Contents 1 Etymology 2 Dating 3 Paleogeography and climate 3.1 Glacial features 3.2 Major events 3.3 Palaeocycles 3.3.1 Milankovitch cycles 3.3.2 Oxygen isotope ratio cycles 4 Fauna 4.1 Humans 5 Deposits 6 See also 7 References 8 External links

Etymology[edit] Charles Lyell introduced the term "pleistocene" in 1839 to describe strata in Sicily that had at least 70% of their molluscan fauna still living today. This distinguished it from the older Pliocene Epoch, which Lyell had originally thought to be the youngest fossil rock layer. He constructed the name "Pleistocene" ("Most New" or "Newest") from the Greek πλεῖστος, pleīstos, "most", and καινός, kainós (latinized as cænus), "new";[4] this contrasting with the immediately preceding Pliocene ("More New" or "Newer", from πλείων, pleíōn, "more", and kainós; usual spelling: Pliocene), and the immediately subsequent Holocene ("wholly new" or "entirely new", from ὅλος, hólos, "whole", and kainós) epoch, which extends to the present time.

Dating[edit] Human timeline view • discuss • edit -10 — – -9 — – -8 — – -7 — – -6 — – -5 — – -4 — – -3 — – -2 — – -1 — – 0 — Human-like apes Nakalipithecus Ouranopithecus Sahelanthropus Orrorin Ardipithecus Australopithecus Homo habilis Homo erectus Neanderthal Homo sapiens ← Earlier apes ← LCA-Gorilla separation ← Possibly bipedal ← LCA-Chimpanzee separation ← Earliest bipedal ← Earliest stone tools ← Earliest exit from Africa ← Earliest fire use ← Earliest in Europe ← Earliest cooking ← Earliest clothes ← Modern speech ← Modern humans P l e i s t o c e n e P l i o c e n e M i o c e n e H o m i n i d s Axis scale: millions of years ago. Also see: Life timeline and Nature timeline The Pleistocene has been dated from 2.588 million (±.005) to 11,700 years BP[5] with the end date expressed in radiocarbon years as 10,000 carbon-14 years BP.[6] It covers most of the latest period of repeated glaciation, up to and including the Younger Dryas cold spell. The end of the Younger Dryas has been dated to about 9640 BC (11,654 calendar years BP). It was not until after the development of radiocarbon dating, however, that Pleistocene archaeological excavations shifted to stratified caves and rock-shelters as opposed to open-air river-terrace sites.[7] In 2009 the International Union of Geological Sciences (IUGS) confirmed a change in time period for the Pleistocene, changing the start date from 1.806 to 2.588 million years BP, and accepted the base of the Gelasian as the base of the Pleistocene, namely the base of the Monte San Nicola GSSP.[8] The IUGS has yet to approve a type section, Global Boundary Stratotype Section and Point (GSSP), for the upper Pleistocene/Holocene boundary (i.e. the upper boundary). The proposed section is the North Greenland Ice Core Project ice core 75° 06' N 42° 18' W.[9] The lower boundary of the Pleistocene Series is formally defined magnetostratigraphically as the base of the Matuyama (C2r) chronozone, isotopic stage 103. Above this point there are notable extinctions of the calcareous nanofossils: Discoaster pentaradiatus and Discoaster surculus.[10][11] The Pleistocene covers the recent period of repeated glaciations. The name Plio-Pleistocene has, in the past, been used to mean the last ice age. The revised definition of the Quaternary, by pushing back the start date of the Pleistocene to 2.58 Ma, results in the inclusion of all the recent repeated glaciations within the Pleistocene.

