post-glacial rebound oor Spaans
post-glacial rebound
Vertalings in die woordeboek Engels - Spaans
Ajuste postglacial
en
rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period
rebote post-glacial
rebote postglacial
repercusión post-glacial
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Due to steady post-glacial rebound it became connected with the mainland during the early Littorina Sea stage.
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Post-glacial rebound in the Scandinavia region resulted in the formation of the Baltic Sea.
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Because of post-glacial rebound, this island in Lake Mälaren is now connected to the island Ekerö.
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Due to post-glacial rebound, the islands Svartön, Mulön, Granön and Björkön have merged with the island.
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Post-glacial rebound in Scandinavia resulted in the emergence of coastal areas around the Baltic Sea, including much of Finland.
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Though created at shorelines, post-glacial rebound can raise shingle beaches as high as 200 metres (660 ft) above sea level, at the High Coast in Sweden.
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In addition, post-glacial rebound has caused numerous significant changes to coastlines and landscapes over the last several thousand years, and the effects continue to be significant.
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Due to the effects of post-glacial rebound, the whole of Scandinavia started to rise at a considerable rate out of the ocean after the end of the last ice age.
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As post-glacial rebound elevated the southern part of the Canadian Shield more rapidly than the north, the region began to drain northward into the Caniapiscau River, a tributary of the Koksoak River, and ultimately into Ungava Bay.
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The Lapland trade on which Tornio depended started to decline in the 18th century, and the harbour had to be moved downriver twice as a result of the rising of the land (post-glacial rebound), which made the river too shallow for navigation.
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A land bridge can be created by marine regression, in which sea levels fall, exposing shallow, previously submerged sections of continental shelf; or when new land is created by plate tectonics; or occasionally when the sea floor rises due to post-glacial rebound after an ice age.
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Post-glacial rebound - Wikipedia, the free encyclopedia
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coastline has changed considerably in the last millennium due to post-glacial rebound.
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Due to the post-glacial rebound the process is still going on, with new skerries and islands being slowly created and old ones enlarged or merged.
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In practice, it had, however, lost its strategic importance when its access by water gradually failed as the land rose due to the constant post-glacial rebound.
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In practice, however, it had lost its strategic importance when it gradually lost ready access to navigable waters as the land rose owing to the constant post-glacial rebound.
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In practice, however, it had lost its strategic importance when it gradually lost ready access to navigable waters as the land rose owing to the constant post-glacial rebound.
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Parts of Earth’s crust are rising very slowly owing to post-glacial rebound, but using GPS, researchers have found that West Antarctica is rising faster than almost anywhere else in the world.
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Post-glacial rebound (sometimes called continental rebound) is the rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period, through a process known as isostatic depression.
Por costes reales constatados se entenderá los costes reales de las operaciones materiales, contempladas en el anexo V, que se han producido durante el periodo de referencia sobre la base de una facturación individual de dichas operaciones o sobre la base de un contrato firmado al respectoParaCrawl Corpus ParaCrawl Corpus
Long-term effects also include a response from the Earth's crust, due to ice melting and deglaciation, in a process called post-glacial rebound, when land masses are no longer depressed by the weight of ice.
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The current elevation of these terraces depends on the total amount of post-glacial isostatic rebound, which is unknown.
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For example, over the past 100 years, the rate of sea level rise varied from about an increase of 0.36 inches (9.1 mm) per year along the Louisiana Coast (due to land sinking), to a drop of a few inches per decade in parts of Alaska (due to post-glacial rebound).
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22 sinne gevind in 14 ms. Hulle kom uit baie bronne en word nie nagegaan nie.