shelf back - перевод на русский
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shelf back - перевод на русский

PORTION OF A CONTINENT THAT IS SUBMERGED UNDER AN AREA OF RELATIVELY SHALLOW WATER KNOWN AS A SHELF SEA
Shelf break; Continental shelves; Continental Shelf; Shelf sea; Continental shelf break; Coastal Shelf; Outer continental shelf; Inner continental shelf; Mid continental shelf; Mid-continental shelf; Coastal shelf; Continental shelve; Outer shelf; Shelf-ecosystem; Shelf ecosystem
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  • [[Bathymetry]] of the ocean floor showing the continental shelves and [[oceanic plateau]]s (red), the [[mid-ocean ridge]]s (yellow-green) and the [[abyssal plain]]s (blue to purple)}}
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shelf back      
корешок (книги)
off-the-shelf         
WIKIMEDIA DISAMBIGUATION PAGE
Off the shelf (disambiguation); Off the shelf; Off-the-shelf (disambiguation)

[ɔfðə'ʃelf]

общая лексика

готовое к использованию

относится как к ПО, так и к аппаратным средствам, off-the-shelf components - готовые компоненты

нефтегазовая промышленность

имеющийся в наличии

пригодный для использования

готовый к немедленному использованию

прилагательное

общая лексика

имеющийся в наличии

в продаже

стандартный (о запасных частях и т. п.)

пригодный к использованию

без (значительных) изменений (в технике, строительстве и т. п.)

готовый

off-the-shelf         
WIKIMEDIA DISAMBIGUATION PAGE
Off the shelf (disambiguation); Off the shelf; Off-the-shelf (disambiguation)
off-the-shelf adj. готовый; - off-the-shelf items

Определение

off the shelf
not designed or made to order.

Википедия

Continental shelf

A continental shelf is a portion of a continent that is submerged under an area of relatively shallow water, known as a shelf sea. Much of these shelves were exposed by drops in sea level during glacial periods. The shelf surrounding an island is known as an insular shelf.

The continental margin, between the continental shelf and the abyssal plain, comprises a steep continental slope, surrounded by the flatter continental rise, in which sediment from the continent above cascades down the slope and accumulates as a pile of sediment at the base of the slope. Extending as far as 500 km (310 mi) from the slope, it consists of thick sediments deposited by turbidity currents from the shelf and slope. The continental rise's gradient is intermediate between the gradients of the slope and the shelf.

Under the United Nations Convention on the Law of the Sea, the name continental shelf was given a legal definition as the stretch of the seabed adjacent to the shores of a particular country to which it belongs.