Land bridge is essentially a historical term; it refers to dry land exposed during periods of low sea level (see regression), connecting what are now separate continents or islands. The best-known is the Bering land bridge, which connected North Asia and Alaska during the last ice age, enabling humans to migrate from Eurasia to the Americas by walking. Another land bridge connected Great Britain to Europe at around the same time. A historic land bridge surviving to the present day is the Sinai, connecting North Africa with Southwest Asia; across this land bridge hominids and humans have migrated out of Africa. A land bridge does not have to be narrow enough to be called an isthmus.
The most recent time of low sea level occurred about 20,000 years ago when worldwide sea levels were about 120 meters below today´s level. Only 10,000 years ago, sea level was still 20 meters below today´s level. Sea level has continued to slowly rise about 1-2 meters in the past 5,000 years.
A land bridge that rose from the sea floor because of upthrust at the edge of a continental plate is Central America. Where the Cocos Plate, an oceanic tectonic plate off the west coast of Central America is being subducted in a convergent boundary under the North American Plate to the north and the South American Plate to the south, first an island arc, and then continuous dry land have been created. 12,000 years ago was when the first humans crossed over to North and South America
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