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Warmer periods within an ice age
An interglacial period (or alternatively interglacial, interglaciation) is a geological interval of warmer global average temperature lasting thousands
Interglacial
Interglacial period which began 130,000 years ago
The Last Interglacial was the interglacial period that began about 130,000 years ago at the end of the Penultimate Glacial Period, and ended about 115
Last_Interglacial
Period of long-term reduction in temperature of Earth's surface and atmosphere
periods are called glacials or ice ages, and warmer periods are called interglacials. Earth's climate alternates between icehouse and greenhouse periods
Ice_age
Current geological epoch
Pleistocene together form the Quaternary period. The Holocene is an interglacial period within the ongoing glacial cycles of the Quaternary, and is equivalent
Holocene
Geological era
ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods
Glacial_period
Northwest European equivalent of the Holocene epoch
The Flandrian interglacial or stage is the regional name given by geologists and archaeologists in the British Isles to the period from around 12,000 years
Flandrian_interglacial
Chronology of the major ice ages of the Earth
referred to as glacial periods and interglacial periods, respectively. The Earth is currently in such an interglacial period of the Quaternary glaciation
Timeline_of_glaciation
Series of alternating glacial and interglacial periods
the Pleistocene glaciation, is an alternating series of glacial and interglacial periods during the Quaternary period that began 2.58 Ma (million years
Quaternary_glaciation
interglacial (German: Donau-Günz-Interglazial), Danube-Gunz warm period (Donau-Günz-Warmzeit), often just Danube-Gunz, or also Uhlenberg interglacial
Danube-Gunz_interglacial
First epoch of the Quaternary Period
glacial cycle, oscillating between cold glacial periods and warmer interglacials, with sea levels dropping at peak glaciation by as much 120 metres (390 ft)
Pleistocene
The Gunz-Haslach interglacial (German: Günz-Haslach-Interglazial) and the Gunz-Haslach warm period (Günz-Haslach-Warmzeit) are historical terms for a hypothetical
Gunz-Haslach_interglacial
Marine Isotope Stage 9 (MIS 9) was an interglacial (warm) Marine Isotope Stage. It was the last period of the Lower Paleolithic. Estimates of its dating
Marine_Isotope_Stage_9
Holstein or Holsteinian interglacial (German: Holstein-Warmzeit or Holstein-Interglazial), also called the Mindel-Riss interglacial (Mindel-Riß-Interglazial)
Holstein_interglacial
Ice age of the last 34 million years, in particular in Antarctica
decreasing mean temperatures and increasing amplitudes between glacials and interglacials. During the glacial periods of the Pleistocene, large areas of northern
Late_Cenozoic_Ice_Age
Stage of the Pleistocene Epoch
termination of the Penultimate Glacial Period and the onset of the Last Interglacial period (corresponding to the beginning of Marine Isotope Stage 5). The
Middle_Pleistocene
Period of major glaciations of the Northern Hemisphere (115,000–12,000 years ago)
also known as the last glacial cycle, occurred from the end of the Last Interglacial to the beginning of the Holocene, c. 115,000 – c. 11,700 years ago, and
Last_Glacial_Period
Interglacial period of history of the British Isles during the middle Pleistocene
Pleistocene stage of the geological history of the British Isles. It was an interglacial which preceded the Wolstonian Stage and followed the Anglian Stage. It
Hoxnian_Stage
Ancient warm and cool periods
odd-numbered stages are lows in the oxygen-18 figures, representing warm interglacial intervals. The data are derived from pollen and foraminifera (plankton)
Marine_isotope_stages
Opposing climate states on Earth
of years and should not be confused with the much smaller glacial and interglacial periods, which occur as alternating phases within an icehouse period
Greenhouse_and_icehouse_Earth
The Haslach-Mindel interglacial (German: Haslach-Mindel-Interglazial) and the Haslach-Mindel warm period (Haslach-Mindel-Warmzeit) are historical terms
Haslach-Mindel_interglacial
Early and middle Pleistocene glacial and interglacial periods in North America
Quaternary geologists for the early and middle Pleistocene glacial and interglacial periods of geologic time in North America from ~2.5–0.2 Ma (million years
Pre-Illinoian
Country in Northwestern Europe and the Caribbean
coastal and aeolian derived sediments during the Pleistocene glacial and interglacial periods. Nearly the entire west Netherlands is composed of the Rhine-Meuse
Netherlands
Glaciation in North America during the Last Glacial Period
