「glacier」の共起表現一覧(1語右で並び替え)
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ski area; the Snocoach tours of the Athabasca | Glacier, a distributary of the Columbia Icefield; Ath |
ur forms the east side of the mouth of Morris | Glacier, about 6 nautical miles (11 km) northwest of |
he Big Muddy was not covered by the Wisconsin | Glacier, about 70,000 to 10,000 years before present. |
Haast named the Franz Josef | Glacier after the Emperor of the Austro-Hungarian Emp |
ctic Names (US-ACAN) in association with Byrd | Glacier after Captain Delbert S. Cornwell, U.S. Navy, |
ommittee (UK-APC) in association with Neptune | Glacier after John Couch Adams (1819-92), the Cambrid |
lf and discovered a route up the Axel Heiberg | Glacier along this coast to reach the polar plateau. |
ssengers for a scenic flight over Franz Josef | Glacier, although none of the passengers nor Openshaw |
The falls are fed by the Ramnefjellbreen | glacier, an arm of the great Jostedalsbreen glacier. |
etres, is situated at the top of the Tabuchet | glacier, and allows access to the north face. |
th this discovery Scott gave the names Ferrar | Glacier and Taylor Glacier essentially as now applied |
The range is bounded on the west by Rawle | Glacier and Leitch Massif, on the northwest by Black |
re it became usual to give the same name to a | glacier and its glacier tongue. |
ow by colliers Caesar and Brutus, stores ship | Glacier, and tug Potomac. |
at the east side of the terminus of Beardmore | Glacier and mark the northern termination of the Comm |
al research events in the Dry Valleys, Darwin | Glacier, and Bratina Island areas from 1984. |
Task Force 43, along with USCGC Edisto, USCGC | Glacier and USCGC Westwind, for which she was awarded |
climb is on the steep snow and ice of Skillet | Glacier, and an ice axe and crampons should be used i |
d of Ross Ice Shelf, located east of Amundsen | Glacier and midway between MacDonald Nunataks and O'B |
all sides," which was reached by "a crevassed | glacier and a 50 degree snow/ice face." |
ember reconnaissance team that explored Scott | Glacier and Reedy Glacier as possible destinations fo |
between Morris Peak, on the east side of Liv | Glacier, and the west side of the Scott Glacier. |
mp, which obtained aerial photographs of this | glacier and adjacent coastal areas, 1946-47. |
alty Mountains, and at the junction of Newnes | Glacier and Moubray Glacier which fall steeply from i |
alty Mountains, and at the junction of Newnes | Glacier and Moubray Glacier which fall steeply from i |
he main ridge that lies south of the Gangotri | Glacier, and Kedarnath Dome, a subpeak of the main pe |
It dividies Wright Valley from Taylor | Glacier and Taylor Valley, and was named by the Victo |
de, standing between the upper part of Lillie | Glacier and the Greenwell Glacier in northern Victori |
a channel at the bottom of an ice-sheet or a | glacier, and are usually close to the glacier terminu |
the geology in the mountains between the Byrd | Glacier and Nimrod Glacier. |
It lies at the head of the Gangotri | Glacier and forms the eastern anchor of the group. |
area beyond Shackleton Inlet to the Beardmore | Glacier, and was the first to find a practicable rout |
ighest peak on the south side of the Gangotri | Glacier, and Kedarnath Dome is the third highest. |
ice becomes detached from the main body of a | glacier and melts in place depositing the sediments i |
Balakun is situated between Bhagirathi Kharak | glacier and Satopanth glacier.The peak is situated no |
ands at the east side of the mouth of Barrett | Glacier and is the northwesternmost summit in Gabbro |
ulins can go all the way to the bottom of the | glacier and can be hundreds of meters deep, or may re |
large portions of it will be picked up by the | glacier and deposited later as a glacial erratic. |
Shell | Glacier and Endeavour Piedmont Glacier lie on its slo |
udes the mapping of the bed under Pine Island | Glacier and the discovery of a subglacial volcano. |
The water originates from the Athabasca | Glacier, and volumes are higher in early summer, caus |
(30 mi) wide, situated southward of Minnesota | Glacier and forming the southern half of the Ellswort |
n between India and Pakistan over the Siachen | Glacier and coined the term Oropolitics to describe t |