Paleogeography and climate[edit] The maximum extent of glacial ice in the north polar area during the Pleistocene period. The modern continents were essentially at their present positions during the Pleistocene, the plates upon which they sit probably having moved no more than 100 km relative to each other since the beginning of the period. According to Mark Lynas (through collected data), the Pleistocene's overall climate could be characterized as a continuous El Niño with trade winds in the south Pacific weakening or heading east, warm air rising near Peru, warm water spreading from the west Pacific and the Indian Ocean to the east Pacific, and other El Niño markers.[12] Glacial features[edit] 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. (May 2015) (Learn how and when to remove this template message) Pleistocene climate was marked by repeated glacial cycles in which continental glaciers pushed to the 40th parallel in some places. It is estimated that, at maximum glacial extent, 30% of the Earth's surface was covered by ice. In addition, a zone of permafrost stretched southward from the edge of the glacial sheet, a few hundred kilometres in North America, and several hundred in Eurasia. The mean annual temperature at the edge of the ice was −6 °C (21 °F); at the edge of the permafrost, 0 °C (32 °F). Each glacial advance tied up huge volumes of water in continental ice sheets 1,500 to 3,000 metres (4,900–9,800 ft) thick, resulting in temporary sea-level drops of 100 metres (300 ft) or more over the entire surface of the Earth. During interglacial times, such as at present, drowned coastlines were common, mitigated by isostatic or other emergent motion of some regions. The effects of glaciation were global. Antarctica was ice-bound throughout the Pleistocene as well as the preceding Pliocene. The Andes were covered in the south by the Patagonian ice cap. There were glaciers in New Zealand and Tasmania. The current decaying glaciers of Mount Kenya, Mount Kilimanjaro, and the Ruwenzori Range in east and central Africa were larger. Glaciers existed in the mountains of Ethiopia and to the west in the Atlas mountains. In the northern hemisphere, many glaciers fused into one. The Cordilleran ice sheet covered the North American northwest; the east was covered by the Laurentide. The Fenno-Scandian ice sheet rested on northern Europe, including Great Britain; the Alpine ice sheet on the Alps. Scattered domes stretched across Siberia and the Arctic shelf. The northern seas were ice-covered. South of the ice sheets large lakes accumulated because outlets were blocked and the cooler air slowed evaporation. When the Laurentide ice sheet retreated, north central North America was totally covered by Lake Agassiz. Over a hundred basins, now dry or nearly so, were overflowing in the North American west. Lake Bonneville, for example, stood where Great Salt Lake now does. In Eurasia, large lakes developed as a result of the runoff from the glaciers. Rivers were larger, had a more copious flow, and were braided. African lakes were fuller, apparently from decreased evaporation. Deserts on the other hand were drier and more extensive. Rainfall was lower because of the decreases in oceanic and other evaporation. It has been estimated that during the Pleistocene, the East Antarctic Ice Sheet thinned by at least 500 meters, and that thinning since the Last Glacial Maximum is less than 50 meters and probably started after ca 14 ka.[13] Major events[edit] Further information: Timeline of glaciation Ice ages as reflected in atmospheric CO2, stored in bubbles from glacial ice of Antarctica. Over 11 major glacial events have been identified, as well as many minor glacial events.[14] A major glacial event is a general glacial excursion, termed a "glacial." Glacials are separated by "interglacials". During a glacial, the glacier experiences minor advances and retreats. The minor excursion is a "stadial"; times between stadials are "interstadials". These events are defined differently in different regions of the glacial range, which have their own glacial history depending on latitude, terrain and climate. There is a general correspondence between glacials in different regions. Investigators often interchange the names if the glacial geology of a region is in the process of being defined. However, it is generally incorrect to apply the name of a glacial in one region to another. For most of the 20th century only a few regions had been studied and the names were relatively few. Today the geologists of different nations are taking more of an interest in Pleistocene glaciology. As a consequence, the number of names is expanding rapidly and will continue to expand. Many of the advances and stadials remain unnamed. Also, the terrestrial evidence for some of them has been erased or obscured by larger ones, but evidence remains from the study of cyclical climate changes. The glacials in the following tables show historical usages, are a simplification of a much more complex cycle of variation in climate and terrain, and are generally no longer used. These names have been abandoned in favor of numeric data because many of the correlations were found to be either inexact or incorrect and more than four major glacials have been recognized since the historical terminology was established.