000 to 11,000 years ago, between the Sangamonian Stage and the current interglacial, the Holocene. The maximum ice extent occurred about 25,000–21,000 years
Wisconsin_glaciation
Peninsula located in northern Antarctica
of the West Antarctic Ice Sheet has fluctuated in response to glacial–interglacial cycles. During glacial epochs, this ice sheet was significantly thicker
Antarctic_Peninsula
Moraine relief in Ivrea, Italy
periods of time between two successive glacial pulsations are called interglacial periods and are characterized, in mountainous and foothill areas, by
Ivrea_Morainic_Amphitheatre
Cave in France alternately inhabited by Neanderthals and Upper Paleolithic Modern Humans
populations. During the earliest period, the Last Interglacial (Eemian), a particularly temperate interglacial period, temperatures were very high for about
Mandrin_Cave
Transition from full glacial conditions during ice ages to warm interglacial conditions
the transition from full glacial conditions during ice ages, to warm interglacials, characterized by global warming and sea level rise due to change in
Deglaciation
Discredited 1970s hypothesis of imminent cooling of the Earth
acceptance. The length of the current interglacial temperature peak is similar to the length of the preceding interglacial peak (Sangamon/Eem), and so it could
Global_cooling
Extinct species of elephant native to Europe and West Asia
temperate and Mediterranean woodland and forest habitats, flourishing during interglacial periods, when its range would extend across Europe as far north as Great
Straight-tusked_elephant
Biostratigraphic stage in the British Isles
The Bramertonian Stage is the name for an early Pleistocene biostratigraphic stage of geological history the British Isles. It precedes the Pre-Pastonian
Bramertonian_Stage
Last interglacial stage in the North American regional subdivision of the Quaternary
The Sangamonian Stage (or Sangamon interglacial) is the term used in North America to designate the Last Interglacial (130,000-115,000 years ago) and depending
Sangamonian
Glacial period in Europe
follows the Holstein interglacial (Hoxnian Stage in Britain) and precedes the Eemian interglacial (globally known as the Last Interglacial and the Ipswichian
Saale_glaciation
Partial hippopotamus skeleton discovered in Leeds, England
Museum in Leeds, West Yorkshire, England. The skeleton dates to the Last Interglacial (also known as the Eemian and the Ipswichian in Britain) around 130,000
Armley_Hippo
Extinct species of large cattle
It probably evolved in Asia and migrated west and north during warm interglacial periods. The oldest-known aurochs fossils date to the Middle Pleistocene
Aurochs
Last glacial period in the Alpine region
depending on whether the long transition phases between the glacials and interglacials (warmer periods) are allocated to one or other of those periods. The
Würm_glaciation
Britain where interglacial deposits that accumulated during part of this stage were first discovered. The stratotype for this interglacial is the Cromer
Cromerian_Stage
Prehistoric human occupation of Britain
Palaeolithic, Britain was primarily inhabited by humans during warm interglacial periods, when Britain exhibited a temperate climate similar to modern
Prehistoric_Britain
Half of Earth that is north of the Equator
The long glacial periods were separated by more temperate and shorter interglacials which lasted about 10,000–15,000 years. The last cold episode of the
Northern_Hemisphere
Glacial Period in Britain c,352,000 - c130,000
approximately 374,000 until 130,000 years ago. It precedes the Last Interglacial (also called the Eemian Stage) and follows the Hoxnian Stage in the British
Wolstonian_Stage
Human-caused changes to climate on Earth
climate cycled through ice ages. One of the hotter periods was the Last Interglacial, around 125,000 years ago, where temperatures were between 0.5 °C and
Climate_change
Freshwater loch
Cam Loch (the crooked loch) is an irregularly-shaped freshwater loch, about 5 km long, on a north-west to south-east orientation, located slightly north
Cam_Loch,_Sutherland
Emergent coastal landform
marine terrace sequences, most of which were formed during separate interglacial highstands that can be correlated to marine isotope stages (MIS). A marine
Raised_beach
Period of the Pleistocene epoch
Historical names of interglacials. Region Interglacial 1 Interglacial 2 Interglacial 3 Alps Günz-Mindel Mindel-Riss Riss-Würm North Europe Waalian Holsteinian
Anglian_stage
Interglacial period of the Early Pleistocene
The Waalian interglacial (German: Waal-Warmzeit or Waal-Interglazial) or Waalian Stage was an interglacial period of the Early Pleistocene in north-west
Waalian_interglacial
Period between 130,000 and 80,000 years ago
