Thule Land Bridge

From Wikipedia, the free encyclopedia
Image of the Thule Land Bridge in Context with the North Atlantic

The Thule Land Bridge (also called the Thulean North Atlantic Bridge[1]) was a land bridge, now submerged beneath the Atlantic Ocean, that connected the British Isles to central Greenland.[2] The land bridge appeared during the Late Paleocene and disappeared during the early Eocene. The Thule Land Bridge is theorized to have connected southern Europe to North America by way of the British Isles and Greenland.[3]

References[]

  1. ^ Maria Hlynska, Leroy Leggitt, Alexey A. Kotov (January 2015). "Miocene Cyclopid Copepod from a Saline Paleolake in Mojave, California". www.researchgate.net. Retrieved 18 July 2021.CS1 maint: multiple names: authors list (link)
  2. ^ Maria Hlynska, Leroy Leggitt, Alexey A. Kotov (January 2015). "Miocene Cyclopid Copepod from a Saline Paleolake in Mojave, California". www.researchgate.net. Retrieved 18 July 2021.CS1 maint: multiple names: authors list (link)
  3. ^ Maria Hlynska, Leroy Leggitt, Alexey A. Kotov (January 2015). "Miocene Cyclopid Copepod from a Saline Paleolake in Mojave, California". www.researchgate.net. Retrieved 18 July 2021.CS1 maint: multiple names: authors list (link)


The Paleocene Epoch, the first epoch during the Paleogene Period of the Cenozoic Era.

The Eocene Epoch, the middle epoch during the Paleogene Period of the Cenozoic Era.

Retrieved from ""