「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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