corresponds to the Last Interglacial, also called the Eemian (in Europe) or Sangamonian (in North America), the last major interglacial period before the Holocene
Marine_Isotope_Stage_5
Extinct species of mammal
(Bos primigenius). Its presence in Europe is usually linked to warmer interglacial periods, however, an isolated skull from the late Pleistocene of the
Bubalus_murrensis
Classification of European archaeology
part of the Hoxnian Interglacial (corresponding to the global Marine Isotope Stage 11 and the continental Holstein Interglacial) around 424–415,000 years
Clactonian
mountain ranges partitioned different residual populations. In the interglacials those species that had survived extinction gradually repopulated the
History of Central European forests
History_of_Central_European_forests
The Biber-Danube interglacial (German: Biber-Donau-Interglazial) or Biber-Danube warm period (Biber-Donau-Warmzeit) is a historical term for a hypothetical
Biber-Danube_interglacial
Last glacial period and its associated glaciation in northern parts of Europe
Pleistocene ice age. The preceding warm period in this region was the Eemian interglacial. The last cold period began about 115,000 years ago and ended 11,700
Weichselian_glaciation
Project to drill through Greenland ice sheet
as an indication of repeated violent climate change during the last interglacial period in Greenland. The first drilling of the Greenland Ice Core Project
Greenland_ice_core_project
record of the climate in the region, including the periods of humid interglacial climate (the "green Sahara"), which allowed people to cross what is today
List of World Heritage Sites in Libya
List_of_World_Heritage_Sites_in_Libya
Glacial stage
Wisconsin (glacial) Sangamonian (interglacial) Illinoian (glacial) Yarmouthian (interglacial) Kansan (glacial) Aftonian (interglacial) Nebraskan (glacial) As developed
Kansan_glaciation
First age of the Holocene epoch
been correlated with the end of Younger Dryas (from near-glacial to interglacial) and a "shift in lower deuterium excess values". After the sudden rise
Greenlandian
Periods of colder and warmer climate during the Quaternary period
The odd-numbered interstadial MIS 5, also known as the Sangamonian interglacial, contains two periods of relative cooling, and so is subdivided into
Stadial_and_interstadial
Brno in the Czech Republic. It refers to a Mid-Pleistocene-Cromerian interglacial most important paleontological site in Central Europe. Stránská skála
Stránská_skála
Body of water existing over 100,000 years ago near the modern Baltic Sea
water located approximately where the Baltic Sea is now during the Last Interglacial (also known as the Eemian or Marine Isotope Stage 5e), roughly 130,000
Eemian_Sea
Effect on the Earth's climate from slow orbital changes
asserted that the length of the current interglacial temperature peak will be similar to that of the preceding interglacial peak (Sangamonian/Eem Stage). Therefore
Orbital_forcing
Sea level variations over geological time scales
term (<1 million years), and short term (<1 million years) with glacial-interglacial cycles due to Milankovitch cyclicity. The depth of the ocean basins is
Past_sea_level
Amount by which an orbit deviates from a perfect circle
of seasons, and it plays a role in the natural pacing of glacial and interglacial periods. Apsidal precession also slowly changes the place in Earth’s
Orbital_eccentricity
Change in glacial cycles c. 1m years ago
from extreme glacial conditions to a warm interglacial. This led to less dynamic ice sheets. Interglacials before the MPT had lower levels of atmospheric
Mid-Pleistocene_Transition
Extinct species of rhinoceros
extent woody plants. It reached its maximum geographical extent during interglacial periods, when its range would extend at least as far north as Germany
Narrow-nosed_rhinoceros
Landscape in Washington state, US
been at least 17 complete interglacial-glacial cycles since about 1.77 million years ago, and perhaps as many as 44 interglacial-glacial cycles since the
Channeled_Scablands
Biogeographic realm
Wherever these areas were found, they became source populations during interglacial periods. When the glaciers receded, plants and animals spread rapidly
Holarctic_realm
interspersed at more or less regular intervals by milder but shorter interglacial stages. Human populations during this period consisted of nomadic hunter-gatherers
Prehistory_of_France
Group of lakes in New York, United States
sediment down to the bedrock bottoms of the Finger Lakes, patches of interglacial deposits are likely preserved locally within or near hanging valleys
Finger_Lakes
Earth's southernmost continent
"Genomic evidence for West Antarctic Ice Sheet collapse during the Last Interglacial" (PDF). Science. 382 (6677): 1384–1389. Bibcode:2023Sci...382.1384L.
