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词汇 example_english_glacial-period
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Examples of glacial period


These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
The abrupt return to base line values of some excursion curves may reflect this glacialperiod and associated nondeposition.
Innumerable boulders, relics of the glacialperiod encumbered the track, the only sound we heard was the croak of the curlew the whistle of the golden plover.
They fear that the beginning of a second glacialperiod is upon them.
From the
Hansard archive

Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
They are important in determining sea level rise since the last glacialperiod.
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Low outcroppings of rock in the mown turf were grooved and scarred by the last glacialperiod.
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Some of the plant species have survived the last glacialperiod by turning into relict organisms.
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During the last glacialperiod, ice enclosed nearly all of these mountains.
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The most important one is believed to be a result of the melting of continental ice sheets at the end of the last glacialperiod.
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After an important retreat, the glacier again advanced 11,000 years ago during the last glacialperiod.
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At the end of the last glacialperiod, the sea level rose, cutting the island off from the mainland.
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It was not, however, covered by ice during the last glacialperiod, which peaked around 20,00022,000 years ago.
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Here the villages are no longer located in the valley floor, but higher up on sunny terraces formed in the glacialperiod.
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The last glacialperiod ended about 10,000 years ago, resulting in the present distribution of ecoregions.
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During the last glacialperiod the region was covered by a large glacier which had little movement because of the flat terrain.
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Because these beetles are normally associated with tree line habitats, their location suggests an altitudinal tree limit during the glacialperiod.
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The story of the novel takes place 80,000 years ago, during the last glacialperiod.
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These wild horses probably moved to the mountains to escape global warming that accompanied the end of the last glacialperiod.
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Thus, the end of the last glacialperiod is not the end of the last ice age.
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After this early maximum, the ice coverage was similar to today until the end of the last glacialperiod.
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As it inhabits the areas covered by ice sheets during the last glacialperiod, the species has been called a glacial relict.
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The boulder field was created about 20,000 years ago during the most recent glacialperiod.
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Lindenhof hill bases on the remains of the last glacialperiod.
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The last glacialperiod of the current ice age ended about 10,000 years ago.
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He maintained that the late glacialperiod was followed by one of exceptional rainfall, for which he proposed the name of pluvial.
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These were common throughout the area after the last glacialperiod, but have vanished with forestation.
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The last glacialperiod ended about 12,000 years ago, before which all but the highest peaks of the park were covered in ice.
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The ancient shoreline of the last glacialperiod is now under approximately 390 feet (120 meters) of water.
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The surface was transformed by ice in the last glacialperiod.
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During the last glacialperiod, lower sea levels and a drier climate revealed a much wider peninsula, largely savanna.
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This would indicate the presence of humans well before the last glacialperiod.
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In the warm period that followed the glacialperiod, vegetation grew on the shores of these waters.
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All glaciers in the park today are said to be remnants of this glacialperiod.
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At the end of the last glacialperiod the continental glaciers were melting to the north.
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At the end of the last glacialperiod the basin filled with meltwater.
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They were formed during the last phase of the glacialperiod and consist predominantly of granite.
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Forests of the glacialperiod were dominated by various spruce species and jack pine; fir was abundant in some locations.
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During the last glacialperiod these formerly free-gas reservoirs likely became trapped as hydrates as atmospheric and subsurface temperatures dropped.
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However, at least two volcanoes predate the last glacialperiod and both are highly eroded.
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The earth is currently in an interglacial, and the last glacialperiod ended about 10,000 years ago.
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The beginning of civilization roughly coincides with the receding of glacial ice following the end of the last glacialperiod.
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It received its name from an eponymous plateau, a moraine of the last glacialperiod.
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This phase of activity began at a time when remnants of glacial ice were still present and continued after the glacialperiod.
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The impact of earlier karstification (solutional erosion) has been eliminated by the last glacialperiod.
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This plant has survived the last glacialperiod as a relict organism.
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During the glacialperiod, glacier formation was accompanied by a lowering in the sea level, which likely helped expose the now submerged continental shelf.
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This deposit formed during the last glacialperiod 14,000 years ago.
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The island was formed by debris and erosion at the end of the last glacialperiod.
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This important ecosphere preserves the area where several ecosystems converge - an event that harkens back to the last glacialperiod.