[14][15][16] Historical names of the "four major" glacials in four regions. Region Glacial 1 Glacial 2 Glacial 3 Glacial 4 Alps Günz Mindel Riss Würm North Europe Eburonian Elsterian Saalian Weichselian British Isles Beestonian Anglian Wolstonian Devensian Midwest U.S. Nebraskan Kansan Illinoian Wisconsinan Historical names of interglacials. Region Interglacial 1 Interglacial 2 Interglacial 3 Alps Günz-Mindel Mindel-Riss Riss-Würm North Europe Waalian Holsteinian Eemian British Isles Cromerian Hoxnian Ipswichian Midwest U.S. Aftonian Yarmouthian Sangamonian Corresponding to the terms glacial and interglacial, the terms pluvial and interpluvial are in use (Latin: pluvia, rain). A pluvial is a warmer period of increased rainfall; an interpluvial, of decreased rainfall. Formerly a pluvial was thought to correspond to a glacial in regions not iced, and in some cases it does. Rainfall is cyclical also. Pluvials and interpluvials are widespread. There is no systematic correspondence of pluvials to glacials, however. Moreover, regional pluvials do not correspond to each other globally. For example, some have used the term "Riss pluvial" in Egyptian contexts. Any coincidence is an accident of regional factors. Only a few of the names for pluvials in restricted regions have been strategraphically defined. Palaeocycles[edit] The sum of transient factors acting at the Earth's surface is cyclical: climate, ocean currents and other movements, wind currents, temperature, etc. The waveform response comes from the underlying cyclical motions of the planet, which eventually drag all the transients into harmony with them. The repeated glaciations of the Pleistocene were caused by the same factors. Milankovitch cycles[edit] Main article: Milankovitch cycles Glaciation in the Pleistocene was a series of glacials and interglacials, stadials and interstadials, mirroring periodic changes in climate. The main factor at work in climate cycling is now believed to be Milankovitch cycles. These are periodic variations in regional and planetary solar radiation reaching the Earth caused by several repeating changes in the Earth's motion. Milankovitch cycles cannot be the sole factor responsible for the variations in climate since they explain neither the long term cooling trend over the Plio-Pleistocene, nor the millennial variations in the Greenland Ice Cores. Milankovitch pacing seems to best explain glaciation events with periodicity of 100,000, 40,000, and 20,000 years. Such a pattern seems to fit the information on climate change found in oxygen isotope cores. The timing of our present interglacial interval (known as the Holocene, Postglacial, or the Present Interglacial) to that of the previous interglacial, beginning about 130,000 years ago (The Eemian Interglacial), suggests that the next glacial might begin in about 3,000 years.[citation needed] Oxygen isotope ratio cycles[edit] Main article: Oxygen isotope ratio cycle In oxygen isotope ratio analysis, variations in the ratio of 18O to 16O (two isotopes of oxygen) by mass (measured by a mass spectrometer) present in the calcite of oceanic core samples is used as a diagnostic of ancient ocean temperature change and therefore of climate change. Cold oceans are richer in 18O, which is included in the tests of the microorganisms (foraminifera) contributing the calcite. A more recent version of the sampling process makes use of modern glacial ice cores. Although less rich in 18O than sea water, the snow that fell on the glacier year by year nevertheless contained 18O and 16O in a ratio that depended on the mean annual temperature. Temperature and climate change are cyclical when plotted on a graph of temperature versus time. Temperature coordinates are given in the form of a deviation from today's annual mean temperature, taken as zero. This sort of graph is based on another of isotope ratio versus time. Ratios are converted to a percentage difference from the ratio found in standard mean ocean water (SMOW). The graph in either form appears as a waveform with overtones. One half of a period is a Marine isotopic stage (MIS). It indicates a glacial (below zero) or an interglacial (above zero). Overtones are stadials or interstadials. According to this evidence, Earth experienced 102 MIS stages beginning at about 2.588 Ma BP in the Early Pleistocene Gelasian. Early Pleistocene stages were shallow and frequent. The latest were the most intense and most widely spaced. By convention, stages are numbered from the Holocene, which is MIS1. Glacials receive an even number; interglacials, odd. The first major glacial was MIS2-4 at about 85–11 ka BP. The largest glacials were 2, 6, 12, and 16; the warmest interglacials, 1, 5, 9 and 11. For matching of MIS numbers to named stages, see under the articles for those names.