Antarctica
Extinct species of rhinoceros native to Eurasia during the Pleistocene
the woolly rhinoceros. It was predominantly present in Europe during interglacial periods. In Europe its range extended northwards to central Poland, southern
Stephanorhinus_kirchbergensis
Transition period from full glacial to full interglacial climates in the glacial cycle
is a relatively rapid transition from full glacial climates to full interglacial climates. For the Quaternary period, terminations are numbered using
Termination_(geomorphology)
Very long term changes in Earth's temperature
studies on glacial/interglacial temperature. The last 3 million years have been characterized by cycles of glacials and interglacials within a gradually
Geologic_temperature_record
Study of hydrology over geological time
variations in the Earth's orbit and the cycle of glacial periods and interglacials. For example, variations in the water level of Lake Lisan correlates
Paleohydrology
Obsolete system of climatic periods
century, which defines the alternation of glacial and interglacial periods on a global scale. Interglacial periods are warmer and, therefore, wetter on average
African_pluvial_periods
Third division (unofficial) of the Pleistocene Epoch
end of the Penultimate Glacial Period and the beginning of the Last Interglacial around 130,000 years ago (corresponding with the beginning of Marine
Late_Pleistocene
Last glacial period in southern Chile
is known as the Nahuel Huapi Drift. The preceding interglacial is known as the Valdivia interglacial after its type locality of Valdivia. The characteristics
Llanquihue_glaciation
Eurasian sea northeast of the Mediterranean
and 10). The Karangat marine transgression occurred during the Eemian Interglacial (MIS 5e). This may have been the highest sea levels reached in the late
Black_Sea
period Timeline of glaciation Quaternary glaciation Illinoian Stage Interglacial Interstadial Penultimate Glacial Period Last Glacial Period Last Glacial
Glacial_history_of_Minnesota
Island northwest of continental Europe
Channel and Britain becoming an island during warm interglacial periods like the Last Interglacial/Eemian (130–115,000 years ago), though it remained
Great_Britain
Cave in North Yorkshire, England
fossilized bones of a variety of mammals from the Eemian interglacial (globally known as the Last Interglacial, ~130-115,000 years ago), when temperatures were
Kirkdale_Cave
Geological period in North America in the Quaternary
It precedes the Sangamonian Stage (corresponding to the global Last Interglacial) and follows the Pre-Illinoian Stage in North America. The Illinoian
Illinoian_(stage)
Country in Northern Europe
accusative. The earliest archaeological finds in Denmark date back to the Eem interglacial period from 130,000 to 110,000 BC. Denmark has been inhabited since around
Denmark
Species of large semi-aquatic mammal
Belgium, the Netherlands, and western Germany during interglacial periods, such as the Last Interglacial (130–115,000 years ago). Analysis of ancient DNA
Hippopotamus
Lake in Montana, United States
massive glacial dammed lake, Lake Missoula, of the era of the last interglacial. Flathead Lake is a natural lake along the mainline of the Flathead River
Flathead_Lake
Major ice sheet
period Timeline of glaciation Quaternary glaciation Illinoian Stage Interglacial Interstadial Penultimate Glacial Period Last Glacial Period Last Glacial
Cordilleran_ice_sheet
Topics referred to by the same term
in Ipswich, Suffolk Ipswichian interglacial, alternative name for the Eemian Stage, Pleistocene English interglacial period dating from 75,000 to 130
Ipswich_(disambiguation)
Landlocked basin (endorheic basin)
sediments will settle out and be deposited. At times in between glaciers (interglacial), salt deposits may be present because of the arid climate and the evaporation
Pluvial_lake
Glacial complex in the Calabrian age of the Pleistocene epoch
of the Pleistocene epoch and lies between the Tegelen and the Waalian interglacial. The transition from the Tegelen to the Eburonian started about 1.78
