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A less severe cold period or ice age is shown during the Jurassic-Cretaceous (150 Ma). There have been five or six major ice ages in the history of Earth over the past 3 billion years. The Late Cenozoic Ice Age began 34 million years ago, its latest phase being the Quaternary glaciation, in progress since 2.58 million years ago.
The history of Chiloé, an archipelago in Chile's south, has been marked by its geographic and political isolation. The archipelago has been described by Renato Cárdenas, historian at the Chilean National Library, as “a distinct enclave, linked more to the sea than the continent, a fragile society with a strong sense of solidarity and a deep territorial attachment.” [1]
Last Glacial Period, not to be confused with the Last Glacial Maximum or Late Glacial Maximum below. (The following events also fall into this period.) 48,000–28,000: Mousterian Pluvial wet in North Africa 26,500–19,000: Last Glacial Maximum, what is often meant in popular usage by "Last Ice Age" 16,000–13,000
In central and southern Chile (33°–42° south), the landscape is partially covered with glacial sediments from the Andes. In Zona Austral (south of 42° south) the depression dips below sea level, appearing occasionally in islands such as Chiloé. Its southern end is the Isthmus of Ofqui.
This is a timeline of Chilean history, comprising important legal and territorial changes and political events in Chile and its predecessor states. To read about the background to these events, see History of Chile .
Throughout Earth's climate history (Paleoclimate) its climate has fluctuated between two primary states: greenhouse and icehouse Earth. [1] Both climate states last for millions of years and should not be confused with the much smaller glacial and interglacial periods, which occur as alternating phases within an icehouse period (known as an ice age) and tend to last less than one million years ...
Late Cenozoic Ice Age 33.9 million years ago to present Divisions within the current ice age For divisions prior to 33.9 million years ago, see Geologic time scale: Period Epoch Age; ↑ Paleogene: Oligocene 33.9 to 23.03 Ma (last epoch of the Paleogene Period) Pyrotherium romeroi and Rhynchippus equinus, Oligocene of South America: Rupelian 33 ...
Reconstruction of the past 5 million years of climate history, based on oxygen isotope fractionation in deep sea sediment cores (serving as a proxy for the total global mass of glacial ice sheets), fitted to a model of orbital forcing (Lisiecki and Raymo 2005) [2] and to the temperature scale derived from Vostok ice cores following Petit et al. (1999).