「Glacial」の共起表現(1語右で並び替え)

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共起表現

「Glacial」の共起表現一覧(1語右で並び替え)

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Its solution in	glacial acetic acid, by oxidation with chromic acid,
He proved that	glacial acetic acid and vinegar acetic acid were the
is to add 4-methylpropiophenone dissolved in	glacial acetic acid to bromine, creating an oil fract
he laboratory, solutions of alkyl nitrites in	glacial acetic acid are sometimes used as mild nitrat
by the treatment of dry cadmium acetate with	glacial acetic acid and acetyl bromide.
It also dissolves in	glacial acetic acid and a diluted mixture of nitric a
nts for the production of ethylene glycol and	glacial acetic acid.
lace and then several drops of 0.2% iodine in	glacial acetic acid.
her aluminium hydroxide, acetic anhydride and	glacial acetic acid in water, forming the basic alumi
anhydrous Pb(SCN)2 is treated with bromine in	glacial acetic acid to afford a 0.1M solution of thio
It is soluble in methanol and	glacial acetic acid.
r esterification) between isoamyl alcohol and	glacial acetic acid as shown in the reaction equation
In one synthetic path, nitroethane in a	glacial acetic acid solution with an ammonium acetate
reaction of a magnesium/calcium compound with	glacial acetic acid.
The lake is natural, having been formed by	glacial action and is 50 hectares in size.
ed within a rock hollow formed as a result of	glacial action during the ice ages.
peatlands across the North-West formed by the	glacial action at the end of the last Ice Age, and pa
nstones Formation of the Old Red Sandstone by	glacial action during the succession of recent ice ag
well as numerous valleys have been formed by	glacial action over hundreds of thousands of years.
Beacons National Park Fan Fawr was subject to	glacial action in the ice ages.
kilometre (0.62 mi) wide, and was created by	glacial action during the last ice age.
canyons, showing millennia of erosion, where	glacial action would have otherwise smoothed out the
ny between the two World Wars which suggested	glacial action creating the craters.
The crater has been completely filled by	glacial action, so that no trace appears on the surfa
a disproportionately wide valley, created by	glacial action.
es, and the part played in their formation by	glacial action.
	Glacial activity spanned virtually the whole of Carbo
n from around 150 published sources, covering	glacial activity mainly from the past 30000 years.
	Glacial activity has shaped the landscape 3,000 metre
although a common origin for diamicton is by	glacial activity.
he canyon is Phelps Lake which was created by	glacial activity.
This was the last	glacial advance that entered Michigan and covered onl
the so-called Drenthe II stage and the final	glacial advance of the Warthe stage.
lows covered the floor of Behm Canal, another	glacial advance scoured away much of the flow, leavin
These annual	glacial advances and recessions cause parallel ridges
	Glacial Aerial Tramway Kaprun III has two stretches,
Pillar of the	Glacial Aerial Tramway Kaprun III, tallest aerial lif
Pylon of the	Glacial Aerial Tramway Kaprun, the tallest in the wor
The Urstrom is a geologists' name for a great	glacial age river of the Polish and north German plai
iverted waters of the Bridge River, which are	glacial and milky-green in colour.
ks formed from sediments deposited by marine,	glacial and freshwater sources between 355 and 180 mi
Palaeozoic rocks of Norway, and with the late	glacial and post-glacial changes of sea level in the
his Ph.D. in 1942, he became a specialist in	glacial and periglacial morphology.
ey and Hendon station found a large extent of	glacial beds and fossils, and these were thought to e
This is linked to its	glacial beginnings.