is formed from the melt water of the Baltoro | Glacier and Biafo Glacier. |
dro exploration road accessing the Affliction | Glacier and north side of Plinth was partially reopen |
e 1960s, and one in 1969-70 visited the Scott | Glacier and named Marble Peak and Surprise Spur. |
3422 meter peak is located between the Keltie | Glacier and Mill Glacier, on the east side of the Bea |
o are separated from one another by the Teton | Glacier and Mount Owen. |
Axel Heiberg | Glacier, Antarctica |
after two helicopters had crashed on Fortuna | Glacier, April 21, 1982. |
reat of the glaciers (in this area the Fraser | Glacier); archeological digs in the area, focussing o |
The remains of a cirque | glacier are visible in the walls around lake seal. |
Icebergs breaking from the | glacier are often so large (up to a kilometer (3,300 |
Petersen | Glacier are located in Grand Teton National Park, Wyo |
the open meadows and moraines below the Mons | Glacier are reached. |
The Ruetz River flows from the | glacier area of the valley to the Wipptal in north-ea |
SAE (1961-62) which explored the Axel Heiberg | Glacier area. |
re the Mile One Stadium in St. John's and the | Glacier Arena in Mount Pearl, while the S. W. Moores |
Amundsen used this | glacier as his route up onto the polar plateau on his |
tified frozen remains found atop a California | glacier as those of a World War II era airman named E |
ndia currently is the area above the Gangotri | Glacier at the source of the Ganges. |
It merges into the larger Graveson | Glacier at the east margin of the mountains. |
Water from moulins often exits the | glacier at base level, sometimes into the sea, and oc |
Originating from the Yamunotri | Glacier at a height 6,387 mtrs., on the south western |
Elevations bordering the Beardmore | Glacier, at the western extremity of these mountains, |
that forms the southwest side of the Gangotri | Glacier basin; this ridge contains other well-known p |
The | Glacier Bay Water Shrew (Sorex alaskanus) is a specie |
ner Cooper, "The Recent Ecological History of | Glacier Bay, Alaska" Ecology 4 (1923): 93-128. |
Cooper's travels in | Glacier Bay, Alaska, compelled him to lead scientists |
Ursus americanus emmonsii, | Glacier bear |
outhern hemisphere, ski-plane trips to Tasman | Glacier became a key part of the Mt Cook tourism . |
It rises from the Man Talai | Glacier below the Pin Parbati pass and flows in a gra |
Glacier Blanc | |
normal route climbs the entire length of the | Glacier Blanc. |
th face is glaciated, being the source of the | Glacier Blanc. |
ere was a period when ice from the Wye Valley | Glacier blocked the exit of the river into the Wye. |
ik Range (views including Wapta Icefield, Bow | Glacier, Bow Peak, Mount Thompson, Crowfoot Glacier a |
The | glacier Buarbreen in is an offshoot of the Folgefonna |
gist Christopher J. Burgess and describes the | glacier, but also the excellent helicopter support pr |
of siachen and saltoro ridge including gyong | glacier, but these glaciers are not tributaries of Si |
ence that these are not two parts of a single | glacier but are two glaciers apposed. |
ct the amount of movement that is made by the | glacier by a large percentage especially if the slope |
Glacial silt, which is carried from the | glacier by streams, ensures a turquoise appearance to |
Glacier Camp is an uninhabited locality in far northw | |
The township is situated in a dramatic | glacier carved basin on the shores of the lake and is |
The tributary | glacier causes the central glacier to thicken and dow |
the most typical cause for the formation of a | glacier cave. |
n 1978 they were the longest mapped system of | glacier caves in the world. |
These | glacier caves were visited and documented at least as |
aradise Ice Caves (also known as the Paradise | Glacier Caves) were a system of interconnected glacie |
Glacier Chaser Marzen Lager '09 | |
Lake Bucura is a | glacier cirque lake, situated in the Retezat Mountain |
The | Glacier class icebreaker was similar to the Wind clas |
ish Antarctic Expedition, 1901-04, to a small | glacier close west of The Watchtower on the south sid |
e of -6 Celsius and 98% humidity, replicating | glacier conditions in which it was found. |
