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1 slope processes
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2 slope processes
modelé des versants; processus de versant -
3 slope processes
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4 slope
* -
5 slope
pente; versant* -
6 slope
Abhang; Böschung; Hang; Leite* -
7 Hangprozesse
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8 modelado de vertientes
Diccionario geografía española-Inglés > modelado de vertientes
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9 modelé des versants
Dictionnaire français-anglais de géographie > modelé des versants
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10 processus de versant
Dictionnaire français-anglais de géographie > processus de versant
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11 склоновые процессы
Русско-английский географический словарь > склоновые процессы
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12 skråningsprosesser
subst. (geologi) slope processes pl -
13 скала
скала
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
cliff
A steep coastal declivity which may or may not be precipitous, the slope angle being dependent partly on the jointing, bedding and hardness of the materials from which the cliff has been formed, and partly on the erosional processes at work. Where wave attack is dominant the cliff-foot will be rapidly eroded and cliff retreat will take place, especially in unconsolidated materials such as clays, sands, etc., frequently leaving behind an abrasion platform at the foot of the cliff. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > скала
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14 falaise
скала
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
cliff
A steep coastal declivity which may or may not be precipitous, the slope angle being dependent partly on the jointing, bedding and hardness of the materials from which the cliff has been formed, and partly on the erosional processes at work. Where wave attack is dominant the cliff-foot will be rapidly eroded and cliff retreat will take place, especially in unconsolidated materials such as clays, sands, etc., frequently leaving behind an abrasion platform at the foot of the cliff. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Франко-русский словарь нормативно-технической терминологии > falaise
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15 Klippe
скала
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
cliff
A steep coastal declivity which may or may not be precipitous, the slope angle being dependent partly on the jointing, bedding and hardness of the materials from which the cliff has been formed, and partly on the erosional processes at work. Where wave attack is dominant the cliff-foot will be rapidly eroded and cliff retreat will take place, especially in unconsolidated materials such as clays, sands, etc., frequently leaving behind an abrasion platform at the foot of the cliff. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Немецко-русский словарь нормативно-технической терминологии > Klippe
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16 скала
скала
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
cliff
A steep coastal declivity which may or may not be precipitous, the slope angle being dependent partly on the jointing, bedding and hardness of the materials from which the cliff has been formed, and partly on the erosional processes at work. Where wave attack is dominant the cliff-foot will be rapidly eroded and cliff retreat will take place, especially in unconsolidated materials such as clays, sands, etc., frequently leaving behind an abrasion platform at the foot of the cliff. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-английский словарь нормативно-технической терминологии > скала
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17 скала
скала
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
cliff
A steep coastal declivity which may or may not be precipitous, the slope angle being dependent partly on the jointing, bedding and hardness of the materials from which the cliff has been formed, and partly on the erosional processes at work. Where wave attack is dominant the cliff-foot will be rapidly eroded and cliff retreat will take place, especially in unconsolidated materials such as clays, sands, etc., frequently leaving behind an abrasion platform at the foot of the cliff. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-французский словарь нормативно-технической терминологии > скала
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18 cliff
клиф
Отвесный береговой обрыв, образовавшийся в результате абразии.
[ Словарь геологических терминов и понятий. Томский Государственный Университет]Тематики
- геология, геофизика
Обобщающие термины
EN
скала
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
cliff
A steep coastal declivity which may or may not be precipitous, the slope angle being dependent partly on the jointing, bedding and hardness of the materials from which the cliff has been formed, and partly on the erosional processes at work. Where wave attack is dominant the cliff-foot will be rapidly eroded and cliff retreat will take place, especially in unconsolidated materials such as clays, sands, etc., frequently leaving behind an abrasion platform at the foot of the cliff. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Англо-русский словарь нормативно-технической терминологии > cliff
См. также в других словарях:
slope wash — A collective term for non fluvial, incipient alluvial processes (e.g., overland flow, minor rills) that detach, transport, and deposit sediments down hill and mountain slopes. Related sediments (slope alluvium) exhibit nominal sorting or… … Glossary of landform and geologic terms
slope alluvium — Sediment gradually transported down mountain or hill slopes primarily by non channel alluvial processes (i.e., slope wash processes) and characterized by particle sorting. Lateral particle sorting is evident on long slopes. In a profile… … Glossary of landform and geologic terms
slope wash processes — See slope wash … Glossary of landform and geologic terms
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Io (moon) — ] Unlike most satellites in the outer Solar System (which have a thick coating of ice), Io is primarily composed of silicate rock surrounding a molten iron or iron sulfide core. Most of Io s surface is characterized by extensive plains coated… … Wikipedia
Gelifluktion — Gelifluktion[1] (lat. gelare, ‚gefrieren‘ und fluere, ‚fließen‘) bezeichnet langsame Bewegungen von Substrat an Hängen im periglazialen Milieu. Letzteres unterscheidet sie von der Solifluktion, die nicht an dieses Milieu gebunden ist. Allerdings… … Deutsch Wikipedia