Rollstone Hill in Fitchburg, where a massive	glacial boulder stood (it is now on the small triangl
	Glacial centres expanded across the continents, produ
dge, the slopes again steepen, reflecting the	glacial cirque between Southwest Hunter and Hunter th
f the Steinerne Rinne, a huge couloir and old	glacial cirque, that runs southwards up to the crossi
ciated during the ice ages and at least three	glacial cirques are evident, of which Craig Cerrig-gl
	Glacial cirques form the heads of Tuckerman Ravine on
western wall of Pinkham Notch, holds several	glacial cirques.
e and limestone basin, 30 - 40 feet (12 m) of	glacial clay and silt and a 1 - 2-foot (0.61 m) mixtu
st deposited under extremely cold, dry post -	glacial conditions.
The mountain has a north facing	glacial cwm known as Y Gylchedd.
s steep cliffs, that form the backwall of the	glacial Cwm Dulyn.
amatic morphology: with two fine aretes, dark	glacial cwms and splendid rocky character.
"Response of a major river system to the last	glacial cycle: geomorphology and internal architectur
he Fort Wayne Moraine, which was a deposit of	glacial debris that acted as a natural dam at the sit
nd carbonate rock, including readily-attacked	glacial debris, which would releasing large amounts o
les) in diameter, deeply eroded and buried in	glacial debris.
The river valley was filled with	glacial debris.
the "Big Stone" as it is known locally, is a	glacial deposit on the moorlands of Tatham Fells, sit
d on a shelf or terrace of land, probably the	glacial deposits formed after the creation and later
The causeway is made of	glacial deposits left by receding ice sheets at the e
The rock is common in	glacial deposits just south of its source location, a
e soil in Leelanau Peninsula is complex, with	glacial deposits of clay, sand, and loam on top of be
ume report, for which he authored sections on	glacial deposits, Paleozoic and Precambrian bedrock g
astern Wisconsin, a region mantled with thick	glacial deposits, led him to recognize multiple episo
countless thousands of years of sediment and	glacial deposits.
athered look of other rocks in Rhode Island's	glacial deposits.
The lowest slopes are generally covered in	glacial diamicton derived from the igneous lithologie
ion and led to his appointment as head of the	glacial division of the US Geological Survey in 1881.
ion types, which have developed on the acidic	glacial drift overlying magnesian limestone that is c
erve are lakes formed in shallow valleys when	glacial drift blocked off the outflow to the sea.
ciated portion of North America devoid of the	glacial drift of surrounding regions.
nd varied situations, although it prefers the	glacial drift and well-drained borders of streams.
View, but progressed slowly due to the dense	glacial drift below.
y, which has eroded deeply into an underlying	glacial drift of boulder clay, sands and gravels, is
most of Iowa, which is on the whole is absent	Glacial Drift.
ility of early geologists to find evidence of	glacial drift.
Kensington is home to 16 named hills of	glacial drumlin origin; the highest, Indian Ground Hi
ase of Eemian interglacial phase before final	glacial episode of Pleistocene 126,000 ± 5,000 years
ly formed by the terminal moraine of the last	glacial episode (Wisconsin glaciation).
rimary mechanism of sediment transport during	glacial episodes of the Pleistocene when sea levels w
The effect of the	glacial epoch upon the distribution of insects in Nor
of Man" "On the Changes of Climate during the	Glacial Epoch" "On the Glacial Phenomena of the Outer
In the	glacial era, the Ythan River at this point would have
	Glacial eratics litter its slopes, with a large one l
s, grey wagtails and heron.During the Ice Age	glacial erosion eroded one side of the valley resulti
	Glacial erosion was likewise responsible for scooping
usetts landscape, the peninsula was shaped by	glacial erosion and moraine deposits left by retreati
This	glacial erosion resulted in the very steep northern a
e District, subscribing much of the layout to	glacial erosion.
Cyclopean stairs form as a result of	glacial erosion.
c quartzite, but before a regional episode of	glacial erosion; if correct it occurred between 900-6
Plastic moulding, gouging and other	glacial erosional features become present upon the gl
s of the data revealed giant sand waves, huge	glacial erratic boulders and several uncharted wrecks
The Glumsten, a	glacial erratic is mentioned as early as in the 11th
the rock comes from Canada and is the largest	glacial erratic rock in the Willamette Valley.