Cone | Glacier contains two arms that surround the volcano. |
It is formed in northwestern Montana, in | Glacier County 21 mi (34 km) N of Browning, Montana, |
rder lies the Blackfeet Indian Reservation in | Glacier County, Montana. |
formed in the Blackfeet Indian Reservation in | Glacier County, in northwestern Montana, by the confl |
he Rockies), was found by Robert W. Harmon in | Glacier County, in the territory of the Blackfoot, in |
One possibility is that a moving | glacier created the separation. |
lyeska, near Anchorage, where he attended the | Glacier Creek Ski Academy. |
According to them, the Gangotri | glacier, currently 30.2 km long and between 0.5 to 2. |
The length of the | glacier currently decreases about 10 m (33 ft) each y |
The | glacier derives its name from "Strom Camp" near its f |
It is occupied by the terminus of the Nimrod | Glacier descending at a low gradient from the borderi |
Amundsen | Glacier, descending from the Queen Maud Mountains to |
Melt water from the Ipasha | Glacier descends 580 feet (180 m) over Ipasha Falls e |
Allison | Glacier descends from the west slopes of Royal Societ |
Rutgers | Glacier descends southwest from Johns Hopkins Ridge a |
The | glacier drains southeast between the Deep Freeze and |
This | glacier drains the central Anare Mountains and flows |
s geological formation produced by a receding | glacier during the last Ice Age. |
d here about 14,000 years ago by a retreating | glacier during the last glacial period. |
when the volcano was constructed on top of a | glacier during the Late Pleistocene period. |
is surrounded by several galciers the Prazon | glacier en the Ruan glacier as well as the Tenneverge |
n of Bowers Mountains just S of where Sheehan | Glacier enters Rennick Glacier. |
Ghost | Glacier EP (2008) |
The annual | Glacier equilibrium line separates the accumulation a |
The force of the | glacier erodes the surrounding softer material, leavi |
n the following towns: Libby, Whitefish, West | Glacier, Essex, East Glacier Park, Browning, Cut Bank |
the melting of snow or ice that runs off the | glacier, evaporation, sublimation, calving, or erosiv |
Named by the Texas Tech Shackleton | Glacier Expedition (1964-65) for John C. Shenk, who w |
es both an hourly regional train and 10 daily | Glacier Express trains between Zermatt and the ski re |
etre gauge trains calling at Brig include the | Glacier Express. |
During the last ice age, a | glacier extended across this area almost to where Don |
t to apply plasticity theory to understand to | glacier flow . |
ed his attention to studying the mechanics of | glacier flow, with an emphasis on basal sliding, surg |
wegian geographer who worked on the theory of | glacier flow. |
/ -54.433; -36.2) is a | glacier flowing northeast into St. |
The | glacier flows south into Schwartz Cove on the south s |
The | glacier flows at a rate of 20-35 m (66-115 ft) per da |
The Lituya | Glacier flows from the south side of the mountain and |
The Angel | Glacier flows down the north face of Mount Edith Cave |
Runoff from the | glacier flows into Leigh Lake. |
He was on the Board of Directors of the | Glacier Food Group. |
This type of snow is associated with | glacier formation through the process of nivation. |
Glacier formation can take days to years depending on | |
Retreat of the Ice Age | glacier formed Littorina Sea. |
cago, on the southern margin of the Wisconsin | Glacier, found successive lower outlets as the glacie |
e range borders the eastern side of Beardmore | Glacier from the Ross Ice Shelf to Keltie Glacier. |
The Erebus Ice Tongue, coming off the Erebus | Glacier from 3,800 m (12,500 ft). |
who are interested in trekking over the Biafo | Glacier, from Nagar to Skardu and if you wants to cli |
Srebarna | Glacier from Bransfield Strait, with Great Needle Pea |
cock and overlooking the terminus of Ironside | Glacier from the south, in the Admiralty Mountains, V |
Byrd | Glacier from Landsat |
e Kalindi Khal which separates the Chaturangi | glacier from the Arwa valley. |
bott Spur separates the lower ends of Rutgers | Glacier from Allison Glacier. |
Panoramic view of lake and | glacier from the northern shoreline |
1,700 metres (5,600 ft) in Skjomen, where the | glacier Frostisen can be seen. |