Fauna[edit] See also: Quaternary extinction event Both marine and continental faunas were essentially modern but with many more large land mammals such as Mammoths, Mastodons, Diprotodon, Smilodon, Aurochs, Short-faced bear, giant sloths, Gigantopithecus and others. Isolated places such as Australia, Madagascar, New Zealand and islands in the Pacific saw the evolution of large birds and even reptiles such as the Elephant bird, moa, Haast's eagle, Quinkana, Megalania and Meiolania. Pleistocene of Northern Spain showing woolly mammoth, cave lions eating a reindeer, tarpans, and woolly rhinoceros. Pleistocene of South America showing Megatherium and two Glyptodon. The severe climatic changes during the ice age had major impacts on the fauna and flora. With each advance of the ice, large areas of the continents became totally depopulated, and plants and animals retreating southward in front of the advancing glacier faced tremendous stress. The most severe stress resulted from drastic climatic changes, reduced living space, and curtailed food supply. A major extinction event of large mammals (megafauna), which included mammoths, mastodons, saber-toothed cats, glyptodons, the woolly rhinoceros, various giraffids, such as the Sivatherium; ground sloths, Irish elk, cave bears, Deinotheriidae, Gomphothere, bear dogs, dire wolves, and short-faced bears, began late in the Pleistocene and continued into the Holocene. Neanderthals also became extinct during this period. At the end of the last ice age, cold-blooded animals, smaller mammals like wood mice, migratory birds, and swifter animals like whitetail deer had replaced the megafauna and migrated north. The extinctions were especially severe in North America where native horses and camels were eliminated. Asian land mammal ages (ALMA) include Zhoukoudianian, Nihewanian, and Yushean. European land mammal ages (ELMA) include Gelasian (2.5—1.8 Ma). North American land mammal ages (NALMA) include Blancan (4.75–1.8), Irvingtonian (1.8–0.24) and Rancholabrean (0.24–0.01) in millions of years. The Blancan extends significantly back into the Pliocene. South American land mammal ages (SALMA) include Uquian (2.5–1.5), Ensenadan (1.5–0.3) and Lujanian (0.3–0.01) in millions of years. The Uquian previously extended significantly back into the Pliocene, although the new definition places it entirely within the Pleistocene. Humans[edit] Main articles: Human evolution, Paleolithic, and Models of migration to the New World The evolution of anatomically modern humans took place during the Pleistocene.[17][18] In the beginning of the Pleistocene Paranthropus species are still present, as well as early human ancestors, but during the lower Palaeolithic they disappeared, and the only hominin species found in fossilic records is Homo erectus for much of the Pleistocene. Acheulean lithics appear along with Homo erectus, some 1.8 million years ago, replacing the more primitive Oldowan industry used by A. garhi and by the earliest species of Homo. The Middle Paleolithic saw more varied speciation within Homo, including the appearance of Homo sapiens about 200,000 years ago. According to mitochondrial timing techniques, modern humans migrated from Africa after the Riss glaciation in the Middle Palaeolithic during the Eemian Stage, spreading all over the ice-free world during the late Pleistocene.[19][20][21] A 2005 study posits that humans in this migration interbred with archaic human forms already outside of Africa by the late Pleistocene, incorporating archaic human genetic material into the modern human gene pool.[22] Hominin species during Pleistocene

Deposits[edit] Pleistocene non-marine sediments are found primarily in fluvial deposits, lakebeds, slope and loess deposits as well as in the large amounts of material moved about by glaciers. Less common are cave deposits, travertines and volcanic deposits (lavas, ashes). Pleistocene marine deposits are found primarily in shallow marine basins mostly (but with important exceptions) in areas within a few tens of kilometers of the modern shoreline. In a few geologically active areas such as the Southern California coast, Pleistocene marine deposits may be found at elevations of several hundred meters.