Doane Rock is a	glacial erratic located in Eastham, Massachusetts on
It is a	glacial erratic boulder on which a cast-iron memorial
t be certain, however, whether or not it is a	glacial erratic because its rock types match those of
d after Dighton Rock, an 11-foot (3.4-m) high	glacial erratic that once sat on the banks of the Tau
Big Rock (also known as Okotoks Erratic) is a	glacial erratic situated between the towns of Okotoks
Since 1901 a	glacial erratic marks the place of death on the forme
The stone is a	glacial erratic located in desolate peatland.
The Bowder Stone is a large	glacial erratic in Borrowdale at grid reference NY254
Several	glacial erratic boulders are also found on the Chase,
This is a	glacial erratic, brought from probably hundreds of mi
ed up by the glacier and deposited later as a	glacial erratic.
the rock is often used as a type example of a	Glacial Erratic.
ows many signs of the last ice age, including	glacial erratics (boulders left behind when the ice r
ndinavia, northern North America, and Russia,	glacial erratics are common.
they were brought much nearer to the site as	glacial erratics by the Irish Sea Glacier.
Geologists have found	glacial erratics on Rattlesnake at heights up to this
e boulder is one of the world's largest known	glacial erratics.
ubglacial to proglacial record of Pleistocene	glacial events.
Its valley contains the best-developed	glacial features in the Kosciuszko National Park alpi
Schematic drawing of	glacial features illustrating how moulins transport s
f the Niagara Escarpment and is noted for its	glacial features, especially potholes.
is characterized by a till moraine and other	glacial features, such as kames and kettles.
the Maligne Valley watershed which is mainly	glacial fed.
ute was dug through a highly unstable area of	glacial fill, making it extremely treacherous.
covered in Victoria Road and seen as a chance	glacial find, there is no record of prehistoric finds
Cairlinn, Ulster Scots: Carlinford Loch) is a	glacial fjord or sea inlet that forms part of the bor
In 1934, however, there was calamity: a	glacial flood roared down the Mendoza canyon and comp
sses beneath the park known as the "Wisconsin	Glacial Flow", an ancient river channel now filled wi
e wide at its center, The Lake was created by	glacial forces in a previous Ice Age.
at room temperature unless it is in its pure	glacial form.
Names (US-ACAN) (1997) after husband and wife	glacial geologists Thomas B. Kellogg and Davida E. Ke
g, and during the summers he investigated the	glacial geology of northern Europe and the British Is
His well-known memoir on	glacial geology written in collaboration with Edmund
t the University of Michigan and authority on	glacial geology of the central United States.
Henry Carvill Lewis's Papers and Notes on the	Glacial Geology of Great Britain and Ireland, issued
umberland' (vols i-vi); 'Contributions to the	Glacial Geology of Spitzbergen' (with Dr J W Gregory,
shed in 1894 entitled Papers and Notes on the	Glacial Geology of Great Britain and Ireland, edited
1879 to Minnesota to study the resources and	glacial geology of that state.
work on the geology of gold bearing minerals,	glacial geology, and for his description of the mutua
ncluding alluvial chronology, periglacial and	glacial geology, wind action, soil and vegetative eff
He became an authority on	glacial geology, and wrote much, especially in conjun
as a Site of Special Scientific Interest for	Glacial Geology.
d prominently in the study and development of	glacial geology.
positioning systems, geodesy, crustal motion,	glacial geophysics, airborne geospatial systems, seis
the Eastern side a happenstance of the final	glacial gouging.
monstrates a sequence of fluvial (or possibly	glacial) gravels, marine intertidal silts and marine
The	glacial grooves on Kelleys Island are cut into the Co
	Glacial grooves stemming from the Wisconsin glaciatio
33° to 30° N. latitude, including most of the	glacial Gulf Coast from about 84° W. longitude.
eresting area when it comes to looking at the	glacial history of Britain.
