climatology