See also[edit] Climate state Geologic time scale Pleistocene megafauna Timeline of glaciation

References[edit] ^ ^ Jones, Daniel (2003) [1917], Peter Roach, James Hartmann and Jane Setter, eds., English Pronouncing Dictionary, Cambridge: Cambridge University Press, ISBN 3-12-539683-2 CS1 maint: Uses editors parameter (link) ^ "Gibbard, P. and van Kolfschoten, T. (2004) "The Pleistocene and Holocene Epochs" Chapter 22" (PDF).  (3.1 MB) In Gradstein, F. M., Ogg, James G., and Smith, A. Gilbert (eds.), A Geologic Time Scale 2004 Cambridge University Press, Cambridge, ISBN 0-521-78142-6 ^ "Pleistocene". Online Etymology Dictionary.  ^ "Major Divisions". Subcommission on Quaternary Stratigraphy. International Commission on Stratigraphy. 4 January 2016. Retrieved 25 January 2017.  ^ For the top of the series, see: Lourens, L., Hilgen, F., Shackleton, N.J., Laskar, J., Wilson, D., (2004) "The Neogene Period". In: Gradstein, F., Ogg, J., Smith, A.G. (Eds.), A Geologic Time Scale 2004. Cambridge: Cambridge University Press. ^ Moore, Mark; Brumm (2007). "Stone artifacts and hominins in island Southeast Asia: New insights from Flores, eastern Indonesia". Journal of Human Evolution. 52: 88. doi:10.1016/j.jhevol.2006.08.002. PMID 17069874. Retrieved 10 April 2014.  ^ Riccardi, Alberto C. (30 June 2009) "IUGS ratified ICS Recommendation on redefinition of Pleistocene and formal definition of base of Quaternary" International Union of Geological Sciences ^ Svensson, A.; Nielsen, S. W.; Kipfstuhl, S.; Johnsen, S. J.; Steffensen, J. P.; Bigler, M.; Ruth, U.; Röthlisberger, R. (2005). "Visual stratigraphy of the North Greenland Ice Core Project (NorthGRIP) ice core during the last glacial period". Journal of Geophysical Research. 110: D02108. Bibcode:2005JGRD..110.2108S. doi:10.1029/2004jd005134.  ^ Gradstein, Felix M.; Ogg, James G. and Smith, A. Gilbert (eds.) (2005) A Geologic Time Scale 2004 Cambridge University Press, Cambridge, UK, p. 28, ISBN 0-521-78142-6 ^ Rio, D.; Sprovieri, R.; Castradori, D.; Di Stefano, E. (1998). "The Gelasian Stage (Upper Pliocene): a new unit of the global standard chronostratigraphic scale". Episodes. 21: 82–87.  ^ National Geographic Channel, Six Degrees Could Change The World, Mark Lynas interview. Retrieved February 14, 2008. ^ Yusuke Suganuma, Hideki Miura, Albert Zondervan, Jun'ichi Okuno (August 2014). "East Antarctic deglaciation and the link to global cooling during the Quaternary: evidence from glacial geomorphology and 10Be surface exposure dating of the Sør Rondane Mountains, Dronning Maud Land". Quaternary Science Reviews. 97: 102–120. doi:10.1016/j.quascirev.2014.05.007. CS1 maint: Uses authors parameter (link) ^ a b Richmond, G.M.; Fullerton, D.S. (1986). "Summation of Quaternary glaciations in the United States of America". Quaternary Science Reviews. 5: 183–196. doi:10.1016/0277-3791(86)90184-8.  ^ Roy, M., P.U. Clark, R.W. Barendregt, J.R., Glasmann, and R.J. Enkin, 2004, Glacial stratigraphy and paleomagnetism of late Cenozoic deposits of the north-central United States, PDF version, 1.2 MB. Geological Society of America Bulletin.116(1-2): pp. 30-41; doi:10.1130/B25325.1 ^ Aber, J.S. (1991) "Glaciations of Kansas" Boreas 20(4): pp. 297-314 - (contains a summary of how and why the Nebraskan, Aftonian, Kansan, and Yarmouthian stages were abandoned by modern stratigraphers). ^ Rogers, A.R.; Jorde, L.B. (1995). "Genetic evidence on modern human origins". Human Biology. 67: 1–36.  ^ Wall, J.D.; Przeworski, M. (2000). "When did the human population start increasing?". Genetics. 155: 1865–1874.  ^ Cann, R.L.; Stoneking, M.; Wilson, A.C. (1987). "Mitochondrial DNA and human evolution". Nature. 325: 31–36. doi:10.1038/325031a0. PMID 3025745.  ^ Stringer, C.B. (1992) "Evolution of early modern humans" In: Jones, Steve; Martin, R. and Pilbeam, David R. (eds.) (1992) The Cambridge encyclopedia of human evolution Cambridge University Press, Cambridge, ISBN 0-521-32370-3, pp. 241–251. ^ Templeton, A. R. (2002). "Out of Africa again and again" (PDF). Nature. 416 (6876): 45–51. doi:10.1038/416045a.  ^ Eswarana, Vinayak; Harpendingb, Henry; Rogers, Alan R (2005). "Genomics refutes an exclusively African origin of humans". Journal of Human Evolution. 49 (1): 1–18. doi:10.1016/j.jhevol.2005.02.006. PMID 15878780.  Ogg, Jim; June, 2004, Overview of Global Boundary Stratotype Sections and Points (GSSP's,, Accessed April 30, 2006.

External links[edit] Wikimedia Commons has media related to Pleistocene. Wikisource has original works on the topic: Cenozoic#Quaternary Late Pleistocene environments of the southern high plains, 1975, edited by Wendorf and Hester. Pleistocene Microfossils: 50+ images of Foraminifera Stepanchuk V.N., Sapozhnykov I.V. Nature and man in the pleistocene of Ukraine. 2010 Human Timeline (Interactive) – Smithsonian, National Museum of Natural History (August 2016). v t e Quaternary Period Pleistocene Epoch Holocene Epoch Early Middle Late Preboreal Boreal Atlantic Subboreal Subatlantic v t e Geologic history of Earth Cenozoic era¹ (present–66.0 Mya) Quaternary (present–2.588 Mya) Holocene (present–11.784 kya) Pleistocene (11.784 kya–2.588 Mya) Neogene (2.588–23.03 Mya) Pliocene (2.588–5.333 Mya) Miocene (5.333–23.03 Mya) Paleogene (23.03–66.0 Mya) Oligocene (23.03–33.9 Mya) Eocene (33.9–56.0 Mya) Paleocene (56.0–66.0 Mya) Mesozoic era¹ (66.0–252.17 Mya) Cretaceous (66.0–145.0 Mya) Late (66.0–100.5 Mya) Early (100.5–145.0 Mya) Jurassic (145.0–201.3 Mya) Late (145.0–163.5 Mya) Middle (163.5–174.1 Mya) Early (174.1–201.3 Mya) Triassic (201.3–252.17 Mya) Late (201.3–237 Mya) Middle (237–247.2 Mya) Early (247.2–252.17 Mya) Paleozoic era¹ (252.17–541.0 Mya) Permian (252.17–298.9 Mya) Lopingian (252.17–259.8 Mya) Guadalupian (259.8–272.3 Mya) Cisuralian (272.3–298.9 Mya) Carboniferous (298.9–358.9 Mya) Pennsylvanian (298.9–323.2 Mya) Mississippian (323.2–358.9 Mya) Devonian (358.9–419.2 Mya) Late (358.9–382.7 Mya) Middle (382.7–393.3 Mya) Early (393.3–419.2 Mya) Silurian (419.2–443.8 Mya) Pridoli (419.2–423.0 Mya) Ludlow (423.0–427.4 Mya) Wenlock (427.4–433.4 Mya) Llandovery (433.4–443.8 Mya) Ordovician (443.8–485.4 