「Glaciation」の共起表現(1語右で並び替え)

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共起表現

「Glaciation」の共起表現一覧(1語右で並び替え)

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fornia, dated to the last ice age, Wisconsin	glaciation about 13,000 years ago.
urian periods, culminating in the Hirnantian	glaciation and the Ordovician extinction event.
ue to thin, rocky soil following Pleistocene	glaciation and a slightly cooler climate, although upla
a was missed by the most recent Wisconsonian	glaciation, and therefore is a region of deep river val
ed to as 'knobs', may have partially escaped	glaciation and resemble the rugged and forested hills o
ng that Karl Schimper originated the idea of	glaciation and proposed the radical idea that ice sheet
nd and gravel as a result of the Pleistocene	glaciation and the consequent re-routing of Pittsburgh'
The Laurentian Abyss is a product of	glaciation and water currents from the Saint Lawrence S
his region was ice-free during the Wisconsin	glaciation and underwent hundreds of thousands of years
o species survived the most recent period of	glaciation and inhabited Europe as recently as 10,000 y
cal terrain shows obvious evidence of recent	glaciation and is covered by thin soil and acidic peat.
end moraines that were formed in the Saalian	glaciation and Weichselian Ice Age.
arents-Kara Ice Sheet during the Weichselian	Glaciation, approximately 80,000 years ago.
the Lake Superior basin during the Wisconsin	glaciation around 10,000 B.P. (Before Present).
fore edge of the ice sheet of the Wisconsin	glaciation, as the lobe of the Laurentide ice sheet beg
Glacial grooves stemming from the Wisconsin	glaciation at Kelleys Island, Ohio
The Huronian (Makganyene) global	glaciation began at the start of the Rhyacian and laste
carbonate appears at the top of the Gaskiers	Glaciation, believed by many to be global in extent.
ere on flows through a wide valley formed by	glaciation but with a broad flat base formed from re-wo
as found to be present after the Wisconsinan	glaciation, but is not a current taxon of this former P
During this time,	glaciation caused the climate to rapidly fluctuate and
es formed when this area was at the limit of	glaciation during the last Ice Age.
he regional landscape was strongly marked by	glaciation during the Wisconsinan ice period.
akawea marks the maximum southwest extent of	glaciation during the ice age.
Area, an area of North America which escaped	glaciation during the last ice age.
s, led him to recognize multiple episodes of	glaciation during the Pleistocene.
w it and similar plants were able to survive	glaciation events during the ice ages.
te of the late Precambrian showed some major	glaciation events spreading over much of the earth.
This region escaped the	glaciation experienced by areas to the east and west du
poor of nutrients but relict flora from the	glaciation grasslands grow favorably.
ock layers representing different periods of	glaciation, had long been known and published in Englan
his led subsequently to the recognition that	glaciation had affected southern England.
ries which first led to the recognition that	glaciation had once reached southern England.
Several periods of	glaciation have carved Teewinot Mountain and the other
Several periods of	glaciation have carved Middle Teton and the other peaks
Several periods of	glaciation have carved South Teton and the other peaks
Several periods of	glaciation have carved Mount Owen and the other peaks o
of the surrounding area was once subject to	glaciation, Hemlock Stone could have been the outcome o
sheet during the later phases of the Saalian	glaciation, i.e. during the so-called Drenthe II stage
imply flows through a landscape opened up by	glaciation in the last Ice Age.
over and rising sea levels - at the end of a	glaciation increase the rate of precipitation.
ly thought only to consist of the Hirnantian	glaciation itself, but has now been recognized as a lon
evels were lower than today's due to distant	glaciation locking up the Earth's water during ice ages
Later	glaciation made the valleys steeper and smoother.
Widespread evidence of	glaciation may be seen in the U-shaped form of various
When a period of	glaciation modifies the landscape by creating glacial t
of time, which includes the Pre-Illinoian B	glaciation of North America.
C4c Stage of Europe and the Pre-Illinoian J	glaciation of the early Pre-Illinoian Stage of North Am
A legacy of the	glaciation of this area during the last ice age is the
C5-6 Stage of Europe and the Pre-Illinoian I	glaciation of the early Pre-Illinoian Stage of North Am
	Glaciation or increased snow in mountain ranges around
sent in northern Arizona in late Wisconsinan	glaciation period.
that its origin was overlapping, interlobate	glaciation retreat, between the Lake Ontario Lobe and t
ned the open tundra habitat as the Wisconsin	glaciation retreated far to the north.
nited States, south of where the Wisconsinan	glaciation spread about 11,000 years ago.
t advance of ice sheets during the Illinoian	glaciation stopped just north of Garden of the Gods.
This formed the last gasp of the Devensian	glaciation, the final stage of the Pleistocene epoch an
glaciated valley (as a sidenote, because of	glaciation, the valley is also experiencing post-glacia
da Bog is a wetland created by the Wisconsin	glaciation, the most recent of the so-called ice ages t
eek publication gave a name to the Illinoian	glaciation, the southernmost penetration of glacial ice
ited the mountain and recognised evidence of	glaciation there .
as one of the few parts of England to escape	glaciation, tin ore was readily available on the surfac
ade the transition from the last Pleistocene	glaciation to the current interglacial, or Holocene.
The Huronian	glaciation took place in the Siderian between 2400 Mya
e presence of such polish indicates that the	glaciation was relatively recent (in geologic time scal
ence in sea level caused by the Wisconsinian	glaciation was likely around -400 feet (120 m) from the
have been formed at the end of the Wisconsin	glaciation, when retreating glaciers provided large amo
ch of the ‘Proto-Soar' until the Pleistocene	glaciation when the valley was blocked by sands and gra
eved to have been formed by the processes of	glaciation where a combination of ice sheet advances, m

共起表現

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「Glaciation」の共起表現一覧(1語右で並び替え)