「Glaciation」の共起表現(1語左で並び替え)

Weblio 辞書 > 英和辞典・和英辞典 > Glaciationの意味・解説 > Glaciationに関連した共起表現

意味

例文

類語

共起表現

「Glaciation」の共起表現一覧(1語左で並び替え)

該当件数 : 92件

over and rising sea levels - at the end of a	glaciation increase the rate of precipitation.
of time, which includes the Pre-Illinoian B	glaciation of North America.
xtensively glaciated during the last British	glaciation.
ere on flows through a wide valley formed by	glaciation but with a broad flat base formed from re-wo
The hilltops are rounded by	glaciation.
the Late Pleistocene Epoch was dominated by	glaciation (the Wisconsin glaciation in North America a
he regional landscape was strongly marked by	glaciation during the Wisconsinan ice period.
r-type erosion rather than erosion caused by	glaciation.
imply flows through a landscape opened up by	glaciation in the last Ice Age.
This formed the last gasp of the Devensian	glaciation, the final stage of the Pleistocene epoch an
evels were lower than today's due to distant	glaciation locking up the Earth's water during ice ages
as one of the few parts of England to escape	glaciation, tin ore was readily available on the surfac
ed to as 'knobs', may have partially escaped	glaciation and resemble the rugged and forested hills o
Area, an area of North America which escaped	glaciation during the last ice age.
as Long Lake, is a prairie lake formed from	glaciation 11,000 years ago.
carbonate appears at the top of the Gaskiers	Glaciation, believed by many to be global in extent.
The Huronian (Makganyene) global	glaciation began at the start of the Rhyacian and laste
300 million years ago, was a period of great	glaciation.
urian periods, culminating in the Hirnantian	glaciation and the Ordovician extinction event.
ly thought only to consist of the Hirnantian	glaciation itself, but has now been recognized as a lon
The Huronian	glaciation took place in the Siderian between 2400 Mya
The Huronian	glaciation (or Makganyene glaciation) extended from 240
ng to some geologists triggered the Huronian	glaciation.
C5-6 Stage of Europe and the Pre-Illinoian I	glaciation of the early Pre-Illinoian Stage of North Am
t advance of ice sheets during the Illinoian	glaciation stopped just north of Garden of the Gods.
eek publication gave a name to the Illinoian	glaciation, the southernmost penetration of glacial ice
that its origin was overlapping, interlobate	glaciation retreat, between the Lake Ontario Lobe and t
C4c Stage of Europe and the Pre-Illinoian J	glaciation of the early Pre-Illinoian Stage of North Am
the Ice Age of the early Pleistocene Kansan	glaciation.
that flowed through the area during the last	glaciation.
southern edge of the ice sheet from the last	glaciation (approximately 10 000 years ago), and can be
osits from before, during and after the last	glaciation.
Since the end of the last	glaciation (about 12000 years ago), whitefish have been
Later	glaciation made the valleys steeper and smoother.
te of the late Precambrian showed some major	glaciation events spreading over much of the earth.
es formed when this area was at the limit of	glaciation during the last Ice Age.
eved to have been formed by the processes of	glaciation where a combination of ice sheet advances, m
ock layers representing different periods of	glaciation, had long been known and published in Englan
When a period of	glaciation modifies the landscape by creating glacial t
ng that Karl Schimper originated the idea of	glaciation and proposed the radical idea that ice sheet
glaciated valley (as a sidenote, because of	glaciation, the valley is also experiencing post-glacia
ers are also found on the Chase, remnants of	glaciation.
akawea marks the maximum southwest extent of	glaciation during the ice age.
ited the mountain and recognised evidence of	glaciation there .
The Laurentian Abyss is a product of	glaciation and water currents from the Saint Lawrence S
Several periods of	glaciation have carved Teewinot Mountain and the other
Several periods of	glaciation have carved Middle Teton and the other peaks
o species survived the most recent period of	glaciation and inhabited Europe as recently as 10,000 y
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
Widespread evidence of	glaciation may be seen in the U-shaped form of various
s, led him to recognize multiple episodes of	glaciation during the Pleistocene.
ue to thin, rocky soil following Pleistocene	glaciation and a slightly cooler climate, although upla
ch of the ‘Proto-Soar' until the Pleistocene	glaciation when the valley was blocked by sands and gra
ade the transition from the last Pleistocene	glaciation to the current interglacial, or Holocene.
nd and gravel as a result of the Pleistocene	glaciation and the consequent re-routing of Pittsburgh'
significantly lowered due to the Quaternary	glaciation.
gion was deeply eroded during the Quaternary	glaciation.
cal terrain shows obvious evidence of recent	glaciation and is covered by thin soil and acidic peat.
s Fahrenheit) cooler than present represents	glaciation.
sheet during the later phases of the Saalian	glaciation, i.e. during the so-called Drenthe II stage
end moraines that were formed in the Saalian	glaciation and Weichselian Ice Age.
f the UK has not been affected by full scale	glaciation.
w it and similar plants were able to survive	glaciation events during the ice ages.
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.
e presence of such polish indicates that the	glaciation was relatively recent (in geologic time scal
poor of nutrients but relict flora from the	glaciation grasslands grow favorably.
This region escaped the	glaciation experienced by areas to the east and west du
A legacy of the	glaciation of this area during the last ice age is the
During this time,	glaciation caused the climate to rapidly fluctuate and
of the surrounding area was once subject to	glaciation, Hemlock Stone could have been the outcome o
arents-Kara Ice Sheet during the Weichselian	Glaciation, approximately 80,000 years ago.
e sheet which existed during the Weichselian	Glaciation.
ciers of the latest Ice Age, the Weichselian	glaciation.
lores remained isolated during the Wisconsin	glaciation (the most recent glacial period), despite th
have been formed at the end of the Wisconsin	glaciation, when retreating glaciers provided large amo
ered northern Wisconsin during the Wisconsin	Glaciation.
fornia, dated to the last ice age, Wisconsin	glaciation about 13,000 years ago.
ned the open tundra habitat as the Wisconsin	glaciation retreated far to the north.
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
his region was ice-free during the Wisconsin	glaciation and underwent hundreds of thousands of years
the Lake Superior basin during the Wisconsin	glaciation around 10,000 B.P. (Before Present).
da Bog is a wetland created by the Wisconsin	glaciation, the most recent of the so-called ice ages t
rie, that occurred during the late Wisconsin	glaciation.
nited States, south of where the Wisconsinan	glaciation spread about 11,000 years ago.
sent in northern Arizona in late Wisconsinan	glaciation period.
as found to be present after the Wisconsinan	glaciation, but is not a current taxon of this former P
ence in sea level caused by the Wisconsinian	glaciation was likely around -400 feet (120 m) from the
a was missed by the most recent Wisconsonian	glaciation, and therefore is a region of deep river val

共起表現

「Glaciation」の共起表現(1語左で並び替え) - Weblio英語共起表現検索

「Glaciation」の共起表現一覧(1語左で並び替え)