Mya) Late (443.8–458.4 Mya) Middle (458.4–470.0 Mya) Early (470.0–485.4 Mya) Cambrian (485.4–541.0 Mya) Furongian (485.4–497 Mya) Series 3 (497–509 Mya) Series 2 (509–521 Mya) Terreneuvian (521–541.0 Mya) Proterozoic eon² (541.0 Mya–2.5 Gya) Neoproterozoic era (541.0 Mya–1 Gya) Ediacaran (541.0-~635 Mya) Cryogenian (~635-~720 Mya) Tonian (~720 Mya-1 Gya) Mesoproterozoic era (1–1.6 Gya) Stenian (1-1.2 Gya) Ectasian (1.2-1.4 Gya) Calymmian (1.4-1.6 Gya) Paleoproterozoic era (1.6–2.5 Gya) Statherian (1.6-1.8 Gya) Orosirian (1.8-2.05 Gya) Rhyacian (2.05-2.3 Gya) Siderian (2.3-2.5 Gya) Archean eon² (2.5–4 Gya) Eras Neoarchean (2.5–2.8 Gya) Mesoarchean (2.8–3.2 Gya) Paleoarchean (3.2–3.6 Gya) Eoarchean (3.6–4 Gya) Hadean eon² (4–4.6 Gya)     kya = thousands years ago. Mya = millions years ago. Gya = billions years ago.¹ = Phanerozoic eon. ² = Precambrian supereon. Source: (2015/01). International Commission on Stratigraphy. Retrieved 13 July 2015. Divisions of Geologic Time—Major Chronostratigraphic and Geochronologic Units USGS Retrieved 10 March 2013. v t e Continental glaciations General Canadian Shield Glacial history of Minnesota Lake Agassiz Lake Chicago Lake Tight Last Glacial Maximum Laurentide Ice Sheet List of prehistoric lakes Post-glacial rebound Proglacial lake Teays River Timeline of glaciation Landforms Erosional Fjord Glacial striae Ribbon lake Roche moutonnée Tunnel valley U-shaped valley Depositional Drumlin Drumlin field Erratic block Moraine Pulju moraine Rogen moraine Terminal moraine Till plain Veiki moraine Glacifluvial Diluvium Esker Giant current ripples Kame Kame delta Kettle hole Outwash fan Sandur North American places Canada Arrowhead Provincial Park, Ontario Big Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics Train, Alberta Lion's Head Provincial Park, Ontario Origin of the Oak Ridges Moraine, Ontario Ovayok Territorial Park, Nunavut United States Chippewa Moraine State Recreation Area, Wisconsin Coteau des Prairies, South Dakota Devil's Lake State Park, Wisconsin Glacial Lake Wisconsin, Wisconsin Glacial Lakes State Park, Minnesota Horicon Marsh State Wildlife Area, Wisconsin Ice Age Floods National Geologic Trail, Idaho, Oregon & Washington Ice Age National Scientific Reserve, Wisconsin Ice Age Trail, Wisconsin Interstate State Park, Minnesota & Wisconsin Kelleys Island, Ohio Kettle Moraine State Forest, Wisconsin Lake Bonneville, Utah Lake Lahontan, Nevada Lake Missoula, Montana Mill Bluff State Park, Wisconsin Oneida Lake, New York Two Creeks Buried Forest State Natural Area, Wisconsin Withrow Moraine and Jameson Lake Drumlin Field, Washington Yosemite National Park, California Eurasian and Antarctic places Antarctica Hardangerfjord Killary Harbour Lambert Glacier Monte Rosa Ross Ice Shelf Svalbard Time periods Illinoian Stage Interglacial Interstadial Last glacial 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Gravettian culture Hafting Hand axe Grooves Langdale axe industry Levallois technique Lithic core Lithic reduction analysis debitage flake Lithic technology Magdalenian culture