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1 ледниковый период
1) General subject: Ice Age, boulder period, ice-age, the Ice Age, the glacial era2) Geology: boulder-period, drift epoch, glacial epoch, glacial period3) Construction: ice period4) Mining: Great Ice Age, Pleistocene5) Ecology: glacier period6) Drilling: glacial drift7) Oceanography: glacial age8) Makarov: Cryogenic period, Drift period, ice age (интервал времени в несколько миллионов лет, в течение которого имеет место общее похолодание климата и неоднократные разрастания оледенения - ледниковые эпохи)9) General subject: glacial aftertossing, ice aftertossing -
2 ледниковый период
Русско-английский большой базовый словарь > ледниковый период
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3 ледниковая эпоха
1) Geology: glacial epoch, glacial period, ice age2) Fishery: the Ice Age3) Ecology: glacial phase4) Makarov: drift epoch, glacial age (часть ледникового периода, длительный и непрерывный этап в развитии Земли, характеризующийся сильным похолоданием климата и развитием покровных оледенений в полярных и умеренных широтах), ice period -
4 начальный период
1. initial term2. initial stageледниковый период, ледниковая эпоха — ice age
девон, девонский период — Age of Fishes
Антонимический ряд:Русско-английский большой базовый словарь > начальный период
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5 продолжительность ледового периода
ледниковый период, ледниковая эпоха — ice age
Русско-английский военно-политический словарь > продолжительность ледового периода
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6 на период
1. during the terms of2. for a period3. for the term ofза прошедшие годы; в период между — in the intervening years
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7 отнести
1. take; carry; put; refer to; ascribe2. attribute3. driftотнес; отнесенный — drifted away
4. referСинонимический ряд:1. отложить (глаг.) отложить; отодвинуть; отсрочить2. причислить (глаг.) причесть; причислить -
8 интервал времени внутри ледникового периода
Makarov: time within the Ice AgeУниверсальный русско-английский словарь > интервал времени внутри ледникового периода
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9 интервал времени внутри ледникового периода, разделяющий ледниковые эпохи
Универсальный русско-английский словарь > интервал времени внутри ледникового периода, разделяющий ледниковые эпохи
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10 отнести смещение пластов к ледниковому периоду
General subject: refer an upheaval to the ice ageУниверсальный русско-английский словарь > отнести смещение пластов к ледниковому периоду
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11 отнести смещение платов к ледниковому периоду
General subject: refer an upheaval to the ice ageУниверсальный русско-английский словарь > отнести смещение платов к ледниковому периоду
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12 фауна ледникового периода
Makarov: fauna of the ice AgeУниверсальный русско-английский словарь > фауна ледникового периода
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13 фауна
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14 обмен элементами фауны
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15 фауна
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16 отнести
1. consider (refl.); refer2. considering (refl.); refering -
17 акватическая фауна
Русско-английский военно-политический словарь > акватическая фауна
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18 неритическая фауна
Русско-английский военно-политический словарь > неритическая фауна
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19 фауна
Русско-английский словарь по информационным технологиям > фауна
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20 циркуляция морской воды
циркуляция морской воды
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
sea circulation
Large-scale horizontal water motion within an ocean. The way energy from the sun, stored in the sea, is transported around the world. The currents explain, for example, why the UK has ice-free ports in winter, while St. Petersburg, at the same latitude as the Shetland Islands, needs ice breakers. Evidence is growing that the world's ocean circulation was very different during the last ice age and has changed several times in the distant past, with dramatic effects on climate. The oceans are vital as storehouses, as they absorb more than half the sun's heat reaching the earth. This heat, which is primarily absorbed near the equator is carried around the world and released elsewhere, creating currents which last up to 1.000 years. As the Earth rotates and the wind acts upon the surface, currents carry warm tropical water to the cooler parts of the world. The strength and direction of the currents are affected by landmasses, bottlenecks through narrow straits, and even the shape of the sea-bed. When the warm water reaches polar regions its heat evaporates into the atmosphere, reducing its temperature and increasing its density. When sea-water freezes it leaves salt behind in the unfrozen water and this cold water sinks into the ocean and begins to flow back to the tropics. Eventually it is heated and begins the cycle all over again. (Source: MGH / WRIGHT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Русско-английский словарь нормативно-технической терминологии > циркуляция морской воды
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