Sediment locked within the ice of the | glacier, gets transported by the streams of meltwater |
has its origins in the ice ages when a minor | glacier grew at this spot. |
f Kalabaland Glacier-Sankalp Glacier-Yangchar | Glacier group. |
When built, | Glacier had the largest capacity single armature DC m |
The | glacier had an area of 4.9 km² (1.9 mi²) in the 1980s |
Between the years 1893 and 1953, Saskatchewan | Glacier had retreated a distance of 1,364 metres (4,4 |
The ice content of the | glacier has been assessed as 0.137 cubic km. |
This landform may often be observed after the | glacier has melted and usually has a delta (in the se |
This | glacier has been constantly receding since measuremen |
he vast majority of glaciers worldwide, Peyto | Glacier has been retreating rapidly, especially since |
At the age of 73, while on a | glacier, he twisted his knee in a snow-covered crevas |
terial from the Indian mainland to Siachen, a | glacier, helipad and battleground near the Line of Co |
has been discovered that the real source is a | glacier higher in the mountains. |
It is part of the Portage | Glacier Highway and at 13,300 feet (4,050 m), is the |
Both ski trips in the winter and | glacier hiking trips in the summer often combine a tr |
w is a lava flow that has impounded against a | glacier, ice sheet, ice field or any other body of gl |
hill probably stood out above the Usk Valley | glacier ice during the ice age. |
lorations on the flow of streams in Antarctic | glacier ice sheets. |
s that were thrust up by a lobe of Laurentide | glacier ice emanating from the Mackenzie Valley and m |
as indicated by temperature proxies found in | glacier ice, sea bed sediment, tree ring studies or o |
sin is about 855 km²; 31,6 km² are covered in | glacier ice. |
ulation zone is also defined as the part of a | glacier's surface, usually at higher elevations, on w |
d by this sediment can halt a steadily moving | glacier if it interferes with the underlying sediment |
cal party which sledged past the mouth of the | glacier in December 1929. |
everal geographical features, including Guyot | Glacier in Alaska, Mount Guyot in North Carolina, and |
Saskatchewan | Glacier in 2005, showing the path of glacial retreat. |
by the Indian Military to capture the Siachen | Glacier in the disputed Kashmir region, precipitating |
After British exploration of the Gangotri | Glacier in 1933, a German expedition led by R. Schwar |
Bolgrad | Glacier in Sentinel Range, Antarctica is named after |
e and are typically found at a flat area of a | glacier in a region of transverse crevasses. |
originates from a lake formed by the Thamsar | Glacier in higher Dhauladhar range. |
Leverett | Glacier in Antarctica is about 80 km (50 mi) long and |
kilometer island of ice has broken off from a | glacier in Greenland. |
(25 miles) and forming the SW wall of Hammond | Glacier, in the Ford Ranges of Marie Byrd Land. |
kilometers (5.2 mi) in length, is the longest | glacier in Austria and in the Eastern Alps reaching f |
ntain drops 8,000 feet (2440 m) to the Lituya | Glacier in approximately 3 miles (4.8 km), and the so |
Griffith on the ridge at the head of Vaughan | Glacier, in the Hays Mountains of the Queen Maud Moun |
st to Anderson Heights overlooking Shackleton | Glacier in the east. |
first held in front of 1500 attendees at The | Glacier in Mount Pearl. |
ker is a mountain peak located east of Willis | Glacier in the Saint Johns Range, Victoria Land, Anta |
pper Parvati valley from the unexplored Debsa | Glacier in 1992,1993 and 1995.The Debsa Pass(5340 met |
ocated at the northeastern end of the Baltoro | Glacier in the Karakoram range of the Himalaya. |
The Beardmore | Glacier in Antarctica is one of the largest glaciers |
Aerial view of the Beardmore | Glacier in 1956. |
The Somov Sea north of Victoria Land and a | glacier in Queen Maud Land (both East Antarctica) bea |
Aerial view of the Axel Heiberg | Glacier in 1956-57 |
Monte Clapier is home to the southernmost | glacier in the Alps, located on the Italian side at s |
He sets off for the nearby | glacier, intending to kill himself. |
Glacier inventory of Thatte, Saltoro, Sumdo, Fasten N | |
The Gangotri | glacier is a traditional Hindu pilgrimage site. |
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