Metallurgy Microblade technology Mining Prepared-core technique Solutrean industry Striking platform Tool stone Uniface Yubetsu technique Other tools Adze Awl bone Axe Bannerstone Blade prismatic Bone tool Bow drill Burin Canoe Oar Pesse canoe Chopper tool Cleaver Denticulate tool Fire plough Fire-saw Hammerstone Knife Microlith Quern-stone Racloir Rope Scraper side Stone tool Tally stick Weapons Wheel illustration Architecture Ceremonial Göbekli Tepe Kiva Standing stones megalith row Stonehenge Pyramid Dwellings Neolithic architecture British megalith architecture Nordic megalith architecture Burdei Cave Cliff dwelling Dugout Hut Quiggly hole Jacal Longhouse Mud brick Mehrgarh Neolithic long house Pit-house Pueblitos Pueblo Rock shelter Blombos Cave Abri de la Madeleine Sibudu Cave Stone roof Roundhouse Stilt 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list British Isles and Brittany Venus figurines Burial Burial mounds Bowl barrow Round barrow Mound Builders culture U.S. sites Chamber tomb Severn-Cotswold Cist Dartmoor kistvaens Clava cairn Court tomb Cremation Dolmen Great dolmen Funeral pyre Gallery grave transepted wedge-shaped Grave goods Jar burial Long barrow unchambered Grønsalen Megalithic tomb Mummy Passage grave Rectangular dolmen Ring cairn Simple dolmen Stone box grave Tor cairn Tumulus Unchambered long cairn Other cultural Astronomy sites lunar calendar Behavioral modernity Origin of language trepanning Prehistoric medicine Evolutionary musicology music archaeology Prehistoric music Alligator drum flutes Divje Babe flute gudi Prehistoric numerals Origin of religion Paleolithic religion Prehistoric religion Spiritual drug use Prehistoric warfare Symbols symbolism Anthropology portal Earth sciences portal Evolutionary biology portal Geology portal Paleontology portal Authority control GND: 4046350-3 NDL: 00566708 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Pleistocene - Photos and All Basic Informations

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PueblitosPuebloRock ShelterBlombos CaveAbri De La MadeleineSibudu CaveNess Of BrodgarRoundhouse (dwelling)Stilt HousePrehistoric Pile Dwellings Around The AlpsWattle And DaubCheck DamCisternFlush ToiletReservoirWater WellFeature (archaeology)BrochBurnt MoundFulacht FiadhCausewayed EnclosureTor EnclosureNeolithic Circular Enclosures In Central EuropeGoseck CircleCursusHengeThornborough HengesList Of Oldest BuildingsMegalithic Architectural ElementsMiddenTimber CircleTimber TrackwaySweet TrackPrehistoric ArtBasket WeavingBeadworkBedChalcolithicHistory Of Clothing And TextilesTimeline Of Clothing And Textiles TechnologyHistory Of CosmeticsMiddle Stone AgeHistory Of Hide MaterialsShoeÖtziJewelleryAmberMirrorPotteryCardium PotteryGrooved WareLinear Pottery CultureJōmon PotteryUnstan WareSewing NeedleWeavingHistory Of WineAreni-1 WineryHistory Of The Wine PressPrehistoric ArtCategory:Prehistoric ArtArt Of The Upper PaleolithicArt Of The Middle PaleolithicBlombos CaveList Of Stone Age ArtBird 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