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The earliest known settlers followed herds of large game to the region during the last glacialperiod.
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After the last glacialperiod, tree species spread to recover the newly exposed land.
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The glacialperiod ice-fields and subsequent large meltwater streams would have made settlement difficult at that time.
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The rebound movements are so slow that the uplift caused by the ending of the last glacialperiod is still continuing.
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This hill is part of the terminal moraine of the last glacialperiod.
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During the last glacialperiod, the region was covered by ice sheets two to three kilometers deep.
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During the last glacialperiod the sea-level has fluctuated 2030 m as water was sequestered, primarily in the northern hemisphere ice sheets.
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On the lake's western shores there are large moraine systems of which the innermost belong to the last glacialperiod.
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The maximum extent of glaciation within this last glacialperiod was approximately 22,000 years ago.
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The surrounding area is characterized by rolling drumlins formed during the last glacialperiod, some of which reach 150 m above sea level.
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Melting ice since the last glacialperiod has resulted in the preservation of a superb raised beach sequence.
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At times of maximum glacial extent during the last glacialperiod the sea level was about 100 m lower compared to today.
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Continuous human habitation dates to around 12,000 years ago, at the end of the last glacialperiod.
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At the end of the glacialperiod there was an ice front here.
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It was formed during the last glacialperiod.
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Southeastern forests of the glacialperiod were dominated by various spruce species and jack pine; fir was abundant in some locations.
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The sand was formed during the last glacialperiod, when large glacial lakes formed and deposited silt.
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Sweetmere is one of many small kettle lakes which formed at the end of the last glacialperiod when the temperatures began to increase.
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During the last glacialperiod, plant and animal species from many different biomes moved into the area.
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The area's lakes, wetlands, and sloughs interspersed with knobby hills are a kettle-and-kame landscape created during the last glacialperiod.
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Wonky holes are located along riverbeds which existed in the last glacialperiod ending about 11,000 years ago.
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Near the end of the last glacialperiod, roughly 10,000 years ago, glaciers began to retreat.
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It probably became extinct during the end of the last glacialperiod.
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Geologic features of the park include remnants of the last glacialperiod, where retreating glaciers left kames, eskers, and kettles.
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However, they all likely formed in the past 10,000 years after the last glacialperiod as evidenced by a small amount of erosion.
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In 1998, the average global aragonite saturation state was 390%, a range commonly experienced since the last glacialperiod and a percentage above which calcification rates plateaued.
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However, the increased rate of carbon dioxide release into the atmosphere by humans may delay the onset of the next glacialperiod until at least 50,000130,000 years from now.
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Parts of this ancestral cone were fragmented and transported by glaciers 14,000 to 18,000 years ago during the last glacialperiod of the current ice age.
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Because this region was likely harsher during the glacialperiod, it is doubtful that an already ill-equipped species would have been able to establish let alone survive.
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An interstadial is a warm period during a glacialperiod of an ice age that is of insufficient duration or intensity to be considered an interglacial.
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The processes as monitored by stable isotopes seem too slow to generate distinct glacial periods.
Due to the favorable climate of the location, people lived there about 50,000 years ago during the last glacialperiod, as burial sites show from this era.
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Due to the enormous amount of water frozen in ice sheets during the last glacialperiod, the sea level was at least 100 m lower than it is today.
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During that last glacialperiod, the sea-level dropped to about 130 m lower than at present as a result of the accumulation of ice in the northern hemisphere.
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An attempt to frame a working hypothesis of the cause of glacial periods on an atmospheric basis.
Their size during the last glacialperiod presumably depended on the relative gain and loss of reproductive capacity in the population of elks during that time.
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These consisting of glacial periods where conditions are colder than normal, separated by interglacial periods.
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All the region has been eroded by glaciers during three glacial periods.
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High contents correspond to warm interglacial periods, and low to glacial periods.
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During the glacial periods there were large drops in sea level, so the coast-line was greatly modified.
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This volcanic event was also followed by a period of erosion, and likely one or more glacial periods.
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North, east and west of the mountain top is in great cirque from that in the glacial periods when glaciers were more extensive than today.
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Outwash from the last of numerous glacial periods left thick glacial deposits of sand and gravel, providing the geologic foundation for globally rare pine barrens.
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These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
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