Eburonian
Stage of Pleistocene
The Pastonian interglacial, now called the Pastonian Stage (from Paston, Norfolk), is the name for an early or middle Pleistocene stage of geological history
Pastonian_Stage
Antarctic ice cores. It corresponds to an increase in amplitude of glacial-interglacial cycles. The MBE roughly corresponds to the transition between MIS 12
Mid-Brunhes_Event
spatial population dynamics in the European fallow deer since the Eemian interglacial". Scientific Reports. 14 (1): 3015. Bibcode:2024NatSR..14.3015B. doi:10
Deer_of_Great_Britain
Segment of the continental ice sheet that covers East Antarctica
Davies, Siwan M.; Ramsey, Christopher Bronk (2020-02-11). "Early Last Interglacial ocean warming drove substantial ice mass loss from Antarctica". Proceedings
East_Antarctic_Ice_Sheet
Second period of the Neoproterozoic Era, with major glaciation
Between the Sturtian and Marinoan glaciations was a so-called "Cryogenian interglacial period" marked by relatively warm climate and anoxic oceans, along with
Cryogenian
Continent
The long glacial periods were separated by more temperate and shorter interglacials which lasted about 10,000–15,000 years. The last cold episode of the
Europe
Large mass of glacial ice
disappearance of these ice sheets marked the beginning of the current Holocene interglacial period, and the ongoing retreat and future fate of the Greenland and
Ice_sheet
Earth and climate scientist
Thesis Isotope stratigraphy and tephrochronology of the last glacial-interglacial transition (14-9 KA BP) in the British isles. (1998) Doctoral advisor
Chris_Turney
Animals which inhabit caves periodically or accidentally
these animals lived there in the latter part, at least, of the third interglacial epoch, and on through the fourth and last glacial advance, when, although
Trogloxene
the Haslach-Mindel interglacial (often regarded as part of Günz) and succeeded by the Mindel-Riss interglacial (Holstein interglacial). The Mindel glaciation
Mindel_glaciation
Discrepancy between past temperatures and the amount of incoming solar radiation
before each interglacial warming period, and it is claimed that the resulting reduced albedo of northern ice sheets assists in interglacial warming. Dust
100,000-year_problem
Global climate phenomenon
Pacific show variations in primary productivity, related to glacial-interglacial variability and precessional periods (23 ky) related to changes in the
El_Niño–Southern_Oscillation
Extinct species of mammal
and then entered central North America at the beginning of the Last Interglacial (locally known in North America as the Sangamonian) around 130,000 years
Bison_antiquus
Alpine glacial period in the Pleistocene epoch
Stratigraphic Table of Germany, was the end of the Holstein interglacial (known as the Mindel-Riss interglacial in the Alpine Foreland and corresponding to the Samerbe
Riss_glaciation
INTERGLACIAL
INTERGLACIAL
INTERGLACIAL
INTERGLACIAL
Girl/Female
Tamil
Raswitha | ரஸà¯à®µà¯€à®¤à®¾Â , ரஸà¯à®µà¯€à®¤à®¾ Â
Boy/Male
Hindu, Indian, Punjabi, Sikh
Friend; Bravely Upholding the Truth
Boy/Male
Indian, Punjabi, Sikh
Meditation; Contemplation
Surname or Lastname
English
English : habitational name from the place in Lancashire, so named from Middle English ald, old ‘old’ + holm ‘island’, ‘dry land in a fen’, ‘promontory’.English : topographic name from Old English (e)ald ‘old’ + hamm ‘water meadow’, ‘low-lying land by a river’.English : Colonist and trader John Oldham was born in Lancashire, England, in about 1600 and emigrated to America in 1623, arriving at Plymouth, MA, in July on the ship Anne.
Girl/Female
Indian, Modern
Mind; Mind Identifier
Boy/Male
American, Australian, British, English
Dweller at the Broad Meadow; English Surnames Related to Bradley; Broad Clearing in the Wood
Biblical
a band; a troop
Girl/Female
Tamil
Channakka | சாநà¯à®¨à®•à¯à®•à®¾
Beautiful lady
Boy/Male
German
Dominant Ruler
Girl/Female
Arabic, Muslim, Sindhi
Daughter of Alqamah
INTERGLACIAL
INTERGLACIAL
INTERGLACIAL
INTERGLACIAL
INTERGLACIAL