In	glacial ice this zone is at approximately 30 m (100 f
around 12000 years ago at the retreat of the	glacial ice .
A marginal lake of meltwater trapped between	glacial ice sheet and the Lincolnshire Wolds spilled
The main valley was excavated by	glacial ice during the course of the ice ages as it b
n glaciation, the southernmost penetration of	glacial ice into what was to become the Midwestern Un
The mere originated as a detached mass of	glacial ice melted in situ towards the end of the las
owe their steepness in part to the action of	glacial ice during the succession of ice ages.
1850), there has been a reduction of mountain	glacial ice worldwide of 50% since 1850.
oraine marking the maximum extent of the last	glacial ice sheet to reach the northeastern coast.
steep lava cliffs from their interaction with	glacial ice and can have thicknesses of 100 m (330 ft
cene period when this area was buried beneath	glacial ice during the last ice age.
Precipitation and therefore	glacial ice contain water with a low 18O content.
The	glacial ice scraped off and carried with it rocks and
ll as indicating the direction of flow of the	glacial ice, the depth and extent of weathering of th
t a vertical pipe right through the overlying	glacial ice, instead forming hyaloclastite and pillow
arge amounts of 16O water are being stored as	glacial ice, the 18O content of oceanic water is high
in UMB49T) was isolated from 120,000 year old	glacial ice, 3,042 metres (1.9 mi) deep, from Greenla
Firn becomes	glacial ice-the long-lived, compacted ice that glacie
l in the region soon after the retreat of the	glacial ice.
shape as a result of their confinement within	glacial ice.
er, ice sheet, ice field or any other body of	glacial ice.
forty years studying the history embedded in	glacial ice.
lcanism and related phenomena associated with	glacial ice.
ed the laminated or ribboned structure of the	glacial ice; and ascribed the movement of glaciers to
e Pleistocene and displays major landforms of	glacial influence.
associated with his studies of sea level and	glacial isostasy during the Quaternary.
For a time, it was thought that the	Glacial Kame Culture did not produce ceramics, but th
Excavation of	Glacial Kame sites frequently yields few projectile p
in, Ohio, Indiana, Michigan, and Ontario, the	glacial Kame peoples use the gravel ridges formed by
The Zimmerman Site, a leading	Glacial Kame site
g the most common types of artifacts found at	Glacial Kame sites are shells of marine animals and g
The	Glacial Kame Culture was a culture of Archaic people
s reason, it appears that different groups of	Glacial Kame peoples independently developed differen
k savanna, tall grass praries, and an ancient	glacial kettle lake.
k lies on a sandur formed from the outwash of	Glacial Lake Grantsburg.
Lake Wisconsin; for the prehistoric lake, see	Glacial Lake Wisconsin.
, named for geologist William G. Tight, was a	glacial lake located in what is present-day Ohio, Ken
ed, a stony hill that was once an island when	glacial Lake Chicago covered the area thousands of ye
	Glacial Lake Connecticut formed over what is now Long
main product of his many years of study ("The	Glacial Lake Agassiz") was published in 1895 as Monog
Spring Lake is a small	glacial lake in the Town of Berlin, Rensselaer County
anticline surface layer, presumably chalk, by	glacial lake outburst floods
In other cases, such as	Glacial Lake Missoula and Glacial Lake Wisconsin in t
s Point, the meltwater would have flowed into	Glacial Lake Wisconsin, a prehistoric proglacial lake
	Glacial Lake Minong was a proglacial lake that formed
	Glacial Lake Duluth was a proglacial lake that formed
Lake Bled (Slovene: Blejsko jezero) is a	glacial lake in the Julian Alps in northwestern Slove
ibrarian who is best known for his studies of	glacial Lake Agassiz.
	Glacial Lake Minong
	Glacial Lake Duluth

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共起表現

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「Glacial」の共起表現一覧(1語右で並び替え)